STUDY OF THE ALBION - SCIPIO FIELD OF MICHIGAN Thesis for the Degree of M. S. MICHIGAN STATE UNIVERSITY WILLIAM CLIFTON BISHOP 1967 - 3 9 M - ” fi 5 . ” . 4 . ; a « . a m l i V 24220-002 I I I I I I I I I IIIII I I II I I I I I I I I I I I I I I I I I I 293 10034 II II I I I?an“F I Mm ”- MSU LIBRARIES ”- RETURNING MATERIALS: Place in book drop to remove this checkout from your record. be charged if book is returned after the date stamped beIow. FINES win N9 1 1 gooififi' ‘ I": W1 Itflflcs>41ng§§3 , 00 A175 h~-v‘>v, JUN 2"7‘7990 ' Igfl'fiflzooo 1 80514380“! STUDY OF THE ALBION - SCIPIO FIELD OF MICHIGAN BY William Clifton Bishop A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Department of Geology I967 ABSTRACT STUDY OF THE ALBION - SCIPIO FIELD OF MICHIGAN by William Clifton Bishop The Albion - Scipio Field of south-central Michigan produces from the Middle Ordovician Trenton - Black River formations. This synclinal field trends in a northwest-southeast direction conforming to the structural grain of the Michigan Basin. Information from radioactivity logs provided data in determining thickness and the structure of formations encountered. Close spacing of wells permitted the correlation of some reservoir characteristics. Discontinuous fracturing of the Trenton - Black River limestones, along lines of pre-existing weakness present in the basement complex, has served as an avenue for solution activity during Devonian time. This solution activity has caused the development of a trough in the Trenton limestone. Oil and gas entrapment are controlled by the degree of fracturing, solution activity, dolomitization, and cross faulting. Similar features may be seen in other Trenton - Black River Fields which may assist in petroleum exploration. Acknowledgments The writer gratefully acknowledges the guidance and patience of Dr. James H. Fisher. The writer also acknowledges the cooperation and assistance of Dr. w. J. Hinze, Dr. A. T. Cross and Dr. J. J. Zinn. Special thanks are due to Garland D. Ellis and the officials of the Michigan Department of Conservation, Geological Survey Division who made this thesis possible by furnishing information and resource data. TABLE OF CONTENTS ABSTRACT ACKNOWLEDGMENTS TABLE OF CONTENTS LIST OF FIGURES AND PLATES INTRODUCTION Location History of the Albion - Scipio Field Production History of the Field Purpose of Investigation Method of Investigation Previous Work TECTONIC FRAMEWORK Description of Tectonic Features and Possible Effects on the Michigan Basin Theories Relating to ”Trent” structures in the Michigan Basin STRATIGRAPHY General Middle Ordovician LOCAL STRUCTURE LOCAL VARIATIONS OF ISOPACH INTERVAL RESERVOIR RELATIONSHIPS FORMATION OF TRAP OTHER TRENTON PRODUCING AREAS CONCLUSIONS REFERENCES APPENDIX Page ii iii iv 20 20 22 28 32 35 39 42 47 48 50 List of Figures — w w b m x c w o o 0 \ Area of Investigation Albion - Scipio Field Trenton - Black River Annual Oil Production Albion - Scipio Field Production Trenton Structure of The Michigan Basin Structural Elements of the Michigan Basin Area Bouguer Gravity Anomaly Map Stratigraphic Chart of Formations Encountered in the Albion - Scipio Field Lithology of The Trenton and Black River Limestones and Areas of Oil and Gas Production from these Rocks l0. Thickness of Trenton and Black River Rocks ll. Contours on Top of Trenton Limestone l2. l3. Synclinal Development Diagrammatic NE - SW Section of Albion - Scipio Field l4. Trenton - Black River Fields Page N ‘ - I - V m I3 14 l8 2] 25 26 27 29 37 44 List of Plates 1. 3 C / (M «L V2// Correlation Chart II. Trenton Structure III. "Clinton” Structure IV. Traverse LS. Structure V. Sunbury Structure VI. Trenton - ”Black River” lsopach VII. ”Clinton” - Trenton lsopach VIII. Niagara - “Clinton” lsopach IX. Salina - Niagara lsopach X. Traverse LS. - Salina lsopach XI. Berea - Bedford - Traverse LS. lsopach INTRODUCTION Location The largest Ordovician petroleum field in Michigan is located in the south central portion of the state. The Albion - Scipio Field, often referred to as simply ”the Trend,ll extends approximately 35 miles in a northwest - southeast direction through Hillsdale, Jackson and Calhoun counties. (Figure l). ”The Trend” includes several linear oil fields with a maximum width of less than one mile. Oil and gas are pro- duced from a dolomitized fracture or fault zone in the Trenton and Black River formations of Middle Ordovician age. The depth of production varies from approximately 3,200 feet in the southeast portion of the field to 4,500 feet in the northwest portion of the field. History of the Albion - Scipio Field Prior to the development of the present ”Trend" discovery well, only a few widely spaced Trenton tests had been drilled. Most of these wells were drilled as a result of gravity surveys; others as hunches or on the sparse subsurface data available (Ives, I960). The Albion Gas Field was discovered in l94l, the gas having been produced from a shallow zone in the Devonian Traverse limestone. The field was developed to four wells and was located over the present deeper Albion - Scipio Field production. An earlier Trenton test (in the Albion Gas Field) had been cored, and showed some fracturing and oil saturation in the dolomitized Trenton formation, but was plugged and abandoned without further testing as a dry hole in the Trenton formation (Ives and Ells, I959). The cumu- lative production of the Albion Gas Field was 6,1]4 MCF of gas before it ——————————————v—_¥ ' -—..-,—.:‘:;_-___‘ .‘_' ~'- “‘_-_—.==4 ' '-'“ .‘-- ~— .— —— _~ \ ‘ \\\\ , \I\ /.// 0 AREA Hills-dale O F 4A _—1 ——— Flgure I INVESTIGATION was abandoned in 1948. The discovery well of the Albion - Scipio Field was drilled in Scipio Township. The location of the well was not based on geology, and was between two gravity highs. According to Ives' (I960) description of the discovery well: I'The test, Perry No. l Houseknecht, NW E, SE %, NE E, Section l0, TSS, R3W, was spudded in May of I955. The top of the Trenton was penetrated at 3,563 feet. The first gas shows were re- corded in September of I956 at a depth of 3,650 feet. It was not until January of the follow- ing year that oil was encountered at a depth of 3,776 feet. The well finally bottomed out at 3,900 feet in July and was completed for flowing I0 barrels of oil per hour." After several off-set wells with similar sizable production had been completed, the field was named after the township of Scipio. With the discovery of the Scipio Field, there was further stimulation of wild- cat drilling in south central Michigan. Twelve miles north of the Scipio Field, in December of I958, the Albion Township discovery was completed which was only a mile and a half from the abandoned Albion Gas Field. The Albion discovery well, Rosenau No. I, at a depth of 4,324 feet, had an initial production of 200 barrels of oil per day. A wildcat well was started in Pulaski Township between Scipio and Albion townships about the same time as the Albion Field discovery well was started. It was not completed until early January of I959, with the first show of gas at the depth of 3,766 feet and the first oil at 3,8l5 feet. The Blair No. I well became the Pulaski Field discovery well with an initial production of 386 barrels of oil per day flowing. The Pulaski Field completed the excellent Iineation of the three fields, Albion - Pulaski - Scipio, into a trend as shown in Figure 2. Further wildcat discoveries and ”on Trend" 34w Raw T IS \ T28 ALBION ‘ W . T38 keuusm T48 AW SCIPIO T158 Figure 2 a? R development merged the three fields and extended the ”Trend” southeast to Adams Township, Hillsdale County in I959 and northwest to Lee Town— ship, Calhoun County in I960. Production History of the Field In Michigan, prior to the discovery of the Albion - Scipio Field in I956, there were five Trenton - Black River Fields, the oldest discovered in l920.. These fields produced approximately a half a million barrels of oil. Figure 3 illustrates annual Trenton - Black River oil production in Michigan. From the discovery of the Albion - Scipio Field to the end of I963, the field has produced over 40 million barrels of oil. Figure 4 summarizes production of the field on an annual basis. Perhaps the most significant Trenton - Black River production is the Lima - Indiana Field located in Ohio and Indiana. A near abandoned field now, it has produced since l884 and cumulative production has been estimated at over 500 million barrels of oil. The wells within the Albion - Scipio Field are located along the dolomitized "fracture trend” and produce from the Trenton limestone and the BlackRiver linestone. The average oil pay is about 60 feet thick, but the production and pay thickness are irregular depending on the pre- sumed degree of fracturing and solution activity. Many extensive lost circulation zones and high gas pressure build-ups are encountered in the Trenton - Black River section and this has made well completions diffi- cult and has added to the difficulty in direct examination of producing horizons. The field has a characteristic gas cap and oil-water inter- face. The following is a short history of pressure declines and the barrels of oil produced per pound of decline between the initial survey and subsequent surveys (obtained from records of the Michigan Geological Survey). R E V I R K C A L B - N O T N E R T N O I T C U D O R P L I O L A U N N A - 2 I . . ” l I L l D L E I F O I P I C S - N O I B L A Y R E V O C S I D s _ — — — — — 4 4 6 2 6 o s 8 5 6 6 4 5 2 3 0 3 a 4 6 4 4 4 2 4 o 4 5 3 6 3 . 4 3 R A E Y 3 e r u g i F " 3 ‘ 6 r o S N O I L L I M . n o r o S L E R R A B W S . N O I T C U D O R P D L E I F O I P I C S - N O I B L A ' 0 4 S N O I L L I M F C M S A G 3 A 6 L A U N N A _ _ _ , s — — - r / / / / / ” O M N I T M « . 0 2 F O S N O I L L I M L I O F O S L E R R A B / I l l ’ I s l l e w : l l e w 9 0 I ’ ’ 6 2 3 6 2 6 I 6 0 6 9 5 8 5 7 ' 5 6 5 4 e r u g i F -2850- Datum Data from Survey to Survey Cumulative from original survey Pressure Oil Production Pressure Oil Production Decline Per. Lbs. Drop Decline Per. Lbs. Drop p.s.i. Barrels p.s.i. Barrels 5/62-IO/62 l0/62-5/63 5/63 -5/64 -5l -52 -79 43,720 57,649 70,636 -4l3 -465 -537 40,900 42,773 47,430 The field is presently prorated at lIO barrels of oil and/or I65 thousand cubic feet of gas per day per well. Oil reserves have been estimated in excess of 5,000 barrels of oil per drilled acre Ives (I959) and as of January I, I964 approximately 9,800 acres had been proven productive. Presently, the Albion - Scipio Field is producing an estimated 60% of the oil and 40% of the gas for the entire state of Michigan. Purpose of Investigation The purpose of this investigation is to attempt to determine the geological causes of oil and gas accumulation in the Albion - Scipio Field. Albion - Scipio is an important oil producing field in the Michigan basin and exhibits many geological problems on which few studies have been presented for the entire field. Method of Investigation Radioactivity logs for 865 wells within the Albion - Scipio Field and adjacent area, were used solely for structural control and formation thickness data (listed in appendix). Gamma ray - neutron logs have been recorded for approximately 95% of the wells drilled in the field area. ID The gamma ray type of mechanical log was used principally for Iithologic definition and correlation for this investigation. The neutron log was used principally for porosity determination. The formations in the Michigan basin are generally an alternating sequence of carbonates, argillaceous carbonates, shales and evaporites, shown in Figure 8. The majority of the formations can be correlated by gamma ray - neutron log characteristics, however, some formation characteristics are not easily identified on either gamma ray or neutron logs. The formations in this investigation that appear in quotation marks are formations that are chosen on radiation characteristics, which may or may not conform to standard formation descriptions. These subsurface formation markers are generally accepted by Michigan geologists but some of these markers can- not be correlated with the regional geology and their use is limited. A gamma ray log cross-section, northwest - southeast, through the Albion - Scipio Field, is shown in Plate I. The eight "type” wells, with an ap- kn ‘Q proximate five mile spacing, are used for correlation only, and because of the relative position of the wells, up or down, the regional dip should not be inferred within the field. Exceptionally dense control for correlation purposes can be obtained due to the 20 acre spacing of wells within the field. A short distance from the field, wildcat drill- ing is very sparse and control becomes deficient in detail. In areas of the field that are regarded as pertinent to this study, Iithologic logs, pressure data and other well records have been examined. Previous Work Many oil companies having an active interest in the Albion - Scipio Field, have initiated detailed investigations and research but none of this information, to the author's knowledge, has been published. Numerous small articles have been published about the trend field. The only sig- nificant investigation is that of Ells (I962), which is a detailed study of three designated areas of the field. Hinze and associates (I962) directed a shallow seismic refraction survey in the vicinity of the Albion - Scipio Field. Other areas of investigation include a one well core analysis by Kirschke (I962) and a multi-well study of the Ordovician rocks in Hillsdale County and adjacent areas by O'Connell (I958). There has been no study published that deals with the Albion - Scipio Field in its entirety with as much control available as in the present investi- gation. TECTONIC FRAMEWORK Description of Tectonic Features and Possible Effects on the Michigan Basin The general characteristics of the Michigan Basin Figures 5 and 6, can be outlined as follows: (I) diameter of approximately 400 miles, (2) near oval shape with a northwest - southeast axis of elongation, (3) in cross section, an asymmetrical basin with a relatively steep north- east slope, (4) deepest portion Of basin has l4,000 to l5,000 feet of Paleozoic sediments, (5) many structural features within the basin have a northwest - southeast trend. There is little agreement on the exact cause and age of the for- mation of the Michigan Basin, but it is generally the opinion that the basin was formed in late Precambrian or Ordovician time, (Pirtle, I932) (Newcombe I934). The Wisconsin Arch, which strikes N 20° N, is believed to be a Precambrian mountain range of the magnitude of the Alps, Alleghenies or Rockies which was base leveled before Paleozoic time (Pirtle, I932) (Lockett, I947). The Kankakee Arch, according to Pirtle (I932), is a relatively smaller uplift which is closely related to the Wisconsin Arch in age. Pirtle (I932) proposes that the Kankakee Arch is a southeast- ward continuation of the Precambrian deformation that formed the Wisconsin Arch. Lockett (I947) does not agree with Pirtle, and proposes that the arches are not related because of difference in elevation of the two arches at their junction. Lockett further proposes that the Kankakee Arch is divided by the Logansport sag, and the eastern portion, referred to as the Wabash spur, might be related to the Cincinnati arch. l2 Figure 5. TRENTON STRUCTURE (PIRTLE,32I Figure 6. STRUCTUAL ELEMENTS OF THE MICHIGAN BASIN AREA (LOCKETT,47) The formation of the Cincinnati Arch began as early as the Lowville stage of Middle Ordovician time, but the northern portion did not de- velop until the Cincinnatian Epoch of Upper Ordovician time. As a result of the Appalachian Orogeny starting to develop in Mississippian time, the Cincinnati Arch becomes a strongly positive feature bringing about a more symmetrical Michigan Basin, (Newcombe, I934). A very early mountain chain that extended from Canada to northwest Ohio was probably an extension of the Cincinnati Arch, and is reflected in the younger sediments as the Findlay Arch and Algonquin axis. The Findlay Arch and Algonquin axis are separated by the Chatham sag, which was formed in post Middle Ordovician time, (Lockett, I947). The Al- gonquin axis, according to Sanford and Quillian (I957), has no relation to the Findlay Arch but is said to be an isolated basement high rather than an extension of the early mountain chain forming the Findlay Arch. The structural features of the Canadian Shield region, together with the major structural features flanking the southern portion of the Michigan Basin, set the geologic framework for the Michigan Basin and to a large extent control the development of smaller structural features and fracture systems within the basin. Theories Relating to ”Trend” Structures in the Michigan ”Basin” As shown in Figure 5, many structural features of the Michigan Basin parallel a northwest - southeast direction. A few of these sub- surface features are 40 to 60 miles long and 200 to 300 feet in relief. Stonger features such as the Howell Anticline have a relief of approxi- mately l,OOO feet. The Albion - Scipio Field parallels this same north- west - southeast direction of deformation that is prominent in the I6 Michigan basin. Many theories have been proposed to eXplain the develop- ment of these structurally aligned features. Prevailing opinion is that the origin of principal structures now existing in later sediments are controlled by intermittent movement along old trends of folding or lines of structural weakness which exist in the basement rocks and are closely related to the early history of the basin itself, (Newcombe, I934) (Pirtle, I932) (Lockett, I947). Causes for the deformation of the Pre- cambrian basement differ widely from: lateral orogenic forces (Pirtle, I932); torsional twisting and tearing (Newcombe, I934); to basin sub- sidence (Lockett, I947). According to Pirtle (I932), the orogenic force that formed the system of Precambrian mountains, presently the Wisconsin and Kankakee Arches, formed the Michigan Basin originally as a part of a long, broad geosyncline paralleling these old mountains. The oblong trend of the basin is more evident Ln older formations while the younger series re- veal a more circular form. The highly folded metamorphic rocks and lines of structural weakness underlying the basin, formed at the time of the geosyncline would closely parallel its axis of elongation. Horizontal compression, active during successive periods of deposition, reflected deformation in accumulating sediments along these old lines of structural weakness and folding. Newcombe (I934) proposed that the Michigan Basin formed prior to Keweenawan time. In post Keweenawan time, an orogenic force from the northeast to easterly direction deformed the basin, resulting in an asymmetrical basin with the steep flank to the northeast. The basin con- tinued to warp downward until Mississippian time. The lateral force of the developing Appalachian crogeny extended as far as the Cincinnati Arch and brought about a more symmetrical basin. This changed the axis of downwarp, and therefore the depocenters are not aligned. The downwarp- ing of the basin, a changing vertical force with horizontal forces ap- plied from diametrically opposite directions, would cause torsion, and shearing would result. The exact movement would probably be a torsional downbending taking place along lines of pre-existing weakness. North- west - southeast trending anticlines in the Michigan Basin that are asymmetrical with a steep or faulted southwest flank would be an example of this type of movement. Lockett (I947) suggests that the general structural features border- ing tne southern part of the Michigan Basin, in Precambrian time, were mountain ranges of a magnitude similar to the Alps, Alleghenies or Rockies. These mountain highs were the original mass to be deposited in the basin and start the downwarping of otherwise positive features. The downwarping continued in the three basins, (Michigan, Illinois and Pittsburgh - Huntington basins) with the increasing accumulation of sediments. The basins were separated only by the positive regional arches. Then this downwarping force separated the Kankakee Arch and Findlay Arch at the shortest distance between the basins and fonmed the Logansport sag and Chatham sag respectively. “The division of the original Kankakee-Wabash axis with the bilateral shift toward each basin is an indication of the extent of the tension stress which accompanied the downwarp of this arch under the weight of accumulated sediments on either side.” (Lockett, I947) The Chatham sag is developed in much the same way. The Michigan Basin and the Pittsburgh - Huntington basin are connected by a syncline. The junction of this syncline, shown in Figure 6 and the Findlay-Algonquin axis, causes a depression of the axis of probably over 2,000 feet. This structural depression referred to as the Chatham sag developed in post Ordovician time. The Chatham sag, because of its magnitude, be- comes the main factor in establishing northwest - southeast structural features. According to Lockett (I947): ”A system of fractures or lines of weakness develop in the basal complex through the unsupported end (Chatham sag area), and parallel with northeast and southwest sides of the basin which remained positive.” Structural features, such as the Howell Anticline, Lockett believes, are not created by orogenic forces when considering their magnitude in re- lation to the basin. An actively forming fold absorbs the lateral pres- sures which caused it; therefore, presumable deformation forces are not transmitted. Lockett (I947) proposes that: ”Michigan lines of structural trends conform to primary fractures thus produced. The basic lines of weakness under the basin may therefore be considered as a result of simple subsidence.” The most recent interpretation of the Michigan Basin basement is based on geophysical studies (Figure 7). Structural trends in the northern part of the basin are north-south rather than northwest- southeast. This was also noted by Newcombe (I934), but explained by differential compaction and subsidence rather than basement structure. According to Hinze (I964), the southeast quarter of the Michigan Basin has been relatively active, structurally. STRATIGRAPHY General The stratigraphy sequence encountered in the Albion - Scipio Field includes rocks of the Cambrian, Ordovician, Silurian, Devonian, Missi- ssippian and Pennsylvanian systems. Figure 8 shows a general strati- graphic section along the Albion - Scipio Field. Variable or average thicknesses recorded in the chart pertain only to the area of investi- gation and do not necessarily apply to the stratigraphic sequence for the Michigan Basin. Generally, most formations dip northward to north- eastward at about 50 feet per mile. Most of the formations increase in thickness northward toward the center of the basin as shown on Plate I. The Niagaran Series is an exception and thins basinward. According to Ells (I962): ”The rocks of Middle and Late Silurian age are of special significance since the for- mer are believed to be a reef and biostrome complex and the latter largely a marine evaporite sequence. The Niagaran Series is thickest in the shelf regions of the basin and thins basinward. The upper part of the Niagaran, sometimes called Guelph - Lockport, has been identified with reef and inter-reef facies of a regional reefal complex which is concentrated around the margins of the Michi- gan Basin." In Lee Township there are at least two Niagaran pinnacle reefs asso- ciated with the field. One reef to the northeast produces oil from a single well and the other pinnacle reef to the southwest produces gas from one well. Southward along the field and toward the shelf region of the basin, 20 sTRATIORARNIO ONART OF EORNATIONO ENcouNTERED IN TNE ALDION-scmo HELD cLATURE "m RRINOIPAL MAIL! LITNDLOOY Thickness REOENT RI_._EIsTOc'ENE' ‘T—DIFT -- _ TSOF—‘J- - NARsNALL as. gflgfifif d— I6O' cOLDwATER sNALE sod-1050' " "SUNI'ORY LK. Iii-56' ' BEREA 33 5 BEDFORD SILTS__TTON 30.40. 6mg -.-I ANTRIN SHALE WO-I ’ T “TRAVERDE ru'.’ sNALE fi-OO' .. Tam“ LINEsTONE DNALrLs.115-2OO , , . 3 5 __L__ LINE CHERTY L3. _ LimmLJic—EE: LUCAS RN. DOLDNITE a 266 300 E O E. g Aw" E z a 5 g E o C H H SHALE m 426'- m AMY D a: _I 9 onum- a < LOW DOLMTE and a g OUNTON DOLOMITE m MES—"m“, 1002-1ij: T A M 3 SNALE sad—330' 5 TRENTON ”9'35“ SMALE DOLONITE §$JTICA m SANDY 8H. FRAIRE Du CHEN BLACK RIVER LinesTDNE zed-36d LINESTOIE 346-366 DOLONITE 60" sANDsTONE " 31'. PETER Bag)? sAN . "' ,0. ,0. FIGURE 8. (M M ”JO.” 22 the lower part of the Salina formation thins, pinches out and rests un- comformably on the Niagara Series, as shown in Plate I. The Late Silurian, Bass Islands formation and the Early Devonian, Bois Blanc for- mation, also thin, pinch out and rest unconformably on the 6- unit of the Salina formation. The first bedrock encountered in drilling is Mississippian in the south part of Albion - Scipio, and Pennsylvanian to the north. Then successively younger and truncated series are en- countered toward the center of the basin. As shown on Plate I, the re- maining formations have relatively continuous and conformable charac- teristics many of which can be correlated on gamma ray logs. Middle Ordovician The oldest rocks penetrated are those of the Lower Ordovician Prairie du Chien group. The members, in ascending order, of this group are the Oneota dolomite, the New Richmond sandstone and the Shakopee dolomite. Overlying the Prairie du Chien group is the Middle Ordovician St. Peter sandstone which is encountered in some wells. The relation- ship between the St. Peter sandstone and the Prairie du Chien Group is unconformable due to pre- St. Peter erosion of the Prairie du Chien group. The St. Peter sandstone is a white to brown, predominantly pure, friable sandstone with fragmental chert and pyrite locally common. The Glenwood shale, overlying the St. Peter sandstone, is a green- gray calcareous shale. The shale is usually sandy and pyritic. The sand grains found within the shale have the general characteristics of the underlying St. Peter sandstone. The Glenwood shale, sometimes re- ferred to as the basal member of the Black River formation, is correlated with the Glenwood of Wisconsin. 23 The Black River formation conformably overlies the Glenwood shale and is principally a brown to gray crystalline limestone containing interbedded dolomite. The Black River limestone is considered to be finer grained and not as fossiliferous as the over—lying Trenton lime- stone (Cohee, I958). The Black River ranges from 230 to 360 feet in thickness. The Trenton and Black River limestones are separated by an argillaceous limestone and shale section. This section,-which is ap- proximately 3 feet thick, is often referred to as the Black River shale and is a characteristic marker bed over a large area. The Trenton limestone lithology is very similar to that of the Black River limestone. The uppermost bed of the Trenton limestone con- sists of about five to ten feet of crystalline dolomite which is charac- teristic of this area. The Trenton is approximately 350 feet in thick- ness with little variation within the area. The Trenton limestone is overlain by the Upper Ordovician, Utica shale which is a thick sequence of gray to black, hard, fissile shale. In the area of south-central Michigan, the Trenton - Black River formations generally consist of limestone and interbedded dolomite, which occurs in different proportions in different areas. Toward the west edge of the basin, as shown in Figure 9, the Trenton - Black River rocks are entirely dolomite. Along the margin of the basin and the Findlay and Kankakee Arches, they are limestone and dolomite. In the central portion of the Michigan basin, the Trenton - Black River rocks are entirely limestone. According to Cohee (I958), the oil and gas pro- duction is almost entirely limited to the area where the Trenton - Black River sequence is dolomite and limestone or is entirely dolomite. 24 The Trenton - Black River sequence thins slightly over the Kankakee and Findlay Arches as shown in Figure l0. The greatest thickness is in the ”thumb” area of Michigan and extends to Ontario, Canada indicating that the Chatham sag probably served as the first connection between the Michigan Basin and the seas to the east. The structure of the Trenton - Black River, as shown in Figure ll, indicates the center of the basin near Clare and Gladwin Counties and Il,OOO feet plus of structural relief. , i W / / / % ‘ 0 ~ \ -§ \ \ \ \ § \ \ \ \ § Q \ W \ \ 2 ; : . . FIGURE '0 THICKNESS OF TRENTON AND BLACK RIVER ROCKS (AFTER ”I! AND IUROESSJOOO) EXPLANATION Thickness interval won. .0 Area of Men and Block Rlver outcrop 11 control point le 9; ‘5’ 3“miles: i0 4 . 6 A . . . . . . . . . . \ . . . . . I I 1 . . . . . . . . . . . . . . m 9 a m . { f o o t - . . . . . . . 0 . 0 O . u i n } . . . . . \ . O O . . . L e . . . - 3 : “ . 0 . 0 m . O . u . e e . . . - o 0 0 “ e n . . . . . . . o . . . 8 M T 0 . . H . 1 . . 0 . . u . e e O . . . 0 0 u e u 0 0 . . . . . . 0 0 s . . . . o n u . m . a t . o fl 0 o 0 u . e . . s . . . . o . . . . 7 O . . l o . . . . O . . . FIGLRE II. CONTOURS ON TOP OF TRENTON LIMESTONE (AFTER CONE “NR“SOJOOO) LOCAL STRUCTURE The formations in the Albion - Scipio Field area generally dip in a north to northeasterly direction. Structure contours on the top of the Trenton limestone, shown in Plate II, illustrate this regional dip. The Trenton limestone is the uppermost producing horizon, and therefore is the lowest unit penetrated generally by wells drilled in the area. Formation data correlated for this plate will be more extensive than the overlying or underlying formations. This is due to the lack of logging of formations other than the producing formation because of economics or lack of interest. Production from the Trenton - Black River is charac- terized by a structural depression or syncline. The depression trends in a northwest - southeast direction and varies in relief from a few feet with an average depth of 30 feet. The synclinal development is asymmetrical (Figure l2). The steep slope is to the northeast, and the gentle slope is to the southwest side of the field. The appearance of the I'anticlinal nose,“ or high, paralleling the northeast side of the field is due to the angle at which the vertical axis of the syncline strikes across the regional dip. This depression or syncline is associ- ated with the production of oil and gas from the fractured Trenton - Black River limestone which is subsequently dolomitized and develops porosity. The depression is strongly developed and continuous in the Trenton limestone except where it is displaced by a fault in Pulaski Township. The writer proposes that this fault is a low magnitude fault which is mainly strike slip with a displacement of approximately one-half mile to the west. The fault presumably dips to the near vertical position with 28 SYNCUNAL DEVELOPMENT WITH LATER TILTING OF FORMATIONS W E FIG” l2. TILTING OF FORMATIONS WITH LATER SYNCLINAL DEVELOPMENT 30 a smaller component of downward movement on the north side of the fault. The dip of the depression increases to the north of the fault and the depression loses definition just north of the fault area. This type of fault, often referred to as a wrench fault has separated the otherwise continuous reservoir and has played an important role in the entrapment of the oil. In the southern portion of the Albion - Scipio Field the syncline becomes poorly defined and discontinuous. A large high area in Adams and Fayette County may have an effect on field development, Plate II. The structure contour map of the ”Clinton” formation as shown in Plate III illustrates a similar syncline development over the Albion - Scipio Field. In many areas the magnitude of the depression is approxi- mately similar to that shown by the Trenton, but generally the depth of the syncline is slightly less. The steep northeast side of the syncline is still present indicating presumably a vertical origin of the syncline after the tilting of the formations. The fault in Pulaski Township is still present. The characteristics of the fault are similar except for a possible decrease in magnitude of vertical displacement. The structur- al high in Adams and Fayette is present on the Clinton map as it was on the Trenton map. In general the structure of the Trenton limestone and the Clinton formation are approximately identical. In the course of the geologic sequence of formation development, the Albion - Scipio syncline would have been subject to sedimentation and-a filling of the syncline. At such time, barring further subsidence the syncline would not appear in later formations and, these formations would be preceeded by thickening in the synclinal area. The structure of the top of the Traverse limestone (Upper Devonian) as shown in 3l Plate IV illustrates this general absence of the Albion - Scipio syn- cline. There are a few remnants of the syncline expressed as local de- pressions in some areas, but generally synclinal trend is no longer present. In Albion Township (T35,R4W,Sec.l4 and IS) the formation of a low relief anticline has developed in contrast to possible syncline develop- ment. The small amount of closure that exists in this area, has pro- duced gas in a dolomitized section of the Traverse limestone. This field, now shown by four abandoned gas wells, was the old Albion Gas Field which was discovered in l94l. The structure of the Sunbury formation, as shown on Plate V, has still fewer remnants of the former synclinal depressions expressed as local structural lows. The structural high of the Albion Gas Field has become a more positive feature in Mississippian time. In summary of local structural conditions in the Albion - Scipio Field, it can be illustrated that the formation of the linear syncline or depression developed after the regional tilting of formations. The structural development was also post-Clinton and pre-Mississippian. During the Mississippian period small local synclines and anticlines de— veloped in this area. LOCAL VARIATIONS 0F ISOPACH INTERVAL Shown in Plate VI is the thickness of the interval from the top of the Trenton limestone to the top of the Black River Shale. This plate illustrates two concepts of major importance to the development of the Albion - Scipio Field. The first concept is that of reservoir fluid relationships which will be reviewed on page 35. The second concept is that of volume reduction due to dolomitization. The Trenton limestone shows a definite thinning over the linear synclinal area. Well penetra- tion is largely controlled by the level of oil in two major reservoirs. Wells penetrating the Black River Shale are located generally in two areas where the oil — gas interface is below the Trenton limestone. The interval in question averages about 350 feet thick and an approximate maximum thinning of 8-9% of this sequence would be needed to produce a syncline of an average depth of 30 feet. The thinning that occurs ranges from 0% to IIZ with an average maximum thinning of approximately 4%. The writer is of the opinion that if this rate of thinning is ex- tended to the entire Trenton - Black River sequence, then the synclinal development is primarily due to solution, dolomitization, volume re- duction, and subsequent thinning. Solutions entering the formation by way of a fracture zone may dis— solve calcium carbonate. If this solution contained a sufficient pro- portion of magnesium ion, dolomite might then be deposited. Even though this takes place molecule by molecule, this mechanism can be used to ex- plain large areas of dolomitization, porosity and large vugs or solution 32 33 cavities lined with dolomite crystals. Therefore the loss of volume and subsequent thinning of the Trenton - Black River formations may be due to solution activity. The top of the Clinton to the top of the Trenton interval is il- lustrated in Plate VII. This interval has local thinning and thickening with no definite pattern associated with possible deposition related to the synclinal depression developed in the Trenton limestone. It was illustrated previously that the Clinton structures are approximately similar to Trenton structures, and the thickness sequence further in- dicates that sedimentation was not influenced by pre-existing structures. The Middle and Late Silurian rocks are believed to be a reef and biostrome complex (Ells, I962). The thickness sequence of the interval from the top of the Niagara to the Clinton is shown on Plate VIII. This illustrates reef and biostrome characteristics as described by Ells. The area covering the largest portion of the Albion - Scipio is believed to be covered by a biostrome complex. In the shelf regions of the basin, probably extending as far as the north portion of Albion Township (T35,R4W), the biostrome complex thickness may vary possibly due to local highs rather than structural lows. In the northern portion of Albion Township the sequence thins abruptly, illustrating the possible basin- ward limits of the biostrome environment. Beyond this area in a basin- ward direction the biostrome conditions change due to water depth and pinnacle reefs develop as illustrated in the extreme north portion of the field. The development of the biostromal covering over an extensive area of the field illustrates no thinning or thickening pattern which can be associated with pre-existing structural high or low areas of the syncline or depressional trough. 34 The deposition of sediments that follows shows that they are largely controlled by pre-existing Niagara biostromal and reef develop- ment. The Salina thickness sequence as shown on Plate IX illustrates local thinning over pre-existing Niagara highs, and local thickening over Niagara lows. ‘ Evidence for the linear synclinal development which is associated with the Albion - Scipio Field is recorded primarily in Devonian time. Plate X illustrates a thickening relation of the interval from the top of the Traverse limestone to the top of the Salina formation, which is definitely related to the synclinal depression associated with the Albion - Scipio Field. Structural activity during the Devonian is also evident in Albion Township with the formation of the small anticlinal structure shown on Plate IV. The lower Mississippian is shown on Plate XI by the thickness in- terval from the top of the Berea-Bedford formation to the top of the Traverse limestone. During this interval there is local thickening of sediments within the syncline and no large area of thickness is indicated which would suggest other than local synclinal developments. In summary of local thickness variation the author proposes that the syncline or depression associated with the Albion - Scipio Field de- veloped primarily in Devonian time. RESERVOIR RELATIONSHIPS The complexity of the relationship of dolomite and limestone in the Albion - Scipio Field has been revealed in detailed studies (O'Connell, I958) (Kirschke, I962) (Asseez, I964). On the whole there is a dis- tinctive increase of dolomite and decrease of limestone within the pro- ducing areas of the field as compared to edge wells of no production where little dolomite is encountered. A detailed study of a non-produc- ing edge well indicates that presumably there is primary dolomite along bedding planes and secondary dolomite associated with fractures at an angle to the bedding planes (Asseez, I964), but apparently not enough for petroleum production. In the field the fractures are generally not of great magnitude and have little displacement. The dolomitizing waters moving into inter- connected fractures have dolomitized the limestone to varying degrees. Porous zones such as fossil zones, originally present in the limestone, have definitely increased the amount of dolomitization activity, and interbedded shales have localized some of the dolomitization. Complete dolomite sections of the Trenton - Black River rock, in the Albion - Scipio Field, are not as numerous as compared to those sections contain- ing limestone and dolomite (Ells and Ives, I964). Apparently, there has not been a development of one major fault break down the length of the field. Had this occurred, one would expect a continuous dolomite zone down the length of such a fracture. A more plausible explanation is that there is a zone of small fractures down the length of the field where dolomitization has varied with the degree of fracturing. The oil and gas production is related mainly to porosity developed 35 36 in dolomite sections. In some sections the dolomite has very little porosity, and as a consequence is barren of oil and gas. The overall porosity of dolomite sections is about five per cent, and the average permeability is between three and four millidarcys; however, this varies greatly with sections that have vugular porosity (Ives, I960). The position of oil-gas interfaces, and water contacts are, at least, at three different levels within the Albion - Scipio Field. Plate VI illustrates two levels of production by the distribution and depth of penetration of wells into the producing horizon. According to Smiley (I964), three levels of production exist in the Albion - Scipio Field. Bottom hole pressure surveys are conducted on three data by the Michigan State Geological Survey. These data are listed as follows: Group No. | (Datum - 2850 feet) includes all of the area south of the center of Pulaski Township. Group No. II (Datum - 3150 feet) includes all of the field area north of the center of Pulaski Township, except Lee Township. Group No. III (Datum - 3820 feet) includes only Lee Township. The positions of these data are illustrated in Figure l3. These data are the closest approximation to the center of oil producing zones. These zones are separated by dry wells penetrating dense limestone sections in the Trenton - Black River rocks. The writer suggests that these production zones are separate reservoirs which are characterized by low pressure pumping wells in the northern area of each reservoir and high pressure flowing wells in the southern portion of each reservoir. 5 3 2 : 0 3 38 Pressure decline curves for each reservoir also show no communication between reservoirs. FORMATION OF TRAP As illustrated in Plates ll through XI, the writer suggests that the main development of the Albion - Scipio Field occurred in Devonian time. The nature of the reservoir rock prior to deformation was a denser, more crystalline limestone with local lenses of shale, fossil zones and interbedded primary dolomite. During Late Silurian or Early Devonian time, a shearing movement of the basement complex along a line of pre- existing weakness produced a long linear fracture zone in the Trenton - Black River limestone. There is little evidence of either vertical or horizontal movement, but horizontal movement is believed to be more likely. The nature of the fracture in the Trenton - Black River is that of a long highly fractured system which fades northward into small dis- continuous fractures. To the south the fracture zone bifurcates and then fades into an irregular pattern. Shortly after the development of the fracture zone its continuity was broken by an east-west wrench fault in Pulaski Township. The north side of the east-west fault develops fracturing due to downward movement, and possibly the opposite side was stationary which thus escaped fracturing. Dolotimization of the Trenton - Black River rocks took place during Devonian time. The resulting dolomitization produced porosity of vary- ing degrees, and is controlled by the extent of connecting fractures and porous zones present in the rock. By the process of solution activity, the Trenton - Black River rocks thinned and this was a major factor in the development of the narrow linear synclinal depression. This de- pression has a vertical axis of downward movement, and when imposed on 39 40 the tilted formations will have a steep northeast slope. In cross section, this development was not uniform for the entire area, but de- pended on the relative amount of solution activity, dolomitization, and subsequent volume reduction. Dolomitization occurred in an east-west direction on the down-thrown side of the Pulaski Township fault. This later formed a favorable trap for fluids. This type of Trenton - Black River entrapment can be seen in the Dover Field of Canada and in the Bowling Green fault area of the Lima - Indiana Field. The down-thrown side of both of these areas has developed porosity in a similar manner, whereas the up thrown side is void of porosity if structures were not present before faulting occurred. Oil migration into the trap is believed to be either a lateral or an ascending migration. A downward migration has been proposed with the source rock as the Utica shale, however, the Trenton limestone charac- teristically has a non-porous crystalline dolomite surface underlying the Utica shale and seemingly there would be little migration of fluids along this surface. The Trenton - Black River rocks contain organic material of sufficient amounts to warrant it as a source rock with dateral migration of fluids along porous zones into the trap. One well, not directly associated with the field (T45, R3w, Sec.28, SE SE NE) produced 40 barrels of oil per day from below the Glenwood formation. It would seem apparent that the source rock could exist be- low the Trenton - Black River rocks and that the oil has migrated from the lower source rocks up into the reservoir rocks. The result of the loss of volume of the Trenton - Black River for- mation is expressed in the overlying formations as a settling effect in- to a forming low or linear depression. The formations above will reflect 4l this same linear depression with no thickening but during Devonian time the linear depression was filled with sediments and therefore is not present in Mississippian time. The axis of this syncline or depression is vertical from the Trenton formation to the Clinton formation, however, this may be obscured upward from the Clinton formation by the Niagara and Salina sequence as proposed by Ells (l962). Other limestone formations occurring within the Albion - Scipio fracture zone may undergo the same development as outlined above, and may accentuate the depression either below or above the Trenton - Black River formation. The Albion Gas Field located above the Albion - Scipio Field may be evidence of a similar fracture zone located in the same structurally weak area. The extension of fracture zones in portions of the Albion - Scipio Field are still to be developed by drilling. Isolated fractures may still exist in the northern portion of the field. The connections of isolated production zones to the main oil pool are presently being de- veloped. East-west extensions along the Albion - Scipio Field should be limited to the erratically fractured southern portion of the field. Exploration for fields similar to the Albion - Scipio Field is very difficult. The presence of glacial drift complicates geophysical ex- ploration and low linear relief features add to the difficulty of geo- logic exploration. In the Michigan Basin other lines of structural weakness must exist. Movement along these lines may produce similar fields to the Albion - Scipio "Trend” and would suggest that they would parallel this prominent northwest-southeast direction characteristic in the Michigan Basin. OTHER TRENTON PRODUCING AREAS Michigan Trenton - Black River oil fields are distributed to the southern portion of the state. These fields are listed in Table l, (and shown in Figure l4) which lists the fields by date of discovery, and shows relative importance of production. Such fields as Sumpter, New Boston, Springport, and Tekonsha are one and two well fields of which little can be determined other than that they have production of little significance from locally dolomitized portions of Trenton lime- stone. The Northville, and Freedom Fields, shown in Figure I4,_produce.from the flanks of northwest-southeast trending anticlines. In the North- ville Field, the discovery well produces 80% of the total production from the northeast flank of an anticline. This anticline appears to be directly associated with the Howell Anticline. The Freedom Field is located on the west flank of an anticline that is possibly associated with the Lucas Monocline. The Deerfield Field in Monroe County was discovered in I920, but was not actively developed until I937. The field still produces today with 22 active wells. Porous zones in the dolomitized portion of the Trenton limestone are located on the western flank of the northwest- southeast Deerfield Anticline which is associated with the Lucas Mono- cline. The Hanover Field, (T45, RZW), discovered in I959, originally as a gas field which later unexpectedly changed to an oil field after sizable production of gas was drawn off. This field is close to the Albion - 42 43 Table I. SUMMARY OF MICHIGAN'S TRENTON OIL FIELDS* FIELD DISC. -ABAND. NO.WELLS CUMM.O|L.PROD. Deerfield Sumpter I920 I94I 47 2 New Boston I943 I949 Freedom I954 I956 Northville I954 Albion-Scipio I957 Hanover I959 Tekonsha I959 - I963 Springport I960 673,647 (bbls) 7 2,349 7,217 548,479 40,687,406 384,97I 2,698 488 * Obtained from the Annual Statistical Summary of Michigan's Oil and Gas Fields, I963; Geological Survey, Michigan Department of Conservation. Figure I4. TRENTON-BLACK RIVER FIELDS 45 Scipio Field, T45, RZW), and because it appears to be of similar type, northwest-southeast structure may be associated directly with the de- formation of the Albion - Scipio Field. The Hanover Field is in the active drilling state of development which when completed will possibly show a relationship to the Albion - Scipio Field. The Dover and Colchester Fields of Ontario, Canada have features similar to those of the Michigan, Albion - Scipio Field. The Colchester Field although north-south trending, has the same syncline development in the Trenton limestone with associated dolomitization, as does the Albion - Scipio Field (Burgess, I962). The Colchester Field, discovered in I959, and developed to six producing wells (I960), is a small struc- ture, but nevertheless has developed apparently in a similar manner as the Albion - Scipio Field. The east-west trending Dover Field has de- veloped porosity on the fractured dolomitized down-thrown side of a fault. This field produces oil and gas and was discovered in I9l7. Similarities may be seen in this field, the Bowling Green fault area of the Lima - Indiana Field, and the fault in Pulaski Township of the AI- bion - Scipio Field. In each case production is developed on the frac- tured down-thrown side of the fault. The oldest Trenton oil field is the Lima - Indiana Field. Dis- covered in I884, it once produced 80% of the nations oil. The Lima - Indiana Field is a collective name for many small oil fields located in Ohio, and Indiana on the northern flank of the Findlay Arch. These fields are associated with three types of structures. In the Bowling Green Fault porosity is developed on the down thrown side of the faulted Trenton by fracturing and subsequent dolomitization. Porosity is also developed in low structure anticlines that occur basinward from the 46 flank of the Findlay Arch. Oil entrapment occurs in crests of anti- clines and monoclines paralleling the flank of the Findlay Arch. In the southern portion of the Findlay Arch, gas and some small amounts of oil collected in the crest of the low domed Cincinnati Arch. All of the previously mentioned Trenton - Black River formation oil fields have the characteristics of porosity with dolomitization that is in various ways structurally controlled. CONCLUSIONS The Albion - Scipio Field, Michigan's largest single oil producing field, exhibits a northwest-southeast trending syncline developed on the Middle Ordovician Trenton limestone. This northwest plunging syncline has approximately 30 feet of relief, and is directly associated with fracturing, solution activity, dolomitization, and the development of a porosity oil trap in the Trenton - Black River limestones. The Albion - Scipio Field was formed in Devonian time by a movement along lines of pre-existing weakness in the basement complex. The movement was re- flected in the tilted Trenton - Black River limestones not as a single continuous fracture but as a system of fractures trending northwest- southeast. These fractures served as a channel way for solutions that dissolved the calcium carbonate and provided sufficient additional mag- nesium ions to make possible the precipitation of dolomite. This solu- tion activity created an approximate 8-9% loss of volume of the Trenton - Black River limestone which created the subsidence in the Trenton - Black River formations. Devonian sedimentation filled the subsiding depression and it was no longer present after Devonian time. Oil migrated laterally from the Trenton - Black River formations into separate step leveled pools caused by a cross fault and forming the present Albion - Scipio Field. 47 REFERENCES Asseez, Olayinka L., I964, A Chemical and Petrographic Analysis of Wooden No. 6 Well; Middle Ordovician From Hillsdale County, Michigan. ‘Unpublished Master's Thesis, Michigan State University. Burgess, R. J., I960, Oil in Trenton Syncline. The Oil and Gas Journal, Vol. 58, No. 33, August l5, I959, pp. l24-I3l. Carman, Ernest J. and Stout, Wilber, I934, Relationship of Accumulation of Oil to Structure and Porosity in the Lima - Indiana Field. Problems of Petroleum Geology, Am. Assoc. Petroleum Geologists, pp. 52l-529. Cohee, G. V., I947, Cambrian and Ordovician Rocks in the Michigan Basin and Adjoining Areas. Am. Assoc. Petroleum Geologists, Vol. 32, p. I4I7. , and Landes, K. K., I955, Oil in the Michjgan Basin. Habitat of Oil, A Symposium; Am. Assoc. of Petroleum Geologists, I958, Tulsa, Oklahoma. Ells, Garland D., I962, Structures Associated with the Albion - Scipio Oil Field Trend. Michigan Dept. of Conservation, Geological Survey Division. , and Ives, Robert E., I959, South Michigan's Oil Bonanza. World Oil, October I959, pp. l36-l40. Hamil, D. F., l96I, A Detailed Chemical Analysis For Calcium and Magnesium of the Sun Oil Company_Peterson-Howard Well #1 Core Sample. Unpublished Master's Thesis, Michigan State University. Hinze, W. J., Secor, G. B. and Merritt, D. W., I962, A Shallow Seismic Refraction Survey in the Vicinity of the Albion - Scipio - Pulaski Oil Fields, Michigan. Michigan State University, Dept. of Geology. Hussey, Russell C., I952, The Middle and Upper Ordovician Rocks of Michigan. State of Michigan, Dept. of Conservation, Geological Survey Division, Publication 46, Geological Series 39. Ives, Robert E., I960, Trenton - Black River Formation Development in Michigan. The Interstate Oil Compact Commission Committee Bulletin, Vol. II, No. I, June I960, pp. 79-86. Kirschke, W. H., I96l, A Petrographic Analysis of the Peterson-Howard Well No. l Core Jackson County, Michigan. Unpublished Master's Thesis, Michigan State University. 48 49 Landes, K. K., I946, Porosity Through Dolomitization. Am. Assoc. Petroleum Geologists, Vol. 3], pt. I, pp. 305-3I8 Lockett, J. R., I947, Development of Structures in Basin Areas of Northeastern United States. Am. Assoc. Petroleum Geologists, Vol. 3l, pp. 429-446. Newcombe, Robert B., I932, Oil and Gas Fields of Michigan, State of Michigan, Dept. of Conservation, Geological Survey Division, Publication 38, Geological Series 32. , I934, Structure and Accumulation in the Michigan ”Basin” and its Relation to the Cincinnati Arch. Problems of Petroleum Geology, Am. Assoc. Petroleum Geologists, pp. 53I-556. O'Connell, J. F., I958, Study of Ordovician Rocks from DeeereIIs in in the Hillsdale, Northville and Adjacent Areas in Southeast Michigan. Unpublished Master's Thesis, Michigan State University. Pirtle, G. W., I932, Michigan Structural Basin and its Relationship to Surrounding Areas. Am. Assoc. Petroleum Geologists, Vol. I6 Pt. I, ppffil43-l52. Price, L. W., et al, (Compilers), I957-l963, Michigan's Oil and Gas Field, Annual Statistical Summary. State of Michigan. Dept- of Conservation, Geological Survey Division. Sanford, B. V. and Howie, W. C., I956, ”Eastern Canada.‘I Symposium, Sobre Yacimientos De Petroleo Y Gas, XX Congreso Geolo'Gico Internacional. APPENDIX Well Locations and Formation Tops 50 SI Well Locations and Formation Tops All wells are listed in the order of Township, Range, Section, and State Permit Number. Formation Tops are recorded in feet with respect to sea level. Abbreviations SB... ............. . ................. Sunbury formation BB .................................. Berea-Bedford formation TL .................................. Traverse limestone SL .................................. Salina formation (G-Unit) NG. ................................. Niagara formation CL .................................. ”Clinton" formation TR .................................. Trenton formation- BR .................................. "Black River Shale” GW ............ . ..................... Glenwood formation 5 9 9 3 - 1 0 7 3 - 5 2 3 3 - 1 9 5 2 - 0 9 2 2 - 2 1 6 1 - 2 5 8 - 6 4 5 - 2 3 5 - 0 8 3 2 2 E S W S 5 1 . C E S 0 3 9 3 - 7 8 6 8 4 1 3 3 - 5 7 5 2 - 6 2 3 2 - 9 8 5 1 - 0 4 5 - 5 2 5 - 8 7 5 2 2 W S W S E S 5 I . C E S 3 9 9 3 - 9 9 6 3 - h e 3 3 - 0 9 5 2 - 3 4 2 2 - 8 7 5 1 - 0 5 8 - 4 4 5 - 0 3 5 - 7 0 2 3 2 W S E S E S 5 1 . C E S 3 2 7 3 - 8 4 3 3 - 8 0 6 2 - 4 1 3 2 - 3 4 5 1 ~ 7 6 8 ~ 2 7 7 1 2 E N W S W S 6 1 . C E S 9 h 9 3 - 8 0 7 3 - 8 3 3 3 - 7 9 5 2 - 4 9 2 2 - 7 4 5 1 - 8 5 8 - 4 4 5 - 1 3 5 - 7 3 6 3 2 E S 6 1 . C E S 8 0 9 3 - 5 6 6 3 - 8 8 2 3 - 7 4 5 2 - 3 6 2 2 - 0 0 6 1 - 1 4 8 - 7 3 5 - 4 2 5 - 8 0 1 2 2 E S E S 2 2 . C E S 0 2 7 3 - 6 9 3 3 - 6 1 6 2 - 2 8 1 2 - 7 9 5 1 ~ 9 5 8 ~ 0 5 5 - 6 3 5 - 3 6 1 5 2 E S E N W N 6 1 . C E S 2 2 7 3 - 1 5 3 3 - 6 1 6 2 - 1 4 3 2 - 4 3 6 1 - 1 8 8 - 9 6 5 - 3 5 5 - 2 8 9 4 2 E N E N E N 7 I . C E S 9 3 3 2 - 6 6 6 1 - 0 9 8 - 7 8 5 ~ 2 7 5 - 1 7 7 3 2 E N 3 1 . C E S 9 4 3 2 - h 3 6 l - 0 7 8 - 1 7 5 - 8 5 5 - 5 7 8 4 2 E S E N 3 I . C E S 0 6 6 3 - 3 8 2 3 - 2 4 5 2 - 6 5 2 2 - 5 7 5 1 - 6 3 8 - 3 3 5 ~ 9 1 5 - 3 4 3 2 2 E S E S E S 2 2 . C E S 1 6 6 3 - 6 8 2 3 - 6 9 5 2 - 6 6 2 2 - 7 7 5 1 ~ 1 4 8 - 7 3 5 - 3 2 5 - 6 2 5 2 2 E S E S 2 2 . C E S 4 5 6 3 - 6 7 2 3 - 5 4 5 2 - 0 5 2 2 - 5 5 5 1 ~ 0 3 8 - 6 2 5 - 3 1 5 - 3 2 6 2 2 E S W S . C E S 8 6 6 3 - 2 9 2 3 - 0 6 5 2 - 5 2 1 2 - 8 5 5 1 - 0 3 8 - 9 2 5 - 6 1 5 - 6 2 7 2 2 E S E N E S 2 2 . C E S 4 5 6 3 - 7 7 2 3 - 6 3 5 2 ~ 4 3 2 2 - 2 5 5 1 - 9 2 8 - 5 2 5 ~ 2 1 5 - 7 2 7 2 2 E S W S E S 2 2 . C E S 5 6 6 3 - 9 8 2 3 - 7 4 5 2 - 6 6 2 2 - 1 8 5 1 - 1 4 8 - 7 3 5 - 4 2 5 - 8 9 7 2 2 E S W N E S . C E S R B R T L C O N L S L T B B B S T I M R E P E T A T S N O I T A C O L 1 3 6 3 - 5 5 2 3 - 1 0 5 2 - 7 4 1 2 - 1 6 5 1 - 6 8 2 2 - 4 1 6 1 - 0 7 8 - 1 7 5 - 7 5 5 - 5 9 8 1 2 1 2 0 3 2 W S E S 2 3 . C E S w h R S I T E N E S 3 1 . C E S w 5 R S I T 2 3 9 3 - 8 8 6 3 - 0 1 3 3 - 0 7 5 2 - 6 9 2 2 - 3 1 6 1 - 5 4 8 - 1 4 5 - 9 2 5 - 3 0 9 2 2 W S 3 2 . C E S 0 5 6 3 - 4 7 2 3 - 7 4 5 2 - 5 9 0 2 - 1 7 4 1 - 0 2 8 - 5 1 5 - 2 0 5 - 8 7 2 4 2 W S W N E S 2 2 . C E S 3 9 8 3 - 8 4 6 3 — 3 7 2 3 - 2 3 5 2 - 6 7 2 2 - 0 8 4 1 - 3 1 8 - 1 1 5 - 8 9 4 - 3 8 3 2 2 E S 6 2 . C E S 2 0 9 3 - 6 5 6 3 - 1 8 2 3 - 1 4 5 2 - 6 9 2 2 - 1 8 5 1 - 8 2 8 - 5 2 5 ~ 3 1 5 - 6 8 3 2 2 E N E S 6 2 . C E S 0 9 8 3 - 6 4 6 3 - 8 6 2 3 - 0 3 5 2 - 2 6 2 2 - 3 5 4 1 - 1 0 8 - 0 0 5 - 6 8 4 - 0 4 4 2 2 W S E S W N 6 2 . C E S 9 5 6 3 ~ 4 8 2 3 - 9 4 5 2 - 4 8 2 2 - 2 5 5 1 - 1 2 8 - 0 2 5 - 6 0 5 - 0 5 4 2 2 W N E S 6 2 . C E S 7 9 8 3 - 3 5 6 3 - 5 7 2 3 - 7 3 5 2 ~ 9 8 2 2 - 6 6 4 1 - 6 0 8 - 1 9 4 - 3 8 7 2 2 W N W S E S 6 2 . C E S 1 8 8 3 - 5 3 6 3 - 9 5 2 3 - 6 1 5 2 - 7 3 2 2 - 3 6 4 i - 2 0 8 - 9 9 4 - 7 8 4 - 0 2 0 3 2 E S W S 6 2 . C E S 2 9 8 3 - 4 4 6 3 - 9 6 2 3 ~ 8 2 5 2 - 7 6 2 2 - 5 7 4 1 - 7 0 8 - 5 0 5 ~ 1 9 4 - 2 3 2 3 2 4 8 8 3 - 9 3 6 3 ~ 2 6 2 3 - 1 2 5 2 - 5 7 1 2 - 5 4 5 1 - 5 0 5 ~ 3 9 4 ~ 6 9 8 3 2 5 4 6 3 - 1 7 2 3 - l 3 5 2 ~ 6 7 2 2 - 8 7 4 1 - 0 1 8 - 6 0 5 - 6 9 4 - 5 8 9 4 2 E S E S E S 5% 5% 6 2 . C E S 6 2 . C E S 6 2 . C E S 5 5 6 3 - 1 8 2 3 - 0 4 5 2 - 3 8 2 2 - 3 5 5 1 - 9 1 8 - 2 1 5 - 4 0 5 - 6 8 0 5 2 W N E S 6 2 . C E S 9 6 6 3 - 2 9 2 3 - 3 5 5 2 - 3 5 2 2 - 6 7 5 1 - 3 3 8 - I 3 5 - 8 1 5 - 1 5 8 3 2 W S W S 3 2 . C E S 6 8 6 3 - 9 0 3 3 - 5 6 5 2 ~ 7 1 3 2 - 0 1 6 1 - 1 4 8 - 9 3 5 - 5 2 5 - 7 2 6 1 2 W S W S 4 2 . C E S 4 5 6 3 - 8 7 2 3 - 8 3 5 2 - 3 5 2 2 - 7 3 5 1 - 1 3 8 - 4 2 5 - 0 1 5 - 9 4 9 2 2 W S E N E S 2 2 . C E S 7 “ 6 3 - 0 7 2 3 - 3 4 5 2 - 7 2 5 1 - 7 2 8 - 3 2 5 - 8 0 5 - 9 7 7 3 2 W S E S 2 2 . C E S 1 9 2 2 - 0 9 5 1 - 0 5 8 - 2 4 5 - 8 2 5 - 9 0 0 4 2 W N E N E S 2 2 . C E S 7 6 6 3 - 9 9 2 3 - 3 5 5 2 - 2 7 5 1 - E S R T L S L T L C G N G R B B B B S 8 3 8 - " 8 5 2 2 - W S N O I T A C O L 4 9 8 2 2 T I M R E P E T A T S 2 2 . C E 9 4 7 3 ~ 5 0 5 3 - 0 3 1 3 - 2 7 3 2 - 5 6 0 2 - 5 4 5 1 - 4 9 6 - 8 9 3 - 5 8 3 - 4 6 0 3 2 E S E S E S 8 1 . C E S 4 1 5 3 - 9 3 1 3 - 1 7 3 2 - 7 6 0 2 - 9 4 5 1 - 1 1 4 - 8 9 3 - 6 4 4 4 2 4 / w W N % 3 C 8 I . C E S 1 2 1 3 - 2 6 3 2 - 7 3 0 2 ~ 2 4 5 1 - 6 9 6 - 1 0 4 - 6 8 3 - 2 9 0 4 2 4 / W S r o C 8 1 . C E S 2 9 4 3 - 3 4 1 3 - 3 7 3 2 ~ 3 7 0 2 - 9 5 5 1 ~ 5 0 7 - 8 0 4 - 7 9 3 - 2 9 5 2 2 E S W N W N 8 1 . C E S 8 0 5 3 - 4 3 1 3 - 8 6 3 2 - 7 6 0 2 - 2 5 5 1 - 2 0 7 - 6 0 4 - 4 9 3 - 5 8 7 2 2 w s i N C 8 1 . C E S 7 2 1 3 - 3 6 3 2 - 6 4 0 2 - 2 3 5 1 - 6 8 6 - 5 0 2 2 2 E N E N d M 9 1 . C E S 0 1 1 3 - 5 5 3 2 - 7 3 0 2 - 9 4 5 1 - 9 8 6 - 4 9 3 - 1 8 3 - 3 7 4 2 2 E N E S M M 9 I . C E S 6 3 1 3 ~ 6 7 3 2 ~ 5 6 0 2 - 1 5 5 1 ~ 3 0 7 - ' 5 1 8 2 2 E N E N E S 9 I . C E S 5 2 7 3 - 9 7 4 3 - 6 0 1 3 - 1 5 3 2 - 0 4 0 2 - 4 2 5 1 - 8 9 6 - 7 5 7 3 2 E S E N E S 9 1 . C E S 6 4 7 3 - 3 0 5 3 ~ 8 2 1 3 - 6 7 3 2 - 1 5 0 2 - 3 4 5 1 - 7 9 6 - 2 0 4 - 0 9 3 - 3 9 8 2 2 M N W S M N 0 2 . C E S 8 9 4 3 - 5 2 1 3 - 8 6 3 2 - 2 8 0 2 - 9 3 5 1 - 4 9 3 - 7 7 3 - 6 7 6 1 2 W N W N M N 0 2 . C E S 1 9 4 3 - 5 1 1 3 - 6 5 3 2 - 0 5 0 2 - 4 5 5 1 - 4 9 6 - 7 9 3 - 5 2 1 3 - 8 6 3 2 - 7 6 0 2 - 0 5 5 1 - 9 9 6 - 9 9 3 - 7 8 3 - 4 8 3 - 9 6 2 4 2 W N W S E S 0 2 . C E S 2 0 4 4 2 W S E N 0 2 . C E S 9 1 1 3 - 1 6 3 2 - 0 7 0 2 - 4 6 5 1 - 6 9 6 - 8 9 3 - 3 8 3 4 2 8 9 3 2 W N E S W N 0 2 . C E S R B R T L C O N L S L T B B B S T I M R E P E T A T S N O I T A C O L S I ' 8 3 - 0 0 6 3 - 3 2 2 3 - 6 7 4 2 - 9 0 2 2 - 8 8 5 1 - 7 0 8 3 ~ 2 6 5 3 - 7 8 1 3 - 5 2 4 2 - 4 4 1 2 - 9 0 6 1 - 0 9 7 - 0 5 7 - 5 8 4 - 2 7 4 - 5 3 8 2 2 E S E S W N 5 3 . C E S 9 2 1 3 - 3 6 3 2 - 0 6 0 2 - 2 4 5 1 - 2 9 6 - 7 9 3 - 5 8 3 - 3 3 1 3 - 1 7 3 2 - 8 6 0 2 - 9 4 5 1 ~ 9 9 6 - 3 0 4 - 2 9 3 - 3 5 5 3 2 2 1 4 2 2 7 2 5 2 2 E S w s E S 8 1 . C E S E S w s W N 8 I . C E S W N % 5 C 7 . C E S w 4 R 5 2 T 9 0 7 3 - 3 6 4 3 - 6 8 0 3 - 9 1 3 2 - 3 4 0 2 - 7 9 4 1 ~ 5 8 4 3 ~ 8 0 1 3 - 0 5 3 2 - 9 4 0 2 - 6 3 5 1 - 8 0 5 3 - 1 3 1 3 - 1 8 3 2 - 4 5 0 2 - 3 5 5 1 ~ 3 3 0 5 2 6 9 0 5 2 8 3 4 3 2 7 7 4 3 ~ 2 0 1 3 - 0 4 3 2 - 2 5 0 2 - 5 2 5 1 ~ 2 9 3 ' 8 7 3 - 8 2 7 4 2 W S E S 0 2 . C E S 0 2 . C E S E N W S 0 2 . C E S W S E S E S 1 2 . C E S R B L C G M L S B B B S T I M R E P E T A T S N O I T A C O L 6 1 1 3 - 8 5 3 2 - 1 5 0 2 - 9 4 5 1 - 3 7 4 4 2 E S E S 0 2 . C E S 7 8 6 3 - 0 4 4 3 - 6 6 0 3 - 6 0 3 2 - 6 0 0 2 - 1 9 4 1 - 7 7 6 - 3 8 3 - 7 6 3 - 3 3 0 3 2 E S E N E S 9 2 . C E S 1 4 4 3 - 4 6 0 3 - 5 9 2 2 - 0 0 0 2 - 9 8 3 1 - 4 9 3 - 6 7 3 - 7 1 7 1 2 E S E S E S 7 2 . C E S 4 3 4 3 - 0 6 0 3 - 7 0 3 2 - 4 0 0 2 - 0 8 4 1 - 9 6 6 - 6 7 3 - 0 6 3 - 4 8 5 2 2 E S - E S 9 2 . C E S 4 6 0 3 - 2 0 3 2 - 0 0 0 2 - 5 6 4 1 - 0 8 6 - 5 8 3 ~ 9 6 3 ~ 2 3 0 3 2 W S W S E S 8 2 . C E S 3 I ” 3 - 2 4 0 3 - 3 8 2 2 - 0 0 0 2 - 6 6 4 1 - 1 7 6 - 6 7 3 - 0 6 3 - 0 0 2 2 E N 2 3 . C E S 8 1 4 3 - 5 ' I ' 0 3 - 0 9 2 2 - 6 0 0 2 - 5 4 4 1 - 8 7 6 - 4 8 3 - 6 6 3 - 4 6 9 1 2 W N E N E S 3 3 . C E S 3 1 0 3 - 3 5 2 2 - 2 6 9 l - 7 8 3 1 - 1 7 6 - 3 7 3 - 6 5 3 ~ 4 5 7 2 2 E S E N E S 2 3 . C E S 1 4 0 3 - 6 8 2 2 - 7 8 9 1 - 1 4 4 1 - 7 8 6 - 7 7 3 - 0 6 3 - 3 9 2 2 2 E S W S E S 3 3 . ¢ 5 5 0 5 0 3 - 7 8 2 2 - 3 0 0 2 - 4 5 4 1 - 2 8 6 - 7 7 3 - 0 6 3 - 4 8 3 2 2 E S E S 3 3 - C E S 1 4 0 3 - 9 7 2 2 ~ 6 9 9 1 - - - 0 5 4 l - 6 8 6 - 9 7 3 - 1 6 3 - 8 4 5 2 2 E S E S 3 3 . C E S 9 4 o 3 - 9 8 2 2 - 6 0 0 2 - 7 3 4 1 4 9 7 6 - 9 7 3 - 1 6 3 - 8 2 6 2 2 E S E S 3 3 - C E S 2 5 6 3 - 0 0 4 3 - 9 2 0 3 - 6 7 2 2 - 1 9 9 1 - 8 3 4 1 - 5 7 6 - 2 7 3 - 4 5 3 - 0 9 6 2 2 E S W S 3 3 - C E S 3 ' ~ ' 0 3 - 6 8 2 2 - 4 8 9 1 - 3 3 4 1 - 6 7 6 - 8 7 3 - 2 6 3 - 4 9 6 2 2 E S 3 3 - C E S - 4 - W G R B R T L C G N L S L T B B 8 5 T I M R E P E T A T S N O I T A C O L 5 5 6 3 - 9 0 4 3 - 8 3 0 3 - 7 7 2 2 - 3 8 9 1 - 9 1 4 1 - 6 7 6 - 5 7 3 - 8 5 3 - 6 6 9 2 2 W S E N 3 3 . C E S 1 5 6 3 - 6 0 4 3 - 2 3 0 3 + 4 7 2 2 - 1 8 9 1 - 0 4 4 1 - 2 7 6 - 2 7 3 - 6 5 3 - 0 1 5 3 2 E N W S 3 3 . C E S 1 5 6 3 - 2 0 4 3 - 8 2 0 3 - 2 6 2 2 - 6 8 9 1 - 5 3 4 1 - 6 5 6 - 2 7 3 - 7 5 3 - 3 5 0 2 2 4 3 . C E S 7 9 3 3 - 3 2 0 3 - 2 6 2 2 - 7 5 9 1 - 5 1 4 1 - 2 7 6 - 2 7 3 - 5 5 3 - 5 2 8 1 2 W S E N 4 3 . C E S 1 3 4 3 - 3 8 3 3 “ 0 1 0 3 - 0 0 2 2 — 3 5 9 1 - 7 1 4 1 - 0 6 6 - 0 6 3 - 2 4 3 - 9 6 3 3 2 W S W S E S . C E S 3 4 6 3 - 9 8 3 3 - 6 1 0 3 - 3 5 2 2 ~ 1 6 9 1 - 8 1 4 1 - 3 6 6 - 3 6 3 - 7 4 3 - 0 7 3 3 2 W S W S . C E S 8 3 0 3 - 2 7 2 2 - 7 8 9 1 - 2 4 4 1 - 6 7 6 - 3 7 3 - 6 5 3 - 1 0 0 3 2 E S E N 3 3 . C E S 2 5 0 3 - 6 5 0 3 - 4 8 2 2 - 1 0 0 2 - 1 4 4 1 - 2 8 6 - 1 8 3 - 4 6 3 - 7 1 1 3 2 E N W S 3 3 . C E S 6 9 2 2 - 3 0 0 2 - 8 5 4 1 - 1 8 6 - 6 8 3 - 0 7 3 - 7 5 4 3 2 M M E N 3 3 . C E S 3 5 0 3 - 5 9 2 2 - 6 9 9 1 - 0 0 4 1 - 2 8 6 - 7 4 0 3 ~ 7 8 2 2 - 5 0 0 2 - 1 4 4 1 - 4 7 6 - 9 7 3 - 8 7 3 - 1 6 3 - 6 3 7 2 2 E S W N 3 3 . C E S 2 6 3 - 8 4 7 2 2 3 3 . C E S 3 3 0 3 - 2 7 2 2 - 2 8 9 1 - 3 2 4 1 - 7 7 6 ~ 2 7 3 ~ 4 5 3 - 6 0 8 2 2 E S E S 3 3 . C E S ? “ 0 3 ~ 1 9 2 2 - 0 0 0 2 - 2 5 4 1 - 4 7 6 - 9 7 3 - 5 6 3 - 7 3 8 2 2 3 3 . C E S 6 3 8 3 - 0 9 5 3 ~ 4 1 2 3 - 2 6 4 2 - 2 0 2 2 - 2 6 5 1 - 0 8 7 - 1 8 4 - 9 6 4 - 4 5 0 5 2 . C E S 6 6 4 3 - 3 9 0 3 ~ 5 5 3 2 - 3 5 5 1 ~ 9 4 7 ~ 9 2 4 - 6 1 4 - 8 3 6 1 2 E S E S E S . C E S 5 3 5 3 ' 0 6 1 3 - 7 1 4 2 - 4 1 1 2 - 7 5 5 1 - 8 4 7 - 0 4 4 - 9 2 4 - 3 8 6 2 2 E N E N E S 1 1 . C E S 1 1 8 3 - 6 6 5 3 - 0 9 1 3 - 7 4 4 2 - 5 5 1 2 - 0 9 5 1 - 0 6 7 - 0 8 8 2 2 E N W N 2 1 . C E S 9 3 8 3 - 3 9 5 3 - 6 1 2 3 - 5 6 4 2 - 7 0 2 2 - 7 1 6 1 - 0 9 7 - 8 8 4 - 6 7 4 - 3 2 7 2 2 E S . C E S ' w 5 R s e T 4 7 7 3 - 9 2 5 3 4 6 5 1 3 - 3 0 4 2 - 5 8 0 2 - 9 6 5 4 3 4 4 - 1 3 4 - 0 8 6 3 2 W S E N E S 2 1 . C E S 4 9 7 3 - ? ” 5 3 ‘ 5 7 1 3 - 7 0 4 2 - 9 6 0 2 - 0 7 5 1 - 6 4 7 3 2 M M E S 2 1 . C E S 2 3 7 3 - 9 8 4 3 - ‘ 6 1 1 3 - 0 5 3 2 - 6 4 0 2 - 8 3 5 1 - 5 1 4 2 2 E S E S E S 3 1 . C E S R B R T L C 6 N L S B B B S T I M R E P E T A T S N O I T A C O L 0 1 5 3 - 7 3 I 3 - 5 7 3 2 - 1 5 0 2 - 9 4 5 1 - 2 1 4 - 8 9 3 - 2 9 9 2 2 E N E S E S ' 3 1 . C E S 7 4 1 3 - 3 8 3 2 - 5 7 0 2 ~ 9 5 5 1 ~ 6 1 4 - 2 0 4 - 5 8 1 4 2 E N E N E S 3 1 . C E S 9 4 7 3 ~ 3 0 5 3 - 0 3 1 3 - 3 6 3 2 - 3 4 0 2 - 0 4 5 1 - 7 2 5 3 - 5 8 2 3 - 3 1 9 2 - 9 7 1 2 - 4 5 5 3 - 8 1 3 3 - 6 4 9 2 - 0 1 2 2 - 5 7 2 1 - 3 1 3 I - 7 0 8 3 - 2 6 5 3 - 7 8 1 3 - 5 2 4 2 - 4 4 1 2 - 9 0 6 1 - 3 5 5 3 2 5% "IN U) 9 4 7 3 ~ 5 0 5 3 - 0 3 1 3 - 2 7 3 2 - 5 6 0 2 - 5 4 5 1 - 5 8 3 - 4 6 0 3 2 E S E S E S 8 1 . C E S 4 1 5 3 - 9 3 1 3 - 1 7 3 2 - 7 6 0 2 - 9 4 5 1 ~ 8 9 3 - 6 4 4 4 2 4 / w . w N % 5 C 8 1 . C E S 1 2 1 3 - 2 6 3 2 - 7 3 0 2 ~ 2 4 5 1 - 6 8 3 - 2 9 0 4 2 4 / w s C 8 1 . C E S 7 2 1 3 - 3 6 3 2 - 6 4 0 2 - 2 3 5 1 - 5 0 2 2 2 E N E N W N 9 1 . C E S 0 1 1 3 - 5 5 3 2 - 7 3 0 2 - 9 4 5 1 - 1 8 3 - 3 7 4 2 2 E N E S W N 9 1 . C E S 2 9 4 3 - 3 4 1 3 - 3 7 3 2 ~ 3 7 0 2 - 9 5 5 1 ~ 8 0 5 3 - I ' 3 1 3 - 8 6 3 2 - 7 6 0 2 - 2 5 5 1 - 3 3 1 3 - 1 7 3 2 - 8 6 0 2 - 9 4 5 1 - 2 9 3 - 7 9 3 - 4 9 3 - 7 2 5 2 2 E S W S 8 1 . C E S 2 9 5 2 2 E S W N 8 1 . C E S 5 8 7 2 2 8 1 . C E S 9 2 1 3 - 3 6 3 2 ~ 0 6 0 2 - 2 4 5 1 - 5 8 3 - 2 1 4 2 2 E 8 ] 4 4 ' 8 E S 8 1 . C E S 3 8 9 5 2 1 9 9 1 2 E S E S 0 3 . C E S 3 1 . C E S 1 6 3 - 7 0 8 3 2 E N E N W S 0 7 3 . C E S . C E S w 4 R 5 2 T 5 2 7 3 - 9 7 4 3 ~ 6 0 1 3 - 1 5 3 2 - 0 4 0 2 - 4 2 5 1 - 8 9 6 - 6 3 1 3 - 6 7 3 2 - _ 5 6 0 2 - 1 5 5 1 ~ 3 0 7 - 5 1 8 2 2 7 5 7 3 2 E N E N E S 9 1 . C E S E N E S 9 1 . C E S 6 4 7 3 - 3 0 5 3 - 8 2 1 3 - 6 7 3 2 - 1 5 0 2 - 3 4 5 1 - ? 9 6 ~ 2 0 4 - 0 9 3 - 3 9 8 2 2 W S W N 0 2 . C E S 8 9 4 3 - 5 2 1 3 - 8 6 3 2 - 2 8 0 2 - 9 3 5 1 - 7 8 6 - 4 9 3 - 7 7 3 - 6 7 6 1 2 0 2 . C E S R B R T L C L S L T B B B S T I M R E P E I A T S N O I T A C O L 9 0 7 3 - 3 6 4 3 ~ 6 8 0 3 - 9 1 3 2 - 3 4 0 2 - 7 9 4 1 - 4 9 6 - 8 0 5 3 - 1 3 1 3 - 1 8 3 2 - 4 5 0 2 - 3 5 5 1 ~ 5 8 4 3 - 8 0 1 3 - 0 5 3 2 - 9 4 0 2 ~ 6 3 5 1 - 9 8 6 - 3 3 0 5 2 6 9 0 5 2 8 3 4 3 2 7 7 4 3 - 2 0 1 3 - 0 4 3 2 - 2 5 0 2 - 5 2 5 1 7 8 8 6 - 2 9 3 ~ 8 7 3 - 8 2 7 4 2 W S E S 0 2 . C E S 0 2 . C E S E N W S 0 2 . C E S W S E S E S 1 2 . C E S 1 4 4 3 - 4 6 0 3 - 5 9 2 2 - 0 0 0 2 - 9 8 3 1 - 3 9 6 - 4 9 3 - 6 7 3 ~ 7 1 7 1 2 E S E S E S 7 2 . C E S 4 6 0 3 - 2 0 3 2 - 0 0 0 2 - 5 6 4 1 - 0 8 6 - 5 8 3 # 9 6 3 ~ 2 3 0 3 2 W S W S E S 8 2 . C E S 7 8 6 3 - 0 4 4 3 - 6 6 0 3 - 6 0 3 2 - 6 0 0 2 - 1 9 4 1 - 7 7 6 - 3 8 3 - . 7 6 3 - 3 3 0 3 2 E S E N E S 9 2 . C E S 3 1 4 3 - 2 4 0 3 - 3 8 2 2 - 0 0 0 2 - 6 6 4 1 - 1 7 6 - 6 7 3 - 0 6 3 - 0 0 0 2 2 E N W N 2 3 . C E S 4 3 4 3 - 0 6 0 3 - 7 0 3 2 - 4 0 0 2 - 0 8 4 1 - 9 6 6 - 5 7 3 - 0 6 3 - 4 8 5 2 2 E S E S W N 9 2 . C E S 3 1 0 3 - 3 5 2 2 ~ 2 6 9 1 - 7 8 3 1 - 1 7 6 - 3 7 3 ~ 6 5 3 - 4 5 7 2 2 E S E N E S 2 3 . C E S 1 9 4 3 - 5 1 1 3 - 6 5 3 2 ~ 0 5 0 2 - 4 5 5 1 — 4 9 6 - 7 9 3 - 4 8 3 - 2 0 4 4 2 W S E N O 2 . C E S 6 1 1 3 - 8 5 3 2 - 1 5 0 2 - 9 4 5 1 - 9 8 6 - 3 7 4 4 2 E S 0 2 . C E S 9 1 1 3 - 1 6 3 2 - 0 7 0 2 - 4 6 5 1 - 6 9 6 - 8 9 3 - 3 8 3 - 2 8 9 3 2 E S W N 0 2 . C E S 5 2 1 3 - 8 6 3 2 - 7 6 0 2 - 0 5 5 1 - 9 9 6 - 9 9 3 ' ? 8 3 ~ 9 6 2 4 2 W S E S 0 2 . C E S 9 4 0 3 - 9 8 2 2 - 6 0 0 2 - 7 3 4 1 ~ 9 7 6 - 9 7 3 - 1 6 3 - 8 2 6 2 2 2 5 6 3 - 0 0 4 3 - 9 2 0 3 - 6 7 2 2 - 1 9 9 1 - 8 3 4 1 - 5 7 6 - 2 7 3 - 4 5 3 - 0 9 6 2 2 E S 3 3 . C E S 3 3 . C E S R B R T L C L S L T B B B S T I M R E P E T A T S N O I T A C O L 8 1 4 3 - 5 1 ' 0 3 - 0 9 2 2 - 6 0 0 2 - 5 4 4 1 - 8 7 6 - 6 6 3 - 4 6 9 1 2 E N E S 3 3 . C E S 1 4 0 3 - 6 8 2 2 - 7 8 9 1 - 1 4 4 1 - 7 8 6 - 7 7 3 - 0 6 3 - 3 9 2 2 2 E S W S E S 3 3 . C E S 0 5 0 3 - 7 8 2 2 - 3 0 0 2 - 4 5 4 1 - 1 4 0 3 - 9 7 2 2 - 6 9 9 1 - 0 5 4 1 - 6 8 6 - 7 7 3 - 9 7 3 - 0 6 3 - 4 8 3 2 2 E S W N E S 3 3 . C E S 1 6 3 - 8 4 5 2 2 E S E S W N 3 3 . C E S 3 1 ' 0 3 - 6 8 2 2 - 4 8 9 1 - 3 3 4 1 - 6 7 6 - 8 7 3 - 2 6 3 - 4 9 6 2 2 E S SE 3 3 . C E S 3 5 0 3 - 5 9 2 2 - 6 9 9 1 ~ 0 0 4 1 - 2 8 6 - 9 7 3 - 1 6 3 - 6 3 7 2 2 E S 3 3 . C E S 7 4 0 3 - 7 8 2 2 - 5 0 0 2 - 1 4 4 1 - 4 7 6 - 8 7 3 - 2 6 3 - 8 4 7 2 2 W N E S 3 3 . C E S 3 3 0 3 ~ 2 7 2 2 - 2 8 9 1 - 3 2 4 1 - 7 1 ' 0 3 - 1 9 2 2 - 0 0 0 2 - 2 5 4 1 - 7 7 6 - 4 7 6 - 2 7 3 - 4 5 3 - 6 0 8 2 2 E S E S E S 3 3 . C E S 9 7 3 - 5 6 3 - 7 3 8 2 2 W N 3 3 . C E S 5 5 6 3 - 9 0 4 3 - 8 3 0 3 - 7 7 2 2 - 3 8 9 1 - 9 1 4 1 - 6 7 6 - 5 7 3 - 8 5 3 ~ 6 6 9 2 2 W S E N W N 3 3 . C E S 8 3 0 3 - 2 7 2 2 - 7 8 9 1 - 2 4 4 1 - 6 7 6 - 3 7 3 ~ 6 5 3 - 1 0 0 3 2 E S E N W N 3 3 . C E S 2 5 0 3 - 6 3 0 3 4 8 2 2 - 1 0 0 2 - 1 4 4 1 - 2 8 6 - 1 8 3 - 4 6 3 - 7 1 1 3 2 E N W S W N 3 3 . C E S 6 9 2 2 - 3 0 0 2 - 8 5 4 1 - 6 8 3 - 0 7 3 - 7 5 ' 3 2 E N W N 3 3 . C E S 1 5 6 3 - 6 0 4 3 - 2 3 0 3 - 4 7 2 2 - 1 8 9 1 - 0 4 4 1 - 2 7 6 - 3 7 3 - 6 5 3 - 0 1 5 3 2 E N W S E S * 7 9 3 3 ' 3 2 0 3 - 2 6 2 2 - 7 5 9 1 ~ 5 1 4 1 - 2 7 6 - 2 7 3 - 5 5 3 - 5 2 8 1 2 W S E N E S 3 3 4 3 . C E S . C E S 1 5 6 3 ~ 2 0 4 3 - 8 2 0 3 - 2 6 2 2 - 6 8 9 1 - 5 3 4 1 ~ 6 5 6 - 2 7 3 ~ 7 5 3 - 3 5 0 2 2 W S 4 3 . C E S 2 0 5 3 - 1 9 2 3 - 6 1 9 2 - 9 2 1 2 - 7 6 6 1 - 1 9 1 1 - 5 9 5 - 3 0 3 - 7 8 2 - 4 7 6 2 2 W S 2 2 . C E S 5 3 5 3 - 3 7 2 3 - 1 0 9 2 - 2 0 1 2 - 3 4 6 1 - 4 7 1 1 - 6 7 5 - 5 4 5 3 - 2 8 2 3 - 8 0 9 2 - 3 0 1 2 - 7 9 1 1 - 1 8 5 - 9 5 4 3 - 5 0 2 3 - 4 3 8 2 - 9 5 0 4 6 4 6 1 - 8 5 1 1 - 4 4 5 - 1 0 6 1 2 6 0 3 2 2 1 5 3 2 2 W S E S 5 2 . C E S E S E S W N 5 2 . C E S E S E S 0 3 . C E S 6 3 4 3 - 1 8 1 3 - 2 1 8 2 - 1 3 0 2 - 5 4 6 1 - 1 8 1 1 - 1 7 4 3 - 2 1 2 3 - 3 4 8 2 - 0 5 0 2 - 4 1 6 1 - 4 4 1 1 - 9 3 5 - 4 5 5 - 8 3 2 - 1 1 6 9 1 W S W S 3 3 . C E S 7 4 2 - 0 4 8 4 2 E S E N E S 5 3 . C E S 2 8 2 3 - 7 0 9 2 ~ 8 2 1 2 - 0 3 7 1 ~ 8 5 2 1 - 8 7 7 1 2 E S E S 7 1 . C E S 5 8 0 2 - 1 4 6 1 - 1 9 1 1 - 6 6 5 - 5 9 1 1 ~ 1 7 5 - 9 7 2 - 2 9 2 - 1 6 2 - 9 4 4 4 2 W S W S E S 9 1 . C E S 7 7 2 - 9 9 6 9 1 W S E S E S 0 2 . C E S 1 3 4 3 - 3 8 3 3 - 0 1 0 3 - 0 0 2 2 - 3 5 9 I - 7 1 4 1 - 0 6 6 - 2 4 3 - 9 6 3 3 2 W S W S E S 4 3 . C E S 3 4 6 3 - 9 8 3 3 - 6 1 0 3 - 3 5 2 2 ' 1 6 9 1 - 8 1 4 1 - 3 6 6 - 7 4 3 - 0 7 3 3 2 W S W S W N 4 3 . C E S R B R T L C G N L S L T B S T I M R E P E T A T S N O I T A C O L 1 9 6 3 - 1 3 4 3 - 6 5 0 3 - 3 7 2 2 - 5 4 8 1 - 0 9 3 1 - 9 9 6 ~ 9 7 3 - 2 4 7 2 2 E N E S W N 5 . C E S W 3 R 5 3 T 5 0 0 3 - 5 5 2 2 - 8 3 9 1 - 2 5 3 1 - 1 5 6 ~ 0 3 3 - 7 0 8 1 2 W S 7 7 9 2 ~ 0 3 2 2 - 4 3 9 1 ~ 6 3 3 1 - 1 4 6 - 5 5 2 2 ~ 0 1 0 2 - 0 4 3 1 - 3 5 6 - 9 2 3 - 9 1 3 ~ 8 0 8 1 2 2 1 9 1 2 3 3 o 3 - 1 8 2 2 - 8 6 9 1 - 5 8 3 1 - 8 6 6 - 3 4 3 - 7 4 9 1 2 7 2 0 3 - 3 7 2 2 - 0 4 9 1 - 1 3 4 1 - 4 6 3 - 4 1 0 2 2 W S E S E S W S W N W S W N mmmmm . C E S . C E S . C E S . C E S . C E S w 4 R 5 3 T R B R T L C ' G M L S L T B B B S T I M R E P E T A T S N O I T A C O L 8 7 9 2 - 4 2 2 2 - 2 7 9 1 - 3 0 3 1 - 9 2 6 - 8 2 3 - 0 1 3 - 2 5 0 2 2 E S W S E S 3 . C E S 3 8 9 2 - 7 7 2 2 - 7 3 0 2 - 7 7 3 1 - 0 1 0 3 - 1 5 2 2 - 4 5 9 1 - 8 5 3 1 - 7 8 6 - 5 9 6 « 3 9 3 - 6 7 3 - 7 6 0 2 2 W S E N E S 8 6 0 2 2 W S E N W N 6 9 9 2 - 9 7 9 2 ~ 2 4 2 2 - 6 0 9 1 - 7 1 3 1 - 8 2 6 - 4 2 3 - ? 0 3 ~ 9 7 0 2 2 W S E S E S 9 2 2 2 - 0 8 9 1 - 8 8 2 1 - 0 2 6 - 6 1 3 - 7 9 2 - 8 3 1 2 2 W S W S E S 6 0 0 3 - 0 5 2 2 - 1 4 3 1 - 2 4 6 . 5 3 3 - 7 1 3 - 8 4 1 2 2 W S E S 2 2 0 3 - 6 6 2 2 - 2 2 9 1 - 8 6 3 1 - 6 6 6 - 8 5 3 - 0 4 3 - 0 4 1 2 2 W N W S E S 0 0 0 3 - 3 5 2 2 - 6 5 9 1 - 3 6 3 1 - 7 6 6 - 1 6 3 - 3 4 3 ~ 1 5 1 2 2 W N E S 0 9 9 2 - 7 2 2 2 - 0 9 9 1 - 4 1 3 1 - 9 3 6 - 8 3 9 2 2 ' w s w s 5 9 9 2 - 4 3 2 2 - 6 2 9 1 - 5 5 3 1 - 1 6 6 - 8 5 3 - 0 4 3 - 0 1 2 2 2 5% E S E S 2 1 0 3 - 7 5 2 2 - 5 3 9 1 - 5 7 3 1 - 9 9 6 - 6 6 3 - 3 0 8 2 2 E S 9 5 2 2 ~ 3 5 9 1 ~ 3 5 3 I - 1 4 3 - 3 2 3 ~ 6 7 5 1 2 E N E S E S 8 3 3 3 ~ 7 6 9 2 - 0 1 2 2 - 8 3 2 1 - 1 4 6 - 5 I 3 ' _ 8 9 2 - 4 3 6 1 2 E S W S E S 4 5 3 3 ' 3 8 9 2 - 8 2 2 2 - 6 8 8 1 - 3 2 3 1 ~ 1 4 6 - 8 3 3 ~ 2 2 3 - 2 0 7 1 2 E S E N E S 9 4 0 3 ~ 5 8 2 2 - 0 9 9 1 - 5 0 4 1 - 3 7 6 ~ 7 6 3 - 0 5 3 - 4 9 2 2 2 E N E N 9 8 9 2 - 1 3 2 2 - 4 9 8 1 - 3 3 3 1 - 5 4 6 - 3 4 3 - 5 2 3 - 9 5 6 2 2 E S E N 0 3 0 3 - 2 6 2 2 - 3 7 9 1 ~ 1 4 3 1 - 8 9 9 1 2 E S 1 4 0 3 - 8 8 2 2 - 4 6 9 1 - 1 9 3 1 - 7 6 6 - 1 6 3 - 4 4 3 - 7 3 0 2 2 E N E N E S - 0 1 - m mmmmmmmmm:.=r.=r.=r.=r-=r-=r . C E S ' . c E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S 5 0 6 3 ~ 7 5 3 3 - 6 8 9 2 - 9 2 2 2 - 6 2 9 1 - 3 4 3 1 - 6 4 6 - 5 " 3 - 8 2 3 - 3 7 8 2 2 E N W S E S 3 4 3 3 - 3 7 9 2 ~ 9 1 2 2 - - 3 5 9 I - 8 5 2 1 - 2 1 6 - 3 8 2 3 2 E S E S E S 4 4 . C E S . C E S 1 1 6 3 - 4 6 3 3 - 1 9 9 2 - 2 4 2 2 - 8 9 8 1 - 1 5 3 1 - 3 5 6 - 1 5 3 - 4 3 3 - 2 3 2 4 2 E N W S E N . C E S R B L C O N L S L T B B B S T I M R E P E T A T S N O I T A C O L 2 8 2 3 - 2 1 9 2 - 7 5 1 2 ~ 1 2 7 1 - 3 2 2 1 - 1 0 6 - 9 8 2 - 2 9 7 2 2 E S E S E S . C E S 0 3 3 3 - 9 5 9 2 - 1 0 2 2 - I ' 5 7 4 6 4 2 1 - 9 1 6 - 2 2 3 - 4 0 3 - 1 5 4 4 2 . E N E N E S . C E S 9 9 2 3 - 9 3 9 2 - 5 9 1 2 - 5 5 7 1 - 4 3 2 1 - 4 9 5 - 6 9 2 - 0 8 2 - 2 0 5 1 2 E S O I . C E S 5 8 2 3 - 6 1 9 2 - 0 8 1 2 - 0 0 8 1 - 5 4 2 1 - 5 9 5 - 8 9 2 - 2 8 2 - 4 6 5 1 2 W S M M 0 1 . C E S 4 2 9 2 - 1 8 1 2 - 9 9 6 1 - 9 0 2 1 - 6 8 2 - 0 7 2 - 5 9 3 1 2 E S E S 0 1 . C E S 3 4 9 2 - 9 7 1 2 - 9 4 7 1 - 8 1 2 1 - 0 8 5 - 6 8 2 - 8 6 2 - 5 6 5 1 2 W S E S O I . C E S 7 8 9 2 - 0 3 2 2 - 0 6 7 1 - 5 5 2 1 - 6 3 6 - 6 0 3 - 9 8 2 - 3 9 5 1 2 E N W S 0 1 . C E S 6 1 3 3 - . 6 6 9 2 - 0 1 2 2 - 6 3 2 1 - 8 2 6 - 9 9 2 - 3 8 2 - 1 5 6 1 2 E N W S E S O I . C E S 7 2 9 2 - 1 7 1 2 - 0 3 7 1 - 3 3 2 1 - 4 8 5 - 9 8 2 - 1 7 2 - 5 7 6 1 2 W S E S 0 1 . C E S 9 5 9 2 - 9 9 1 2 - 8 6 9 2 - 8 0 2 2 - 1 8 6 1 2 3 3 7 1 2 E N O I . C E S E N E S 0 1 . C E S 6 8 2 3 - 2 3 9 2 ~ 2 8 1 2 - 1 5 7 1 - 2 0 2 1 - . 7 7 5 - 7 6 2 - 2 4 7 1 2 E S W S E S 0 1 . C E S 4 3 3 3 - 5 6 9 2 - 5 0 2 2 - 5 8 7 1 - 0 8 2 1 - 1 2 6 - 0 2 3 - . 3 0 3 - 3 8 7 1 2 E N E N O I . C E S 7 8 2 3 ~ 0 2 9 2 - 8 6 1 2 - 1 4 7 1 - 7 5 2 1 - 4 0 6 - 3 0 3 ' 6 8 2 - 8 4 9 1 2 W S E S 0 1 . C E S 8 2 3 3 - 8 7 9 2 - 5 3 2 2 - 1 3 8 1 - 7 4 2 1 - 8 9 5 - 9 9 3 - 3 8 2 - 9 4 9 1 2 E N E S 0 1 . C E S - 1 1 - R B R T L C L S L T B B B S T I M R E P E T A T S : N O I T A C O L 1 9 2 3 - 5 8 9 2 ~ 5 8 1 2 - 9 8 7 1 - 7 3 2 1 - 0 9 5 - 4 9 2 - 7 7 2 - 5 1 0 2 2 W S E N E S 0 1 . C E S 2 2 9 2 - 9 6 1 2 - 4 0 7 1 - 1 1 2 1 - 3 8 5 ~ 7 8 2 - 0 7 2 - 9 4 0 2 2 E S E S E S 0 1 . C E S 1 9 2 3 - 9 3 9 2 - 8 8 1 2 - 0 2 7 1 - 8 4 2 1 - 1 0 6 - 2 9 2 - 7 7 2 - 5 7 0 2 2 O I . C E S 3 5 9 2 ~ 4 0 2 2 - 5 9 6 1 ~ 9 2 2 1 - 5 9 5 - 0 0 3 - 4 8 2 - 4 9 9 1 2 E N W N O I . C E S 3 9 9 2 - 7 3 2 2 - 3 7 2 1 - 7 9 5 - 9 9 2 - 2 8 2 - 3 8 0 2 2 E N 0 1 . C E S 9 5 9 2 - 6 0 2 2 - 4 0 8 1 - 7 5 2 1 - 3 0 6 - 9 0 2 2 2 E S E S 0 1 . C E S 6 6 9 2 - 3 2 2 2 - 1 6 7 1 - 9 6 2 1 - ? 0 3 ~ 9 8 2 - 4 3 2 2 2 E S 0 1 . C E S 4 2 9 2 - 5 7 1 2 - 0 2 7 1 - 1 3 2 1 - 6 9 5 - 1 0 3 - 3 8 2 - 8 5 2 2 2 W S W S E S O I . C E S 5 2 9 2 - 5 6 1 2 - 1 3 7 1 ~ 2 4 2 1 - 0 1 6 - 7 0 3 - 0 9 2 - 9 5 2 2 2 W S W S 0 1 . C E S 6 5 9 2 ~ 9 9 1 2 - 6 8 6 1 - 1 1 2 1 - 6 4 9 2 - 2 9 1 2 - 3 8 7 1 - 2 2 2 1 - 0 9 5 - 7 8 5 4 4 9 2 - 6 7 2 - 9 8 2 2 2 E S E N O I . C E S 0 6 4 2 2 E S E S 0 1 . C E S 6 4 9 2 - 1 8 1 2 - 7 3 7 1 - 2 1 2 1 - 7 8 5 - 1 9 2 - 3 7 2 - 6 9 4 2 2 E S E N E S O I . C E S 9 7 9 2 - 1 3 2 2 - 9 4 2 1 - 1 0 6 - 1 0 3 - 4 8 2 - 2 1 5 2 2 E S 0 1 . C E S 8 4 9 2 - 9 8 1 2 - 0 8 6 1 - 4 0 2 1 - 8 8 2 - 9 6 2 - 1 6 5 2 2 E N E S E S 0 1 . C E S 0 6 9 2 - 2 9 1 2 - 1 6 7 1 - 6 5 2 1 - 2 1 3 - 4 9 2 - 2 6 5 2 2 E N E N E S O I . C E S 6 5 9 2 - 0 9 1 2 - 0 0 8 1 - 6 6 2 1 - 1 9 2 - 1 4 6 2 2 W S E N 0 1 . C E S 6 3 9 2 - 2 8 1 2 - 8 5 7 1 ~ 2 5 2 1 - 8 8 9 2 - . 1 2 2 2 - n i 7 1 ~ 1 5 2 1 - 1 9 2 - 5 2 1 4 2 0 1 . C E S 9 1 7 3 2 W S E S 0 1 . C E S - 2 1 - 1 6 S 3 - 6 1 3 3 - 6 4 9 2 - 1 9 1 2 - 1 8 7 1 - 0 7 2 1 - 4 1 6 - 6 1 3 - 9 9 2 - 6 3 2 4 2 W N W S W N 0 1 . C E S R B L C L S L T B B B S T I M R E P E T A T S N O I T A C O L 3 1 3 3 ~ 1 4 9 2 - 5 7 1 2 - 1 4 7 1 - 5 4 2 1 - 2 2 6 - 1 2 3 - 5 0 3 - 6 2 8 1 2 6 4 9 2 ~ 2 9 1 2 - 5 9 6 1 - 8 0 2 1 - 1 9 5 ~ 3 9 3 ~ 8 7 2 ~ 0 1 6 2 2 7 9 2 3 ~ 9 2 9 2 - 6 7 1 2 - 5 0 7 1 - 4 1 2 1 - 4 9 5 - 5 9 2 - 5 7 2 - 4 4 1 3 2 3 9 2 3 - 2 2 9 2 - 5 6 1 2 - 9 1 7 1 - 9 4 2 1 - 6 5 6 - 8 8 2 - 7 4 5 3 2 8 4 3 3 - 6 7 9 2 - 3 1 2 2 - 9 8 7 1 - 2 9 2 1 - 4 4 6 - 3 4 3 - 4 2 3 - 9 3 7 1 2 7 0 9 2 - 1 0 1 2 - 5 7 6 1 ~ 3 9 1 1 ~ 6 7 5 - 2 8 2 - 4 6 2 - 4 4 1 2 2 E S W S W S W S E N I I . C E S I I . C E S I I . C E S I I . C E S 2 1 . C E S 4 1 . C E S 5 0 9 2 - 6 5 1 2 - 3 1 7 1 - 4 9 1 1 - 0 7 5 - 7 7 2 - 9 5 2 - 4 1 2 2 2 W S 4 1 . C E S 0 2 9 2 - 3 6 1 2 - 4 9 6 1 - 6 0 2 1 - 3 9 2 - 6 7 2 - 1 0 4 2 2 4 1 . C E S 7 0 9 2 - 6 6 1 2 - 3 9 6 1 - 5 3 2 1 - 2 2 4 2 2 W S 4 1 . C E S 2 1 9 2 - 7 5 1 2 - 7 9 6 1 - 0 1 2 1 - 8 9 2 - 0 8 2 - 5 8 4 2 2 4 1 . C E S 2 9 8 2 - 0 4 1 2 - 4 4 7 1 - 1 3 2 1 - 6 9 2 - 0 8 2 - 6 9 9 2 2 W S 4 1 . C E S 0 2 9 2 - 3 6 1 2 - 1 4 7 1 - 9 3 2 1 - 1 1 3 - 3 9 2 - 9 3 3 3 2 4 1 . C E S 8 8 8 2 - 7 6 1 2 - 7 5 6 1 - 0 8 1 1 - 1 6 2 9 0 E N E S E N 5 1 . C E S 6 2 9 2 - 7 7 1 2 4 6 0 7 1 - 3 0 2 1 - 2 7 5 - 0 8 2 - 1 6 2 - 4 9 3 1 2 E N E S W N 5 1 . C E S 5 7 2 3 - 2 0 9 2 - 8 5 1 2 - 5 4 7 1 - 5 7 2 1 - 1 9 5 1 2 E S E S 5 1 . C E S 7 3 9 2 ~ 0 8 1 2 - 6 9 7 1 - 3 4 2 1 ~ 7 7 5 - ' 5 8 2 - 6 6 2 - 9 4 6 1 2 E N W N E S 5 1 . C E S 2 2 9 2 - 0 7 1 2 - 1 3 7 1 - 8 6 2 1 - 0 9 5 ' 8 9 2 - 0 8 2 - 0 4 0 2 2 5 3 W N E S 5 1 . C E S R B R T L C 6 N L S L T B B 8 5 T I M R E P . E T A T S N O I T A C O L 7 1 9 2 - 2 6 1 2 - 5 0 7 1 ~ 7 9 1 1 - 8 6 5 - 5 7 2 - 7 5 2 - 0 5 0 2 2 E N E S E S 5 1 . C E S 6 2 9 2 - 4 7 1 2 - 2 6 7 1 - ' 6 8 2 1 - . 0 0 6 - 4 0 3 - 7 8 2 - 3 6 1 2 2 E S . E S w n 5 1 . C E S 7 2 9 2 - 6 6 1 2 - 5 8 6 1 - 5 0 2 1 - 0 7 5 - 8 7 2 - 0 6 2 - 6 7 1 2 2 E N E N E S 5 1 . C E S 9 2 9 2 - 6 7 1 2 - 1 7 7 1 - 7 6 2 1 - 3 9 5 - 1 0 3 - 3 8 2 - ‘ 7 7 1 2 2 E S W N W N 5 I . C E S 1 2 9 2 - 3 6 1 2 - 0 4 7 1 - 3 8 2 1 - 2 9 5 - 9 9 2 - 2 8 2 - 8 0 2 2 2 E S E S E S 5 1 . C E S 0 8 2 3 - 2 2 9 2 - 4 7 1 2 - 5 4 2 1 - 8 8 5 2 9 2 - 5 7 2 - 2 2 2 2 2 E S E N W N 5 1 . C E S 6 1 9 2 - 4 6 1 2 - 3 2 7 1 - 0 3 2 1 - 9 8 5 - 6 9 2 - 7 7 2 - 0 6 2 2 2 E N W N 5 I . C E S 0 3 9 2 - 3 7 1 2 - 0 3 7 1 - 5 4 2 1 - 6 8 5 - 1 9 2 - 4 7 2 - 7 8 3 2 2 E N W S E S 5 1 . C E S 6 9 8 2 - 6 5 1 2 - 2 6 7 1 - 6 9 2 1 - 4 1 9 2 - 3 7 1 2 ~ 3 9 6 1 - 1 4 2 1 - 9 2 9 2 - 8 7 1 2 - 6 2 7 1 - 3 4 2 1 - 0 9 3 2 2 5 5 4 2 2 3 2 5 2 2 5 1 9 2 - 6 7 1 2 - 8 2 7 1 ~ 1 4 2 1 - 4 9 2 - 1 7 2 - 1 0 6 2 2 W S E N E S 5 1 . C E S E S E N E S 5 1 . C E S E N W S W N 5 I . C E S E N E S 5 1 . C E S 4 1 9 2 - 9 4 1 2 - 5 4 7 1 ~ 7 6 2 1 - 7 9 5 - 1 0 3 - 5 8 2 - 2 0 8 2 2 5% W N E S 5 I . C E S 5 0 9 2 - 4 5 1 2 - 4 3 7 1 - 0 4 2 1 - 1%: 7 9 2 - 9 7 2 - 1 5 9 2 2 E S W N 5 1 . C E S 3 6 2 3 - 4 0 9 2 - 1 7 l 2 - 7 5 7 1 - 9 8 2 1 - 5 9 5 ' 4 8 2 - 7 1 0 3 2 E S W S E S 5 I . C E S 6 0 9 2 - 1 5 1 2 - 5 2 7 1 - 3 2 2 1 - 3 9 5 ' 9 9 2 ' 2 8 2 - 9 1 2 3 2 - W N W N 5 1 . C E S 0 0 9 2 - 5 6 1 2 - 0 3 7 1 - 9 7 2 1 - 1 9 5 “ 0 1 7 3 2 E S W S W N 5 1 . C E S 2 0 9 2 - 5 4 1 2 - 9 5 7 1 ~ 4 8 2 1 - 6 9 5 - 7 8 2 - 0 3 8 3 2 W S E S E S 5 1 . C E S - 4 1 - 2 2 5 3 - 7 7 2 3 - 6 0 9 2 - 6 4 1 2 - 8 3 7 1 - 6 3 2 1 - 4 0 6 - 3 6 2 3 - 6 9 8 2 - 0 4 1 2 - 1 6 7 1 - 3 8 2 1 - 3 0 6 - 3 I 3 ~ 7 9 2 - 9 7 2 3 - 1 1 9 2 - 8 5 1 2 - 1 3 2 1 - 7 1 6 ~ 9 1 3 - 3 0 3 - 2 1 0 4 2 3 0 5 1 2 2 8 8 2 2 W S E S 5 1 . C E S 6 1 . C E S E N E N E S 6 1 . C E S R B L C 6 N L S L T B B B S T I M R E P E T A T S N O I T A C O L 8 6 4 3 - 2 2 2 3 - 1 5 8 2 - 9 9 0 2 - 8 3 7 1 - 0 6 2 1 - 3 6 5 ~ 6 7 2 - 9 5 2 - 7 5 6 2 2 E S E S E S 2 2 . C E S 5 2 2 3 - 4 5 8 2 - 7 9 0 2 - 8 3 7 1 - 7 7 2 1 - 5 7 5 - 6 8 2 - 9 6 2 - 8 6 8 2 2 W N E S E S 2 2 . C E S 7 1 2 3 ~ 9 4 8 2 - 0 0 1 2 - 9 3 7 1 - 8 4 2 1 - 4 6 5 - 5 7 2 - 2 0 2 3 2 E S E S 2 2 . C E S 0 0 9 2 - 7 4 1 2 - 9 7 7 1 - 1 9 2 1 ~ 0 0 6 - 8 9 0 3 2 E N E S 2 2 . C E S 9 4 2 3 - 8 9 8 2 - 1 4 1 2 - 3 5 7 1 - 1 8 2 1 - 2 9 5 - 9 9 2 - 3 8 2 - 4 8 3 1 2 E N E S E S 2 2 . C E S 9 0 2 3 - 2 8 8 2 - 2 2 1 2 - 8 5 7 4 5 7 2 1 - 0 8 5 - 7 1 4 1 2 E S E N E S 2 2 . C E S 6 1 9 2 - 1 7 1 2 - 9 4 7 1 - 8 7 2 1 - 5 9 5 - 0 0 3 - 4 8 2 - 3 3 5 1 2 E N E N E S 2 2 . C E S 8 1 9 2 - 7 6 1 2 - 4 6 7 1 - 7 8 2 1 - 0 9 5 - ? 9 2 ~ 0 8 2 - 5 4 4 2 2 E N E N 2 2 . C E S 4 4 2 3 - 6 8 8 2 - 5 2 1 2 - 5 5 7 1 - 4 8 2 1 - o 9 5 ~ 9 9 2 - 2 8 2 - 5 6 8 3 2 E N W S E N 2 2 . C E S 6 4 2 3 - 7 7 8 2 - 4 2 1 2 - 8 5 7 1 - 2 8 2 1 - 4 9 5 - 6 8 2 - 0 1 1 4 2 E N W S 2 2 . C E S 8 4 2 3 - 8 9 8 2 - b - - - - 5 9 1 1 2 W S ' W N . C E S 1 7 8 2 - 9 1 1 2 - 9 5 7 1 - , 8 6 2 1 - 6 8 5 - 7 9 2 - 1 8 2 - . 5 7 2 3 2 E N W S E S 2 2 . C E S 3 9 8 2 - 6 5 1 2 - 7 5 7 1 ~ 5 8 2 1 - 5 9 5 - 8 6 3 3 2 E N W N 2 2 . C E S 4 8 8 2 - 2 5 1 2 - 1 5 7 1 - 5 7 2 1 - 3 9 5 - 9 9 2 ~ 2 7 4 3 2 E S 2 2 . C E S 0 7 8 2 - 3 2 1 2 - 9 5 7 1 - 2 7 2 1 - 4 9 2 - 6 7 2 - 7 8 5 3 2 E S E N 2 2 . C E S W G R B R T L C C N L S L T B B T I M R E P E T A I S _ N O I T A C O L 2 8 4 3 - 5 3 2 3 - 4 6 8 2 - 6 1 1 2 - 6 0 7 1 - 2 4 2 1 - 4 7 5 ~ 6 8 2 - 8 5 2 3 - 4 8 8 2 - 0 3 1 2 - 4 9 6 1 - 2 2 2 1 - 1 8 5 - 1 9 2 - 1 3 2 3 - 9 5 8 2 - 3 0 1 2 - 4 9 6 1 - 0 5 2 1 - 5 6 5 ~ ? 7 2 ~ 7 4 2 3 ~ 7 7 8 2 ~ 4 2 1 2 - 9 1 2 1 - 3 7 5 ~ 6 8 2 - 8 8 8 2 - 4 3 1 2 - 3 2 7 1 - 9 4 2 1 - 8 7 5 - 8 8 2 - 4 1 9 2 - 5 0 1 2 - 9 1 7 1 - 7 5 2 1 - 6 8 5 - 5 9 2 - 1 7 8 2 - 9 1 1 2 - 0 8 2 1 - 2 9 2 - 0 8 8 2 - 4 2 1 2 - 1 5 7 1 ~ 4 7 2 1 - 3 7 5 - 2 8 2 - 7 8 8 2 - 9 4 1 2 - 0 5 7 1 - 6 8 2 1 - 1 8 5 - 7 8 2 - 1 9 8 2 - 6 4 1 2 - 4 2 7 1 - 2 6 2 1 - 3 8 5 ~ 2 9 2 - 1 8 8 2 - 3 2 1 2 - 3 5 7 1 - 0 8 2 1 - 1 7 5 ~ 1 8 2 - 7 9 8 2 ~ 4 4 1 2 - 0 1 7 1 - 9 4 2 1 - 6 8 5 - ? 9 2 ~ 3 3 3 1 2 4 3 3 1 2 5 8 3 1 2 5 1 4 1 2 6 1 4 1 2 2 3 5 1 2 8 4 6 1 2 6 9 6 1 2 5 1 7 1 2 9 0 1 2 2 5 3 2 2 2 8 5 6 2 2 W S W S 3 2 . C E S W S W S E S 3 2 . C E S W S E S 3 2 . C E S W S E S 3 2 . C E S E S 3 2 . C E S W N E S 3 2 . C E S E S 3 2 . C E S E N £2 3 2 . C E S 3 2 . C E S E S W S 3 2 . C E S W S E S 3 2 . C E S E S E S 3 2 . C E S 1 5 2 3 ~ 9 9 8 2 - 6 4 1 2 - 4 8 7 1 - 8 8 2 1 - 3 8 5 - 0 9 2 - ' 3 4 1 3 2 W S W N 3 2 . C E S 4 2 2 3 - 4 5 8 2 - 8 0 1 2 - 6 1 7 1 - 5 4 2 1 - 4 6 5 - 2 7 2 - ' 4 3 9 1 2 E N W N 6 2 . C E S 9 2 2 3 ~ 3 6 8 2 - 8 1 1 2 - 6 0 2 1 - 4 4 5 - 6 5 2 - 4 2 6 2 2 W N W N E S 6 2 . C E S 8 2 2 3 - 9 6 8 2 - 2 2 1 2 ~ 5 9 1 1 - 5 4 5 ~ 9 5 2 ~ 9 2 6 2 2 E N 6 2 . C E S 4 1 2 3 ~ 2 5 8 2 - 6 0 1 2 - 0 0 7 1 - 2 3 2 1 - 4 4 5 - 1 5 2 - 8 6 9 2 2 W N E N E S 6 2 . C E S 6 2 2 3 - 9 6 8 2 - 0 1 1 2 ~ 3 2 7 1 - 6 5 2 1 - 6 4 5 - 6 5 2 - 7 9 9 2 2 . E S 6 2 . C E S - 6 1 - 9 0 2 3 ~ 3 5 8 2 - 8 9 0 2 - 3 3 7 1 - 8 4 2 1 - 1 4 5 - 8 4 2 - 0 3 2 - 9 3 0 3 2 5 5 E S 6 2 . C E S 6 0 2 3 - 8 5 8 2 - 8 9 0 2 - 4 1 7 1 - 0 2 2 1 - 1 3 5 - 8 3 2 - 1 2 2 - 2 5 1 3 2 W S E N E S . C E S 6 0 2 3 - 2 5 8 2 - 0 8 0 2 - 5 9 6 1 ~ 0 2 2 1 - 4 3 5 - 2 4 2 - 5 2 2 - 7 6 2 3 2 E S . C E S 9 8 1 3 ~ 4 4 8 2 - 1 8 0 2 - 8 5 6 1 - 4 7 1 1 - 9 0 5 - 1 2 2 - 5 0 2 - 6 9 2 3 2 E S W S . C E S 5 9 I 3 ~ 4 3 8 2 - 8 5 1 1 - 2 1 5 - 6 2 2 - 9 0 2 - 4 2 3 3 2 E S E S . C E S 0 8 1 3 - 1 3 8 2 - 5 6 0 2 - 6 5 6 1 - 1 3 2 1 - 0 2 5 - 0 3 2 - 3 1 2 - 6 7 1 3 - 4 2 8 2 - 7 6 0 2 - 1 1 7 1 - 1 1 2 1 - 2 1 5 - 2 2 2 - 5 0 2 - 3 5 3 3 2 7 3 5 3 2 E S W S E S . C E S W S E S E S . C E S 7 0 2 3 ~ 3 5 8 2 ~ 8 9 0 2 - 2 2 7 1 - 8 3 2 1 - 9 2 5 - 6 3 2 - 9 1 2 - 2 5 5 3 2 W S E N W N . C E S 3 4 4 3 ~ ‘ 2 9 1 3 - 2 2 8 2 - 9 7 0 2 - 2 5 6 1 - 3 8 1 1 - 6 1 5 - 6 7 5 3 2 E S E S . C E S 9 6 4 3 - 3 2 2 3 ~ 4 5 8 2 — 7 0 1 2 - 4 3 7 1 ~ 4 6 2 1 - 3 6 5 ~ 3 7 2 ~ 5 5 2 ~ 6 8 5 3 2 W N W N . C E S 5 9 1 3 ~ 2 4 8 2 - 1 8 0 2 - 9 0 7 1 ~ 3 4 2 1 ~ 5 2 5 ~ 4 3 2 - 8 1 2 - 2 0 6 3 2 W S E S . C E S 9 9 1 3 - 0 4 8 2 - 1 8 0 2 - 4 2 7 1 - 0 3 2 1 ~ 2 7 8 2 - 9 0 1 2 - 9 4 7 1 - 0 7 2 1 - 3 5 5 ~ 6 3 5 ~ 0 6 2 - 2 4 2 - 4 0 6 3 2 W S . C E S 4 4 2 - 7 2 2 - 5 2 7 3 2 W S . C E S 9 6 8 2 - 2 1 1 2 - 5 3 7 1 - 8 4 2 1 - 4 5 5 - 3 6 2 - 6 4 2 - 1 4 7 3 2 W S . C E S 6 6 8 2 - 2 0 1 2 - 0 4 7 1 - 2 5 2 1 - 6 5 5 - 2 7 5 4 2 E N W S . C E S 9 9 1 3 ~ 2 4 8 2 - 9 8 0 2 - 7 2 7 1 - 6 3 2 1 - 8 4 5 - ? 5 2 ~ 0 4 2 - 6 0 9 4 2 W S . C E S 4 7 1 3 - 0 1 8 2 - 4 5 0 2 - 9 4 6 1 - 9 9 1 1 - 3 5 5 - 5 6 2 - 8 4 2 - 0 7 4 1 2 W S W N W N . C E S 1 6 8 2 - 4 0 1 2 - 1 2 7 1 - 1 5 2 1 - 3 5 5 - 5 6 2 - 8 4 2 - 0 5 9 3 2 E N , E N E S . C E S - 7 1 - L T B B G R B R T G N L S L C W L N O I T A C O 8 5 T I M R E P E T A T S R B R T L C G N L S L T B B B S T I M R E P E T A T S N O I T A C O L 7 1 2 3 - 1 5 8 2 - 7 9 0 2 - 7 3 7 1 - 9 4 2 1 - 7 6 5 - ? 7 2 ~ 0 6 2 - 1 9 2 4 2 E N E N W N 7 2 . C E S 2 3 1 3 - 6 6 7 2 - 2 0 0 2 - 4 2 6 1 ~ 4 5 1 1 - 2 0 5 - 4 2 2 - 8 0 2 — 3 1 5 1 2 W S W S E S 5 3 - C E S 6 7 1 3 ~ 6 2 8 2 - 9 6 0 2 - 2 5 7 1 - 8 2 2 1 - 3 2 5 - 9 1 2 2 2 E N W N W N 5 3 - C E S 2 6 1 3 - 1 1 8 2 - 3 5 0 4 6 7 6 1 - O l 2 l - 1 1 5 - 7 2 2 - 0 1 2 - 1 7 1 3 2 E N E S E S 5 3 - C E S 2 5 1 3 ~ 6 0 8 2 - 2 5 0 2 - 8 7 6 1 - 9 9 1 1 - 0 0 5 - 7 1 2 - 0 0 2 - 7 4 2 3 2 E N W S E S 5 3 . C E S 3 6 1 3 - 6 0 8 2 - 9 5 0 2 - 6 9 6 1 - 9 0 2 1 - 6 0 5 - 0 2 2 - 3 0 2 - 8 4 2 3 2 E N E S W N 5 3 - C E S 9 7 1 3 ~ 8 2 8 2 - 0 8 0 2 - 2 9 6 1 ~ 4 1 2 1 - 4 1 5 - 9 2 2 - 2 1 2 - 0 0 3 3 2 E S E N E S 5 3 - C E S 1 7 1 3 - 8 1 8 2 - 8 5 0 2 - 7 1 7 1 - 1 2 2 1 - 3 7 1 3 - 7 1 8 2 - 9 5 0 2 - 8 6 6 1 - 9 2 2 1 - 9 6 1 3 ~ 0 2 8 2 - 0 6 0 2 - 7 8 6 1 - 0 1 2 1 - 3 2 2 - 7 0 2 - I ' 5 3 3 2 3 7 4 3 2 4 7 4 3 2 E S E N W N 5 3 - C E S E N E N W N 5 3 . C E S E N W N E S 5 3 : c e s 6 6 1 3 ~ 7 1 8 2 - 0 5 0 2 - 1 9 6 1 - 5 0 2 1 - 1 2 2 - 4 0 2 - 4 0 5 3 2 E N W S W N 5 3 - C E S 7 6 1 3 ~ 9 1 8 2 - 5 5 0 2 - 7 0 7 1 - 4 1 2 1 - 5 3 2 - 7 1 2 - 2 6 5 3 2 E N E S 5 3 . C E S 3 5 1 3 - 2 7 1 3 - 3 7 1 3 - 5 8 7 2 - 2 3 0 2 - 7 6 6 1 - 8 8 1 1 - 5 2 2 - 8 0 2 - 1 3 6 3 2 E S W N E S 5 3 o C E S 6 0 8 2 - 1 5 0 2 - 7 8 6 1 - 7 1 2 1 - 6 3 2 - 9 1 2 - 2 8 6 3 2 E N W N 5 3 - C E S 7 1 8 2 - 6 4 3 - 6 9 6 1 - 7 0 2 1 - 4 2 2 - 7 0 2 - 9 4 9 3 2 E S E S E S 5 3 . C E S 8 5 1 3 - 1 9 7 2 ~ 2 1 0 2 - 6 9 6 1 - 0 9 1 1 - 6 3 2 - 9 1 2 - 5 8 5 1 2 E S W S E S 6 3 . C E S 9 5 1 3 - 1 9 7 2 ~ 9 3 0 2 - 2 8 6 1 - 0 0 2 1 - 6 5 4 2 2 W S E S E S 6 3 . C E S 4 6 1 3 - 3 9 7 2 ~ 9 1 0 2 ~ 5 6 6 1 - 5 8 1 1 - 0 3 2 - 3 1 2 - 6 0 6 2 2 E S W S W N 6 3 . C E S - 8 1 - _ _ W G R B R T L C O N L S L T B B 8 5 T I M R E P E T A T S N O I T A C O L 7 0 4 3 ~ 7 0 1 3 ~ 9 8 7 2 - 9 2 0 2 - 7 6 6 1 - 1 8 1 1 - 3 2 2 - 5 0 2 - 3 0 1 3 2 W S E N E S 6 3 . C E S 5 4 1 3 - 4 9 7 2 - 7 4 0 2 - 6 8 6 1 - 3 3 2 1 - 9 9 1 - 1 8 1 - 6 5 7 2 W S W S E S 6 3 . C E S 2 7 1 3 - 8 1 8 2 - 7 5 0 2 - 7 9 6 1 - 2 1 2 1 - 0 1 5 - 6 2 2 - 0 1 2 - 6 4 8 2 2 W S W S 6 3 . C E S 3 6 1 3 - 7 1 8 2 - 0 5 0 2 - 9 8 6 1 - 4 1 2 1 - 3 I 5 - 9 2 2 ~ 3 1 2 - 7 6 9 2 W S E S 6 3 . C E S 0 7 1 3 - 0 1 8 2 - 0 6 0 2 - 0 7 6 1 - 0 0 2 1 - 7 1 5 - 0 6 5 3 W S 6 3 . C E S 4 6 1 3 - 6 1 8 2 - 6 6 0 2 - 3 9 6 1 - 4 1 2 1 - 4 1 5 - 0 3 2 - 4 1 2 - 2 4 9 3 W S 6 3 . C E S 4 6 1 3 - 7 9 7 2 - 0 3 o 2 - 3 8 6 1 - 8 8 1 1 - 3 1 5 - 1 3 2 - 4 1 2 - 5 5 6 4 W S E N 6 3 . C E S 8 9 3 3 - 6 4 1 3 - 1 8 7 2 - 0 0 0 2 - 6 7 6 1 - 4 7 1 1 - 0 1 5 - 0 3 2 - 4 1 2 - 3 8 8 1 2 4 8 3 3 ~ 9 2 1 3 - 4 6 7 2 ~ 1 8 9 1 - 5 2 6 1 - 3 5 1 1 - 3 0 5 ~ 4 2 2 - 9 0 2 - 4 8 4 2 E S E S 2 9 7 2 - 7 1 0 2 - 3 8 5 1 - 3 0 1 1 - 3 8 4 - 5 0 2 - 9 8 1 - 4 0 6 2 W S W S 9 7 7 2 - 7 9 9 1 - 2 7 5 1 - 3 5 1 1 - 5 8 4 - 4 7 5 2 W S W S E S 2 6 3 3 - 9 0 1 3 - 6 4 7 2 - 7 7 9 l - 3 2 6 1 - 4 3 2 1 - 1 8 4 - 9 9 1 ~ 3 8 1 - 8 0 9 2 W S E S E S 1 8 3 3 - 9 2 1 3 — 5 6 7 2 - 6 8 9 1 - 5 1 6 1 - 8 4 1 1 - 5 9 4 - 1 1 2 - 6 9 1 - 5 1 1 3 2 W S E S 4 3 1 3 - 9 6 7 2 - 6 9 9 1 - 1 3 6 1 - 7 5 1 4 - 4 9 4 - 1 6 6 3 2 W S 2% 4 3 1 3 - 4 7 7 2 - 0 6 9 1 - 0 7 5 1 - 9 5 1 1 - 0 9 4 - 3 I I 3 - 3 6 7 2 - 4 8 9 1 - 6 1 6 1 - 0 2 1 1 - 6 8 4 - 2 0 2 - 6 8 1 - 9 8 7 3 3 1 9 9 1 W S W S E N W S E S 2 8 0 3 - 0 3 7 2 ~ 4 5 9 1 - 3 7 5 I - 0 8 0 1 - 9 6 4 - 6 8 1 - 0 7 1 - 9 1 4 1 2 E S W S E S 0 2 7 2 - 8 4 9 1 - 0 5 5 1 ~ 3 6 0 1 - 1 8 4 - 0 0 2 - 3 8 1 - 1 3 9 9 1 E S E N E S \O\O\O\O\O\O\O\DI\I\-I\- . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S W 3 R 5 4 T - 9 1 - W G R B R T L C O N L S L T B S T I M R E P E T A T S 1 1 1 0 1 T A C O L 6 7 0 3 - 3 3 7 2 - 7 4 9 1 - 1 6 5 1 - 2 6 0 1 - 7 7 4 - 9 3 7 2 ~ 0 7 9 I - 3 0 6 1 - 7 0 1 1 - 9 6 4 - 3 7 1 - 9 7 1 - 4 5 4 1 2 3 2 5 1 2 1 0 1 3 - 0 5 7 2 - 3 8 9 1 - 3 7 5 1 - 3 8 0 1 - 0 8 4 - 0 8 1 - 2 5 7 1 2 E S E S 5 8 0 3 - 9 3 7 2 - 1 6 9 1 - 0 6 5 1 - 5 7 0 1 - 6 7 4 - 4 9 0 3 - 6 5 7 2 - 0 9 9 1 - 3 2 6 1 - 4 3 1 1 - 8 7 4 - 9 7 1 - 9 7 1 - 5 3 0 2 2 3 1 2 2 2 6 0 1 3 - 6 4 7 2 - 2 9 9 1 - 9 2 6 1 - 4 3 1 1 - 3 8 4 - 0 8 1 - 8 1 2 2 2 E S E S W S E S E S E S 2 8 0 3 - 0 2 7 2 - 6 4 9 1 - 1 6 5 1 - 6 7 0 1 - 0 7 4 - 0 9 0 3 ~ 7 3 7 2 ~ 8 6 9 1 - 7 8 5 1 - 1 9 0 1 - 6 9 0 3 - 4 4 7 2 - 6 7 9 4 3 1 6 1 - 6 2 1 1 - 7 7 4 ~ 3 8 4 - 0 8 1 - 2 6 3 2 2 E S 7 7 1 - 7 7 1 - 0 6 3 2 2 W S E S 1 6 3 2 2 E S W S 2 1 1 3 - I ' 5 7 2 - 8 3 9 1 - 1 0 6 1 - 0 3 1 1 - 3 7 4 - 0 7 1 - 1 1 4 2 2 E N E S 0 1 1 3 - 4 5 7 2 - 7 9 9 1 - 5 2 6 1 - 0 5 1 1 - 3 8 4 - 1 8 1 - 5 9 4 2 2 E S 7 8 0 3 1 4 7 2 - 7 5 9 1 ~ 2 8 5 1 - 7 9 0 1 ~ 1 7 4 4 ? 7 1 ~ 1 6 4 2 2 W S E S W N 7 3 1 3 - 1 8 7 2 - 7 0 0 2 - 6 1 6 1 - 1 6 1 1 - 0 9 4 - 8 8 1 - 6 2 6 2 2 W N 2 0 1 3 - 5 5 7 2 - 1 8 9 1 — 4 9 5 4 2 3 1 1 - 0 7 4 - 3 8 1 - 7 6 1 - 6 0 5 2 2 9 9 0 3 - 7 5 7 2 - 8 8 9 1 - 8 0 6 1 - 0 3 1 1 - 0 9 4 - 3 0 2 - 7 8 1 - 3 8 0 8 0 5 7 2 ~ 6 8 9 1 - 7 0 6 1 - 9 3 1 1 - 8 7 4 - 5 9 I - 9 7 1 - 2 1 1 3 - 6 5 7 2 - 3 9 9 I - 4 1 6 1 - 3 4 1 1 - 5 7 4 ~ 8 8 1 — 3 7 1 - 0 2 5 2 2 2 8 5 2 2 3 8 5 2 2 W N W S E N W S W N E N W N E S 9 8 0 3 - 7 2 7 2 - 6 5 9 1 - 9 7 5 I - 0 1 1 I - 8 6 4 - 0 9 1 - 5 7 1 - 4 3 6 2 2 W S E S - 0 2 - E S E S E S W S E N E S . C E S 7 P— P— b— h~ n~ 6- n~ n— n— F— n— n— n- n— n— r~ E- . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S W C R B R T L C L S L T B B B S T I M R E P E T A T S N O I T A C O L 0 4 3 3 - 9 8 0 3 - 6 2 7 2 - 9 3 9 1 - 5 5 5 I - 5 6 0 1 - 8 8 4 - 5 0 2 - 9 8 1 - 1 3 7 2 2 6 0 1 3 . 7 4 7 2 - 5 7 9 1 ~ 7 9 5 I - 9 1 1 1 - 6 8 4 - 0 0 2 - 4 8 1 - 6 8 2 4 2 E N W S 7 1 1 3 ~ 4 5 7 2 - 6 6 9 1 - 9 7 5 I - 2 1 1 1 - 9 9 4 - 2 2 2 - 3 0 2 - 6 2 2 1 2 E S E N 7 8 9 . C E S . C E S . C E S 9 2 3 3 - 1 7 0 3 - 8 0 7 2 - 9 0 9 1 ~ 2 9 9 - 6 4 4 - 9 0 3 3 - I ' 5 0 3 - 1 9 6 2 - 3 0 9 1 - 8 9 4 1 - 2 1 0 1 - 2 6 4 - 5 2 3 3 ~ 1 7 0 3 ~ 0 1 7 2 - 8 2 9 1 ~ 7 4 0 1 - 0 7 4 - 9 4 6 2 2 3 7 9 1 2 0 4 3 2 2 E S W S 5 1 . C E S E S W S 6 1 . C E S E S 6 1 . C E S 5 5 0 3 - 4 9 6 2 - 1 1 9 1 - 3 5 5 1 - 8 1 0 1 - 0 6 4 - 7 6 1 - 8 4 5 4 2 W S W N 6 1 . C E S 1 5 0 3 - 4 6 0 3 4 8 8 6 2 - 2 0 9 1 - 1 4 5 1 - 3 3 0 1 - 8 0 7 2 - 3 2 9 1 ~ 6 5 0 1 - 3 7 4 ~ 3 7 4 6 8 1 - 9 6 1 - 0 2 4 1 2 5% 7 1 . C E S 5 2 9 4 2 6 1 . C E S 9 8 0 3 ~ 6 2 7 2 - 6 3 9 1 - 5 7 5 1 - 2 7 0 1 - 0 8 4 - 4 9 1 - 8 7 1 - 3 1 7 1 2 7 I . C E S 8 5 0 3 - 3 0 7 2 - 1 2 9 1 - 5 3 5 1 ~ 9 3 0 1 - 5 6 4 - 1 8 1 - 9 6 1 - 8 2 8 1 2 W S 7 1 . C E S 5 5 0 3 - 2 9 6 2 - 8 9 2 3 - 2 4 0 3 - 9 7 6 2 ~ 8 9 8 1 - 1 1 5 1 - 9 2 0 1 - 2 5 4 - 6 0 9 1 2 0 2 9 1 2 E S E N 7 1 . C E S W S W N 7 1 . C E S 9 9 2 3 - 6 4 0 3 - 5 8 6 2 - 9 0 9 1 - 9 1 5 1 - 4 2 0 1 - 0 7 4 - 6 3 2 - 6 2 2 - 0 6 9 1 2 E S E N E S 7 1 . C E S 4 0 3 3 - 8 4 0 3 - 8 9 6 2 - 2 1 9 1 - 0 2 5 1 - 8 3 0 1 - 5 6 4 - 5 8 1 - 9 6 1 - 3 0 1 2 2 W S E N 7 1 . C E S 6 5 0 3 ~ 2 0 7 2 - 6 1 9 1 - 5 3 5 1 ' 7 3 0 1 ~ 7 6 4 - 9 3 9 1 2 W N W S E S 7 1 . C E S 2 6 0 3 - 0 0 7 2 - 2 2 9 1 - 8 3 5 1 - 0 5 0 1 - 0 8 4 - 9 9 1 ~ 3 8 1 - 0 5 1 2 2 E N W S E S 7 1 . C E S 9 5 0 3 - 5 9 6 2 - 3 1 9 1 - 1 4 5 1 - 4 4 o 1 - 5 7 4 ~ 0 9 1 - 4 7 1 - 2 3 2 2 2 E S 7 1 . C E S - 1 2 - w c R B R T L C C N L S L T B B B S T I M R E P E T A T S N O I T A C O L 2 0 3 3 - 1 4 0 3 - 9 7 6 2 - 8 9 8 1 - 5 2 5 1 - 3 2 0 1 - 7 5 4 - 3 8 1 - 0 7 1 - 7 6 2 2 2 W S E N E S 7 1 . C E S 6 4 0 3 . 4 8 6 2 - 1 0 9 1 - 3 9 4 1 - 6 1 0 1 - 2 6 4 - 5 8 1 - 1 7 1 - 4 3 9 2 2 E S E S 7 1 . C E S 3 5 0 3 - 6 0 7 2 - 1 1 9 1 - 6 3 5 1 - 4 3 0 1 - 7 6 4 - 9 8 1 - 4 7 1 - 1 0 5 3 2 E S 7 1 . C E S 6 2 3 3 - 9 6 0 3 ~ 5 0 7 2 - 3 2 9 1 - 1 4 5 1 - 1 5 0 1 - 8 7 4 - 5 9 1 - 0 8 1 - 0 2 5 3 2 E N E S 7 1 . C E S 9 4 0 3 - 8 8 6 2 - 4 0 9 1 - 0 4 5 1 - 7 3 0 1 - 3 6 4 - 2 7 4 4 2 E S E S 7 1 . C E S 0 5 0 3 - 1 9 6 2 - 0 1 9 1 - 5 1 5 1 - 1 3 0 1 - 5 4 4 - 3 7 1 - 9 5 1 ~ 7 7 6 1 2 E N W S E S 8 1 . C E S 0 6 0 3 - 5 0 7 2 - 0 3 9 1 ~ 9 2 5 1 - 9 5 0 1 - 6 6 4 - 2 8 1 - 7 6 1 - 7 9 6 1 2 E N E N E S 8 1 . C E S 7 1 ' 0 3 - 5 9 6 2 - 9 1 9 1 - 8 1 5 1 - 0 3 0 1 - 5 4 4 - 7 6 1 - 5 5 1 - 4 8 7 1 2 E N E S E S 8 1 . C E S 6 7 0 3 - 1 2 7 2 - 9 4 9 1 - 8 4 5 1 ~ 1 6 0 1 - 2 7 4 - 8 8 1 - 3 7 1 - 7 8 8 1 2 E N E N 8 1 . C E S 4 5 0 3 - 3 9 6 2 - 6 1 9 1 - 9 2 5 1 - 5 3 0 1 ~ 0 5 4 - 7 7 1 - 1 6 1 - 1 5 0 2 2 E N E S W N 8 1 . C E S 8 4 0 3 - 6 8 6 2 - 2 0 9 1 - 2 0 5 1 - 0 2 0 1 - 6 4 4 - 5 6 1 - 4 5 1 - 1 7 1 2 2 E S E N 8 1 . C E S 3 6 0 3 - 5 5 0 3 ~ 3 2 7 2 - 8 2 9 1 - 7 6 5 1 - 0 6 0 1 - 0 6 4 - 9 7 1 2 2 E N E S 8 1 . C E S 2 9 6 2 - 2 1 9 1 - 7 1 5 1 - 6 2 0 1 - 8 4 4 - 1 7 1 - 6 5 1 - 4 4 3 2 2 E N W S 8 1 . C E S 1 8 0 3 - 7 1 7 2 ~ 1 5 9 1 - 6 6 6 1 - 7 6 0 1 - 0 8 4 - 4 0 5 2 2 E N 8 1 . C E S 8 6 0 3 - 3 0 7 2 - 7 2 9 1 - 1 4 5 1 - 3 5 0 1 - 0 6 4 - 4 8 1 - 1 7 1 - 8 9 5 2 2 E N E S 8 1 . C E S 4 1 3 3 - 5 6 0 3 - 2 0 7 2 - 6 2 9 1 - 5 4 5 1 - 6 5 0 1 - 0 6 4 - 6 8 1 - 0 7 1 - 8 2 8 3 2 E N W S 8 1 . C E S 1 5 0 3 - 1 9 6 2 - 0 1 9 1 - 1 2 5 1 - 2 3 0 1 - 1 5 4 - 8 7 1 - 3 6 1 - 5 0 7 2 2 E S E S 8 1 . C E S 3 7 6 2 - 8 9 8 1 - 5 8 4 1 - 7 0 0 1 - 6 4 4 - 1 7 1 - 6 5 1 - 7 8 2 4 2 E S E S E S 8 1 . C E S - 2 2 - W C R B R T L C 6 N L S L T 8 8 8 5 T I M R E P E T A T S N O I T A C O L 6 9 2 3 - 3 I ' 0 3 - 2 8 6 2 - 9 9 8 1 ~ 3 1 5 1 - 0 2 0 1 - 0 5 4 - 3 7 1 - 9 5 1 ~ 3 8 6 4 2 E S 8 1 . C E S 8 4 0 3 - 5 8 6 2 - 2 0 9 1 - 8 9 4 1 - 9 1 0 1 - 7 4 4 - 6 7 1 - 0 6 1 - 2 4 9 9 2 E S W N E S 8 1 . C E S 5 8 6 2 - 6 9 8 1 - 4 1 0 1 - 6 5 4 - 8 7 1 - 3 6 1 - 2 8 0 2 2 E N E N E S 9 1 . C E S 5 2 2 3 ~ 0 8 9 2 - 2 2 6 2 - 2 3 8 1 - 4 3 4 1 - 1 7 9 - 9 3 4 ~ 9 6 1 - 4 5 1 - 9 5 1 2 2 E S W S E S 9 1 . C E S 4 9 2 3 - 2 3 0 3 - 9 6 6 2 - 8 8 8 1 - o 9 4 1 - 4 1 0 1 - 7 4 4 - 5 7 I - 1 6 1 - 7 4 2 2 2 E N E N 9 1 . C E S 5 6 2 3 - 2 1 0 3 - 6 5 6 2 - 7 7 8 1 - 3 9 4 1 - 0 1 0 1 - 1 4 4 - 1 7 1 - 6 5 1 - 2 2 0 3 2 E N E S E S 9 1 . C E S 1 0 0 3 - 5 4 6 2 - 6 6 8 1 - 7 2 4 1 - 9 2 9 - 9 9 3 - 9 2 1 - 6 1 1 - 6 7 3 1 2 W S E S E S 0 2 . C E S 2 6 6 2 - 7 4 8 1 - 7 6 9 - 6 2 4 - 7 5 1 - 9 3 1 - 3 7 2 1 2 W S E S 0 2 . C E S 3 7 6 2 - 0 9 8 1 - 0 9 4 1 - 0 9 9 - 3 2 4 - 2 5 1 - 7 3 1 - 9 8 3 1 2 W S E N W N 0 2 . C E S 8 4 6 2 - 1 6 8 1 - 6 9 3 1 - 5 4 9 - 9 1 4 - 5 4 1 - 1 3 1 - 8 1 4 1 2 W S E S 0 2 . C E S 3 6 2 3 ~ 0 1 0 3 - 0 5 6 2 - 5 7 8 1 - 9 3 4 1 2 W S ' 1 ’ M 0 2 . C E S 6 8 6 2 - 4 0 9 1 - 1 0 5 1 ~ 4 1 0 1 - 7 4 4 - 1 7 1 - 6 5 1 — 1 6 4 1 2 W N W S E S 0 2 . C E S 2 5 2 3 - 4 0 0 3 - 4 4 6 2 - 8 5 8 1 - 2 9 3 1 - 2 4 9 - 3 1 4 - 4 4 1 - 1 3 1 - 7 3 4 2 2 W S W S 0 2 . C E S 4 3 0 3 - 7 7 6 2 - 5 1 8 1 2 W N E S 0 2 . C E S 7 5 6 2 ~ 8 8 8 1 - 8 4 4 1 - 9 6 9 - 9 1 4 - 9 4 1 - 5 3 1 ~ 9 6 4 2 2 E S W N 0 2 . C E S 6 5 6 2 - 8 6 8 1 - 1 0 4 1 - 4 4 9 - 3 1 4 - 3 4 1 - 0 3 1 - 1 7 5 2 2 E S E S E S 0 2 . C E S 2 6 2 3 - 1 1 0 3 - 1 5 6 2 - 5 6 8 1 - 4 0 4 1 - 2 4 9 - 0 2 4 - 6 4 1 - 9 6 6 2 - 1 9 8 1 - 8 1 4 1 - 1 7 9 - 7 1 4 - 8 4 1 - 3 3 1 - 5 3 I - 2 5 6 2 2 E S E N 0 2 . C E S 2 6 6 2 2 W S E N E S 0 2 . C E S - 3 2 - w 0 R B R T L C G N L S L T 8 8 B S T I M R E P E T A T S N O I T A C O L - - - - - - - - 3 5 6 2 - 3 9 8 1 - 3 4 4 1 - 8 4 9 - 6 0 4 - 8 3 1 - 4 2 1 - 8 8 6 2 2 E S W N E S 0 2 . C E S - - - - - - - - - 5 5 6 2 - 7 7 8 1 - 3 0 4 1 - 8 4 9 - 0 1 4 - 1 4 1 - 6 2 1 - 3 3 7 2 2 E S E S W N 0 2 . C E S - - - - - - - - 6 7 6 2 - 9 9 8 1 - 0 3 5 1 - 5 2 0 1 5 5 4 - 6 7 1 - 2 6 1 - 9 3 7 2 2 W N W N W N 0 2 . C E S - - - - - - - - 3 6 6 2 - 4 8 8 1 - 2 0 4 1 - _ 8 3 9 - 0 0 4 - 3 3 1 - 0 2 1 - 3 5 7 2 2 E S W S W N 0 2 . c t s - - - - - - - - 0 6 6 2 - 5 7 8 1 - 9 7 3 1 - 3 4 9 - 7 0 4 - 7 3 1 - 4 2 1 - 4 1 9 2 2 E S W S E S 0 2 . C E S 9 6 2 3 - 4 2 0 3 - 4 6 6 2 - 4 7 8 1 - 5 6 4 1 - 7 8 9 - 4 3 4 - 2 6 1 - 8 4 1 - 5 9 0 3 2 E N w s W N 0 2 . C E S - — - - - - - - 4 8 6 2 - 4 6 8 1 - 1 9 3 1 - 0 4 9 - 5 0 4 - 7 3 1 - 1 2 1 - 7 7 4 3 2 E S E N N S 0 2 . c e s - - - - 2 3 0 3 - 0 7 6 2 - 6 8 8 1 - 5 1 - 6 1 0 1 8 5 4 - 9 7 1 - 5 6 1 - 3 2 5 3 2 E N W N W N 0 2 . C E S - - - - - - - - - 4 6 6 2 - 0 8 8 1 - 7 9 4 1 - 6 0 0 1 1 4 4 - 0 7 1 - 5 5 1 - 1 9 5 3 2 W N E N E S 0 2 . C E S - - - - - - - - 0 5 6 2 . 2 7 8 1 - - - - 5 2 9 - 1 1 4 - 2 4 1 - 8 2 1 - 7 0 6 3 2 E S E N E S 0 2 . C E S 1 7 2 3 - 6 1 0 3 - 6 5 6 2 - 1 7 8 1 - 1 4 3 1 - 6 1 9 - 4 1 4 - - - - - - - 0 3 2 3 2 E S E S E S 1 2 . c e s - - - - - - - - - - 4 5 6 2 - 4 6 8 1 - 7 8 3 1 - 8 2 9 - 9 0 4 - 8 3 1 - 5 2 1 - 3 7 0 5 2 w s w s w s 1 2 . c e s 6 9 2 3 - 7 3 0 3 - 7 7 6 2 - 4 7 8 1 - 2 9 3 1 - 2 5 9 - 5 1 4 - 9 3 1 - 4 2 1 - 4 4 3 3 2 w s E S E S 4 2 . C E S 9 3 2 3 - 0 9 9 2 - 0 3 6 2 - 1 5 8 1 - 9 5 3 1 - 7 1 9 - 7 0 4 - 5 3 1 - 0 2 1 - 5 8 9 1 2 E N E S E S 8 2 . c : s - - - - - - - - 6 3 6 2 - 5 4 8 1 - 9 4 3 1 - 3 1 9 - 7 7 3 - 8 0 1 - 6 9 - 5 6 2 2 2 w s w s E S 8 2 . C E S - - - - - - - - - 8 3 6 2 - 9 4 8 1 - 4 6 3 1 - 6 2 9 - 0 9 3 - 1 2 1 - 6 0 1 - 6 1 4 2 2 w s w s W N 8 2 . c e s - - - - - - - 5 3 6 2 - 8 4 8 1 - 6 7 3 1 - 7 2 9 - 3 9 3 - 9 1 1 - 6 0 1 - 0 8 4 2 2 w s W N £2 8 2 . C E S - - - - - - - - - - 4 4 6 2 - 3 6 8 1 - 6 5 3 1 - 0 1 9 - 1 9 3 - 4 2 1 - 1 1 1 - 1 9 4 2 2 W N W N W N 8 2 . c e s - 4 2 - W G R B R T L C G N L S L T B B B S T I M R E P E T A T S N O I T A C O L 3 4 2 3 ~ 3 9 9 2 ~ 2 4 6 2 - 2 5 8 1 - 4 3 3 1 - 1 1 9 - 4 9 3 - 3 2 1 - 4 1 1 - 6 4 5 2 2 E S 8 2 . C E S 1 3 6 2 - 1 5 8 1 - 0 6 3 1 - 1 1 9 - 9 8 3 - 5 1 1 - 2 0 1 - 3 1 5 2 2 W S E S 8 2 . C E S 4 4 6 2 - 5 5 8 1 - 3 5 3 1 - 5 2 9 - 5 9 3 - 6 2 1 - 0 1 1 - 5 8 5 2 2 W S E S 8 2 . C E S 8 4 6 2 - 5 5 8 1 - 2 5 3 1 ~ 0 2 9 - 6 8 3 - 7 1 1 - 3 0 1 - 7 1 6 2 2 W S E S E S 8 2 . C E S 3 4 6 2 - 5 5 8 1 - 8 4 3 1 - 9 0 9 - 0 9 3 - 2 2 1 - 7 0 1 - 6 8 6 2 2 W S 8 2 . C E S 1 3 6 2 - 1 4 8 1 - 9 5 3 1 ~ 5 2 9 - 4 9 3 - 3 2 1 - 1 1 1 - 1 4 8 2 2 W S E S 8 2 . C E S 4 1 6 2 - 4 2 8 1 - 1 3 3 1 - 8 1 9 - 5 8 3 - 2 1 1 ~ 0 0 1 - 1 2 9 2 2 E S W S E S 8 2 . C E S 3 2 6 2 - 2 3 8 1 - 5 3 3 1 - 6 1 9 - q 9 3 - 4 8 2 3 2 E S W S 8 2 . C E S 6 3 6 2 - 1 4 8 1 - 6 6 3 1 - 3 2 9 - 3 0 4 - 8 2 1 - 5 1 1 - 1 7 5 3 2 W S E N 8 2 . C E S 5 3 2 3 - 4 8 9 2 - 6 2 6 2 - 2 3 8 1 - 9 3 3 1 ~ 6 9 8 - 9 9 3 - 5 2 1 - 3 1 1 - 1 3 0 4 2 E S E N 8 2 . C E S 4 7 9 2 ~ 4 1 6 2 - 0 3 8 1 - 7 7 3 1 - 2 3 9 - 3 8 3 - 1 1 1 - 8 9 - 3 5 9 3 2 E S W S W S 8 2 . C E S 1 9 9 2 ' 9 2 6 2 - 6 4 6 2 - 4 6 3 4 2 5 3 8 4 2 E S , » V N 8 2 . C E S E S W S 8 2 . C E S 8 1 2 3 - 8 6 9 2 - 1 1 6 2 - 4 2 8 1 ~ 0 7 3 1 - 1 2 9 - 1 0 4 - 0 3 1 - 5 1 1 - 3 6 4 2 2 E S E S 9 2 . C E S 7 3 6 2 - 5 3 8 1 - 4 6 3 1 — 2 1 9 - 1 9 3 - 0 2 1 - 4 0 1 - 8 8 3 2 2 E S E S E S 9 2 . C E S 4 3 6 2 ~ 4 4 8 1 - 5 3 3 1 ~ 7 1 9 - ? 8 3 ~ 8 1 1 - 4 0 1 - 1 2 5 2 2 E S E N E S 9 2 . C E S 1 3 6 2 - 9 4 8 1 - 2 5 3 1 - 6 1 9 - ? 8 3 ~ 6 1 1 ~ 2 0 1 - 2 4 5 2 2 E N E S E S 9 2 . C E S 3 4 6 2 - 4 7 8 1 - 8 3 3 1 - 1 7 8 - 1 9 3 - 3 2 1 - 9 0 1 - 0 7 5 2 2 E N E N E S 9 2 . C E S - 5 2 - 2 9 1 3 - 0 5 9 2 - 5 9 5 2 - 4 0 8 1 - 4 1 3 1 - 6 1 3 - 0 1 1 - 8 0 2 3 - 6 5 9 2 - 9 9 5 2 - 5 1 8 1 - 6 3 3 1 - 1 0 9 - 1 8 3 - 2 1 1 - 9 4 9 2 - 3 9 5 2 ~ 7 0 8 1 - 3 0 3 1 - 0 9 8 ~ 3 8 3 - 0 3 6 2 - 0 6 8 1 - 7 3 3 1 - 4 0 9 - 6 7 3 - 9 0 1 - 8 2 6 2 - 2 5 8 1 - 5 4 3 1 ~ 7 0 9 - 0 8 3 - 4 1 1 - 4 2 6 2 - 9 3 8 1 ~ 8 3 3 1 - 6 1 9 - 6 8 3 - 6 1 1 - 3 0 1 - 9 9 7 2 2 6 7 0 3 2 3 8 8 3 2 0 2 9 0 2 5 4 1 3 2 5 3 9 3 2 E S E N W N 9 2 . C E S E N E S W N 9 2 . C E S E N E S 9 2 . C E S E N E N E S 2 3 . C E S E N E N E N 2 3 . C E S E N E S E S 2 3 . C E S R B R T L C 6 N L S L T B B B S T I M R E P E T A T S N O I T A C O L 3 1 6 2 - 5 1 8 1 - 5 1 3 1 - 0 6 3 - 0 9 - 8 7 - 1 4 1 2 2 W S E N E S 3 3 . c e s 0 3 6 2 - 5 2 8 1 - 1 3 3 4 7 8 8 - 6 6 3 - 7 2 2 2 2 E S 3 3 . C E S 8 0 6 2 - 5 1 8 1 - 0 3 3 1 - 0 0 9 - 8 7 3 - 6 0 1 - 1 9 - 1 4 2 2 2 W S E N 3 3 . C E S 2 2 6 2 - 2 3 8 1 - 1 5 3 1 - 3 0 9 ~ 3 7 3 - 6 0 1 - 1 9 - 6 5 2 2 2 3 3 . C E S 4 9 5 2 - 0 1 8 1 - 3 0 3 1 - 9 7 8 - 9 6 3 ~ 6 9 - 1 8 - 3 6 2 2 2 W S 3 3 . . C E S 8 9 5 2 ~ 7 2 6 2 - 6 3 8 1 - 3 3 3 1 - 7 1 9 - 0 8 3 - 8 0 6 2 - 6 2 8 1 - 6 2 3 1 - 0 0 9 - 3 6 3 - 9 8 5 2 ~ 2 1 8 1 - 0 5 3 1 - 1 1 9 - 2 5 3 - 0 3 6 2 - 9 3 8 1 - 7 0 4 1 - 8 1 9 - 4 1 6 2 - 1 3 8 1 - 0 1 3 1 - 4 2 6 2 - 6 3 8 1 - 4 6 3 1 - 4 1 9 - 9 7 3 - ? 5 3 ~ 4 7 3 - - 6 2 - 0 0 1 - 6 8 - 4 6 5 2 2 E N E S 3 3 . C E S 3 6 3 2 2 1 9 3 2 2 4 6 4 2 2 3 0 5 2 2 8 0 5 2 2 3 6 5 2 2 E S W S 3 3 . C E S E S 3 3 . C E S E S SE 3 3 . c e s E S E S E S 3 3 . C E S E S E S 3 3 . c e s E N 3 3 . C E S 7 1 2 3 - 2 6 9 2 - 1 0 6 2 - 7 0 8 1 - 8 3 3 1 - 2 7 5 2 - 5 9 7 1 - 6 9 2 1 - 5 0 6 2 - 7 1 8 1 - 9 6 3 4 4 1 6 2 - 5 1 8 1 - 6 0 3 1 - 6 7 3 - 2 7 3 - ? 5 3 ~ 9 7 1 3 ~ 7 2 9 2 - 2 7 5 2 - 3 8 7 1 - 1 8 2 1 - 3 5 8 - 0 6 3 - 2 9 - 1 1 6 2 - 1 2 8 1 - 8 9 2 1 - 3 9 8 ~ 1 7 3 - - 7 2 - R B R T L C 6 N L S L T B B B S T I M R E P E T A T S N O I T A C O L 0 3 6 2 - 4 4 8 1 - 7 2 3 1 - 7 1 9 - 0 8 3 - 0 0 6 2 2 E N E S 3 3 . C E S 1 8 5 2 - 4 9 7 1 - 4 4 3 1 - 7 9 8 - 4 5 3 - 2 8 - 7 6 - 5 0 6 2 2 E S W S E S . C E S 5 1 6 2 - 7 2 8 1 - 1 6 3 1 - 9 1 9 ~ 7 7 3 - 2 0 1 0 9 - 0 3 6 2 2 E S E S . C E S 6 9 5 2 - 6 2 8 1 - 3 3 3 1 - 2 0 9 - 3 5 3 - 9 7 ' 5 6 - 4 5 6 2 2 E S E S . C E S 1 2 6 2 - 8 2 8 1 - 7 6 3 1 - 7 1 9 - 0 3 3 - 1 8 5 2 - 8 9 7 1 - ? 7 8 ~ 9 5 3 - 5 1 6 2 - 8 2 8 1 - 7 3 3 1 - 0 1 9 - 5 6 3 - 0 6 6 2 2 3 6 6 2 2 6 9 6 2 2 E N W S E S . C E S W S E S E S . C E S E S E N W N . C E S 2 0 6 2 - 5 1 8 1 - 4 2 3 1 - 6 9 8 - 0 5 3 - 8 7 - 4 6 - 5 2 7 2 2 E S E N E S . C E S 2 8 1 3 - 3 3 9 2 ~ 3 8 5 2 - 8 9 7 1 ~ 6 1 3 1 - 7 6 8 - 5 6 3 - 6 9 - 2 8 - 0 4 7 2 2 W S E S . C E S 5 2 6 2 - 1 4 8 1 - 0 7 3 1 ~ 5 2 9 - 6 8 3 - 3 1 1 0 0 1 1 6 7 2 2 E N W N . C E S 5 2 6 2 - 8 3 8 1 ~ 9 2 3 1 - 0 2 9 - 6 7 3 ~ 4 0 1 2 9 - 7 8 7 2 2 E N E S . C E S 7 1 6 2 - 3 3 8 1 - 1 5 3 1 - “ 7 3 - 1 0 1 1 1 8 2 2 E N E S d N . C E S 6 6 3 - 1 8 - 2 1 8 2 2 E N E S . C E S 4 9 - 2 7 8 2 2 W S . C E S 2 9 - 2 5 9 2 2 W S . C E S 0 9 9 2 2 8 3 3 3 2 4 8 7 3 2 W S E S . C E S E N E N E S . C E S W S W S E S . C E S 7 1 3 3 - 6 6 0 3 - 5 0 7 2 - 7 2 9 1 - 9 2 4 1 - 8 1 6 2 - 8 2 8 1 - 1 2 3 1 - 2 1 9 - 9 0 2 3 ~ 6 5 9 2 - 6 0 6 2 - 8 1 8 1 - 7 9 2 1 - 8 0 2 3 - 5 5 9 2 - 8 9 5 2 - 6 0 8 1 - 7 1 3 1 - 6 8 8 - 2 8 5 2 - 2 0 8 1 - 1 4 3 1 - 2 1 9 - 8 1 3 - 2 7 3 - ? 6 3 ~ 6 7 3 - 8 5 3 ~ 6 9 1 - 1 3 8 3 2 E N E N 3 3 . C E S 9 8 - 4 7 1 4 2 E N E N W S 3 3 . C E S 6 8 - 3 3 2 4 2 W N W S E N 3 3 . C E S 2 9 - 3 8 2 4 2 W N W S W S 3 3 . C E S 5 2 4 2 2 W S W S E S 4 3 . C E S R B R T L C 6 N L S L T B S T I M R E P E T A T S N O I T A C O L 2 0 6 2 - 7 0 8 1 - 6 5 3 4 0 2 9 - 0 6 3 - 4 8 ~ 2 7 - 7 2 4 2 2 W S W S W N 4 3 . C E S 0 8 5 2 - 3 9 7 1 ~ 0 3 3 1 ~ 9 9 8 - 0 6 3 - 6 7 - 8 2 4 2 2 W S E S 4 3 . C E S 0 9 5 2 - 0 1 8 1 - 8 0 3 1 - 6 5 3 - 6 8 - 2 7 - 7 4 7 2 2 W S E S 4 3 . C E S 8 9 1 3 - 7 3 9 2 - 0 8 5 2 - 0 8 7 1 - 3 1 3 1 - 1 6 3 - 2 9 - 6 7 9 2 - 2 1 6 2 - 0 2 8 1 - 1 4 3 1 - 0 7 3 - 4 9 5 2 - 4 2 8 1 - 8 0 3 1 - 4 5 3 - 9 7 ' 6 8 - 7 7 7 2 2 7 5 9 2 2 5 1 0 3 2 W S 4 3 . C E S E S W S SE 4 3 . C E S W S 4 3 . C E S 6 9 1 3 - 5 3 9 2 - 8 7 5 2 - 9 7 7 1 ~ 3 2 3 1 - 9 5 3 - - - - - 7 9 1 3 2 W S E N E S 4 3 . C E S 1 6 9 2 - 3 0 6 2 - 3 1 8 1 - 1 1 3 1 - 5 7 3 - 5 0 1 - 3 9 - 1 6 3 4 2 W N E S . C E S 5 8 5 2 - 6 8 7 1 - 1 1 3 1 - 8 5 3 - 8 0 6 4 2 E S W S W S . C E S 7 8 5 2 - 6 0 8 1 - 9 2 3 1 - 1 7 3 - 0 0 1 - 6 8 - 8 9 1 3 2 W S E S . C E S - 8 2 - 8 3 2 3 - 6 7 9 2 - 7 1 6 2 - 4 2 8 1 - 7 4 3 1 - 4 1 1 - 3 0 1 - 1 9 6 2 2 W N E N E S . C E S 2 6 1 3 - 8 0 8 2 - 9 3 0 2 - 5 5 6 1 - 2 1 5 - 1 2 2 - 0 0 4 2 2 E N E S . C E S 2 3 1 3 - 6 8 7 2 - 6 1 0 2 - 8 6 6 1 - 9 9 4 - 9 1 2 - 1 0 2 L 5 4 1 2 2 E N . C E S w 4 R 5 4 T 0 5 1 3 - 0 0 8 2 - 8 6 9 1 - 8 6 6 1 - 3 9 1 1 - 9 0 5 ~ 4 5 1 3 - 3 0 8 2 - 5 2 0 2 — 8 6 6 1 - 5 8 1 1 - 6 9 4 - 9 5 1 3 - 5 6 1 3 ~ 9 0 8 2 - 8 2 0 2 - 0 8 6 1 - 4 0 2 1 - 0 0 5 - 7 1 2 - 0 0 2 - 6 1 4 3 - 1 6 1 3 - 3 9 7 2 ~ 7 1 0 2 - 6 6 6 1 - 8 8 1 1 - 5 1 5 - 4 3 2 - 8 1 2 - 3 4 5 2 2 E N C . C E S 3 6 1 3 - 7 0 8 2 - 3 3 0 2 - 9 7 6 1 - 3 0 2 1 - 1 0 5 - 9 0 5 2 2 W S W N . C E S R B R T L C L S B B B S _ _ T I M R E P E T A T S _ N O I T A C O L 9 4 1 3 - 7 9 7 2 ~ 9 2 0 2 - 1 7 6 1 - 6 0 2 1 - 6 9 4 - 6 1 2 - 9 9 1 - 3 7 5 2 2 E N W S E S . C E S 4 7 1 3 - 0 2 8 2 - 6 4 0 2 - 8 7 6 1 - 3 1 2 1 - 7 2 2 - 9 0 2 - 6 1 6 2 2 W N E N W N . C E S 8 3 1 3 - 9 8 7 2 - 1 2 0 2 - 9 5 6 1 - 1 8 1 1 - 9 8 4 - 9 0 2 - 2 9 1 - 3 5 6 2 2 E S E N E S . C E S 0 6 1 3 - 2 0 8 2 - 3 2 0 2 - 8 5 6 1 - 5 7 1 1 - 0 0 5 - 9 0 2 - 2 9 1 - 7 8 6 2 2 E S E S E S . C E S 6 6 1 3 - 4 1 8 2 - 4 5 0 2 - 4 9 6 1 - 5 1 2 1 - 6 2 2 - 0 1 2 - 5 9 6 2 2 W N E N W N . C E S 9 4 1 3 - 5 9 7 2 - 4 2 0 2 - 0 6 6 1 - 1 9 1 1 - 5 9 4 - 5 1 2 - 9 9 1 - 9 0 7 2 2 E S E N I l ‘ v . C E S 7 0 8 2 - 4 3 0 2 - 2 7 6 1 - 9 0 2 1 - 9 9 4 - 4 1 2 - 9 9 1 - 5 3 7 2 2 E S E S W N . C E S 8 9 3 3 - 7 4 1 3 - 8 7 7 2 - 7 1 0 2 - 8 7 6 1 - 7 9 1 1 - 7 9 4 - 8 1 2 - 1 0 2 - 3 2 9 2 2 . C E S 2 2 1 3 - 1 8 7 2 - 0 1 0 2 - 0 5 6 1 - 7 7 1 1 - 2 0 5 - 3 1 2 - 7 9 1 - 2 4 8 2 2 E S W S E S . C E S 5 5 1 3 - 8 9 7 2 ~ 4 2 0 2 - 0 7 7 1 ~ 0 0 2 1 - ? 9 4 ~ 5 4 8 2 2 W N E S E S . C E S 3 3 1 3 - 9 7 7 2 - 1 1 0 2 - 5 5 6 1 - 9 8 1 1 - 1 5 1 3 - 2 9 7 2 - 7 1 0 2 - 2 6 6 1 - 3 0 2 1 - 7 0 5 - 9 9 4 - 0 2 2 - 4 0 2 - 1 9 8 2 2 E S W S W N . C E S 5 9 8 2 2 E S . C E S 0 5 1 3 — 9 8 7 2 - 3 1 0 2 - 2 5 6 1 - 7 9 1 1 ~ 3 0 5 - 2 2 2 - 6 0 2 - 2 2 9 2 2 E N E S . C E S - 9 2 - 5 5 7 2 2 6 8 7 2 2 5 9 7 2 2 E S E S . C E S E N W N E S . C E S E S . C E S 1 0 4 3 - 8 4 1 3 - 2 8 7 2 - 0 1 0 2 - 3 5 6 1 - 4 7 1 1 - 8 7 3 3 ~ 9 2 1 3 - 2 6 7 2 - 2 9 9 1 - 0 8 6 1 - 0 7 1 1 - 6 4 1 3 - 9 7 7 2 - 6 0 0 2 - 0 5 6 1 - . 2 7 1 1 - 7 4 1 3 ~ 1 8 7 2 - 8 0 0 2 - 1 5 6 1 - 7 7 1 1 - 4 2 2 - 7 2 0 3 2 4 1 1 3 2 0 8 2 3 2 9 5 5 3 2 E N E N W N 1 . C E S W S E N . C E S E N E S E S . C E S E N E N W S . C E S 7 7 3 3 - 6 2 1 3 - 2 6 7 2 - 5 9 9 1 - 5 3 6 1 - 4 6 1 1 - 1 1 2 — 6 9 1 - 8 0 6 3 2 W S E N E S . C E S R B R T L C G N L S B B B S T I M R E P E T A T S N O I T A C O L 0 5 1 3 - 3 8 7 2 - 5 2 0 2 ~ 9 6 6 1 - 2 8 1 1 - 2 1 2 - 4 9 1 - 5 2 2 5 2 W N . C E S 9 2 1 3 - 7 6 7 2 - 8 9 9 1 - 8 2 6 1 - 7 5 1 1 - 5 0 2 - 8 8 1 - 8 1 6 2 2 E N E N 2 1 . C E S 7 0 1 3 - 5 4 7 2 - 4 7 9 1 - 6 9 5 4 6 3 1 1 ; 6 0 2 - 1 9 1 - 6 4 9 2 2 2 1 . C E S 9 6 7 2 - 8 8 9 1 - 8 1 6 1 - 8 4 1 1 - 6 9 1 - 9 7 1 - 4 3 7 2 2 E N E N 2 1 . C E S 5 9 0 3 ~ 3 3 7 2 - 5 5 9 1 ~ 2 2 1 1 - 8 9 1 - 2 8 1 - 9 0 4 4 2 E N E S 2 1 . C E S 6 4 0 3 - 3 9 7 2 - 1 4 4 2 - 5 3 6 1 - 3 6 1 1 - 6 6 4 2 ~ 2 6 6 1 - 4 9 1 1 - 3 6 4 1 7 7 - 3 8 4 2 - 4 6 6 1 - 3 1 2 1 - 5 8 7 - 8 2 3 - 7 3 - 6 5 - - 0 3 - 1 4 - 5 5 7 4 2 W N E S LIJ (D 9 1 . C E S 3 9 4 4 2 . W N w N 4m 2 9 1 . C E S 3 3 - 0 2 - 8 2 5 2 2 E S w 5 9 1 . C E S 4 0 2 3 - 8 6 9 2 - 0 1 6 2 - 8 3 8 1 - 5 0 5 1 - 5 9 9 - 9 8 1 - 2 7 1 - 0 1 3 4 2 E N E N 0 2 . C E S 3 6 0 3 - 1 0 8 2 - 7 4 4 2 - 3 4 6 1 - 8 7 1 1 - 3 7 7 - 9 9 2 - 9 2 - 7 1 - 9 9 4 2 2 w N w 5 9 1 . C E S 3 2 2 3 - 5 7 9 2 ~ 5 1 6 2 - 0 4 8 1 - 7 8 4 1 - 0 3 2 3 - 5 6 9 2 - 4 0 6 2 - 3 0 8 1 - 9 1 3 1 - 3 9 0 3 ~ 1 3 8 2 - 7 7 4 2 ~ 6 7 6 1 - 5 0 2 1 - 5 8 9 - 5 3 9 - 3 8 7 - 8 4 - . 9 1 7 4 2 8 1 . C E S 9 7 1 - 3 6 1 - 1 5 5 3 2 E S E N 2 2 . C E S 6 1 1 - 5 0 1 - 0 4 9 1 2 W S E S . C E S w 2 R S 5 T _ w G R B R T L C G M L S L T 8 5 T I M R E P E T A T S _ N 0 1 1 A 0 0 L 5 9 0 3 ' 4 3 8 2 - 7 7 4 2 ~ 8 6 6 1 - 6 1 2 1 - 3 0 8 - 6 2 3 - 2 4 - 4 5 8 4 2 E N W S W N 9 1 . C E S 7 5 8 2 - 2 9 4 2 - 1 8 6 1 - 2 3 2 1 - 1 2 8 - 2 4 8 2 - 7 8 4 2 - 3 8 6 1 - 6 3 2 1 - 0 2 8 - 2 2 8 2 - 9 6 4 2 - 8 6 6 1 - 5 9 1 1 - 7 8 7 - 6 9 4 2 - 0 8 6 1 - 4 2 2 1 - 4 1 8 - 6 3 3 - 9 2 3 - 5 3 3 - 8 0 3 - 2 5 - 0 7 9 4 2 E N W N E S 9 1 . C E S 5 4 - 7 9 9 4 2 W N W N 9 1 . C E S 2 5 - 0 9 0 5 2 E N W N W S 9 1 . C E S 8 2 - 6 4 1 5 2 W N E N W N 9 1 . C E S 0 8 0 3 - 8 1 8 2 - 3 6 4 2 - 6 5 6 1 - 4 7 1 1 - 3 0 8 - 0 1 3 - 4 2 - ' 1 7 3 3 2 E S W N W N 0 2 . C E S 4 8 0 3 - 6 2 8 2 - 5 7 4 2 - 0 7 6 1 - 8 9 1 1 - 6 0 8 - 6 1 3 - 3 9 9 2 ~ 9 2 7 2 - 9 7 3 2 - 9 6 5 1 ~ 6 0 1 1 - 1 1 7 - 4 5 2 - 1 4 8 2 - 8 8 4 2 - 0 8 6 1 - 6 1 2 1 - 5 0 8 - 8 2 3 - 5 4 - 3 3 - 6 1 8 4 2 1 4 8 4 2 3 0 8 3 2 W N W N E S 0 2 . C E S E N W S W N 0 2 . C E $ ~ W S 0 3 . C E S 9 5 0 3 ~ 7 9 7 2 - 1 4 4 2 - 8 1 6 1 - 5 8 1 1 - 4 6 7 - 3 3 - 7 2 - 2 8 8 3 2 E S E N W N 0 3 . C E S 9 3 8 2 ~ 5 8 4 2 - 5 7 6 1 - 8 2 2 1 - 2 1 8 - 2 3 3 - 6 4 - 5 2 6 4 2 E N W N W N 0 2 . C E S 2 4 9 2 - 4 7 6 2 - 8 2 3 2 - 7 1 5 1 - 3 4 0 1 - 4 6 6 - 0 3 2 - 4 6 9 2 - 2 0 7 2 - 4 5 3 2 - 6 4 5 1 - 0 8 0 1 - 6 8 6 - 2 4 2 - 2 3 / 3 2 / 0 8 6 2 - 4 3 3 2 ~ 1 3 5 1 - 9 5 0 1 - 9 7 6 ~ 5 3 2 - 1 3 / 1 1 # 6 3 x 2 4 / 6 7 8 2 2 w 5 w s 1 3 . C E S 2 8 2 3 2 W S E N W N 1 3 . C E S 3 9 8 3 2 W S ; w c 1 3 . C E S 4 2 7 2 - 1 7 3 2 ~ 3 7 5 1 - 9 0 1 1 - 3 1 7 - 2 5 2 - 3 1 / 8 2 / 8 7 3 4 2 W N é w 3 / N C 1 3 . C E S 8 0 7 2 - 5 6 3 2 - 7 6 5 1 - 8 7 0 1 - 7 9 6 - 9 4 2 - 6 1 { 9 2 / 3 8 3 1 2 a 3 / S c 1 3 . C E S 1 2 7 2 - 0 7 3 2 - 5 7 5 1 - 8 9 0 1 - 8 0 7 - 5 5 2 - 0 1 / 2 2 / 0 1 7 2 2 g w C 1 3 . C E S 1 9 6 2 - 2 4 3 2 - 4 3 5 1 - 8 5 0 1 - 4 7 6 - 2 3 2 - 2 3 / 3 4 / 0 9 7 2 2 W S g w 3 / N C 1 3 . C E S - 1 3 - 9 6 9 2 - 2 0 7 2 - 3 5 3 2 - 2 5 5 1 - 2 6 0 1 - 9 9 6 - 5 3 2 ~ 8 2 / 2 4 / 1 5 5 4 2 W N 1 3 . C E S 4 8 9 2 - 1 2 7 2 - 0 7 3 2 ~ 4 7 5 1 - 9 9 0 1 - 6 0 7 - 3 5 2 - 2 2 7 2 - 2 7 3 2 - 2 6 5 1 - 7 9 O I - 2 5 2 - 3 1 x 2 1 { 4 2 / 2 5 5 4 2 E S 1 3 . C E S 5 2 / 8 5 6 4 2 1 3 . C E S 6 5 7 2 - 6 0 4 2 - 4 8 5 1 - 3 5 1 1 - 3 4 7 - 9 8 2 - 2 2 - 1 1 - 6 4 7 4 2 E N E S 1 3 . C E S 0 0 0 3 - 6 3 7 2 - 8 8 3 2 - 5 7 5 1 - 8 2 1 1 - 8 2 7 - ? 7 2 ~ 7 4 7 2 - 0 9 3 2 - 6 7 5 1 - 8 9 0 1 - 1 2 7 - 0 7 7 2 - 8 1 4 2 - 5 8 5 1 - 0 4 1 1 - 5 4 7 - 8 4 7 2 - 6 0 4 2 - 3 9 5 1 ~ 1 1 1 1 - 3 3 7 - 3 8 2 - 8 2 7 2 - 9 7 3 2 - 1 7 5 1 - 7 1 1 1 - 4 1 7 - 1 6 2 - 9 3 7 2 - 9 8 3 2 - 5 8 5 1 - 9 1 0 1 - 1 2 7 - 9 6 2 - 4 2 7 2 - 1 8 3 2 - 8 6 5 1 - 0 0 1 1 - 9 9 6 - 1 6 2 - 5 / 4 - 7 1 / 0 1 / 7 1 / 2 1 / 7 8 7 4 2 0 3 9 4 2 3 4 9 4 2 4 4 9 4 2 5 9 9 4 2 5 7 0 5 2 4 8 0 5 2 E N W S E S 1 3 . C E S E S E N E S 1 3 . C E S E N W S , " 3 1 3 . C E S E N E S W N 1 3 . C E S 1 3 . C E S E S W N 1 3 . C E S E S E N 1 3 . C E S 9 4 7 2 - 1 0 4 2 - 8 7 5 1 - 7 2 1 1 - ? 2 7 ~ 5 7 2 - 8 9 0 5 2 E N ! " 5 N 1 3 . C E S 3 5 7 2 - 6 0 4 2 - 6 8 5 1 - 7 4 1 1 - 4 4 7 - 4 2 0 3 - 3 6 7 2 - 2 1 4 2 - 3 0 6 1 - 1 2 1 1 - 3 4 7 - 9 7 2 - 6 9 9 2 - 6 3 7 2 - 8 8 3 2 - 1 7 5 1 - 6 0 1 1 - 8 0 7 - 8 6 2 - 9 9 9 2 - 7 3 7 2 - 1 9 3 2 - 9 7 5 1 - 7 0 1 1 - 4 2 7 - 6 7 2 - 1 1 - 4 5 7 2 - 7 0 4 2 - 3 9 5 1 - 8 4 1 1 - 5 4 7 - 4 9 2 - 8 2 - 0 5 7 2 - 1 0 4 2 - 2 9 5 1 - 9 1 1 1 - 7 2 7 - 7 7 2 - 2 1 - - 2 3 - 1 0 3 5 2 2 9 3 2 2 1 3 4 2 2 2 0 9 3 2 4 0 4 4 2 5 6 4 4 2 E N E S 1 3 . C E S E N E S 2 3 . C E S E S E S 2 3 . C E S E S W S 2 3 . C E S W N W S E S 2 3 . C E S W S E N E S 2 3 . C E S L S L T B B G N R B R T L C 2 6 _ N O I T A C O L B S T I M R E P E T A T S W G R B R T L C G N L S L T B B B S T I M R E P E T A T S N O I T A C O L 9 0 0 3 - 3 5 7 2 ~ 7 0 4 2 - 1 9 5 1 - 2 4 1 1 - ? 3 7 ~ 0 9 2 - 3 2 - 1 1 - 4 5 6 4 2 E S E S 2 3 . C E S 1 1 0 3 - 7 4 7 2 - 0 0 4 2 - 9 8 5 1 ~ 0 1 1 1 - 3 2 7 - 9 7 2 - 1 1 — 1 { 8 8 6 4 2 E S E S W N 2 3 . C E S 5 5 7 2 - 4 0 4 2 - 7 8 5 1 - 0 3 1 1 — 7 3 7 - 3 8 2 ~ 6 1 — 1 - 7 8 5 4 2 W S W N W N 2 3 . C E S 5 4 7 2 - 3 0 4 2 - 4 9 5 1 - 8 3 1 1 - 8 3 7 - 4 8 2 - 8 1 - 6 - 5 4 7 4 2 W S W N E S 2 3 . C E S 9 3 7 2 - 0 9 3 2 - 9 7 5 1 - 4 1 1 1 - 9 1 7 - 2 7 2 - 9 9 9 2 - 6 3 7 2 - 0 9 3 2 - 4 8 5 1 - 6 6 0 1 ~ 0 3 7 - 9 7 2 - 6 2 0 3 - 6 6 7 2 - 0 2 4 2 - 3 0 6 1 - 1 6 1 1 - 2 5 7 - 1 0 3 - 3 1 - 2 3 - 0 2 - - 6 6 9 4 2 W N W N E S 2 3 2 3 , . C E S 5 6 7 4 2 1 3 9 4 2 E S W S W N 2 3 . C E S W S E S E S 2 3 . C E S 3 4 7 2 - 5 9 3 2 - 4 8 5 1 - 4 1 1 1 - 1 2 7 - 1 7 2 - 8 { 5 4 0 5 2 W S W S W N . C E S 7 6 7 2 - 7 1 4 2 - 3 0 6 1 - 0 7 1 1 - 1 6 4 7 9 2 - 6 1 - 6 4 0 5 2 W N W N 2 3 . C E S 0 3 7 2 - 9 8 3 2 - 6 8 5 1 - 6 0 1 1 - 5 1 7 ~ 3 7 2 - 5 % 1 3 1 5 2 W S W S E S 2 3 . C E S 6 6 9 2 - 9 5 7 2 - 9 0 4 2 - 5 9 5 1 - 4 6 1 1 - 8 4 7 - 6 9 2 - 5 1 - 3 8 1 5 2 W S W N 2 3 . C E S 5 0 0 3 - 1 4 7 2 - 3 9 3 2 - 7 7 5 1 ~ 9 0 1 1 - 9 1 7 - 3 7 2 - 0 8 7 2 2 W S W S E S 3 3 . C E S 4 0 2 3 - 1 4 9 2 - 2 8 5 2 - 8 8 7 1 - 1 0 3 1 - 3 6 8 - 4 5 3 - 6 8 - 2 7 - 8 4 0 2 2 E N E N E S 1 4 7 2 - 4 9 3 2 - 7 7 5 1 - 8 1 1 1 - 5 2 7 - 4 7 2 - 4 { 9 0 0 3 2 W S W S W N 3 8 8 2 - 8 2 5 2 - 9 8 8 2 - 2 3 5 2 - 7 4 7 1 - 9 8 2 1 - 5 4 8 - 5 4 3 - 6 0 9 2 - 2 5 5 2 - 4 1 7 1 - 4 1 3 1 - ' 6 6 8 - 4 5 3 - 1 9 8 2 - 5 3 5 2 ~ 8 4 7 1 - 3 9 2 1 - 8 4 8 - 4 4 3 - 0 8 - 5 2 5 1 2 5 4 8 1 2 6 9 3 2 2 6 7 7 0 2 W S W S W N W S E S E S W S W S W S E N E S E S 3 NNNM 3 . C E S . C E S . C E S . C E S . C E S . C E S w 3 R 5 5 T - 3 3 - 1 0 9 2 - 5 5 5 2 - 6 6 7 1 - 3 9 2 1 - 8 7 5 2 - 9 8 7 1 - 6 0 3 1 - 3 5 8 - 7 7 8 ~ 5 4 3 - 7 7 ~ 4 0 9 2 - 3 6 5 2 - 6 8 7 1 - 3 3 3 1 - 2 9 8 - 8 4 3 - 1 8 - 8 5 5 2 - 5 6 7 1 - 3 1 3 1 - 6 6 8 - 1 4 3 - 2 7 - 9 9 8 2 - - 6 6 5 2 - 3 7 7 1 - 8 9 2 1 - 1 7 8 - 4 5 3 - 7 7 5 2 ~ 9 8 7 1 - 7 7 2 1 - 1 9 8 - 5 5 3 ~ 9 7 8 2 - 1 4 5 2 - 4 4 7 1 - 4 7 2 1 - 4 4 8 - 1 4 3 - 8 6 - 1 8 5 2 - 0 0 8 1 - 2 5 3 I - 5 0 9 ~ 1 5 3 - 0 8 - 0 0 9 2 - 1 6 5 2 - 1 7 7 1 - 2 5 3 1 - 2 0 9 - 2 6 3 - 6 1 9 2 - 4 7 5 2 - 3 0 8 1 - 2 5 3 1 ~ 9 5 3 - 7 8 - 9 8 6 1 2 5 3 7 1 2 6 8 7 1 2 2 3 8 1 2 3 1 9 1 2 5 3 9 1 2 8 6 1 2 2 2 9 1 2 2 3 2 2 2 2 W S E N W N E S W N E S E S E N E S E S W S ' W S W S E S W S E S - 2 9 8 2 - 4 5 5 2 - 4 7 7 1 ~ 4 0 3 1 - 3 6 8 - 3 5 3 - 6 8 - 2 7 - 8 3 2 2 2 W S E S E S 1 9 8 2 - 8 4 5 2 ~ 6 5 7 1 - 1 1 3 1 - 1 7 8 - 8 5 3 ~ 9 3 2 2 2 E S E S d M - 4 3 - 0 0 9 2 - 8 5 5 2 - 6 1 7 4 1 0 3 1 - 4 7 8 - 9 4 3 ~ 9 7 - 7 6 - 1 8 3 1 2 E S W S 2 9 8 2 - 7 4 5 2 - 2 1 9 2 - 5 4 5 2 - 1 6 7 1 - 8 9 2 1 - 1 6 8 - . 5 4 3 ~ 3 5 3 - 8 7 - 5 6 - 7 4 9 0 2 W S E S 1 3 1 1 2 E S W S E S 3 7 8 2 - 0 1 5 2 - 7 3 7 1 - 1 7 2 1 - 7 4 8 - 8 0 9 2 - 1 7 5 2 - 4 8 7 1 - 0 5 3 I - 3 9 8 - 0 6 3 - 0 2 5 1 2 2 2 5 1 2 W S E N E S W S W S E S 3 9 8 2 - I 1 5 5 £ 5 6 7 1 - 2 3 3 1 - 1 8 8 - 8 5 3 - 7 8 - 6 6 5 1 2 W S W N E S 1 4 3 - 7 5 6 1 2 E N W S E S L S L T B B G N G R B R T L C W N O I T A C O L B S T I M R E P E T A T S on mmmmmmmmmmmmmmmmm . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S 1 7 1 3 - 4 1 9 2 - 7 5 5 2 - 2 7 7 1 + 8 1 3 1 - 1 6 3 - 8 8 ~ 1 0 2 2 2 E N W S E S 6 7 8 2 - 1 2 5 2 - 8 3 7 1 ~ 6 6 2 1 - 3 4 3 - 0 8 - 5 6 - 3 4 2 2 2 E S E S E S 5 1 9 2 - 8 6 5 2 - 0 0 8 1 - 2 5 3 1 - 4 5 3 - 0 8 - 7 6 - 6 6 2 2 2 W N W S 5 9 8 2 - 2 5 5 2 - 5 6 7 1 - 1 9 2 1 - 4 0 9 2 - 8 5 5 2 - 8 7 7 1 - 6 1 3 1 . 1 2 9 2 - 8 8 5 2 - 3 0 8 1 - 2 4 3 1 - 7 4 5 2 - 3 6 7 1 - 5 9 2 1 - 2 5 3 - 6 5 3 - 2 5 3 - 7 4 3 - 0 8 - 6 6 - 3 0 4 2 2 E S 5 6 - 8 7 8 2 2 W S E S 1 9 2 2 2 E S E S E S 4 6 3 2 2 E S E N W N 5 9 8 2 ~ 1 4 5 2 - 6 1 9 2 - 4 7 5 2 ~ 9 8 7 1 - 3 1 3 1 - 8 1 9 2 - 7 6 5 2 - 9 0 8 1 - 1 3 3 4 4 9 8 2 - 0 3 5 2 ~ 0 4 7 1 - 4 7 2 1 - 7 6 5 2 - 4 8 7 1 - 4 4 3 1 - 6 7 5 2 - 9 8 7 1 ~ 3 5 3 1 - 9 6 5 2 - 0 8 7 1 - 5 3 3 1 - . 0 6 5 2 - 1 7 7 1 - 5 0 3 1 - 0 7 1 3 - 5 1 9 2 - 9 5 5 2 - 6 6 7 1 - 2 5 2 1 - 8 5 3 ~ 2 5 3 - 7 5 3 - 5 6 3 - 4 6 3 - 4 7 3 - 4 5 3 - - - - - 0 7 2 3 2 E N W S - - - - - 2 2 4 3 2 W N W N 1 7 - 1 6 8 2 2 E N E S W N 9 7 - 0 0 9 2 2 E S 0 8 - 6 2 0 3 2 ! E N E N E S 6 4 3 2 2 E S E N W N 3 5 3 2 2 9 5 4 2 2 E N E S E S E N E N E S 0 7 4 2 2 E S E S E N 4 5 8 2 - 2 0 5 2 - 6 0 7 1 - 0 2 2 1 - 7 0 8 - 5 4 3 - 7 8 7 0 2 W N E N 3 7 5 3 - C , - - - 7 5 9 3 2 E N W S on 03 01 05 01 J? :T :3 :1 gr :1 :r :r :r :r :r :r 03 . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S - 5 3 - R B R T G N L T L C 2 9 _ N O I T A C O L B B B S T I M R E P E T A T S R B R T L C G N L S L T B S T I M R E P E T A T S N O I T A C O L 4 5 8 2 - 3 0 5 2 ~ 7 0 7 1 - 3 6 2 1 - 6 3 8 - 5 4 3 - 9 4 8 2 - 6 9 4 2 - 4 0 7 1 - 5 3 2 1 - 2 3 8 - 0 5 3 - 5 5 - 0 7 - 5 3 9 0 2 W S W N 8 w 0 2 E N E S E S 9 9 . C E S . C E S 0 6 8 2 - 0 1 5 2 - 1 1 7 1 - 6 9 2 1 - 5 2 8 - ? 3 3 ~ 7 5 ~ 4 7 6 0 2 E S O 1 . C E S 9 5 8 2 - 0 2 5 2 - 6 7 6 0 2 E N W S E S 0 1 . C E S 7 3 5 2 ~ 9 4 7 1 - 9 2 3 1 - 2 6 8 - 4 4 3 - 6 5 - 1 0 6 9 1 E N E S 0 1 . C E S 6 3 5 2 - ~ 8 4 7 1 - 3 9 2 1 ~ 5 4 8 - 8 4 3 - 2 6 - 2 2 3 2 E N W N E S 0 1 . C E S 2 0 1 3 - 5 4 8 2 - 0 9 4 2 - 5 9 6 1 - 6 4 2 1 - 9 1 8 - 1 6 8 2 - 1 1 5 2 - 7 2 7 1 ~ 6 7 2 1 - 6 2 8 - 1 3 3 - 6 3 3 - 1 7 - 6 5 - 1 5 - 3 3 7 0 2 9 9 7 0 2 w s E N E S O I . C E S E N W S W N 0 1 . C E S 9 7 8 2 - 9 3 5 2 - 1 3 8 2 - 7 7 4 2 - 1 9 8 2 - 4 3 5 2 - 7 6 8 2 - 3 1 5 2 - 4 2 7 1 - 9 6 2 1 - 7 3 8 - 9 3 3 ~ 7 5 8 2 - 5 0 5 2 - 9 1 7 1 ~ 3 6 2 1 - 2 2 8 - 5 2 3 - 0 6 - 5 4 - 9 1 - 0 6 0 1 2 E S E S O 1 . C E S 7 4 1 1 2 3 0 3 1 2 W N W N O 1 . C E S E N E N E S O 1 . C E S 8 1 5 1 2 E S W S 9 1 . C E S 7 4 7 1 2 E N E S 0 1 . C E S 5 6 8 2 - 5 1 5 2 ~ 8 2 7 1 - 3 9 0 3 - 1 4 8 2 - 6 8 4 2 - 0 0 7 1 - 7 4 2 1 - 3 2 3 ~ 9 6 8 2 - 4 1 5 2 - 7 4 8 1 - 4 3 7 1 - 5 6 2 1 - ? 3 8 ~ ? 3 3 ~ 3 2 5 2 ~ 6 3 7 1 - 4 5 2 1 - 7 3 8 - 0 3 3 ~ 6 6 1 2 2 8 6 2 2 2 1 0 3 2 2 1 7 3 4 2 w N E N SE 0 1 . C E S E S W S E S 0 1 . C E S W N E N E N 0 1 . C E S E N E S O 1 . C E S 9 5 8 2 ~ 7 0 5 2 - 9 1 7 1 - 5 6 2 1 - 9 1 8 - 6 3 3 ~ 4 5 7 1 2 N N E S O I . C E S - 6 3 - R B R T L C G N L S L T B B B S T I M R E P E T A T S N O I T A C O L 2 7 8 2 - 3 2 5 2 - 2 4 7 1 - 7 5 8 2 - 7 1 5 2 - 0 2 7 1 - 9 4 8 2 - 4 0 5 2 - 6 1 7 1 - 4 4 2 1 - 6 2 8 - 9 3 3 - 5 9 2 - 3 2 3 - 2 4 - 1 5 8 0 2 W S W S 1 1 . C E S 3 0 7 0 2 W N W S 1 1 . C E S 2 7 7 0 2 W S W S 1 1 . C E S 5 5 8 2 - 1 1 5 2 - 8 0 7 1 - 1 1 2 1 - 5 2 8 - 1 3 3 - 2 5 8 2 - 7 9 4 2 ~ 2 0 7 1 - 2 3 2 1 - 3 1 8 - 2 2 3 - 7 5 ~ 0 5 9 0 2 9 6 2 1 2 E S 1 1 . C E S W N E S 1 1 . C E S 9 9 8 2 - 9 9 8 2 - 3 4 5 2 - 7 4 7 1 - 2 6 2 1 - 0 3 8 - 4 4 3 - 1 6 - 4 0 3 1 2 W N W N 1 1 . C E S 6 5 8 2 - 7 0 5 2 - 2 1 7 1 - 5 0 2 1 - 6 1 8 - 5 2 3 ~ 2 7 8 2 - 7 2 5 2 - 9 3 7 1 - 7 3 2 1 ~ 9 3 8 ~ 2 4 3 - 3 2 1 3 - 5 6 8 2 - 0 1 5 2 - 1 1 7 1 - 5 2 2 1 - 8 1 8 - 8 2 3 - 6 6 - I 7 9 6 1 ~ 4 1 2 1 - 1 1 8 - 5 1 3 - 4 5 3 1 2 0 8 3 1 2 6 4 9 1 2 4 7 9 1 2 W S E N 1 1 . C E S M N M M 1 1 . C E S E N E S 1 1 . C E S E S 1 1 . C E S 6 9 0 3 - 3 4 8 2 ~ 9 8 4 2 - 0 0 7 1 - 5 2 2 1 - 5 1 8 - 6 1 3 - 1 5 - 8 8 9 1 2 W S E S E S 1 1 . C E S 4 0 5 2 - 8 0 7 1 - 0 6 2 1 - 4 2 8 - 3 1 3 ~ 6 5 1 2 2 W S E N W S 1 1 . C E S 8 3 1 3 ~ 8 7 8 2 - 2 2 5 2 - 1 3 7 1 - 0 8 2 1 - 4 2 8 - 4 4 3 - 4 4 8 2 - 9 8 4 2 - 5 8 6 1 - 7 0 2 1 - 1 9 7 ~ 6 1 3 - 5 0 1 3 ~ 0 5 8 2 - 7 9 4 2 ~ 9 0 7 1 ~ 9 4 2 1 - 6 1 8 - ? 1 3 ~ 2 5 - 0 7 0 3 - 1 1 8 2 - 8 5 4 2 - 5 5 6 1 - 8 7 1 1 - 9 7 7 - 6 8 2 - 2 6 0 3 - 8 0 8 2 - 6 5 4 2 - 7 5 6 1 ~ 9 8 1 1 - 7 8 2 - 4 2 - 7 6 8 2 - 2 1 5 2 - 1 2 7 1 - 4 6 2 1 - 2 2 8 - 0 3 3 - 3 6 - 8 7 7 2 2 1 8 7 4 2 9 0 9 0 2 2 7 5 1 2 8 4 0 3 2 6 0 3 3 2 W S E N E S 1 1 . C E S E S W S 2 1 . C E S E N W N 1 1 . C E S W S 2 1 . C E S W S W S 3 1 . C E S W S E S E S 3 1 . C E S - 7 3 - N S R T L C 6 N ; 4 L S L T B B B S T I M R E P E T A T S N O I T A C O L 4 7 0 3 - 5 1 8 2 - 5 6 4 2 - 4 7 6 1 - 7 4 2 1 - 0 0 8 - 7 0 3 - 6 4 - 2 3 - 4 9 7 3 2 W S W S 3 1 . C E S 7 7 0 3 ~ 6 1 8 2 - 3 6 4 2 - 2 6 6 1 - 1 9 1 1 ~ 4 7 7 - 2 9 2 - 6 2 - 3 1 - 9 6 7 4 2 E S W S E S 3 1 . C E S 0 3 8 2 - 6 7 4 2 - 6 8 6 1 - 1 0 2 1 - 2 9 7 ~ 0 6 2 - 0 9 8 0 2 E N E N W N 4 1 . C E S 9 3 8 2 - 1 9 4 2 - 6 0 7 1 - 0 3 2 1 - 1 2 8 - 3 1 3 ~ 9 4 - 5 3 ~ 8 3 9 0 2 E N d M 4 1 . C E S 2 8 0 3 - 4 3 8 2 - 2 8 4 2 - 6 9 6 1 - 7 7 1 1 ~ 0 0 8 - 5 0 3 ~ 7 3 8 2 - 3 9 4 2 - 7 0 7 1 - 6 1 8 - 2 8 4 2 - I 8 8 6 1 - 0 9 1 1 - 6 8 7 - 7 4 8 2 - 8 8 4 2 - 6 8 6 1 - 3 5 4 2 - 1 7 7 1 ~ 2 3 8 2 - 4 9 4 2 ~ 4 0 7 1 - 9 4 2 1 - 8 0 8 - ? 0 3 ~ 3 0 3 - 3 1 1 1 2 9 2 1 1 2 5 1 2 1 2 5 0 3 1 2 5 1 3 1 2 H N E N E S 4 1 . C E S W N W N E S ' 4 1 . C E S W N W S 4 1 . C E S W N W S E S 4 1 . C E S W S W N E S 4 1 . C E S 6 3 3 1 2 W N E S E S 4 1 . C E S 9 1 8 2 - 3 7 4 2 - 3 5 5 1 2 W S W S E S ~ 4 1 . C E S 0 2 8 2 - 9 7 4 2 ~ 9 8 6 1 - 6 3 2 1 - 3 9 7 - 9 8 2 - 0 1 ~ 9 7 5 1 2 W S E N W N 4 1 . C E S 2 4 8 2 - 5 9 4 2 - 6 4 7 1 - 1 1 8 - 3 0 3 ~ 3 2 - 0 4 6 1 2 E S 4 1 . C E S 3 1 8 2 - 8 6 4 2 - 2 7 6 1 - 0 3 2 1 - 0 0 8 - * 6 8 2 - 7 0 8 2 - 5 5 4 2 - 8 6 6 1 - 8 5 2 1 - 5 8 7 ~ 0 9 2 - 2 2 8 2 - 3 8 4 2 - 9 8 6 1 - 0 1 3 1 - 1 0 8 - 4 9 2 - 0 3 8 2 - 7 8 4 2 - 6 8 6 1 - 1 2 2 1 - 3 8 7 - 5 9 2 ~ 0 3 - 4 1 - 3 4 7 1 2 5 5 7 1 2 9 5 0 2 2 4 1 1 2 2 W S E N E S 4 1 . C E S E S E S 4 1 . C E S W S E S E S 4 1 . C E S W S E S W N 4 1 . C E S 3 0 5 2 - 5 9 6 1 ~ 3 1 2 1 . 0 0 3 - 3 2 - 9 6 1 2 2 E N W S E S 4 1 . C E S - 8 3 - W G R B R T L C L S L T B B B S T I M R E P E T A T S N O I T A C O L 6 5 0 3 - 0 1 8 2 - 2 6 8 2 2 E S E S E S 4 1 . C E S 1 2 8 2 - 3 7 4 2 ~ 0 9 6 1 - 0 6 2 1 - 1 4 - 6 2 - 0 2 9 2 2 E S E N 4 1 . C E S 9 8 0 3 ~ 4 2 8 2 - 1 7 4 2 - 5 7 6 1 - 6 0 1 1 - 1 8 7 - 1 4 8 2 - 1 9 4 2 - 2 0 7 1 - 6 5 2 1 - 9 1 8 - 2 5 0 3 2 9 1 5 3 2 E S E N E S 4 1 . C E S W N E N 4 1 . C E S 0 8 0 3 - 6 7 7 2 - 3 7 4 2 ~ 1 8 6 1 - 3 2 2 1 - 0 1 8 3 2 E N E S 4 1 . C E S 8 7 0 3 - 5 2 8 2 - 2 7 4 2 - 7 7 6 1 - 7 0 2 1 - 1 9 7 ~ 1 2 8 2 - 2 7 4 2 - 4 7 6 1 - 2 1 2 1 - 3 9 7 ~ 7 3 - 9 2 - 4 1 - 6 2 2 4 2 E S E N W S 4 1 . C E S 6 0 9 3 2 E N E S W N 4 1 . C E S 4 2 8 2 - 0 8 4 2 - 4 8 6 1 - 2 1 2 1 - 2 2 - 1 1 - 4 3 9 4 2 E S W S 4 1 . C E S 1 3 9 2 - 5 0 8 2 — 5 5 4 2 - 7 6 6 1 - 4 7 1 1 - 6 0 2 1 - 6 0 8 - 6 6 0 3 - 9 1 8 2 - 8 7 4 2 - 2 1 7 1 - 8 1 2 1 - ? 3 3 ~ 9 6 - 4 4 7 2 - 6 9 3 2 - 5 3 6 1 - 6 5 1 1 - 0 4 7 - 2 9 2 - 0 1 8 2 - 8 5 4 2 - 5 6 6 1 - 5 9 1 1 - 1 3 - 8 1 - 3 7 7 0 2 7 1 3 1 2 4 5 5 1 2 5 7 9 1 2 5 2 2 1 2 E N E S d M 5 1 . C E S W N 5 1 . C E S E N E S E S 5 1 . C E S E N E N W M 5 1 . C E S W S W S W S 1 2 . C E S 8 1 8 2 - 3 7 4 2 - 3 8 2 2 2 E S W S E S 4 1 . C E S 9 2 8 2 - 8 8 4 2 - 1 9 6 1 - 9 2 2 1 - 2 1 8 - 4 4 - 9 2 - 8 1 5 2 2 E N W S 4 1 . C E S 3 2 8 2 - 1 7 4 2 - 9 7 6 1 - 1 1 2 1 - 6 3 4 3 9 2 ~ 9 2 - 5 7 - 3 1 8 2 2 E S E S 4 1 . C E S 2 6 7 2 - - 2 1 4 2 - 0 1 6 1 - 9 3 1 1 ~ 9 3 7 ~ 7 8 2 - 8 1 - 9 6 7 2 - 0 2 4 2 - 2 1 6 1 - 2 4 1 1 - ? 3 7 ~ 7 6 2 - 2 - 3 - 2 1 { 4 4 3 1 2 W S W N d M 3 2 . C E S 5 9 5 1 2 E S E S - 3 2 . C E S - 9 3 - 3 5 0 3 ~ 7 8 7 2 - 5 3 4 2 ~ 9 3 6 1 - 3 6 1 1 - 6 4 7 - 4 7 2 - 1 1 - “ 4 { 1 9 7 1 2 E N E S 3 2 . C E S 9 0 0 3 ~ 4 5 7 2 - 6 0 4 2 - 7 0 6 1 - 4 3 1 1 - 9 4 7 - 7 6 2 - 1 { 5 1 / 8 1 9 1 2 E S W S E S . C E S 5 6 7 2 - 8 1 4 2 - 7 1 6 1 - 9 4 1 1 - 7 4 7 - 0 7 2 - 3 3 8 1 2 E S E S 3 2 . C E S 3 3 4 2 - 5 2 6 1 - 0 4 1 1 - 2 4 7 - 8 7 2 - 6 { 2 0 9 1 2 E S E S 3 2 . C E S 3 1 0 3 ~ 6 5 7 2 - 6 0 4 2 - 3 0 6 1 - 7 2 1 1 - 6 2 7 - 5 7 2 ~ 7 8 7 2 - 8 3 4 2 - 0 4 6 1 - 3 5 0 1 ~ 3 6 7 - 9 8 2 - 8 6 7 2 - 2 2 4 2 - 0 2 6 1 — 6 1 1 1 - I 5 7 ~ 8 6 2 - 9 8 7 2 - 9 3 4 2 - 1 3 6 1 - 3 6 7 ~ 8 7 2 - 7 9 9 2 ~ 4 4 7 2 - 4 9 3 2 - 3 9 5 1 ~ 7 0 1 1 - 1 1 7 - 5 5 2 - 8 { 1 7 7 2 ~ 9 1 4 2 - 4 2 6 1 - 5 4 1 1 - 4 3 7 - 5 7 2 ~ 1 1 - 3 { 9 1 { 1 3 9 1 2 9 8 9 1 2 4 - - 2 2 3 1 1 2 2 1 6 1 2 2 7 6 1 2 2 E N W S E S . C E S W S E N E S . C E S E S E S E S . C E S E S E N . C E S E S SE . C E S E S W S . C E S 1 1 8 2 - 4 6 4 2 - 2 6 6 1 - 5 9 1 1 ~ 5 8 7 ~ 4 9 1 2 2 E N E S W N . C E S 6 8 7 2 - 4 3 4 2 - 1 3 6 1 - 7 4 1 1 - 2 5 7 - 0 4 2 2 2 E S E S . C E S 3 6 7 2 - 2 1 4 2 - 4 1 6 1 - 3 4 1 1 - 4 3 7 - 4 7 2 - 8 { 4 4 2 2 2 W S E N E N . C E S 3 0 8 2 - 9 0 5 2 - 4 5 6 1 - 8 2 2 1 - 3 7 7 - 1 8 2 - 1 8 3 2 2 E N E S . C E S 1 0 8 2 - 8 4 4 2 - 8 5 6 1 ~ 0 9 1 1 - ? 8 7 ~ 0 9 2 - 0 1 - 1 2 4 2 2 E N E N . C E S 5 9 7 2 ~ 4 4 4 2 - 6 4 6 1 - 5 1 2 1 - 1 9 T - 8 9 2 - - - - 5 6 4 2 2 E N E S E S . C E S 2 6 4 2 - 0 6 6 1 - 5 8 1 1 - 6 5 7 - ? 7 2 ~ - - - - - 7 0 5 2 2 E N . C E S 3 9 7 2 ~ 4 4 4 2 - 9 5 6 1 - 7 5 1 1 - 9 4 7 ~ 6 7 2 - 5 6 5 2 2 E N W S . C E S - 0 4 - L C G N L S L T R B . R T ; 4 9 . N O I T A C O L T I M R E P E T A T S B B B S w c R B E I L 9 6 N L S L T B B B S _ T 1 M R E P E I A T S N O I T A C O L 1 4 0 3 - ‘ 8 8 7 2 ~ 6 3 4 2 ~ 2 4 6 1 - 0 6 1 1 ~ 3 4 7 - 2 8 2 ~ 0 1 ~ 7 4 4 2 ~ 3 4 6 1 ~ 1 4 6 ~ 5 9 7 2 - 4 4 4 2 ~ 1 4 6 1 ~ 6 9 1 1 ~ 1 0 8 2 ~ 8 4 4 2 ~ 7 4 6 1 ~ 0 0 2 1 ~ 5 8 7 ~ 5 8 7 - 5 8 2 ~ 0 2 ~ 8 8 2 ~ 2 2 ~ 8 0 8 2 ~ 3 5 4 2 - 3 6 6 1 ~ 5 9 1 1 ~ 5 8 7 - 6 9 2 ~ ~ - - 0 8 7 2 ~ 7 2 4 2 ~ 9 1 6 1 ~ 2 5 1 1 ~ 8 5 7 - 3 9 2 ~ - - - 4 { 8 - 9 - 7 6 5 2 2 E N 3 2 . C E S 3 4 9 3 2 4 4 9 3 2 2 3 3 1 2 1 4 9 1 2 E N E N E S 3 2 . C E S E N E N W S 3 2 . C E S E N E N E N 3 2 . C E S W S 4 2 . C E S W S W N 4 2 . C E S 5 9 7 2 - 2 4 4 2 ~ 4 4 6 1 ~ 2 9 7 2 ~ 2 4 4 2 ~ 0 4 6 1 ~ 4 8 1 1 ~ 2 6 4 2 ~ 0 6 6 1 ~ 8 9 1 1 ~ 5 8 7 - 9 1 7 - 8 9 2 ~ 7 2 ~ 3 1 - 4 0 1 2 2 W N W N 4 2 . C E S 0 9 2 ~ 2 2 ~ - ‘ - - 2 8 1 2 2 0 2 3 2 2 E S W N 4 2 . C E S W S W N 4 2 . C E S 7 3 0 3 ~ 1 8 7 2 ~ 9 2 4 2 - 4 2 6 1 ~ 1 7 1 1 ~ 6 6 7 ~ 5 8 2 ~ 7 1 ~ 8 5 4 2 2 W S W N W N 4 2 . C E S 3 1 8 2 ~ 2 6 4 2 — 1 6 6 1 ~ 7 9 1 1 ~ 5 7 7 ~ 0 9 2 ~ 4 2 ~ 1 1 - 1 8 8 2 2 W N E N W N 4 2 . C E S 5 6 0 3 ~ 6 5 0 3 ~ 8 3 0 3 - 2 7 7 2 ~ 0 2 4 2 ~ 8 0 6 1 ~ 5 4 1 1 ~ 9 0 8 2 ~ 6 5 4 2 ~ 8 5 6 1 ~ 1 0 2 1 ~ 5 0 8 2 ~ 4 5 4 2 ~ 2 5 6 1 ~ 2 1 2 1 ~ 5 8 7 - 9 9 2 ~ 7 0 8 2 ~ 5 5 4 2 - 1 5 6 4 8 8 1 1 ~ 4 1 4 8 8 2 ~ 3 0 8 2 ~ 1 5 4 2 ~ 8 4 6 1 ~ 7 6 1 1 ~ 3 6 7 ~ 7 8 2 ~ 8 1 ~ 2 1 8 2 ~ 2 6 4 2 ~ 1 6 6 1 ~ 1 9 1 1 ~ 1 9 7 - 5 9 2 - 9 2 - 4 - 5 1 - 0 2 2 3 2 0 9 7 3 2 9 3 9 3 2 3 8 0 4 2 E N W S 4 2 . C E S d M J N E N 4 2 . C E S E N 4 2 . C E S E S 4 2 . C E S 5 0 8 2 ~ 4 5 4 2 ~ 2 5 6 1 ~ 7 1 1 1 - 8 5 7 - 0 9 2 ~ 2 2 - 7 8 1 4 2 E N E S 4 2 . C E S - 1 4 - I 3 T - 8 8 7 ~ 8 7 2 ~ 0 1 ~ 4 { 5 8 9 2 2 E S E S 4 2 . C E S 9 0 3 ~ 5 3 - 2 2 - 0 5 0 3 2 W N M M E S 4 2 . C E S 7 3 0 3 ~ 8 7 T 2 - 2 2 4 2 ~ 0 3 6 1 ~ 6 3 1 1 - 1 5 7 ~ 0 7 2 ~ ; W G R B R T L C G N L S L T B B 8 8 6 { T I M R E P E T A T S _ N 0 1 T A C O L 4 4 3 4 2 W S J N W S 4 2 . C E S 2 5 0 3 ~ 4 9 7 2 - 3 4 4 2 ~ 0 5 6 1 ~ 1 8 1 1 ~ 7 1 8 2 ~ 5 6 4 2 - 0 6 6 1 ~ 8 8 1 1 ~ 5 1 8 2 ~ 8 5 4 2 ~ 8 4 6 1 - 0 0 2 1 ~ 6 6 4 2 ~ 5 6 6 1 ~ 2 8 1 1 ~ 9 7 7 ~ 5 6 7 ~ 1 7 7 - 2 7 7 - 0 9 2 ~ 4 2 ~ 1 1 ~ 0 5 4 4 2 E N E S W N 4 2 . C E S 2 0 3 ~ 2 3 - 8 1 ~ 4 7 5 4 2 E N E N I A M 4 2 . C E S 2 0 3 ~ 1 3 - 8 1 ~ 5 1 5 4 2 E N E S 4 2 . C E S 0 3 - 6 1 ~ 2 7 9 4 2 E N E N W N 4 2 . C E S 4 6 7 2 ~ 7 1 4 2 ~ 6 0 6 1 ~ 3 1 1 1 - 4 2 7 ~ 0 1 { 4 2 { 0 6 7 1 2 W N E S , " 4 ‘ N 5 2 . C E S 4 6 7 2 ~ 1 3 4 2 - 6 1 6 1 ~ 2 3 1 1 ~ 5 3 7 - 4 ~ 0 1 { 1 6 7 1 2 W N E S E S . C E S 5 9 3 2 ~ 5 8 5 1 ~ 1 2 1 1 ~ 8 3 T - 3 1 { 1 2 { 8 2 9 1 2 E S W N , W N . C E S 0 5 7 2 ~ 0 0 4 2 ~ 5 7 5 1 ~ 5 6 7 2 ~ 8 2 4 2 ~ 3 2 6 1 - 6 8 0 1 ~ 8 4 7 ~ 5 0 0 2 2 2 2 0 2 2 E S I ‘ I ‘ N E S . C E S E N W N . C E S 7 3 7 2 ~ 1 9 3 2 ~ 4 8 5 1 ~ 7 1 1 1 ~ 6 1 7 ~ ? 5 2 ~ If 0 2 { 0 2 & 2 W S E S . . C E S 6 2 7 2 ~ 8 9 3 2 ~ 8 7 5 1 - 6 1 1 1 ~ 8 1 7 ~ 8 5 2 ~ 1 1 { 1 2 { 7 8 & 2 E S W S . C E S 1 1 4 2 ~ 9 0 6 1 ~ 4 3 7 ~ 4 1 2 ~ 9 / 1 2 { 9 2 6 1 2 d M d M d N 5 2 . C E S 5 5 7 2 - 6 0 4 2 ~ 0 1 6 1 ~ 3 3 1 1 ~ 0 3 1 - 8 6 2 - 2 4 1 2 2 W N W S 3 0 0 3 ~ 9 3 7 2 ~ 7 8 3 2 ~ 6 8 5 1 ~ 3 0 1 1 ~ 0 2 7 ~ 2 5 2 ~ 4 1 { 7 2 / 4 6 1 2 2 E S E N . C E S 4 4 7 2 ~ 5 0 4 2 ~ 5 0 6 1 ~ 3 3 1 1 ~ 3 2 7 ~ 2 6 2 - 6 5 7 2 - 0 1 4 2 ~ 4 0 6 1 ~ 5 1 1 1 ~ 4 3 7 - 9 5 2 ~ 1 9 1 2 2 3 9 1 2 2 W S E N W N . C E S , » ’ 4 5 E S . C E S 8 2 7 2 - 0 8 3 2 ~ 7 7 5 1 - 8 0 1 1 ~ 0 1 7 - 6 4 2 - 8 1 { 1 3 / 6 9 1 2 2 E S W S E S . C E S - 2 4 - W G R B R T L C G N L S L T B B 8 5 T I M R E P E T A T S _ 3 N O I T A C O L 0 6 7 2 ~ 8 0 4 2 ~ 6 0 6 1 ~ 9 1 1 1 - 5 3 7 - 0 6 2 ~ 3 / ' 6 1 { 4 7 2 2 2 W N E N E S . C E S 0 0 0 3 - 1 4 7 2 ~ 2 9 3 2 ~ 6 8 5 1 ~ 6 2 1 1 - 8 3 7 - 0 2 3 ~ 3 3 7 2 ~ 4 8 3 2 ~ 1 8 5 1 ~ 0 1 1 1 4 ? 2 7 ~ 7 6 2 ~ 9 2 7 2 ~ 1 8 3 2 ~ 1 8 5 1 ~ 7 0 1 1 ~ 2 2 7 ~ 9 4 2 ~ 5 1 / 9 2 { 5 7 7 2 ~ 8 0 4 2 ~ 8 9 5 1 ~ 0 2 1 1 - 8 3 7 - 8 5 2 ~ 2 5 7 2 ~ 3 0 4 2 - 1 0 6 1 ~ 3 1 1 1 ~ 1 2 7 ~ 1 6 2 ~ 8 2 7 2 ~ 0 8 3 2 - 6 1 5 4 7 6 0 1 ~ 4 1 7 ~ 3 6 2 ~ 2 2 7 2 ~ 3 7 3 2 - 5 6 5 4 0 1 1 1 ~ 2 1 7 ~ 5 6 2 ~ 1 { 4 { 1 { 1 ~ 5 2 / 8 1 { 5 1 / 4 1 { 5 9 6 1 2 E S W N E S . C E S 5 0 3 2 2 2 8 3 2 2 2 6 4 2 2 1 6 0 3 2 9 0 3 3 2 0 8 7 4 2 W S E S . C E S W S E S E S . C E S E S E S r C E S E N W S W S . C E S W S E N . C E S E S W N . C E S 6 5 7 2 - 4 5 7 2 - 0 1 4 2 ~ 7 0 6 1 ~ 2 3 1 1 ~ 0 4 7 ~ 0 7 2 ~ 9 8 8 1 2 E N E N E S . C E S 4 0 4 2 ~ 1 0 6 1 ~ 1 4 1 1 ~ 0 3 7 ~ 9 6 2 ~ 0 1 { 2 9 8 2 2 E N E N W N . C E S 0 5 7 2 ~ 1 0 4 2 ~ 0 9 5 1 - 1 3 1 1 ~ 5 2 7 ~ 6 ~ 1 { 5 2 0 3 2 E N W N E S . C E S 3 6 9 2 - 0 0 7 2 ~ 3 5 3 2 - 9 4 5 1 ~ 4 0 1 1 ~ 6 9 6 ~ 1 5 2 ~ 7 3 7 2 ~ 7 8 3 2 ~ 2 2 7 ~ 3 8 2 ~ 3 2 7 2 ~ 4 7 3 2 - 3 7 5 1 ~ 7 1 1 1 ~ 6 1 7 ~ 1 5 2 ~ 6 1 7 2 ~ 0 7 3 2 ~ 4 6 5 1 ~ 8 0 1 1 ~ ? 1 7 ~ 3 5 2 ~ 2 0 7 2 ~ 5 5 3 2 - 7 4 5 1 ~ 3 6 0 1 ~ 1 5 2 ~ 5 1 { 3 1 { 3 1 { 2 1 9 2 - 9 0 7 2 ~ 8 5 3 2 ~ 9 4 5 1 ~ 4 0 1 1 ~ 6 9 6 ~ 7 4 2 ~ 6 2 { - 3 4 - 9 9 9 2 ~ 3 4 7 2 ~ 4 9 3 2 ~ 7 9 5 1 - 2 1 1 1 ~ 8 1 7 ~ 3 6 2 ~ O 4 1 { 8 2 { 8 3 4 2 2 E N E N W N 6 3 . C E S 6 2 { 5 1 5 2 2 E N E N E S 6 3 . C E S 7 2 { 0 3 { 6 9 5 2 2 6 3 6 2 2 1 7 9 2 2 E N E S E S 6 3 . C E S E N E S 6 3 . C E S E N , 4 4 N E S 6 3 . C E S 5 3 5 4 2 2 6 3 1 2 E N E S E S . C E S E N E S E N . C E S _ W G R B R T L C G N L S L T B B 8 5 T I M R E P E T A T S N O I T A C O L 3 3 9 2 ~ 0 7 6 2 ~ 3 2 3 2 - . 1 1 5 1 ~ 1 5 0 1 ~ 9 5 6 ~ 8 2 2 ~ 6 3 { 8 4 { 8 1 1 3 2 E S E S E S 6 3 . C E S 9 4 9 2 ~ 4 8 6 2 ~ 7 3 3 2 - 7 2 5 1 ~ 4 4 0 1 ~ 7 6 6 ~ 4 3 2 ~ 8 2 { 6 7 9 2 ~ 3 1 7 2 ~ 2 6 3 2 ~ 6 5 5 1 ~ 7 8 0 1 ~ 3 9 6 - 4 4 2 ~ 1 2 { 1 4 { 4 3 { 9 4 3 3 2 3 9 7 4 2 E S E N E S 6 3 . C E S E N E N \O m . C E S 3 4 9 2 - 7 1 7 2 ~ 0 7 3 2 - 4 5 5 1 - 6 2 1 1 ~ 6 2 7 ~ ? 5 2 ~ 9 { 2 3 / 0 5 7 3 2 W S ] E N 3 2 7 2 ~ 6 7 3 2 - 0 6 5 1 ~ 2 2 1 1 ~ 4 2 7 ~ ? 5 2 ~ 1 1 { 2 2 { 6 3 0 4 2 , % 4 5 W N 8 0 7 2 ~ 2 6 3 2 ~ 8 4 5 1 ~ 4 3 1 1 ~ 1 2 7 ~ 6 4 2 ~ 1 9 0 4 2 W S E S 9 6 9 2 ~ 1 1 7 2 ~ 7 6 3 2 ~ 6 5 5 1 - 8 3 1 1 - 4 2 7 ~ 1 5 2 ~ 7 0 7 2 ~ 3 6 3 2 ~ 8 4 5 1 ~ 8 2 1 1 ~ 9 2 7 ~ 3 5 2 ~ 3 1 { 2 1 { 5 2 / 5 2 / 0 6 4 4 2 W S E S 6 3 6 4 2 W S E S E N 8 3 9 2 - 4 2 7 2 ~ 5 7 3 2 - 9 5 5 1 ~ 0 2 1 1 ~ 9 1 7 - 5 4 2 ~ 3 1 / 6 2 { 9 8 6 4 2 W N W S E S 9 7 9 2 - 8 0 7 2 ~ 1 6 3 2 ~ 3 7 9 2 - 7 0 7 2 ~ 0 6 3 2 ~ 3 4 5 1 ~ 4 3 1 1 ~ 8 1 7 - 1 5 2 ~ 9 2 7 4 2 3 1 8 4 2 E S W S W S E S W S E S 3 0 7 2 ~ 9 5 3 2 ~ 6 4 5 1 ~ 0 2 1 1 ~ 0 2 7 ~ 1 5 2 ~ 2 1 { 5 2 / 3 2 7 4 2 W S W S E S 7 8 9 2 ~ 3 2 7 2 ~ 6 7 3 2 ~ 7 6 5 1 ~ 9 9 0 1 - 9 1 7 ~ 6 6 2 ~ 2 1 { 5 2 6 2 2 E S W N 2 0 7 2 ~ 6 5 3 2 - 1 4 5 1 ~ 7 3 1 1 ~ 3 2 7 ~ 1 5 2 ~ 3 1 / 6 2 { 7 7 0 5 2 W S E S E S 2 3 7 2 - 7 8 3 2 - 3 7 5 1 ~ 9 0 1 1 ~ 9 2 7 ~ 1 7 2 - 1 { 7 9 2 2 2 W N ] C I M E S 9 3 7 2 - 1 9 3 2 ~ 7 7 5 1 ~ 8 1 1 1 ~ 5 2 7 ~ 8 7 2 ~ 1 1 ~ 5 6 3 2 2 W N E N W N 4 8 9 2 ~ 0 2 7 2 ~ 3 7 3 2 - 2 6 5 1 ~ 6 9 0 1 ~ 4 3 7 - 0 6 2 ~ 8 8 9 2 ~ 3 1 7 2 ~ 5 6 3 2 - 7 5 5 1 ~ 9 0 1 1 ~ 0 1 7 ~ 0 7 2 - 2 { 6 ~ - 4 4 - 6 { 6 6 0 3 2 1 W S E N 5 1 / 9 4 0 3 2 W N W S 1 61 fifi flfi GW 03 NW OW 00 «1 (V) :T :r :r :r .1)“ . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S W 2 R S 6 T - - - 9 9 1 2 - 6 9 9 2 - 1 1 9 1 - 0 0 1 1 - 1 2 1 - 9 9 2 - 1 - 1 1 / 1 9 9 9 2 M N S N 3 8 4 ' 9 3 5 2 6 6 2 - 9 2 1 2 - 9 1 9 2 - 6 9 9 1 - 9 9 0 1 - 6 6 9 - 9 4 2 - 0 2 / 4 9 / 9 1 1 9 2 E N 3 9 M N - - - 6 1 1 2 - 0 1 9 2 - 9 0 9 1 - 9 6 0 1 - 9 0 1 - 1 9 2 - - - - - - - 1 1 1 9 2 3 N M S 3 8 4 4 ~ 5 3 3 ' 3 3 s 9 1 6 2 - 2 1 1 2 - 9 9 9 2 - 9 9 9 1 - 0 1 1 1 - 9 1 1 - 9 9 2 - 1 / 9 1 / 9 2 6 9 2 a s M N M N 4 ' 3 3 8 9 1 6 2 - 2 1 1 2 - 9 9 9 2 - 9 9 9 1 - 9 0 1 1 - 9 0 1 - 1 4 2 - 9 1 / 1 9 / 0 6 6 9 2 a s 3 N M N 4 ' 3 3 5 - - - 9 9 1 2 - 1 9 9 2 - 1 1 9 1 - 1 1 1 1 - 6 0 1 - 0 9 2 - 1 / 6 1 / 9 1 1 4 2 3 N M N 3 8 4 ' o a s - - - 1 2 1 2 - 4 1 9 2 - 0 9 9 1 - 4 6 0 1 - 4 0 1 - 0 9 2 - 9 1 / 2 9 / 4 4 1 4 2 E N 3 3 3 S 4 ' 3 3 9 - - - 2 2 1 2 - 9 9 9 2 - 0 9 9 1 - 9 1 1 1 - 2 1 1 - 6 4 2 - 6 1 / 2 9 / 2 1 9 4 2 3 9 S N 3 S 4 ' 3 3 8 9 9 6 2 - 0 6 9 2 - 9 4 9 2 - 4 9 9 1 - 4 2 1 1 - 9 1 1 - 6 4 2 - 9 1 / 6 2 / 2 9 4 4 2 a s 3 3 3 8 4 ' 9 3 5 1 1 0 9 - 9 4 1 2 - 9 6 9 2 - 1 1 9 1 - 9 1 1 1 - 4 2 1 - 1 1 2 - 1 / 9 1 / 6 9 4 4 2 3 N M N M N 4 ' o a s - - - 9 2 1 2 - 1 1 9 2 - 2 1 9 1 - 1 9 0 1 - 2 0 1 - 1 9 2 / 6 1 / 6 2 / 4 9 4 4 2 E N a s M S 4 ' 3 3 5 9 6 6 2 - 9 9 1 2 - 9 9 9 2 - 9 9 1 - 9 0 1 1 - 0 1 1 - 2 9 2 - 2 / 9 1 / 0 9 9 4 2 3 N M N M S - - - 6 4 1 2 - 9 6 9 2 - 9 9 9 1 - 4 0 1 1 - 9 1 1 - 1 1 2 - - - - - - - 9 0 1 4 2 E N E N E N - - - 9 2 1 2 - 6 1 9 2 - 1 9 9 1 - 9 0 1 1 - 9 2 1 - 9 9 2 - - - - - - - 1 0 9 4 2 M N 3 N M N 4 9 9 ' o a s “ 9 3 5 ~ 3 3 3 - - - 1 9 1 2 - 4 6 9 2 - 1 1 9 1 - 9 1 1 1 - 9 9 1 - 1 9 2 - 9 1 - 0 6 6 9 4 2 E N M N M N 9 ' 0 3 5 9 6 6 2 - 2 9 1 2 - 4 9 9 2 - 9 1 9 1 - 9 0 1 1 - 9 2 1 - 9 1 2 - - - - - - - 6 9 6 4 2 M N 3 N a s 1 0 0 9 - 9 9 1 2 - 1 6 9 2 - 9 9 9 1 - 9 0 1 1 - 9 2 1 - 1 1 2 - 1 1 - 2 / 6 1 6 4 2 E N M N 3 9 9 9 ' 3 3 5 ' 3 3 5 s u b h - - - - 1 4 1 2 - 9 6 9 2 - - - - - - - - - - - - - - — - - - - 4 1 1 9 2 3 8 M S M N 4 ' 3 3 9 M 0 2 9 S 1 1 0 S N T S 1 1 9 9 S S l I W H B d 3 1 v 1 S 0 1 1 v 0 0 1 _ 9 0 R B R T L C G N L S L T B B 8 8 T I M R E P E I A T S N O I T A C O L 8 8 9 2 ~ 1 3 7 2 ~ 4 8 3 2 ~ 3 8 5 1 - 5 0 1 1 ~ 8 1 7 ~ 5 7 2 - 5 / 0 6 1 5 2 W N 8 0 9 2 ~ 2 4 6 2 ~ 6 9 2 2 ~ 4 8 4 1 ~ 3 6 0 1 ~ 7 6 6 ~ 5 2 2 ~ 5 3 / 8 4 { 6 3 1 2 2 W S E N W N 6 8 9 2 ~ 4 2 7 2 ~ 6 7 3 2 - 7 5 5 1 - 2 2 1 1 ~ 4 1 7 - 9 6 2 ~ 6 - 8 { 3 7 0 4 2 E N E N W N 8 4 9 2 - 2 8 6 2 ~ 3 3 3 2 - 5 2 5 1 - 8 4 0 1 ~ 8 7 6 ~ 2 3 2 ~ 8 2 { 2 4 { 2 9 7 4 2 E N W S J - I N 9 1 9 2 - 5 5 6 2 ~ 3 1 3 2 - 7 9 4 1 - 3 8 0 1 ~ 8 7 6 ~ 2 4 2 ~ 3 I / 5 2 / 4 3 8 1 2 E S E S E S 7 4 9 2 ~ 0 8 6 2 ~ 2 3 3 2 - 9 1 5 1 ~ 7 8 0 1 ~ 9 8 6 ~ 4 4 2 - 5 2 9 2 ~ 6 5 6 2 ~ 2 1 3 2 ~ 4 9 4 1 ~ 0 8 0 1 ~ 9 6 6 ~ 7 3 2 - 5 1 / 2 2 { 9 2 { I 8 1 0 3 2 E N E N W N 6 3 / 5 7 8 3 2 E N W S E S 9 3 9 2 - 5 7 6 2 ~ 3 3 3 2 - 5 2 5 1 ~ 1 6 0 1 ~ 9 8 6 ~ 5 4 2 ~ 1 1 { 9 2 / 6 5 9 1 2 E N W S E S 4 5 9 2 ~ 0 8 6 2 ~ 4 4 3 2 ~ 3 3 5 I - 0 6 0 1 ~ 9 4 6 ~ 9 4 2 ~ 1 1 { 4 2 { 9 1 0 2 2 W N E N E S 4 3 9 2 ~ 3 7 6 2 - 2 3 3 2 ~ 2 2 5 1 ~ 9 0 1 1 - 4 0 7 - 9 5 2 - 3 / 7 3 9 2 - ' 0 7 6 2 ~ 7 2 3 2 ~ 6 1 5 1 ~ 1 0 1 1 ~ 6 8 6 ~ 1 5 2 ~ 2 1 { 3 1 / 1 2 { 8 3 0 2 2 E S W N E S 7 3 1 2 2 E S E N E S 5 5 9 2 ~ 3 9 6 2 ~ 7 4 3 2 ~ 1 3 5 1 - 4 9 0 1 ~ 0 0 7 ~ 0 6 2 ~ 2 { 4 1 { 0 1 5 2 2 W N M ‘ I 4 1 N 8 5 6 2 ~ 7 1 3 2 ~ 8 9 4 1 ~ 8 1 1 1 ~ 4 9 6 ~ 2 5 2 ~ 0 1 { 1 2 { 2 3 7 2 2 E S W S E S 5 5 6 2 ~ 2 1 3 2 ~ 4 9 4 1 ~ 1 9 6 ~ 9 4 2 ~ 2 1 { 4 2 { 1 5 7 1 2 E S E S E S 7 4 9 2 ~ 5 8 6 2 ~ 9 3 3 2 - 0 3 5 1 ~ 9 5 0 1 - 0 9 6 ~ 2 4 2 - 8 1 { 5 5 9 2 ~ 1 9 6 2 ~ 7 4 3 2 ~ 4 3 5 1 ~ 4 7 0 1 ~ 6 8 6 ~ 0 5 2 ~ 0 1 { 0 3 / 2 2 { 0 8 1 3 2 8 9 2 3 2 7 4 9 2 ~ 1 8 6 2 ~ 9 3 3 2 - 7 2 5 1 ~ 7 9 0 1 - 7 8 6 ~ 0 5 2 ~ 1 1 { 3 2 { . 4 8 0 4 2 0 7 6 2 ~ 8 2 3 2 ~ 6 1 5 1 ~ 4 2 1 1 ~ 1 9 6 ~ 1 5 2 ~ 1 { 9 1 / 1 9 7 4 2 ! 1 N E N W N E N W N E 5 W N E S E S W S E N E S Ln \0 \D \O r- P~ P~ d3 d3 GD G3 G3 d3 03 GD 03 03 03 . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S - 6 4 - 4 8 9 2 ~ 0 4 3 2 ~ 3 2 5 1 - 5 2 1 1 ~ 1 1 7 - 5 4 2 ~ 0 5 3 2 ~ 7 3 5 1 - 7 1 1 1 ~ 4 1 7 ~ 9 4 2 ~ 9 3 3 2 - 3 2 5 1 - 1 2 1 1 - 3 1 7 - 7 4 2 ~ 5 1 / 1 1 { 9 1 { 3 2 3 2 ~ 0 1 5 1 ~ 3 2 1 1 ~ 9 9 6 ~ 3 5 2 ~ 8 3 3 2 ~ 5 2 5 1 ~ 9 0 1 1 ~ 5 0 7 - 2 6 2 ~ 1 1 3 2 ~ 4 9 4 1 ~ 3 0 1 1 ~ 9 8 6 ~ 0 4 2 ~ 2 2 { 3 3 3 2 - 8 1 5 1 ~ 1 1 1 1 ~ 3 0 7 - ? 3 2 ~ 5 2 { 4 2 3 2 ~ 7 0 5 1 ~ 8 0 1 1 ~ 9 9 6 - 8 3 2 ~ 7 2 / 2 1 3 2 ~ 7 9 4 1 - 1 9 0 1 ~ 9 7 6 ~ 7 4 2 ~ 8 2 3 2 ~ 8 0 5 1 ~ 7 2 1 1 ~ 6 8 6 ~ 6 5 2 ~ 8 2 { 0 2 { 6 3 0 5 2 9 5 1 5 2 7 9 1 5 2 2 1 2 5 2 7 5 9 1 2 5 4 0 2 2 7 9 5 2 2 7 7 6 2 2 1 3 5 4 2 1 4 6 4 2 1 ' I S E S E S W S W N E S W S W N W N W N W S W N W S W S ! » N E S W N W S E 8 8 8 8 8 8 8 9 9 . C E S . C E S . C E S . C E S . C E S . C E S . C E S . C E S E N E S O 1 . C E S W S E N E S 0 1 . C E S E N W N W N O I . C E S E N W N E S 0 1 . C E S I 3 3 2 - 9 1 5 1 ~ 0 2 1 1 ~ 5 0 7 ~ 9 5 2 - 6 1 { 6 7 0 5 2 3 2 3 2 - 1 1 5 1 ~ 5 0 1 1 ~ 7 9 6 - 3 5 2 - 5 4 3 2 ~ 1 3 5 1 - 0 9 0 1 ~ 8 9 6 ~ 5 5 2 - 3 2 / 7 1 / 4 6 9 4 2 E S W S W N L C G N T R T A C O L N O I L S B S T L M R E P E T A T S 5 6 9 2 - 3 5 3 2 ~ 1 4 5 1 ~ 0 3 1 1 ~ 4 2 7 ~ 0 1 { 3 2 / 6 6 6 4 2 W N ] W N W N O 1 . C E S 1 7 9 2 - 7 5 3 2 - 3 0 9 4 2 E N E N d N 0 1 . C E S 1 5 3 2 ~ 6 3 5 1 ~ 1 3 1 1 ~ 8 1 7 ~ 2 5 2 - 4 1 { 6 2 { 6 1 9 4 2 W N E N W N 0 1 . C E S 5 5 9 2 ~ 0 0 9 2 ~ 7 4 3 2 ~ 3 0 0 5 2 W N E N E N 0 1 . C E S 0 9 2 2 ~ 2 7 4 1 ~ 2 7 0 1 ~ 4 6 6 ~ 9 1 2 ~ 0 4 { 2 5 { 0 9 9 1 2 E S W N 5 1 . C E S - 7 4 - 3 6 6 4 2 E N E S 0 1 . C E S w 0 R T L C B B B S T I M R E P E T A T S _ _ 3 N O I T A C O L 9 8 8 2 ~ 3 8 2 2 ~ 4 6 4 1 ~ 8 5 0 1 ~ 4 1 9 2 ~ 6 0 3 2 ~ 0 9 4 1 ~ 4 0 1 1 ~ 1 9 8 2 ~ 2 8 2 2 ~ 7 6 4 1 ~ 9 5 0 1 - 7 4 6 ~ 1 4 { 8 1 { 4 3 { 4 5 { 9 2 { 5 4 { 5 9 0 2 2 1 5 8 1 2 9 2 0 2 2 W S I 1 1 4 N E S 5 1 . C E S W N E S J - M 6 1 . C E S E S E N E S 6 1 . C E S 2 0 9 2 ~ 0 0 3 2 ~ 4 8 4 1 ~ 4 7 6 ~ 8 1 { 0 3 { 0 7 0 2 2 W N W S W N 6 1 . C E S 0 2 9 2 ~ 5 1 3 2 ~ 6 9 4 1 - 0 0 1 1 ~ 8 7 6 ~ 0 1 { 3 2 { 7 9 0 2 2 ! A N 6 1 . C E S 6 1 9 2 ~ 8 0 3 2 ~ 5 9 4 4 8 6 0 1 ~ 6 8 6 ~ 4 1 { 7 2 { 4 0 2 2 2 W N 6 1 . C E S 2 1 9 2 ~ 6 0 3 2 ~ 0 9 4 1 ~ 6 8 0 1 ~ 4 1 { 7 2 { 1 5 7 2 2 E N W N ! 1 N 7 1 . C E S 6 9 8 2 ~ 0 9 2 2 ~ 2 7 4 1 ~ 7 3 0 1 ~ 6 4 6 ~ 3 0 9 2 ~ 0 0 3 2 ~ 7 8 4 1 ~ 9 6 0 1 ~ 0 7 6 ~ 3 0 9 2 - 4 9 8 2 ~ 7 9 2 2 ~ 1 8 4 1 ~ 3 7 0 1 ~ 8 6 6 ~ 7 8 2 2 - 0 7 4 1 ~ 8 4 0 1 ~ 1 5 6 - 1 1 3 2 ~ 4 9 4 1 ~ 9 9 0 1 - 0 8 6 ~ 4 2 { 1 3 { 1 2 { 1 2 { 6 ‘ 3 { 5 3 { 5 4 { 4 3 { 5 3 { 1 5 { 7 5 7 2 2 3 3 8 2 2 6 0 0 3 2 5 7 1 3 2 9 1 3 3 2 E N E N E S 7 1 . C E S E N E S W N 7 1 . C E S E N W N E S 7 1 . C E S E N E S E S 7 1 . C E S 7 1 . C E S . 4 1 9 2 ~ 7 0 3 2 - 3 8 4 1 ~ 5 6 0 1 ~ 4 5 6 ~ 2 2 { 5 3 { 9 6 1 4 2 E N E N W N 8 1 . C E S 7 8 2 2 ~ 0 7 4 1 ~ 7 2 0 1 ~ 5 4 6 ~ 9 3 { 3 5 { 3 7 2 3 2 W S W N W N 6 1 . C E S 8 9 2 2 - 9 7 4 4 8 6 0 1 ~ 6 6 6 ~ 6 2 { 8 3 { 3 1 4 3 2 W N W S E S 6 1 . C E S 4 0 3 2 ~ 1 8 4 1 ~ 7 7 0 1 - ? 7 6 ~ 8 1 3 2 ~ 7 9 4 4 3 0 1 1 ~ 3 9 6 ~ 3 2 { 3 1 { 5 3 { 6 2 { 6 8 2 1 2 0 0 2 2 2 E N E S , f I 7 1 . C E S E N E N W N 7 1 . C E S - 8 1 1 - 0 1 9 2 ~ 3 8 8 2 ~ 3 7 2 2 ~ 3 6 4 1 ~ 3 0 0 1 ~ 2 0 6 ~ 8 5 { 1 7 { 9 7 0 3 2 E N W S E S 2 1 . C E S 9 9 2 2 - 0 9 4 1 ~ 7 2 0 1 ~ 6 4 6 ~ 2 4 { 6 5 { 8 7 0 5 2 W S W N W N . C E S W 3 R 5 6 T 11CHIan STATE UNIV. LIBRARIES IIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIII 31293100340508