Report on the 1993 Exploration Program
on the
B X Claims
115 P 15
Dawson Mining Division Yukon Territory
for
Yukon Mining Incentives Program
by B,A,Lueck B. Sc. (honours)
Geologist
Table of Contents
Introduction 3 Summary 3 Location, Access and Physiography 4
Regional Geology and Mineralization 5
Previous Work 6 Local Geology 6 Current Program 6 Soil Geochemistry 6 Rock Geochemistry 7 Trenching 7 Discussion 8 Conclusions and Recommendations 9
Expenditures 11 Appendix (assay sheets)
Table of Figures
Fig. 1 Location Maps 4A, 4B Fig. 2 Grid Location Map and Local Geology in pocket Fig, 3 Grid Geochemistry in pocket Fig. 4 Rock Sample Locations, Trench Locations in pocket
List of Tables
INTRODUCTION
The B X Claims are located on the boundary between the Dawson and Mayo Mimng Divisions, north of Red Mountain on map sheet 115 P 15 They cover a region underlain by Paleozoic shales, carbonaceous shales, and quartzite These sedimentary rocks are intruded by stocks, dykes and volcanic breccia Hydrothermal brecciation and quartz-tourmaline stockwork veinmg are well developed Sulphide mineralization is largely oxidized with minor remnant pyrite and arsenopyrite
Exploration focused on defining gold in soil anomalies, which were later trenched if acessible Deep frozen talus hindered proper evaluation of the trenched areas
SUMMARY
The 1993 exploration program on the B X Claims succeeded in defining a strong gold in soil anomaly A total of 550 soil samples were assayed for gold to a detection limit of 5 ppb Elevated gold values occurred over large areas of the gnd, and the anomalous zones extend off the edges of the grid, to the northwest and southeast Rock sampling has succeeded in identifying three types of mineralization which assay over 1 g\T Au
Rock sampling and analyses have determined that the intensely veined and brecciated quartzite with preserved sulphides does not contain the greatest gold values Imtially umnteresting, sulphide poor, altered shale and slightly altered intrusive rock, has been shown to host economically significant amounts of gold
Fractured and altered shale, with minor oxidized quartz and tourmaline veinlets, assayed 2 13 g / T Au and 106 g / T Ag This sample is average matenal fi-om one of the trenched areas, and this type of fracturing and mineralization is considered by the writer to be common and widespread surrounding the contact area of the shale with a micaceous granodioritic stock A grab sample of quartz nch graphitic shale with minor pjoite selvedges on the quartz lenses assayed 567 opt Au
Adjacent to the gold beanng shale, a quartz biotite porphyry is slightly altered and cut by small veinlets of oxidized quartz and tourmaline with relict pynte and arsenopyrite
This zone assayed 1 5 g\T Au and 23 6 g/T Ag This type of altered intrusive is abundant, and like the gold bearing shale unit, poorly sampled due to it's inconspicuous nature
A more localized area of brecciation and veining in another exposure of quartz-biotite porphyry assayed 1 29 g/T Au and 18 g/T Ag while another sample from nearby assayed 365 g /T Au and >200 g/T Ag The first sample is more representative of average matenal at this outcrop,while the latter is the more local and intensely altered matenal The extent of this mineralization is unknown due to heavy talus
Breccia zones are often well developed within the quartzites and intense
stockwork quartz veinmg with erratic arsenopyrite is common and widespread Gold values are poor and have consistently assayed below 1 g/T from this unit, even in
spectacularly mineralized breccias Future work should focus on carefully delineating the intrusive bodies beneath the soil anomaly, and any zones of shale, as these two units host gold values m excess of 1 g/T Grids should be extended to delineate the extent of the gold in soil anomaly, and magnetic and resistivity geophysical surveys carried out over the extended grid Coincident geochemical and geophysical anomalies which coincide with subsurface shale or intrusive rock would warrant dnlling
The sample of quartz veining in shale which assayed 567 OPT Au and >50 g/T Ag indicates that higher grade mineralization exists on the property Exploration targets include high grade shear zones containmg quartz veins in shale, and low grade disseminated and stockwork mineralization in altered shale and intrusive rock
A check silt sample of the pup draining the known mineralized area re-assayed 1.3 g/T, which IS consistent with previous results Gold in soil anomalies attain values greater than 6 7 g/T Au This high concentration of gold in silt and soil also suggests the presence of high grade gold mineralization beneath the surface
LOCATION . ACCESS and PHYSIOGRAPHY
The property is located at the headwaters of Hobo Creek, north of Red Mountain on map sheet 115 P 15 The center of the known mineralization is located at
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approximately 136 43'W and 63 59TSF The claim block can be accessed by very rough 4x4 trail which heads over the Clear Creek pass, down Josephine Creek and up Hobo Creek A useable airstnp is located 4 miles from the property Access is currently being improved by local placer mining activity
The claim block covers a sparsely timbered upland region of the Yukon Plateau The region is unglaciated, but recently uplifted, as evidenced by the numerous, extensive bench gravel deposits in the area Some deeply weathered gravels on Hobo Creek are completely oxidized and cemented into a concrete-like deposit
Mountain slopes are steep but do not outcrop well, except on ridges Blocky talus of unknown depth covers 90% of the area
REGIONAL GEOLOGY and MINERALIZATION
The claim block is located within the heart of the Selwyn Basin The Selwyn Basin consists of a Paleozoic assemblage of shales, cherts and quartzite which formed off the continental margin of North Amenca
This basin hosts the Fort Knox deposit, an intrusive hosted gold deposit of large tonnage and low grade This deposit occurs in Alaska within a region of the Selwyn Basin that has been offset to the northwest by the Tintma Trench
Intrusive bodies occur throughout the Selwyn Basin in the Yukon, and stocks are often associated with gold mineralization The Brewery Creek deposit, 25 miles to the northwest, is largely intrusive hosted and hosts in excess of 17 million tons of 056 opt Au Another sigmficant intrusive hosted deposit occurs at Dublm Gulch, some 25 miles to the northeast, but drill results are unavailable As well, a strong gold m soil anomaly,
accompamed by extensive surface gold mineralization, occurs at Clear Creek 10 miles southwest of the property
PREVIOUS WORK
Mineralization m this area was unknown prior to discovery of gold mineralization on the BX claims in 1992 by B Lueck and B Wondga
Interest in this area was sparked by a regional gold and arsenic in silt anomaly on Hobo Creek, shown on the goverment geochemicl surveys Detailed sampling of silts in the area localized the anomaly to the region of the original BX 1-8 claims
Prospecting and geologic mapping was done in 1992, but no rock samples were collected which assayed over 1 g/T Au A strong gold in silt anomaly, however, indicated that further work was required
LOCAL GEOLOGY
The claim block is underlam by Paleozoic sediments of the Selwyn Basin,
consisting of graphitic shale, carbonaceous shale, chert and quartzite Sometime during the Mesozoic, these sediments were intruded by porphyritic subvolcanic stocks and dykes of granodionte and granite This intrusive zone was later cut by more recent subvolcanic dykes and volcamc breccias Intense alteration, brecciation and veining are widespread Vein and breccia infilling are dominated by quartz and tourmaline Sulphide mineralization consists of pynte, arsenopyrite and minor galena and stibnite Veining and brecciation is pervasive thoughout the various rock types, although shale and granodiorite are the only rock types which have been shown to host economic concentrations of Au
THE 1993 WORK PROGRAM Geochemistry
The initial stage of the 1993 work program consisted of grid establishment, soil sampling, and fiirther prospecting of the original BX claims Additional staking was also undertaken in order to establish a better ground position
A north-northeast trending baseline was established and lines were run every 100 m along the length of the 1700 m baseline Individual lines were 800 m or longer in length and samples were collected at 25 m spacings along each hne
The soil samples were dned, screened and pulvenzed, and fire assayed for gold to a detection unit of 5 ppb A compilation of the gold in soil anomaly is shown in figure 3 A widespread gold in soil anomaly is indicated by the sampling, even though geochemical response may be significantly hampered by extensive frozen talus Several zones show gold in soil values in excess of 1 g/T Au, with one sample assaying off the scale ( >6 7 g/T), even on repeat analyses
The grid gold m soil geochemical response indicates a north-west trending zone of widespread gold mineralization A strong response is localized to the weat on the gnd and concides with an intrusive and shale contact region Steep slopes and extensive talus made trenching of this area impossible
Rock Geochemistry
Rock samples taken from zones of trenching, and gold in soil anomalies, were analyzed for Au and 32 elements, in order to see which other elements were associated with the gold Gold and silver show good correlation, although the highest silver values do not necessanly contain the highest gold values
Other elements statistically associated with gold on this property are arsenic, bismuth, cadmium, copper, molybdenum, lead and antimony This geochemical suite is typical of intrusive hosted deposits Future geochemical surveys should use multi-element analyses to help define mineralized zones, as the geochemical dispersion pattems of gold are often erratic, due to the fact that gold occurs as discrete particles in the soil Multi-element anomalies are more useful for defimng sub-surface nuneralization because the associated base metal anomalies are often better defined than the gold anomalies Trenching Proeram
Cat trenching was undertaken on the property m August of 1993 A D- 6 Cat was mobilized to the property from Whitehorse via truck to Clear Creek, and then walked in over existing cat trails Steep topography hindered trenching of many of the stronger gold
in soil anomalies Accessible anomalies were usually covered with deep talus, frozen a few feet below the surface
Trenched areas were sampled for both average matenal and select sampled for intensely altered, veined, or sulphide mineralized rock Select grab samples invariably show discouraging gold values, but average, slightly altered and mineralized shale and intrusive rock contains gold values greater than 1 g/T and up to 2 13 g/T Au A grab sample of conformable quartz lenses and stringers in shale, with minor euhedral pyrite on the selvedges, assayed 567 0 P T Au
Overall, the trenching failed to expose sigmficant amounts of bedrock and
therefore proper sampling of bedrock regions was not accomplished Given the extensive land distubance required to expose bedrock in this area, fijrther trenching is not
recommended Multi-element geochemical surveys, geophysical surveys, and detailed bedrock and talus mapping will readily delineate zones of mineralization Drilling of these targets is recommended to evaluate the grade, occurrence, and extent of the identified gold beanng rocks on the BX claims
DISCUSSION
The BX claims host poorly explored gold mineralization, which
has been partially delineated by soil geochemistry, rock sampling and prospecting The target is a large, low grade, disseminated or stockwork gold deposit hosted by both the intrusive rocks, and the altered and veined shales adjacent to the intrusives
Hydrothermal brecciation and silica-tourmaline flooding are pervasive and intense over large areas of the property There is so much veimng and brecciation that it is difficult to know what to sample Exploration efforts were frustrated by the fact that the 'best looking' rocks do not contain economic gold values
The nature of the gold occurrence has been detemined through this season's work, and this will greatly aid the fiiture exploration of this area Gold occurs associated with slightly altered, quartz-tourmaline veined intrusive rock and shale Higher grade gold
occurrences are related to quartz-pyrite segregations in shale, and the only sample assayed 567 0 P T Au The property hosts excellent potential for the discovery of significant reserves of gold
CONCLUSIONS and RECOMMENDATIONS
The 1993 exploration program on the BX claims has delinated a strong gold in soil anomaly, accompamed by a strong creek silt gold anomaly Preliminary sampling of bedrock material underlying the geochemical anomaly shows that.gold is present in economically significant amounts in shale and granodionte on this property
Bulk tonnage potentail for rock grading > 1 g/T Au has been shown to exist in slightly altered, extensive igneous and sedimentary umts High grade gold mineralization has also been shown to exist in quartz veins and stringers in shale
It IS recommended that future programs use the techniques of multi-element soil sampling programs, coupled with ground geophysical surveys, to deliniate potential ore zones Carefiil mapping of the distribution of intrusive rock and shale, in outcrop and in talus, will help define the best sub-surface target area It is recommended that several drill holes, moderately spaced (75-100 m) and drilled at a 45 degree angle, are requu^ed to evaluate the occurrence Contact zones between intrusive and shale hold the best potential for ore Holes should be dolled to at least 500' to get a good section through the geology, and to penetrate into unoxidized bedrock Vein and breccia zones are several hundred feet wide on the surface and long holes are required to thoroughly sample the mineralized zones
Rock Sample Descriptions
3-Zone- Stockwork quartz-tourmahne stnngers m fractured quartzite Arsenopynte can be seen on some fresh surfaces
HT-1- Altered sedimentary and volcamc rock adjacent to the intrusive Secondary biobte growth occurs on fractures Typical "skam" texture and mineralogy
HT-2- Best grab sample of massive arsenopynte m brecciated quartzite
HT-3- Fractured intrusive rock from trenched zone Minor quartz-tourmaline stnngers in poorly altered biotite beanng porphyry
HT-4- Fractured and altered shale from trenched zone adjacent to the mtmsive rock Minor quartz crystals on oxidized fractures
HT-QTZ - Quartz vemed quartzite from highly anomalous zone underlain by shale and quartzite Stnngers lack sulphides of any kind
N-1- A sample of sulphide bearing dyke matenal from near the north end of the gnd The dyke crosscuts carbonaceous shale in an area of high gold m soil response
CSV- Highly o-xidized and limonitic breccia with quartz-tourmahne veinlets, in quartzite adjacent to the intmsive body
S-4- Minor pynte in altered quartzite from a trenched area of high gold in soil response Bedrock is largely shale
S-5- Slightly altered biotite-quartz porphyry with quartz-tourmahne and mmor scoroditein fiacture fillings
S-6- Spectacularly brecciated and mineralized quartzite from adjacent to the intmsive porphyry Arsenopynte is abundant
S-7- Quartz-arsenopynte veins in quartzite
7+OOS 3+OOE - Quartz-tourmahne stockwork and quartz stockwork veimng in brecciated quartzite
Yukon Mining Incentives Program
Statement of Expenditures:, BXClaims Target Evaluation Program For; Brian Lueck
Description of Program: May 25 to Aug 30 , 1993
Phase 1; Prospecting, Grid Establishment, Geochemical Soil Sampling (550 samples) Phase 2: Cat Trenching, Rock Sampling, Report Preparation
Itemized Expenditures:
Mobilization B Lueck (Van -Whse) 3000 km @ 36 5/km 1095 00
1 Hotel 86.36 2 Hipchains and compass 258.89
3 Maps 17 54 4 Flagging Hipchain thread 125 12 Mobilization B. Lueck, B. Wodga, D Trudeau, D McLeod
( Whse -Daw -Clear Creek) 600 km @ 36 5/ km 219 00 5 Hotel 78 11 6 Helicopter 2685 1 0 ^ 7 HeUcopter 2899.97 v/
8 Wages D Trudeau (20 days @$i50/day) 3000 00v/ 9 Wages D McLeod (20 days @ $150/day) 3000 00 J 10 Wages B Wondga (25 days @ $200/day) 5000 00 ^ 11 Cat Rental 5000 00
12 Truck Rental (with camper) 4337 40 13 Damage to Fuel Tank and Skid 550 00
14 Trucking Cat (Whse -C Creek), Fuel 3393 77 V^ 15 Trucking of Cat (C Creek-Whse ) 1575 00 16 Cat Operator Wages 1650 00 17 Flagging, thread and markers 161 18 Camp Costs D Trudeau, D McLeod (2 x 20days x 52 85/day) 2114 00 \ /
B Lueck, B Wondga (2 x 25days x 52 85/day) 2642 50%/ Cat Operator (15days x 52 85/day) 792 75 \ / 18 Assav costs (to date') 6000 00
Binart) D i a g r a n 3 r d U a l S t a t s Nana = AUJ»PB a r i t h n e t i c N » 5^41 Hax » 6.67E4^3 Mean ~ 6 8 . 0 H i n » 2 . 0 0 StDw = 3 1 4 . 0 C o n t o u r s
Grid spacing:
X = 26.4
Y = 55.6
Influence - 4
Exponent - 2.00
Contour interval
= 0.750 StDv
O 300.0
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Chemex Labs Ltd.
Analytical Chemists * Geochemists 'Registered Assayers 212 Brooksbank Ave., North Vancouver
British Columbia, Canada V7J 201 PHONE 604-984-0221
To. LUECK. BRIAN 6876 BROOKS ST VANCOUVER, BG V6T3J7 Project. Comments BX CLAIMS
Page Number 1-A Total Pages . 1
Certificate Date 08-SEP-93 Invoice No 19319953 P O. Number Account KIS SAMPLE U P i T - l aT-2 BT-3 aT-4 IT-QTZ U-l 9SV 3-4 S-5 S-6 S-7 7+OOS 3+OOE . PBEP CODE 205 205 205 205 305 205 205 205 205 205 205 205 205 205 274 274 274 274 274 274 274 274 274 274 274 274 274 274
CERTIFICATE OF ANALYSIS A9319953
Au p p b Ag Al AS Ba Be Bi Ca Cd Co Cr Cu Fe Oa Hg K La Hg Hn FA+AA ppm % ppm ppm ppm ppm % ppm ppm ppm ppm % ppm ppm % ppm % ppm < 5 0,8 0 , 3 3 748 60 < 0 , 5 16 0 , 3 6 < 0 , 5 5 101 260 1,42 < 10 < 1 0 . 2 1 < 10 0.18 60 < 5 0,6 0 , 2 1 4040 SO < 0 , 5 < 2 0 , 0 1 < 0 , 5 1 287 17 0.90 < 10 < 1 0,10 20 0.01 30 50 < 0,2 1,20 90 190 < 0 , 5 8 1,23 < 0 , 5 32 88 7 1 2,62 10 < 1 0,36 40 0,95 160 490 2 . 6 0 , 1 5 >10000 180 < 0 . 5 28 0 , 0 3 0 , 5 39 150 74 2 , 7 1 < 10 < 1 0,02 < 10 0.02 40 1500 23.6 0 . 6 8 >10000 2020 0 . 5 138 0 . 0 1 1,0 1 103 69 2 , 2 8 10 < 1 0.28 60 0,04 30 2130 106,0 1 , 4 8 >10000 150 < 0 , 5 64 0 , 1 1 7 . 5 9 72 765 >15.00 50 2 0,36 360 0.02 110 20 1,6 0 . 3 0 800 70 < O.S 4 0 , 0 1 0 , 5 1 226 119 2 . 1 3 < 10 < 1 0 , 1 1 20 0.02 20 45 0.2 2 . 8 3 196 60 0 . 5 2 1.95 < 0 . 5 30 77 69 4 , 4 1 10 < 1 0,24 10 1,13 ISS 365 >300 0 . 2 2 >10000 210 < 0 . 5 334 0 . 1 7 9 4 . 0 < 1 98 359 7.46 10 3 0.45 30 0.01 10 < 5 1,4 0 . 2 8 88 30 < 0 . 5 < 2 0.04 < O.S 7 326 10 1.33 < 10 < 1 0.02 10 0.07 275 1290 18.0 0 . 2 8 >10000 210 < 0 . 5 42 0 . 0 1 2 . 5 4 126 536 2,94 < 10 < 1 0,12 20 0 , 0 1 10 125 8,0 0 . 5 1 5410 110 < 0 . 5 12 0 . 0 1 1.0' < 1 136 141 2,17 < 10 < 1 0,14 40 0 , 0 1 10 240 11.4 0 , 1 0 >10000 90 < 0 , 5 46 0 , 0 1 1.0 43 209 61 4 , 4 5 < 10 < 1 0,03 20 < 0 , 0 1 I S 15 0,6 0 . 2 1 260 20 < 0 . 5 2 0 . 0 1 < 0 . 5 < 1 308 31 1.12 < 10 < 1 0,07 10 0 . 0 1 30 « a-— • , ^ « . CERTIFICATION.
I ^ C M V ^ ^ x V .
Chemex Labs Ltd.
Analytical Chemists' Geochemlsts * Registered Assayers 212 Brooksbank Ave, North Vancouver
British Columbia, Canada V7J 2C1 PHONE- 604-984-0221 To LUECK, BRIAN 6876 BROOKS ST VANCOUVER, BC V6T3J7 Project • Comments: BXCLAIMS Page Number 1-B Total Pages 1 Certificate Date 08-SEP-93 Invoice No. 19319953 P O Number
Account KIS
CERTIFICATE OF ANALYSIS A9319953
SAMPLE PREP CODE Mo p p a Na % Ni ppm P ppm Pb ppm Sb ppm Sc p p o S r p p n Ti % T l p p n 0 ppm V ppm V p p m Zn p p n IVSP BX 3 -a r - i aT-2 aT-3 ZONE 205 205 205 205 205 274 274 274 274 274 0,04 < 0,01 0,17 0,01 < 0.01 9 820 3 290 135 1510 14 380 6 48 2 162 740 3510 < 2 18 4 13 204 32 0,06 3 < 0,01 98 0,19 16 < 0,01 20 < 0,01 < 10 < 10 < 10 < 10 < 10 < 10 < 10 < 10 < 10 < 10 15 2 85 4 7 < 10 < 10 < 10 < 10 < 10 16 6 40 12 48 aT-4 aT-QTZ a - 1 3SV 3-4 205 205 205 20S 205 274 274 274 274 274 7 0,02 3 8100 >10000 2310 IS 433 < 0.01 < 10 < 10 53 < 10 66 1 < 0.01 S 140 70 30 < 1 3 < 0,01 < 10 < 10 2 < 10 24 3 0,40 56 2060 32 3 3 124 0,28 < 10 < 10 104 10 28 1 0,02 4 380 >10000 >10000 4 55 < 0,01 < 10 < 10 3 20 6 1 < 0,01 10 150 180 156 < 1 2 < 0,01 < 10 < 10 4 < 10 24 S-5 3-6 3-7 7+OOS 3+OOE 205 205 205 205 274 274 274 274 2 < 0,01 4 280 160S 1270 2 15 < 0,01 < 10 < 10 1 < 10 2 9 < 0,01 1 300 2430 104 < 1 37 < 0.01 < 10 < 10 2 < 10 6 1 < 0.01 4 130 198 560 < 1 5 < 0.01 < 10 < 10 1 < 10 12 1 < 0.01 3 120 36 10 < 1 3 < 0.01 < 10 < 10 2 < 10 8
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WO 13980 Sample Au ppb Ag ppm L400N Cv L400N L400N L400N L400N L400N L400N L400N L400N L400N L400N L4D0N fL400N -•%L400N L400N -L400N L400N yL400N 9L400N « 4L400N t L 4 0 0 N L400N L400S L400S L400S L400S L400S L400S L400S L400S L400S L400S L400S L400S L400S L400S L400S L4D0S L400S L400S L400S L400S 2+50E 2+75E 3+OOE 0+25W 0+50W 1+OOW • 1+25W 1+50W 1+75W 2+OOW 2+25W 2+50W 2+75W 3+OOW 3+25W 3+50W 3+75W 4+OOW 4+25W 4+50W 4+75W 5+OOW 0+00 0+2SE 0+50E 0+75E 1+OOE 1+25E 1+50E 1+76E 2+OOE 2+25E 2+50E 2+75E 3+OOE 0+25W 0+60W 0+75W 1+OOW 1+25W 1+50W 1+75W 22 67 41 15 26 10 24 38 30 29 29 42 92 50 21 49 46 75 175 302 222 15 13 19 29 42 36 15 10 20 31 29 31 21 27 31 24 36 24 14 15 165 Certified by
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WO 13990 Sample Au ppb Ag ppm L600S » L600S VL600S ^L600S L600S ^LSOOS 9L600S L600S (iL600S (^Leoos $L600S 9L600S L600S L600S L600S L600S L600S Leoos L600S L600S L600S •-I L600S ^ L 6 0 0 S «L600S ©L700S L700S L700S L700S ©L700S L700S L700S L700S L700S . L700S ^L700S SL700S '9L700S L700S L700S L700S 2kL700S ^L700S 2+OOE 2+25E 2+50E 2+75E 3+OOE 0+25W. 0+50W 0+75W 1+OOW 1+25W 1+50W 1+75W 2+OOW 2+25W 2+50W 2+75W 3+OOW 3+25W 3+50W 3+75W 4+OOW 4+25W 4+50W S+OOW 0+00 0+2SE 0+50E 0+7SE 1+OOE 1+2SE 1+SOE 1+75E 2+OOE 2+2SE 2+50E 2+75E 3+OOE 0+25W 0+50W 0+75W 1+OOW 1+2SW ^ 8 91 ^ 3 ^ 2 579 .40
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Assay Certiflcate Pagel1
WO 13990 Sample Au ppb Ag ppm L700S (aL700S L700S & L700S L700S L700S dL700S «L700S ©L700S 0L7OOS OL700S #L700S L700S fL700S L700S ; L700S nL700S >L700S tL700S ©L700S c L700S L800S '. L800S L800S L800S L800S 'L800S L800S L800S L800S L800S L800S L800S L800S L800S L800S L800S L800S 'L800S L800S L800S '800S 1+50W 1+75W 2+OOW 2+25W 2+50W 2+75W 3+OOW 3+25W 3+60W 3+75W 4+OOW 4+25W 4+50W 4+75W 5+OOW 5+25W 5+50W 5+75W 6+OOW 6+2SW 6+50W 0+00 0+25E 0+50E 0+75E 1+OOE 1+25E 1+50E 1+75E 2+OOE 2+25E 2+SOE 2+7SE 3+OOE 0+2SW O+SOW 0+7SW 1+OOW 1+25W 1+50W 1+75W 2+OOW Certified by
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