PROSPECTING REPORT
- SUDCAN PROJECT -
- EDEN TOWNSHIP -
Prepared by:
Robert G. Komarechka P.Geol. of BEDROCK CONSULTING
#1 - 545 Granite St. Sudbury, Ontario P3C 2P4
41I06SE2003 2.25060 EDEN 010
PROSPECTING REPORT SUDCAN PROJECT - EDEN TWP.
CONTENTS
Introduction ...................................................................................................................... 2Location A Access ............................................................................................................ 2Mining Claims Examined ............................................................................................... 2Previous Exploration Work ............................................................................................. 3Work Undertaken ............................................................................................................3Property Geology .............................................................................................................4Prospecting Activities ...................................................................................................... 4
Traverse l .............................................................................................................4Traverse 2 .............................................................................................................5Traverses .............................................................................................................5Traverse 4 ............................................................................................................. 6
Conclusion ........................................................................................................................ 7Recomendations ............................................................................................................... 7References ........................................................................................................................ 8Certificate......................................................................................................................... 9Appendices ...................................................................................................................... 10
Appendix l - Sample Descriptions ................................................................... 11
Maps - General Index Map l....................................................................................... 2-i- Plan of Physical Work Map 2 ................................................... in back pocket- Current Aylmer Tp. Claims Map 3 ......................................... in back pocket
Sudcan Eden Twp Report Bedrock Consulting Nov. 6,2002 pg l
PROSPECTING REPORT SUDCAN PROJECT - EDEN TWP.
INTRODUCTION
On July 3, 2002, Bedrock Consulting was contacted by J. M. O'Shaughnessy of Sudcan Ltd. to prepare a proposal for a prospecting report on a property in EdenTwp.
The prospecting program consisted of 4 traverses over 4 field days including the collection of samples, map and report preparation. The location of this work is shown on Map # 2.
The purpose of the program was to investigate from field observations, the possibility of Long Lake type gold mineralization and possible targets for PGM exploration.
LOCATION A ACCESS
The study area is located in Eden township approximately 1.5 kilometer southeast of Long Lake, on claims S1271267 and S1211266 centred about UTM 17 NAD 83 co ordinates 488000mE and 5127000mN. The location is shown on the general index map. l as well as on the keymap on map 2. The site is located within the Sudbury Mining Recorders District.
Access to the site is obtained by traveling south of Sudbury form Hwy 69 south on Long Lake Rd. then turning left on to Tilton Lake Rd to outside the city limits. Several kilometers beyond the city limits the road forks. Take the right fork on tto Wavy Trail and continue about l .5 kilometers down a hill and across Wavy Creek for about 3km. At this point at the crest of a knoll where the hydro line crosses the road, a small quad trail is found on the left heading in a southwestern direction. Continue travelling by quad on this road for about two km. at which point the trail forks. Take the left fork and continue for about l .2 km. to the site of the old Long Lake Open Pit. Just before the end of the road, a trail branches to the left. Take this trail for several hundred meters to a dried up swamp downstream from Luke Lake. Access can be obtained to the site by foot from this point.
MINING CLAIMS EXAMINED
The work described herein was performed over the following 2 claim.
Claim Number Number of Units Registered Claimholders
51211266 2x2 John M. O'Shaughnessy51211267 2x3 John M. O'Shaughnessy
58 Forest Park Crescent Thornhill, Ontario L3T 2M7
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 pg 2
w*****"" l-r
i*w* ;
UW*^:
/luni, v?;-—o L? 1
\B!ZOt
IL*)*-,'
?',J i aie'nt
tv*B"U
M^T^STGlUtS"
i- (
S**.
Uwe..c* W
*w*
f*"90 v^i
w**i*r*uUT. c*n*lrw-v
ie\r"W*!*5!S- l**SM
vt .U-" 5PBUS 'l,•^V
'r^ K-*" '^arw
\——'MB-
y^"5
&UI*
"V
,feit^5C
"*-"MMO.!?^
V"**1 H*-"
78*AT*
Map#1General Index Map
\ tW \\
H^-V.̂IwW V
QUEBEC
VBlWWVTt
^-V^l l***1\—v!.-^Ud^\j
vw*" Worn"
V(!nr'*a* H '~
T^OB* *
ef***lii-
La*(e W"' ^rSs-\
7 X\ \ fcjjxW ?^R
Wl"'( * ^^\^3*^E^** Y^J-ocation ofSjy4y Area fc '*-
^r**"*
nx ! If .3~Z*
" \^ -
ipv-^TfafU***
^^iu—^
\ —,-.:~\paudw't" bU
,^*r V—-i±" **BX!f
\ t^:5-'"U**tT
\ -V*"?1 ''iW*^1
^^r^X^
;\r^
?'•""te^ -VqesrLV
^ \ v\"--^aX xJp-V- V/^A^^-.. **r^\^\ fafa*^A^ ^~~^\. *™— \ ^ \ s ^2^\? \- -A u-w^rix ^^ ^Of'i \ -*1
Wn**?"*^D,
aa*idocM BUBV;
,K \Wbc-
\^-
.ct^*^^SjSlNn-*^7^Siri
GEORGIAN
Scale 1: 2^0,000esBW ^
M*n Pg 2i
—p**'
i^e
-;Sri-'fT ̂ '"^^~ -rr^f
v^\^ A V— c- \ > -—y -stpx \ — ^\r^l- Vt^ x^-\ c*^x x \ r- V" V x^"" -
^S^ V—'\—' x\ —. v*"" \-- \\x X1""^ x ~fr^Vfe^ V/ \-^ x \ x\— V^ V^- ^'-ft^C- 3^\^xOi V^Sl-^VTRR^ D̂ \XT 'J 5-^ X l "^ x ^ x "^-- 3?^2^: X^^X^^A--^ VT V x^r"-^^/ \ **r-^^5^^^^^^^v\/^*^v^at!^vxi^.-'rsl-s x\; -fe-*. H /x \y X-X *r*"
^
Lon*('Ck*l- ^
^ x̂ - r01-^-^-^^x^s--/ ^t\*i***\
tut-"
v- \iX V*"*r^AL-^ \- ^^-"0-**?^x '" *n*
L^.? O.V
r\\DCB*
AR*^00^)vs-ti*- MM
PREVIOUS EXPLORATION WORK
Previous Work Summary
YEAR ASSESSMENT WORK BY FILE #
WORK TYPE WORK DESCRIPTION
1972 EDEN-001 3-B1 1974 EDEN-001 3-A1 1981 EDEN-0012
1981 EDEN-00181982 EDEN-0010-A1 1982 EDEN-0011-A1 1982EDEB-0011-B1 1982 EDEN-0011-CI 1982 EDEN-0014 1982 EDEN-0015
1982 EDEN-0016 1982 EDEN-00171982 EDEN-0019-A1
1983 EDEN-0020
1986EDEN-SP001
COPPER-MAN MINES LIMITEDSTAPLE MINING CO LTDD F WHITE, DUPONT OF CANEXPLLTD, JJ HANNILA, LF FRANZEN,LUKE LAKE MINES LTD.DUPONT OF CAN EXPL LTD.DUPONT OF CAN EXPL LTD.DUPONT OF CAN EXPL LTD.DUPONT OF CAN EXPL LTD.DUPONT OF CAN EXPL LTD.DUPONT OF CAN EXPL LTD.DUPONT CANADA.LUKE LAKELTDDUPONT OF CAN EXPL LTD.DUPONT OF CAN EXPL LTD.DUPONT CANADA.LUKE LAKELTDLUKE LAKE MINES LTD.
K LAPIERRE
1987 EDEN-SP002 MILL CITY GOLD INC
OTHERVLFGEOL,MAG,VLF
MAG,VLFPDRILLGEOLGEOLGEOL
PROSPECTUS AMENDMENT12.0LMI19.9 LMI,HTF,MAPPING
24.27 LMI 2 DDH/700 1 BDRX GRID BDRX GRID BDRX GRID
GEOL,GR,IP,MAG 23.4 LMI,BDRX,MAPPING GCHEM, PDRILL 2 DDH7700',DD,CORE AU
GEOL MAG, VLF GEOL
GRD MAPPING 65.5 LMI GRD MAPPING
1988EDEN-SP003 1988 EDEN-SP004
MILL CITY GOLD INC MILL CITY GOLD INC
GCHEM.OTHER DD CORE 8t GRABS.EXPNDGCHEM
MCOMP GEOL/PREVIOUS WORKSUMMARIES
AMAG.AVLF, 1 64 LKM,SUMMARY GLCOMPMAG.VLF 1 29.0 LKM GCHEM 1 5RX GRAB AU
WORK UNDERTAKEN IN THIS REPORT
This report discusses the following work undertaken on the property:
Date Type of Work Performed by
Oct. 17,2002 Oct. 18,2002 Oct. 23, 2002 Oct. 24, 2002 Nov. 13-24/02
Prospecting Prospecting Prospecting Prospecting Report preparation
Robert G. Robert G. Robert G. Robert G. Robert G.
Komarechka Komarechka Komarechka Komarechka Komarechka
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 Pg 3
GENERAL PROPERTY GEOLOGY
The area is underlain by Huronian sediments of the Quirke Lake group consisting of the Serpent and Espanola Fm as well as the Mississagi Fm of the Hough Lake Group. These sediments are in turn intruded by Nipissing Diabase and later felsic intrusions of the Eden Lake granites. A series of northeast to southwest trending faults are shown on Card's map as passing through the area.
The long Lake Gold mine, a significant past gold producer, occurs immediately to the northeast of the property. The mined deposit is located within a Mississagi quartzite pod surrounded by Nipissing diabase adjacent to the Wallingford Fault and nearby granitic rocks of the Eden Lake intrusives.
PROSPECTING ACTIVITIES
Four traverses were undertaken on the property and samples collected in areas of interest. Map 2 shows the location of these traverses and sample locations while Table l describes the samples collected. The location of these traverses were based on areas of previous anomalous assays, areas of low magnetic linears, and IP anomalies as determined from previous work on this property, that being primarily from the work of Dupont of Canada Exploration Ltd. Location was determined by the use of the current OBM map and the use of GPS equipment. UTM NAD 27 co-ordinates were used in locating samples and on Map 2.
Traverse #1
This traverse, conducted on October 17, 2002, located access to the site and the location of the claim boundary between claim 1211267 and 1211266. It also investigated a cross section of the geology on the property and focused on a N-S low magnetic linear as illustrated on the aeromagnetic map and included examination of the area of chargeability anomalies D-4 (e), D-8(a), (b).
Generaly the geology on site matched that of ODM map 2299, with the following variations. In the area of the second swamp area about 250m south of Luke Lake along the claim boundary of claims 1211267 and 1211266 there was an area of white quartzite which appeared to underlay this now dried out swamp area. Breccia appeared prevalent along the contact of this quartzite. Sample BK2- 18-09-02 was collected from this area. This quartzite appeared to trend northeastward along the incoming drainage and extending southwestward to southeastward along the west side of a low depression.
Examination of chargeability anomaly D-4 (e) of the IP survey undertaken by Dunlop of Canada Exploration Ltd. minerals revealed an area of laminated silty argillite - possibly the Espanola Fm. These rocks although indicating limited calcareous content were very distinctive in having fine quartz rich laminations which stood up in relief due to differential weathering. The higher magnetic intensity in this area may be related to the high magnetite content along certain bands see sample BK1-18-09-02 Pyrite was also observed within this sample and may be the cause of the chargeability anomaly in the area.
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 pg 4
Chargeability anomaly D-8(a) was overlain by overburden with nearby Nipissing Diabase being observed. Chargeability anomaly D-8(b) was also covered in overburden.
Traverse #2
This traverse was basically a continuation of traverse #1 from the previous day and investigated several areas of quartz veining as shown on ODM map 2299. The first of these areas is shown just to the southeast of the swamp area previously discussed in traverse #1. This area occurs as a high flat topped ridge of quartzite laced with a quartz vein stockwork. No pyrite or any oxidization was noted in the area and no samples were taken.
A westward traverse along an old cut line then undertaken to intersect the N-S claimline between claims 1211266 and 1211267. The traverse continued southward to post #2 of claim 1211267. The outcrops encountered in the area appeared to be primarily of Killarney (Eden Lake) granite.
Going westward across a low lying area, an outcrop area of quartzite was observed. Near the top of the N-S ridge an area of N-S trending quartz veins were noted. These veins were several meters wide, and consisted of white bull quartz anastomosing in the quartzite host rocks. Sample BK3-18-09-02 was collected from this site.
The traverse continued northward along ridge and encountered a second area of bull quartz veining which was sampled as BK4-18-09-02. This vein had a width of at least several meters and was covered in part with overburden. The host rocks in the area consisted of feldspathic quartzites.
The traverse continued northward encountering the N-S claimline, exiting along this northern direction to Luke Lake.
Traverse #3
This traverse undertaken in October 23, 2002 was carried out along the south shoreline of Luke Lake and encountered a sill of Nipissing diabase. Midway along Luke Lake, just south of a wide peninsula, a creek was encountered that flowed into Luke Lake. Along the north shore of this creek a brecciated area of laminated argillaceous sediments was noted with minor pyrite. Sample BKl-23-l0-02 was collected from this site. Additional breccia as well as mylonitic textures were noted further upstream within the creek bed.
A band of quartzite was also noted on the west side of the creek just south of Luke Lake. Several minor quartz veins within this quartzite and terminating a short distance westward from a dried up swamp area, was examined and sampled as sample BK2-23-10-02. The southern contact of the quartzite with a gabbroic body (possibly Nipissing diabase) shows several areas of rusty pyrite bearing brecciated quartzite. These areas were sampled as BK3, BK4, and BK5-23-10-02. One of these samples, BK5-23-
Sudcan Eden Twp Report Bedrock Consulting Nov. 6,2002 pg 5
10-02 showed minor pink erythrite (cobalt bloom) staining on a fracture plane. Sample BK6-23-10-02 was also collected from the gabbro contact in this area.
Also noted within the gabbro sill just south of this contact was a band of anorthosite rock containing a poikiolitic texture having discrete spherical amphibole clots within a lighter plagioclase matrix. On weathering the plagioclase becomes white and the rock appears very striking. If this unit matches that mapped along the north contact of the gabbro sill by David Mossman for Dupont of Canada Exploration Ltd. then there may be some interesting structural interpretations.
Continuing southward along the creek quartzite was encountered with a Killarney granite sill in contact with a possible narrow segment of quartzite along the east side of the creek. Abundant laminated siltstone was encountered along the west side of the creek and where in contact with the gabbro exhibited extensive plastic deformation and occasional brecciation. Porphyroblast (possibly scapolite) were also observed in these rocks.
Return from this traverse was the same route as the entry, deviating for a traverse conducted along the north shore of the swamp east of Luke Lake. This access route allowed for faster exit and was later used for the next traverse.
Traverse #4
This traverse was conducted on October 24, 2002 at the southwest portion of the property and investigated several anomalous IP chargeability anomalies labelled D-4 on Dunlop's chargeability map.
Access was along the south shore of Luke Lake. Although primarily gabbro, a small near vertical wedge of rafted quartzite was observed about 400m west of sample BK1-28-10-02. In the area of chargeability anomaly D-4(b) a slightly rusty pyrite bearing gabbro was encountered and sampled as sample BK l -24-10-02.
Continuing upstream along the west side of a swampy creek encountered quartzites, then later laminated siltstone and again back into quartzite. Heading westward from this second contact gabbro is encountered often with fine disseminated pyrite. It is felt that this may be the cause of chargeability anomaly D-4(a). Sample BK3-24-10-02 was collected from a rusty gabbro with pegmatoidal pods.
Continuing westward from this point leads to an open wet area. Just along the east edge of this swamp is a thin N-S quartzite band. Going southward along this band there is a splay of the quartzite to the east. The quartzite at this location has a l meter wide band exhibiting bright yellow jarosite staining containing both pyrite and arsenopyrite in a recrystalized siliceous matrix. This 1m wide band pinches out on surface to the east but appears to continue striking west under the swamp. The zone appears to dip at 600 north under a gabbroic sill and may also contribute to the chargeability anomaly D-4(a) if it continues beneath the gabbro.
Sudcan Eden Twp Report Bedrock Consulting Nov. 6,2002 pg 6
CONCLUSION
As a result of the above brief study the following is evident:
1) Quartz veining appears to be concentrated along fracture splays arcuately emanating from the faults in the area. These splays also appear to have quartzite bodies associated along them with associated brecciation and net veined quartz veins.
2) The quartzite bodies are often found in low lying areas such as in some of the dried up beaver dams. These areas appear to correlate with areas of low magnetic intensity.
3) Areas of high chargeability from previous IP surveys seem to have correlation with increases in pyrite content.
4) At least two sample sites appeared to have arsenopyrite associated with them. In both cases they appear within quartzites proximal to a gabbro contact.
5) Some areas of gabbro, previously mapped as Nipissing Diabase appear to have textures typical of anorthosites.
6) A narrow band of poikiolitic gabbro was found south of Luke Lake which may be a continuation of a band mapped earlier by Dupont north of Luke Lake. This band was believed to be found near the upper contact of the gabbro sill. If this is so then the centre of the gabbro sill may represent an anticlinal fold.
7) Some areas of these gabbros, especially in small pegmatoidal patches, occasionally have splotches of pyrite, suggesting hydrothermal activity.
8) The metasediments proximal to the contacts of the gabbro often appear to be either fractured and brecciated with rafted slabs in the case of quartzites and plastically deformed in the case of argillaceous siltstones.
9) The sulphides and arsenopyrites encountered in the metasediments appear to be epigenetic, contained within brittle quartzites, close to the gabbro contacts. The possibility exists that this mineralization may be related to structures of rafted and fractured overlying quartzites which allow for the movement and entrapment of arsenic and sulphurous volatiles and associated elements.
10) The results of this limited work has failed to reveal any large bodies of suphides in the area.
RECOMMENDATIONS
1) Examination of the area north of Luke Lake was not undertaken in this study. Dunlop's IP chargeability anomaly, Zone A as well as B (not on this property) should be examined in light of the correlation of pyrite with these anomalies.
2) Pending assay results, further work in this area should emphasize structural mapping and detail to the presence of quartzite bodies and their associated gabbro contacts.
3) Exploration should be focused on the gabbro quartzite contacts with consideration being given to areas of anomalous jarosite alteration, silicification and the presence of sulphides and arsenopyrites.
4) In selected areas, soil geochemical analysis for Au, As and S followed by local detailed IP surveys over anomalous areas may prove up drill targets in the area.
Sudcan Eden Twp Report Bedrock Consulting Nov. 6,2002 pg 7
REFERENCES
From Assessment Reports on File in the Sudbury District OfficeYEAR ASSESSMEN
T FILE #WORK BY WORK TYPE WORK DESCRIPTION
1972 EDEN-001 3-B1 1974 EDEN-0013-A1 1981 EDEN-0012
1981 EDEN-00181982 EDEN-0010-A1 1982 EDEN-0011-A1 1982EDEB-0011-B1 1982 EDEN-0011-CI 1982 EDEN-0014 1982 EDEN-0015 1982 EDEN-0016 1982 EDEN-00171982 EDEN-0019-A11983 EDEN-0020
COPPER-MAN MINES LIMITED STAPLE MINING CO LTD D F WHITE, DUPONT OF CAN EXPL LTD, JJ HANNILA, LF FRANZEN, LUKE LAKE MINES LTD. DUPONT OF CAN EXPL LTD. DUPONT OF CAN EXPL LTD. DUPONT OF CAN EXPL LTD. DUPONT OF CAN EXPL LTD. DUPONT OF CAN EXPL LTD. DUPONT OF CAN EXPL LTD. DUPONT CANADA.LUKE LAKE LTD DUPONT OF CAN EXPL LTD. DUPONT OF CAN EXPL LTD. DUPONT CANADA.LUKE LAKE LTD LUKE LAKE MINES LTD.
OTHERVLFGEOL.MAG.VLF
PROSPECTUS AMENDMENT12.0LMI19.9 LMI.HTF.MAPPING
1986 EDEN-SPO01 K LAPIERRE
1987 EDEN-SP002 MILL CITY GOLD INC
1988EDEN-SP003 1988EDEN-SP004
MILL CITY GOLD INC MILL CITY GOLD INC
MAG.VLFPDRILLGEOLGEOLGEOLGEOL.GR.IP.MAGGCHEM, PDRILLGEOLMAG.VLFGEOLGCHEM.OTHER
MCOMP
AMAG.AVLF, GLCOMP MAG.VLF GCHEM
24.27 LMI2 DDH/700'BDRX GRIDBDRX GRIDBDRX GRID23.4 LMI,BDRX,MAPPING2 DDHX700',DD,CORE AUGRD MAPPING65.5 LMIGRD MAPPINGDD CORE & GRABS.EXPNDGCHEMGEOL/PREVIOUS WORKSUMMARIES164 LKM.SUMMARY
129.0 LKM 1 5RX GRAB AU
O'Shaunghnessy, Jack2002. Personal papers and maps.
Phemistar1939. ODM Annual Report #48. p 24-27.
Baker, M. B.,1917. Long Lake Gold Mine, Sudbury District, Ontario Bureau of Mines, Vol.XXVI. p 157-162.
Card, K. D.1975. Louise, Eden Geological Report, Ontario Geological Survey, Report #124.
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 Pg8
CERTIFICATE
I, Robert G. Komarechka, of the City of Sudbury, in the Province of Ontario hereby certify as follows:
1. That I am a consulting geologist currently residing in Sudbury.
2. That I am a graduate, BSc. Geology major, of Laurentian University of Sudbury, Ontario, a registered professional geologist in the Province of Alberta affiliated with the Canadian Council of Professional Engineers, and that I have been practicing my profession for nineteen years.
3. That I do not have an interest in the properties.
4. That this report is based on field observations and information collected over the months of August and October of 2002.
Robert G. Komarechka P. Geol.
Dated at Sudbury, Ontario, this 7th day of November, 2002.
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 Pg9
APPENDICES
Sudcan Eden Twp Report Bedrock Consulting Nov. 6,2002 pg 10
APPENDIX l
Sample Descriptions
Sudcan Eden Twp Report Bedrock Consulting Nov. 6,2002 pg 11
Sample Number Rock Name Comments Recommendations
BK1-18-09-02 Quartz Plagioclase Biotite tan brown, 45'*6 quartz, 40(J6 plagioclase, with 1596 biotite, interstitial very fine Assay for Au Biotite Paragneiss octahedra of magnetite occuring more abundantly along fine laminations.
This rock frequently shows contorted fine laminations and has been previously mapped as the Espanola Formation although no evidence of calcite was observed. Areas of higher magnetic intensity of this formation as shown on the magnetometer surveys appear related to magnetite content. Some minor pyrite was observed.
BK2-1 8-09-02 Brecciated Orthoquartzite
BK3-1 8-09-02 Quartz Vein
BK4-1 8-09-02
BK1-23-10-02
Quartz Vein
Calcitic Paragneiss
BK2-23-10-02 Rusty Recrystallized Quartzite
white, finely crystalline, moderately to well sorted, subangular quartz grains, Assay for Aubrecciated with infilling veins of light gray white quartz veins and veinlets.Appears to be an orthoquartzite sequence of the Serpen Formation subjected tofracturing and influx of quartz in part from the orthoquartzite itself. This unit isoften found in flat lowlying areas frequently swampy. Earlier mapping failed toshow the extent of this unit which maybe related to fault splays.
white to clear vitreous massive quarts from one of several veins alongside a Assay for Au possibly fault splay. A minor amount of feldspar was observed in the quartz. The amount of quartz observed was not significan to justify extraction for industrial mineral usess. No sulphides were observed.
simialr to BK3-1 8-09-02 but slightly whiter.
olive green mottled with dark green chlorite and light orange pink feldspathic Assay for Au blotches containing areas of caramel colured microcrystalline calcite. This rock probably represents an altered version of the Espanola Formation adjacent to a granitic gneiss such as sample BK1 -18-09-02.
light gray quartz with biotite and medium crystalline pyrite aggregates. Strong Assay for Au sulphurous smell. Sample appears to be a quartz rich nodule surrounded in part by a micaceous rind.
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 pg 12
BK3-23-10-02
BK4-23-10-02
BK5-23-10-02
Rusty Recrystallized Quartzite
sample similar to BK2-23-09-02 but exibiting more breccia-like features such as crushed quartz fabric with interstitial biotite and iron cabronate between fragments. Possible arsenopyrite noted in addition to pyrite.
Assay for Au
Plagioclase Quartz Biotite rustry matirx of cream white plagioclase and quartz containing biotite and Amphibole Gneiss amphibole. Matix contains very fine pyrite scattered erratically throughout.
Very difficult to obtain fresh non rusty samples. Adjacent rock appears to be a gabbrioic anorthosite with garnets and 5*26 of a dark subhedral submetallic mineral too fine to identify but nonmagnetic. Tiny clear accicular crystals of anhydrite noted on rusty surface.
Assay for Au
Recrystallized Quartzite
BK6-23-10-02 Rusty Nipissing Diabase
BK1 -24-1 0-02 Nipissing Diabase
BK2-24-10-02 Nipissing Diabase
white to tan medium crystalline massive recrystallized quartzite and plagioclase. Assay for Au, As Fractures show soft dark green (talc) with orange pink haloes (K+ alteration). Minor pyrite noted. One surface shows pink erytherite staining. Phlogopyte flakes randomly found throughout matrix.
white plagioclase matrix with black amphiboles altered in part ot a biotite and fibrous green amphibole. Scattered pyrite in very finely crystalline aggregates. Sample material was locally very weathered and rusty.
Assay for Au S Pd
dark gray with white mottling of plagioclase, medium crystalline, massive. This Assay for Au ft Pd sample shows a vein of finely crystalline chloritized material that contains very fine pyrite. In addition some very more pyrite occurs in the medium crystalline matrix. The sample was collected to illustrate a possible cause of the IP anomaly in the area of this diabase.
light gray mottled with dark amphibole, medium crystalline, massive. Containing Assay for Au S Pd minor pyrite occasionally associated with the black amphibole and magnetite. The sample was collected to illustrate a possible cause of IP anomaly in the area of this database.
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 pg 13
BK3-24-10-02
BK4-24-10-02
Pegmatoidal Nipissing Diabase
Sulphide Bearing Quartzite
BK4-24-10-02 Pegmatoidal Nipissing Diabase
mottled dark gray amphibole and white plagioclase laths. Very coarsely crystalline. Containing several blebs of multicrystalline pyrite. Magnetite crystals also present. Sample is magnetic and correlates with the magnetometer survey.
light pinkish white quartzite with 3*36 disseminated pyrite. The pyrite being developed as very fine clumps of crystals from clumps of green chlorite blebs. The quartzite is very well recrystallized with a masive interlocking matrix of medium crystalline crystals. The originial quartzite grains being obliterated. Some areas show minor pink feldspar crystals (K+ alteration). Some areas having more abundant green chlorite appear darker gray and contain more pyrite. Some jarosite alterations was noted in areas of orange pinkl feldspar associated with higher amounts of pyrite. Tiny clear accicular crystals of anhydrite noted on surface. A strong arsenic smell was present from one area which was very difficult to sample due to the massiveness of the quartz and its failure to break. The sample site appeared very similar ot the mineralization at the Long Lake Gold Mine. The location also correlatew with the IP anomaly assumed to be due to the pyrite within the Nipissing Diabase in the area.NOTE: This sample site is currently unstaked and lies about 44 meters @ AZ 260" of the line post 400m N of CP #3 claim #1211267.
similar to sample BK3-24-10-02 but somewhat more patchy in the distribution of pegmatite. Sample contains patches of multicrystalline pyrite.
Assay for Au 4 Pd
sample for Au, As
Assay for Au & Pd
Sudcan Eden Twp Report Bedrock Consulting Nov. 6, 2002 pg 14
MINISTRY OF NORTHERN DEVELOPMENT AND MINES
Transaction No:
Recording Date:
Approval Date:
Client(s):
177274
Survey Type(s):
W0370.00302
2003-FEB-26
2003-FEB-27
Work Report Summary
Status: APPROVED
Work Done from: 2002-OCT-17
to: 2002-NOV-24
O'SHAUGHNESSY, JOHN MITCHELL
GEOL
Work Report Details:
Claim# Perform
S 1211266 5805
S 1211267 51,884
52,689
External Credits:
Reserve:
Perform Applied Approve Applied Approve
5805 S616 5616
51,884 51,530 51,530
52,689 52,146 52,146
SO
Assign
5050
50
Assign Approve Reserve
0 5189
0 5354
SO 5543
Reserve Approve Due Date
5189 2004-MAR-01
5354 2004-MAR-01
5543
5543 Reserve of Work ReporW: W0370.00302
5543 Total Remaining
Status of claim is based on information currently on record.
41I06SE2003 2.25060 EDEN 900
2003-Mar-13 16:40 Armstrong-d Page 1 of 1
Ministry ofNorthern Developmentand Mines
Date: 2003-MAR-05
Ministere du Developpement du Nord et des Mines Ontario
GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5
JOHN MITCHELL O'SHAUGHNESSY 58 FOREST PARK CRESCENT THORNHILL, ONTARIO L3T 2M7 CANADA
Tel: (888) 415-9845 Fax:(877)670-1555
Dear Sir or Madam
Submission Number: 2.25060 Transaction Number(s): W0370.00302
Subject: Approval of Assessment Work
We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.
At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.
If you have any question regarding this correspondence, please contact STEVEN BENETEAU by email at [email protected] or by phone at (705) 670-5855.
Yours Sincerely,
Ron GashinskiSenior Manager, Mining Lands Section
Cc: Resident Geologist
Robert Gerald Komarechka (Agent)
Assessment File Library
John Mitchell O'Shaughnessy (Claim Holder)
John Mitchell O'Shaughnessy (Assessment Office)
Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:18033
ONTARIOCANADA
MINISTRY OF NORTHERN DEVELOPMENT AND MINES
PROVINCIAL MINING RECORDER'S OFFICE
Mining Land Tenure Map
' '""*5T tfv'-vLj 513MOON^f'^'-K"V'-'i
5125000N -—-' 5125000N
445000E 490CPOOE
U7M2one 17 5000m grid
Those wishing to stake mining daims should consult yvilh the Provincial Mining Recorders' Office of the Ministry of Northern Development end Mines for additional information on the status of the lands shown hereon. This map is not intended for navigational, survey, or land title determination purposes as the information shown on this map is compiled from various sources. Completeness and accuracy are not guaranteed. Additional information may also be obtained through the local Land Titles or Registry Office, or the Ministry of Natural Resources.
The information shown le derived from digital date available in the Provincial Mining Recorders' Office at the- time of downloading from the Ministry of Northern Development and Mines web site.
General information and LimitationsContact information; Toil Free Map Datum: NAD 63Provincial Mining Recorders' Office Tel; 1 (888) 415-9845 ext 57f Ejection: UTM (6 degree)Willet Green Miller Centre 933 Ramsey Lake Road Fax: 1 (877)670-1444 Topographic Data Source; Land Information OntarioSudbury ON PSE 665 Mining Land Tenure Source: Provincial Mining Recorders' OfficeHome Page; vww.mndm.gnv.onxa/MNDM/MINES/LANDS/mlsmnpge.hlm
This rtrap mey not show unregistered land tenure and interests inland including certain patents, iaases, easBments, right of ways, flooding rights, licences, or other forms of disposition of rights and intersst from Ihe Crown. Also certain lend tenure and land uses that restrict or prohibit free entry to stake mining daims may not be illustrated.
Date ; Time of Issue: Tue Mar 04 15:53:06 EST 2003
TOWNSHIP i AREA PLAN EDEN G-4042
ADMINISTRATIVE DISTRICTS l DIVISIONS
Mining Division SudburyLand Titles/Registry Division SUDBURYMinistry of Natural Resources District SUDBURY
TOPOGRAPHIC
Administrative Boundaries
T' "l Township
i"""] Concession. Uoi
pivj Provincial Park
P'™j ludian Reserve
: " ": Cfrff, Pit 4 Pite
^.,^.m, Contour
r Mifte Shafts
. Mine Hesdfrarne
Railway
Roed
Trail
Natural Gas Pipeline
Land Tenure
Freehold Patent
rjTj Surface And Mining Rights
r^J; SurfBM RighU Only
[TT, Wintry RijjHta Only
Leasehold Patent
r* !l SurtBCfi And Mining Rignts
r^Tj Surface RtlghB Onty
rpi Mlnlne RightB Only
Licence of Occupation
HO Us8tiMDtSp*cifiw)
'Uk'\ Surface And Mining Rignts
Mining Rights Onry
Land USB Permit
Order In Council (Not open for sinking)
Water Power Isspe Agresmenf
Mining Qa)rn
Filed Onty Mining Claima
LAND TENURE WITHDRAWALS
ArrtKK WShrifSWii frpm
Miring Acts Withdrawal Types Wem Surface And Mining Rights Wtltatrewn Ws Syrliice filers Only WHhdiawn Wm Mining Rtgrns Oily WrL*Kirawn
OfO*r in Councli Wilhdrawal Typaa Wsm Surftics And MirrldQ R^ritJ WtMmwn W^s Surfece ftghisOrilj Withdrawn V/nn Minlrifi RJjjrrts Wy Wrtndfavin
IMPORTANT NOTICES
LAND TENURE WITHDRAWAL DESCRIPTIONSIdentifier Type Date Description
764B Wsirt Jan 1,2001 PUBLIC ACCESS POINT 30/11/83W-LL-01B7 Wsm Jan 30. ZOOZ -in hre*"' http:ttww.mndm.80v.cn,cW-LL-C210 Wsm Feb 26,2002 SB href'" hitp:ftwww.mndm.gOT.on.coMNDMfMINESiANDSflMBg;gllK3f2002ordeW-S-Uffiil Ws Feb 22. 19S4 POTENTIAL ROAD W-S-11/8* 22/02/84 S,R.O. 195150
W.-B-11/94 Ws Feb22, 1984 POTENTIAL ROAD W.-S-1V94 22/02/94 S.R.O. 135150W-LL-P187 Wsm Aus29,2002 *a href*' http!ffvww,mniim 1 gov.on.ea*INDM*IINES;LANDSfltvl88^t]W2002orde
41I06SE2003 2.25060 EDEN 200
i/)O)oo
4-
N
Map 2 - Prospecting Sketch SudCan Claims - Eden TownsNn
oH CN
Legend
GraniteGabbroPoikiolitic GabbroLaminated SiltstoneQuartziteQuartz Veins X stockworksFracture, Fault
Accessories
py Pyriteasp Arsenopyriteery Erythrite
Sept T 7, 2002 Sept 18, 2002 Oct. 23, 2002 Oct. 24, 2002
200 300 400 500m
Map Produced by Bob Komarechka of Bedrock Consulting - Nov. 23, 2002l^Po
I-/ALF
EXPIRED
Iz11
YBK2-18-09"K \ r1211267
BK3-18-09-02^
41I06SE2003 2.25060 EDEN 220
