AREA: ROPE LAKE REPORT NO: 2 1
010
WORK PERFORMED FOR: M innova Inc.
RECORDED HOLDER: S AME AS ABOVE (xx)
: OTHER
CLAIM NO.
TB 6464428 TB 646432 S TB 646433
TB 646431, TB 646433, TB 646434 S TB 646439
HOLE NO.
WL-056
WL-057
FOOTAGE
666.52m
DATE
May/88
NOTE
(D
1092.0m May-June/89 (1)
NOTES: ( 1) W8904.497, filed Dec/89
MOLE NUMBER: WL-D57HINNOVA INC.
DRILL HOLE SECORD IMPERIAL UNITS:DATE: 19-0ctober-1989
METRIC UNITS: X
MS ACT NAME: WINSTON LAKE PROJECT NUMBER: W070
DATE STARTED:DATE COMPLETED:
DATE LOGGED:
646431 , 646433 , 646434^^
PLOTTING COORDS GRID: MINE GRID EXT. NORTH: 12700.DON
EAST I 10I40.00E ELEV: 10465.00
COLLAR ASTRONCMIC AZIMUTH: 270* O 1 D"
Hay 22, 1989JLT* 20, 1989Jine 25, 1989
COLLAR SURVEY: NOMULTISHOT SURVEY: NO
ROD LOG: NO
ALTERNATE COORDS GRID:NORTH: O* O EAST: O* O ELEV: 0.00
GRID ASTRONOMIC AZIMUTH: 250' O 1 O"
PULSE EM SURVEY: YESPLUGGED: YES
HOLE SIZE: M
COLLAR DIP: -83* O' O*LENGTH OF THE HOLE: 1092.00*
START DEPTN: O.OOnFINAL DEPTH: 1092.00*
CONTRACTOR: ST. LAMBERT DRILLING LTD.CASING: 4 FT INTACT
CORE STORAGE: CLEAVER LAKE.
PURPOSE: TEST DOWN DIP OF STRONG ALTERATION AND ZN HIM IN VL-W
DIRECTIONAL DATA:
Depth Aitrononlc Dip (•) Ailnrth degreei
50.100.150.200.250.300.350.400.450.500.550.600.650.700.750.800.850.900.950.1000.1050.
25.50.100.150.200.
00 -83'000000000000000000000000000000 -000000000000 25500 24900 23900 236
-77'•76'•74'•69'•68'•64'•62'•57'•55'•SO'•48'•44'•43'
0'0'0'0'0'D'0'0'0'0'0'0'0'0'
•4V30'•40'•38'•36'•35'•34'•S3'
0' -82'0- -82'0' -78'0' -76'
00 23V 0' -72'
0'0'0'0'0'0'0'0'0'0'0'
Type ef lett
ACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDMULTISHOTMULT 1 SHOTMULTISHOTMULTISHOTMULTISHOT
FLAG Coimenu
OKOKOKOKOKOKOKOKOKOKOK FAINTOKOK FAINTOKOKOKOKOKOKOKOKOKOKOKOKOK
Depth (•)
250.00300.00350.00400.00450.00500.00550.00600.00650.00700.00750.00800.00850.00900.00950.001000.001050.001085.00
Astronomic Azimuth
230'232-233'238'244'242'24*'249'25V253'252'254'256'259'268'252'259'26V
*i.-...
0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'
Dip degree*
•70' 0'-67-30'•65' O 1•59' 0'•56' 0'-52' 0'•*9'30'•46-30'•44'SO'•4V 0'•39' 0'•37' 0'•37' 0'•36' 0'•36' 0--36' 0'-34' 0'•34' 0'
.
.
.
.
.
.
.
Type of lett
MULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULT I SHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOT
FLAG Comwnt.
OKOKOKOKOKOKOKOKOKOKOKOKOKOK
PXOKOKOK
,HOLE NUMBER: VL-057 DRILL HOLE RECORD LOGGED IYl C. W.ENN PAAGE: 1
HOLE NUMBER: WL-057MINNOVA INC.
OR ILL HOLE RECORD DATE: 19-October-19B9
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANCLE TO CA ALTERATION MINERALIZATION REMARKS
0.00TO
1.70
OVERBURDEN 06.
1.70TO
412.50
PILLOWED KAF1C FLOW BMA*
Fine grained, dark green, pillowed mafic flow.Strongly foliated and locally laminated 8 .......Perterved pillow telvedge occur every 10-100cm
consisting of hornblende md quartz/feldspar bands (inn-cm tcale). Bands between pillows exhibit strong sausaerltiiation.
21.7-21.8Barren ail Iky white quarti vein.
21.25-Z1.35 FO
30.0-50.1 GR DY
36.1-36.2Conformable quart! vein (long epidote altered
pillow (clvedge.
39.5-42Broken blocky core.
{39.45-39.75} .FT.Fine (rained, pele pink brown tliceoua unit with
harp conformable contact against Mfic...........
48.6-41.8Zone of chloritic vet competent BMA (possibly healed fault?}.
55.3-55.5Epidote altered nan ive pillow cor*.
69.15-69.22Mm l ve epidote altered pillow cor*.
No hydrothermal alteration.* 3X quarti carbonate veining
conformable to the foliation. Approximately 2X quarti at li l Ice sweats * 3cm wide associated with pillow selvedges.
6.6-7.15Ceusseritized pillow selvedge.
18.35-21.25Weak pervasive tausserltisatlon of fine (rained mefic In association with abundant quartz epidote stringer* that ay locally for* vein breccia.
Incipient biotite l phlogopite alteration of felsic tuff.
Strong chlorite development associated with possible fault.
59.2inn w ide band In phlogopite
alteration.land Is conformable with laminated
pillow selvedges
69.9-70.3
Trace to locally 5X pyrite. Pyrite when present appears to be associated with pillow aelvedgec.Trace amounts of pyrrhotite.
18.45-18.6510-15X fine grained pyrite associated
with Irregular quartz vein - geochemed.
23.5Trace pyrrhotite with 2* pyrite In
conformable silica sweat.
U am teal* pyrite clou.
61.852m wide slllcs sweat with abundant fine pyrite.
MOLE NUMBER: VL-057 DRILL HOLE RECORD LOCOED lYi C. GLENN PACE;
HOLE NUMBER: VL-057MlNkOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROM TO
ROCKt m TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
1M.MM.JEpidote altered, Miilve pillow core.
^12.5-117.0} .FLT ZONE*Zone consists of broken and blocky core and fault
breccia at 115.0-115.Z.fault breccia It pale green with on scale breccia
fragments In fine grained pale green tiatrlx.Faulting fi ......................................
117.0(MA becomei nore homogeneous and passive. The laminated pillow selvedges decrease and the flow
5X pale brown phlogopite associated with laminated, sausseritiied, pillow selvedge.
71.75-71.9Massive, sausseri 11led and possible brecciated pillow core.
W. 0-89.0Abundant mi-cm scale phlogopite bands associsted with laminated pillow selvedges.
85.0-85.0JIX mn scale pale yellow, glassy clou-
garnet/staurolite 1 w ith incipient phlogopite.
90.0-91.0n hematite stained hairline quartz/ feldspar atringers.
94.9-95.0Zone of epidote alteration.
Minor carbonate vein associated with faulting.
Trace - 5X leucoxene generally located within aauaserltltad pillow eoret.
K f ine to coarse anhedral to subhedral pyrite.
Trace to locally 3X fine disseminated pyrite.
93.J-93.J52X very fine grained pyrite associsted
with Intarplllow silica sweet.
107.171.2cm wide pyrite blob in silica
aweat.
110.5-110.65X very fine grained, disseminated
pyrite associated with conformable quartz vein.
Trace pyrite fnd fault breccia.
129.0
HOLE NUMBER: UL-057 DRILL NOLI KECORC LOWED IT I C. 8LENN FACE l
HOLE NUMBER: Ut-057HINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
menTO
ROCK TYPE TEXTURE AND STRUCTURE
becomes nore pillowed with medium grained massive causteritiied pillow cores.
141.10-141.15 Vuggy quarti/feldsper dyke.
144.3-144.35 Vuggy felsic dyke.
144.5-144.6 Broken core.
171.5-186.0 Broken and blocky - core fractures parallel to
Local rubble zones at: 175.7-176.0 176.5-178.8 179.8-180.4 181.6-181.7 185.6-185.7 2cm of chloritic fault gouge at 180.35.
{180.35} .UT.
166.0 BMA exhibit* an-cti acaU hornblende va quartz/ feldspar lamination*, lamination* occur along pillow aelvadgat and auy locally be tautierltlied.
201.5-201.6 Small acalt faulting offaettlng am tea i e
207.65-208.22 In t Dyke Medium grained, atrong foliation, light speckledgreen
{209.4-211.21} .10. At above.
218.05-218.15
ANGLE TO CA
47
50
60
TOto30
TO
ALTERATION
Locally abundant irregular quartz
None to local phlogopite at am tcalaband*.
Nona.
MINERALIZATION
Minor pyrite associated with conformable quart! vein.
174.8-175.6
pyrite.
Trace to 2X pyrite concentrated In the laminated pillow selvedge*.
Nona.t
REMARKS
HOLE NUMB. DRILL HOLE RECORD LOGGED IT: C . GLENN PAGE:
HOLE NUMBER: UL-057MINNOVA INC.
CHILL HOLE RECORD DATE: 19-0ctob*r-1989
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
As above with 1X mn ecale anhedral feldspar pheno's.
223.15-Z23.4Possible chert surrounding BHA pillow. Chert looks recrystalliied and contains 2X anhedral pink feldspar.
215.1-215.3finely laminated interpillow mafic tuff.Lamination A ............................
256.0-256.2 Broken core.
256.3-256.*Massive, aauaaerltlied pillow core; aimilar core at 256.5-256.8.
265.6-Z73Broken and blocky core; possible healed fault with fault breccia at 268.2. fault S .........................................
2T7.4-277.9Snail saueserltized pillow corn that exhibit
amygdaloidal outer tint.Amygdules are < 1am in diameter and exhibit a gradatlonal contact.
Z79-Z94.5BMA exhibits a fine grained, dark green apeckled gabbroic appearance. Strong foliations .............................. 60
290.J-J90.5Milky white quartz vein conformable with fabric.
Weak hematite staining of feldspar pheno't.
225.0Hematite staining appears within
quartz feldspar stringers and along fracture surfaces.
None.Trace amount* of leucoxene tt very
fine grained chalky white patches.
Nona.
3X fine sub-euhedral pyrite disseminated along margins and within chert.
243.12-243.253-5X fine pyrite disseminated in and
around possible recrystallited interpillow cherts.
252.1-253.21-5X fine grained pyrite disseminated
in very fir* grained aiafic flow. Pyrite also occurs as fine bands.
Z67.15Minor pyrite associated with quartz/
feldspar vein.
Trace pyrite.
Trace - U pyrite.
HOLE NUHBE' "^-057 DRILL HOLE RECORD LOCOED BY; B. CLENN PAGE) S
HOLE NUMBER: WL-057MINNOVA INC.
DRILL MOLE RECORD DATE! 19-0ctob*r-1989
FROM TO
ROCKTEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
299.2-299.65 tectonic bx Small ^ < 1 cm) fragments of (MA surrounded by
numerous quartz carbonate veins. Zone 8 ..........................................
299.82-300.5Milky white quartz vein, conformable to fabric fi Upper contact is sharp.Lower 10cm of vein contains abundant fragments of
BMA volcanics.
318.98-319.42 fD
321.0-321.7Trace to 2X magnetite associated with rims of
massive, sausseritized mafic pillow cores.
324.22-324.51Irregular quartz feldspar vein/dyke.
347.9-348.0Irregular quartz/feldspar vein.
348.3-349.5Thin amygdaloidal bands up to 2cm wide. Amyodules
look very similar to amygdule* associated with Massive, tausserltiitd pillow corts.
372.3-390Mm scale amygdule* occur sporadically (up to 2X) Amygdule! are flattened at 1.5:1 and are not associated with lausserltlzed pillow corts.
390.V5-391.10 Oti/ftp vein/dyke
Weak hematite alteration along hangingwall contact.
334.0-348Patchy w*ak phlogopite alteration of cm acale bands.
Trace - IX very fine grained pyrite.
330-333.223X disseminated pyrite as fine < lam
crystals and blot*.
S89.47-S89.T5-7X pyrite in thin band*.
394.0-394.14-5X m acale^jyrlte stringers.
394.1-394.71-2X pyrite stringers.
J94.7-395.25
HOLE NUKBf DRILL MOLE RECORD LOGGED til C . CLENN PAGE!
HOLE NUMBER: VL-057MJNNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROM TO
412.50 TO
465.92
ROCK TYPE
GABBRO *GB*
TEXTURE AND STRUCTURE
395.25-396 Broken and blocky core.
39S.6-39B.8 Vein bx
406.4-406.6 Vein bx
Gabbro exhibits indistinct contact with BMA. Fine to medium grained gabbro texture becomes
apparent at 412.5 but massive, seusseritiied pillow cores persist.
427.0-432 Gabbro exhibits weak to iocally strong
magnetism in 1-3X very fine grained cub-et*idrat magnetite crystals.
427.4-427.6 INT DY
Dyke Is pale grey-white with 15X mafic clotsInn x 3am.
<437.55-437.9j .FT raft. Finely laminated (an scale) felsic tuff exhibits
fine pink layers alternating with nfic levers. Layer* may contain en acale quarti/feldepar
fragment* ? the layers drape over the top of the fragments.
Tuff ha* been strongly quarti epidote altered
440.5-440.7 DB Irregular but sharp contact.
4440.82-442.1} (OB.
Hanging wall contact sharp egalnst grained .dyke.
441.5-441.73
ANCLE TO CA
TO
20to30
30
ALTERATION
Persistent leucoxene 1-2X.
No hydrothermal alteration. Strong quarti epidote alteration associated with vein breccia.
MINERALIZATION
1-2X very fine grained pyrite stringers.
Trace pyrite.
409.5-409.6 Trace chalcopyrite end .SX pyrite
associated with quarti/feldspar vein.
Trace pyrite.
426.1 Trace chalcopyrite in quarti vein.
492.15Trace chalcopytle In quartz vein.
3X pyrite as very fine (rained cryitat aggregate* - looks remoblllied associated with vein breccia.
f
REMARKS
Gabbro looks extrusive.
MOLE NUMBER: WL-057 DRILL MOLE RECORD LOOSED IT: C. GLENN PAGE!
HOLE NUMBER: WL-057MINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROMTO
465.92TO
471.90
471.90 TO
480.20
ROCKTYPE
PILLOWEDMAFIC FLOW SMA/BSF.SIRDSHITFLOW
LAMINATED CHERT MAFICTUFF ANDINTER MEDIATESEDIMENT CRT/Win T
TEXTURE AND STRUCTURE
Granite xenolith within diabase dyke.
4449. 87-456. If *OB.Contacts S ...............,......................
{4S1.i-t53.lL Broken core - possible *FLT7*
456.45-456.52 DB
.|456. 1-464. 15f *flHA7.Possible pillowed BMA has local intrusive -
gabbro textures but alto exhibits quart: epidotealtered pillow cores. Upper contact is obscuredby dyke.
Lower contact is also dyked out.
{464. 15-465. 92f -tib*Diabase dyke exhibits amygdaloidal texture with
quartt carbonate rimmed amygdules in the middleof the dyke.
Very fine grained pillowed, dark green mafic flowexhibits < 2X feldspar glomerocryst! generally< Ion in diameter but as large as ton in diameter.Well foliated and locally laminated on mn scale.Laminations My indicate interpillow cherty seds.
Pillows are massive and exhibit quart! epidotealteration.
Mixed tone of finely laminated cherty tuffs.Mf le tuffs, flows and sediments.
471.9-473.05Finely laminated recrystsKiad and disrupted
chert and cherty felsic and Mf ic tuffs(nn-cm scale).Unit exhibits 5X (mn scale) magnetite crystals.
ANGLETO CA
52
10
63
ALTERATION
None.
470.J5-470.8VAlteration of ISF consisting of:10X cordierite15-20X biotite5-10X anthophylliteAlteration in sharp contact with trash
MflC
None.
*72.1-*T2.Z5Strong quart! epidote alteration
MINERALIZATION
Trace pyrite.
460.0-460.3IX pyrrhotite as mn scale stringers.
Trace pyrite.
466.9Trace chalcopyrite in quart! vein.
Trace -U very fine graineddisseminated pyrite.
REMARKS
HOLE NUMBER: WL-057 DRILL MOLE RECORD LOGGED BYl C. CIENN PAGE)
HOLE NUMBER: wl-057MINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1v89
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
The fine laminations ney give way to more massive granular looking sediments. The magnetite may be derived from the tediment portion of this unit.
473.D5-473.2 Thin mafic flow.
Very fine grained, dark green, well foliated.
473.2-473.* Int tuff Pale brown-preen, very fine grained, locally
cherty banded on cm scale. Green cm scale bands alternating with pale brown intermediate bands up to 6cm wide. Narrow cherty lection occurs at 473.35-473.4 and
exhibits fine lamination.
473.4-473.6 Intermediate garnetiferous sediment massive, fine
grained, granular, grey-green sediment.
473. 6-473. B Ha Tuff Dark green, very fine grained, finely banded
mafic tuff. Sands are composed of quartz and feldspar material alternating with more massive, mafic bands.
Lower 3cm of mafic tuff exhibit 2X mn scale anhedral magnetite crystals-possible contamination from underlying sediment.
4473.B-476.58L *U* Flow Mafic flow with tuff/sediment flow top.
473.B-474.2 Finely laminated tuffaceous sediment -
massive from 473.B-474.0 with cm scale
474.2-474.5
ANCLE TO CA
W
62
70
69to 5556
62
ALTERATION
creates pervasive pale green colour.
None.
None.
5X cm scale garnets. 2-5X * mm scale magnetite crystals.
tt f ine phlogopite is thin wisps and mm scale ragged clots.
473.8-474.0 3X cm tcale garnets related to sedimentary component in flow top.
MINERAL RATION
None.
None.
None.
Trace pyrite.
REMARKS
HOLE NUMBER: UL-057 DRILL MOLE RECORD LOGGED IVt G. GLENN PAGE: 9
HOLE NUMBER: WL-057HINNOVA INC.
DRILL MOLE RECORD DATE: 19-0ctober-1989
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
Very fine grained, dark green mafic flow that exhibits cubhedrat amphibole phenocryst*. This flow ends abruptly at another tuffaceous sediment flow top as described above, and grades Into massive mafic flow. Lower flow exhibits a possible pillow core adjacent to the lower contact. Core is quarti epidote altered.Lower contact fi ..........................,......
476.56-477.53 Felsic TuffVery fine grained, white to green, felsic
matrix locally supporting fine m scale mafic clots.
4477.53-460.2* *MA* flow Dark green, very fine grained moderately foliated mafic flow. Flow exhibits local garnet and chlorite (retrograded from garnet)
4460.2-482.3} *Alt FT*Sharp upper contact to felsic S .................Upper .Tim exhibits weak to moderate alteration with fine grained granular texture. Lower portion of unit Is intensely altered.Colour varies from pale grey white to blue brown.Strong foliations .....................,........Unit exhibits fine lamination at 480.1.Lamination tn scale fi ...........................
karren white quartz veins at:480.3-460.35460.4-460.4J4tO.76-4BO.82
70
None. Trace pyrite.
Trace - IX very fine grained, disseminated phlog.
478.8-479.53-5X garnet 2-Jmm in diameter,
euhedral. 2-SX chlorite - retrograded from
garnet. Chlorite exhibits euhedralshape of garnets.
480.2-480.95Weak to moderate alteration consisting
of fine grained:cordierite 5Xblotite/phlogoplte 7X
460.95-482.3Intense alteration consisting ef:
cordierite 10-15Xbiotlte/phlogopite 15-20*staurolite 5X
Trace * IX very fine grained disseminated pyrite.
Trace pyrite.
480.20TO
(95.62
GABBRO CB. Dark green to medium grained, massive to weakly
foliated mafic intrusive with fine grained chiliad contact 8 ........................................
Gabbro exhibits amphibole porphyritic texture and locally exhibits cm scale quartz/feldspar
78
None.
None.
None.
Nona.
HOLE NUMBER: UL-057 DRILL HOLE RECORD LOGGED BY! G. GLENN PAGE) 1 0
HOLE NUMBER: Wt-057HINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROMTO
495.62TO
501.90
501.90TO
530.95
COCKTYPE
TRANSITIONZONE T2*
GABBRO*GB.
TEXTURE AND STRUCTURE
Clots - look similar to "Bird thlt" In BSf.fluartz/feldspar clots make up 2X and are very
faint.
Transition lone marked by appearance of 3-5Xphlogopite as wisps and w i spy blotches. The tileof the amphibole crystals increases to 2-3ffro indiameter.
The grain site then increases to 2-lam. Lowercontact is marked by blotches of quartz/feldsparbetween 501.S-501.55. The transition lone thenbecomes very fine grained and exhibits a granulartexture and weak magnetism.
Fine to medium grained, moderately well foliated.Dark green, speckled mafic intrusive. Locally mylook pillowed with massive quartz epidote atter'nOverall gabbro is homogeneous.
510.6-511.11cm wide quartz-carbonate vein running parallel
to CA.
^521. 0-530.9} *CLR Raft*
521.0-522.6Mixed clotted rhyolite and fine grained gabbro.
Contacts are indistinct.
521.0-521.2 Mafic tuff/CLRQuartz veins marking contact between lau i ve
mafic tuff and finely laminated intermediate tuff.
521. 20-521. JIntermediate tuff exhibits fine m acale
ANGLETO CA
71
n59
ALTERATION
Trace - 1X leucoxene.
Trace phlogoplte/biotlte (relativelyunaltered)*
MINERALIZATION
Trace pyrite.
Trace pyrite.
None.
3-5X medium grained euhedral pyrite -predominantly atsociated with quartzvein. 1-2X very fine grainedinterfollal pyrite.
REMARKS
MOLE NUMBER: WL-05T DRILL HOLE RECORD LOGGED (Y: G. GLENN PAGE! 11
HOLE NUMBER: UL-057MINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
521.3-521.95More massive mafic tuff/clotted rhyolite, very fine grained, dark brown green. Lower contact with gabbro is sharp 8 ..........
Trace - 2X very fine grained phlogoplte/blotlte of the mafic layers.
None - trace biotlte/phlogopite.
521.95-522.65 GBFine to medium, dark green speckled gabbro. Lower
contact with massive, clotted rhyolite is indistinct over 20cm.
522.65-530.95 CLRIntermediate felsic clotted unit consisting of
very fine grained pale white grey quartz/feldspar matrix with 10-60X mafic clots < 1mm in size.Unit is moderately foliated S ...................
No hydrothermal alteration.
69
2-3X very fine grained bedded pyrite.
2-4X fine to medium grained pyrite associated with 2-3cm wide blue quartz vein.1-2X very fine grained disseminated
pyrite.
Trace pyrite.
526.7-526.910X coerce euhedral pyrite associated
with 2 milky white quartz veins.
530.95TO
904.00
GABBRO GB* As above. Locally magnetic contact with clotted
rhyolite is aharp but irregular 8 ...............
5*3.35-5*3.9 MD
60
565.75-566.4Milky white quartz vein.
579.1-586.62 Up phyrlcGabbro with 20* im acale feldspar phenc's. Local pale green phlogopite occurs in wisp* and increases to 2-3X downhole.Zone ends abruptly at fault zone.
581.15-581.25
581.65-581.8
GR DY
GR DY
585.92-586.1* Felcic Dyke
{586.62-589.6} *FLT ZONE*Strong fabric developed In gabbro leading up to 10cm chlorite fault gouge at 587.8-587.9.2cm of chloritic fault gouge at 589.3.
65Strong chlorite developed associated
with fault lone.
Trace pyrite.
565.75-565.15Chalcocite In quartz vein.Est: 2* Cu l 0 .40m
Locally the gabbro any exhibit extrusive textures - massive quartz epidote altered pillow cores.Intrusive is possibly partially
extrusive.
Possible t rant It ion sane T
Trace pyrite.
HOLE NUHBEft: W.-057 ORlli HOLE RECORD LOGGED BY I G. GLENN PAGE l 12
HOCE NUMBER: WL-057MINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROH TO
ROCK TrPE TEXTURE AND STRUCTURE
ANCLE TO CA ALTERATION MINERALIZATION REMARKS
588.2-594.5Locally weakly banded and mgnetlc gabbro bands are * 2mm in diameter and are quartz/feldspar in composit ion.Banding G .......................,..............
592.25-593.35 Mo fsp
623.1-633.15 Milky white qv.
634.6-63A.68 Mi Iky white qv.
636.05-636.2Quart! epidote bleached tone.
650.02-650.43Gabbro contains 1-2X feldspar glomerocryst* that range from 20mm x 3om to 25mm x 25mm
655.62-655.9Gabbro exhibits 2im wide quartz and quart i l feldspar bands. Banding doesn't look like veining.Ouartt gabbro composition is also exhibited at
660.0-660.2.
655.9-656.2 DB
{671.15-672.25f *FD.Light pink, massive, homogeneous felsic dyke with 5cm intrusive breccia on upper contact.Contacts sharp G ................................
73
42
ei672.42-672.62 As above.
FD
{674.65-675.9} .FO. As above.
Gabbro still exhibits 3X very fine grained leucoxene as fine ufsps.
613-61430X quartz epidote veining parallel to
CA.Locally strong hematite associated
with veining creates a red green hue
1-2X very fine grained leucoxene.
661.25-661.353-5X mn (cale phlogopite witpe.
672.8-673.23t phlogopite as an scale wisps in
fresh looking gabbro. Similar phlogopite rich tones it: 673.6-674.65 (SX)
Trace pyrite.
None.
624.5Pyrite associated with quartz vein
minor hematite staining.
3X fine euhedral pyrite associated with quartz vein.
2X pyrite associated with qv.
Glomerocrvsts support for partly extensive nature to gabbro ?
Trace - 1X disseminated pyrite. 4671.15-675.9} .felsic dyke (warn 7.
HOLE NUMBER: Wl-057 DRILL MOLE RECORD LOGGED IT: G. GLENN PAGE: 13
HOLE NUMBER: WL-057HINNOVA INC.
DRILL HOLE RECORD DATE: 19-0etober-1989
fROHto
ROCK TYPE TEXTURE AND STRUCTURE
{675.9-680.451 *PX. Meta pyroxenite displaying dark green - black
colour, medium grained size, granular texture and strong magnetism.
from 678.4-676.7 and broken core at 679.2-679.5.
{680. 45-681 .05} *T2. Transition tone displaying strong phlogopite
alteration, medium grain site, and granular texture. Colour is dark brownish green.
685. 82-656. 0 KD
691.8-692.7 Strong foliated gabbro. Foliation Increases in intensity towards centre of the lone.
698.4-733.7 Gabbro starts to display pseudo banded appearance with bands < t "m wide composed of quartz/feldspar. Locally the quartz/feldspar forms ntrix (up to
SO*) and m scale amphibole crystal*. Banding 8 .......................................
712.5-713.4 GR DY
4728.6-730.6f -OB. Diabase dyke has sharp irregular contacts that run tubparatlel to the CA.
73J.7-744.5 Gabbro displays medium to coarse grain ill*
with feldspar crystals up to 4mn In diameter. ftp has a rolled appearance and have been localized Into bands.
744.5 Typical gabbro texture and appearance returns.
ANGLE TO CA
BOBS
73
10 15
ei
ALTERATION
682.2-682.5 690.0-690.S
2-3*. pervasive chlorite alteration of met* PX.
10X phlogopite as pervasive wisps surrounding amphibole crystals
Trace phlogopite.
Trace - 1X leucoxene.
713.4-713.6 2X phlogopite as wisps.
MINERALIZATION
None.
None.
None.
712.4 1mm wide band of magnetite (SOU) and pyrite (50X).
center of the band and nay encapsulate an acale monetite crystals
j
REMARKS
HOLE NUMBER: Ut-057 DRILL HOLE RECORD LOGGED IY: C. GLENN fACE l 14
HOLE NUMBER: Wl-057M1NNOVA 1MC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROM10
904.00TO
910.15
ROCKTin
QUARTZFELDSPARPHYSIC FLOW.OFF.CAMP FLOW
TEXTURE AND STRUCTURE
^45. 5-7*7. Of *GR DY.
7*8.95-749.45 GR DY
756.4-757.0 GR DY
775. 92-776. e MDFeldspar phyric.
BOS. 5Blue quarti vein - barren.
812,85-813.5 MD
852.9-653.0 GR DY
Sharp but Irregular contact against gabbro S ,...OFF ranges from blue grey to grey white In colour
fine grained and massive to weakly foliatedfoliation B .............
904.0-906.4
ANGLETO CA
30
30
30
47
as
ALTERATION
755.9-756.15Silicified gabbro with 3-5X phlogopite
as patches.
758.75-759.11-2X phlogopite as wisps.
Weak quarti epidote bleachingassociated with abundant stringers.
827.55-827.65Ouarti epidote bleached zone.
862.4-863.935-7X quarti carbonate stringers at
various angle*.
866.0-866.t85-10X quarti carbonate stringers.
872.2-872.4Silicified gabbro.
873.4-873.5euarti epidote bleached gabbro.
MINERALIZATION
751.9Minor pyrite associated with irregular
quarti/feldspar vein.
755.9-756.153X very fine grained disseminated
pyrite.
Minor pyrite associated with uppercontact of granite dyke.
None.
809.4Minor pyrite associated quarti epidote
vefning.
866.0-866.185X pyrite associated with quarti
carbonate stringers.
Hone - trace pyrite.
f
REMARKS
MOLE NUMBER! VL-057 DRILL HOLE RECORD LOGGED IT l 6 . GLENN PAGE l IS
HOLE NUMBER: UL-057MINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
OFF it fine grained, dark blue grey and looks weakly altered.
906.4OFF le pale grey white with little to no mafic content.Locally it exhibits a very fine grained sugary
texture.
^912.8-913. U \ vCRT/MTxVery fine grained, dark green, bedded cherty
mafic tuff. Thick mafic beds seperate thin cherty felsic bands.Unit is disrupted and may represent flow bottom breccia to OFF.
From 91J.16-913.26Fault with fault breccia disrupts the bedding.Fault S .......,.................................
913.26-9U.1 Ma FlowDark green, very fine grained, mafic flow with
moderate foliation fi .............................Lower contact with OFF is sharp fi ...............
920.5-923.0 Intermediate phase?Fine grained granular, grey brown lone
exhibiting strong foliation fi ....................Contacts with pale grey white OFF are indistinct
over 20cm.
922-930.75 Patchy alteredOFF ranges from fine grained sugary, pale grey -
white relatively unaltered OFF to coarse granular strongly altered OFF.
Lower contact with gabbro as (harp 8 ............
89
90
Alteration consists of 5X biotite/ phlogopite as im em scale wisps/bands. Trace -U sillimanite it 905.9-906.2.
Incipient biotlte/phlogoplte.
929.2-929.5 MD
None.
5-10X biotite. Trace sillimanite
Local strong alteration consisting of:biotite/phlogoplte 20-30Xchlorite 10*quart! 5XZona* of strong (Iteration occur it:925.7-925.6926.9-927.tZ928.6-926.79J0.65-9J1.15
909.0Trace chalcopyrite.
913.16-913.265-7X pyrite, very fine to fine grained
disseminated and bedded in matrix of brown silica ?
Trace - IX very fine grained diseminated pyrite.
Trace pyrite.
Trace sphalerite in quartz vein (t 929.6-929.7.
MOLE NUMBER: WL-057 DRILL HOLE RECORD LOGGED til 6. GLENN PAGE: 16
HOLE NUMBER: WL-057MINNOVA INC.
DRIU HOLE RECORD BATE: 19-0ctober-1989
FI! OH TO
930.15 TO
937.70
937.70 TO
939.65
939.65 TO
977.85
977.85 TO
981. W
981. M TO
982 75
982.75 TO
984.85
ROCK TYPE
GABBRO tcGB*
TRANSITION ZONE *T2*
META-
PYROXEKITE PX*
TRANSITION ZONE*TZ*
ALTERED QUARTZ PHYRICRHYOLITE FLOW
CAMP FLOU
MAFIC FIOU MA/MO? )* LADDER FLOU OR DYKE?
TEXTURE AND STRUCTURE
Dark green, fine to medium grained, massive, speckled differentiated mafic intrusive. Upper contact displays 15cm chilled margin and
is quartz bearing. Lower contact with transition lone it faulted.
^37.7f .FIT. Dark green, chloritic, weakly magnetic fine
grained unit.
Dark green-blue, massive, homogeneous unit exhibiting strong magnetism - 15-20}. mn scale magnetite crystals.
{940. 8t -f LI. 1cm chloritic fault gouge.
Dark green, fine grained, equigranular transition tone exhibiting minor pervasive chlorite as matrix to dark green amphibole phenos. Only trace feldspar present. Upper contact is marked by disappearance of
magnetism exhibited by PX and the development of chlorite.
Moderate altered OFF exhibiting, moderate to
Fine to medium grained and grey-blue-brown
Dark green, fine grained, weakly bedded moderately foliated mafic flow.
982.4-983.1 Possible flow top exhibiting weak bedding -
ANCLE TO CA
76
80
ALTERATION
None.
Moderate pervasive chlorite alteration and minor carbonate veins.
Minor quartz carbonate vefning.
Minor pervasive chlorite.
Weak to moderate pervasive biotite S-10Xcordierite < 3X
Moderate to strong brickwork style
biotite 20-SOXcordierite 20-50X
over 10cm.
None.
MINERALIZATION
None.
None.
None,
None.
Trace pyrite.
REMARKS
HOLE NUMBER: WL-057 DRILL HOLE RECORD LOGGED Ifl G. GLENN PAGE: 17
HOLE NUMBER: WL-057MINNOVA IHC.
DRILL HOLE RECORD DATE: 19-0etober-1989
FROM TO
9M.65 TO
998.00
998.00 TO
1016. Z5
1016.25 10
1023.75
ROCK TYPE
ALTERED QUARTZ (FELDSPAR) PORPHYRY
ALTERED MAIN OFF-
OUARTZ FELDSPAR PORPHYRY nOFP* MAIM Off
HIKED ALTERED SILICEOUS AND TUFFACEOUS
TEXTURE AND STRUCTURE
possible chert layers 7 Chert ? layers tp to aim thick are milky uMte.
983.1-98A.e5 Mafic flow 7 It dark green, homogeneous and weak
feldspar pnyric -feldspars < Inn In tile.
Grey brown, fine grained, locally granular, quartz phyric felsic unit. Unit exhibits thin discontinuous (mf ic-chloritlc
Quart! occurs as fine grained groundmass exhibiting a mosaic appearance.
4990.35-992.B} *OR DY. Granite /pegmatite dyke with 15X coarse euhedral
biotite.
Pile grey, massive, homogeneous, very siliceous quartz feldspar porphyry. Quartz eyes make up 20-50* in very fine grained siliceous matrix, feldspar makes up < 1W as very fine grained white subhedral pnenocryste.
{998.0- 1001. 35} *GR DY. As above.
1005.3-1005.45 GR DY As above.
1005.6-1005.9 GR DY At above.
1006.1-1006.5 GR DY As above.
1016.25-1019. 45 Massive, altered siliceous sediments prey - green
In colour, moderately foliated end weakly
ANGLE TO CA
06
ALTERATION
Weak alteration consisting of * 5X biotite associated with mafic tuffaceous layers.
fine silky wisps to 2-SX Trace garnet
Weak pervasive biotite alteration Trace garnet. Locally strong, brickwork style
alteration with biotite and cordierite.
10W.O-10M.5 SX garnet and retrograde garnet -
chlorite with silica rims.
Pervasive moderate to strong Iteration consisting of trice garnet, 1C* cordierite, S-10X biotite (In fine
MINERALIZATION
Trace pyrite.
Trace pyrite.
Trace pyrite. '
REMARKS
Tuffaceous arenite 7
Clastic/reworked sediment component dominates with tuff c securing as minor conponont i
MOLE NUMBER: VL-057 DRILL MOLE RECORD LOGGED (YI G. GLENN PAGE t IB
HOLE NUMBER: WL-057MINNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROM TO
ROCK WE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
SEDIMENTS MIXED ALT SEDS* PICK LAKE SEDIMENTS
Upper contact (harp 8
1019.45-1019.85Well laminated distal wacke.
grained silceous matrix) Garnet increases to 5-7X between 1019. -1019.45
None - incipient biotite. Trace pyrite.
Bedding 8 ....................................Cm acale alternating beds of mixed felsic and
mafic aiateriaU
1019.85-1021.12Massive, altered siliceous sediment as above.Lower contact t ...,,....,.,.......,..........
1020.12-1020.45 GR DY
1021.12-1022.BWell laminated distal wacke.Alternating felsic and mafic material.
Bedding 8
1022.8-1023.75Massive to weakly layered, green - grey altered aediment/tuff exhibits weak to moderate (to locally strong) alteration.Bedding when present is defined by sausterltlzed felsic layers.Bedding fi .......................................
69
87
80
78
No to very minor cherty component hence clastic sediments.
1020.022X pyrite associated with 2cm wide
milky white quart! vein.
Hematite stained.
None - incipient biotite.
Weak pervasive 5-7X biotite locally (1026.1-1026.6)Biotite increases to JO-40* with trace
cord!trite, anthophyllite and < 5X chlorite.
None - trace.
1023.75TO
1039.1C
MIXED ALTERED FELSIC VOLCANI CLASTIC ANDTUFFACEOUS SEDIMENTS tCLR/SEDS*
This wit is defined by the appearance of a cherty component to the well laminated zones
Unit varies from massive grey-green to well laminated grey-white felsic layers alternating with hornblende-rich layers.
1023.75-1026.6Mixed altered intermediate tuff and CRT. Zone Is fine grained to very fine grained and grey to grey brown In colour. The cherty component exhibits layering 8 ....................................... 78
Variable.Ranges from moderate pervasive with
brickwork style overprint consisting of biotite and cordierite, minor staurolite and sillimanite.
Alteration varies tuffaceous zones exhibit S-10X biotite, up to 10* waxy green cordierite.Cherty tuff zones:
None to trace pyrite.
None.
HOLE NUMBER: WL-057 DRILL DOLE RECORD LOGGED (Y: G. GLENN f Mf: 1 9
HOLE NUMBER: Ut-057M1NNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1989
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
The nore tuffaceous tones are massive.
1026.6-1027.15 CRT/ITWell layered cherty Intermediate tuff.layering is mm - cm scale, sub-parallel to CA
Lower contact is possibly faulted - now healed 8.
1027.15-1028.45Well laminated CRT - as above.Bedding t . ......................................
1026.45-1028.95 MTDark preen, weakly layered, very fine grained
mafic tuff.Layering S .....................................Lower contact occupied by 4cm wide barren white
quart! vein S ........,..........................Small fault offsetting bedding running parallel
to CA.
1028.95-1033.4 Mixed CRT/1T/MT. tedding a .......
1011.4-1015.8 FTMassive to weakly layered grey felsic tuff.
41033.8-1034.8f *CR DV*
1035.4S-1035.88 GR DY
1034.8-1039.1well laminated CRT/sediments.Laminations li on HID scale.Unit exhibits a layered grey-black and white colour with pervasive light grey overprint and exhibits tp to SK m scale, euhedral, magnetite crystals.
65
78
80
5X biotite, < 3X cordierite.
Biotite and cordierite alteration developed In nore mafic layers.
None.
1028.35-1028.45Minor carbonate veining.
Alteration varies with the felsic to Intermediate units virtually unaltered but the mafic exhibiting weak-moderate biotite, cordierite, trace garnet alteration
Trace biotite as fine clots.
Hematite stained.
Hematite stained.
None - fresh.
None.
Trace - IX pyrite associated with carbonate veins.
Trace very fine grained disseminated pyrite.
None - trace pyrite.
Trace - U very fine grained disseminated pyrite.
Trace pyrite. Magnetite occurs disseminated throughout well banded units Indicating sedimentary component.
HOLE NUMB' DRILL HOLE RECORD LOGGED IT: C. CLENM PAGE t 20
HOLE NUMBED: Ut-057MINNOVA IHC.
DRILL HOLE RECORD DME: 19-0etober-1989
FROM TD
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
1016.6-1036.75 MDDark green black feldspar phyric mafic dyke.
MIXED ALTERED CHERTY TUFF xCLR*
{1039.1-1044.4 J .CRT.Very well laminated, alternating black and white layers.This CRT appears to be cleaner than the above
unit.Bedding S .......................................
1044.4-1059.12Weakly altered intermediate tuff and siliceous clotted volcaniclastic*.Intermediate tuff generally fine grained, medium
to dark grey, crass i ve to weakly layered.
Siliceous clotted volcaniclastic generally white with < IX mm scale mafic clots.
1057.75-1057.90 GR DY
{1057.90-1059.12f *GB DY*
1041.0-1041.25 MD Feldspar phyric.
41M2.6-1MJ.6l. *OB.
1044. 4-1059.12Typical CLR exhibiting minor local changes in
composition from intermediate to felsic siliceous matrix. Colour is grey white supporting mn scale mafic clots - locally up to 10X.
{1047.351; *FLT.
{1057.92-1059.121} *GB DY*Park green, medium to fine grained at contacts
mafic dyke.Lower contact B ...............................
Weak patchy biotite grading into locally strong brickwork alteration consisting of cordierite, biotite.
Weak pervaiive biotite. Locally in more Intermediate sections (1046.0- 1049.0) alteration Is 10X biotite and trace cordierite.
1055.0-1055.0Waak pervasive hematite staining of
siliceous clotted rhyolite.
10S4.5-1054.TPossible sillimanite K as very fine silky wisps.
Trace pyrite.
None.
Lack of disseminated magnetite indicates cleaner tuffaceous origin.Minor magnetite occurs on lamination surface.
1051.0Trace molybdenite in 5cm wide milky
white quartz vein.
NOLE NUMBER: UL-057 DRILL MOLE RECORD LOGGED (Y: G. GLENN FACE: 21
HOLE NUMBER: Wl-057M1NNOVA INC.
DRILL HOLE RECORD DATE: 19-0ctober-1v89
FROM TO
1066.2270
1072.00
ROW TYPE
GRANITE•GR.
E. O.K.
TEXTURE AND STRUCTURE
1059.12-1066.22 Patchy altered siliceous clotted votcanfclaitfc. Characterized by very tiliceous CLR windows in hazy contact with nediim grey, mast i ve biotite altered patches.
LocaKy, strong brick work style alteration overprints medium pervasive biotite.
White to pale pink massive to weakly foliated. Granite exhibiting both quart* and feldspar •m scale anhedral crystals. Fine to mediun grained, contains < 5X wispy
hornblende.
{1068.7-1071.31f rfO* Feldspar phyrlc.
1071.8-1072.3 MD
^075. *-1076. K \ *ti*
1089.9-1090.0 MD
End of Mole.
ANGLE TO CA
75
ALTERATION
Clotted rhyolite windows exhibit weak biotite alteration of mafic clots and trace - U sillimanite as white wftps sometimes within the mafic clots. The massive grey sediment exhibits incipient very fine grained biotite, trace cordierite and locally strong brickwork alteration consisting of cordierite in biotite matrix, ie: 1059.6-1059.75
Hematite staining.
MINERALIZATION
Trace very fine grained disseminated pyrite.
1064.95 Trace molybdenite In brickwork altered
sediment.
None.
REMARKS
HOLE NUMBER: UL-057 PRILL HOLE RECORD LOGGED IT l G. CLENN PAGE! 12
of ' Report rOOCUMbNI NONoj.he.Dcve.op.en,
pf
Ontario
Name! Address of Recorded Holder
[NOVA
SUITE 3970 - P. O. BOX 91, COMMERCE COURT WEST, TORONTO, ONTARIO MSL 1C7Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed
. 70for Performance of the following .vork, (Check one only)
Manual Work
rjshatl Sinking Drifting or other Lateral Work,
FJ Compressed Air, other Power driven or mechanical equip.
FJj Power Stripping
KjDiamond or other Core drilling BQ
FJl.and Survey
All the work was performed on Mining cialmls): TB 646428, 646431, 646432, 646433, 646434, 646439:
Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below) additional claims
WORK PERFORMED BY t ST. LAMBERT DRILLING CO. LTD., P. O. BOX 473,
DURING THE PERIOD: May lith, 1989 to
D. D. H. WL-56 - May lith - 22nd, 1989CRfbtTS /)v*/*-} S"?C /. 76
s f~.[.t o**~e*Cffb/f* tfff&t 0737. f j. —*-* A ,i f** t "70 no
C-Afb/T *4*rh *D. D. H. WL-57 - May
Total footage dril!1,758.52 Meters x
QNXAfl'O GEOLOGICAL22nd, rT(.. JvWQ ,t2Qwir-i
OFFICE:
DEC2V 198ed' 2 8 ff E' u ET V^
To be used for this Bnumrssion- ,~3
PgnHfil fir— fvitMrf submission ___ 8.
June 20th, 1989
Claim TB 646428 168 M.
646432 412 M.
646433 86.52 Mpth ,of- Hole ———— 666.52 M.
L98.9Claiii TB 646431 225 M
646433 221 M
^ 646434 483 M
646439 163 M
J^^-J /r, ^ 1,092 M7759 D lys/Feet94 Days/Eae eate of R8port
VALLEY FI ELD, QUEBECJ6S 4V7
*B
CC' 666.52 M.ro :.: -lir.: : : r: , ,ro ., ~; MCO ' "* Cj O
-1 rn i-~^5 *~ nl^ -?^092 - 0 M-
5 JL^w^*^^^^^ ^~*Total —1,758.52 M
•T
Recor64d Holder or Agent (Signature*
tfl^/t/s t ~ sCertification Verifying Report of Work
1 hereby certify that 1 have e penonal end Intimate knowledge of the facts set forth In the deport of Work annexed hereto, having porfomind the work or witnessed lame during and/or after its completion and the annexed report Is true.
Name and Postal Address of Penon Certifying
IAN R. MORRISON C/O MINNOVA Inc. 2606 VICTORIA AVENUE, EAST, THUNDER BAY,Certified by (Signature)
ONTARIO P7C 1E7Table of Information/Attachments Required by the Mining Recorder
Date Certified
7 V AJf^ S 7 7Type of Work
Manual Work
Shaft Sinking, Drifting or other Lateral Work
Compressed air, other power driven or mechanical equip.
Power Stripping
Diamond or other core drilling
Land Survey
Specific Information per type
Nil
Type of equipment
Type of equipment end amount expended. Note: Proof of actual cost must be submitted within 30 days of recording.
Signed core log Ihowing; footage, diameter of core, number end angles of holes.
Nemo and address of Ontario land surveyor.
Other Information (Common to 2 or more types)
Names and addresses of mon who performed manual work /operated equipment, together with dates and hours of employment.
Names and addresses of owner or operator together with dates when drilling/stripping done.
Nil
Attachments
Work Sketch: thoso are required to show the location and extent of work in relation to the nearest claim post.
Work Sketch (as above) in duplicate
Nil
W (85/12)
300
DICKISON LAKE G-3187 0 I5'
49 U 07 30 —
Green hedge
Lake
1103020 H0302I
wm l * -n , TB
1103005 i 1103006 l1103002 l "03003 | 1103004
NortMtne LaJte
103000 11081436 11081439 i IOW442
1103012 ; 103013 l H030IBJ.——-A--
l 646 4d748J6467^ j^ _ J
565714 f! Co At S1565664 .556216
___ | _"
814469(814474 |8I4 493 ' \,'8144~~~'"*""~'
1814487 181 - - -l- - - -t- - -
654420 654421 646583 l 64 6566j646 5.87 -|— —-"- ——^- " ^ - -J - -L^d^^ K646585 '646588 1646589814484 814485----- ———— L.---—— - r
654422 1646584 ion i l814453 .814454 - — — -l — -
Y n - .y—646436 |8464pO
~ ~ ~ ~ ~ ~ l646733 16^6736,646737 _ '6 ^b^4 t 645306 '645307 .645308
07J 38,6806 '6464381646435 ,64643! 64642 9 '646728- —Jl—————— J— — ~ J 7" — — - H- — — -(-^r-s.^ -j— — —— i- — — — -^ 646 4 |B '646-H9 '64 64 20
8 386805 ^646439*^64643^^6464321646428 [646414 j646 415^6^5416 [646417 j,. ,- , ,.J^ l " "l l ~" fTB3i46 674264
49 0 07 30
N-
CDl
OLLJ
OCO<to <O<DC LU Q. Q.
49 0 00 49 0 00'
870 30' 870 I5'
PAYS PLAT LAKE G-606
REFERENCES
LEGENDH l r, HW A-v ,", \" ' : -J
OTHf'u RfjAP'"
TRAILS
SURVLYEO LINES:TOWNSHIPS, BASF L 'NFS, ETC LOTS. Mirj'NG ( l A l VS PA H 1.1 i S \
UNSURVt""- ( ' INbS.LOT LINLbPARCEL BOUNDARYMINING CI AIMS ETt.
RAILWAY AND RtGHl Of WAY
UTILITY LINtS
NONPtRfcNNIAl STReAM
FLOODING UR l l OODING RIGHTS
SUBDIVISION uR ( I.IMPOM l Ir PL AN
RESERVAT IONS
ORIGINAL SHOHH iNfc
MAR^H OR MUSKEG
MINbS
TRAVtRSE- MONUMFN l
DISPOSITION OF CROWN LANDS
OF DOCUMENT SYMBOL
PATENT. SURFACE 8t MINING RIGHTS *
.SURFACE RIGHTS ON L Y . . . . ©
.MINING RIGHTS ONLY O
LEASE, SURFACE 8, MINING RIGHTS H
SURFACE RIGHTS ON L Y . H
" MINING RIGHTS ONLY . y
LICENCE OF OCCUPATION . .... ... .
ORDER IN COUNCIL ...... . .
RESERVATION ... . ... . ...
CANCELLED ...... .. ®
SAND fi. GRAVEL ..... . ... . (f)
NOTE; M INING R IGHTS IN PARCELS P ATENTED PRIOR TO MAV 6 .1913, VESTED I N ORIGINAL P ATENTEE B V THE PUBLIC LANDS A CT R SO 1970 CHAP 380, S F C 63. SU8SEC 1
SCALE 1 INCH = 40 CHAINS
O lOOO i?OOO 60 OO
WE T RI ',10OO
i l K M?000
(2 KM i
AREA
ROPE LAKEM.N.R. ADMINISTRATIVE DISTRICT
TERRACE BAYMINING DIVISION * G-***^-r*"
THUNDER BAYLAND T ITLES/ REGISTRY DIVISION
THUNDER BAY
Ministry ofNaturalResources
Land
Management
BranchOntario
Oate F EB. 17,1982 Number
G-609
42Efl3SW8ai03 21 ROPE LAKE 200