52F10SE00ie a.13967 TURTLEPOND LAKE 010
BOND GOLD CANADA INC.
REPORT ON A GEOLOGICAL MAPPING AND SAMPLING PROGRAM
WHITEWATER PROPERTY
TURTLEPOND LAKE AREA, ONTARIO
February, 1991 Toronto, Ontario
sv ft
SUMMARY
In July 1989, Bond Gold Canada (BGC) staked 88 claims north
of, and contiguous with, the originally optioned (ie. Johnson and
Glatz Option) Whitewater Property, thus increasing BGC's land
holdings in the Turtlepond area to 157 claims. The claims
acquisition was prompted by the encouraging results of the 1988
mapping and sampling program. BGC currently holds 67 (100% owned)
claims, which have been partially covered by the 1989 geological
mapping program.
The purpose of the 1989 exploration program was to trace the
northerly strike extension of narrow, auriferous quartz vein shear
zones outlined during the 1988 mapping program on the Whitewater
Property.
The mapping survey was not successful in extending the quartz
veined shear zones to the north.
However, airphoto lineament analysis has defined 4 major
structural trends on the Whitewater Property, 2 of which are known
to host gold mineralization. The intersection and along strike
extension of these structural trends offer very attractive targets
for significant gold mineralization.
Additional mapping, sampling and prospecting is recommended
to evaluate a number of these high priority structural targets.
2.1396? TURTLEPOND LAKE 010C
TABLE OF CONTENTS
Page No.
1.0 Introduction........................................... 1
1.1 Location and Access............................... 11.2 Property.......................................... 3
2.0 Previous Work.......................................... 5
3.0 Regional Geology....................................... 6
3.1 Property Geology.................................. 83.2 Petrography......................................12
4.0 Alteration............................................ 13
5.0 Mineralization........................................14
6.0 Regional Structural Geology........................... 15
6.1 Structural Geology............................... 17
7.0 Conclusions........................................... 26
8.0 Recommendations.......................................26
9.0 References............................................ 27
LIST OF TABLES
Page No.
Table 1 Land Status...................................... 3
LIST OF FIGURES
Figure 1 Location Map
Figure 2 Index Map
Figure 3 Regional Geology
Figure 4 Vesicular Pillow Structure
Figure 5 Riedel Shear Fracture Systems
Figure 6 Stereonet Plot
Figure 7 Development of R-Type Riedel shear fractures in a system of brittle-simple shear (after Tchalenko 1970)
Figure 8 Initial development and progressive deformation of tension veins (after Kerrich and Allison 1978)
Figure 9 Regional Compilation Map
Figure 10 Stereonet plot derived from Lineament Analysis Study
LIST OF APPENDICES
APPENDIX 1 Geology and Topography Maps:
Map 1 Extension of the Johnson GridMap 2 Northern ExtensionMap 3 Moose Bay Reconnaissance
1.0 INTRODUCTION
This report describes the results of the 1989 Exploration
Program carried out by Bond Gold Canada Inc. (BGC) on the
Whitewater Property.
The 1989 exploration program consisted of linecutting,
geological mapping, prospecting and stripping. The work was
performed during the period July 16th to August 29th, 1989. A
total of 33km of grid were mapped at a scale of 1:2,500.
A total of 50 samples were collected and submitted to Custom
Fire Assay Lab in Cochenour, Ontario and analyzed for gold.
1.1 Location and Access
The Whitewater Property is located within the Manitou-Wabigoon
Lakes portion of the Archean Superior Structural Province.
The claims are situated in the Kenora Mining District of
northwestern Ontario, approximately 25km southeast of Dryden, south
of the Wabigoon Lake Indian Reserve No. 27 and centred on the east
shore of Stanawan Bay of Dinorwic Lake (Figure 1).
Access to the property is afforded by float and/or ski
equipped fixed wing aircraft, or by boat from Dinorwic Landing,
PROPERTY LOCATION
Tram-Can*
REGIONAL LOCATJON MAP
WABIGOON LAKE
WHITEWATER OPTION
GLAT2 OPTION
20 Kilometres
Bond Gold Canada Inc.
WHITEWATER PROPERTYHwtrnm OWTAMO
LOCATION MAP Figure 1
which can be accessed via the Jack Fish Road south for 12km from
the Trans Canada Highway and then 10km along an old logging road
to the lake.
1.2 Property
The Whitewater property presently totals 1,082 ha comprising
67 unpatented mining claims.
The purpose of the current work was to extend the geological
survey to cover the newly acquired northern claims (ie. Northern
Extension) (Figure 2).
As of February 1, 1989 the Northern Extension claims were in
good standing. The status of the claims is summarized in
Table 1:
TABLE 1 LAND STATUS
Property No. of Claims
Northern 67 claimsExtension
Claim number
1092700-10927111092750-109277410805701080513-108057810805191080520-10805221080529-10805471092720-1092723
Expiry Dati
91-10-2791-10-2792-06-2192-06-2191-06-2192-06-2192-06-2193-10-27
NORTHERN EXTENSION(88 Claims)
Moose Bay Reconaissance (Map 3 )
DINORWIC LANDING
OHNSONOPTION
i -1(57 Claims)Extension of the Johnson Grid (Map 1)
280 0 500m
0.25 0.2S 0.8 mil*
BOND GOLD CANADA INC.WHITEWATER PROJECT
INDEX MAPFigure 2
2. PREVIOUS WORK
2.1 Minnehaha Gold Occurrence - Glatz Option
The first reported work on the property was the development
in 1905, of a 30m shaft and 7.6m crosscut on the Minnehaha gold
occurrence on the Glatz Option (Corkill 1907; 1909). A 7.6m pit
was sunk and some trenching was completed in 1908, at which time
operations ceased (Corkill 1909) . The property was reactivated
in 1910 and a 12.2m adit was established in 1911.
The property was staked in 1982 and optioned in 1983 to
Asamera Minerals Inc. Asamera Inc. carried out a ground magnetic
and electromagnetic survey, humus and lithogeochemical surveys and
geological mapping over the entire claim group.
The claims subsequently lapsed and the prospect was staked by
A. Glatz (a Dryden prospector) in late 1987. Glatz collected three
samples, one obtained from an outcrop near an old test pit returned
a value of 4.80g Au/t. Two grab samples from the dump pile in the
vicinity of a 30.5m deep shaft returned values of 2.74g Au/t and
2.06g Au/t respectively.
In 1987 the OGS examined the property and collected grab
samples from the dump pile at the aforementioned shaft. The
samples yielded values of 60ppb Au, 1350ppb Au and a value of 14ppb
6
Au from a pyritic wallrock sample. A grab sample from the wallrock
of the test pit returned 5,700ppb Au, while a sample from the
quartz vein material returned 490ppb Au.
3.0 REGIONAL GEOLOGY
The property is located in the Manitou-Wabigoon Lake belt of
the Wabigoon Subprovince of the Archean Superior Structural
Province. The Wabigoon Subprovince is bounded transitionally to
the north by the sediment-dominated English River Subprovince and
to the south, across the Quetico Fault, by the sediment-dominated
Quetico Subprovince (Figure 3).
The Wabigoon Subprovince is a major tectonostratigraphic
subdivision of the Superior Structural Province, which consists of
belts of metavolcanic rocks with lesser metasedimentary rocks that
are cut by granitic intrusions (Blackburn et al, 1985).
The mafic volcanic rocks in this subprovince consist of
massive basaltic and/or andesitic flows and subordinate pyroclastic
rocks.
The felsic volcanics generally consist of massive to well
banded lava flows with banded to massive tuff and tuff breccia.
Bands of clastic sediments, such as conglomerate, sandstone,
siltstone, argillite and greywacke are intimately associated with
FELSJCANO ROCKS
INTERMEDIATE INTRUSIVE
METAMORPHOSED MAFIC AND . _ UVTRAMARC INTRUSIVE ROCKS
^ -gg-t OASTCMEWSEDWENTS
MAFCMETAVOLCANICS
STMBOLS
5000
Bond Gold.Canada Inc. WHrTEWATER PROPERTY
REGIONAL GEOLOGY
Figure 3
8
the felsic volcanics in the region.
There are numerous mafic sills and dikes intruding both the
volcanic and sedimentary sequences. Most predate the main period
of folding (Goodwin, 1969), although some may be syntectonic.
The regional northeast-trending Manitou Straits Fault passes
approximately 1 km southeast of the Whitewater property. Numerous
north to north-northeast trending splays are associated with this
structure. These may represent the prime control on gold
mineralization in the area.
3.1 Property Geology
Geological surveys were conducted on the Northern Extension
portion of the Whitewater property between July 16 and August 29,
1989. The geological maps (see Maps 1, 2 and 3) are included in
Appendix 1.
The predominant rock types found during the mapping survey
include massive to pillowed intermediate and mafic metavolcanic
flows, and their fragraental equivalents.
The rocks are light to dark green and fine- to coarse-grained.
The coarser-grained flows are gabbroic to dioritic in texture. The
9
fine-grained volcanic flows are generally massive, showing some
weak foliation. The volcanic flows are commonly amygdaloidal , with
quartz, carbonate, chlorite and epidote filled amygdules.
Feldspar phenocrysts may also be present within the fine
grained volcanic, or amygdaloidal, flows. The phenocrysts range
in size from 1mm to 5cm.
The amygdules are generally spherical to oblate in plan view.
Deformation can be observed in cross section where the amygdules
have been stretched in the c-axis direction. The amygdules are
commonly weathered out, giving the rock a vesicular flow
appearance.
Pillowed flows are present on the property. They are
characterized by dark green pillow selvedges and light green inner
cores with an axis of elongation up to 0.5m.
Quartz, carbonate, chlorite and epidote amygdules are very
common within the pillowed flows. The configuration of the
amygdules is often the only indicator of the shape of the pillowed
flow. When local deformation and metamorphism has obscured the
diagnostic selvedge, the distribution of the amygdules remain to
suggest the pillow precursors (Figure 4).
The flow breccias identified on the property are monolithic.
10
*;**»• «** ' •
tPillowtopdirectior
A) Pillowed andesite showing abundant anygdules and veiicles towards the tops of the pillows.
--1*-*;./.*.?...( , • *••»,«.
J
3) If the pillow selvages are obscured, a pod-like pattern of amygdules remains, suggesting the precursor flow was pillowed.
Figure 4
11The fragments are angular to sub-rounded with no apparent sorting
or bedding. Although the fragments are compositionally similar,
they may differ in colour, grain size and texture. The brecciated
flows commonly grade into massive units.
Carbonatization associated with the volcanic flows is evident
as small carbonate stringers and amygdules uniformly distributed
throughout the rock. Carbonate (and carbonate with chlorite) is
also present within sheared areas of the metavolcanics. Satterly
(1941) suggests that the carbonate-chlorite schists are derived
from intermediate to basic lavas, and that the presence of
carbonate alteration has little significance as a pathfinder to
gold mineralization. Disseminated sulphide mineralization may be
present without significant gold values.
The intrusive rocks on the property are medium to coarse
grained, dioritic to gabbroic in composition. As no contacts were
observed, clear intrusive relationships were not apparent.
Therefore, some of the outcrops defined as intrusive may also be
a product of slow cooling or the recrystallization from
metamorphism.
Some outcrops are so altered and sheared (with an alteration
assemblage consisting of carbonate, quartz and chlorite) that the
protolith could not be discerned.
12
3.2 Petrography
A petrographic study was carried out on 16 representative rock
samples from the Whitewater property (including the North
Extension). The study was undertaken to determine the metamorphic
grade, the products of alteration, and to identify the rock. The
following was concluded from the study:
1. The rock assemblage is more felsic in composition than
mafic. Observations and identification focused on the
origin of the quartz in the samples. A portion of the
quartz seemed to be clearly introduced during alteration,
as it occurs as fine veinlets and/or stringers. In
contrast, there is an abundance of very fine-grained
quartz found in the more siliceous samples that may be
primary, suggesting an igneous origin. The felsic
constituents present in the rock suggest they are
intermediate (ie. andesite to quartz andesite) in
composition.
2. Products of alteration identified by the petrographic
study were similar in their mineral assemblage for each
of the intermediate, mafic and intrusive rock samples.
The alteration assemblage was dominated by epidote,
chlorite, bleaching and uralitization (araphibolitization)
13
of pyroxene, and minor silicification. The metamorphic
grade of this assemblage is essentially greenschist
facies.
3. Some of the samples identified as mafic flow containing
chlorite knots appear to have a plutonic protolith (ie.
gabbro). The chlorite knots are the product of the
alteration of pyroxene into amphibole and chlorite.
4. A number of samples previously identified as flow breccia
appear to be massive to foliated, intermediate to mafic
volcanic flows. The fragments described in hand specimen
are identified as epidote aggregates named epidosite.
Epidosite consists essentially of massive aggregates of
very fine, prismatic epidote grains, totally replacing
the mineralogy, including feldspar microlites. The
identification of the rock was based on the lack of sharp
contacts between fragments and groundmass, a
characteristic expected in a breccia. The composition
and texture of the groundmass and aggregates are similar,
the only difference being the degree of alteration.
4.0 ALTERATION
The alteration encountered on the property is for the most
part weakly developed. Alteration may be classified by its
14
association with: a) mineralized shear zones and b) country rock.
Sericitization and iron carbonatization (ie. ankerite) are the
common types of alteration associated with shearing containing
sulphide mineralized quartz and quartz-carbonate veins.
Chloritization and carbonatization are the principal types of
alteration found associated with the host country rocks.
Replacement of amphibole by chlorite is observed in the coarse
grained volcanic rocks, with the ghost outlines of amphibole
crystals preserved. Weak carbonatization is present, characterized
by hair-line fractures filled with calcite.
5.0 MINERALIZATION
No significant gold values were found during the 1989
Exploration Program on the Whitewater property.
The mineralized zones are very similar in character. They are
intensely altered, sericitized, pyritized intermediate to mafic
flows cut by anastomosing quartz stringers. The zones have a
maximum width of 1 metre.
The mineralized zone found on the Johnson Option occurs within
an area of structural complexity and alteration that extends north
and northeast throughout the Whitewater-Kaminnassin-Turtlepond
15
Lakes area (C.E. Blackburn 1987). The shear zones are associated
with the Manitou Straits Fault, a regional fault structure that
controls most of the known gold mineralization in the area.
Petrography suggests the host rock for the gold bearing quartz
veins found on the Johnson Option is different in composition from
the host rock in the Upper Manitou Lakes area. The host rock
assemblage associated with gold mineralization on the Whitewater
Property consists of intermediate to mafic volcanic flow sequences.
In the Upper Manitou Lakes area, auriferous quartz veins occur
within, or in close proximity to, felsic to intermediate
pyroclastic rock and subvolcanic porphyry intrusives.
Despite differences in the lithological composition between
the two environments, gold is associated with quartz veins and
appears in both environments to be structurally controlled.
6.0 REGIONAL STRUCTURAL GEOLOGY
The Whitewater Property is located approximately 2km west of
the Manitou Straits Fault (Figure 9), which controls or is
associated with gold mineralization in the Upper Manitou Lake area
(Figure 3).
A subsidiary of the Manitou Straits Faults has been identified
on the Whitewater Property (K. Leonard, 1988) and named the Western
16
Branch of the Manitou Straits Fault (Figure 9).
The Lower Manitou Lake area is intruded by two genetically
distinct fault types. The first type is associated with intense
shearing, producing broad schistose, phyllitic and mylonitic bands
along which fault movement has occurred (i.e. the Manitou Straits
Fault). The second fault type is more brittle in nature and lacks
well developed schist zones. An example is the BQV shear zone on
the Johnson Option, which is a conjugate structure to the Manitou
Straits Fault.
Jens Touborg, consultant to B6C, has identified four regional
fracture sets (Figure 10). The dominant fracture set trends 067°,
the second and third set of lineaments form a conjugate set
relative to the Manitou Straits Fault oriented at 022° and 119"
respectively and a fourth set trending 152°.
Touborg's regional lineament interpretation concurs with the
structural information obtained at the property scale from the 1989
Exploration Program (Figure 3). In the Upper Manitou Lake area
(ie. Gold Rock Camp), gold mineralization is spatially associated
with the Manitou Straits Fault, which corresponds to the dominant
ENE trend delineated from the lineament map.
Conversely, gold mineralization on the Johnson Option has been
found along a NNE trending shear zone (ie. the BQV shear zone).
17
This orientation is conjugate to the Manitou Straits Fault.
The fourth fracture orientation is associated with late stage
dyke emplacement along a zone of dilatancy. The gold potential
along this structure is not known at this time.
6.1 Structural Geology
Structural mapping suggests four fracture systems on the
Whitewater Property. These trends are summarized on the stereonet
plot (Figure 6), and concur with the interpreted regional airphoto
lineament and airborne geophysical data compiled on the Whitewater
Property.
Chris Ludwig, BGC's Denver based geophysicist, reviewed the
airborne VLF-EM and magnetic data and has interpreted a subtle
N-S grain and several possible cross structures oriented at roughly
045°, 090° and 315°.
Lineament analysis indicates four predominant fabrics oriented
as follows:.
1) a northeast-southwest (045° - 225°) trend which
corresponds to the Manitou Straits Fault (C.E. Blackburn,
1979; OGS Map 2443 and Report No. 189).
18
2) a north-northeast south-southwest (010° - 190") trend
which corresponds to tension fractures. This structural
trend is associated with gold mineralization found on the
Johnson Option.
3) an east-west (080° - 260°) trend which corresponds to
tension fracturing.
4) a northwest-southeast (315°-135°) trend which corresponds
to dilatancy fractures associated with late stage dike
intrusion.
The fabrics plotted on the stereonet clearly illustrate an
example of a strain ellipsoid or an R-Type Riedel shear fabric
system (Figure 5).
In brittle - ductile shears, the brittle response of the rock
results in the formation of continuous fractures and vein
development. The vein may be parallel to the shear fabric or
oblique (tension fracture) to the shear fabric (Figure 5).
19
\
\\
Riedel sheer fractures system.
Figure 5
20
Schmidt net.
FIGURE 6 189 poles plotted from the Glatz Option Property
Contour Intervals 3-67-9 10-14 15-24 25 to >
21
The structures are generally associated with alteration
products such as silicification, pyritization and sericitization.
This alteration assemblage was found during the 1988 mapping
program along the auriferous BQV shear zone on the Johnson Option.
The gold mineralization on the Johnson Option is associated
with the NNE-SSW structural trend which represents tension
fracturing associated with the Manitou Straits Fault.
No mineralization has been found associated with the E-W
structural trend, however the potential of this structure could be
as significant as the NNE-SSW BQV structure.
22
s
Figure 7 Development of R-Type Riedel shear fractures
in a system of brittle-simple shear (after Tchalenko
1970).
The data shown on Figure 7 indicates that R-type Riedel shears
are the most dilatant and therefore are attractive targets for gold
mineralization.
Directional axis D represents the Manitou Straits fault, axes
P and R represent oblique shearing tension fractures. Axis R
represents dilatancy fractures which corresponds to the latest
structural event. This fabric is for the most part parallel to
maximum compression, and therefore, perpendicular to the Manitou
Straits Fault system.
23
4
\ /
MJW3M»
/ \
e o
sM
(Fig. 8). Initial development and progressive
deformation of tension veins (after Kerrich and Allison
1978).
Figure 8 above shows development of tension fractures with
increasing deformation. The sigmoidal tension veins correlate with
the P and R fabric of the R-Type Riedel shears.
V7"•\/
l WABIGOON LAKE 7 I.R. No. 2 7 /
WABIQOON LAKp I.R. No.27
WHITEWATERPROPERTYJOHNSON
OPTION
GLATZ OPTION
BOND GOLD CANADA INC.WHITEWATER PROPERTY
NORTHWESTERN ONTARIO
REGIONAL COMPILATION MAP_____Figure 9_______««__«___
25
N030
W
N067
N119
Schmidt net.N1S2
FIGURE 10 461 pole derived from a Jens Touborg lineament map
Contour Intervals 5-20 21-25 26-45 46-70 71 to >
CERTIFICATE OF QUALIFICATION
I, Jean-Pierre Londero of 50 Dundonald Street, Toronto, Ontario, do hereby certify that:
1. I am a graduate of the University of Quebec in Montreal, Quebec, and hold a Bachelor of Science degree in Geology, 1984.
2. I am a geologist employed by Bond Gold Canada Inc. and have practised my profession continuously since graduation.
3. I personally supervised the fieldwork described herein.
^JeahrPierre iTondero
( ,-
26
7.0 CONCLUSIONS
The 1989 mapping, sampling and stripping program carried out
on the Whitewater Northern Extension grid, the extension of the
Johnson grid, and the Moose Bay reconnaissance areas, did not
outline any significant gold mineralization.
A total of 50 samples were collected and the best gold value
returned 1.71g Au/t.
8.0 RECOMMENDATIONS
Additional mapping, prospecting and stripping is warranted to
screen additional high priority ground geophysical anomalies and
favourable structural intersections and trends indicated by
lineament analysis in order to determine drill targets.
Submitted by:
J.P. Londero S. Bohan
9.0 REFERENCES
27
S.J. Bate, 1988 Report on Magnetic meter, FVLF-Electromagnetic
and Horizontal Loop Electromagnetic Surveys on
the Whitewater Lake Property - Wabigoon Area,
Northwestern Ontario. MPH Consulting Limited.
J. Satterly, 1941 Geology of the Dryden - Wabigoon Area; Ontario
Department of Mines, Annual Report for 1941.
Volume L. , Part II. Accompanied by Map. 50ae,
scale 1:63, 360 or 1 inch to 1 mile.
Blackburn C.E. et al, 1987
Kenora Resident Geologist's Area 1987. Ontario
Ministry of Northern Development and Mines,
Kenora.
J.M. Moore, R.L. Norton, 1982
Short Course on Physical Volcanology Applied
to Metavolcanic Rocks. Department of Geology
Carlton University.
28
Delisle P.O., Bohan S., 1988.
Geological Report on Whitewater Lake Property.
District of Dryden, Northwestern Ontario. Bond
Gold Canada Inc.
C.E. calvine et al, 1988
Geology of the Upper Manitou Lake Area
District of Kenora. Ontario Geological Survey
Report 189.
Bruce E. Hobbs et al, 1976
An Outline of Structural Geology
Ed. John Wiley & Sons, 571 pages.
Mmistry otNorthtfn Developmentand Mines
Report©! WorkW 91IQ
52F10SE0«I« 2 . 1 3967 TURTLEPONO LAKE 300
Mining Act (Geophytteal, Geological and Qeochemleal Surveys) ^^^^^iiS^oi^^
Mining Claims Traversed (List in numericaltpMfaf Provision*
rat «nt survey:
Ens* 40 days. (This memoes ttnecimtng)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse side and enter totaxs) here
Airborne Credits .
Note: Special provisions credits do not apply to Airborne Surveys.
Geophysical
• Magnetometer
•Other
Geological
Geochemical
Geophysical
• Electromagnetic
• Magnetometer
• Other
Geological
GeochsmicsJ
Electromagnetic
Magnetometer
Other
°sr
3D
Days per Claim
Days per Claim
——
Total miles flown over claim(s).Date • , R»e»ded Holder or Aoant (Signature)
Mining ClaimPrefix Number
Mining CWmPreta NumMr
JflAR-
MWnoCWmNumber
BEGEMS*f199ll
Certification Verifying Report of Work
MININGTotal number of mining claims covered by this report of work.
7
1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in this Report of Work, after its completion and annexed report is true.
having performed the work or witnessed same during and/or
Name and Address of Person Certifying
i Telephone No.
For Office Use Only
Total Days i Date Recorded Cr. Recorded |
'SEE REVISED WORK STATEMENT
Recervea Stamp
362169(0*1
(2)Ontario
Northern Development <ind Mines
Report of WorkAct (Geophysical, Geological and Qeochemical Surveys)
tnetruettona• Please type or pom.• Mafaf» Section 77, l» Mining Act tor anaaameot work itojwtmwa
and maximum eredtt* allowed per eurvey type.• it numMr of mining claim* traversed exceede apace on trw» form.
attach • M. . . • •• Technical Reports and mtpt * dupftoaia ahouM be. eubmrrted to
Mining Land* Section, Mineral Development and lands iraneh:
ana Addreta of Author (of Oeo-
Credits Requested per Each Claim in Columns at right Mining Claims Traversed iSpecial Provtatona
ft* first survey:
Enter 40 days. (This include* line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse tide ana enter totaKs) here
Airborne Credit*
Note: Special provisions credits do not apply to Airborne Surveys.
.Oeoprtydcal
• Bectromagnetto
• Magnetometer
• Other •
Geological
Qeochemical
Geophysical
• Electromagnetic
• Magnetometer
•Other
Geological
Geochemical
Electromagnetic
Magnetometer
Other
Days per Claim
*tr>
Days per Claim
Days per Claim
Total miles flown over claim(s). IDate / Recorded Holder or AgenUSlgnature)&*• *c/v 1%~/^ a^^
Mining ClaimNumber
Jst in numerical seguepoe)Mmmo Claim
Preix Nurnbar
RECEIVE ;D
MARd>f199
Number
Certification Verifying Report of Work
mining claims covered by this report of work.
I hereoy certify that I have a personal ana intimate knowledge of the facts set fonh in this Report of Work, having performed the work or witnessed tame during and/or after its completion ana annexed report is true.Name and Address of Person Certifying
For Office Use Only
Total Days i Dale R Cr. Recorded
I Date Approved as Recorded i Provincial Manager. Mining ftnds
I "SEE REVISEIJ) WORK STATEMENT
i(
36? 189/061
Toohnteai Att«s*mont WorkCrwfltt 12,13967
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Alrtaorn* Q
fround
Q Ortdlt* IMV« botn r«duo*d DNOUM of portM oovtragt of cMim.
Q CraoltihtMbotnraduotdbMauMofoomKtlom to work d«t»« and flgun* of •ppltcont.
K.1092760 1092764-765 1092769-770 1092704-705 1080518-519 1080529-531 incl. 1080534-536 incl. 1080538 1080546
Special eradlt* undor toctton 77 (18) for tha following mining daiim
No cr»dH» Km been rilowtd for the fotlowUm mining dalrmnot tuffletootiy eov*r*d by th* MIVIV Q ImuffteiMt toehnleot dtu fllod
K.1080520, 1080537, 1080539, 1080547.
Th* Mining Record* m»y r*duo* th* *OOM enxlltt If HMMMTV In order that th* total number of appr•xeead the maximum aflowtd w foltovn: OMphydcet • W; Oaologooal • 40; Oaochamlcel • 40; faction 77(19) • W.
t day* recorded on each claim doe* not
arioMinistry ofNorthern Developmentand Mines
Ministeredu Developpement du Nord etdes Mines
Mining Lands Section159 Cedar Street, 4th FloorSudbury, OntarioP3E 6A5Telephone: Fax:
Your File: Our File:
(705) 670-7264 (705) 670-7262
W. 9110. 025, 26 2. 13967
May 27, 1991
Mining RecorderMinistry of Northern Developmentand Mines808 Robertson StreetP. 0. Box 5200Kenora, OntarioP9N 3X9
Dear Sir /Madam:
RE: Notice of Intent dated April 26, 19-91 for Geological Survey on mining claims K. 1092754 et al. in the Turtlepond Area.
The assessment work credits, as listed with the above-mentioned Notice of Intent have been approved as of the above date.
Please inform the recorded holder of these mining claims and so indicate on your records.
Yours sincerely,
7Ron.Ion. C. Gashinski,Provincial Manager, Mining LandsMines & Minerals Division
LJ/jl Enclosures:
cc: Bond Gold Canada Inc. Toronto, Ontario
Assessment Files Office Toronto, Ontario
Resident Geologist Kenora, Ontario
D
STANAWAN
1092701 1092704
NORTHERN EXTENSION (88 Claims)
Moose Bay Reconaissance (Map 4)
Extension of t he Johnson G rid ( Map 2)
Glatz Grid (Map 1)
025 0 026 O.Smil*
BOND GOLD CANADA INC. WHITEWATER PROJECT
INDEX MAP
'4Yi,
a
Legend
LITHOLOQY
Gabbro
Intrusive felsic dyke
Metamorphosed intermediate to maficvolcanic flowIp - plagioclase - phyric flowIpi - pillowedIc - chlorite knotsIq - quartz knots1M - massive flowIb - breccia flow
SYMBOLS
Strike and dip of SIStrike and dip of S2Mineral lineationStrike and dip of quartz vein/veinlet: barrenOutcrop; large, smallShear zoneGeological contact; observedQuartz vein trendTrenchShaftAdit
Claim post; located, assumedCliff face; height in metresRidge; height in metresPathStream; intermittentSwampBeaver lodge
50 0
Scale 1:250050 IOO (50 20O
metres
52Fi85Eeeie 2 .13967 TURTLEPOND LAKE S00
BOND GOLD CANADA INC.
WHITEWATER PROJECTNORTHWESTERN ONTARIO
MOOSE BAYRECONAISSANCE
GEOLOGICAL MAPGEOLOGIST:
SCALE' 1-2,500
DRAWN BY:J. Meek & A ssoc. Ltd.
REVISED:
DATE:November 1989
DRAWING I:
LITHOLOQY
GabbroDINOROWICIntrusive felsic dyke
Metamorphosed intermediate to maficvolcanic flowIp - plagioclase - phyric flowIpi - pillowedIc - chlorite knotsIq - quartz knots1M - massive flowIb - breccia flow
LAKE
SYMBOLS
Strike and dip of SIStrike and dip of S2Mineral lineationStrike and dip of quartz vein/veinlet: barrenOutcrop; large, smallShear zoneGeological contact; observedQuartz vein trendTrenchShaftAditClaim post; located, assumedCliff face; he.ight 1n metresRidge; height in metresPathStream; intermittentSwampBeaver lodge
1 fv*»tcJ«s A(f*dL wi^ +fid»tt. + cj.utt.'fjL.)
Scale 1:250050 100
IT 13967BOND GOLD CANADA INC.
WHITEWATER PROJECTNORTHWESTERN ONTARIO
NORTHERN EXTENSION
GEOLOGICAL MAPDRAWN BY:
J. Meek & Assoc. Ltd5ZFI8SE0B16 2.13967 TURTLEPOND LAKE
O -. • '"• • " •" •-'.'•>, : •-• • ;v ""•' ' ^.'S "•'4-V)
KAMINNASIN
LAKE
Scale 1:250050 IOO
f'.'l 8967BOND GOLD CANADA INC.
WHITEWATER PROJECTNORTHWESTERN ONTARIO
EXTENSION OF THE JOHNSON GRID
GEOLOGICAL MAPGEOLOGIST:
SCALE' h 2,500
JDATE? J. Hetlc & Asioc. Ltd. I Kovtmbar 1969
[DRAWING ir ~
STAN AW AY
EXTNSION (0S ClaifM
.: -. . - -v- • .. ..6. U
Moose Bay Reconaltsance(Map 4 )
j E xtension of t he Johnson G rid (Map 2)
Glatz Grid (Map 1)\i *^ •' ^ ' - * - QtATZ
PTION
BOND GOLD CANADA INC. WHITEWATER PROJECT
INDEX MAP S£F18SEeei« 2.13967 TURTLEPOND LAKE
LITHOLOGY
GabbroL 28-hOON
Intrusive felsic dyke
Metamorphosed intermediate to mafic volcanic flowp - plagioclase - phyric flowpi - pillowed
Ic - chlorite knots Iq - quartz knots 1M - massive flow Ib - breccia flow
SYMBOLS
Strike and dip of SIStrike and dip of S2Mineral lineationStrike and dip of quartz vein/veinlet: barren
Outcrop; large, small
Shear zoneGeological contact; observedQuartz vein trendTrenchShaftAditClaim post; located, assumedCliff face; height in metresRidge; height in metresPathStream; intermittent
SwampBeaver lodge
STANAWA N
NORTHERN EXTENSION (88 Claims)
Moose Bay Reconaissance (Map 4)
OHNSO OPTION
CUiiru)Extension of th* Johnson Grid (Map 2)
Olatz Grid (Map 1)GLATZ OPTION
BOND GOLD CANADA INC. WHITEWATER PROJECT
INDEX MAP52F19SEW1* 2.13967 TURTLEPOND LAKE