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Appendix A Appendix B Appendix C Appendix D Appendix E
Certificate of QualificationsList of ExpendituresDiamond Drill Log K91-1Assay CertificatesWhole Rock Analysis Certificates
List of Plans and Sections
Map l - Surface Plan Showing Drill Hole and Stripping Locations
Map 2 - Drill Hole Section K91-1
SOMfllRY
This report on the Katrine Township property has been prepared by S.J. Carmichael, B.Se., FGAC at the request of Lasse Raitanen, 63 A-2nd Street, Kirkland Lake, Ontario, the registered owner of the claim group. It is intended to complete the OPAP reporting obligations, of which Mr. Raitanen has applied for, and been accepted for a total sum of $10,000.00 (ten thousand dollars). Mr. Raitanen's OPAP grant number is OP91-062. The grant was approved on June 29, 1991.This report will also be submitted to the Ministry of Northern Development and Mines for assessment credits.The property comprises twenty-seven contiguous staked claims with a total area of 1,080 acres. The claims are located in the north- central portion of Katrine Township, District of Timiskaming, Larder Lake Mining Division, approximately seventeen miles northeast of Kirkland Lake.The claims have been worked in the past by Kennco in 1969 (Au, Cu) and by Lac in 1979 (Au). Both companies completed limited diamond drilling and have neither proved nor disproved the possibility of an economic gold or base metal deposit. Mr. Raitanen staked the claims in 1990 and proceeded to evaluate the claims by geophysics and diamond drilling. One hole, drilled under this years OPAP grant indicates the properties possibilities lie in copper mineralization associated with the Little Misema Fault. Drill hole K91-1 intersected a 7.5' section of mineralized core which graded 0.25* copper.Total expenditures for 1991 were $13,064.14 and included the drilling of one hole (K91-1, 399.0') and minor stripping. Additional diamond drilling along strike to the west is highly recommended to further test this horizon. The cost of this program, to include two 400' drill holes is estimated at $10.000.00.
-1-
Raport on the Katrine Township Property
Larder Lake Mining Division
For
Lasse Raitanen
Introduction
This report on Lasse Raitanen's Katrine Township mining exploration
property has been prepared by S. J. Carmichael Geological
Consultants at the request of Mr. Raitanen. It is a summary of work
completed during the 1991 season via an OPAP grant and is intended
to fulfil both OPAP and assessment obligations. An appropriate
program and budget has been included for additional work.
Information on the property is derived from the records of the
Ministry of Northern Development and Mines and publications by the
Ontario Geological Survey. The author of this report visited the
property several times during the 1991 season and both mapped the
stripped area and logged the drill hole. All work was performed
between May and August, 1991.
Property Location, Access and Facilities
The Raitanen claim group is located in the north central portion of
Katrine Township (NTS 32 D/4), District of Timiskaming and within
the Larder Lake Mining Division, approximately 17 miles northeast
of Kirkland Lake. Access to tjie property is via the McVittie-
Pontiac road which branches from the Larder Lake Station road. A
trail suitable for tucks and ATV leads west to the claims from the
Figure
l Property Location Plan
-2-
McVittie-Pontiac road 1.5 miles south of the Katrine/Ben Nevis
Township border.
The claim group is bisected by the Little Miseraa River providing a
water source for diamond drilling and stripping operations.
Facilities capable of supporting a mining operation on the property
are not present. Custom milling facilities are available in
Virginiatown, 10 miles to the southeast.
Topography
The topography is quite rugged; the calc-alkaline volcanic ridges
being more resistant to glacial erosion than normal Abitibi
terrain. Intervening valleys, such as that of the Little Misema
River, may be due to Archean faulting and are worthy of attention
during an exploration program. The north section of the property
becomes increasingly rugged as on approaches the Workman Hills.
Land Tormro
The Katrine property comprises 27 staked contiguous unsurveyed
mining claims with a total area of approximately 1,080 acres. The
claim numbers, recorded dates and applied assessment work are
requires 1240.00 by 11/00/02requires 1240.00 by 11/00/82requbw 1240.00 by 11/08/92require* 1240.00 by 11/08/92requires (240.00 by 11/08/82requires (240.00 by 11/0082requim (240.00 by 11/0802requires (240.00 by 11/0802requbw (240.00 by 11/0002requires (240.00 by 11/0802requires (134.00 by 11/0803requires (240.00 by 11/0802requires (240.00 by 11/0802
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L-1015165 11/08/87 1760.00 requires S240.00 by 11/08*92L-1015166 11/0007 1760.00 requires *240.00 by 11/00/92L-1015168 12/16/87 2200.00 roquns (200.00 by 12/16/93L-1015170 12/16/B7 2398.00 roquiBS S2.00 by 12/16/93L-1046600 07/14*8 1760.00 roqutes S240.00 by 07/14/93L-1046601 07/14/B8 1760.00 requires S240.00 by 07/14/93L-1046602 07/14*8 2266.00 requires S134.00 by 07/14/94L-1046603 07/14*8 2266.00 requires S134.00 by 07/14/94L-1046604 07/14/88 2200.00 requires S200.00 by 07/14/94L-1046605 07/14*8 1760.00 requires S240.00 by 07/14/93L-1046608 07/14*8 2266.00 requires S134.00 by 07/14/94L-1046507 06/27*8 2486.00 requires S314.00 by 06/27/95L-1046598 06/27*8 1760.00 requires S240.00 by 06/27/93L-1046599 0607*8 1760.00 requires S240.00 by 06/27/93
All claims are in good standing at this time. Assessment credits
will have to be applied by September, 1992.
Property History
Reconnaissance mapping of the area was completed by C.w. Knight of
the O.D.M. in 1920 at a scale of l 1^! mile. This was later revised
in 1928 by T.L. Gledhill. In 1964, a geological map and report was
published by W.A. Hogg of the O.D.M. and covered both Katrine and
Arnold Townships.
The earliest documented work on the claims was by prospector Dave
Lowe in the mid 1940's. Mr. lowe uncovered a sulfide showing within
tuffaceous agglomerate on the south bank of the Little Misema River
on present claim L-1015168. Lowe optioned the ground to Kennco
Explorations in 1969 which completed a horizontal loop survey.
Kennco completed two short pack-sack holes over the showing in
June, 1969 and reported low values in gold and copper. Kennco
dropped the option and allowed the claims to lapse.
In 1979, Long Lac Minerals staked a group of 106 claims in Katrine
and Arnold Townships and covered selected locations (covering
showings) with control grids. One of the areas covered is in the
south-central portion of the Raitanen group. Long Lac Minerals
-4-
completed geological mapping, magnetometer and VLF-EM surveys. Four
diamond drill holes followed in 1980 totalling 1,268.0 ft. No
significant assays were reported, however problems with caving
indicates that the holes may not have intersected the Little Misema
River Fault. No further work was completed and the claims were
allowed to lapse.
The property was then staked by Mr. Raitanen between 1987 and 1988.
Airborne magnetometer and HEM surveys were completed. These were
followed by a ground Max Min II survey and reconnaissance whole-
rock sample program.
Regional Geology
The Raitanen claims are underlain by Archean meta-volcanic and
sediments of the Misema River Subgroup of the Blake River Group.
This subgroup is slightly older than the Noranda Subgroup to the
east and contain lesser calc-alkalic felsic volcanics and more of
the intermediate variety. The whole-rock analysis by Raitanen show
a mixture of both calc-alkalic and tholeiitic indicating the claims
lie very close to the Kinojevis-Blake River Groups contact.
G.A. Hogg (1964) reports that the volcanics in Katrine Township
have been folded to a sequence of broad synclines and anticlines.
One major structure, the Misema Lake - Mist Lake Fault trends east
northeast through both Katrine and Arnold Townships. Hogg also
reports that the structure may be host to gold and/or base metal
mineralization.#
Property Geology
Mapping by Long Lac Minerals in 1980 shows that part of the
-5-
Raitanen ground is underlain by intermediate andesitic flows,
fragmental tuffs and agglomerates with minor interflow cherts and
immature sediments. Geochemical studies by Raitanen essentially
supports the Lac mapping and indicates that more felsic sequences
including dacites and rhyolites of both calc-alkaline and
tholeiitic affinities are present.
As stated previously, the Misema Lake - Mist Lake Fault bisects the
claim group and Lowe Showing appears to be controlled by this
structure. Drilling by both Kennco and Lac did not intersect
significant mineralization associated with this structure, however
the 1991 work by Raitanen indicated that neither Kennco or Lac
drilled their holes deep enough to intersect the structure.
1990 EXPLORATION PROGRAM
Summary
The 1990 exploration program including the testing of the Misema
Lake - Mist Lake Fault with one drill hole and the stripping of a
weak Max Min II anomaly.
A) Diamond Drilling
One hole totalling 399.0 ft. was drilled to test the Misema Lake -
Mist Lake Fault, interpreted to lie under or close to the Little
Misema River. A weak VLF-EM anomaly located by Lac Minerals was
also along section. The hole was located at 3+87 E, 6+28 N and
drilled grid south. Although the hole may have been drilled down
dip, it was calculated that the fault would be better tested
drilling this direction, knowing the difficulties Lac Minerals
encountered during their drilling.
-6-
The Misema Lake - Mist Lake Fault was intersected between 283.0'
and 342.0' and consisted of highly fractured and quartz *- calcite
stringers and veins. Two zones of clay gouge were cored indicating
that the fault is more of an alteration zone rather than one
individual fault. The fault zone appears to mark a contact between
calc-alkaline andesite and a darker coloured calc-alkaline basalt.
The entire section was mineralized with trace to l* chalcopyrite.
A 7.5 ft. section from 312.0-319.5' was mineralized with l-2%
pyrite and minor bornite associated with quartz stringers and
assayed Q.25% Cu. Unfortunately, the section was highly broken and
only 50% core recovery was obtained. A 3.0 ft. section further down
hole/ within the alteration/fault zone assayed Q.1% Cu. Gold assays
were nil throughout.
B) Stripping Program
A small area measuring approximately 60m x 10m was stripped and
washed over a weak Max Min II anomaly located at 8+20 E, 2+70 S.
No mineralization was found and a sample of a rusty gossan-like
material assayed nil gold and base metals. One sample was taken for
whole rock analysis and is plotted on the Jenson Cation Plot. It
lies within the calc-alkaline andesite field. The cause of the weak
anomaly appears to be a short cable effect.
The one intersection in drill hole k91-l of Q.25% Cu over 7.5 ft.
is considered interesting and ,worthy of at least two follow-up
holes. Either two holes to the west to intersect the Misema Lake -
Mist Lake Fault with coincidental VLF-EM anomalies or one undercut
-7-
of K91-1 and one hole to the west are recommended. Mineralization
appears to hosted within a broad altered shear/fault zone with
associated disseminated chalcopyrite mineralization and thus
horizontal loop surveying will probably not locate mineralization.
Further geophysics such I.P. or the Geoprobe system are not
required at this time.
The total cost of drilling two 400 ft. holes is estimated at
Respectful
Stewart FGAC
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File Nau E:\EEOCHEH\KATSOU.ROC11-1B-1991 12:02:18Saaple 7174 191-1-7201 k91-l-7217Northing 2+80 N Str DON K9M K91-1Easting L 9*00 E 9.0 ft. 398.0 ft.Syibol 12 l 6Sya Colour 12 l 2Rock Type Calc-Andes Calc-Andes Calc-Basal
Si02 64.16 49.91 63.49no,Al 20jF 62 Da*
HnOHgOCaONazOKzOPzOa
0.5815.396.300.102.692.373.642.340.12
1.1419.409.610.183.675.624.470.720.14
0.5314.477.000.094.730.944.690.460.12
Total 97.69 94.86 96.52
LOI 2.31 3.57 2.96
fig t 45.82 43.06 57.23
Cr 25Hi 30Co 10Se - 37 12V 100Cu 10In 90
KBdSr
ZrTiY
19425435133
1473477
18
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1456834
14
38199272
2043177
16
Density 2.40 2.50 2.41
Appendix A
CERTIFICATE OF QUALIFICATIONS
I, Stewart J. Carmichael, of the Town of Kirkland Lake, in the District of Timiskaming, in the Province of Ontario, Canada, do hereby certify that:
1) I am a consulting geologist with address P.O. Box 271, Swastika, Ontario, POK 1TO.
2) I am a graduate of McMaster University, Hamilton, Ontario,having received the degree of Bachelor of Science, Geology from the Faculty of Science in 1982. I have since practised in the field of mineral exploration continuously since graduation.
3) I am a Fellow of the Geological Association of Canada.
4) I have no direct interest, nor do I expect to receive any interest in the Raitanen claims.
5) In addition to my personal knowledge of the area, I have made use of the records of the Ministry of Natural Resources of Ontario, and of Mr. Raitanen's records in the preparation of this report.
Total Direct and Indirect Costs...................513,070.14
Appendix C
Co-ords 62B.O N
Aziiuth: 1BO.O
Dip: -45.0
Elevation 1000.0
Length: 399.0
Claii: L-101516B
387.0 ELasse Raitanen OPftP
DIAMOND DRILL RECORD
Dip Tests
399.0 180.0 -45.0
HOLE NO.:Page: l
K91-1
Property: RAITANEN-KATRINEPurpose: To Test Little H i sew FaultDrilled by: L. RaitanenDate Started: JUNE 27, 1991Date Completed: AUGUST 7,1991Logged by: S. CarmichaelCore Size: EX
froi (ft)
to (ft)
-Description- Saiple froi to Length Au-l Au-2 Cu-1 Cu-2 No. (ft) - (ft) (ft) ppb oz/ton ppi l
.00 2.50 CASING
2.50 116.00 ANDESITELight green fine grained MSS i ve aiygdularcalc-alkaline andesite. 20Z calcite t- chloritepinhead size aiygdules. 2-5Z quartz t- calcitestringers. FIoHS locally becoming very fine grainedwith clusters of spherules.28.60 10Z quartz stringers, trace pyrite.69.30 70.30 Very fine grained Hith spherules.90.00 Foliation at 42 deg. To C.A.92.20 92.BO Interflow tuff, ash tuff to lapilli,
foliation at 46 degrees to C.A. 101.BO 102.00 Ouartz/calcite vein, dip 41 deg. To
C.A. nil sulfides.
116.00 118.00 FAULT ZONEStrongly foliated andesite froi 116.0-117.0'. Foliation at 42 deg. To C.A. Ground core froi 117.0-118.0'. Nil sulfides. Hi nor calcite *- heutite stringers.
118.00 283.00 ANDESITEContinuation of unit above fault.164.00 2ci vide qnartz/calcite vein. Dip 42
deg. To C.A. Nil sulfides. 234.50 235.70 Hyaloclastite. 241.00 Core becoming blocky and broken. 249.00 Fault, clay gouge. 253.00 Fault, clay gouge, core lost froi
I.C.A.P. ANALYSISMoor U*Mnt* by Fusion nrarr mo. , M9256
Pag* Bo. i l of l
Ml* Bo. i JLOUB
Dtto s JVL-OS-1M1
1W-32S4-M1
8IHPLB t Co •i la
7174 10 10 30 100 90 30
TSL/91
i ruf"-
ul
IMF TOWNSHIPor
BEN NEVIS TP M.325
DISTRICT OF TIMISKAMIN3
LARDER LAKE MINING DIVISION
SCALE: 1-INCH 40 CHAINS
---.--U
CROWN LAND fALE
LEAltLLOCAH O IM,0
it- y irs?*^-;.- ^ .-,.. r^ MINING HlGHTS ONLYSURFACF RIGHTS ONLY
ROADSiMPhUVLUKIND'SR AIL W; i.POWER LINES
MARSH OR MUSKEG
MiNkSCANCFlLFDF ATENTEO ^ R O.
i i16164 ' IOI9I65 1018166
00' s.rforp i ..'-tr rt:.{ r\ c 1^ i ,\'.i 'C
! t -M * O t C' ' Itj^r ' i, ,Q l ; Vt l
Arflas withdrawn from staking under Section 43
of (he Mining Act Order no File Date Disposition
NH W 83,*O 11846^ ib/4/AO
r " r -'1r^ ,\- jV-o- A c '
Op*n*d Order no 0-IOJ/B7 NR 0*e 8 XA7PT t' Wft/M an* Mr-AO/at IM-S
PT n f w W/ftfi (S.R .MR) Op*n*4 by Order No O-IQ4 f A7 NR Per 3
W L 1/89 OPENCO ORDCH O-LB/89 NM iPHII -4
OME OF \SBUt
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i H/f emo114*7*1 i II48TM
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CIRCULATED MAHCH gtf ,
PLAN HO.
ONTAJ IO
MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH
MCVITTIE TR M.370
THE INFORMATION l HAl APPFAHb ON THIS MAC HA'. BEEN rOMPHFD FROM VARIOUS bOUFU.tS AND A(X UHAOY IS NOT GUAMANTEED THOSE WISHING TO TSntof MINING CLAIMS SHOULD CON bULT WITH THF MINING RECORDER MINISTRY OF NORTHERN DEVELOP Mf NT AND MINES, FOR ADniTlONAl INFORMATION ON IMF STATUS OF THE l ANDS SHOWN HFREON