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REPORT ON THE

COMBINED AIRBORNE GEOPHYSICAL SURVEY

ON THE PROPERTY OF

KANGLED RESOURCES LTD.

DAHL, DAMBROSSIO AND DUMAS

TOWNSHIPS, ONTARIO

BY

RECEIVED

JUN ^ 1988

MINING) LANDS SECTION

H. FERDERBER GEOPHYSICS LTD.

June,1988 D. M. Thai, B.Se, Val d'Or, Quebec Geophysicist

H. FERDERBER GEOPHYSICS LTD

REPORT ON THE

COMBINED AIRBORNE GEOPHYSICAL SURVEY

ON THE PROPERTY OP

KANGELD RESOURCES LTD.

DAHL, DAMBROSSIO AND DUMAS TOWNSHIPS, ONTARIO

INTRODUCTION

l l l l l l lI in Dahl, Dambrossio and Dumas Townships, Ontario. Magnetic and

VLF-electromagnetic data was collected by the airborne division

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From February 19 to 26, 1988 a combined airborne geophysical survey was completed on the property of Kangeld Resources Ltd

of H. Ferderber Geophysics Ltd. The survey was flown in the north-south direction for a total of 540.74 miles from a base

at Wawa.

The magnetic survey provides information which help define underlying geological strutures and identifies potential economic mineralized concentrations which may contain variations in accessory magnetic minerals. The VLF- electromagnetic survey outlines conductive zones which may represent metallic sulphide deposits and/or shear zones

containing economic mineralization.

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PROPERTY DESCRIPTION, LOCATION AND ACCESS

The Kangeld Resources property is comprised of 453 claims in Dahl, Dambrossio and Dumas Townships, Algoma District, Sault Ste Marie Mining Division, Ontario. The claims cover

approximately 7248 hectares with 139 claims in Dahl, 193 claims in Dambrossio and 121 claims in Dummas Township. These claims are registered with the Ontario Mining Recorder's Office in Sault Ste Marie and are listed in Appendix I .

The claim group is located just east of the Obatanga Provincial Park in the vicinity of Kabenung Lake. It is approximately 20 miles north of the town of Wawa, and 24 miles south-southeast of the town of White River. Access is readily obtained from

the Trans Canada Highway 17 which passes through the central

western part of the property. Several series of interconnected all weathered and dry weathered roads exiting off Highway 17

cut throughout the western portion which can also be reached by boat on Kabenung Lake.

The eastern portion of the property can be reached by travelling on the all weathered highway to the town of

Dubreuilville. Several interconnected bush roads lead to the property by this highway.


Kabenung Lake, Lonely Lake/ Desolation Lake and several small

lakes, creeks, swamps cover about 2(^ area of the western half,

The eastern half is covered only about 5% by small lakes and

swamps and cut by several creeks such as Soderston and Tea creeks. The rest of the property is forested. Topographic relief is low to moderately high due to the presence of hilly terrain in the area.

Supplies, services and qualified manpower are available in the Wawa-White River Area.

GEOLOGY

The property is located in the northern edge of the east

extension of the Kabenung Lake Greenstone Belt of the Superior

Province of the Canadian Shield. The Belt extends eastward

from Kabenung Lake for a distance of over 50 miles (Goodwin 1962).

The Ontario Department of Mines Geological Compilation Map

2220, the Manitouwadge - Wawa sheet, accompanied by the Ontario Division of Mines Map 2333 indicate that the area is underlain by Archean metavolcanics in the south, metasediments in the center and felsic metamorphic rocks in the north. Each unit

takes up approximately one third of the total area.



-4-

The mafic metavolcanics are composed of massive to foliated

andesites to basalts. Pillowed andesites to basalts are also common. Some units of the metavolcanics are metamorphosed to amphibolitic facies.

The metasediments are composed mainly of greywacke, shale,

arkose, quartzite and conglomerate. Bands of iron formation

are mapped within the metasediments along the strike direction, along the southern boundary and also within the metavolcanics.

North of the claim group is underlain by felsic igneous and metamorphic rocks which are composed mainly of granitic, granodioritic and dioritic gneisses.

The area underwent several severe structural changes. Early

batholithic intrusion is evident around West Kabenung Lake and Dickenson Lake where granitic plugs are centered. Several northeast and north-northwest trending faults offset the

underlying rocks at six locations on the property and numerous locations in the surrounding areas. Folding is prominent in the metavolcanics and may have occurred prior to the granitic intrusion and faulting. Several discontinuous, narrow late diabase dykes crosscut all the underlying rocks. These dykes

appear trending northeast and some continue into the felsic metamorphic rocks in the north.



-5-

Although there is lack of surface mineral occurrences on the

property, the greenstone belt hosts numerous gold and base

metal showings. Gold, copper, iron and molybdenum were encountered in the surrounding, of the Kabenung Lake intrusion mainly within the metavolcanics.

Goudreau Mine, located about 7 miles southwest of the property,

is a past producer. The host rocks are of mafic metavolcanics which are cut by felsic and mafic intrusives and veins. The main vein, strikes N65O - 90OW, dip 60O - 80OS has been tracedfor 2,000 feet and is from 6 inches to 11 feet wide,

of gold averaged 0.11 ounces per ton of ore milled.

Production

Recovery

Years: 1926, 1932, 1936-1938, 1940

Gold

(ounces)

2,450

Silver

(ounces)

351

Ore Milled

(Tons)

23,211



Magpie Station (Regnery Occurrence) is located about 5 miles

southeast of claim group. Gold mineralization is encountered in the metavolcanics. Mineralized zone is 120 feet long and

110 feet wide. Surface samples range from 0.06 to 0.2 ounces of Au per ton. Drilling has been carried out down to 200 feet depth.

The Mishibishu Lake Greenstone belt, located about 2 kilometers

south of the Kabenung Lake Greenstone belt, possesses similar

geological setting as the Kabenung Lake Greenstone Belt and hosts several gold and base metal showings. Recent ambitious

exploration programs after the discovery of Hemlo revealed encouraging results.

The No Name Lake gold showing was discovered in 1984 on the Central Crude-Noranda property in the Mishibishu Lake Greenstone Belt approximately 25 miles southwest of the

property. Grab samples containing gold values of up to 0.744 oz/ton, were collected in quartz veins within a shear zone between mafic volcanic rocks and an intermediate volcanic flow and pyroclastic rocks. Recent smapling during the summer of 1987 identified a structure 200 to 700 meters wide and 4 km long, containing seven anomalous gold zones, ranging in widths from 0.5 m to 11 m. Grab and chip samples assayed from 0.01 oz/ton to 28 oz/ton. The gold was found in intermediate to felsic metavolcanic rocks located on the Central Crude Noranda Property.



-7-

The Mishibishu Lake Deformation Zone associated with several of

the gold occurrences in the Mishibishu Greenstone Belt is comprised of several shear zones totaling up to 500 meters is

also host to the Magacon (Muscocho Exploration Ltd.), the Scuzzy little lake (Dominion Explorers Ltd.) and the Discovery

(Westfield Minerals Ltd.) gold showings. They are situated near volcanic-sediment contacts along the deformation zone.

The geology of the Kangled Resources property in the Kabenung Lake Greenstone Belt is similar to that of the Mishibishu

Greenstone belt and has similar potential discovery of gold mineralization.

INSTRUMENTATION AND SURVEY METHODS

The survey was completed using a 1972 Cessna 172, fixed-wing aircraft, call letters CF-EWK, owned and operated by H.

Ferderber Geophysics Ltd. The pilot and navigator/operator were Y. Saucier and d. Thai, respectively, of Val d'Or.

Geophysical sensors were mounted on modified wing tips. The geophysical, navigation and data aquisition systems are described below.

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mMagnetometer

~8~"

The magnetometer used was a GEM Systems GSM-11, high

sensitivity airborne proton (Overhauser) magnetometer. Theinstrument continuously measures the Earth's magnetic field ata 0.01 gammareadings per

an accuracychannels for

sensitivity for 1 reading per second to 10second. For the survey 4 readings per second at

of 0.04 gammas were read. The analog output has 2coarse and fine displays.

VLF-EM System

A Herz Totem 2A VLF-EM System was used to measure the changesin the totalfrequencies

field and vertical quadrature field on twosimultaneously, with an accuracy of 11;. The

primary transmitting stations were Cutler Maine/ (NAA)frequency 24

KHz.

.0 KHz and Seattle Washington, (NLK) frequency 24.8

Radar Altimeter-

The ground clearance was measured with a King 10/10 A radaraltimeter. The survey was flown at a mean clearance of 300feet with the altimeter producing an accuracy of 5% (15 feet)at this altitute.


Tracking Camera and Video Centre

A RCA TC-200 colour video camera and Galaxy 200 video centre was used to record the flight path on standard VHS type video tapes. Manual fiducials were recorded simultaneously on video tapes along with geophysical data for accurate flight path recovery.

Data Aquisition System

A Picodas Group Inc. PDAS 1100 data aquisition system featuring seven analog inputs with two frequency inputs and external interfacing was used. A Termiflex Corp. ST/32 Keyboard control unit and Sharp Corp. LCD display unit are connected to the data aquisition system. At present this system stores the VLF-1 inphase, VLF-1 quadrature, VLF-2 inphase, VLF-2 quatrature, magnetic field (coarse), magnetic field (fine), and altimeter readings on 3.5 inch floppy diskette. The data is then printed out in digital and profile forms.

The survey was conducted on north-south lines at an aircraft altitude of 300 feet. The lines were flown at spacings of 400 feet at a speed of approximately 90 miles per hour. Navigation was visual using airphoto mosaics, at a scale of one inch to 1320 feet.

•1U- H. FERDERBER GEOPHYSICS LTD

DATA PRESENTATION

Flight lines, fiducial points and geophysical responses were reproduced from the airphoto mosaics at a scale of one inch to 1320 feet (1:15,840). The outline of the claim group, claim map and property boundary are shown on each map sheet.

The aeromagnetic data was corrected for diurnal variations by using a base line as reference. The data was then reduced to a base level of 58,000 gammas, contoured at 25, 100 and 1000 gamma intervals and presented on Maps MG-1, MG-2.

The VLF-EM data was transferred from diskettes to printed form. A base value was determined for the VLF-EM data and the change in the total field strength as a percentage of the base value was calculated. The values were plotted on Maps EM-1, EM-2. The positive values were contoured at intervals of 2%. The conductor axes were determined and labelled l, 2, 3, etc. No priority was attached to the labelling system.


-J.J.- H. FERDERBER GEOPHYSICS LTD

SURVEY RESULTS AND INTERPRETATION

Magnetic Survey

Map MG-1 presents the magnetic data collected on the western

half of the claim group. The airborne magnetic survey outlines three distinctive and extremely high magnetic zones against

background of about 58,800 gammas; one located at the south center over Kabenung Lake and the other two at the southeastern

and northwestern corners. These extremely high magnetic readings (up to 71,000 gammas) are commonly encountered in

areas of iron formation which indicate the extend of the metavolcanics and/or metasediments containing ferrie minerals.

Several moderately high magnetic zones (about 59,200 to 59,800 gammas) are also delineated along the center of the claim group

and they appear trending approximately in the east-west direction. These moderately high magnetic areas are probably underlain by mafic metavolcanics.

Several east-west trending magnetic lows encountered the north of the claim group representing underlying rocks of very low magnetic susceptability, in this case the felsic intrusive and metamorphic rocks. One lone series of moderately magnetic high

in the north center within the magnetic lows may represent

impingement of the mafic metavolcanics into the intrusive rocks.



-12-

Geological contacts such as the mafic metavolcanics and the intrusive rocks can be readily observed by the contrast of the low magnetic and moderatly high magnetic. Whereas the distinction between mafic metavolcanics and metasediment are not always obvious.

A north-northeast ti*ending fault is delineated by the breakages and distortions of contour lines in the far east corner. The presumed fault appears to be short, sub-vertical and correspond very well with surface geology.

A second north-northeast trending fault is delineated by the abrupt changes of the contour lines in the east center of the area and labelled as fault 2. It is believed to be sub- vertical fault with significant north-south displacement and correspond very well with surface geology. The fault appears continuing into Kabenung Lake.

The third fault is delineated in the southeast corner of the area and continues into the northwest corner of Map MG-2. The presumed fault is located in the metavolcanic and metasedments with significant northeast-southwest displacement.

MG-2 presents magnetic data collected on the eastern half of the claim group. The iron formation within the mafic metavolcanics in the southeastern corner of Map MG-1 continues about 3/4 mile into the eastern half. A small magnetic depression just north of this area along the boundary indicate the south impingement of the felsic metamorphic rocks which is believed to be displaced by late faulting. A north-northwest trending fault (fault 4) cuts across the property and causes northward displacement of the iron formation bearing metasediments. The fault appears to continue

-J..J- H. FERDERBER GEOPHYSICS LTD

into the felsic metamorphics. Iron formation in the

metasediments can be readily distinguished by a northeast trending series of magnetic highs. It is much thinner and probably buried deeper than the ones previously mentioned.

Mafic metavolcanics lie just south of the distinctive iron formation and are recognized by the moderate to moderately high

magnetic susceptability except the southeastern corner off the

property where another iron formation is detected.

Several late diabase dykes are present in the eastern half.

They can be distinguished as a series of northwest trending, thin and elongated high magnetic bodies. One northeast

trending late diabase dyke is also delineated in the southeast corner of the map and probably continues off the property.

VLF-electromagnetic

Map EM-1 and EM-2 present VLF-electromagnetic data collected in the claim group. The survey outlines 14 conductive zones on the property and they are described below in numerical order from west to east.


Conductive zone l, located to the far west of map EM-1, is a long continuous zone with moderate amplitude response. The zone splits at the east end where it overlies Kabenung Lake. The zone also overlies along the shoulder of a presumed iron formation and is probably caused by conductive minerals associated with the iron formation and/or geological contact between the metasidements to the south and mafic volcanics to the north.

Conductive zone 2, located in the center of map EM-1, is continuous, weak in amplitude and east-west trending. The zone overlies an anomalous low elongated magnetic body and a creek and also has its east end over Kabenung Lake. The conductive zone is probably caused by surface conductivity of the overburden and lake.

Conductive zone 3, located in the south center of Map EM-1, is continous, very week in amplitude. It overlies an anomalous high magnetic zone and Kabenung Lake. The zone is probably caused by surface conductivity of the lake shore.


Conductive zone 4, located in the south east of map EM-1,

exhibits very high amplitude of up to 601. The zone trends in two main directions, north-south and east-west forming a ring

of discontinuous zones. The zone overlies an area where metasediments cut the mafic volcanics and subsequently being displaced by two major faults. Bands of iron formations are also present in the area. The conductive zone may represent

possible faults/shear zones along with geological contacts.

Conductive zone 5, located along the northern boundary on map

EM-1, is an isolated short and strong conductive zone overlying

a probable fault zone. This could represent discontinuous shear zone along fractured zone within felsic metamorphic rocks.

Conductive zone 6, located in the northeastern corner of Map EM-1 along the boundary, is a discontinuous, strong conductive zone overlying isolated magnetic highs within the felsic metamorphic rocks. The zone may represent isolated mafic

intrusive rocks associated with shears.


-Ab- H. FERDERBER GEOPHYSICS LTD

Conductive zone 7, located in the southwestern corner of Map EM-2 overlapping Map EM-1, is a continuous east-west trending zone exhibiting moderate amplitude reponse. The zones lies over the edge of a presumed iron formation within the mafic metavolcanics and along the contacts with the metasediments.

It could represent conductive minerals associated with the iron formation and/or shear zone along geological contact.

Conductive zone 8, located along the boundary of Maps EM-1 and EM-2, is an isolated strong zone overlying a lake. This probably reflect conductive overburden of lake shores. -.

Conductive zone 9, located in the central western part of Map EM-2, is a long, continuous and moderately strong in amplitude. The zone also overlies part of an elongated moderately high magnetic body and partly over a creek. This could represent alteration zone along a possible diabase dyke and/or surface response along the creek.

Conductive zone 10, located in the northwestern corner of Map EM-2, is short and discontinuous conductor with relatively high amplitude. The zone lies along a presumed displaced fault among the metasediments, mafic volcanics and felsic metamorphic rocks and possibly represent shear along a fault or fractured zone.



Conductive zone li, located in the northwestern corner along the claim boundaries , i s comprised of two isolated zones with very high amplitude response. These could reflect effect of conductive overburden or lake shore since the two overlie small lakes.

Conductive zone 12, located in the center of Map EM-2, is a long discontinuous and east-west trending conductor. The zone appears splitting at the two ends and exhibits moderate amplitude reponse. The zone overlies a series of small lakes and swamps and also along an elongated magnetic depression. This may reflect surface response and/or geological contacts among units of the metasediments.

Conductive zone 13, located to the south center of Map EM-2, overlies a series of small lakes, swamps and creeks. It may represent surface conductivity of the surrounding topography.

Conductive zone 14, located to the northeastern corner of Map EM-2, is a long, continuous, east-west trending conductive zone. Its amplitude response is weak to moderate. The zone overlies the approximate geological boundary between the metasediments and felsic metamorphic rocks as well as a series of small lakes and swamps. The zone could represent possible geological contact and/or surface conductivity.



-18-

CONCLUSION AND RECOMMENDATION

The combined airborne magnetic and VLF-electromagnetic survey were successful in helping outline the underlying geology and delineating conductive zones representing possible shear/fault

zones on the Kangeld Resources Property, Sault Ste Marie Mining Division, Ontario.

The results of the magnetic survey indicate that the claim

group is underlain by Archean metasediments, metavolcanics and felsic metamorphic rocks. The northern parts of the claim

group along off the boundary generally exhibit low magnetic susceptability which are typical of felsic metamorphic and intrusive rocks. Southward impingement of these units along with geological contacts can be readily observed.

Metasediments and mafic metavolcanics underlying the south and

central parts of the claim group are distinguishable by their moderate magnetic susceptability. Metasediments are composed

mainly of conglomerate, greywacke, shale, arkose and quartzite. Mafic metavolcanics are of andesitic to basaltic in

compositions. Bands of iron formation in various sizes are interbedded with both rock types and easily characterized by

distinctive high magnetic signatures. Faulting, folding, batholithic intrusion etc. have caused major structural and

lithological changes among these unitsresulting in the complexity of magnetic patterns. In some cases the distinction

among the units are not apparent from the magnetic maps.


-J. 9- H. FERDERBER GEOPHYSICS LTD

Several possible fault zones as well as geological contacts, late diabase dykes were delineated and marked on maps.

i

The VLF-electromagnetic survey delineated fourteen conductive

zones of various physical property and underlying geology. Conductive zones 2 , 3 , 8, 11 and 13 are believed to be caused

by surface effects such as conductive overburden, lakes, swamps, topographic relief etc. Others are thought to represent bedrocks conductivity which may be associated with sulphide and gold bearing structures and formations.

The structural and lithologic complexity of the property, as

indicated by the magnetic and electromagnetic maps, suggests that the claims are located in a good geologic environment for

economic gold and/or base metals mineralization. Areas of similar geologic environments in the region host numerous past

and present producing mines as well as mineral occurrences. These areas are undergoing intense gold and base metal exploration.


Further work is warranted on the. property. Line cutting along with ground geophysics and detailed geological mapping should be carried out. A preliminary diamond drilling program is to be drawn upon results the previous phases may warrant.

Respectfully submitted,

H. FERDERBER GEOPHYSICS LTD.

Daniel M. Thai, B.Se. Geophysicist

l

W SSM 978626978627978628978629978630978631978632978633978634978635978636 ^978637978638978639978640978641978642978643978644978645978646978647978648978649978650978651978652978653978654978655978656978657978658978659978660978661978662978663978664978665978666978667978668978669978670978671978672978673978674978675

APPENDIX 1

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- UJj/UM LIST

SSM 978726978727978728978729978730978731978732978733978734978735978736978737978738978739978740978741978742978743978744978745978746978747978748978749978750978751978752978753978754978755978756978757978758978759978760978761978762978763978764978765978766978767978768978769978770978771978772978773978774978775

H. FERDERBER GEUPHYSICS LTD ,

SSM 978776978777978778978779978780978781978782978783978784978785978786978787978788978789978790978791978792978793978794978795978796978797978798978799978800978801978802978803978804978805978806978807978808978809978810978811978812978813978814978815978816978817978818978819978820978821978822978823978824978825


WSSM 978826978827978828978829978830978831978832978833978834978835978836978837978838978839978840978841978842978843978844978845978846978847978848978849978850978851978852978853978854978855978856978857978858978859978860978861978862978863978864978865978866978867978868978869978870978871978872978873978874978875

-2-

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H. FERDERBER GEOPHYSICS LTD .

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f \, Ministry ol Report olVVprk.l. Northern Development l Q fcj 15

and Mines (Geophysical/Geological,.Ontario s~*. ^. GaocltffuicaJ-and fjawendit^ Gaoc

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M.- InltiInttructions: Pleaw tvnp or nrint

jj(8

Miltype ol Stirvcy(s)

Airborne Magne t ic....a nd V LF - E l e c t oma gn e ̂ j. uClaim Holder(s) " '

H. and L. Mineral HoldingsAddress '

C/o Durham-Geological Services InCy, ^-, 0 P.P. Box 734, Timmins, Ontario, P4ft 7G2

2.11383 DAHL 300

l uamp.rossip, pafti.,..JDumas——Prospector's Licence No//, /^ ,, , .

T ....46.4.5....

Survey Company

H. Ferderber Geophysics Ltd.Name and Address of Author (of Geo-Technicaf report)

R. Campbell - G. Henri ksen r 169 P^rrânl-H

Date of Survey (from a to)

19. .02 188 126 .02 88Day j Mo. f Yr. | T)ay | Mo. | Yr.

of li

600

Val Or , JQP ?H1Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:Enter 40 days. (This includes line cutting)

For each additional survey: using the same, grid:

Enter 20 days (for each)

Man Days

Complete reverse sida* w * and enter total(s) ho|dC C V

MAY

MINING 1

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

GoochoMiical

Geophysical

! E "^ V'Ô)6110- Magnetometer

*~ - RaoTometric

.ANDfSECTSOHGeological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

- ————— -

Days per Claim

————— ̂

— — ———

Days per Claim

__ 4D.

40

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days crcdi-ts per claim selected , in columns at right. S

Date Recorded Holder or Agont/Sîgniujre)m.Certification Verifying Rejjort of \A(o

Mining Claims Traversed (List in numerical sequence)Mining Claim

Prefix

JSSlI..

F

A. ?l

Number

978626 ei

s.e.e atlaj:

— --- — — -- —— -

'

.. -. ........ -. - . -—

fiAUlT SIS. KMiMI'C P'''n c L \

W* 5 1vi.. ......— ..........

—- ———— -..—..

Expend. Days Cr.

fll

:hed t

———

———

' u r388"--.-p,

-— — —

'P

J

Mining ClaimPrefix

)l

R E

F*CC(

Number

.

CORD

APR 5 1988

ipi wo, ^..,,— ,^

---••-

...... . - ... ... .

Expend. Days Cr.

-- ————

.... ———

. ..

y n

— — - -

For Office Use OnlyTotal Days Cr. Recorded

Total number of mining claims covered by this report O* work.

/if T/A/ ( :;______Date Recorded

Appcdvcd as R.ecordod

Mining Recorder

Branch Director /f 7

1 hereby certify that 1 have a personal and intimate knowledge of the (nets set forth in or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person

Harry Ferderber,Certifying

169 Perreault ave . , Val d

the Report of Work annexed hereto, having performed

'Or,

the work

Quebec J9P 2H1Dnto Certified Corti, ';if I)V (Signature)

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APPENDIX l - CLAIM LIST

SSM 978626 978627'978628978629978630978631978632978633978634978635978636978637978638978639978640978641978642978643978644978645978646978647978648978649978650978651.978652978653978654978655978656978657978658978659978660978661978662978663978664978665978666978667978668978669978670978671978672978673978674978675

SSM4 978676978677978678978679978680978681978682978683978684978685978686978687978688978689978690978691978692978693978694978695978696978697978698978699978700978701978702978703978704978705978706978707978708978709978710978711978712978713978714978715978716978717978718978719978720978721978722978723978724978725

SSM 978726978727978728978729978730978731978732978733978734978735978736978737978738978739978740978741978742978743978744978745978746978747978748978749978750978751978752978753978754978755978756978757978758978759978760978761978762978763978764978765978766978767978768978769978770978771978772978773978774978775

SSM 978776978777978778978779978780978781978782978783978784978785978786978787978788978789978790978791978792978793978794978795978796978797978798978799978800978801978802978803978804978805978806978807978808978809978810978811978812978813978814978815978816978817978818978819978820978821978822978823978824978825

-2-

SSM 978826978827978828978829978830978831978832978833978834978835978836978837978838978839978840978841978842978843978844978845

- 978846978847978848978849978850978851978852978853978854978855978856978857978858978859978860978861978862978863978864978865978866978867978868978869978870978871978872978873978874978875

SSM 978876978877978878978879978880978881978882978883978884978885978886978887978888978889978890978891978892978893978894978895978896978897978898978899978900978901 '978902978903978904978905978906978907978908978909978910978911978912978913978914978915978916978917978918978919978920978921978922978923978924978925

SSM 978926978927978928978929978930978931978932978933978934978935978936978937978938978939978940978941978942978943978944978945978946978947978948978949978950978951978952978953978954978955978956978957978958978959978960978961978962978963978964978965978966978967978968978969978970978971978972978973978974978975

SSM 978976978977978978978979978980978981978982978983978984978985978986978987978988978989978990978991978992978993978994978995978996978997978998 978999K979000979001979002979003979004979005979006979007979008979009979010979011979012979013979014979015979016979017979018979019979020979021979022979023979024979025

-3-

SSM 979026979027979028979029979030979031979032979033979034979035979036979037979038979039979040979041 979044"979045979046

SSM

979054979055979056979057,979062979063979064979065979070979071

979072979073 979078~979079979080979081979082979083979084979085979086979087979088979089979090979091979092979093979094979095979096979097979098.

Ministry ofNorthern Developmentand Mines

Ontario

Geophyslcal-Geological-Geochemical Technical Data Statement

File.-

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s). Township or Area. Claim Holder(s)—

Airborne Magnetic arid VLF-Electomagnetic

Dambrossio, Dahl and Dumas

H. s L. Mineral Holdings

Survey Company H. Ferderber Geophysics Ltd.

Author of Report Dan Thai ̂ ^^—————————--Address of Anthnr

Covering Dates of

Total Miles of Line Cut.

169 Perreault Ave., Val d'Or Que

Feb. 19 to 26, 1 988———-————(linecutting to office)

Flown 540.74

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer——Radiometric———Other______

DAYS per claim

Geological.Geochemical.

AIRBORNE CREDITS (Special provision credit* do not apply to airborne turveyi)

Magnetometer--33—Electromagnetic ——33 Radiometric ————(enter days per claim)

u 1Au .eport or Agent

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

SSM 978626 et. al.(prefix) (number)

see attached appendix*t********i********i***t***********T*r*********4***x

i

l

TOTAL CLAIMS. 453

SELF POTENTIALInstrument——————————————————————————————————————— Range.Survey Method____________i——.-—.—.——-———.-—————-————-...——....--.—...

Corrections made.

RADIOMETRICInstrument.Values measured.

Energy windows (levels)___________________________',___________ Height of instrument_____________________________Background Count. Size of detector____________________________________________

Overburden.________________________________________v———(type, depth — include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey—————-———^——————-——..——.^.Instrument.————-..-...—-.—....—...—.....——.—.—— Accuracy._______.—————————^————^^.Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYSType of ^irvry(g). Airborne Magnetic and VLF-ElectomacmeticInstrument(s) G EM GSM-11 Herz Totem 2A

(specify for each type of survey)Accuracy.—:_____0.04 gamma and 11

(specify for each type of survey)Aircraft mid Cessna 172—^-—,^—--^-————Sensor altitude___inn frrt-

Navigation and flight path recovery method -Ua vi ga f irm W&Q ^isiial on airphoto mocaicj. Flight path recovery was obtained with a RCA colour video camera Panasonic^--^Jiutix. v jutitji^ l l J. L.U J.

Aircraft altitude____300 feet____________________Line Sparing 4nn f*Miles flown over total area 540. 74___________________Over daims only ^70 . 5ft


SSM 978626978627978628978629978630978631978632978633978634978635978636978637978638978639978640978641978642978643978644978645978646978647978648978649978650978651978652978653978654978655978656978657978658978659978660978661978662978663978664978665978666978667978668978669978670978671978672978673978674978675

SSM 978676978677978678978679978680978681978682978683978684978685978686978687978688978689978690978691978692978693978694978695978696978697978698978699978700978701978702978703978704978705978706978707978708978709978710978711978712978713978714978715978716978717978718978719978720978721978722978723978724978725

SSM 978726978727978728978729978730978731978732978733978734978735978736978737978738978739978740978741978742978743978744978745978746978747978748978749978750978751978752978753978754978755978756978757978758978759978760978761978762978763978764978765978766978767978768978769978770978771978772978773978774978775

SSM 978776978777978778978779978780978781978782978783978784978785978786978787978788978789978790978791978792978793978794978795978796978797978798978799978800978801978802978803978804978805978806978807978808978809978810978811978812978813978814978815978816978817978818978819978820978821978822978823978824978825

-2-

SSM 978826978827978828978829978830978831978832978833978834978835978836978837978838978839978840978841978842978843978844978845978846978847978848978849978850978851978852978853978854978855978856978857978858978859978860978861978862978863978864978865978866978867978868978869978870978871978872978873978874978875

SSM 978876978877978878978879978880978881978882978883978884978885978886978887978888978889978890978891978892.978893978894978895978896978897978898978899978900 .978901978902978903978904978905978906978907978908978909978910978911978912978913978914978915978916978917978918978919978920978921978922978923978924978925

SSM 978926978927978928978929978930978931978932978933978934978935978936978937978938978939978940978941978942978943978944978945978946978947978948978949978950978951978952978953978954978955978956978957978958978959978960978961978962978963978964978965978966978967978968978969978970978971978972978973978974978975

SSM 978976978977978978978979978980978981978982978983978984978985978986978987978988978989978990978991978992978993978994978995978996978997978998978999979000979001979002979003979004979005979006979007979008979009979010979011979012979013979014979015979016979017979018979019979020979021979022979023979024979025

-3-

SSM 979026979027979028979029979030979031979032979033979034979035979036979037979038979039979040979041979044979045979046979049979054979055979056979057979062979063979064979065979070979071

SSM 979072979073979078979079979080979081979082979083979084979085979086979087979088979089979090979091979092979093979094979095979096979097979098

Ontario

Ministry ofNorthern Developmentand MinesMinisters du Developpement du Nord et des Mines

June 24, 1988 Your file: W8805-068 Our file: 2.11283

j ONTARIO GEOLOGICAL SURVEY

ASSESSMENT FILESOFFICE

JI'N 28 19

RECEIVED

Mining RecorderMinistry of Northern Development and Mines875 Queen Street EastBox 669Sault Ste. Marie, OntarioP6A 2B3

Dear Madam:

Re: Notice of Intent dated June 10, 1988Airborne Geophysical (Magnetometer b Electromagnetic)Survey submitted on Mining Claims SSM 978626 et alin the Townships of Dambrossio, Dahl and Dumas

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,

U4jk*r^ -^ W.R. CoVfan, ManagerMining Lands Section Mines b Minerals Division

Whitney Block, Room 6610 Queen's Park Toronto, Ontario M7A 1W3

Telephone: (416) 965-4888

Enclosure

cc: Mr. 6.H. FergusonMining and Lands Commissioner Toronto, Ontario

H. and L. Mineral Holdingsc/o Durham Geological Services Inc.P.O. Box 734Timmins, OntarioP4N 762

Resident Geologist Wawa, Ontario

Ministry ofNorthern Developmentand Mines

Technical Assessment Work Credits

Ontario

.Date

June 10, 1988

File

2.11283Mining Recorder's Report of Work No,

W8805-068

Recorded HolderH. and L. Mineral Holdings

Township oKX&XX

Dambrossio, Dahl, Dumas

Type of survey and number of Assessment days credit per claim

Geophysical *5*5

Electromagnetic rtay?

33Magnetometer . riays

Other ' Hays

Section 77 (19) See "Mining Claims Assessed" column

Geological days

GfiochemiRal riays

Man days Q] Airborne 0

Special provision j | Ground [~1

[~1 Credits have been reduced because of partial coverage of claims.

0 Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

See attached Schedule "A"

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claims| | not sufficiently covered by the survey f"| insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19} - 60.

828 (85/12)

ATTACHMENT "A 1


SSM 978626978627978628978629978630978631978632978633978634978635978636978637978638978639978640978641978642 978643-978644978645978646978647978648978649978650978651,978652978653978654978655978656978657978658978659978660978661978662978663978664978665978666978667978668978669978670978671978672978673978674978675

SSM 978676978677978678978679978680978681978682978683978684.978685978686978687978688978689978690978691978692978693978694978695978696978697978698978699978700978701978702978703978704978705978706978707978708978709978710978711978712978713978714978715978716978717978718978719978720978721978722978723978724978725

SSM 978726978727978728978729978730978731978732978733978734978735978736978737978738978739978740978741978742978743978744978745978746978747978748978749978750978751978752978753978754978755978756978757978758978759978760978761978762978763978764978765978766978767978768978769978770978771978772978773978774978775

SSM 978776978777978778978779978780978781978782978783978784978785978786978787978788978789978790978791978792978793978794978795978796978797978798978799978800978801978802978803978804978805978806978807978808978809978810978811978812978813978814978815978816978817978818978819978820978821978822978823978824978825

•( ATTACHMENT

SSM 978826978827978828978829978830978831978832978833978834978835978836978837978838978839978840978841978842978843978844978845978846978847978848978849978850978851978852978853978854978855978856978857978858978859978860978861978862978863978864978865978866978867978868978869978870978871978872978873978874978875

SSM 978876978877978878978879978880978881978882978883978884978885978886978887978888978889978890978891978892978893978894978895978896978897978898978899978900978901978902978903978904978905978906978907978908978909978910978911978912978913978914978915978916978917978918978919978920978921978922978923978924978925

SSM 978926978927978928978929978930978931978932978933978934978935978936978937978938978939978940978941978942978943978944978945978946978947978948978949 '978950978951978952978953978954978955978956978957978958978959978960978961978962978963978964978965978966978967978968978969978970978971978972978973978974978975

SSM 978976978977978978978979978980978981978982978983978984978985978986978987978988978989978990978991978992978993978994978995978996978997978998978999^979000979001979002979003979004979005979006979007979008979009979010979011979012979013979014979015979016979017979018979019979020979021979022979023979024979025

x - -

Attachment-3-

SSM 979026979027979028979029979030979031979032979033979034979035979036979037979038979039979040979041 979044"979045979046979049* 979054979055979056979057979062979063979064979065..979070979071

SSM 979072979073 97907JT979079979080979081979082979083979084979085979086979087979088979089979090979091979092979093979094979095979096979097979098.

H. FERDERBER GEOPHYSICS LTD. G EOPHYSICAL a GEOLOGICAL SURVEYS 169 PERRAULT AVENUE, VAL D'OR, QUEBEC J9P 2H1 TELEPHONE 818-824-2075

June 3, 1988

Ontario Ministry of Northern Development and MinesManager, Mining Lands SectionMineral Development and Lands BranchMines and Minerals Division R ECEIVEDWhitney Block, Room 6610Queen's Park . HIM 6 1988Toronto, Ontario J UN . IWOM7A 1W3

MINiNG LANDS SECTIONRe: Report, Maps and Technical Data Statement

for Report of Work on 453 claims (SSM 978626 et. al.) in Dahl, Dambrossio and Dumas Twps., W8805-068.

Dear Sir:

Enclosed are two copies of a report and maps and a technical

data statement for 453 claims in Dahl, Dambrossio and Dumas

Townships, W8805-068.

Yours truly,

R.A. Campbell, B.Se, Geologist

RAC/pb

REFERENCES' AREAS WITHDRAWN FROM D ISPOSITION

. . M.R.O.-MINING RIGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

. M.+ S. -MINING AND SURFACE RIGHTS

.'- Dticrjptlon Order No. Dat* Olspoiltlon ' Fill , V^tO/B* J2/2I/84 9RO

42C07SWe^2 2.11283 DAHL

R E C E l V L

2 S 1983M? t', M.

BERNST TWP.

CL I-

RESERVE'.ONE-HALF MILE MIDI KTRI* ON IACH • IDE OP HIGHWAY N*. (T JULY, 11 WOFILE N*. lesooeftlU. WITHD**WM F ttOM STAKINB UNDER SECTION *a MJHIHO

D.H-0GRAVEL

Flit: 164226

200

*VT?-j?auf*

-^TBWDWf ~V-T ^

^KSî^l irroitr***? l-T*Z

r " i""' '•ut n -J a i,

i 1^SSM SSM ^ ' ^J3SM

SSM. , 3SM .-I3SM ^ SSM 'SSMXN.-^SM 3SM

Cfa \T*I4. l****** l

LALIBURT TWR

LEGENDHIGHWAY AND RO^TE NeJ; ; • •*j f;. OTHER ROADS ; , ^. V VTRAILS ,! "' '..''''''-

, ' - "' '' .,- ' -SURVEYED LINES^ - ;'. J ' " ---;

TOWNSHIPS, BASELINES, ETC.'LOTS, MINING CLAIMS, PARCELS, ETC.-' '.','v^.'"- ';*jTffi

^SURVEYED LINES:' '--: , '. V : ," ,-;'; -'^K^^^'l^ÛNSURVEYED LOT LINESPARCEL BOUNDARY - " MINING CLAIMS ETC. . ,

RAILWAY AND R IGHT OF WAYUTILITY LINESNON-PERENNIAL STREAM , '. :FLOODING OR FLOODING RIGHTS Y I SUBDIVISION OR COMPOSITE PLAN' f;RESERVATIONS , , ; v, -'.ft'.^'-fORIGINAL SHORELINEMARSH OR MUSKEGMINESTRAVERSE MONUMENT

'"^LiTSip-'^' ;, . '. "Tt^f^ J

HIT .' ' -. j.*1'' *-.r.'f; , ,'\ '."•i.-"- -.'.' • f&.'i '^.NT - ' J .' .:- ••t- . - 1 .- .- ',S -•.•/",Âi --^ ' ^./---lYV't"J.V

-,:- -V; *-.'';vf.^ f^*/

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT .

PATENT, SURFACE ft MINING " .SURFACE R IGHTS

, M l N l NG RIGHTS ON L Y J^l^l'-J^ril-

LEASE, SURFACE Si MINING" .SURFACE

" .MINING RIGHTS

LICENCE OF OCCUPATION ^.^:;uiiluîi

ORDER-m-COUNtlL...:il:;-..V.^^L^4i^

R ESE R V ATION' ̂ ......^. Jî^^CiîlLLi

CANCELLED , J^.j..^_^l.iU-1^^^;^ SAND S GRAVEL .....^JC-l.î.-.i.^.-îii

.NOTE; M INING RIGHTS IN PARCELS PATENTED PRIOR TO

1B13, VESTED IN ORIGINAL PATENTEE BV THE LANDS ACT, R.S.O. 1 970, CHAP.. &Q. SEC.. S3i-.

: - - . - ' - ';".''~.'' v'."",-^ ; --X-v^1/^'^^'^fc^1 SCALE: 1 INCH-40'CHAINS ^:^.'M\: ; 'J^rf^^' -' ' •^••••^''>. i ::;•''fi^:^îf/

1 -'. V 1 -' -.'', *'•'."^•".••*^',^'V-y^yJi*5iflno Bonn . "*:•• v: aoArfsi!*'1-1 '*'!

FEETO 10OO 2000 4000

O 200 METRES

1000 , . il KMI '

TOWNSHIP

DAMBROSSIOM. N. R. ADMINISTRATIVE DISTRICT^

'MINING DIVISION

- SAULTLAND TITLES/ R EGISTRY DIVISION

Ontario

Minlstryof Land , VNatural ManagementResources Branch

Dal* MARCH 9,1983 Nurnbir

-

REFERENCESAREAS W ITHDRAWN FROM DISPOSITION

M.R.O. -MINING RIGHTS ONLY

S.R.O.- SURFACE RIGHTS ONLY

M.4 S. - MINING AND SURFACE RIGHTS

Otter ip t Ion Order No. Data D isposition F ile

SEC. 3(1/80 W 22/81 4/12/fll S.R.O, 188948

SAND and GRAVEL

GRAVEL FILE 162971

M.T.C. PIT 1262

M.T.C. PIT 2F4

PIT 2PS

PIT FILE 104226

FILE 124226

PIT * F3

M T.C.

M T C

GRAVEL

M T. C

DATE OF ISSUE

MAY O "i 1987

SAULT STE MARIE MINING RECORDER'S OFFICE H-

00<Q. < T. O

42C07SWO002 2.11283 DAHL 210

STE. MARIEWINING ntvR C C L l V Li

P.M.

ASHLEY TWP.

-- IM

m L JTpJir^Pj? \a Ji^OC"M . t - - . . i T. —— . . ""fc*|l*L - . m

KNICELY TWP.

OO) COoo: CD

o

KILLINS TWP.

LEGENDHIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS.

SURVEYED LINES:TOWNSHIPS, BASE LINES. ETC.LOTS, MINING CLAIMS, PARCELS, ETC.

UNSURVEYED LINES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC,

RAILWAY AND RIGHT OF WAY -*

UTILITY LINES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION OR COMPOSITE PLAN ,

ORIGINAL SHORELINEMARSH OR MUSKEG

MINESTRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT, SURFACE ft MINING RIGHTS..—.............. 0

" .SURFACE RIGHTS ONLY........................ O

" , MINING RIGHTSONLY.^__....,..,......M-. O

LEASE, SURFACE Si MINING RIGHTS...—..-"....™——. B

" .SURFACE RIGHTS ON LY...........-.....™....™ B

" , MINING RIGHTS ONLY...........-.^.......—-. QLICENCE OF OCCUPATION .._......................™. TORDER-IN-COUNCIL .......~...................™..—— OCRESERVATfON ___,....._.,........................... ©

CANCELLED _,—..-..-^^-....-.................... ®SAND 81 GRAVEL ._......__.............™™...——.. ©

NOTE: MINING RIGHTS IN PARCELS PATENTED PRIOR TO MAV 6, 1813, VESTED IN ORIGINAL PATENTEE BY THE PUBLIC LANDS ACT, R.S.O. 1070, CHAP. 3*0, SEC, 63, BUBSEC 1.

SCALE: 1 INCH - 40 CHAINS

FEET1000 2OOO 4OOO 6OOO aooo

O 2OQ METRES

1000 11 KM)

2000 (2 KM)

TOWNSHIP

DAHLM.N.R. ADMINISTRATIVE DISTRICT

WAWAMINING DIVISION

SAULT STE. MARIELAND TITLES/ REGISTRY DIVISION

ALGOMAMinistryof LandNatural ManagementResources B ranch

Ontario

Hit* OCTOBER, I9B4((••••l

G-2419

DA

MB

RO

SS

IO

TR

M.1

559

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CLAIM MAP

DAHL TWP

tfV -' -^ ; O

KNICELY TWP'LALIBURT

TWP

O >

LEGENDTOTAL FIELD CONTOUR INTERVAL 2 5 GAMMAsFIDUCIAL POINTLINE DIRECTIONBASE VALUE sncor GAMMASMAGNETIC LOWIOOO GAMMAS

K .'O GAMMAS

2f GAMMAS

PO".;iBLE FAULT

2.11283 DAHL 230

TYPE OF WORK

AIRBORNE MAGNETIC SURVEYCLIENT

KANGELD RESOURCES LTD.PROJECT

Sy^C-*/'/x ^ ' t'-\

H. Ferderber Geophysics Ltd

AREADAHL,DAMBROSSIO,

DUMAS TWPS,ONTSCALE

- /A m ileDRAWN BY

DATEMAY 1988

MAP OR SHEET NO.MG-

DUMAS TWPDAMBROSSIO TWP

CLAIM MAP

Scole :____\

i* v -A TO A" 1-1^1 ' ex 1- IU.A , v i,,A

tXto C-^ V ' " 'r **fc t -ftfa V-',-6fa

* ' ,A0 ' ,0^ , ,A^ l ^ ^ ' ..^

Ai.lBURT TWP LECLAIR TWP

LEGEND

O >

TOTAL FIELD CONTOUR INTERVAL 25 GAMMA:FIDUCIAL POINTLINE DIRECTIONBASE VALUE ssooo GAMMASMAGNETIC LOW1000 GAMMAS

100 GAMMAS

?.5 GAMMA

POSSIBLE FAULT

POSSIBLE DYKE

TYPE OF WORK

AIRBORNE MAGNETIC SURVEYCLIENT

KANGELD RESOURCES LTD.PROJECT

/

*,^*^—

H. Ferderber Geophysics Ltd.


DUMAS TWPSPNT.SCALE

mile

DRAWN BY

DATEMAY 1988

MAP OR SHEET NO.MG-2

42C07SW0a02 2.11283 DAHL 240

DAMBROSSIO TWP

CLAIM MAP

. : o^ ~~~""^ "i -^ l eh 1

KNICELY TWP LALIBURT TWP

o

LEGENDTOTAL FIELD CONTOUR INTERVAL 2 CONDUCTOR AXISFIDUCIAL POINT LINE DIRECTION STATION USED: CU-LEH t,, UNE- i to 7-., 1/5 to

SFATTI F f^r l !MF C, 7^ t.LESS THAN ZERO

2 D-- ,0

TYPE OF WORK

AIRBORNE VLF-EM SURVEYCLIENT


PROJECT•-.J,

H. Ferderber Geophysics Ltd


DUMAS TWPS,ONTSCALE

7 -l^ /A m ile

DRAWN BY

DATEMAY 1988

MAP OR SHEET NO.EM'

250

DAMBROSSIO TWP

CLAIM MAP A Scole ; l" E

J^l —_ —— —.-,——.P't SMV ; # ' xC^^

rVv* !^i # I V*f'-:'i*^J ,hV^^-^ ,v \ # J ^3y~

DUMAS TWP

f' ^ ' .^ ' ^ i #v \*P , A -^ •^ ~^JP [ -^^^ i f-L.LPL-.-Fi-.-J*

'

,

ii/j^j^k^^-i^ ^ ̂ i ALIBURT TWP LECLAIR TWP

O >

LEGENDTOTAL FIELD CONTOUR INTERVAL 2 "/o CONDUCTOR AXISFIDUCIAL POINTLINE DIRECTIONSTATION USED: CUTLER for LINES i *o ?s, 175 to 20;LESS THAN ZERO S EATTLE fur L INES 6 t o ' 75

7o

OVo

TYPE O F WORK

CLIENT

PROJECT

AIRBORNE VL.F-EM SURVEY


H. Ferderber Qaophysics Ltd

AREA DAHL, DAMBROSSIO, DUMAS TWPS,ONT

SCALE- /^ mile

DRAWN BY

DATEMAY 1988

MAPOfl SHEET N O.

2.11283 DAHL 260

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