GEOLOGICAL SURVEY LARDER LAKE MINING DIVISION FOR · Claim 4225382 is located in Holloway Township,...

e ,

GEOLOGICAL SURVEY

ON THE

NEWMAN -16

HOLLOWA Y TOWNSHIP

LARDER LAKE MINING DIVISION

DISTRICT OF COCHRANE, ONTARIO

FOR

TIGER GOLD EXPLORATION CORPORATION

JULY 27, 2009 MISS WENDY K. WELLER

GEOTECH

R · JUL 2 9 2009

GEOSCIENCE ASSESSMENT OFFICE

Geological survey - N -16 by Wendy Weller

TABLE OF CONTENTS

TABLE OF CONTENTS 2

SUMMARY 3

TI'l"TRODUCTION 4

LOCATION AND ACCESS 5

PROPERTY HISTORY 5

REGIONAL GEOLOGY 5,6

ECONOMIC GEOLOGY 6

TOPOGRAPHY 7

OBSERVATION OF FIELD RESULTS 8,9

CONCLUSIONS 9

REFERENCES 10

ASSESSMENT DATA FORM 11

CERTIFICATE 12

MAPS

LOCATION AND ACCESS (FIGURES la) 5a)

TABLE 1 - TABLE OF LITHOLOGIC UNITS FOR THE HOLLOWAY 5b)

TOWNSHIP

GEOLOGICAL SURVEY MAP NO. N-16/2009/geo In back pocket

Geological survey - N-16 by Wendy Weller

SUMMARY:

The report includes a Geological Survey as required by The Ministry of Northern

Development and Mines for assessment work purposes.

The report includes an introduction to the property, property history, general geology,

field observations and conclusions based on the field surveys.

Technical data is provided at the back of this report. Field data is compiled on the

accompanying plan maps N-16/2009/geo, found in the back of this report.


INTRODUCTION

GEOLOGICAL SURVEY ON THE

NEWMAN -16 GROUP HOLLOWAY TOWNSHIP

LARDER LAKE MINING DIVISIN DISTRICT OF COCHRANE, ONTARIO

The NEWMAN -16 Group is a single block of sixteen claims (one block) in this group.

Claim 4225382 is located in Holloway Township, Larder Lake Mining Division.

A Geological Survey was started on the new block of claims called the NEWMAN-

16 Group. The NEWMAN-16 Group has a new (2008) south grid (half of the block was

grided), the baseline was established from the number 4 comer post for a distance of 800

meters east to the 800 meter line post towards the number 1 comer post . For the purpose of

this report, the new south grid was used in this section of the claim, to identify the geological

and topographical features noted in this survey. In the remaining half east of the grid all

comer posts, line posts and claim lines as well as access trails as tie-in points for the Magusi

River, creeks, ponds, outcrops, vegetation boundaries and glacial eskers for this survey. There

are has been no stripping or drilling noted in by pervious owners. One third of this block of 16

units has been timbered in 2007 (winter) in the early 2000.

The traversing around this block of 16 units was extremdy difficult due to the extreme wet

conditions and the timbering operations of 2000. Due to the amount of second growth

covering the claim block north and south of the Magusi River. For the south section of the

block, south of the Magusi River a small 4 wheeler trail was used for access.

Geological Survey was contracted out to Miss Wendy K. Well{:r. All drafting and

contouring and report writing was done by Miss Wendy K. Weller.

Finalization of the report and all assessment data forms were completed by Mrs. Gerry

Perron.


LOCATION AND ACCESS

The claim group consists of (16) units of contiguous unpatented mining claims located

in the southwest part of Holloway Township. Access to the property is via the Harker

Holloway access road and a secondary mining road which goes parallel to the Harker-Elliott

boundary.

The NEWMAN-I6 Group is found in the Larder Lake Mining Division, and they are

within the jurisdiction of the Kirkland Lake Resident Geologist. Access is from Kirkland

Lake towards the east for 13 kilometers to the Harker-Holloway road (Highway 672). Follow

672 north for 49 kilometers to Highway 10 I.East on Highway 101 to a timber access road at

Holloway Lake than south to the extended winter logging road (4 wheeler accessible) that

crosses the new west baseline and south grid.

Ownership of the claims has been attested to by Tiger Gold Exploration Corporation,

103 Government Road East, Kirkland Lake, Ontario, and was not independently ascertained

by the writer.

PROPERTY HISTORY

At present time, the first survey completed on the NEWMAN-16 GROUP, by Tiger

Gold Exploration Corporation, was a detail magnetometer and vlf. Survey done last

October/November,2008 and approved by the ministry.

-;ii;) -

FIGURE Ie - TABLE OF LITHOLOGY

1953

CENOZOIC RECENT: PLEISTOCENE:

PRECAMBRIAN KEWEENAWAN:

MATACHEWAN:

ALGmIAN:

PRE-ALGOMAN:

KEEWATIN:

\ 'olcanics:

Sediments:

North Half of Holloway Township

Table of Formations

Peat: stream deposits. Sand, gravel, boulders; varved clay.

Great unconformity

Quartz diabase.

Intrusive c01ltact Quartz diabase, diabase.

Intrusive c01ltact Feldspar porphyry; felsite; lamprophyre.

Intrusive am/act Diabase, gabbro; peridotite and dunite (serpelltillized); p~Tu.\:ellite.

Intrusive contact

{

'Rhyolite; rhyolite agglomerate and tuff. Andesite, basalt; pillow lava; diabasic lava; spherulitic la\'a; frag

mental lava (flow breccia or agglomerate); tuff and chert; talcchlorite schist; carbonate-chlorite schist.

Faulted contact Greywacke; slate; conglomerate; iron formation.

Geological survey - N-16 by Wendy Weller Page 6

REGIONAL GEOLOGY

The O.D.M. Annual Report, being Vol. LXII, Part 7, 1953, tith:~d Geology ofthe North

Half of Holloway Township by J. Satterly only covers the north part of the township and does

not describe at all any part of the south half in which the property O(;curs. From the report,

only a general description can be made of the geology and related topographical features.

The underlying bedrock is Precambrian, and is composed of magnesium rich and iron

rich tholeiitic basalts and andesite. These rocks are dark green to black and grey to green

flows. The trend of these flows appear to be northeast to southeast direction. The area of the

claim block occurs on the north side of the contact between the Upper and Lower Blake River

Group.

The contact with the overlying Blake River Group (upper and lower groups) can be

defined from air magnetic data, however a zone of vertical gradation up to a mile wide mayor

may not be present.

Blake River Volcanic Rocks are composed of calc-alkaline minerals. Massive and

pillow flows occur in sequence with pillow and pyroclastic breccia and lapilli and ash tuff.

Chemically they represent rhyolite, dacite, andesite and basalt. Rocks of the Blake River

Group underlie the base metal camp of Noranda, Quebec. Eastern Clifford and Ben Nevis

Townships have several base metal showings as well as relatively more bed rock exposures

then has the Elliott Groups.

ECONOMIC GEOLOGY

For the Blake River Group, a megacauldron has been defmed which occupied what is

now the central part of the Blake River Synclinorium. Within such a large feature, the sense

of vent vs.proximal vs. distal positioning becomes rather vague. The three will have


completely inter-fingered with each other through time. In general, base metal deposits form

in proximal to vent areas. Stratiform gold deposits are likely to be found in distal regions.

Holloway Township is known for gold occurrences, they are located along margins of

alkaline rocks (Jensen, 1978). Alteration is present in shear zones, and fractures which

contain quartz, epidote, calcite, chalcopyrite, pyrite and specular hematite.

TOPOGRAPHY

The easterly flowing Magusi River occupies a marked regional depression in the south

section of the property. From the north side of this valley the rock rises to flat topped rock

hills which occupy the northern part of the group of properties that this block of 16 belongs to.

The area is largely drift covered (clay, boulders) with numerous low rounded rocks projecting

a few feet above the overburden. In the center section of the west sidt: of the new grid a large

glacial esker is noted that runs south/east. East of the m:w grid, the area is flat to a gentle

south slope towards the Magusi River.

There are three large drainage creeks that drain south into the Magusi River. These

creeks are found at the bottom of steep (clay) ravines. These bottoms may possibly be the

topographic expression of north-south fault zones. The relief over this block of claims does

not exceed 50 to 75 meters. Erosion due to timbering operations ,md natural erosion has

exposed small outcrop showings throughout the block.

A quarter of the property was timbered out in 200012007. In these areas a very thick

second growth of alder, willow, poplar, birch and maple stand. Three quarters of the

remaining vegetation is thick/wet spruce bog. Very thick sections of allder/poplar surround the

Magusi River and the 2 main creeks that feed the Magusi River.


2009 NEWMAN-16 (SIXTEEN MINING CLAIMS)

GEOLOGICAL SURVEY

OBSERVATION OF FIELD RESULTS

Within the boundaries of the property (N-16) the rocks consist of the Keewatin type

Volcanics of Archaean age. The volcanic fonnations have a general e:ast-westerly strike with

steep dips of 180 to 185 degrees to the south.

-1.Pillow Lava Deposits (2) within the magnesium-rich sequences are of basalt composition.

Description: Dip angle 180 degrees - 183 degrees

Fresh face- dark to light green

Weathering colour -light green, to rust brown

On the weathered surface, the edges show a lighter colour than the matrix.

Many of the blocks are large portions of broken pillows.

Salvages - ranges from 1 inch to 2 inches in thickness, quartz filled with epidote

stringers, pillows tightly packed together, locally phenocrysts of plagioclose up to 1-2 cm. in

dimension are concentrated in the pillows outer limits.

2a Andesite Description:

weathered - dark green

fresh face - light green

grain size - fine to medium


Containing 10 to 15% homeblende with some chlorite. The feldspar ground mass has

been largely altered to secondary mineral of which epidote appears to be the most common.

~Flow Top Breccia !Pillow Breccia (2b) within the magnesium-rich sequences are of

basalt composition.

Description: Colour - dark green to black, Weathering colour - dark brown,

fine grained, intense fraturing - 50 degrees to 58 degrees

Irregular patches of epidote with spider quartz stringers, non magnetic

A closely spaced series of brecciated and fragmental flow tops with similar appearance to

dacite. The fragments range in size from one-sixteenth of a inch to a inch. The fragments

have been fractured and re-cemented with lava material.

Samples have been taken for whole rock analysis.

CONCLUSIONS:

This fall the remaining east section of the new south grid will bt~ established for the

purpose of running a magnetometer and electromagnetic surveys. At the completion of these

surveys all information will be pooled for further investigation of the ground.

Respectfully Submitted

August 27,2009

Miss Wendy K. Weller

Agent! Land Manager/ Geo-tech.

Geological survey - N -16 by Wendy Weller Page 10

REFERENCES

Ontario Geological Survey - Miscellaneous Paper 123

Geology and Petrogenesis of the Archean Abitibi Belt

In Kirkland Lake Area, Ontario

J.S. Jensen and F.F. Langford 1985

Sixty Second Annual Report of the Ontario Department of Mines

Vol. LXII, Part VII, ]!953

Rocks and Minerals of Ontario

Geology of the North Half of Hoilloway Township

J. Satterly

Hewitt, D.F. and Freeman, E.B.

Rocks and Minerals of Ontario, Ont. Dept. Mines and

Northern Affiars, GC13, 145p.


ASSESSMENT DATA FORM

Type of Work:

Prospecting:

Physical: GEOLOGICAL SURVEY

Geochemical:

Assay/Analyses:

Cost of Work: $3,106.00

Recorded holder:

Name:

THE PERRON GOLD CORP.

Geological: NEWMAN-16 GROUP

Drilling:

Other Work:

Dollars applied: $3,1.06.00

Survey Company:

Name: TIGER GOLD EXPLORATION

CORPORATION


Address: 103 Government Road East Kirkland Lake, Ont. P2N 1 A9

Survey/Report Information:

Start of work: July 13,2009

Draughting time: July 23,25/09

Completion of report: July 27, 2009

Author: MISS WENDY K.WELLER

Work performed on claims: L-4225382

Work applied to claim(s):

PLEASE SEE ASSEMENT DATA FORM

Address: 103 Government Road East Kirkland Lake, Ont. P2N lA9

End of work: July 20, 2009

Report time: July 26,27/09

Persons who performed work (supervisor first):


WENDY K. WELLER

Mrs. Gerry Perron (secretary)

Page 11

Geological survey- N-16 by Wendy Weller

CER TIFI CATE

I, Wendy K. Weller, of Virginia town, Ontario, do hereby certify:

1) That I am a Geotech and reside at:

17 Hilltop Crescent Box 252 Virginiatown, Ontario POK 1XO

Page 12

2) That I graduated from the Haileybury School of Mines as a certified

Diamond Driller in 1982. I had a staking license for the past 24 years.

3) That I was employed as a Diamond Driller for Heath and Sherwood for

1 year.

4) That I have been practicing as a Geotech for a period of twenty (23)

years and I am qualified to write this report.

5) That I supervised and participated in this survey.

el7/ / (

Dat / OJ

Wend K. feller

Geotechl AgentlLand Manager

\

! \ (

- • • u { ~ ..

I ,

I i ....

I

: I

, I

I \ ~/ { ~ I ___ .1.-/" I

If 1

-I. i " - ... ..

. I

\ . ..... .

'. I

\ V' , /.

14 \ . /.

I '~'t/

v

- - ) --

---- c::' -r I

, ';> "-

... ..

- . - - -\ - -

" 4-/ \ <:

7

/ //-"\ (/ "'- /'

+ l !

;1/

SYMBOLS

Claim Post ~ Line Post ,. Claim line __ _

Traverse Line ~')

Vegetation Boundary ,/"" ., ;J , i

", .-, Access Trail •• / '" F our wheeler trail ," ' " .

Spruce1~- Pine .1- Alder ,;/:

Poplari' Birch i.o.~

Outcrop / -:; Ground elevation .,:-" ... ,. '" . . :~ ~~ ~-.

LEGEND

Pleistocene Gravel, sand, alluvium peat and clay

EARL Y PRECAMBRIAN i Early Precambrian . I

. Upper Blake River Group j

2 - sequences are of basalt composition I Pillow Lava Deposits within magnesium-rich 2a - Andesite

2b - Flow top BrecciaIPillowed Breccia

NEWMAN-16 BLOCK HOLLOWAY TOWNSHIP LARDER LAKE MINING DIVISION

SCALE 1: 5000m v

t I 0 0 ~c, ?..Oo~-Vi

_J_l - t Report by: Miss Wendy K. Weller

Map No. N-16/2009/geo

I '

- - ~- "Y _ ' - .•. - _ _ , • •.• _ J 1

GEOLOGICAL SURVEY LARDER LAKE MINING DIVISION FOR · Claim 4225382 is located in Holloway Township,...

Documents

Transcript of GEOLOGICAL SURVEY LARDER LAKE MINING DIVISION FOR · Claim 4225382 is located in Holloway Township,...