geol rpt of the transway prop klotz lake...42f13sw8824 63.435* klotz lake 010 geological report of...

42F13SW8824 63.435* KLOTZ LAKE 010

Geological Report of the Transway Property

Klotz Lake

Mining District of Thunder Bay, Ontario

By Eddy Canova,

Geologist.

January 1984.

42F13SW0824 63.4350 KLOTZ LAKE

TABLE OF CONTENTSO10C

GEOLOGY

REGIONAL GEOLOGY.

LOCAL GEOLOGY.

ECONOMIC GEOLOGY.

DONE

ION...................................

tfDATIONS

X: Table I and Table II...............

. . . . . . . . . . . . . . .p.

. . . . . . . . . . . . . . .p.

. . .. . . . . . . . . . . .p.

...............p.

...............p.

...............p.

........ .......p.

. . . . . . . . . . . . . . .D.

333578

911

p.2

INTRODUCTION

The Transway Property located in the Mining District of

Thunder Bay flanks the eastern boundary of the Banque-Or Property.

It is approximately 50km east of Long Lac along the Trans Canada

Highway 11 .

The property consists of 24. claims investigated during the

period of Oct.24 and Dec.15* 1983. Line cutting, Mag and Horizon

tal Loop EM were carried out between Oct.24 and Dec. 15. Mapping,

soil geochemistry, outcrop stripping, detailed mapping and channel

sampling were subcontracted to a Geological Consultant during the

period of Nov. 6 to Nov. 30.

This geological and geophysics program consisted in outlining

and following up the diorite contact with the weakly foliated

basalts-pillow basalts. Silicification and quartz veinihg occur

ring at or close to the diorite-basalt contact is considered impor

tant, since gold occurrences on the Banque-Or Property occur at the

diorite-basalt contact.

P.3

GEOLOGY

REGIONAL GEOLOGY

The Klotz Lake area is within an east-west to southeast

trending early Precambrian metavolcanic metasedimentary sequences

of the Wabigoon Subprovince. The metavolcanic-metasedimentary

sequences have been intruded by felsics and lenticular mafic intru

sions. Cutting all the units are Proterozoic diabase dykes and

sills.

LOCAL GEOLOGY

The Transway Property has east-west to southeast trending

mafic to intermediate metavolcanics. The metavolcanics are intru

ded by diorites, differentiated diorites to gabbros, and diabase

dykes.

Most of the Transway Property is covered by Archean mafic

volcanics. These consist of dark green, fine to medium grained,

equigranular, weakly magnetic to non-magnetic basalt flows and

pillow basalts. Pillows are well outlined in a few localities,

i.e., the west part of the property. Pillow edges are defined by

the presence of calcite, epidote, and plagioclase veinlets. It

appears that tops could be to the south. This thick basic volcanic

pile is occassionally coarse grained, equigranular with interlock

ing crystals, and they may be confused for gabbros. Quartz veins

or veinlets are not frequent in this thick volcanic pile. How

ever, veining is more abundant close to the intrusives. Pyrite is noticeable in trace amounts and rarely up to 3-4-^.

Lithological changes in the mafic volcanic pile are not fre

quent however they are noticeable where outcropping is of higher density(Refer to the MapI). One unit is a dark green foliated,

medium grained amygdaloidal basalt with ^-2% pyrite and weakly

magnetic. The amygdules are round, 1/2 cm in size, consisting of

quartz and calcite, and comprising 10# of the rock. Another unit

is a mafic agglomerate that is approximately 25m thick, has traces

of pyrite and 1 to 2cm angular mafic volcanic fragments. The unit

p./t,

is hard, silicified and has been recrystallized due to deformation

and metamorphism. There are sections in the volcanic pile which

have a lighter color index, have more plagioclase and may be ande-

sitic. The andesite is lighter green, hard , foliated with bands

of plagioclase, epidote and calcite paralleling the foliation,

and with ^-2% pyrite.

At the southwest corner of the property is a grey, fine grain

ed, hard, well foliated, siliceous intermediate volcanic dacite.

The dacite has fine to medium sized quartz eyes(*1mm), pods of

quartz and feldspar, few narrow quartz veins and 1? pyrite. How

ever at times the rock unit appears to be a fine grained, biotite bearing mica schist(metasedimentary).

At the western end of the claim, group is an extension from the

Banque-Or Property of a massive, non-magnetic, medium grained

diorite tongue trending southeast. The diorite consists of equi granular crystals of plagioclase, K-feldspar, and hornblende

distributed homogeneously, and with J\*lo pyrite. The massive, homo

geneous diorite has block jointing; however* at the contact,- with

the basalt, the diorite is foliated, the feldspars are weakly al

tered, silicification and quartz veining is more frequent. De

formation of the diorite; eg. stripped outcrop II(Refer to Mapl),

has given rise to shearing, folding of the foliation and boudinage

of quartz veins. Pyrite is abundant in such veins, ranging from

1-105&. These shear zones, in which quartz veins occur, trend 116 and dip 60 0 SW. The diorite-basalt contact is visible in several

places and is.displaced at one location by a southwest trending

fault.Just east of the diorite is a north-south trending dyke which

is approximately 50m wide and traced for 1km on the property. The

dyke is dark green, medium grained( i2mm), massive, equigranular,

weakly to strongly magnetic, friable and oxidized in places, and

interlocking grains in what appears to be a differentiated diorite to magnetic gabbro. Texturally,this magnetic gabbro dyke is not a

diabase dyke. The gabbro consists of 45-50^ plagioclase, ^4.0/S

amphiboles and pyroxenes, '\-2'][, pyrite, 5-7# magnetite, and 31 ac

cessories. The dyke is most probably easily traced with the mag-

p.5

netic survey.

At one outcrop a magnetic diabase dyke approximately 2m wide

cuts the basalts at approximately 49*. The diabase is black, fine

to medium grained, massive, has fine plagioclase laths and traces

of pyrite.

At two localities(LCH70E7UON 4 L8E/410N) there is a quartz

feldspar porphyry vein and a quartz feldspar porphyry subangular

boulder. The porphyry is whitish-green, fine to medium grained

and has traces of pyrite.

Structurely the units trend approximately 110* and dip 70*to

80*south, and the foliation varies between 90*and 130*and dips 70*

to 80* south. Shearing in the diorite trends HO* and 60* and dip

60* SW and 81* SE respectively. Faulting occurs along generally

two directions; one is at 210 and the other between 11 O* and 130*.

The faults have disrupted and exposed the diorite and gabbro dyke.

Another feature noticed at the stripped outcrop II is boudinage of

the quartz veins. This indicates tensional and compressional for

ces during deformation.

ECONOMIC GEOLOGY

A few quartz veins cut the thick basalt volcanic pile. These

are narrow, approximately 2cm, trending 120 to 130 and with 1-25?

pyrite. These veins might not carry any gold.

Closer to the diorite-basalt contact and occurring within both

the diorite and basalt, are wide and more extensive quartz veins.

Quartz veins vary between 30 and 150cm, and extend for several tens

of meters. The veins are weakly oxidized and have from 2 to ^0%

pyrite in certain veins. The advent of the diorite intrusion may

have given rise to silicification and quartz veining by supplying

geothermal heat required for the percolation of hydrothermal

fluids. These fluids have the capability of carrying and remobi-

lizing gold into favorable structures, hence, these quartz veins

may carry gold.

Two areas were stripped for further investigation of the

quartz veins. Stripped outcrop l(Refer toMapI) has several quartz

p.6

veins occurring over a width of 50cm and trending 89" in a fine

grained basalt. The veins contain approximately 5^ dessiminated

to massive pyrite. Two channels were cut and six samples were sent

for gold assaying. Stripped outcrop II (Refer to Mapl), of much

larger dimensions, is a diorite which has several irregular quartz

veins varying between 10 and 150cm. The quartz veins generally

trend 60 and 130, and have 2-3^ pyrite except in one vein '\Q'fc py

rite is present. The quartz veins have been injected through de

formed sections of the diorite. Four channels have been cut and

twelve samples have been sent in for gold assaying.

.

p.7

SURVEYS DONE

Two hundred and twenty-three soil samples of the B horizon

were collected along lines 0,1,2,3.4*5,6, and VE. These were all

analyzed for gold. Each sample has been listed on Table I (Refer

to Appendix) and plotted onto the Map II.

Rock samples of various lithologies and quartz veins mineral

ized with pyrite were sampled. These rock samples and channel

samples were analyzed for gold. Each sample is listed on Table II (Refer to Appendix) and plotted onto the Maps I and II.

Other surveys done were Mag and Horizontal Loop EM. Results

will be plotted geophysics maps.

p.8

CONCLUSION

The Transway Property, geologically speaking, consists of a

thick volcanic pile of basalts intruded by an east-southeast

trending diorite tongue extending from Banque-Or's Property into

Transway's. The basalts are also intruded by a north-south trend

ing magnetic gabbro dyke and a northeast trending magnetic dia

base dyke. Wherever the basalt has been intruded by the diorite,

silicification and quartz veining has resulted along the contact,

within the basalt and also within the diorite. The quartz veins

vary in size from 10 to 150cm and are mineralized with 2 to 105?

pyrite. These hydrothermally injected quartz veins may signify

the presence of gold. The diorite may have helped remobilize any gold present in minor quantities within the basalts and reconcen-

trated it in quartz veins at the basalt-diorite contact or even

within the basalts, eg. stripped outcrop I. Hence, these quartz

veins at the stripped outcrop I and II, and at the basalt-diorite contact are interesting drilling targets for gold.

Also of relavent interest for drilling targets are the basalts

occurring between the diorite and gabbroic dyke, eg. stripped out-itf-

crop I. Here the basalts overly the diorites and hence remobili-zation may have taken place within the basalts. There may then

be more quartz veins than those seen at surface at the stripped

outcrop I. Quartz veining does also occur close-by to the gab

broic dyke, eg. sample EC-256. This area may be considered as a

possible drilling target all depending upon the assay results from

the grab sample and from the soil samples.In conclusion, three areas are considered as possible drilling

targets, because of frequency of quartz veining, abundance of

pyrite and proximity to diorite. These are:

1) To drill the north basalt-diorite contact.2) To drill the quartz veins within the diorite at the

stripped outcrop II.

3) To drill the basalt just overlying the diorite, eg.

stripped outcrop II.

P.9

RECOMMENDATIONS

1) Remap in detail the diorite-basalt contact.

2) Detailed prospecting for quartz veins at the basalt-

diorite contact, in the diorite, in the basalt close to the diorite

and at the gabbro-basalt contact.

3) Further stripping at the stripped outcrop I, detailed

mapping of it and channel sampling.

4) Proper cleaning of the stripped outcrop II, mapping of

any other quartz veins and further channel sampling.

5) Channel sampling of the quartz vein located at 55N and 330E, eg. sample EC-256.

6) Drilling of three proposed targets: a) the basalt-diorite

contact, just north of the stripped outcrop II, b) quartz veins in

the diorite, eg. stripped outcrop II, and c) drilling the basalts overlying the diorite, eg. stripped outcrop I.

p.10

CERTIFICATE

I, Eddy Canova, certify that:

a) I am a practicing professional geologist

residing at 4682 Robert Boul., in St. Leonard,

Quebec.

b) I graduated in 1977 from McGill University.c) I am a member of the Mineralogical Associa

tion of Canada, Association of Engineering

Geologists and Prospectors.

d) I do not have any direct or indirect interests

in the company Transway Exploration Ltd., and I

do not hope to receive any interests, either

directly or indirectly.

Eddy Canova,

Geologist.

p.11

APPENDIX

TABLE I

SOIL GEOCHEMISTRY

ABBREVIATIONS FOR TABLE I

Vegetation

B.F.Ce.Bi.Po.Sp.T.A.J.P.

Relief

Balsum FirCedarBirchPoplarSpruceTag AldersJack Pine

Ba. BasaltDac. DaciteDi. DioriteGab. GabbroGd. GroundGl. GlacialSt. SteepN,S. North, SouthE,W. East, West

Moisture Content

D. M. W.

DryMoistWet

Soil Type

Pe, Sa, Si, CI, Or,

PebblesSandSiltClayOrganics

Grain Size

Fi. FineMe. MediumCo. Coarse

Color

Br. Bl. Gn. Go. Gr. Re. Ta.

BrownBlackGreenGoldenGreyRedTan

Ye. Dr. Li.

YellowDarkLight

SampleNumber

83SB201

83SB202

83SB203

83SB204

83SB205

83SB206

83SB207

83SB208

83SB209

83SB210

83SB211

83SB212

83SB213

83SB2U

83SB215

83SB216

83SB217

83SB218

83SB219

83SB220

83SB221

83SB222

83SB223

m

Station

760S 600E

Vegetation

BF.Ce.

780S 600E SF,8i,Ce.i

800S 600E BF,Bi,Po.

820S 600E

8403 600E

860S 600E

880S 600E

900S 600E

920S 600E

940S 600E

104.0S 700E

1020S 700E

1000S 700E

980S 700E

960S 700E

940S 700E

920S 700E

900S 700E

880S 700E

860S 700E

840S 700E

820S 700E

800S 700E

BF,Po.

BF,Po,Sp.

BF,Po.

BF,Bi,Po,Sp.

BF,BI,Po,Sp.

Bi,Po,Sp.

Bi,Sp.

Sp.

Sp.

Sp.

JP.Sp.

JP,Sp.

JP.Sp.

JP,Sp.

Bi,JP,TA.

Po,Sp,TA.

Sp.

Sp.

Sp.

Sp.

Relief

Flat.

Flat.

MoistureContent

W

W

Gd Rising W.

Gd Rising W.

Gd Rising W.

Gd Rising W

Gd Rising W.

Flat.Dac.O/C E.

Flat.Dac.O/C.

Flat.Dac.O/C.

Flat, Gl. Till.

Flat, Gl. Till.

Flat, Gl. Till.

Flat, Gl. Till.

Flat,Dac.07C W.

Flat.Dac.O/C W.

Flat,Dac.07C W.

Flat,Dac.07C W.

Flat, Gl. Till.

Flat.

Flat.

Flat.

Flat.

M

D

D

D

D

D

D

D

D

M

D

D

D

D

D

M

M

M

W

M

M

Soil Type

Or.80%C1.207,

Sa.95*Pe.5*

Sa.95#Pe.5^

Sa.85^Pe.15^

Sa.955SPe.555

Sa.95#Pe.55?

Sa.85#Pe."IO^Si.5#

Sa.85#Pe.10*Cl.5JG

31=65/^1=355?

Sa.60jKSi.355fC1.55K

Si.90^Sa.10^

Si.8055Sa.205S

Si.90^Sa.1055

Si.9555Sa.555

Si.95?Sa.5^

Si.955?Sa.555

Si.9055Sa.1055

Si.9555Sa.555

Si.9055Sa.10^

Si.95^Sa.555

Or.8055C1.20^

Si.9055Cl.1055

Si.90?Cl.1056

GrainSize

Or.

Pe.Co.Sa.

Pe.Co.Sa.

Pe.Co.Sa.

Co.Sa.

Co.Sa.

Pe.Co.Sa.

Pe.Co.Sa.

Si.

Fi.Sa.

Si.

Si.

Si.

Si.

Si.

Si.

Si.

Si .

Si.

Si.

Or.

Si.

Si.

Color

Bl.

Br . iiBr. iBr.

Ru.Br.

Br.

Br.

Br.

Gr.

Gr.

Li.Br.

Li.Br.

Ru.Br.

Li.Br.

Li.Br.

Ru.Br.

Ru.Br.

Li.Br.

Li.Br.

Li.Br.

Bl.

Li.Br.

Li.Br.

TABLE II

ROCK SAMPLE LOCATION AND DESCRIPTION

SampleNumber

EC-250

EC-251

EC-252

EC-253

EC-254

EC-255

EC-256

EC-257

EC-258

EC-259

EC-260

EC-261

EC-262

EC-263

EC-264

EC-265

EC-266

EC-267

EC-268

EC-269

EG070

Location

695N 304E

209N 302E

206N 297E

199N 296E

59N 292E

66N 299E

55N 325E

BL 316E

70S 293E

72S 272E

396S 306E

356S 222E

100S 215E

69N 296E

84N 292E

1075N 156E

542N 134E

479N 94E

140N 71E

108N 109E

655N 122E

Rock Description

Basalt with 1cm quartz veins ft epidote.

Quartz vein with epidote, oxidized, sheared, 6 injected with a small diorite vein.

Medium grained, massive diorite.

Amygdaloidal basalt, weakly oxidized.


Recrystallized pillow basalts.

Quartz vein ft pods in a basalt.

Weakly magnetic, weakly oxidized basalt.

Medium grained, altered, friable diorite.

Medium to coarse grained, recrystallized basalt withn 3mm amphiboles.

Medium grained pillow basalt.

Medium grained, porphyritic diorite.

Foliated basalt.

Fine grained, massive basalt.

Foliated diorite, altered feldspars, quartz veinlets, and in contact with basalt.

Fine grained, magnetic, weakly foliated pillow basalt.

Medium grained, magnetic basalt.

Medium grained, weakly foliated basalt, with a few quartz veins.

Fine to medium grained quartz-feldspar por phyry, 172m wide, cutting pillow basalt.

Weakly foliated diorite .altered feldspars, and has quartz veins.

Medium grained, weakly magnetic basalt.

Mineralization

'{-2'}, Py.Dessiminated±21 Py.

li Py.Dessiminated*4?Py. Blebs.

1-2* Py.

Trace Py.

±21 Py.*3* Py.Trace Py.

Trace Py.

Trace Py.

Trace Py.

Trace Py.

Trace Py.

4* Py.*4* Py.

Trace Py.

21 Py.

-2* Py.Dessiminated

.AssayRe suits (

SampleNumber

EC-271

EC-272

EC-273

EC-274

EC-275

EC-276

EC-277

EC-278

EC-279

EC-280

EC-281

EC-282

EC-283

EC-284

EC-285

EC-286

EC-287

EC-288

EC-289

EC-290

t

Location

259N 30E

161N 56E

82N 16E

99S 63E

100S 68E

108S 33E

112S 22E

86N 1UE

120N U5E

116N U7E

110N USE

89S 100E

17N 217E

42N 222E

38N 168E

67N 181E

72N 183E

120N 208E

621N 406E

169N 462E

Rock Desription

Weakly magnetic pillow basalts.

Fine grained, weakly foliated basalt, veinlets of quartz and feldspar, weakly oxidized.

Weakly foliated diorite, cut by quartz-feld spar veinlets.

Medium grained diorite.

Chloritized, weakly oxidized diorite in contact with basalt.

Medium grained, recrystallized, silicified basalt.

Weakly oxidized quartz vein in basalt.

Wide, irregular quartz vein in diorite.

Weakly magnetic, recrystallized, silicified and chloritized basalt.

Foliated diorite, silicified and some calcite.


Foliated diorite close to basalt contact.

Several quartz veins over 172m in a basalt. Veins are oxidized.

Silicified basalt with a few quartz veins.

Recrystallized basalt close to diorite.

Medium grained fi massive diorite.

Fine grained recrystallized basalt.

Oxidized quartz vein in basalt.

Foliated, weakly magnetic basalt, few quartz veins.

Medium grained recrystallized basalt.

Mineralization

Trace Py.

Trace Py.

*21 Py.

*21 Py.Trace Py.

±21 Py.Trace Py.

±21, Py.

Trace Py.

Trace Py.

-51 Py. Massive ft Dissiminated .

21 Py.

-31 Py.-21 Py.

Assay Results(

SampleNumber

EC-291

EC-292

EC-293

EC-294

EC-295

EC-296

EC-297

d/Sal

Cl7Sa2

Cl7Sa3

02/Sal

C27Sa2

C27Sa3

C27Sa4

C27Sa5

C37Sa1

C37Sa2

C37Sa3

C47Sa1

C47Sa2

Location

174S 363E

378S 394E

390S 359E

404S 361E

927S 571 E

530N 500E

137N 253E

18N 21 7E

17. 5N 217E

17N 217. 5E

84. 5N 142E

85N 142E

85. 5N 142E

86N 142E

87N 142E

17.5N214-5E

17N 214.5E

16. 5N 215E

82N 143. 5E

82N U3E

82N 142. 5E

Rock Description

Medium grained, equigranular, massive, weakly magnetic gabbro.

Strongly magnetic, oxidized gabbro.

Strongly oxidized, recrystallized basalt.

Foliated basalt, oxidized along joints.

Grey, fine grain, foliated, siliceous dacite.

Weakly magnetic, chloritized basalt with fine veinlets of quartz-feldspar.

Oxidized basalt with a few quartz veinlets.

Fine to medium grained basalt, sampling 50cm.

Oxidized quartz veins with a few interlayers of basalt, sampling 50cm.

Basalt, sampling 50cm.

Diorite 6 quartz contact, diorite weakly foliated at contact, sampling 50cm.

Fractured white quartz vein, sampling 50cm.



Diorite fi quartz-diorite contact, sampling 60cm.


Quartz veins with some interlayers of diorite Sampling 40cm.


Northeasterly sheared ft foliated diorite, sampling 50cm.

Fractured smokey quartz vein, sampling 50cm.

Sheared 6 foliated diorite with a quartz pod, sampling 50cm.

Mineralization

Trace Py.

Trace Py.

21, Py.

Trace Py.

Trace Py.

22 Py.

Trace Py.

Trace Py.

-52 Py.Dessiminated or as stringers.

Trace Py.

-12 Py.

-32 Py.Dessiminated.

12 Py.12 Py.*12 Py.

Trace Py.

-52 Py. Massive or Dessiminated .

Trace Py.

12 Py.

2-32 Py.Dessiminated

12 Py .

Assay Results(

SampleNumber

Location Rock Description Mineralization Assay Results(

05/Sal

C57Sa2

06/Sal

C67Sa2

S-2

86.5N 138E

86N 138E

102N 1UE

101 .5N1UE

86N 137.5E

Weakly oxidized diorite, sampling 50cm

20cm quartz-feldspar vein, sheared 4 foliated diorite, Py. occurs along contact, sampling 50cm.

Medium grained, massive diorite,sampling 40cm

5cm quartz vein in weakly oxidized diorite, altered feldspars, sampling 30cm.

20cm quartz vein in a sheared ft foliated diorite, grab sample beside channel 5.

"\-2l Py.Dessiminated

3* Py.

-1* Py.-31 Py.Dessiminated.

10-15/& Py.Massive, along contact.

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t/i LO

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SampleNumber

83SB051

83SB052

83SB053

83SB054

83SB055

83SB056

83SB057

83SB058

83SB059

83SB060

83SB061

83SB062

83SB063

83SB064

83SB065

83SB066

83SB067

83SB068

83SB069

83SB070

83SB071

83SB072

83SB073

83SB074

83SR075

Station

180S 200E

160S 200E

UOS 200E

120S 200E

100S 200E

SOS 200E

60S 200E

4.0S 200E

20S 200E

10S 200E

BL 200E

10N 200E

20N 200E

30N 200E

4.0N 200E

50N 200E

60N 200E

70N 200E

SON 200E

90N 200E

100N 200E

11 ON 200E

120N 200E

UON 200E

150N 200E

Vegetation

Sp.

Bi,Po,Sp.

Bi,Sp.

Sp.

Sp.

Sp.

Sp.

Sp.

Sp.

JP,Sp.

JP,Sp.

JP,Sp.

JP.Sp.

JP,Sp.

JP,Sp.

JP,Sp.

JP,Sp.

Jp,JP.JP.Bi.JP.JP,Sp.Bi, JP.

JP.JP.

Relief

Gd Rising N,Ba 0/C.

Gd Rising N,Ba 0/C.

Gd Rising N.Ba 0/C.

Top of Ridge, Sloping W,Ba 0/C.



Sloping N,Ba 0/C.

Ba 0/C.

Ba 0/C.

Ba 0/C.

Flat.Ba 0/C * Qtz.Vn.

Flat,Ba 0/C * Qtz.Vn.

Sloping N,Ba 0/C.

Sloping N,Ba 0/C + Qtz.Vn.

Flat.Ba 0/C, Contact Ba-Di NW.

Flat,Ba O/C.Contact Ba-Di N.

Flat,Ba 0/C, Contact 5m NW.

0/C, Contact Ba-Di.

Sloping N.O/C, Contact Ba-Di.

Flat,Ba 0/C S.

Flat,Ba 0/C N.

Flat,Ba 0/C N.

Flat.Ba 0/C.

Flat.Ba 0/C. .

Flat,Ba 0/C.

MoistureContent

MT\ U

D

D

D

M

M

D

M

M

M

D

D

M

W

W

No

No

No

D

W

M

W

No

D

Soil Type '

Si.35?Or.35#Ci.30g

GrainSize

Si.

i 01. /5JwSa.15#Pe.5'sCl.5/? Pe . Si .^n 'TO^CIa O K, "f r 1 ea! "J -L * l W A'Oa . f. j /o L/X . j ja

Si.70*Sa.25JfC1.55fQ -i 70 ' S! Q*a ^ c tff r* ~\ c oftJJ.* fVy/jQci.rfC^/y'-'-L-P/b

Sa.65JfSi.30JfCl.5JfSi.755fSa.20JfCl.55fSi.65J6Sa.25JfClitOJfSi.80JfSa.15?Cl.5JfSa.60JfSi.35JfCl.5JfOr. 100^

Si.80JfSa.15JfCl.5Jf

Sa.65JfSi.30JfCl.5JfSa.655fCl.255fSi.10JfSi . 40^C1 . 35%0r=25%8a=3%

Sample. On Outcrop.

Sample. On Outcrop.

Sample. On Outcrop.

Sa.80#Pe.10j5Si.10#

Sa.70JgSi.20#Pe.10Jf

Si.655fC1.35Sf

Si.50JfCl.35JfOr.15Jf

Sample. On Outcrop.

Sa.85#Si.10#Pe.5#

Si.

Si.

Si.

Fi.Sa.

Si.

Si.

Si.

Fi.Sa.

Or.

Si.

Fi.Sa.

Fi.Sa.

Cl-Si.

Pe.Co.Sa.

Pe.Co.Sa.

Si.

Si.

Me-Co.Sa.

Color

Dr.Br.

R e . 3 r . i

Li.Br. l

Re.Br.

Gr.Br.

Li.Br.

Br.

Br.

Li.Br.

Gr.Br.

Li.Br.

Bl.

Br.

Br-Dr.Br.

Dr.Br.

Bl.

Br.

Br.

Dr.Br.

Dr.Br.

Br.

SampleNumber

83SB076

83SB077

83SB078

83SB079

83SB080

83SB081

83SB082

83SB083

83SB084

83SB085

83SB086

83SB087

83SB088

83SB089

83SB090

83SB091

83SB092

83SB093

83SB094.

83SB095

83SB096

83SB097

83SB098

83SB099

83SB100

*

Station

160N 200E

1 SON 200E

200N 200E

220N 200E

245N 200E

260N 200E

260N 100E

240N 100E

220N 100E

200N 100E

180N 100E

160N 100E

150N 100E

140N 100E

130N 100E

120N 100E

11 ON 100E

100N 100E

90N 100E

SON 100E

70N 100E

60N 100E

40N 100E

17N 100E

BL 100E

Vegetation

JP.TP q-r,fj i , w \J .

JP.JP.JP.TA.

JP.

JP.

JP.

Bi,JP,Po.

JP.Po.

JP,TA.

Bi,JP.

Bi, JP.Po.

Bi, JP.Po.

Bi,JP,Po.

Bi,JP.

Bi, JP.

JP.

JP.

Bi.JP.

JP.

JP.

JP.

JP.

Relief

Flat,Ba 0/C S.t\r) s T ^ -; v, ^ M 13 a M 1 r J ̂ 4. i t .i- fcj -L-Li (X, J-lf-Od v^/ W*

Flat.

Flat.Ba 0/C W.

Sloping N,Ba 0/C.

Flat , Swampy.

Flat,Ba 0/C.

Flat.Ba 0/C.

Sloping S,Ba 0/C.

Sloping S,Ba 0/C N.

Flat.

Flat.

Flat.

Gd Rising S, 0/C S.

Gd Rising S, 0/C S.

Gd Rising S, Contact Ba-Di.

Gd Rising S, Contact Ba-Di.

Gd Rising S, Di 0/C.

Top of Ridge, Di 0/C.

Top of Ridge, Di 0/C.

Flat, Di 0/C.

Flat, Di 0/C.

Flat, Di 0/C.

Flat, Di 0/C.

Flat, Di 0/C.

MoistureContent

M

M

D

D

D

M

D

D

D

D

D

M

M

M

M

M

D

D

D

M

W

W

M

W

M

Soil Type

Sa.755SCl.1555Si.1055

Sa.505SC1.30?Si.205S

Si.7555Sa.15/5Cl.1055

Sa.6555Si.2555Cl.1055

Si.6055C1.4055

Sa.8555Si.1055Pe.5#

Si. 70^Sa. 2055C1.1055

Sa.753KSi.20jKCl.55K

Si.75JtCl.155KSa.105f

SiT75JKCl.15JKSa?105K

Si.70JfSa.20jKCl.10jK

Si.70JfSa.20JfCl.10Jf

Sa.60jfSi.35JfCl.55

Si.3555Cl.3555Sa.2555Pe.555

Si.70JfCl.20JfSa.10Jf

Si.60JfCl.20JfSa.20Jf

Si.75JfSa.15SKCl.10Jf

Si.7555Cl.2055Sa.55?

Si.55JfClUOJfSa.5jK

Cl.70JfSa.20JfSi.10Jf

Cl.60JfSi.30jKOr.10SK

Cl.75JKOr.25JK

Si.60jKCl.25JfSa.155K

Or. 60*01.4055

Si.60jKCl.35JfSa.355f

GrainSize

Me . Sa.

Fi.Sa.

Si.

Me.Sa.

Si.

Pe. Fi.Sa.

Si.

Fi-Me.Sa.

Si.

Si.

Si.

Si.

Fi.Sa.

Pe.Si.

Si.

Si.

Si.

Si.

Si.

CI.

CI.

CI.

Si.

Or.

Si.

Color

Br.

Br.

Br.

Br.

Br.

Li.Br.-Ta.

Dr.Gr.Br.

Br.

Br.

Li.Br.

Li.Br.

Li.Br.

Br.

Br.

Li.Br.

Br.

Br.

Br.

Br.

Dr.Gn.Br.

BI.

Dr.Br.

Br.

BI.

Br.

SampleNumber

33SB101

333B1Q2

83SB103

83SB10A

83SB105

83SB106

83SB107

83SB108

83SB109

83SB110

83SB111

83SB112

83SB113

83SB1U

83SB115

83SB116

83SB117

83SB118

83SB119

83SB120

83SB121

83SB122

83SB123

83SB124

83SB125

t

Station

-1 f? r*i j* rt r-*. Tti/o 1 OC.6l. 1 c; -j n p. TTH, ^ i^v i ^ i/ J-J

633 100E

70S 100E

SOS 100E

90S 100E

100S 100E

11 OS 100E

120S 100E

130S 100E

UOS 100E

160S 98E

BL OOOE

20N OOOE

AON OOOE

50N OOOE

60N OOOE

70N OOOE

SON OOOE

90N OOOE

100N OOOE

11 ON OOOE

120N OOOE

130N OOOE

HON OOOE

Vegetation

JP.

JP.

JP.

JP.

JP.

JP.

JP.

JP.

Bi,JP,Po.

Bi, JP.

JP.

JP.

Bi,JP,Po.

Bi, JP,Po.

Bi, JP,Po.

Bi,JP,Po.

Bi,JP,Po.

Bi, JP.Po.

Bi,Po.

Bi,JP,Po.

BF,Bi,JP,Po.

Bi, JP,Po,TA.

Bi, JP,Po,TA.

BF,Po,TA.

Bi, JP,Po,TA.

Relief

Flat, Di 0/C.

Flat, Di 0/C.

Sloping S, Di 0/C.

Sloping S, Di 0/C.

Sloping S, Contact Di-Ba 0/C.

Sloping S, Contact Di-Ba 0/C.

Sloping S,Ba 0/C.

Sloping S,Ba 0/C.

Sloping S,Ba 0/C.

Flat,Ba 0/C.

Flat.Ba 0/C.

Flat,Ba 0/C.

Gd Rising E, Di 0/C.

Gd Rising E, Di 0/C.

Sloping N,Di 0/C E.

Gd Rising E, Di 0/C E.

Flat.

Flat.

Flat, Di 0/C, Contact Di-Ba Nearby.

Flat, Di 0/C E, Contact Di-Ba Nearby.

Flat, No 0/C, Contact Di-Ba Nearby.

Flat, No 0/C, Contact Di-ba Nearby.

Flat, No 0/C.

Flat.

Flat.

MoistureContent

W

D

M

W

M

D

M

W

M

W

M

M

W

W

M

M

D

D

D

M

D

D

D

D

D

Soil Type

Si. 65*01. 35*

Si.70*Sa.20*C1.10*Q ̂ ^LC^CO O^^PI ^ o ̂Ol*D,?^Od.*^C..yAJL'X* i W /o

Si.80*Cl.15*Sa.5*

C1.65*Si.30*Or.5*

Si.60*C1.30*Sa.5*Or.5*

Or. 60*01. 30*Sa^10*Pe^2*

Si. 80*Sa. 10*01.10*

C1.65*Si. 30*Sa. 5*

C1.70*Si.25*Sa.5*

Si.65*Cl.20*Sa.12*Pe.3*

Sa.65*Si.30*Pe.5*

Or. 80*Si. 15*C1.5*c? 4 o r\cf r* ~\ i c of c? ** c ofoi*o\j]fcujL.i:?5doao#ri o tr c^ o .s -i r\ Of r* i c ofoa. op/ooi .lU^ulo/oSi.75*Cl.15*Sa.10*

Sa.85*Si. 10*C1.5*

o 1 * /w/vL/J. * 1 L//&O51 3fOri- f t* gf f*~\ o r\Of o n C Ofbi.op/bOl.jJU/tooa*:)^

Si.85*Cl.10*Sa.5*

Si.90*Cl.10*

Si. 90*01.10*

Si. 90*01.10*

Si. 95*01. 5*

GrainSize

Si.

Si.

Si.

Pe.Me.Sa.

Si.

CI.

Si.

Or.

Si.

CI.

CI.

Si.

Me-Fi.Sa.

Or.

Si.

Co.Sa.

Si.

Me-Co.Sa.

Si.

Si.

Si.

Si.

Si.

Si.

Si.

Color

Gn. 31 .

Li.Br.

Gn.Br.

Li.Br.

Dr. Gn.Br.

Li.Br.

Br.

Bl.

Li.Br.

Br.

Br.

Li.Br.

Br.

Bl.

Li .Gn. Br .

Li.Br.

Br.

Br.

Ye.Br.

Br.

Li.Br.

Ye.Br.

Ye.Br.

Li.Br.

Ye.Br.

Sampljg

Number

83SB126

83SB127

83SB128

83SB129

83SB130

83SB131

83SB132

83SB133

83SB134

83SB135

83SB136

83SB137

83SB138

83SB139

83SBUO

83SBU1

83SBU2

83SBU3

83SB1U

83SBU5

83SBU6

83SBU7

83SBU8

83SBU9

83Saj50

Station

160N OOOE

180N OOOE

200N OOOE

220N OOOE

240N OOOE

260N OOOE

280N OOOE

300N OOOE

100S 400E

120S 4-OOE

UOS 400E

170S 400E

180S 4-OOE

200S 400E

220S 4-OOE

240S 4.00E

260S 400E

280S AOOE

300S 400E

320S 4-OOE

340S 400E

360S 400E

380S 400E

390S 400E

4.00S 4-OOE

Vegetation

Bi, JP.Po.TA.

Bi.JP.TA.

Bi,JP,TA.

Bi, JP.Po.

Bi,JP,TA.

Bi.JP.

Bi,JP,TA.

TA.

JP.

JP.

JP.

JP.

JP.

JP,Sp.

BF,Bi,Sp.

Bi,TA.

Po,TA.

Ce,TA.

BF,Bi, Sp.

Bi,Po,Sp.

Bi,Po.

Bi,Po.

Bi,Po,Sp.

Bi,Po.

Bi,Po,Sp.

Relief

Flat, No 0/G.

Flat, NO 0/C.

Flat.

Flat.

Flat.

Flat,Ba 0/C E.

Flat.Ba 0/C E.

Flat,Ba 0/C E.

Side of Hill.Ba 0/C.

Sloping S,Ba 0/C.

Sloping S,Ba 0/C.

Sloping S,Ba 0/C.

Sloping S,Ba 0/C.

Sloping S,Ba 0/C.

Flat f Ba 0/C N.

Flat.

Flat , Swampy .

Flat , Swampy .

Flat, Swampy.

Gd Rising S,

Gentil Slope,

Gl Slope, Gab 0/C W.

Gl Slope, Gab 0/C.

Sloping S, Gab 0/C.

Sloping S, Gab 0/C.

Moisture

Content

DT-\

u

T\ LJ

W

M

D

D

M

D

W

M

M

D

W

M

D

M

W

W

W

D

M

M to W

D

D

Soil Type

Si.9556C1.55f

3i. 95^01. 5/5

Si.90?6cl*l05fPe^356Si.90#Cl^10#Pe^2#

Si.90#Cl^10^Pe^2#

Si.955KC1.5S5

Si.90^Cl^10^Pe^255

Si.85S8Sa.105tCl.5Sf

Sa.95^Si^55SCl^1jS

Sa.95^Si.5?

Si.75StC1.25Jt

Si.75S8C1.25S8

Cia556Si.30SfOr.25JK

Si.755fC1.255f

Sa.6055Si.^.O^

Sia5SfCiao^Or.15Sf

Or.705fC1.30?

Or.855fCl.15Jf

Or.85SfCl.155f

Sa.7555Si.20^Pe.5/?

Si.95SfC1.5Sf

Sa.75^Si.25#

Sa.85^Si.1 5li

Sa.SO^Si. 2055

Si.85#Sa.155S

GrainSize

Si.Si .

Pe.Si.

Pe.Si.

Pe.Si.

Si.

Pe.Si.

Si.

Me.Sa.

Me-Co.Sa.

Si.

Si.

CI.

Si.

Fi.Sa.

Si.

Or.

Or.

Or.

Pe.Co.Sa.

Si.

Me.Sa.

Me.Sa.

Me.Sa.

Si.

Color

Ye.Br.

Ye . Br .

Ye.Br.

Ye.Br.

Ye.Br.

Ye.Br.

Ye.Br.

Ye.Br.

Li.Br.

Li.Br.

Li.Br.

Br.

Dr. Gr.

Br.

Li.Br.

Gr.Br.

Bl.

Bl.

Bl.

Br.

Go.Br.

Li.Br.

Br.

Br.

Ru.Br.

SampleNumber

633B151

833B1 52

83SB15383SB154

83SB15583SB15683SB15783SB15883SB15983SB16083SB16183SB16283SB16383SB16483SB16583SB16683SB167

83SB16883SB16983SB17083SB17183SB172

83SB17383SB174

83^175

Station

l -i f~ . ~ ^ ^. "7-

A20S 400Ei o f*\ O 1 f^ f*\ TT14 J? W O 4- U w JCj

4403 4.00E

4503 4.00E

4653 4.00E

4 75S 4-OOE

500S 400E

520S 400E

541S 400E

560S 400E

5803 400E

600S 4.00E

621 S 400E

8603 500E

84-13 500E

8203 500E

8003 500E

7803 500E

7613 500E

7403 500E

7203 500E

700S 500E

6803 500E

6603 500E

Vegetation

3i,Po,Sp.

Bi,Po,Sp.

Bi,Sp.

Bi.Sp.

Bi,Sp.

JP.

Bi,JP,Sp.

JP,Po,Sp.

Bi,Po,Sp.

Bi,Po,Sp.

Bi,Po,Sp.

Bi,Po,Sp.

BF,Bi,Po,Sp.

Bi,JP,TA.

BF.TA.

Bi,TA.

BF,TA.

Ce,Po,TA.

Ce.

Ce.

Sp,TA.

JP,Sp.

Bi,Sp.

Ce.

Bi,Sp,TA.

Relief

Sloping S.

Gab 0/C.

Sloping S, Gab 0/C

On 0/C.

On 0/C.

Ba 0/C

Sloping S,Ba 0/C.

Sloping S.

Sloping S,Ba 0/C W.

Gentil Sloping S

'Flat

Flat

Flat

Flat.

Flat, Gab 0/C E.

Flat.

Flat.

Flat.

Flat, Swampy.

Flat, Swampy.

Flat.

Flat.

Flat.

Flat,E-W Road.

Flat.

MoistureContent

M

No

D

No

No

M

M

D

D

D

M

D

D

D

D

W

M

M

W

W

D

D

D

W

D

Soil Type

Sample. On Outcrop.

Sa.7555Si.2055C1.555Sample. On Outcrop.

Sample. On Outcrop.

CI. 655531.3555Sample. On Outcrop.Si.50#Sa.155SPe.5?Si.90JfCl.105fSi.60JfSa.305fCl.105fCI. 6055S1.4055Sa.8055Si.1555Pe.555Sa. 905531. 555Pe. 555Sa.8555Pe.1055Si.555Or.50JfSi.405fCl.105fSa.705fSi.205fC1.205fSa.9055Pe. 55531. 555Sa. 955531. 55fSa.905SSi.5560r.556Or.80JfC1.20JfO Q f\ (0 C* J -^ C ff T^ f~ fifO ex * O \j /o O L* 1 ^ fO i 6*^/0

Sa. 905531. 5^5Pe. 5?Sa.9055Si.5550r.55S

Sa.8556Pe.1556Sa.855fCl.105fPe.55f

GrainSize

Fi.Sa.

Me.Sa.

CI.

Pe.Si.

Si.

Si.CI.Pe. Me.Sa.

Pe. Me.Sa.

Pe.Co.Sa.

CI.

Me.Sa.

Pe.Co.Sa.

Co.Sa.

Co.Sa.

CI.

Pe. Fi.Sa.

Pe. Fi.Sa.

Fi-Me.Sa.

Pe.Sa.

Pe. Me.Sa.

Color

Br.

iRu.Br.

i

Dr.Br.

Dr.Br.

Ru.Br.

Br.

Br.

Br.

Br.

Br.

BI.

BI.

Br.

Br.

Br.

BI.

Ru.Br.

Gr.

Br.

Br.

Br.

oHOo•H

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NL,

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SamuleNumber

83SB201

Station Vegetation

760S 600E BF.Ce.

83SB202

83SB203

83SB204

83SB205

83SB206

83SB207

83SB208

83SB209

83SB210

83SB211

83SB212

83SB213

83SB2U

83SB215

83SB216

83SB217

83SB218

83SB219

83SB220

83SB221

83SB222

83SB223

780S 600E j BF,8i,Ce.

800S 600E

820S 600E

840S 600E

860S 600E

880S 600E

900S 600E

920S 600E

940S 600E

1040S 700E

1020S 700E

1000S 700E

980S 700E

960S 700E

94.0S 700E

920S 700E

900S 700E

880S 700E

860S 700E

840S 700E

820S 700E

800S 700E

| BF,Bi,Po.

BF.Po.

BF,Po,Sp.

BF,Po.

BF,Bi,Po,Sp.

BF,BI,Po,Sp.

Bi,Po,Sp.

Bi,Sp.

Sp.

Sp.

Sp.

JP,Sp.

JP,Sp.

JP,Sp.

JP,Sp.

Bi,JP,TA.

Po,Sp,TA.

Sp.

Sp.

Sp.

Sp.

Relief

Flat.

Flat.r* A s T ^ T -^ ~ T,T uu. iLj.oj.iiti A .

Gd Rising W.

Gd Rising W.

Gd Rising W

Gd Rising W.

FlatjDac.O/C E.

Flat.Dac.O/C.

Flat.Dac.O/C.

Flat, Gl. Till.

Flat, Gl. Till.

Flat, Gl. Till.

Flat, Gl. Till.

Flat.Dac.O/C W.

Flat,Dac.07C W.

Flat,Dac.07C W.

Flat,Dac.07C W.

Flat, Gl. Till.

Flat.

Flat.

Flat.

Flat.

MoistureContent

W

W

M

D

D

D

D

D

D

D

D

M

D

D

D

D

D

M

M

M

W

M

M

Soil Type

Or.8056Cl.2056

Sa.95*Fe.5^

Sa.95%Fe.555

Sa.85#Pe.1555

Sa.9555Pe.5JSSa.95#Pe.5J?Sa.8555Pe.10j5Si.555Sa.8556Pe.1056Cl.5Ji31=65^01=3555Sa.60j6Si.35J6Cl.5J6Si.9055Sa.10jSSi.8055Sa.2055Si.90jSSa.10jSSi.9555Sa.555Si.95#Sa.5jSSi.955SSa.5!SSi.90jSSa.10#Si.9555Sa-.555

Si.9055Sa.10jSSi.955SSa.5JSOr.80j6Cl.20j6Si.90j6Cl.10j6Si. 90J5C1.1055

GrainSize

Or.

Pe.Co.Sa.

Pe.Co.Sa.

Pe.Co.Sa.

Co.Sa.

Co.Sa.

Pe.Co.Sa.

Pe.Co.Sa.

Si.

Fi.Sa.

Si.

Si.

Si.

Si.

Si.

Si.

Si.

Si.

Si.

Si.

Or.

Si.

Si.

lColor

Bl.

Br.l

Br.

Br.

Ru.Br.

Br.

Br.

Br.

Gr.

Gr.

Li.Br.

Li.Br.

Ru.Br.

Li.Br.

Li.Br.

Ru.Br.

Ru.Br.

Li.Br.

Li.Br.

Li.Br.

Bl.

Li.Br.

Li.Br.

T R AN SWAY EXPLORATIONSKLOTZ LAKE AREA

INC.

SCALE '1=2500

O-- —

(H—-V——Z.

LEGEND

— . ——. PROPERTY BOUNDARY

—.——. CLAIM BOUNDARY

CLAIM POST

:rr.r^- TRACTOR ROAD

SWAMP

g******* BEAVER DAM

SURVEY INFORMATION

INSTRUMENT

SURVEY OATES

SURVEY BY

TRANSMITTER

COIL SEPARATION

FREQUENCY

DRAWN BY PJVomos

DATE More h 1985

DDH

43f I38WM34 63.06* KUOTZ l-*Ki eoo

T R AN SWAY EXPLORATIONS INC.KLOTZ LAKE AREA

H. L. ELECTROMAGNETIC SURVEY H

SCALE l 2500

O----iT V

x "V

-

1 "7**i--'x •''•*/^CHOWDER

.///J /jj

LAKE ,/^

6 8 5/4^3 2 ,//?^

- v x.,-J'S v-' a 'x

L .2f

fl ,/fa^ W \;ffi

* ffis/*-*y 6]856I/685610

V

'/'

.V v/ \\ //o

648191,^'//

1t

1t

14

" W'i f 1*5v// J/"/

w/o V//

LEGENDIn PhOM Coma. Out Phaaa fiomn.

_.__. PROPERTY BOUNDARY

—.——. CLAIM BOUNDARY

O CLAIM POST

z:^rr- TRACTOR ROAD

\L' SWAMP

BEAVER DAM

7an-

.i.i \

(mil)SURVEY INFORMATION

INSTRUMENT

SURVEY OATES

SURVEY BY

TRANSMITTERt

COIL SEPARATION

FREQUENCY

DRAWN BY

DATE

APEX MoxMIn II

NOV 1983, FEB 1984

M. E. HALL

100 m

888 Hz,

M Vomos

MARCH 1984.

43FI38WM84 63.438* KLOTZ LAKE

o \


NC

H. L. ELECTROMAGNET/C SURVEY

SCALE '/'2500

LEGENDJfi Phqte Comp. Out Phma Como Imm


.——. CLAIM BOUNDARY

CLAIM POST

zi^rz- TRACTOR ROAD

\\, SWAMP

BEAVER DAM

•H

SURVEY INFORMATION

-t ,

l)*rt•l

INSTRUMENT

SURVEY OATES

SURVEY BY

TRANSMITTER .

COIL SEPARATION

FREQUENCY

DRAWN BY

DATE

APEX MoxMi'n II

NOVI983, FEB. 1934

M. E. HALL

3555

M Vbmctt

MARCH 1984

eeo

'.i.

T R AN SWAY EXPLORATIONSKLOTZ LAKf AREA

MAGNETIC SURVEY

INC

SCALE l 2500

LEGEND

_.__. PROPERTY BOUNDARY

—'.——. CLAIM BOUNDARY

O CLAIM POST

ri^rz- TRACTOR ROAD

\if S WA M P

BEAVER 0AM

FAULTS (Assumed)

CONTOURS ot 250 gammas

SURVEY INFORMATION

INSTRUMENT

SURVEY OATES

SURVEY BY

TRANSMITTER

COIL SEPARATION

FREQUENCY

DRAWN BY

DATE

GEOMETR/CJ G 816

NOV 1983 i

M. E. HALL

P Vamos

MARCH 1984

43PI38WM84 03.436* KLOTZ LAKB 230

r

SO


NC.

VLF SURVEY

SCALE 1=2500

^ L __ __ y^ g " vj 4

//•a/ lv/ 1 S ~*AS''\ "~~" ~~'"FT -—"4k. , — "*; \^------~*.~g.f y,// -.^/^^r/-

LEGENDIn Phot e .Out of Phoa*

• *


CLAIM BOUNDARY

CLAIM POST

s: i r: s. TRACTOR ROAD\J-i

\\f SWAMP

BEAVER DAM

Imm.SURVEY INFORMATION

INSTRUMENT

SURVEY DATES

SURVEY BY

TRANSMITTER

COIL SEPARATION

FREQUENCY

6EONIC EM 16 VL R*

DEC. 1983-, JAN .1984

M. E. HALL

CUTLER, ANNAPOLIS (Sea report)

DRAWN BY

DATE

P J. VAMOS

FEB . 1984

42F136WM2* M.43M KLOTZ LAKE

geol rpt of the transway prop klotz lake...42f13sw8824 63.435* klotz lake 010 geological report of...

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