COAL LICENf3 NUMBERS 7020 TO 7036 INCLUSIVE

NTSmIwJMl3m

93 F/16 WEST AND 93 F / E EASP

OP

STATEMENT OF QUALIFICATIONS

BRIAN P. FLY"

This is t o c e r t i f y t h a t I obtained my Bachelor of Science Degree i n

Geology at t h e Univers i ty of Natal, South Africa i n 1971.

S ince graduation I spent one year i n base metal explora t ion i n South

Africa and a t o t a l of f i v e and one h a l f years i n coa l explora t ion i n

Western Canada. O f t h i s per iod, fou r years have been i n t h e C o a l

Div is ion of Gulf Canada Resources Inc . , dur ing which time I have been

r e spons ib l e f o r t h e planning and superv is ion of eva lua t ion programs

involv ing diamond and r o t a r y d r i l l i n g , as well t h e design of reg iona l

exp lo ra t ion programs i n Western Canada and t h e Arctic. A t t h e present

time I hold t h e pos i t i on of Supervisor Regional Exploration.

APPENDIX Iv

Coal Quality Analysis Results - Drilling

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Coal Refercnoe

27 t 54 GULF CANADA No. 23-17407

24 t 48 21

18

ROMAX - 0.24) 0.01% t 30 15

12 1 2 4

9 t 1 8

3 I:', 6

3

0 0 I- VITRINITE TYPE (V-STEP)

LIMI

-_GULF CANADIIBFSO- LORING LABORATORIES LTD FILE NO 22935 -!!!J:_E, . h b m @ n n C E R T I F I C A T E o f C O A L T E S T I N G p.o. #mo23-17406 D A T E ~ ~ U ~ 5, 1 4 8 2

SAMPLE NO.

- i-

No. 1

IDENTIFICATION

Raw Coal

% RE'

SINK

% VCL

AATTEI -

27.13 34.70 36.99

25.46 32.57 j4.72

- %

S -

54 69 74

-

BTU ILB.

5,556 7,106 7,575

SWTE3EW OF QUALIFICATIONS

m c sa”

This is to certify that I obtained a Bachelor of Science Degree

in Geology at Concordid University in 1979.

My geological experience has been primarily in exploration and

mapping in Saskatchewan, Alberta, British Colmbia, and the Northwest

Territories. My background has been in uranium, oil and gas, and -1

exploration. I have keen employed as a geologist in the Coal Division

of G u l f Canada Resources Inc. since late 1980.

I I I 12

MILES 0 5 10 1-

5 10 IS 0 KILOMETERS

SCALE I: 250,800

MT GREER COAL PROJECT LOCATION MAP

Location:

The Mount Greer coal property is situated in central British

Columbia, approximately 140 kilometres west of Prince George.

Access:

Access to the property is via gravel road from either Vanderhmf

or Fort Fraser. The distance in both cases is approximately 40 kilo-

metres.

Licences and (xlmership:

The Mount Greer coal property is comprised of 17 licences with a

total area of 4302 hectares, in which Gulf Canada Resources tias 100%

ownership.

Faploration:

A ten day mapping program of the licence block was m in the

s~lloer of 1981. A second program, in the winter of 1981, comprised cme

rotary hole drilled to obtain are and quality analyses m a reported

subsurface 9.8 metre coal zone. This zone was reported by E ti B

Exploration in 1978 while drilling for uraniferous sedimnts.

RDH-81-001

Q

10

20

,30

.40

.50

UNCQNFORMITY

SCALE (m)

0.8 m -

ANGULAR UNCQNFORMITY

\ \ \ \ \ \ \ ’ \

\

I I

I I

I I I I

I I

I I I I

I I

I I I

I I

GULF CANADA RESOURCES INC. edDM*on

cALa4a”

MT. GREER COAL PROJECT

GENERALIZED STRATIGRAPHIC COLUMN

Stratigrwy:

The Mount Greer licence block is underlain by the Tertiary hdako

Group. ?his unit consists of basal sediments, in association with

minor coal beds, overlain by a predominantly basaltic volcanic cap

rock. Underlying the Endako Group are layered volcanic flows of the

Tertiary Qtsa Lake Group.

structure:

There is no evidence of mjor faulting or folding in the area,

though a l l scale flexures occur in the sub-horizontal basal Endako

sediments.

The lack of ecOncPnic seam precluded the calculation of a pten-

tial resource.

The Head Analysis of samples taken proved the coal to be lignitk

in rank.

Further mrk is mt mrited and it is reconmended that the pro-

perty be dropped.

STATEEZENT OF QUALIFICATIONS

SUblWIRY

1.0.0 I m ~ c ! r I m

1.1.0 Location 1.2.0 History 1.3.0 Licences 1.4.0 Ownership 1.5.0 Access 1.6.0 Biophysical Environment

2.0.0 EXPIDRATION

2.1.0 Objectives 2.2.0 Introduction 2.3.0 Cartography 2.4.0 Exploration

2.4.1 Geologic Mapping 2.4.2 Rotary Drilling

2.5.0 &clamtion 2.6.0 Project Management and Contractors

3.0.0 GEOIXX;Y

3.1.0 Regional Geology 3.2.0 Stratigraphy

3.2.1 Cotsa Lake Group 3.2.2 End& Group

3.2.3 Tbpley Intrusives 3.2.2.1 Coal Ikvelopnent

Page No.

1

1 1

7

7 7 8 8

8 8

10 10

12

12 14

14 14 18 20

3.3.0 Structure 20

4.0.0 RESOURCE POTENTIAL

5.0.0 COAL QUALITY

5.1.0 D r i l l Hole Analysis

6.0.0 RECCMMEN!XTICNS

7.0.0 SELECTED BIBLIOGRAPHY

Page No.

2 1

22

22

24

25

LISP OF FIGURES

Figure No.

1.1

1.2

1.3

2.1

3.1

3.2

3.3

5.1

3.1

Page No.

Mount Greer Location Map 2

Detailed Licence Map 4

Mount Greer Regional Access Map 5

Drill Hole Location Map 9

Stratigraphy - Table of Fomtions Mount Greer Coal Fropr ty - Geology

13

15

Drill Hole Log Comparison 19

Coal Analysis F l w Sheet

hdako Sedimnt Outcropping

23

16

LISP OF APPENDICES IN TGPP

I Legal kscripticn of Licences

I1 Geology Map (1:50,000)

I11 Drill Core Log

IV Coal Quality Analysis Results - Drilling

APPENDICES IN l"AL SLEEVE

V Geophysical IDJS

1.0.0 INTmrnI(3N

1.1.0 Iocation

The Wunt Greer coal property is s i tua ted i n cent ra l

Br i t i sh Colunbia a p p r o x h t e l y 140 kilometres west of Prince

George, B.C. The l icences lie ktween G r e e r C r e e k and the

Nechako River, south of Highway 16, which is geographically

located a t 53"50' north l a t i t u d e and 124"32' w e s t longitude

(Figure 1.1).

1.2.0 Eistcay

G.M. Dawson of the G e o l o g i c Survey of Canada f i r s t repor-

t e d coal i n the area i n 1878. H e made br ie f E n t i o n of a four

foot seam along t h e N e c h a k o River bank near Mount Greer. H.W.

Tipper, also of the G.S.C., mapped the region i n the ea r ly

1950's and produced the only geologic map of the area to date.

The Dawson seam w a s not delineated, though large lignitic b u l -

d e r s were recorded along the Nechako River.

The sediments of the Ter t ia ry Endako G r o u p were d r i l l e d

i n the 1970's to determine i f uranium placer deposits existed.

The core logs fa i l ed to prove the above, but ver i f ied the exis-

tence of subsurface coal seams. No s tudies or analyses were

conducted cn the -1 and the base E t a 1 claims were ultimately

surrendered.

- 1 -

7” --* - -..-.. -.. -.. -..-..

I

- 2

124O 15’

SCALE 1:250,000 MILES

0 5 10 5 0 5 10 15

K I LOM ET ERS

W D,rmon CALGARY ALBEilTA

MT. GREER COAL PROJECT I , ~ LOCATION MAP

PREPARED 8 V

AWROVED 8Y: E. s. D A T E F E E . 82 (DRAWINGNO. 1.1 1 SCALE I : 250 000

-

After conpleting a regional study, Gulf Canada Resources

Inc. obtained l icences i n the area on the basis of one of those

core logs, which reported a 9.8 m e t r e coal zone at depth. This

report details the r e s u l t s of a l l phases of the Mount Greer coal

property evaluation.

1.3.0 Licences

The Mount Greer property is comprised of seventeen licen-

ces as shown i n Figure 1.2. The l icence block consists of 4302

hectares and was acquired on March 1, 1981. ?he legal descrip-

t i o n of the property is enclosed i n Appendix I.

1.4.0 Cmership

The Mount Greer coal l icences are wholly owned by Gulf

Canada Resources Inc.

1.5.0 Access

Tim graded logging roads converge and cut through the

center of the licence block. These mads feed i n t o F o r t Fraser

and Vanderhmf, which are 35 and 43 kilometres from the property

respectively (Figure 1.1). Highway 1 6 and the Canadian National

Railroad, between Prince R u p e r t and Prince George, pass through

both towns. Regional access to the area is depicted in Figure

1.3.

- 3 -

7021

M20

H

30'

7033

7029

7025

7032

i t L1326

7031

7027

E .I

I I I

I I

I I I L1338 I I

7050

7026

7022 I I I I I

3052

3%

GULF CANADA RESOURCES INC. wana

CALWII" A L I I f R T I

MOUNT GREER COAL PROJECT

COAL LICENCE MAP

- 4 -

I

in

I

1.6.0 Biophysical Fnvironment

The region, as part of the Interior Plateau, was heavily

scoured during glaciation resulting i n a gentle to undulating

topographic te r ra in .

Mount G r e e r forms the topographic high, imediately west

of the licence block, a t 1254 metres, while the mrshes in the

central and eastern portions of the property represent the t o p

graphic lows a t approximately 825 metres.

The area is vegetated by hoth open and dense forest cover

comprised essentially of primary and secondary growths of black

spruce. Small clusters of poplar occupy the low lying and w e l l

drained regions.

Moose frequent the marshlands, but the heavy bush growth

and high degree of land cultivation r e s u l t in few large game

sightings in the region.

- 6 -

2.1.0 Chjectives

?he cbject ives of the 1981 Mount G r e e r exploration pro-

gram w e r e :

a ) to map the property and delineate any p t e n t i a l coal-

bearing strata;

b) to locate and twin a d r i l l hole beside EN-1, where a 9.8

metre seam was recorded;

to estimate an in-situ resource p t e n t i a l . C)

2.2.0 Intrcduction

The Gulf Canada Resources exploration of the Mount G r e e r

area comnced with a 1 0 day mapping program i n the sunnner of

1981. Subsequent to the i n i t i a l f i e l d evaluation, a me hole

ro t a ry d r i l l program w a s run f o r 7 days i n the winter of t h a t

year.

- 7 -

2.3.0 cartography

The Geological Survey of Canada published a geological

map of the study area at a 1:253,440 scale. This map is out of

p r i n t and is available only from G.S.C. Memir 324.

Topographic mps a t a 1:50,000 scale were u t i l i zed for

f i e l d p lo t t ing of data.

2.4.0 Ekplcuatim

2.4.1 Geologic Mapping

I n i t i a l exploration of the licence block w a s done

from June 16 to 27, 1981. Personnel were based i n Fraser

Lake, approximately 50 kilometres northwest of the

PropertY.

The wrk aonsisted of ground traverses over the

e n t i r e l icence area. Results of the mpping program are

plo t ted on a 1:50,000 base nap in Appendix 11.

2.4.2 IlDtKy milling

Field personnel were based i n Vanderhmf, 42 kilo-

m e t r e s southwest of the townsite, from December 10 to 16,

1981. One 15.2 c e n t h t r e diameter rotary drill hole,

RDH 81-001 (Figure 2.1), was twinned beside EN-1, previ-

ously d r i l l e d by E & B Exploration i n 1978, to a depth of

308 metres.

A 12 m e t r e i n t e rva l w a s cored (Figure 3.3) and

logged but intersected no coal. The descr ipt ive log is

enclosed in Appendix 111.

- 8 -

124°730’ 124O IS’

SCALE 1:2SO,OOO MILES

0 5 10 B Q 6-- I 0 IS

K I LOMET ERS

GULF CANADA RESOURCES INC. cAL(wv ALBERTA

w-

MT. GREER COAL PROJECT

DRILL HOLE LOCATION

Coal chip samples collected were tes ted v ia petro-

graphic and head ana lys i s mthcds. A l l r e s u l t s are

enclosed i n Appendix IV.

A geophysical logging contractor produced 1:200

metric scale logs of g m - n e u t r o n , densi ty , focused beam

and caliper, along with deviation masuremnts . All logs

are enclosed i n Appendix V i n the in te rna l sleeve.

2.5.0 &clamation

The d r i l l site w a s leveled prior to d r i l l i n g and w a s

recontoured upon completion of the program. There w a s a minimal

amun t of disturbance and reseeding of the site is to te con-

t r ac t ed out i n the spring of 1982.

2.6.0 Project Management and Contractors

The 1981 coal exploration program was mnaged by

B.P. Flynn (Supervisor, Regional Exploration) of Gulf Canada

Resources Inc.

- 10 -

Field operations f o r the geologic mapping phase were

supervised by a consulting geologist , J . M . IXlford. The drill

program was supervised by E. Swanbergson of Gulf Canada

Resources Inc. The geological report w a s prepared by

E. Swanbergson.

The following addi t ional technical personnel contributed

to the Mount G r e e r C o a l Project:

1 Geoloclical Assis tants

R. Jackson M. DesRoches M. Rausch R. Maylor J. Newal l

A. Vora Field Bookkeepr

The following contractors, suppliers and service compa-

nies e r e used during the project:

Can-West Dri l l ing Inc. Eric Weinhardt (Catskinner) G l e n n ' s Motor Inn Fraser Lake Inn Canuck Truck Renta l Camday Truck Rental Neville Crosby Inc. Cyclone Engineering Ltd. Loring Lahoratories D.E. Pearson and Associates Totem Distr ibutors Levitt Safety CCIIEX Packaging Ltd. Alida Surplus Ltd. Ceitrich-Post Ltd. Prairie 'n Peak International Survival Supplies Economy Bookbindery Co. Ltd.

Prince George Vanderhoof Vanderhwf Fraser Lake Prince George Calgary Vancouver Edmonton Calgary Victoria Calgary Prince George Vancouver Calgary Calgary Calgary Calgary Calgary

- 11 -

3.0.0 GEOLOGP

3.1.0 Pegicnal Geology

The Wunt Greer region consists of extrusive flow rocks,

intrusive plutons, and sedimentary rocks.

The flow rocks, mainly basalt, andesite and related tuffs

and breccias, are comnly of limited lateral extent resulting

in unconformities and incomplete stratigraphic sequences. For

example, Grtiary rocks are known to te unconformably in contact

with plutonic rocks of the Jurassic.

The mjor plutons that intruded the region occurred

during the Lawer Jurassic and the Upper Jurassic.

The mst extensive stratigraphic unit is the Tertiary

Endako Group. C o a l has ken reported in the basal sediments of

this unit which were subsequently overlain by basaltic and ande-

sitic flows, also of the Endako Group. The highly recessive

Endako sediments are in close time association with the volcanic

flm rocks and, to facilitate geologic mpping, were considered

a single stratigraphic unit.

Pleistocene glaciation substantially remved or huried

evidence of the Endako Group, and sedimentary exposures are

rare.

- 12 -

.-

FORMAT ION

Endako Group

Ootsa Lake Group

L I THO LOGY

Stream and lake deposi ts, talus, sai l

G lac ia l and g l a c i o - f l u v i a l depos i t s

EROSIONAL INTERVAL

Basalt, andesite; related tu f f and breccia; shale, s i l t s tone greywacke and l ign i te

ANGULAR UNCONFORMITY

Rhyol i t ic and dacit ic tu f f and breccia ; shale sandstone and conglomerate

Rhyolite .docite, trachyte, andesite; minor basalts; related tu f f and breccia

Baso l t , ondesite, minor rhyol i te, sandstone and conglomerate

PERIOD OR EPOCH

Recent

P l e i s t o c e n e

Miocene and ( 7 ) Later

Upper Cretaceous

to

Lower Cretaceous

GULF CANAOA RESOURCES INC. co* hrlM

CALGARY ALBERTA

MT. GREER PROPERTY TABLE OF FORMATIONS

- 13 -

3.2.0 Stratigraphy

Local to the Mount Greer licences, outcroppings are

r e s t r i c t e d to the Ter t ia ry Ootsa Lake Group, End& Group, and

t h e Jurassic Topley Intrusives.

Any d r i l l i n g i n the region was halted upon entry in to the

Ootsa Lake Group, resul t ing i n nominal pre-Miocene d r i l l hole

data.

3.2.1 ODtSa Lake Group

The m l c a n i c flot and mi or sedimer of

the Ootsa Lake Group are angularly unconformable to

underlying Mesozoic rocks.

hcevious work by Tipper divided the group i n t o

two; the Andesite Unit and the Rhyolite Unit. The Ande-

site Unit is Upper Cretaceous i n age and is i n excess of

500 metres thickness. fie Rhyolite Unit is Paleocene i n

age and has an undetermined thickness.

The contact ketween these uni ts is l i t ho log ica l ly

gradational and highly a rb i t ra ry .

3.2.2 hdako Group

The Tert iary End& Group unmnformably overlies

the Ootsa Lake Group and consis ts of sedimentary rocks of

t h e late Oligocene overlain by volcanic rocks of the late

Oligocene, Miocene, and younger.

- 14 -

I24O 30' 124O 15'

GULF CANADA RESOURCES INC. Coal Division

ALBERTA I CALGARY

TERTIARY ENDAKO GROUP

MILES 0 0 1 5 10 1s

Mt. GREER COAL PROPERTY GEOLOGY

KILOMETERS PREPARED BY: ]SCALE I: 250,000 DATEFEE. 82 DRAWING NO. 3.2

- 15 -

The Endah G r o u p entirely e r l i e s the licence

block as depicted i n Figure 3.2.

f ie basal sediments of the hdako f i l l p-ocene

valleys and vary in thickness fran 10 to 300 metres.

photo 3.1 Coal-bearing Endako Sediments o u t m i n g near

Cheslatta Falls (40 kms. southwest of the property)

The sediments m i s t of mnotcnous shale, silt-

stone, and sandstone sequences plus minor omglomerate

and l i gn i t i c coal.

Cberved outcroppings of the Endako sediments

(Photo 3.1) proved the existence of l igni te i n the Group.

These outcrops are covrprised of coal lenses, less than

- 16 -

45 cm thick, interbedded with s i l t y sediments and k n t o -

n i t e k d s .

D r i l l hole logging r e s u l t s from RDH 81-001 shmed

t h a t the End& sediments consis t essent ia l ly of:

110 metres - sandstone, siltstone, shale inter- beds

50 metres - sandstone and shale interbeds 50 metres - shale and s i l t y shale interbeds 45 metres - f ine ly t d d e d sandstone, s i l t s tone

and shale interbeds 25 m e t r e s - unlogged to base of uni t

Caving problem prevented logs from k i n g run to T.D.

Overlying the basal sediments are the Endako

extrusive flow rocks consisting essent ia l ly of andesite

and basalt. These volcanics are approximately 430 metres

th ick and were f o m d from a series of flows, of limited

lateral extent, overlying each other.

Mount Greer consists almst en t i r e ly of vesicular

to q g d a l o i d a l basalt with the kst exposures k i n g on

the south face. No Endako sediments outcrop m the

licence block.

- 17 -

3.2.2.1 coal Developnt

The repxted seam developnent in drill hole

EN-1 was disproved by this program (Figure 3 . 3 ) .

There is 110 coal of significant thickness within

the Endako sediments cn the Mount Greer proprty.

The discrepancies between the twinned holes

can be accounted for by:

i) erroneous logging of original hole, or

ii) the existence of a mjor washout initiated

by tectonic uplift local to the region.

Of the two mssibilities, the former is the

mre probable.

One coal zone 0.8 metres thick was

intersected at a depth of 246.3 metres and was

analyzed to be lignitic in rank.

Stringers of lignite have been observed at

Cheslatta Falls as shown in Photo 3.1. Similar

coal banding m y exist in the Endako sediments on

the licence block but such beds are not in

evidence on the geophysical logs and, if present,

are too thin for propr downhole tool resolution.

- 18 -

E B B EXPLORATION uranium core hole

EN-I I978

.. .. 2001-..-1 .. - ..

??--

247.2 249.3 250

260

270

280

G.C.R.I. cool drill hole RDH-81-001

I80

213.6

225.6

ma

275

1981

I 0

k $ - n W v)

-. -.-. -.- - ~ .. .. - .-- _- - . . . . .

cored ___ 'interval . . . . . --- . . . . . - _-- --- . . . . ,

In I- 2 W

0 W v)

r

- log interpretation

0 SANDSTONE

0 SILTSTONE

MUDSTONE - CONGLOMERATE

C - c - c CARBONACEOUS CLAYSTONE

COAL LAMINATIONS

r>a CORE LOSS

metres

I:\

0 1 0 I 2 3 rnatrer

sCnLE

GULF CANADA RESOURCES INC. c d D k p .

max. depth

geophysicol reached by MOUNT G R E E R i tools D R I L L H O L E COMPARISON

3.2.3 Topley Intrusives

The Topley Intrusives were emplaced during the

Lower Jurassic and, within the imp area, consist of

granite, granodiorite and diorite. These rocks underlie

a large portion of the Mount Greer area and are known to

be i n contact w i t h rocks of Tertiary age inmediately west

of the property.

3.3.0 Structure

The Endako sediments l ie m an unconformity and are best

described s t ructural ly a s subhorizontal, though the regional dip

trends gently east.

Regionally fau l t l ineations are observable on airphotos

though none are evident on the licence block. %ere is m

evidence as to the degree of displa-nt along f a u l t planes.

- 20 -

The lack of economic coal seams precluded the calculat ion

of a W t e n t i a l resource.

- 2 1 -

5.0.0 CaAL QUALITY

5.1.0 D r i l l Hole Analysis

Rotary d r i l l hole RDH 81-001 lost c i rcu la t ion a t a depth

of 225 metres, and the chip samples collected are believed to

have mme f m the coaly zone at 246.3 metres (refer to focused

beam log i n Appndix V).

The mall sample col lected w a s sen t f o r petrographic and

head analysis, as per ASTM methods, the r e s u l t s of which are

recorded i n Appendix IV.

The coal was determined to he l i g n i t i c with an average

BTU value of 15.69 MJfig.

- 22 -

Air dried a t 35OC for 24 hours

Crushed in hammer mill to pass 100% at 60 mesh

Anal ysed for proximate, calorif ic

ASTM methods and sulphur values as per

ALBERTA

MT. GREER PROGRAM COAL ANALYSIS FLOW SHEET

6.0.0 -1CNS

It is recomnded that all coal licences held in the Mount Greer

licence block be surrendered.

- 24 -

7.0.0 SELM3TED BIBLIOC;RAPBY

Adamon, R.S., Street, P.J. Less Develop4 Thermal Coal & p i t s of and Campbell, D.D. : British Columbia; blmge, Campbell and

Ass., Vancouver, 1974.

Tipper, H.W.: Nechako River Map Area - British Columbia; Dept. of Mines and Technical Surveys, G.S.C. Memoir 324.

- 2 5 -

AppluDIx I

Legal kscripticn of Licences

Licence

7020

' 7021

- 7022

7023

7024

7025

. 7026 7027

7028

7029

7030

7031

7032

7033

7034

7035

7036

!!32

93-F-15

93-F-15

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

93-F-16

Lot 1326: 93-F-16 93-F-16

Lot 1327: 93-F-16

Lot 1338: 93-F-16 93-F-16

H

n

E

E

E

E

E

E

E

E

E

E

E

E

D E

E

D E

21, 22, 31, 32 306

41, 42, 51, 52 306

3, 4, 13, 14 278 (except lot 1338)

(except lots 1326, 1327, 1338)

5, 6, 15, 16 76

7. 8. 17. 18 37 (except.lo& 1323,

1326, 1327)

9, 10, 19, 20 (except lot 1323)

23, 24, 33, 34

25, 26, 35, 36 (except lot 1327)

27, 20, 37, 38 (except lot 1327)

29, 30, 39, 40

43, 44, 53, 54

45, 46, 55, 56

47, 48, 57, 58

49, 50, 59, 60

244

306

283

159

306

30 6

306

306

306

259

259

259

APPJmDIx I1

Geolosy Map (1:50,000)

'I

xxxxx

82/02/23 GULF CANADA RESOURCES INC. - C O A L O l V I S I O N - D R I L L CORE LOG

PROJECT: H T G BLOCK: XX DATA SOURCE: ROIQ31001

DEPTH DEPTU I N T R V A L SAHP. SEAM rp- LL LITtlOLOLT

*

213.55 213.59

213.59 213.65

21 3.65 213.19

213.79 214.19

214.19 214.26

214.26 214.96

214-96 215.16

* 215.16 215.29

215.29 215.85

* D E K I T E S MEASURED BCA

0.04

0.06

0.14 '

0.40

0.07

0 070

0 020

0.13

0 056

MUDSTONE

SANDSTONE

MUDSTONE

SANDSTONE

WUDSTONE

S I L T S T O N E

SANDSTONE

SI LTSTONE

MUDSTONE

PAGE 1

----a-m OK. G Y .SL D A U GREYS ARE CAEY-GREEN-

W E L .GY 0 S L O A L L G R E Y S ARE GREY-GREEN.

G Y - S L O A L L GREYS ARE GREY-GREEN.

MOO.GY.SLD A U G R E Y S ARE GREY-GREEN; CORE B R O K E N N MIDDLE.

G Y - S L O

GY. S L O SANDY A T BASE.

W EL .Gym S W

GY. S L O T H I N C O A L BANDS I N PART.

GY. SLD

1

x x x x x

82/02/23 I

G U L F CANADA RESOURCES I N C - - C O A L D l V l S I O N - D R I L L CORE LOG PAGE 2

PROJECT: MTG BLOCK: XX D A T A SOURCE: R D H 8 1 0 0 1

DEPTH D E P T H I N T R V A L SAMP. SEAM W E E Q L TO T H I C K 10L J ITHOLOGY

215.85 216.01 0.16 S 1 LTSTONE

*

216.01 216.32 0131 MUDSTONE

216.32 216.41 0.09 SANDSTONE

216.41 217.18 0-77

217.18 217.79 0.61

217.79 217.82 0.03

217082 218.24 0 -42

218.24 218.64 0.40

218.64 2le.87 0.23

MUDSTONE

WUDSTONE

SANDSTONE

MUDSTONE

MUDSTONE

MUDSTONE

GY. SLD I R R E G U L A R COAL FRAGMENTS UP TO 5 CM Tt- CK.

W E L o G Y - S L D

D K - G Y - S L D M I N O R C A R 0 P L A N T FRAGMENTS I N PART.

S L T Y .OK - GY .S L O P L A N T FRAGMENTS I N PART.

CG. M0D.G Y. SLD

S L T Y o DK .I GY .S LD

D K - G Y CDRE BROKEN I N MIDDLE.

S L T Y *OK 0 GY *SLD

1

* DEMTES MEASURED B C A

X X X X X

82/02/23 G U L F CANADA RESOURCES INC. - C O A L D I V I S I O N - D R I L L CORE LOG

PROJECT: MTG BLOCK: XX D A T A SOURCE: R D H B l O O l

D E P T H DEPTH I N T R V A L SAMP. SEAM 811! FRoM TO T H l C K - LD ID J ITHOLOGY

2i8.87 218.99

218.94 219.26

219.26 219.46

219.46 219.93

219.93 219.95

219.95 220-21

220.23 220.60

220.60 220.93

0.07

0-32

0 020

0.47

0.02

0.26

0.39

0-33

220.93 221040 0 -47

* D E M T E S MEASURED B C A

MUDSTONE

CORELOSS

MUDSTONE

MUDSTONE

SANDSTONE

MUDSTONE

SANDSTUNE

MUDSTONE

SANDSTONE

PAGE 3

OES CR I P T 1 ON

DK.GY.SL0

ROCK

A S ABOVE; I N I T I A L L Y CORED ON L A S T CORE RUN.

DK.GY.SLD M I N O R C A R B L A Y E R S I N M I D D L L .

C G . HOD. G Y o S L D

D K - G Y o S L D

MG. WEL.GY.SLD M I N O R MUDSTONE I N T E R B E D S G R A D A T I O N A L C NTACT A T TOP.

DK.GY o S L D M I N O R P L A N T FRAGMENT5 A N D C O A L FRAGMEP 5 .

M G WEL. G Y CORE BROKEN I N MIDDLE.

Y

e xx xxx .

82/02/2 3 G U L F CANADA WESOURCES INC. - C O A L D I V I S I O N - D R I L L CDRE LOG

PROJECT: MTG BLOCK: XX DATA SOURCE: RDH81001

D E P T H DEPTH I N T R V A L SAWP. SEAM FROM TO THICK. ID c I THOLOGY

221.40 221.71

22 I .If 22 1.73

* 221.73 222.19

222.19 222.36

222.36 222.58

222.58 222.77

222.77 222.85

.,222.85 222.92

222.92 222.98

222.98 223.08

0.31

0.02

0.46

0.17

0.22

0. I9

0 008

0.07

0.06

0.80

MUDSTONE

SANDSTONE

MUDSTONE

MUDSTONE

CORELOSS

S I L T S T O N E

CORELOSS

SANDSTONE

MUDSTONE

SANDSTONE

P A G t 4

DKIGY .SLD M I N O R P L A N T FRAGMENTS-

MG. UEL.GY.SLD

D K - G Y M I N O R C A R B L A M I N A T I O N S .

CARE .OK .BUN. BRKN COLOUR 15 B L A C K T O BROWN TOWARUS B A S t i MINOR COAL L A M I N A T I O N S .

ROCK.

G Y - S L D

ROCK 0

HG.WEL.GY CQRE BROKEN A T TOP.

OK-GY .SLD

DEMTES MEASURED E C A

82/02/23 GULF CANADA RESOURCES INC. - COAL D l V l S l D N - D R I L L CORE LOG

PROJECT: MTG BLOCK: XX DATA SOURCE: RDHBlOOl

D E P T H DEPTH l N T R V A L SAMP. SEAM i%X E;ROM L L I j I c K % ID 1D idJL!!2=

223.08

223.11

* 223.23

223.96

I 224 -04

224.17

224-51

224.59

* 224 -86

224.97

223.1 1

223.23

223.96

224 -04

224.17

224.51

224 059

224 -86

224 097

225 000

0.03

0.12

0.73

0.08

01 13

0.34

0.08

0.27

0.11

0 -03

MUDSTONE

SANDSI'ONE

HUDST W E

MUDSTONE

S 1 L T S TONE

MUDSTONE

CORELOSS

SANDSTONE

MUDSTONE

SANDSTONE

PAGE 5

D K - G Y - S L D C A R E L A M I N A T I O N S 1N MIDDLE.

A S ABOVE.

S LD S L I G H T L Y C A R 0 AT TOP.

D K - G Y .SLD

ROCK

MG-WEL-GY CORE BROKEN A T TOP; MSNOR MUDSTONE INT R E D S .

OK.GY.THN0 CARE I N PART; COLOUR I S GREY TO B L A C K -

MG. WEL.GY.SLD

1

* D E M T E S MEASURED BCA

Y

x x x x x

82/02/23 GULF CANADA RESOURCES INC. - COAL D I V I S I O N - D R I L L CORE LOG P A G t 6

PROJECT: HT6 BLOCK: XX DATA SOURCE: R D H 8 1 0 0 1

D E P T H D E P T H ZNTRVAL SAHP. SEAM D E S C R I P T I O N €I!& FRoU I0 T H I C K L I D j l T H 0 , O G Y

225.00 225.1 1 0.11 HUDSTONE GY-THNB. SLD WAVY BED L A M I N A T I O N S ; COLOUH IS L I G H T 1 0 DARK GREY.

* 225.11 225.35 0.24 MUDSTONE DK. GY.SLD

225.35 225.43 0.08

225.43 225.55 0.12

CORELOSS ROCK.

SANDSTONE MG-WEL-GY CWE BROKEN A T TOP. A T 225.55-BASE OF O R I N G I N T E R V A L ; C I R C U L A T I O N L O S T .