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Pace NINE CasstAR AsBESTOS CORPORATION LIMITED

Screen
Date Round From To % Grade te : 2 ¢ 3 4 %
Oct. 24 37-298’ 304” 57 aR ies Sere oes
25 38 304’ 310’ eal 3K Dep) 6.5 (Pep) 1.8
26 39 310’ ly 4.3 3R 1.6 9.3 3.7 1.4
Di, 40 317’ 324’ 4.0 3T 0.7 9.0 4.4 1.9
28 41 324’ 331’ 4.9 3R 2.8 8.7 3.0 ED
29 42 331’ 338’ 2.0 3T 1.0 7.0 4.4 3.6
30 43 338’ 344’ 3.4 3Z 0.3 5.8 6.2 3.7
31 44 344’ 347’ 4.1 3Z 0.1 We) 5.6 3.0
Nov. 1 45 347’ 351’ 4.8 3Z 0.2 Ue D1 3.2
2 46 BI” 358’ 3.9 3Z 0.6 7.8 4.7 2.9
3 47 358’ 365’ 3.8 Be 0.4 8.2 4.4 3.0
4 48 365’ Bye 12.6 3R 3.0 Vee: 4.2 1.6
D) 49 372’ 379’ 9.6 3F 13.8 0.8 0.9 0.5 + 0.23% Crude
6 50 379’ 386’ 12.8 3 7.8 3.6 3.0 1.6
Ae tees 8 66393. O30 ak AiObe weno een 40) ol uutl 0:24 uGrude
8 52 393’ 400’ 9.2 3K 6.0 5.0 3.3 1.4 + 0.2 % Crude
9 53 400’ 406’ 8.7 3K 8.0 4.5 Ve) 1.0 + 1.0 % Crude
10 54 406’ 412’ 9.6 3R 4.5 6.4 3.2 1.9
11 55 412’ 419’ 11.4 3K 6.7 Dial 2.8 1.4 + 05 % Crude
12 56 419’ 425’ 6.3 3R 4.1 6.5 4.2 1.2
13 Dy 425’ 432’ 11.8 3K 10.9 1.6 Ze 1.0 + 0.4 % Crude
14 58 432’ 439’ 10.4 3R 5.9 4.9 3.8 1.4 + 0.2 % Crude
ADIT COMPOSITE ASSAY
Screen
From To Dist. % Grade 1 2 3 4
188’ 317’ 129’ 7.5 3F 7.85 4.36 2.15 1b3 + Some Crude
317’ 365’ 48’ 3 /: 3Z 0.92 7.84 4.52 2.67
365’ 439’ 74’ 10.2 3K 6.91 4.6 3.14 133) + Some Crude
188’ 439’ Zi 7.6 3K 6.84 4.75 2.76 1.45 + Some Crude

DETAIL OF TUNNEL:

The portal of the tunnel is collared in footwall sediments at elev. 6028 ft.; direction N.53°
54’E.; total length 439 ft.; timbered throughout.

The first 137 ft. of tunnel, crosscut tightly folded and contorted thin bedded argillites with some
thin bedded impure limestone. The attitude of these footwall sediments was not determined in detail,
but generally they strike slightly west of north (N.15° - 20°W.) and dip from a few degrees East to 70°E.

The contact between these sediments and the serpentine is a faulted contact, as exposed in the
tunnel. This contact strikes generally N. 345° or N. 15° W. and dips 47° N.E. This attitude correlates
with the contact as mapped on the surface. I believe the evidence in the tunnel favours a thrust fault
on this contact.

From 137 ft. - 172 ft. the tunnel exposes a dark sheared serpentine with a few narrow veinlets of
asbestos. At 172 ft. there is a marked shear zone striking N. 50° W. dip 70°E. This zone extends to
roughly 185 ft. and contains some chrysotile fibre. From 188 ft. to the face at 439 ft. (251 ft.) the
serpentine is light to medium green in colour, is well fractured and contains numerous veinlets of chrysotile
asbestos. The fibre content varies within limits, both as to quantity and length of fibre, but on the whole
the fibre is uniform, and of good grade, as set out in the above tabulation of muck sampling.

The two main directions of fracturing in the ore section are:
(a) N. 15°-20° W. dip 45° - 60° E. (ie. paralleling the serpentine contact).
(b) N. 50° - 60° W. dip 65° E. to Vert.