DIAMOND DRILLING. CLAIM No, HOLE No, FOOTAGE DATE NOTE NOTES: TOWNSHIP: LITTLE REPORT No, May/ 80 May X 80 June/80.

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1 DIAMO DRILLING 42A11NE8ie9 24 LITTLE 010 TOWNSHIP: LITTLE REPORT No, WORK PERFORMED BY: NORCEN ENERGY RESOURCES INCORPORATED CLAIM No, HOLE No, FOOTAGE DATE NOTE P P P TP19805 TP19806 TP May/ 80 May X 80 June/80 (l) (l) (l) NOTES:

2 4 Note that 824 days of unapplied assessment credits were reported on July 14, 1980 by John Siriunas of MPH Consulting from drill hole TP These 824 days of assessment credits are hereby applied along with additional drilling credits to the above listed 127 claims. The 127 claims have 20 days assessment credit applied to each for a total of 2,540 days of credit. The remaining 9 days credit will be applied at a later date.

3 Energy Resources Limited NORCEN TOWER, 7155th Avenue S.W. CALGARY, ALBERTA T2P2X7 Phone (403) The required information is as follows: Four (4) diamond drill holes (TP19804, TP19805, TP19806 and TP19807) were drilled on this claim group. The specifications for each hole are summarized below: Hole Number Angle at Collar tal Depth Depth Casing Dates TP m (984') 39.6 m June 13, 1980 July 3, 1980 TP m, 97.5 m May 6, 1980 ' May 15, 1980 TP m (ST?') 74.4 m May 21, 1980 May 30, 1980 TP m ( 557') 82.3 m June 4, 1980 June 11, 1980 Core size for all four holes was BQ (l 7/16 m inches or 36.5 m in diameter), Drilling was performed by Bradley Bros. Ltd., Timmins, Ontario. JFG/kd

loionjo. TP19805 'rodfrty A 9.10 'ownship Little ocation L 500 E 225 N CXK)"d By J MS ore Location Timmins lum.irhs Length 174 m Ocarina 0 Q Dio 60" Objective COUCTOR B Grid A,9, 10 Bus Gp.

4 loionjo. TP19805 'rodfrty A 9.10 'ownship Little ocation L 500 E 225 N CXK)"d By J MS ore Location Timmins lum.irhs Length 174 m Ocarina 0 Q Dio 60" Objective COUCTOR B Grid A,9, 10 Bus Gp. DIAMO DRILL RECORD Comment 6 May 1980 ^ Completed 15 May 1980 /^ Y j/t 1 Drilling Co Bradley Bros/ /j// Core Si7e y^l ////SI Casing l ofl in Hot*. 7 A^xfsiis~~ 7 / Dip: Collar h( \^ Etch' Fest Depth Rdg. True 98.8 m 71" 64^' m O Hole No. Location Sketch IT C P" TP19805 Nprtli Clai TiNo. 51 Sea o 1" l ** ' i o' Footage Prom r OVERBURDEN, sand and large boulders D E S C R 1 P T 1 O N No. Length Cu Zn Au Ag 94.8 m 97.5 m 97.5 T 99.5 r CASING REAMED INTO BEDROCK, no core i AESITIC METAVOLCAN1C fine grained, medium green colour, chloritic partings cut by carbonate stringers at average 300 to core axis but rock is ubiguitously carbonated massive texture at start of intersection but rapidly becomes tuffaceous in appearance. The portion 98il m 99.4 m is cut by carbonatequartz veinlets subparallel to the core with some graphite associated but no sulphides though d isseminated pyrite present in host rock ^ " , m m m m DACITIC TUFF finegrained, medium green colour fainlv hard small quartz eves present trace pyrite ubiquitous carbonate and carbonate strineers GRAPHITIC CHERTY ARGILLITE black arpillite, fairly hard but graphitic along. partings sulphide (pyrite) rich at contact with preceding rock type contact at 20O at core axis brecciated and abundant auartzcarbonate stringers at lower contact * * * V. V EAK CC NIHtCTl * K""" m i DACITIC TUFF Similar in appearance to previous tuff unit (99.5 m IO3.6 m) but contains sub rounded to angular fragments and shards of black material similar in appearance to the preceding black argillite

"Moreen DIAMO DRILL RECORD. 273 Sheet No. ll± Footage DESCRIPTION CONTINUED: largest fragment about 10 cm and there are no fragments larger than 5 cm after 105.

5 "Moreen DIAMO DRILL RECORD. 273 Sheet No. ll± Footage DESCRIPTION CONTINUED: largest fragment about 10 cm and there are no fragments larger than 5 cm after m stringers of carbonate still present as well as dark string of chlorite trace disseminated pyrite as well as the occasional lens of pyrite. No.. Length Cu Zn Au m BLACK ARGILLITE narrow zone of argillite and argillaceous zones interbedded with the tuff largest zone about l cm thick but there are several other very thin bands present bedding appearance seems to indicate tops are down the hole. bedding angle still about 20 to core axis darker band of tuff overlies (?) this zone and contains wispy lenses of fine grained pyrite carbonate stringer parallels lower contact of argillite and tuff m DACITIC TUFF slmilar to previous intersection of dacitic tuff some sections are predominantly composed of crystal fragments shards and fragments of argillite are still present m rr CHERTY GRAPHITIC TUFF black argillaceous fragments with quartz, carbonate V. WE/ K CONI UCTOR graphite and probable tuffaceous material at least some of the quartz appears rather granular and may be a crystallized chert carbonate occurs subparallel to bedding (about 20 to the core axis) and at 90 to the core axis. tuffaceous material is very light grey in colour only traces of sulphide (pyrite) is present (pyrite cubes and sheens along graphitic partings) the unit is not continuous over the width of the intersection but is broken up by 0.3'm wide intervals of dacitic tuff containing stockworks of black material (graphite?) m IT DACITIC TUFF similar to previous intersections m m coarse xl and lithic tuff a few large ( l cm) buff coloured fragments, no shards of argillite observed after m, four separate beds observed, contacts at m, m contacts marked by the prcsjence of very thin bands; of^ black argillite, a brecciated appearance to the rock and the presence of buff coloured material.

l"**tt Kneurtct Umit*4. DIAMO DRILL RECORD Hole No TP1 980 Shoe! No. Footago ^145. 4 J 146.

6 l"**tt Kneurtct Umit*4. DIAMO DRILL RECORD Hole No TP1 980 Shoe! No. Footago ^ J n DESCRIPTION DACITIC METAVOLCANIC similar in colour to tuff, very fine grained and no evidence of tuffaceous fragments No. Length Cu Zn Au Aq 1/16.9 J r DACITIC TUFF approaching lapilli size with coarse xl and lithic fragments black shards once again present narrow quartz, breccia zone about m sulphide (pyrite) content of the rocks is still only trace quantity J 153 m GRAPHITIC TUFF dacitic tuff with stockwork of fine graphitic stringers and larger zones of quartzcarbonategraphite at low angle to core ( 10~ 20 ) from m 153 m a few cubes of pyrite are associated ~ 153 m t r r r r r 174 m. DACITIC TUFF.typical as previously described, a few zones of large xlrich sections are present possible graded bedding around m with tops indicated down the hole bedding angle still about 20" to core axis ' i DACITIC TUFF tuff appears darker in colour large block of black argillite at m, some very wispy pyrite lenses m m brecciated and contorted by late quartzcarbonate veins and vcinlcts. ' DACITIC TUFF typical intersection with zones of xlrich sections INTERBEDDED TUFFS A ARGILLITE dacitic tuffs varying from fine grained medium green to medium to light green xl tuff (good contacts between these tuffs) most argillite occurs as fragments in the tuff and as narrow strings but m 172 m s ection of very fine grained medium hardness argillite containing a fine 7, o f very fine gralnedjjyrite locally, argillite does not appear to be particularly graphitic m m another argillite band. * 2316 ^ *, m E OF HOLE

Norcen VJUfW limited DIAMO DRILL RECORD (lole No. oicno TP 19806 "OPt'cly A 9 T 10 ownship L i 1 1 lo :K,..on L 125 K 87.5 N wood By JMS TO Location TIMMINS emuv, Footage Prom 0 74.

7 Norcen VJUfW limited DIAMO DRILL RECORD (lole No. oicno TP "OPt'cly A 9 T 10 ownship L i 1 1 lo :K,..on L 125 K 87.5 N wood By JMS TO Location TIMMINS emuv, Footage Prom m Length OVERBURDEN A CASING sand and gravel boulders near bedrock m' Bearing 180 Dio 65 Objective COUCTOR A Grid A9 r 10 Bus Gp. D E S C R 1 P T 1 O N Commenced 21 Mny 1 98O ^^ S~] Dip: Collar 6S O Completed 30 Mnv 1980X" /f /Si DrillingCo. Bradley B/os. /7/^/ Etch " Fest Depth Rdg. True 79.2 m O B(X^v f/ /a ' Casing Left in Hole ~S f^iss]ff2~ m 58" 49^" (A ^^(^/^^~ ^ ^c^^ f ' / X 7 No. Length Cu to C5zd.'' Location Sketch j""' Zn Au Rg North t Claim No..51*724 Scale: m DACITICRHYODACTIC VOLCANIC autobrecciated appearance, fragments appear to fit back together largest fragments. up to a few cemtimetres dark, mafix between fragments probably chloritic but may be slightly graphitic in past, bedding/foliation about 40" to axis of core, portions definitely tuffaceous looking light green colour, rare pyrite, occasional carbonate veinlet subparallel to the axis of core, gradational contact with next rock type., m 88.4 m INTERBEDDED DACITIC TUFF A ARGILLITE 2319 intimately interbedded rock types proportions of each constituent vary continuously over the length pf the intersectit n had thicknesses from mm up to 2 cm, ubiquitous carbonate in patches and,crosscuttit g microfaultcd veinlets, very chloritic along partings, some partings may be uraphitic, some tuffaceous fragments up to lapilli size occasional pyriterich bed (with up to 17. jjyrite) bedding about 45" to the axis of the core, some portions of the tuff bands are silicified or possibly cherty argillite becomes dominant towards end of intersection ^ m m ARGILLITE banded dark and lighter bands dark bands, very thin, dark green to black, very chloritic especially noticeable along partings, occasional tuff band mostly of intermediate composition and no wider than about 1 cm. Banding at 450 to the axis of the core, carbonate^ strings in variable orientations from subparallel to subperpendicular to axis of the core ^ f

8 DIAMO DRILL RECORD TP Sheet Mn ^ Footage DESCRIPTION continued: (most subparallel though) no obvious distinction between bands on fresh (broken) surface thin darker bands may be more chloritic leading to the development of thejlaty cleavage, occasional pyrite bearing band 93.9 m 94.0 m quartzcarbonate zone subparallel to banding with associated orange earthy carbonate alteration no obvious conductors though there is the possibility of some zones/slips being graphtiic, sampled portions contain the largest pyritebearing bands No. Length n n tt * INTERMEDIATE TO FELSIC (DACITIC) TUFF with interbedded argillite tuff tuff is medium green in colour hardness is variable tuff contains mainly lithe fragments including regular shards of argillite but a few xl (feldspar) rich zones are presents, 3QZ of the intersection is argillite similar to 88.4 m m though in spokes the argillite is definitely cherty in composition, banding bedding about 30" to core axis (146.6 m) pyrite occurs up to 17. locally disseminated in tuff portions, possible' graded bedding in tuffs show tops up the hole (?) banding/bedding about 45 to axis of core (181.7 m) fragments of argillite in tuff occasional up to 2.5 cm in size with angular and subrounded portions within the same fragments fragments also show some elongation parallel to bandingbedding no obvious conductors portions of the argillite bands are brecciated and intimately mixed with the tuffs E OF HOLE... 4^

Hole No. TP 19807 Pronprty A 9, 10 wnship LITTLE Location L 600 N 1537.5 E Logged Ry JMS Corelor*tinn TIMMINS Remarks Footage 0 82.

9 Hole No. TP Pronprty A 9, 10 wnship LITTLE Location L 600 N E Logged Ry JMS Corelor*tinn TIMMINS Remarks Footage m OVERBURDEN A CASING Length ^9 6^ m Bearing o Dip 60" Objective COUCTOR C Grid A9, 10 BUS Gp. DIAMO DRILL RECORD D E S C R 1 P T 1 O N Commenced ^ June 1980 /^ Djp. CjcM!tT 6 0" Completed U J" n e l^j Y J/ J DrillingCo. Bradley.Bj?6s. /X X ' EtchPest Depth Rdg. True Core Size BQ ^*jfc J/ /f~ 82.3 m O Casing Left in Hole S l/ \4 S /[LL*^ m 6 7V/." 60^7." f I ^*S^S*' (^~ s / ' No. Length Hole No.. TP19807 Location Sketch North in ' "rfp Clai n No. 5/5 740 Sea e: l" f 320' 82.3 m 89.0 m MAFIC TUFF extremely carbonated matrix and numerous crosscutting carbonate (calcite) stringers at varying orientations matrix colour variable medium green to light numerous phenocrvsts ("eves") of calcite and green to yellowish green auartz calcite eyes up to 1 cm in diameter quartz eyes up to 5 mm but average 2 3 mm dark rims occur around most of the eves and is most noticeable around the calcite eyes, quartz is usually fairly dark in colour but may occasionally be clear and show yellowish opalescence eyes from of rock foliation at about 407. to axis of the care abundant carbonate veinlets around 88.4 m 89.0 m 89.3 m QUARTZCARBONATE CEMENTED BRECCIA ZONE earthy altered pieces of quartz and carbonate with a few fragments of mafic tuff within the quartzcarbonate matrix 89.3 m m MAFIC TUFF does not contain quartz or calcite eyes some patchy carbonated zones arejresent medium green colour with numerous dark green shards) slightly chloritic on fresh (broken) to black material (rock fragments and faces matrix is slightly carbonated, foliation about 40" t n,,,, c n r *Ka. *~ 97.5 m m minor interelations of more felsic material (dacite) mostly tuffaceous in nature, some zones containing quartz and calcite eyes observed through this portion, contacts parallel to foliation m m bleached and silicified zone.. *~ 1

Moreen Footage J100.6 m 119.2 m DIAMO DRILL RECORD Hole No.. Sheet No.

10 Moreen Footage J100.6 m m DIAMO DRILL RECORD Hole No.. Sheet No.. DESCRIPTION MAFIC TUFF A AGGLOMERATE iumbled assortment of various mafic tuffs with a few fragments of dacitic or rhyolitic tuff matrix was probably originally very muddy fragments subangular to roundedj probably a large amount of sedimentary reworking occasional zone of broken quartz in black (chloritic?) matrix accompanied by yellowish mineral in very thin bands/layers minor interelations of lighter coloured (mafic felsic) tuffs persist. No. Length TP m m QUARTZCARBONATE CEMENTED BRECCIA ZONE similar to 89.0 m 89.3 m thin layers of yellowish material present m bleached silicified tuff inclusion m m m m MAFIC VOLCANIC medium to dark green colour; slightly chloritic on fresh (broken) faces may be a very fine grained tuff but possible flow breccia features around m and m carbonate veinlets and stringers throughout the intersection, rock itself is not particularly carbonad MAFIC TUFF A AGGLOMERATE similar to m m, most fragments are mafic, very few could be considered dacitic, possible fragments up to 0.3 m mostly tuffaceous in nature, varying from fine to coarse grained tuff with some lapilli size. ed ^ m m MAFIC VOLCANIC similar to m m appears to definitely be more tuffaceous in nature than the previous intersection upper and lower contacts are not clear m m m MAFIC TUFF A. AGGLOMERATE similar to m m, contains a few pinkish rhyolitic angular fragments. up to 5 cm in the lower portion of the hole m m massive section m a few cherty fragments present E OF HOLE *^

11 42A1INE8ie9 24 LITTLE

Work performed by: RALPH E. ALLERSTON (NEWMONT)

41Pt4NE8843 24 SOTHMAN 010 Diamond Drilling Township OF SOTHMAN Report NQ; Work performed by: RALPH E. ALLERSTON (NEWMONT) Claim N9 Hole NO Footage Date Note L. 332897 L. 332898 H-l-73 H-2-73 613' 587'