coral lime s chemicals ltd

4?I04NE000G g. l 33 VALFNTINE 010 : ?.]33

:: October 28, 1970,

TW; MINING ACT

SSr.SSMjOT WORK CRKDJTS

BM (Hi)

NAMl: OF APPLICANT:

COMPANY WHICH PLRPORMKl! WORK:

TYPJ: O! 1 WORK:

Coral Lime S Chemicals Ltd.

Selco Exploration Co., Ltd.,

p and gcolopJcaJ mapping for Diamonds.

Valentine and Kilmer.

July 24 to October ?, 19G9.

TOWNSHIPS:

DATi:S O!' WORK:

AMOUNT EXPENDED:

NUMBER o!- ASSESSMENT DAYS ALLOWED: 963.NUMBERS OP CLAIMS ON WHICH

WORK DONE: P 234533 to 38 inclusive

RPCORDlNf, 01' WORK: These claims may be grouped under Sec. 83(6) for the purpose of recording this work

33

SUMMARY

In the vicinity of the diamond discovery nearCora] Rapids 39-'i cubic yards from various types of unconsolidated formations vere washed t No diamonds were found.

COKCLUSJOHr,

1. The sampling programme failed to confirm the presence of diamonds nor did it produce any information to 5;upport tlie c J.aim that diamonds had been found in the area.

2. Geo.logi.cal mapping did not result in the discovery of kimberlite. "Kimbcrlitic" rocks reported by Brown et al arc not true kimberJites.

It i s recommended that the claims in the Coral Rapids area be relinquished.

ACKNOWLKDGKi-JKNTS

Our thanks are due to all those in the office in Toronto who helped with this project in one way or another. In particular ve would like to thank Alex Gribben who did much to organize the project in its planning stages and who helped to orient ? strangers in Toronto. Our thanks are also due to D.Watson for his hospitality in Swastika and also for the efficiency with which he organized the expedition to Coral Rapids, and maintained our camp there.

l l l l l l l l l l l l l l l l l l l l l

1. Sample log sheets (U.K.)

P. Sketch map of Coral Rapids (li.E.)

3. Geo.lotfical map of the Coral lipide area (P.G.B.)

h. Cross sections end pit sections (P.G.R.)

^. Sketch map of breccia, at Coral Rapids (P.O.B.)

6. ])ia[!,rtivi of breccia outcrop by Brown ct al.

1. RROUj'J, I).P. j, BK'liWJT, G., and GKORGK, P.T., (1967): The sourceof alluvia] kimberlite indicator minerals in the James Hay Lowland. Ontario Bept.Mines, Misc. Paper, MF Y.

2. BKOWII, J).])., BKNJIKTT, G., and GKORGK, P.T., (1967): OperationKapUKlU'.sinf.',, Can.Min.Jour., 88, pp. 129-136.

3. GKKHY'J'Sj K. (19^9): Jleport on the Coral Rapids (Canada) diamonddiscovery. Internal report Selection Trust Kxplox-ation Liwited, 3rd July 19^9.

It. MCOMBK, P.G. (.1968): Report on the Otter-Coral Rapids property.Internal report Kimberlite Mining Corporation Ltd.

5. SKIMMING, T. (l^uO): Report on the James Bay Lowlands project.Internal report Selco Kxploration Company Ltd.

6. TRl 1;5BLA.Y, M. (3.9f'3): Report of operations within the licencearea. Exploratory licence of occupation 1330h. Internal report Canadian Rock Company Limited.

7. OTTl.K RAPilDS SHKW. Ontario Dept. Mines, PrcOirninary GeologicalMap P. 370.

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The Coral Rapids investigation was prompted by the claim that two diamonds had been found on the left bank of the Abitibi river by claim stakers employed by a syndicate pegging for limestone. (For the circumstances of the discovery see reference 3).

Subsequently an agreement was made between Selco Exploration arid the syndicate and it was arranged to carry out sampling to evaluate this discovery.

Dr. P. Gratton-Bellew arrived in Canada on the ?hth July to supervise the construction of prospecting equipment etc. lie was joined by Mr. K. Edwards at Kirkland Lake on the 26th August. A camp was established near the "discovery site" on the 2nd September. Sample treatment and geological mapping was completed on the 2nd October.

N. Edwards directed the sampling, pitting andwashing while I'. Gratton-Bcllew did the geological mapping and the microscopic examination of the fine grained concentrates. Relevant parts of this report are marked by their respective initials H.E. or P.G.B.

LOCATION

The discovery site is on the left bank of theAbitibi river just above Cora]. Rapids in Valentine Township (see plate 1).

The Coral Rapids are about 300 miles south of James Hay. The area is in the Porcupine Mining Division of the District of Cochrane. The Ontario Northland Railway which runs from Cochrane to Moosonee (distance 1.60 miles) passes through the area, more or less parallel to the Abitibi river, and provides a ready means of access. A camp was set up alongside the railway at mile 99 (north of Cochrane). An old track, l mile long, leads to the river from mile 99 on the Cochrane-Moosonee railway.

The site of the diamond discovery is 950 feetsouth of the point where the track meets the river bank. At the site an old landslip of the steep river bank has resulted in a semi-circular cliff, on the face of which is exposed a "boulder clay overlain by Abitibi river terrace gravel. The diamonds are claimed to have been picked up in little pools washed in the boulder clay formation.

HISTORY

The first records of diamond exploration in theCoral Rapids area are contained in a report on the "James Bay Low lands Project" by T.Skimming for Selco Exploration Company Ltd. (i960).

...A


Samples of lover gravel vcro pynncd to yield from one to three ounce::; of concentrate. 9'' sampler, vere examined; 1^ vere found to contain pyrope garnet, presumed)] y derived from kimbcrlites. The discovery of ki.mbcr.! ite minerals in the drainage system of the James Hay Lowlands indicates that kimberliter;, and possib.ly diamonds, occur in the area. Little pyrope vas found in the samples tuid the grains vere smtOl, suggesting that they had "possibly" been transported, for some distance fro; i their f-our co. Pyrope garnet vas found hi the Hattaganj and Li.bble Abitibi Rivers but not in the Abitibi. Despite the occurrence of kimberlite Minerals in the area the nature of the: terrain, i.e. muskeg and forests, necessitates a fairly extensive program of sampling to discover kimberlite occurrences. Company policy at that time evident]y did not permit eiaba.rki.ng on such a program. (See "Knc3.osu.re F" to letter number '(lo1 , January 196.1 from T. Parks to the Secretary of .Selection Trust Limited, London, England).

Cora.1 Rapid-; subsequently carried out JniticJly sm the Abitibi, in the grave gravel sampl and concentr abandoned.

3n ]9^? licences to explore for diamonds in the area vere granted to VI.C. Wahl Limited and these wore transferred to the Canadian Rock Cô. îî/ted, who exploration during the 196^-^3 season, see reference 6. .J.] reconnaissance samples were taken in the rivers of drainage system. The presence of kimberlite minerals Is of the Little Abitibi River was confirmed. Large es (]-3 cubic yards) wore then taken at selected sites ated. ?Io diamonds were discovered and the project was

In 1966 outcrops, considered to be kirabcrlitic, vere identified in the Abitibi River, in the vicinity of Coral Rapids, by Messrs. IVovn et al vorking for the Ontario Department of Mines (see reference l arid 2). The kimberlite.*; vere sampled by the "Kimberlite Mining Corporation Limited.". (see reference 'l). Three samples varying froî 600 to 800 pounds in \;eight, vere taken from the kimbex-lite outcrops, the material vras not concentrated, "liejiresertative sa^nxles", of unstated veight, vrere sent to laboratori to be checked for heavy mineral and diamond content. The results of these tests are not available, but it is unlike.!y that diamonds vould have been discovered in such small quantities of kimberlite; presumably they vcro not, as no further work, vas undertaken by the Company.

In June 19^9 the alleged discovery of tvo diamonds at Coral Rapids resulted in the recent investigation.

GEOLOGY (P.G.}3. and U.K.

Aims of the mapping program

There vere tvo reasons for. mapping the area:-

1. to discover the location of the gravels of the Abitibi River terraces and of the marine raised beach deposits.

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Oiler rapids ir; forced by large outcrop:.; of pre cambrian gneiss; Sextant Hti.pi.ds "by a large sill like mass of lamprophyre; Coral Rapids is formed where the river cuts through the Coral.--beari.ng limestone of the Abitibi River Formation (see plate -3); Lone; Rapids and it r, island arc formed by the impure dolomitic .limestone and shale of the Williams Island Formation.

Vegetation

The muskeg which covers the area supports a dense growth of vegetation near the Abitibi River. Spruce trees are dominant, but between the scarp and the river, poplar, birch and cedar also occur. Proceeding avay from the river, on both sides, the Muskeg becomes more swampy and the tree cove}- less dense. West of the railway the muskeg forms a vast swynp which is only sparcely covered by stunted spruce or tamarisk trees (see plate 2). Most of the beaches are covered by a dense growth of pine trees which contrt-st markedly with the spruce of the surrounding muskeg.

Strat i

Pro- cambrian gneiss outcrops at Otter Rapids at the southern end of the area which was mapped. To the north of Otter Rapids the: pre-ct.mbrian is overlain by paleozoic sediments. The sediments which are of Devonian age are flat lying, and gently folded. In the vicinity of Coral Rapids the Devonian rocks arc- represented by coral-bearing .limestones, ai'kose and shale.

The paDeo/.oic rocks are intruded by dykes and sills of lamprophyre and associated calcareous basic breccia. The paleozoic rocks are overlain by glacial deposits of pleistocene age. In the Coral Rapids area, boulder clays, containing pebbles shoving glacial striation?., overlie the arkose and limestone.

Recent deposits consist of boulders, clay, marine terraces (raised beaches) and alluvial gravels. The retreat of the continental ice sheet was followed by extensions of the sea, which advanced as far as the edge of the pre-carabrian shield.

Isostatic adjustment, following the removal of the ice ce.,p, resulted in uplift of the land mass and consequent retreat of the sea. Abandoned shore line features, in the form of raised beach gravels, were left behind, each pause being represented by a ridge of sand containing lenses of fine gravel. The southern most of these gravels occurs ncj.r Otter Rapids and the gravel ridges extend northwards to the present shoreline of Hudson Bay and James Bay.

Rivers, developed on the resulting flat plain,. initially formed vide meander belts with insignificant divides between the drainage system;. Widespread gravels were deposited which now appear a? terraces cf rivers such as the Abitibi. Over their meander belts the revised, beaches were destroyed so that the lateral boundaries of the river gravels are now indicated by the truncated edges of the raised beach ridges.

Recent rejuvenation has resulted in the incision of the major rivers and the Abitibi now flows in a gorge some 70-80 ft. below the level of the plain. The old gravels are now exposed in two terraces at the top of the steep river banks.

.../Y

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Upper Terraces. The upper terraces vary in height from YO to fiB feet above the river in the vicinity of Coral Kupichs. Cross-'Suction "A" (attachment h) shows a hypothetical section of the area, based on the information obtained from pitting. Sufficient information was not obtained from which to draw an accurate section, but some idea of the stratigraphy way be obtained from Section A. The upper terrace consists of sand with gravel lenses and vica versa. These grave] s are underlain by glacial, clay containing striated pebbles. The extent of the high terrace is uncertain as sufficient information was not obtained from the traverses to define it, but it may ve]l extend most of the vay along the vest bank of the river (see pintos 6 and 7)*

Low Terraces. Low terraces, which varied from about 20 to 35 feet above the river, occur at two placer, on the east bank. They appeal- to consist of sand vi.th gravel lenses. The two low terraces occupy sections of an old river channel (see attachment 3).

A hypothetical section across the southern low terrace and river valley is shown in attachment h as Section "B". A low terrace consisting of sand overlain by gravel is shown in plate 5-

Intrusive^ rocks

Four types of basic to ultrabasic intrusive rocks occur in the Coral Rapids area. They are

1. lamprophyre sills

2. Lamprophyre dykes

3. Harrow breccia dykes

H. Breccia pipe (?)

^* Jda'!lP.119Ji^.yZ?,.JL^-l-l- i:l outcrop in the bed of theriver at Sextant. Rapids and in the west bank at Cora3. Rapids (reference l and H). Reference h describes the Sextant Rapids sill as kimberlite, but 35rown ct al (ref. l) call it augite- lamprophyre. We agree with the 3atter interpretation and did not find any rock even vaguely resembling kimberlite at Sextant Rapids, so it is concluded that this rock was misidentified by geologists of the Kimberlite Mining Corporation.

.J^ylKCJi cu"t through the limestone and arkose in the west bank at Coral Rapids for about l mile (see ref. l page I'l and attachment 5)- On the Otter Rapids sheet (ref. Y) a composite Jtaiprophyre-kinborD ite dyke is shown which is also discussed by Brown et al (ref s. l i;nd 2). Ho outcrops of kimberlite were found by us in the vicinity of the lamprophyre dyke. Kimberlite was also reported to have been intersected in a bore hole by Ontario Hydro. The cores were investigated in thin section and analysed by Brown et al (ref. 3 ) and described as

"pale green, moderately soft, and exhibits a frag mental texture. The fragment form about 10# of the rock, arc rounded clark green microcrystalline basaltic fragment s l mru to 2 en in diameter, xenoliths of rounded, altered granitic basement rock l to 2 cm in diameter and rounded quart?, grains, and cleavage fragments of plagioclase, microcline and colourless kyanite ...... The matrix is composed

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of 12# serpentinized clinopyroxene, 3# phlogopite, 10# calcite, 8/5 magnetite, 2/5 ilmenite and 63^ clay minerals ....... An electron microprobeanalyses of the ilmenite gave a large amount of magnesium and iron but only a minor amount of titanium".

As no pyrope or chrome diopside were found in the rock, it vas described as "kimberlitic" rather than kimberlite, but it appears to us to resemble the breccia dykes described belov.

3. Narrow breccia dykes. (see plate 12) Twelve narrovr dykes of soft, dark green altered basic rock intrude the arkose bed rock on the vest bank at Coral Rapids along a distance of about 160 ft. In the same stretch occur 2 lamprophyre dykes, one 2 ft. and the other 9 ft. vide, striking in the same southvest direction as the breccia dykes. The latter are irregular in shape and frequently branched, they vary in vidth from less than one centimetre, vhere they have come up along fractures to about 50 cm wide. The breccia dykes frequently contain inclusions of arkose. Some sections of the dykes appear to be composed almost entirely of arkose.

The rock vhich has a dark olive green colour is very weathered. It is moderately magnetic. In the hand specimen it is virtually impossible to identify any minerals. Numerous rounded grains of soft green material occur, which may represent serpentine replacing olivine. Some calcite also occurs in the rock but whether primary or secondary is not known. A sample of the basic breccia was crushed and panned. The only minerals which were.found were phlogophite, a small amount of zeolite, pyrite and a trace of chalcopyrite. The pyrite is assumed to be of secondary origin, but no evidence of this was found.

14. ^^ccia^Hpje. About \ mile above the rapids, a large lamprophyre intrusion is exposed in the west side of the river bed at low water. The intrusion is a peculiar feature; between thick vertical dykes of fine grained lamprophyre occurs a circular body, about 150 ft. in diameter, consisting of a coarse breccia containing coarse^angular to rounded pieces of a variety of basement rock types. The matrix of the breccia is greenish grey in colour and consists of numerous small black grains which impart an almost mottled appearance to it. A few grains of phlogophite and some calcite were identified. Calcite also occurs in veinlets, about 0.5 mm wide. A sample of the rock which was crushed and panned yielded a concentrate consisting of about 60^ magnetite, some barite and pyrite were also found. The remainder of the concentrate was composed of weathered, unrecognizable grains of a greenish mineral. The breccia contains numerous inclusions of limestone and shale which vary in size from a 0.5 to about 30 cm in size. The contact between the breccia is sharp at the south and gradational at the north. The eastern part of the lamprophyre/ breccia intrusion is obscured by a thick accumulation of boulders.

An extensive magnetic anomaly has been located by the syndicate in the plain west of the river at this point and it seems more than likely that the anomaly is due to a large intrusion of which the various lamprophyric and other basic dykes are the dpophyses. This appears to be confirmed by the fact that the projected strike of the various intrusions meet in the area of the anomaly. A sketch map of the lamprophyre dyke and the

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associated breccia is shown in attachment 5- This lamprophyre complex is also illustrated by Brown et al (p. Ih ref. l) but their interpretation does not agree with ours (see attachment 6). The relationship of the breccia to the lamprophyre is not clear notwithstanding the sharp contact at the south. The limestone outcrop which lies to the west of the breccia is gently folded. The fold axis plunges cast at about 10 degrees. To sum up the basic calcareous breccias which were described above have a superficial resemblance to kimberlite, however, the total absence of any of the kimberlite minerals: diamond, pyrope garnet, ilmenite or chroine-diopside, indicates that the rock is not kimberlite, and to call such rocks kiruberlitic can only be misleading.

Str

An extensive structural feature in the form of a horst block, stretches from the vicinity of Moosonee in a SSW direction for over 200 miles (ref. 2). The bed rock of the horst is gneissic granulite. A magnetic high corresponds with the main portion of the horst while a gravity low runs parallel to it at 25 miles to the west.

T J NG ( N . E .

If the discovery site was correctly indicated then the obvious local source of the diamonds was the Abitibi river terrace gravels overlying the boulder clay. This gravel was sampled at the discovery site and at three other places. The boulder clay and certain marine terrace gravels (raised beaches) were also sampled. Sample l, 2 and 3 were taken from the Abitibi river high terrace; sample h from the underlying boulder clay; sample 5 and 6 from the marine raised beaches; and sample 7 from an Abitibi low terrace in a cut-off meander.

From these three different types of unconsolidated material a total of 39- cubic yards was washed. The attached log sheets (Attachments 1) give details of the samples. Sample locations and pit sections are shown oh the maps (Attachments 3 and 14).

River terrace gravel . The high terrace gravels of the Abitibi are extensively developed on both sides of the river which is now incised with steep banks, some 70 to 90 feet below the plain on which the old gravels were deposited. The gravel varies in thickness from lg to 10 feet and is covered with a thin over burden of sand which is overlain by root mat and swamp soil. The gravels consist of rounded pebbles in a sand matrix. Pebble constituents are buff-coloured limestone (60^) and a variety of pre-cambrian rock types (IjO/O, including granite-gneiss, amphibolite, quartz, etc., biotite schist and pegmatite. Pebbles are generally rounded but range from sub-angular to well-rounded. The gravel is mostly well stratified with the coarsest material at the base. In places there are lenses of sand between the gravel. Average pebble size is two inches and largest is eight inches.

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Boulder Clay. This material underlies; the riverterrace gravels ut the "discovery" r;ite and. is a3.so the substratum at the sites along the left bank where other terrace gravel sampler, were taken. It ir. undoubtedly u boulder clay of glacial, origin. The clay ir; gi'ey 21) colour and plastic vhen vet. Boulders, cobbles and pebble:;, inof.it of which show striation^ are scattered at random throughout the clay. At the cliff exposure the clay is ho to ^0 ft. thick and rests on a coarse grained arkose (the Lower Devonian Sextant f on..1 cation). The material washed war; taken from a sun-dried skin, r- oro e 3 to h inches thick, on the cliff face.

Raised beaches. Raised beaches are present in theCoral Rapids area, but not in the immediate vicinity of the "discovery" site. The gravels are clear3.y differentiated from the river terrace gravel s in that they contain sea shells. The shells are not obvious on casual inflection of the gravel. s but show up tit the top of the light fraction when jigging and gravitating.

The basal, gravel was washed at two places. The pebble constituents are similar to those of the river terrace gravels and. contain the same proportion (60/Ho) of buff limestone and basement rock varieties.

Concentrates were similar in volume and minerals to those of the river terrace gravels, a3.mandi.ne garnet being the dominant mineral in the -i? mm size range.

The two small samples washed should not be reg as being in any way conclusive. Sampling to determine whether the raised beaches of the James Bay lowlands contain diamonds would bc a task beyond the resources of this investigation.

tes. The concentrate varied in quantity but the same luinerals appeared in each type of sample. In general the percentage of concentrate was small, considering the fact that an abundant supply of heavy mineral occurs in the basement garneti ferous gneisses upstream.

The pebble constituents of the gravels were reflected in the jigged materia3. which also showed a ligh fraction (60/0 of buff limestone grains and a darf, heavier, fraction piCv) of derived grai ns.

The -i-f! Kin concentrate was almost entirely composed of almandine garnet, Mostly showing crystal faces. A few grains only of possible pyrope were present. The only other heavy mineral in the -l-2 mm fraction was epidote.

The river terrace gravel and raised, beach gravels contained similar percentages of concentrate (a few cubic centi metres of -i-? mm garnet per cubic yard).

The boulder cloy gave a negligible account of concentrate consisting of a few grains of garnet only.

The riffle concentrates (-2 mm) were collected from each sample and. were being examined under the binocular microscope by Mr. Oratton--Bc.Llew.

.../li

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2 Labourers were engaged on pitting with pick and shovel. The deepest pit was 10g feet and no difficulty was en countered in getting down to bedrock. The gravel was loaded from the pit straight into a swamp "buggy for transport to the working site. Water seepage was removed by bucket with occasional assistance of a lg" centrifugal pump.

Transport

Gravel was transported from pits to washing site by the swamp buggy, which was hired, together with the driver from a contractor in Timmins. The vehicle proved extremely useful and is probably the only satisfactory method of transporting loads across muskeg swamp.

The type used was a "Bombadier" model J.S. It is a tracked vehicle with 2 drive sprockets and 6 pneumatic wheels. The tracks are continuous rubber belts with replaceable steel treads. Power unit is a 251 BHP Chrysler engine; load capacity is 1200-13001bs.

Washing (see plates 8 to li).

Gravel was sized by footshakers into -HO mm, -10+it mm and -^1+2 mm fractions. A riffled sluice box collected -2 mm concentrate. The +10+1* and -h+2 sizes were concentrated in a Joplin jig. The concentrate from the jig was removed at intervals and gravitated. Each batch of concentrate from the jig was gravitated 3 times, the "Eye" being examined for diamonds and concentrate collected. Gravitator tailings were returned to the jig. The riffle cleanup was screened through a 0.7 wm sieve. The +O.T mm fractions was jigged in a Bert jig and concentrates collected. The -0.7 mm size was panned down.

Examination of -2 mm concentrate ( P . G . B . )

The average mineral composition of the high and low river terraces are very similar. About 5 to 10^ of the -2 mra +0.7 mm concentrate consists of rnagnejbitji which occurs as rounded to angular grains and well formed octahedra. Pinkish purple coloured garnets are common, pale amethyst coloured ones also occur but are less common. Both types of garnet occur as angular grains and well formed crystals (rhombic dodecahedr^. Their euhedral shape suggests that they are most unlikely to be of kimberlitic origin. jKenatite! and ^hrorrdt^e occur as rounded grains in the concentrate. Occasional grains of pale green pyroxene and flakes of phlqgophite were also observed. jRarit^e occuring as rounded grains is moderately common. Dark greenish black, rather weathered rounded grains of pyroxene/ amphibole? are also common. Sample 7 (low terrace gravel) had very little concentrate in this size fraction

The -0.7 mm fraction had considerably more heavyminerals than the previous fraction; this is normal in most gravels. M^net^tjD makes up from 10 to 35 percent of this fraction. Garnet is also very plentiful, both the purple and amathyst coloured types are found; the latter are not as numerous as the former. No garnets which might be of kimberlite origin were seen. Well formed crystals of greenish black amphibole are common in all samples. Somewhat less plentiful are angular grains of pale green

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pyroxene. 'J'opa^ comprises about l /o of the samples, it occur;; t 1,:; pale pink rounded grains vith corroded surface:;. (Topax grains are common in the eon c on l rat ea in most pre-cambrian ai-ear.0. A l'evT phlof.op-'i te flakes were found in MO y t samples but the rui.nc.rcJ in not conaon. Occasional minute crystals of zircon vere observed in mo .s t samples. Chromite occurs frequently as we] 3 developed octahcdra '.,vir] as rounded grains in most samples. It was dis tinguished from magnetite by its non-magnetic character. A few Minute black rounded, grains which are thought to be i^J'l^.V'A'c..- were found in .sample l and 2.V'hen broken, these grains appeared similar to fractured specimen:; of ilmenite fron kimberlite. Due to the extremely small sifcc of the grains, however, it is impossible to be certain of their i dent i. f i cat i, on. They could be chromite? The grains of ilmenite are too small for analysis , and in any case, it is difficult to be sure, even from an analysis whether an isenite is derived from a kimberlite of from some other basic roc!: .

The concentrates from the marine raised beach are cssenti ally similar to those of the river terrace gravels, but a sma.11 quantity of pyrite and analcime were found in both samples. No ilmenite was observed.

-i ( P - G . B . )

These samples were taken in order to determine the heavy miner;;! content of various sands and gravels which were found in the area, and also to determine the mineral content of the basic breccia.

Sampler, l, 2 and 't were taken from small freshets washing down into the Abitibi river from the terraces. Sample l was taken from the bend, on the west bank of the Abitibi Hlver just north of Coral Rapids. Sa.mp.le 2 was taken from a freshet in the landslide bcD.ow Pit Sample 2. Sample h was located) in a small landslide just north of the limestone bluff on the west bank of the river at Coral Rapids. Samples 3 and 5 were taken from concentrations of garnet sand in the Abitibi river. Sample 3 was taken just north of Coral Rapids, sample 5 was taken from near the big lamprophyre dyke g mile south of Coral Kapids. Samples 6 and Y were specimens of basic breccia which were crushed and then panned. These have already been described in the section on geology. Sample 8 was taken from some gravel in the Onakawana River, west of the bend on the railway at Coral Rapids Station and sample 9 from angular quartz grit in the Abitibi. River.

The mineralogy of the concentrates of the pan samples was similar to that of the river terrace sampj.es except for a lower content of magnetite. In ^sa-ople^l well formed crystals of barite are common. It was identified by its orthorhombic crystal form. Pale green pyroxene, is less common than in the river , terrace gravels. In .sajap\e^2 barite is also common. A few wedge-shaped crystals of .spj.ienq vere observed, otherwise the mineralogy of this sample was similar to that of the average gravel. /Jamjple 3 is similar to the average except for the presence of pjyritjs which is common. Chromite is also rather more plentiful than in most samples. îl'l^-l^Ji ^ s similar to 3, except for the absence of pyrite. A few grains of mica were seen. Pale green pyroxene is less common than in the average concentrate. .Sa;:vple Ji. differs from the others in that it contains vc7 -y little crystalline pyroxene or amphibole. Botryoidal hernatjrte and CiO;' ;.J;.hitje e.re coramon. As is to be expected. from a garnet sand, XSAll'.li?:î are very plentiful in the concentrate. Small grains of ^cirrto^ also occur and a few yellow grains of pji .lo .ôphite were seen. jHample 8^ (from the Anakavana river) contains

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very little concentrate. Only a few grains of H^GHetajt^e were seen. Both purple and amethyst coloured arnets^ occur but both are scarce. A small quantity of amphibole, pjroxe^ne and a few rounded grains of pink topa'/. also occur,

In sample^), despite the fact that the quartz grit appears to be very pure, the concentrate is similar to that of most other samples. Octahedra of magnetite and ^hromite are common, a few rounded grains which were tentatively identified as jspJjieJL were also seen. A few grains of ^analcime were also present. JPyjrite is moderately common, it occurs as well developed crystals and irregular flakes. A few minute zircon crystals were also seen. Most pan-fulls of grit yielded one or two small colours of gold. The quartz grit beaches are derived from the sand and grit com prising the low terraces. The amount of quartz grit seen in them is small and it it; therefore unlikely that gold in economic quantities could be recovered from it.

COMMKHTS

The sampling results, although not exhaustive, are regarded as sufficient indication that the area is not of interest as a source of diamonds.

It is fairly common knowledge that northern Ontario is considered to be favourable country for diamond occurrences. Kimberlite does occur in the Kirkland Lake district (a fissure on the Upper Canada Mine), and the publication "Operation Kapus kasing" describes altered basic intrusions at Coral Rapids as "kimberlitic". Pyrope garnet has been found in several, rivers draining northwards into James Bay. As far back as 1899 W.H.Hobbs conjectured, that isolated diamonds, found in glacial drift of the Great Lakes region may have derived from sources in northern Ontario. More recently it has been suggested that the presence of the horst block and the associated gravity low in northern Ontario are further evidence of structural favourability for kimberlite intrusion. ,

The only thing lacking is a confirmed diamond discovery.

If diamonds had been found in the gravels sampled during this investigation then a large scale programme of terrace gravel sampling would have been justified as the gravels are very extensively developed.

On the other hand the sparsity of heavy mineralconcentrate in the gravels certainly suggests that economic alluvial deposits are unlikely.

If attention is again directed to the area, prompted perhaps by a confirmed diamond discovery, it is suggested that the raised beaches be investigated. The ridges themselves possibly represent storm beach accumulations with poor concentration. The zone of maximum concentration probably lies on the seaward side of the ridge. The best technique would be to auger at short intervals on a line normal to the ridge to establish the best zone of concentration (li. Edwards).

It must bo considered that in a faet-flowing river such as the Abitibi, diamonds are unlikely to be concentrated in the gravels except under exceptional circumstances, e.c- a whirl pool at a bend in the river. The chance of 2 diamonds being recovered from a handful of concentrate is almost nil when a large volume of it from the same area yielded none. As more than adequate sampled from all the likely diamond bearing horizons in this area, including those at the site of the discovery, were tested with negative results, it must be assumed that the dis covered diamonds were incidental and that the river terraces are not potentially diamondiferous.

A few grains, tentatively identified as ilmenite, were found, but their identification is uncertain and the possibility that they might be of kimberlite origin is even less. The more so as no kimberlite garnets were discovered in the Abitibi river in previous prospecting ventures.

Despite the fact that no diamonds were found in the Abitibi river gravels, the James Bay Lowlands is still a prime target area for diamond exploration, owing to the occurrence of pyrope garnet in the drainage system.

Caution must, however, be exercised in drawing any conclusion from the occurrence of a fevr garnets of kimberlite origin in the Mattagami and Little Abitibi rivers, as they could have their origin a considerable distance away. The occurrence of glacial deposits in the area means that the garnets could possibly have been carried south (for hundreds of miles) by the glaciers and have been subsequently concentrated in the river gravels. If this were the case the kirnberlites might even be under James Bay!

The results of the present survey indicate that little, if any, concentration has occurred in the gravel deposits and therefore the chance of discovering diamonds in other grave], deposits in this region is remote. The only possible exceptions are the gravels of the marine raised beaches near the present shores of James Bay. These gravels are probably similar to those of the raised beaches which are sampled at Coral Rapids, but it would be advisable to check this.

Bearing in mind the complex marine, glacial andfluvial history of the area, what methods of prospecting, if any, have a reasonable chance of success? There are basically three techniques which are used in diamond prospecting:-

(i) Heavy Mineral Sampling

This method has been shown to be successful in delimiting large areas, but in the James Bay Lowlands it has not proved successful in narrowing down the target area.

(i i) Gcochetnical Prospecting

Kimberlites have high magnesium, chromium and titanium contents and these minerals might be used to track down kirnberlites and other basic and ultra basic rocks which are also high in these elements. In the James Bay Lowlands the blanket of glacial and/or marine deposits which covers the bedrock would probably render geochemical sampling ineffective.

.../15

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( i i i) G co] il iy r;i c al I'rosjpecting

Aerial magnetometer survey seens to be tlie only technique which might have some chance of success, but vi t h the current] y available equipment and techniques the chances of discovering it, kimberlite pipe by this Method do not seem too good.

The Russian kimberlite^ produce anomalies of about. 1000 i ', vhcn they outcrop at the surface. A cover of 5 metres of uncon solidated materiel 'reduces the anomaly to about 500 J , this latter figure possibly represents the sort of values which wight be expected over kimberlites, covered by a thin layer of glacial or marine deposits, in the James Bay Lowlands.

Tl\e average si/.e of the larger kimberlite pipes is {'.bout ^00 feet diameter so the geophysical target might be an area about 600 feet in diameter with a value of about ^00 i' . The closest flight line spacing that is practicable is one eight inilc (660 ') and in practice a 1000 feet spacing might be the best obtainable. In either case a kimberlite could vclD lie between two lines and hence go undetected. There is also the question of whether an area of length 600 feet, with a value of ^00 f could be detected, this would depend to some extent on the magnetic intensity of the background. In the James Bay Lowlands, the complex magnetic signature found in most pre-catibrian shield areas is simplified by the blanketing effect of the paleozoic sediments and so the prospects of detecting anomalies due to kimberlite is better, but still very poor. If it is ever intended to prospect large areas for kimberlites by means of aerial magnetometer surveys, serious thought should be given to improving the equipment and techniques which are used in aerial surveying. (P.Gratton-Bellew).


PLATE l

Approximate site of alleged discovery.

l

CORAL RAPIDS

Viev looking south.

PLATE f?

MUSKEG SWAMP l MILE WEST OF THE RAILWAY AT MILE 99-


PLATE 3

.Limestone outcrop.

CORAL RAPIDS AT LOW WATER,

PLATE k

RAISED BEACH ON THE RAILWAY AT MILAGE 106.


PLATE

tn

- gravel horizon.

TYPICAL LOW TERRACE DEPOSIT, WITH SAND OVERLAIN BY GRAVEL.

VIEW LOOKING EAST.


PLATE 6

Pit 1. Upper terrace gravel,

?T,'#te? basal gravel resting on clay.

HJVTEJ7

Pit ?. Upper terrace gravel.

View looking west.

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ROCKING SCREEN

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PLATE 11

RIFFLES BELOW SCREEN AND SWAMP BUGGY.

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INVOICE NO.

j TolopKarto Sif AT EM E NT 1325 Ldwrtnc* Ave. E* 1 1 Don Mills, Ontario

' A1KENKEAD HARDWARE LIMITED

SELCO EXPLORATION CO LTD 121 RICHMOND ST W TORONTO ONT SUITE 1201

29 AUG 1969

C 100370

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MCGILL HARDWARE LIMITEDCOCHRANE, ONTARIO

BUILDING AND ELECTRICAL. SUPPLIES - SPORTING GOODS

To Se]. co Rxrjp ovat.ion Ho.121 Richiaond St. West TORONTO, Cut.

Au*. 29 10TERMS: 3O DAYB

; DATE

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MCGILL HARDWARE LIMITEDCOCHRANE, ONTARIO

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BUILDING AND ELECTRICAL SUPPLIES - — SP

TO, .vSelco Rxnlorations121 Richmond St . WToi'Oivho. Oiit. .

TERMS: 3O DAYS

DATE

Sept. 13 20

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Suite 1201,

DELIVER TO

TERMS N C T

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THIS IS OUR ONLY B1UNO — P^E R2MTT

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WHEN COMPLETED THIS IS YOUR

INVOICE

.5SJiIAS~.,wJ

TRANSPARENT CLOTH .

OPAQUE CLOTH

CRONAFLEX

MYLAR FILM

AUTOPOSITIVES

REPftONEGATIVES

OFFSET . ' ''

PHOTOCOPIES

XEROX

' : FRANK P. FOAD LEMSTED ' :- ' ^ QQ175 King Street East, - 8589

Toronto 2, Ontario. . Phone 364-1148

u fi "rrira E- o (L^*IHt fillCl li Of IKOUU**

lltlCl Illl

130 YORK STREETTORONTO l, ONTARIO

TELEPHONE 363-1435 15056"Thank you lot buying our producti"

QUANTITIES IN THIS COLUMN ARE NOT SHIPPED OR CHARGED BUT WILL FOLLOW

PLEASE DO NOT RETURN MERCHANDISE WITHOUT OUR PRIOR APPROVAL, AND IN ANY COMMUNICATION WITH US CONCERNING THIS INVOICE, BE SURE TO STATE OUR INVOICE NUMBER.,

INVOICE

sKvtnc woras -vvr UWWKK'S KiSK" must be entered

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initialJed by both parlies thereto.

(Roolpl of Goocii ol Ooilinallonj

IVfD IN APWSENf GOOD ORDER (EXCEPT AS NOTED), f ROM 'of Corrlor)

THE GOODS DESCRIBED HEREIN.

CONSIGNEE. DATE

LARED VALUATION .... . -... MAXIMUM LIARILITy ^1.50 KER POUAT) UNLESS DECLAIiED VALUATJIO^ STATES OTHERWISE

(TMi Blll'of Iodine li l* b* Signed by th* Shipper And Coiv;*'r)

CARRIER

PER

130 YORK STREETTORONTO l, ONTARIO

TELEPHONE 363-1435

StHCC 1*M

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, , . r , --- " ' ' -

l ",*^N?.W

| r*;, se o ro(j CAYMFNT

| KNTCA60

ia- ri• ' -.*-

j CHCO'Jf No- 4

SHIPPED VIA

(NO. PCS.

X " QUANTITIES IN THIS

[NO. INV ' cones

DACXffiOM NO.

li u i s 1i " "

1fat,/- 1 6r-

iiOHDCR10 .NQ^î. 4^;.w:-

COLUMN ARE NOT SHIPPED OR

rt

INV

t

-—

^.^-ui**~~i

"J/Z^

i VJ t i 6 N'

CHK'D. 0\f

CHARGED

PLEASE DO NOT RETURN MERCHANDISE WITHOUT OUR PRIOR APPROVAL,

WITH US CONCERNING THIS INVOICE. BE SURE TO STATE OUR

ttyfrcD ,

L/^

i . . , . -u i

— -. . -,..

-

J

'/ioni you /or buying our product*"

...... .... . - . . - . ,. M .-. — j ,

fi '

i t il

luKt/rnf.tt y

^7H

1 3990AMOUNT

V

\

1^0.00 |IK

' V

13.50 J

f

8.10 !171.68 -\

T

li

ji

.BUT WILL FOLLOW j

AND IN ANY COMMUNICATION ou* OIIBK no \ INVOICE NUMBER. . t f\ x i

INVOICE

PACKING SLIP

. ^ Invoice Address (two copies please)'

Suite 1201,121 Richmond Street West,TORONTO l, Ontario.

for

Vi

^Mejjf^feAN^ôafaiiSff•^L//^^fei^-*K

KIRKLAND LAKE MACHINE fi WELDING LTD.P. O. DOX O 2 G

KIRKLAND LAKEi O STATION NOAD KIRKLAND LAKE DIAL oov -

Expert Machinists and Welders•EQUIPPED TO SENVE YOU BETTER 1

Silco Exploration, Suite 1201, 121 Richmond ^t., Toronto, Ontario.

DATE Aug. 29/69.

INVOICE NO. 9143

CUSTOMER'S ORDER NO.

4 ?'

r:'

r-'Ci -'

VjOvlH-.

5t

Repair 2 gravel shakers V. .\ ' : '*" v \ . :;'

jV^r^J.^^x^-.^rJ ' Lbour . : '...o-.,* | (^ j ,. shafting•.rv/r.: — ' j'Tj ^"-TJ""J aluminum111!:!! — .j -i'- — 2. rt— j Keystock: * r " " — j ^'iEtii^.^f/ Iron-;':.",.. A 1 r'ft Q.'- (i^('J:-*i(.*C i-^P/^j ,, Hfln Rp.fiws. mit.K ^- wa.dhftyRn i s v .'s i a u T i o f 4

l-tfi 3&V&

12^ Fed. Sales Tax5^ Prov. Sales Tax

i

21+6.m

7..1.

1.*

1064503530

50

2950

253** ' "'

1 ' ill

63•VIMM"

24 HOUR SERVICE ON EMERGENCIES OR BREAKDOWNS

u

JwVKK, OTStTA.l-J.10


SuLCO KJas L02A?);Qft CO v'.'V ^"'''i'^-'"'^*-,'?'* c^'" 1 v.. .j .v il ~U'(. t.Wi'J*. O t i*

90 80268 90019

DATE tNTCRtV, f. l j (l l OATI 70 BC 6HIPPCD

sH l P

T O

WMEM MAKING F-AYMF;HTSPUSIASE QUOTC IHVOlCe MO.

EXEMPT CERT.

EXEMPT AT SOURCE

INTEREST AT THE RATE OF \*X, PER MONTH CHARGED ON OVERDUE ACCOUNTS


P.O. BOX 829 HAMILTON, ONT.

INVOICE


•sss:,co :-.x PLOP. A? VON coÛ 3:21 SxCHKOXD SV W A , ^^ VOiÔW'VO O.\"'A" '"*/ t-k* ^^ *" ** ^ v * * * y ji-^j

90 80368 90019 1^/2o ^

C M A M C C H U MB C ftU MB C


O D.E I - l N C . A T i ] T.

ODE 3 - EXEMPT CERT.

:ODE 4 - INC. AT 12;

ODE 6 - EXEMPT AT SOUUCE

INTEREST AT THE RATE OF 17, PER MONTH CHARGED ON */ OVERDUE ACCOUNTS

ALL CLAIMS FOR DAMAGES OR DEFICIENCY MUST BE MADEFIVE (s) DAYS FROM RECEIPT OF ORDER

P.O. BOX 829- HAMILTON, ONT.

f ÎNVOICEA-i^

1C LIL .. A ^vision of Acklands Ltd.

^^fe^F UNIT r.' O1 . e . AMOUNTSE™ \*jjfr ^44—H-"""?1P^^r^^^^-— ——^IZ7'weT^HTj UNIT[T71 9ROD QUANTITY UENOT H pR|C ,™j CODE sH'r!!l =^4==

TiO

INTEREST AT THE RATE OF 170 PER MONTH CHARGED ONOVERDUE ACCOUNTS


PUEASE REMIT T'

p O. BOX 829 HAMILTON, Of

INVO1C1

iJ. Division of Acklands Ltd."VV;r VV -f voyrv A W)Jk. i i J l ( ^l/.Vv - w-J^-— "•'—^ j

"CHEoTr NUM'bCR

^121 .y CREDIT DAT"?A^^L^. ..'•.wMIT ICE

? J?/1*. iS'C!'

PATS tMirriu

V.1, p"

/Z~7/!1 TuV

/x

AMOUNT

——————— "5"

/1?^

COOK - X - SALES TAX EXEMPT AT SOURCE -CODE - -t.'*, . NO SALES TAX INCLUDED . CERTIFICATE ,

CODE,- Zn - FEDERAL SALES TAX 1NCLUDED —J—--—- ?R.OV. &

TOTAL

CMAhOt NUMDtK

CREDIT

[i? ! STATION HO. [3j SPIUJCC ST. [^J MCG A UG Hi; Y A V E.,) K l K K U A N D L, A K E TIMMINS

fjAMHYDOWNi: fio,(Y

2gff JjF^WSE "lAYLuff HARD WARE I i MI r E HI" A Division of Acklands Ltd. "

jac.0 ^v-^o--^^^o .JU^tl S J e/ r- /J/ 1-^,

^^7^

-' To

WHEN MAKING PAYMENTS PLEASE QUOTE INVOICE NO. A

COST. ORDCA NO.

fCU..TAX NO.

!ALtl.M",S

PHOV.TTAX NO.

OJANTITYORDERED

^0

DATi^ CNTCRED

DESCRIPTION

DATt TO DC BHIPPED

Mttiii '6v* ^ j

V-v^r-.F'!*

D AT K t-'.'iO

t r-.;'. 1". -. "i A i

r. t s T r. i o u T i o N

i-

PROD CODE

/s

OATt tHIPPCD INVOICt*Tt

QUANTITY SHIPPED

30.

LENGTH ETC.

UNIT PRICE


fi

DISC.

SUB TOTAL

FED. TAX

CODE l - INC. AT J J 7.

COOL 3 - EXEMPT CERT.

CODE* - INC. AT 127.

CODE i - EXEMPT AT SOURCE

INTEREST AT THE RATE OF I70 PER MONTH CHARGED ON OVERDUE ACCOUNTS


PROV. TAX

^ 0 ~TOTAL

3'r

PLEASE REMIT TO

P.O. BOX 829 HAMILTON, ON1

INVOICE

IP;K V. S TYLV* C o WAXY o? CAXADA, LIMITED ~——^—^ ^ J. J^l .jAV v. V-.. P.O. BOX 1006 -ST.C AT MARINES,

. ,INVOICE NO.

TQRONOX) XORDCR DATE

SNIP TO SLCO ir-};?Loj-,i 'V,-Yc--':s co. LTD. 9

BUS ri'Q T!T 1 'i "i '\:' : - "'''O'i FU^'. fj''MJ; '.':.'.A^ICI'j ROUTE CJ.Q *,.,..~ ,,,^ C5 g Q..T ^ ^ ^ RA'.O'iVJAY

SEPT. 9/69DATE OF SHIPMENT

SOT. 11/69

ONTARIOISIVOICE DATE

; Sop 15/69AREA cc.tr.

7-2-05-52-29 05-52-21

CUST. NUMBER

000-6916-01 O

DATE SHIPPED

Sop H/69SHIPPED FROM

.-j

•1

f CUSTOMER OKOCRNO, REQUISITION NO. FED, s. T. LIC. NO. (PREPAID COLLECT

9/XO/6Q 7CXTPA Kcj-iPT.* FtOf 0 . TERMS PNOV. T. X HCENCE NO, NO. INV.

. . "" -. ^...o..,. _ ^ 4 ,*C t' A S T t T Y CKDCRCD

T.

1

it ^

DCSCFilPTlON

72 " c 5: 36" PC-i^o o x fi MJI3H .O.'*?" DlA 0 STEEL VttHE O.XO"Ii.

1^4-302002

?2" x ?6" s PGSo 4 x 4 KESK 0 092ts DXA. STEKI, V/VRS r.TvTi'-K

1-1-302002 : Aooino^ j ^ ————— 1——A- 1 X T t f j T 1C* .N JE fc-Xil-f j

'•'•' '-i - f T 1 ,^^J ' *

li^ss.— Lilj: l".'; 1! . ''.L ^) '*-) ^ |K-K-

DISTRIBUTION

3fe,^*S ^.**

INVOICE

"|~

j1A^ Fi"' f^HGCO ol1 tt 'jkv"'

VIA ~"\

cwxNO. PIECES t, V.U'&HT

1 Prcjno 83//QUANTITY BACKCftO.

PS

QUANTITY O H 1 P P t O

18

18

d. C^s

UNIT PRICE

1.43

1.51

iTiOff^^ ^)Vk |J J, j^^jo

?ST 5^

Q.

AMOUNT

25.74

27.18 52,92

59*.27

2.96

4.15

TOTAL OF INVOICE [^ 66.38.. . . ... . mm ^-S

^/U tx ^

t'' ' l"

l//|j ITEM 40300 Wlfit CLOTH STtlL ' '

\ 1TCM 40340 WtRt CI.OTH (

| | 1 | ITEM C20IO SCRCtNING MACHINES ISIIKS.) ^ '

i j] ITLM &2220 DARS OR hODS N.O.l.D.N.

1| ITEM 3U60 SO EIIVATOR SHAFT tUCtOSURE DOORS. OATES. LATTICE WORK OR 1 || k*lLlt,G XD FLAT OR IN FLAT SECTIONS: ST [t L OR STEEL t WOOD COMBINED.

ITLM 30070 ELEVATOR CARS FBEI6HT OR PASSEN6IR K.O.

j! ITEM QS370 SCREENS OR SIEVES N.O.l.a.N. l NOT NESTED)

i|— n~ri -i i -- -1

rOftM NO. D - 10

SHIPPi;R THE W. S. TYLER COMPANY OF CANADA LIMITED *CENT.PACK1N

LIST

THE MEMORANDUM-

. Tins W. S.TYLER COMPANY OF CANADA, LIMITEDORDER NO.

.fi fi

ORDER DATE

P.O. BOX 1OO6 - ST.CATHARINES, ONTAftIC INVOICE N/., INVOICE

SHIP TO 6

SOLD TOIF SAME

ROUTE

SP;LOO JKPLOIIA^'XCH GO* LTD., S'JXO.'E l:iOX

AUG. 6/69ATE OF SHIPMENT

AUG. 11/69

AREA CODE

7-1-05-52-22

CUST, NUMDCFt

000-5215-01 O

DATE SHIPPED

Avs 12/69SHIPPED FROM

f~ CUSTOMER OHDEH NO.

^•ZJG o S. f oOF. O, 0,

C-'**.T!TY l iKOtstO 1

1^,-C;: *- -j/.sj po q.,* O .-; J \.) i vvij o

CLOTH.

1-4-302002

REQUISITION NO.

TEKMi

B

~

-

FED, S. T. LIC. NO. PREPAID COLLECT

PF(OV. TAX LICENCE NO. NO. INV.

ir.'. r '? P ,A o•^DESCRIPTION

s: 6: MESH

':J^. ".'....-— i-

~YN^"T~r .... w .--.. *. —

CZ::^ i

MS

:

o047" DXA, STEEL WIR:

^ ___ e^|^f—— |

" (T- JO ',j'-H^'-l I^- U'-J

i'j

\ i\ii

VIA

CPKNO. PIECES t WEIGHT

3, Fi'iy/is 2^^'QUANTITY DACK ORO.

*

QUANTITY SHIPPED

9sq.ft.,

K

K

UNIT PRICE

1.W

T IL2/O

T 5^

AMOUNT

12.S7

i/rSi.72

TOTAL OF INVOICE ^V 15*13

NO. 0-7 OITTOFORM*

NV01CE

6 1168 (THREE LINES) JO4 ADELAIDE ST. WEST

TORONTO. August 28th 19 68,'.V* \

\\. .f '-rtf'l'lftf l~

' SOLD TO ,, ^..,..Sn 7 r. n Z.vpl Q rg t i, n/i,.Suite 1201 - 121 Richmond Street, \lest, . Toronto, Ontario

DELIVER TO Kr. P. K. Grattan - Br.11 BM

MI'043;-"i -' /, ' M *.

..(.'..'.;- * *.'B u r i o N

TKNM* n*T

THIRTY PAY*

f X U±3167 j

jj]2262JJ2

J2J1

scotch tape 5/8liquid paperScotch double coated tape 3/4 x S& ydsMasking tape 1& 60 ydsMarket te markersKoh-i-noor markersprismacolor pencils45 ~ 90 set square 14"set square 14"Star gum cleaner #4823bottles rapidograph . '3080 F drawing ink101 Pink pearl eraserpencil tip erasers Rubybox tacksbottle Pelikan drawing ink

'

eacheacheach

each

Con 'd pag

794920

55

3 2.

J,121

152

1

95,59 'i39

40589820

3055151015 '053070

NOTE — ITEMS SKIPPED WILL GO FORWARD EARLIEST POSSIBLE 3168 '

,riREE LINES)1O4 ADELAIDE ST. WEST

tM / T zo

TORONTO, October 24th19 69

41388

SOLD TO Sc]coBxp]orations,e J.^UJ—- J ^ l ' H

Toront.o, Ontariotreet,—Wo y t,

DELIVER TO -J^? Mr - Grattan B e 11 on

A 3646 1-L

1

3

RDCS 41 or

PDCS 16 or

rolls chart

s"

TERMS NET

THIRTY D A V S

NOTE — ITEMS SHORT SKIPPED WILL GO FORWARD EARLIEST POSSIBLE 3646

SELCO r.-VPT.nuATTON COMPANY LIMITED'

Day ACTIVITIES

li

2

5! ^*

x'^l 01

lO

10

li

12

13

X/y

ini l;

'^Js'lt-^.^&t

14

15

IS

17

19

TIME SHEET

Office Use

Day

25

28

29

30

i..31

ACTIVITIES,

or Office Use

SELCO EXPLORATION COMPANY LIMITED

Day

1

o

3

4

5

S

7

8

A J

10

11

12

13

14

15

16

17

18

19

ACTIVITIES1

-

A \- r s V/-4-A \^ TO /e'Vv T i?K. c"^^. ko-vvJ*-iM .IN

Gt/^cx^l cir^KU^f w t^j'^-

b' w 4 '^v

For officeUse

1

Mameij^

Month : To \y Year Mb'/

Day

20

21

22

23

24

25

26

27

23

29

'30

31

ACTIVITIES

'\r

uv

ForOfficeUse

SELCO EXPLORATION CO-lPAilY LIMITED

Da

S

10

11

12

13

14

15

16

17

c|

ACTIVITIES

A*

/o

ForOfficeUse

Name : 1- (- 1"

l Month Year

Day

20

21

22

23

24

25

26

27

28

ACTIVITIESi

f^c^da, cow ft- vv;j c k*- ^ /av Cewxpfei- (.tf*1 y/

J i V ' .,. ,-

ForOffice Use

- 1 ii !; .'

; \3-/•v*

' f\; ^

/.ti ^i iii

:

! l l29 j \ \

\ i l i

30

31.1

i i1 i1 ji

c O fi ri A /f'/? ft O S' S0/! O 'J PC T.


T I M E 55 II E E T

Da ACTIVITIES

J 2

vi (xlI'b -se o o t' OsA-CiO v\ c/

O "i /w -,. ;v

i i

10 /fl u e /'

11

12

t/W/ntfQ

13

14

15

16

17

ity o/-'

12

ForOfficeUse

'X

-r-*-

K ame : f-f. 6 ra //os? -

\ Month: S Year

/KA

Day

20

21

ACTIVITIES

*ffa Csmhwa^i

ForOfficeUse

J/V^-/? (2.^*2.

23

24

25

26 ,Ca

27

28

'CflUj U^Ol'K.UAi*v,u,-c(. ciipit/ ^xcvuuv-t-f

29 f^*\ Uy

30

31

VO *JC , ,, ;J Oxw? -'^-^^k

o tdty /j tt jtyi

SULCO EXPLORATION COMPANY LB1ITED

? I M E S II E E T

10 i

li

12

13

14

15

1G

17

-

Day

1

\ Uo c 2

3

4

5

1

S

1

8

ACTIVITIES

Up^OUAAfJ (^ Co rev l fU/W^

TCM.'(\ pxf. [Cc'i Q^jow.v^Tr\*o G;^0^- AcxjfK^ lo To VUv*.To v

~Dc\M ^\ "Toronto

— fj

l

For Office Use

Name:

i Month: Qc t Year

Day

20

21

23

25

26

27

28

29

30

31.

X

ri* Toronto us o/ /f /si

ACTIVITIESForOfficeUse

p

JUT'•D

SELCO EXPLOPATIOn COMPANY LIMITED

BALANCE FORWARD:

ADD RECEIPTS"PROM:

//97.-SQ/I/

MONTH : S s. h 19

TOTAL TO BE ACCOUNTED FOR: $_

LESS EXPENDITURE LISTED BELOW: $_

BALANCE ON I-IAHD: $

SUMMARY (Office use only)ooo

j

DATE] DETAILS s JOB

r.-i/-

SIGHED:

approved by:

OTHER EXPENSESWITHOUTRECEIPTS

(2)

WITH RECEIPTS

\ -*s J

.a .-/ ^i: __

l^o.oo

TOTAL EXPENSES. (D+ (2) 4- (3)

RECEIPT KO.

OFFICE USE

•g-ifT—Jen*


"BALANCE FORWARD" $

ADD RECEIPTS FROM:

NAME:

MONTH : 19

TOTAL TO BE ACCOUNTED FOR:

LESS EXPENDITURE LISTED BELOW:

"BALANCE ON HAND"

$_

$

SUMMARY (Office use only)

ItO

Approved by:

' A \ A' A

' ; . : '. . ' A. . ' ' ' ' A

. . ' -V A . . ' ' A

' ^' - ' A

.. -' . -:; v -.Ai - *

-: " JUL23SS'06in 65 ' A. \

o 0001.99 - 0001.89 ; o 0001.39-" * 0002.75 : |; * 0.001.39" ; o OOOO.A9 -; V- " * 0.00029 ' . V 000 3.6 5 r - .* noi 38^rS - ;IX' '000 0.69 . ; -. -. . * 001 ^r.53S ; '. "- . ,- CO. 000 0.70 ^-. ' - " .QOU.53T ;; -

275-279 King St. W. TORONTO Phone : 366-89,

ESTABLISHED 1914

THE CANADIAN R/iSLL SUPPLY CO.— Distributors of Now and Reconditioned Electric Motors and Fans —

Carotakor Supplies — Liquid Soaps — Deodorant BlocksCotton Waste - Chamois - Sponges - Mops - Brooms and Brushes

Painters' Drop Shoots - Washed and Sterilized Wipers and Cheese ClothCMS Wax - Simoniz Wax - Old English Wax |

VOUR ORDER OUR ORDER . ^ /' iV ' y '

^T /f ; ' . ;- ' iNAME ' /' -rv- — ... .. ..f rfL- f

ADDRESS

QUANTITY

"'i'

^' ''

40

... /' r r -'•' 7 -' " ""

} \ ' -

' f , p'lS^CR , P T , 0^ , ,

.'

' ^ .

. ., /' ; m ;

1 f l* l&i jrjl± /:l ,'-' /i

\7••v ; /- /w

V S /o•- i f A

PRICE

/- ' / r/•C.* y"'

7jTD

'

TAX

TOTAL

' X,'

AMOUNT

S

isr^

2~0 s

LL-\

"U'A

1 &H

yj^j-1)4

-P—- ——1 ERRORS OR SHORTAGE MUST BE REPORTED IMMEDIATELY

3

'i

.i1 i,

•j j

i

i

j * j i3i|

1 •j

it

R 11 64 C CUSTOMER'S COPY^ ^ OVER SO YEARS OF SERVICE

fwlC WIIIKIS f O* M l LIHITCt

5S s; t-; ij c* o

X\ \

\

fvAa

fc's

X ^^

*-

tx.

r-

!-x

. c

\ o\

r

\: {

f f

ws

pHS

.^

A-O

, So

. l ]

f ^

f,-

C\

C-

r.t 'C

o t-

v\\ c

l

o ofiELCO EXPLOP.ATION COMPANY LIMITED

BALANCE FORWARD:

ADD RECEIPTS'PROM:

HAME:

MONTH: - /-S 10

TOTAL TO BE ACCOUNTED FOR: $

LESS EXPENDITURE LISTED BELOW: $_

BALANCE ON HAND: $

o.

(Office use only)

- Z^j/^/f /S/.oo

lDATE DETAILS t JOB

.y

TOTALS:

at:OTHER EXPENSESWITHOUT RECEIPTS

WITH RECEIPT?

RECEIPTI-JO.

OFFICE USE

SIGNED:

approved by:

TOTAL EXPENSES (D+ (2) 4- (3)

,JSTRIAL SALES (TORONTO) LIMITED l Y(j ^^ij T E

yO U S T R 1 A L ORDER D E S K t PHONE 924-0711j(f' .\\^.~TijJ U| fMl Y W X 6 1 0-49 1 .22^,7 —— 1 "^V^^J "^W

6OLD TO

f

E VIA

. S^LCO COLORATION CO SH.P -ro.

. l 21 RICHMOND ST

. SUITE 1201 TORONTO 1 10 ONTARIO

3^H9M^nn^MWBBMHBMM

78355

'" voiiii oidii. H NO. YOUR onorn no,^

C05'5OATS ouii onui.n NO. re.u Lie. NO,

ORPLR'rn \ DESCRIPTION

S: 4

\ 2 '

\ 2

i 2

o

jl

A403 SCR - '. l M 694 DIODE ' :' ST2 DIODE - ' ' C20B ' A4IBy2 w io;5 STACKPOLE .2TK'?T SPRAGUE " ' - ' - ;

'B' 51 CRL CONTROL NC303 N DELTA 24 572 KNOBS v ^ r " . )

-' ' ".' ' --^ " PLUS

' S. T, PICKED UP 'ON OUR PACKING SLIP C 4041 l S.T.I ,

QUANTITY SHIPPED

" 8 . , 4

2 :- 2

2 2 2

.2 2 2

'S^S.T.1,.'"' 'v ."(

ILIiMi: 1V10 OAVi HIT SO

/ PRICE

247 80

102 269 247

14 23

137 260

28

AMOUNT

1976 320 204 538

. 494 28 46

274 520

5644 56 223

4679

•"""T i.. ' L 'r s - .L "* -J*, ^ - *"

l

* U "

O

O

O

O

O

o

o

o

o

o ; 6

AS WE ARE NOT RESPONSIBLE FOR COODS DAMAGED OR LOST IK TRANSIT KINDLY REFER ALL SUCH CLAIMS TO THE -

CARRIERS FOR ADJUSTMENT. NO COODS TO BE RETURNED OR EXCHANGED WITHOUT OUR AUTHORIZATION. INVOICE

ANT UNFILLED BALANCE OF THIi ORDER WILL BE (HIPPED AS SOON AS POSSIBLE.

O C. k 0. C. , ' Q

^ - ^ K^ ,. . L.E L- !H CJ "T K © S © IM 1 (D jK/INDUSTRIAL- SALES (TORONTO) LIMITED /W

INDUSTRIAL ORDER DESK: P K O N E 924-0711 f ffy- Y W X 610-491-2297 l C~^

SOLD TO

i "

^ VIA.

...-.-l.-.-l

y^Qi . 1 To1 " "" " l j T E

t * ^A'). SFLCO EXPLORATION CO 6H "- T0 . /V/^^f x . 121 RICHMOND S'! T* .-' 1 I . SUITE 1201 ,/ * (j I/A^ . TORONTO 110 ONTARIO /' , N/ A

/* l ft i

14.3 YON OK STREET

RONTO 5, ONTARIO

UKPHONE BS4.O3O1

78356

f YOUR ORDER NO. J V YOUR ORDER NO. ^

. 0053 'OATC

CCf* *1 6Z f QCUANTlTV ORDERED

2O

,* ^

1 8 2

OUR ORDER NO. FED LIC. NO.

DEGCR1PTION

1 444 1 4 HAWiWiOND ' " , - ' 1 432 14 ' FP502K 7 AC 'PLUGS . , . ; 61 F AWPHENOL AGC 5 BUSS FUSE , . . '• SP 23 WELLER IRON VJK 150 CORDOVER WIRE 103 DELTA BUSHING 2 02 SOLDER

PLUS

' ' ' S. T6 PICKED UP 'ON OUR PACKING SLIP C 40412 S.T.I.

QUANTITY SHIPPED

22 4

' - 4 . .5

1 1 1 8 2

* t

5^ S. T. l."

TERMS: 1X-IO DAYS NET 30

^ PRICE

118

78

68 , 58

09 356 100

. 08 27

AMOUNT

236156 272 232

45 356 100

64 54—— 15*15

76 15 91

—i

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C*fc*IEftS FOR ADJUSTMENT. NO tOOGS TO HE RETUKNLD OR EXCHAI.&CD WITHOUT OUR AUTHORIZATION, INVOICE

Ih1 UNFILLED tALANCE OF THIS ORDER WILL HE SHIPPED AS SOON AS POSSIBLE.

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r YOUR OHULH NO.

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DESCRIPTION

730 1 1/8 GREENLEE PUNCH 101 S K',! LLER SYRIPERSG 6 WORKK&NK-'325 HARDWAREV,'T27 FOR W25 DOS2002 DOZ 2173 RUBBER GROt^ETS 27 REAMER 44 ECLIPSE TOOL

PICKED UP 'ON OUR ACKINGSLIP C 40413S.T.I .

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INVOICE

'LV- LS. ^ o ireINDUSTRIAL.SALES (TORONTO) LIMITED | )^fl ,".

INDUSTRIAL ORDER DESK: P K O N E 924 T W X 610-491-2297

643 YONGE STREET

TORONTO 6, ONTARIO

TELEPHONE 084-1

W 78358BOUD EXPLORATION CO

121 RICHMOND ST SUITE 1201 TORONTO 1 10 ONTARIO

SHIP TOi

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OUR ORDER NO.

DESCRIPTION

273 LUGS 111 102 JOHNSON 342004 GUSS FUSES HOLDER AGO 5 BUSS FUSSES FNW FUSES 9 y1,',1 25 MICA WASHER 0203 SCR 2CC) KEYSTONE 200

PcCKED UP 'ON OUR PACKINGSL 1 P C 40426S.T.I .

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SAMPLED

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SELCO EXPLORATIOKJ CO. LTD. CORAL RAPIDS INVESTIGATION

CROSS -SECTIONS

4ai04NE0006 2.133 VALENTINE

230

coral lime s chemicals ltd

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