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John R. Fraser GEOLOGY of the HARVEYS CREEK PROPERTY HA

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John R. Fraser GEOLOGY of the HARVEYS CREEK PROPERTY HA GEOLOGY OF THE HARVEYS CREEK PROPERTY HA-1 CLAIM CAR1600 MINING DIVISION 5Z” 51.2’N; 121’ 22’W NORANDA EXPLORATION COMPANY, LIMITED (NO PERSONAL LIABILITY) John R. Fraser January 1979 TABLE OF CONTENTS Page 1. SUMMARY AND CONCLUSIONS 1 2. INTRODUCTION 1 3. LOCATION AND ACCESS 1 4. CLAIMS AND OWNERSHIP 2 5. HISTORY 2 6. PHYSIOGRAPHY 2 7. REGIONAL GEOLOGY 3 a. PROPERTY GEOLOGY 4 .l GENERAL STATEMENT 4 .2 LITHOLOGIES 4 .2.1 Midas Formation 4 .2.2 Snowshoe Formation 4 .3 STRUCTURE 4 .4 GOSSANS 5 9. REFERENCES APPENDIX 1 - Statement of Costs APPENDIX II - Statement of Qualifications LIST OF TABLES TABLE 1 Stratigraphic Units: Yanks,Peak - Roundtop Mountain Area TABLE 2 Compilation of Geochemical Data (Total Extraction) for Gossan and Rock Samples, Harveys Creek, B.C. LIST OF FIGURES FIGURE 1 Location Map (1:250,000) Follows Page 1 FIGURE 2 Detailed Location Map (1:50,000) Follows Page 2 FIGURE 3 Geology Map (1:5,000) In Pocket FIGURE 4 Section A-A’ (1:5,000) In Pocket 3 t 1. SUMMARY AND CONCLUSIONS A number of iron oxide seeps or transported gossans containing high concentrations of zinc, silver and cadmium occur at the head of the southern branch of Harveys Creek, Cariboo Lake area, British Columbia. These features are underlain by folded, graphitic metasiltstones and phyllites belonging to the Midas Formation of the Late Precambrian to Early Cambrian Cariboo Group. The structural interpretation is that the folds are isoclinal and oveiturned to the southwest. Mineralization to explain the gossans has not been observed. Approximately 9.5 to 12 Km. to the north, in the Cunningham Creek area, Rio Tinto Canadian Exploration has recently discovered conformable bodies of lead-zinc f barite mineralization in Snowshoe and Midas shales and limestones. A trench on the best showing, in Snowshoe Formation carbonate rocks, has been reported to contain a 14.5 meter true-width section which averages 5.98% combined lead-zinc and 2.09 oz/ton silver. It is felt by the writer that the source of the Harveys Creek gossans must be one or more strongly mineralized zones contained within the Midas Formation or, possibly, the Snowshoe Formation. The presence of galena, sphalerite, pyrite and barite in similar rocks on the nearby Rio Tinto claims lends support to this hypothesis. Further work;‘in the form of additional geologic mapping, soil sampling and, if feasible, gravity surveying is necessary in order to outline such zones. Because of the high graphite content of the Midas rbcks, electrical geophysical methods would not be very effective. 2. INTRODUCTION This report describes the results of geological mapping carried out during the period September 16 - September 22, 1978, inclusive, on the HA-1 mineral claim, Cariboo Lake area, Cariboo Mining Division, B.C. The purpose of this work was to obtain geological data regarding the prominent iron oxide seeps known to occur on the property. Approximately on third of the claim was mapped, by chain (Topofil) and compass, at a scale of 1:5000. A base map was prepared by enlarging the appropriate portion of the 1:50,000 sctile topographic map for the area (Cariboo Lake, 93A/14, 1976). The writer was assisted in the field by Mr. lvor Saunders, a Noranda Exploration Company, Limited employee. 3. LOCATION AND ACCESS (Figures 1 F, 2) The L.C.P. for the HA-l mineral claim is located in east central British Columbia, 10.5 kilometers N14OE of the settlement of Keithley Creek and 96.6 kilometers N34’E of Williams Lake. In detail, the property is situated on the southeast trending ridge which separates the drainages of Harveys Creek and Pine Creek. /2 -2- Access from 150 Mile House, located 14 Km. east of Williams Lake on Highway 97, is by paved ot- good gravelled roads to Keithley Creek, a distance of 101 kilometers and thence by helicopter to the property. The Keithley Creek - Barkerville road passes, to the north and west, within 2.5 - 3.0 kildmeters of the claim; this road is in poor condition and should not be driven in other than a four-wheel drive vehicle. 4. CLAIHS AND OWNERSHIP The HA-l mineral claim (Tag bOY717) consists of.sixteen u~nits, four to the east and four to the south. It was located by Percy F. Cox, as agent for Noranda Exploration Company, Limited (No Personal Liability), during the period 3:lO P.M. January 9, 1978 - 12:15 P.M. February 2, 1978 and was recorded on February 14, 1978 (Record 8593). 5. HI STORY The area of the present claim first attracted the attention of Noranda Exploration in late August, 1973 when anomalously high zinc values (to 880 ppm) were found fin silts collected from a northeasterly flowing tributary of Harveys Creek during a reconnaissance silt sampling program in the Cariboo Lake area in July and August of that year. During the follow-up investigation of the anomaly by company personnel, several zones of intense iron oxide staining, underlain by graphitic phyllites and metasiltstones, were discovered. Six two- post claims (HA 1-6; recorded September 5, 1973) were staked by Noranda Exploration Company, Limited to protect this very interesting situation. In mid-September, 1974, the area was revisited and a short program of prospecting and gossan sampling was carried out. The samples were found to contain high concentrations of zinc (530 - 3900 p.p.m.1, silver (2.2 - 5.2 p.p.m.) and cadmium (3.0 - 26.0 p.p.m.). As the gossans were thought to be transported and mineralization, either in outcrop or as float, was not observed, the claims were allowed to lapse. The area of interest was w-staked (HA-11 for Noranda Exploration in early 1978 because of reported discoveries, by Rio Tinto Canadian Exploration, of conformable bodies of lead-zinc mineralization in Snows~hoe and Midas Formation shales and limestones in the Cunningham Creek area, some 9.5 - 12 kilometers to the north. 1 - Unpublished Noranda data - 197’1. 6. PHYSIOGRAPHY (Figure 2) The claim straddles a round-topped, steep-sided, southeast trending ridge that forms the divide between Harveys Creek and Pine Creek. To the northwest, the ridge rises gently to the summits of French Snowshoe Peak (1903 m/6245’) and Base Mountain (1927 m/6322'); to the southeast, it drops steeply to the valley of Cariboo Lake (812 m/2664’). Relief is approximately 455 m (1500’). ../3 -3- Timberline in the vicinity of the claim is approximately 1830 meters (6000’) elevation; between 1675 meters (5500’) and 1830 meters (6000’) elevation, timber is patchy and elongate open spaces are common. Eelbw 1675 meters (5500’), slopes are heavily timbered. 7. REGIONAL GEOLOGY 2 The Yanks Peak - Roundtop Mountain area in which the property is located is underlain by sediments belonging to the Late Precambrian to Early Paleozoic Cariboo Group (Table 1). In the vicinity of the property, only two units, the Midas Formation and the Snowshoe Formation, are exposed with the latter, the youngest, being most abundant. The Midas Formation consists of grey and black, dominantly argillaceous rocks and minor limestone. Ankerite is commonly present and, upon weathering, rocks containing this mineral may assume a reddish-brown colour. This unit, which may be up to 150 meters thick, overlies the Yanks Peak Quartzite and, in turn, is overlain by the Snowshoe Formation. These rocks form several narrow, northwesterly striking, moderately northeasterly dipping bands; at least two of these are believed to pass through the property. The Snowshoe Formation is generally a quartzitic unit with a base of conglomerate or coarse grit. Pebbles in the conglomerate are grey and black quartzi te and are usually deformed. The upper member consists of chlorite schist, limestone and some black slate. This formation is also thought to be about 150 meters thick. Both formations have been intensely folded, possibly experiencing several periods of deformation. The Midas Formation, in addition to folding, also exhibits flowage features due to its position between the more competant Yanks Peak Quartzite below and the Snowshoe Formation above. In the area of the property, the folds, which are isoclinal, are overturned to the southwest explaining the relatively uniform bedding dips to the northeast. The long, narrow bands of Midas rocks mentioned above are anticlinal septa contained in the southwestern limb of the Snowshoe syncline, the axis of which is parallel to the bands and passes through the Cariboo Hudson Mine 5.6 Km north - northeast of the HA-l claim. The plunge of the fold-axes ranges from O” to 20’ to the northwest . Mineral deposits in the region are the gold-bearing quartz-pyritegalena f sphalerite veins (Midas, Homestake, Yanks Peak, Sockett) in the vicinity of Yanks Peak, some 4.3 Km to the west and the gold-bearing quartz-pyrite-galena- sphalerite f scheelite + arsenopyrite veins (Cariboo Hudson, International) and the conformable quartz-scheelite f galena lenses in the Peter Gulch-Simlock Creek area, 4.0 to 5.5 Km to the north-northeast. All of these showings occur in sediments of the Cariboo Group. 2 - From Holland, 1954 . ../4 TABLE 1.: STRATIGRAPIIIC UNITS: YANKS PiXK RXINDTOP MOUNTAIN ARDI.1 (after Holland, 1954) -4- 8. PROPERTY GEOLOGY !I GENERAL STATEMENT The mapped portion of the HA-l claim is underlain by a 670 meter wide, northwesterly trending band of Midas argillaceous sediments that is flanked on either side by quartzitic rocks assigned to the Snowshoe Formation. Five of the six iron oxide seeps noted to date occur within the area of Midas rocks; the sixth and northern most seep has not been examined on theground and, hence, its relationship to the underlying rocks is unknown.
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