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File Created: 19-Dec-2012 by Karl A. Flower (KAF)
Last Edit:  10-Jan-2022 by Del Ferguson (DF)

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NMI
Name ELMER, THUNDER Mining Division Alberni
BCGS Map 092F033
Status Showing NTS Map 092F05E
Latitude 049º 21' 55'' UTM 10 (NAD 83)
Longitude 125º 34' 11'' Northing 5471239
Easting 313432
Commodities Gold Deposit Types I02 : Intrusion-related Au pyrrhotite veins
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Elmer occurrence is located 150 metres south of Ursus Creek, approximately 35 kilometres northeast of Tofino, B.C.

The area is underlain by middle to late Triassic Karmutsen basalt. These basalts are overlain by massive to thickly bedded calcareous mudstones of the Quatsino Formation. These volcanic and stratified rocks have been invaded by a middle to late Jurassic biotite-hornblende granodiorite and quartz diorite. The area has been subjected to major faulting with a dominant northwest-southeast trend.

The Elmer zone consists of two parallel quartz veins located 25 metres apart in an extensive shear zone. The quartz veins vary from 0.2 to 1.0 metre wide and have been detected over a 300 metre strike length. Sulphide mineralization in the veins includes up to 20 per cent pyrite, 10 per cent galena and 5 per cent sphalerite. The veins are hosted by chlorite and carbonate altered quartz diorites.

Sampling of the veins assayed up to 38.4 grams per tonne gold and chip sampling of the host quartz diorites assayed up to 3.4 grams per tonne gold (Assessment Report 26412).

The area was originally explored in 1939 with the discovery of float containing coarse gold near the junction of Ursus and Thunderbird creeks. In 1979, the property was acquired by S. Craig and later optioned to Eldorado Minerals and Petroleum as the Ureka and Opus claims. In 1984, Eldorado completed a program of trenching and geochemical sampling that identified the Camp Zone (MINFILE 092F 067). From 1986 to 1987, Pacific Sentinel Gold completed programs of geochemical surveying, geological mapping and magnetometer and VLF surveys. This work identified three new zones, including the Junction (MINFILE 092F 450), and Mid-Pad (MINFILE 092F 449) occurrences. From 1988 to 1989, Pezgold Resource optioned the property and completed a program of diamond drilling on the Junction zone, and prospecting which led to the discovery of the Elmer zone to the east. In 1990 Pacific Sentinel Gold completed a program of geological mapping, rock sampling and trenching. In 1995, the area was prospected as the Thunderbird claims by S. Salmon. In 1999, the area was claimed as a part of the Thunder claims and a program of geological mapping, geochemical sampling and geophysical surveys were completed on the Elmer zone.

Bibliography
EMPR ASS RPT 9378, 12623, 16450, 19374, 20474, 24426, *26412, 37525
EMPR BULL *8, p. 67-68; 13
EMPR EXPL 1980-171; 1984-162,163; 1987-C145
EMPR PF (Prospectus: Pacific Sentinel Gold Corp., August 31, 1987; Filing Statement: Pacific Sentinel Gold Corp., May 9, 1988; District Geologist photos, 1995; Maps (various) (c.1995); Property Review Statement of Material Change, Pacific Sentinel Gold Corp., 1992; Woodcock, J.R. (1987): The Ursus Creek Project for Baron Ventures Ltd.; Prospectors Report 1995-24 by Simon Salmon)
GSC MAP 17-1968; 1386A
GSC MEM 204
GSC OF 463
GSC P 68-50; 72-44; 79-30; 80-16
GCNL #67, 1984; #11,#13,#104,#227, 1988; #4,#31, 1989
N MINER Jun.12, 1995
V STOCKWATCH Jan.18, 1988
Carson, D.J.T. (1968): Metallogenic Study of Vancouver Island with Emphasis on the Relationships of Mineral Deposits to Plutonic Rocks, Unpublished Ph.D. Thesis, Carleton University

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