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File Created: 03-May-2023 by Karl A. Flower (KAF)
Last Edit:  02-Jun-2023 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name EAGL 1, SOUTH PLATEAU, SOUTHWEST PONDS, EAGL WEST, EAGLE MOUNTAIN Mining Division Liard
BCGS Map 104P003
Status Prospect NTS Map 104P03W
Latitude 059º 03' 27'' UTM 09 (NAD 83)
Longitude 129º 29' 19'' Northing 6546568
Easting 471970
Commodities Gold, Silver, Lead, Zinc, Antimony, Copper Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Slide Mountain, Cassiar
Capsule Geology

The Eagl 1 (South Plateau-Southwest Ponds) occurrence is located near the north side of a series of small lakes on a gentle northwest-facing slope, south of the Dease River and approximately 5.5 kilometres southeast of its junction with the Eagle River.

Regionally, the area is underlain by basaltic intrusive rocks of the Permian Slide Mountain Complex (Blue Dome fault zone). Several kilometres to the southwest alkali feldspar granite intrusive rocks of the Lower Cretaceous Cassiar Batholith are exposed.

Locally, at the South Plateau–Southwest pond zone(s) massive sphalerite-galena breccia and fine-grained pyrite veins in a manganese-iron–stained outcrop. A second zone of mineralization, referred to as Eagl West zone, located approximately 1 kilometre north of the previous zone, comprises an area of silicification and iron carbonate–altered volcanic rocks hosting (chalcedonic) quartz-clay stockworks with disseminated pyrite and lesser galena-chalcopyrite mineralization.

In 1983, three samples (32912C, 32915C and 32918C) from the Eagl West zone yielded from 0.12 to 0.80 gram per tonne gold with up to 22.0 grams per tonne silver, 1.00 per cent lead and 0.20 per cent zinc, whereas a sample (32923C) from the South Plateau zone yielded 0.22 gram per tonne gold, greater than 1.00 per zinc and greater than 100 grams per tonne silver (Assessment Report 12218).

In 1984, channel samples of subcrop from trench 6 on the South Plateau zone yielded up to 0.30 gram per tonne gold, greater than 100 grams per tonne silver, greater than 1.00 per cent zinc, 1.00 per cent lead and 0.057 per cent antimony over 4.00 metres (sample 74540E), whereas a sample (7592E) of quartz vein hosting chalcopyrite-galena mineralization from the area assayed 0.23 per cent copper 0.066 per cent antimony, 12.3 grams per tonne silver and 0.17 gram per tonne gold (Assessment Report 12495).

In 1986, diamond drilling o the South Plateau-Southwest pond zone yielded intercepts of 0.6 gram per tonne gold and 42.1 grams per tonne silver over 2.4 metres, including 2.7 grams per tonne gold and 557 grams per tonne silver over 0.15 metre in hole 1 and 0.4 gram per tonne gold and 23.6 grams per tonne silver over 1.9 metres, including 0.8 gram per tonne gold and 342 grams per tonne silver over 0.10 metre in hole 2 (Assessment Report 15839).

Work History

The area has been explored in conjunction with the nearby Eagl (MINFILE 104P 073) occurrence, 2 kilometres to the east-southeast, and a complete exploration history can be found there.

Bibliography
EMPR ASS RPT *12218, *12495, 15150, *15839, 40516
EMPR BULL 83
EMPR EXPL 1983-558; 1986-A41,C460
EMPR FIELDWORK 1987, pp. 245-248
EMPR OF 1989-9; 1996-11
GSC MAP 381A; 1110A
GSC MEM 194; 319
GSC OF 2779
GCNL #120, 1986; #243, 1988
V STOCKWATCH Jul. 1987
Harms, T.A. (1986): Structural and Tectonic Analysis of the Sylvester Allochthon, Northern British Columbia, Implications for Paleogeography and Accretion, Ph.D. Thesis, University of Arizona

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