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File Created: 30-Nov-1995 by Garry J. Payie (GJP)
Last Edit:  27-May-2020 by George Owsiacki (GO)

Summary Help Help

NMI
Name SETTEA CREEK, SETTEA LAKE Mining Division Liard
BCGS Map 104I026
Status Prospect NTS Map 104I02W
Latitude 058º 14' 51'' UTM 09 (NAD 83)
Longitude 128º 58' 52'' Northing 6456266
Easting 501109
Commodities Gold Deposit Types C01 : Surficial placers
Tectonic Belt Intermontane Terrane Overlap Assemblage, Cache Creek, Stikine
Capsule Geology

Placer gold activity is reported to have occurred on Settea Creek although no gold production has been recorded (Bulletin 28, page 56). A placer gold locality on Settea Creek is plotted on Geological Survey of Canada Open File map 2779, just over a kilometre downstream from Settea Lake and about 64 kilometres southeast of Dease Lake.

The area drained by Settea Creek is mainly underlain by Lower Jurassic Inklin Formation rocks (Laberge Group) and Upper Triassic Sinwa Formation (Stuhini Group) limestone. Inklin Formation rocks comprise phyllitic slate, greywacke and conglomerate.

The Settea Lake placer claims follow the active channel of Settea Creek for over 23 kilometres southeast of Turnagain Lake, and are centred on Settea Lake and the southern side of a wide U-shaped valley. Other placer claims in the area follow small tributaries that feed into the main Settea Creek. In 2013, exploration work on behalf of Golden Bear Mining Ltd. was to test prospective gravels locations in the northern part of the property and to test the hypothesis that the source of gold was from the Wade Lake tributary. A series of 1-2 metre deep test pits were dug by hand in the gravels along a meander in the northern part of the property. These gravels were run through a 2-metre-high banker sluice. They were analyzed by ICP and by BLEG (Bulk Leachable Gold) at ALS Minerals Ltd. in Vancouver. Fine and coarse gold was recovered and analyzed under microscope. A series of stream sediment samples were also collected from the tributary between Wade Lake and Settea Lake. These were collected to better understand the distribution of gold on the Settea Lake property. Stream sediment samples were screened, panned sluiced in a 1.5 metre portable sluice. This exploration has found evidence of low grade, gold-bearing gravels on the property. In the southwest, the highest grades are associated with gravels lain on top of sub-horizontal basaltic bedrock; in the northeast of the property, the highest grades were found in a clay-rich bench along a meander in the Settea River (Assessment Report 34949).

From 2008 to 2012 the property was explored by Golden Bear Mining Ltd.; the results of this work are unknown.

Bibliography
EMPR BULL *28, p. 56
EMPR ASS RPT 9024, 34242, *34949
EMPR OF 1996-11
EMPR PFD 861365, 861961
GSC MAP 29-1962; 9-1957; 1418A; 1712A
GSC OF 610; 2262; *2779
GSC BULL 504
GSC P 78-1A, pp. 25-27
Placer Dome File

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