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File Created: 07-Apr-1997 by Dani J. Alldrick (DJA)
Last Edit:  27-Apr-2020 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name LOOKOUT, KNOB HILL Mining Division Skeena
BCGS Map 103P041
Status Showing NTS Map 103P05W
Latitude 055º 25' 42'' UTM 09 (NAD 83)
Longitude 129º 52' 57'' Northing 6142812
Easting 444152
Commodities Iron Deposit Types G05 : Cyprus massive sulphide Cu (Zn)
Tectonic Belt Coast Crystalline Terrane Stikine
Capsule Geology

The Lookout occurrence is close to Granby Bay on Observatory Inlet and near the historical mining town of Anyox.

The region is underlain by a roof pendant, consisting of volcanic and sedimentary rocks, within the Eocene Coast Plutonic Complex. These pendant rocks have been correlated with Middle-Upper Jurassic Hazelton Group rocks and overlying upper Middle to Upper Jurassic Bowser Lake Group sedimentary rocks (Geological Survey of Canada Open File 3453). The Hazelton rocks consist of variably chloritized pillow and massive basalt with minor mafic tuffs. The overlying Bowser Lake sediments consist of siltstone and sandstone with minor chert and limestone. There are two observable phases of folding in the area, an initial north-northeast trending phase followed by a later east-northeast trending phase.

The large flat hilltop location of the Lookout occurrence has well exposed bedrock; soil and gravel cover appears to have been stripped away decades ago. There is no indication of major trenching work. Exposed strata are massive pillow lavas on the south part of the hilltop, and pyritic lapilli-rich tuff along the western part of the hilltop, including the highest spine of the hilltop. The string of pyritic outcrop knobs trends 100 degrees and dips 75 degrees north. Pyritic outcrop exposures extend for 100 metres along strike to the west of the spot height (535 metres) where they are cut off to the west by a prominent fault (deep gully). There are a set of prominent fine grained quartz veins cutting across this pyritic rock with an attitude of strike 073 degrees and 55 degrees north dip. Overall, this pyritic zone resembles a distinct stratigraphic unit that has been subsequently sheared and cut by minor quartz veins. The pyritic zone is 1 to 2 metres thick over its entire exposed strike length of 100 metres. This pyritic fragmental unit may represent the distal equivalent/extension of a mineralized copper sulphide horizon.

In 2006, Kenrich-Eskay Mining Corp. completed a program of airborne electromagnetic and magnetic surveys, stream sediment and rock sampling, geological mapping and 50 diamond drill holes, totalling 14275 metres, on the area as the Coastal Copper project.

Bibliography
EMPR BULL 63
EMPR FIELDWORK 1985, pp. 211-216; 1988, pp. 233-240; 1990, pp. 235-243; 2005, pp. 1-4
EMPR MAP 8
EMPR OF 1986-2; 1994-14
EMPR ASS RPT 30152
EMR MIN BULL MR 223 B.C. 298
GSC MAP 307A; 1385A
GSC OF 864; 3453
Sharp, R.J. (1980): The Geology, Geochemistry & Sulphur Isotopes of The Anyox Massive Sulphide Deposits, University of Alberta, M.Sc. Thesis
Harrison, D., McKinley, S. (2007-06-18): Technical Report on the Coastal Copper Project, Anyox Area
EMPR PFD 670953, 670954

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