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File Created: 30-Mar-2022 by Garry J. Payie (GJP)
Last Edit:  27-Jan-2025 by Del Ferguson (DF)

Summary Help Help

NMI
Name CD NORTH, GOLDRANGE, NORTH CLOUD DRIFTER Mining Division Clinton
BCGS Map 092N057
Status Showing NTS Map 092N10E
Latitude 051º 31' 44'' UTM 10 (NAD 83)
Longitude 124º 37' 21'' Northing 5709892
Easting 387443
Commodities Gold, Lead Deposit Types I02 : Intrusion-related Au pyrrhotite veins
Tectonic Belt Coast Crystalline Terrane Stikine
Capsule Geology

The CD NORTH occurrence is on a southwest-facing alpine ridge sides west of Ottarasko Creek,14 kilometres west of Tatlayoko Lake, 41 kilometres south of the community of Tatla Lake on Highway 20 and 184 kilometres southwest of Williams Lake, B.C.

The showing is underlain by rocks of the Lower Cretaceous Cloud Drifter Formation consisting largely of sandstone. A granodioritic stock of the Late Cretaceous to the Paleocene Bendor Suite intrudes the Cloud Drifter sediments about 1 kilometre to the west.

The CD North zone consists of an area of hornfelsed sedimentary rocks and intrusive rock where anomalous ridge and spur talus fines yielded samples that graded up to 0.23 gram per tonne gold and rock samples graded up to 0.37 grams per tonne gold, and 0.39 per cent antimony and 0.42 per cent lead (Sample S3690953) (Press Release, Kingfisher Metals Corp., September 28, 2021, and Assessment Report 39734, Tables 3 and 16). Initial signs were considered promising for the formation of auriferous veins.

From 2020 through 2022, Kingfisher Metals Corp. conducted regional exploration on their large Goldrange property, which included the CD North showing. No ground work was documented in the CD North area, but structural interpretations were made in 2022 from airborne data collected in 2020 over the Goldrange project area.

Bibliography
EMPR ASS RPT 39459, 39734, 41643
GSC OF 1163
GSC P 68-33
GSC MAP 5-1968; 1713A
PR REL Kingfisher Metals Corp. Mar. 31, Apr. 14, 21, May 13, Jul. 7, Aug. 9, Sep. 2, *28, Oct. 6, Nov. 16, 2021; Jan. 12, Feb. 1, Mar. 2, 9, 2022

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