Massive sulphide ore with bands of chalcopyrite and sphalerite
Virtual Museum ID: 19-DP05
Massive sulphide ore with bands of chalcopyrite and sphalerite.
The information listed below relates to the current holding location or collection that the sample is from, and whether the item is viewable at that location or is part of a private collection. Coordinates are given as guides, and we remind you that collecting specimens from these locations is not allowed. Caution is advised visiting such sites and Below BC assumes no responsibility for any injuries or trespassing charges that may occur as a result of the viewer entering these sites.
Original Collection:Dave Pighin (DP)
Virtual Museum ID:19-DP05
Date Added to VM:2019-06-16
Sample Origin:Nelson, BC
Specific Site:Kootenay King
Datum:11 (NAD 83)
Primary Features:Massive sulphide ore with bands of chalcopyrite and sphalerite
Primary Mineral Formula:(Zn,Fe)S, CuFeS2
Advanced Geological Information
The following section provides geological data relating to the specimen or the site it was collected from, when available. Information has been obtained from various sources including private and government datasets but may not be up to date. Any geological time periods or ages listed often relate to the primary geology of the area, and may not be the actual date of an event such as mineral formation.
Geological Formation:Lower Aldridge Formation
Stratigraphic Age:1000 to 1600 Million Years Ago
Geological Terrane:Ancestral North America
The Kootenay King workings are located approximately 30 kilometres northeast of Kimberley on the east side of Lakit Mountain.
Regionally, the area is underlain by Proterozoic clastic Purcell metasediments intruded by syngenetic gabbro and diorite sills and dykes of the Moyie intrusions and later intrusions of felsic and lamprophyre suites.
The Kootenay King deposit is a stratiform lead-zinc deposit. Pyrite, galena and sphalerite occur as fine laminations at the top of a coarse sandstone unit (Kootenay King quartzite) within a buff weathering section of the Helikian Lower Aldridge Formation (Purcell Supergroup). The deposit lies within the eastern overturned flank of a major anticline. The Kootenay King quartzite has a hanging wall of black argillites and a footwall of brown siltstones. The anticlinal structure plunges gently to the north.
In 2012, Klondike Gold Corp. completed prospecting at the Kootenay King workings and the surrounding area. Highlights include rock sample SKKG-97, which assayed greater than 1 per cent lead and 66.8 grams per tonne silver, and rock sample MKKG-79, which assayed 0.57 per cent lead, 0.11 per cent zinc and 27.5 grams per tonne silver (Assessment Report 33471).