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File Created: 01-Aug-2013 by Karl A. Flower (KAF)
Last Edit:  20-Jun-2020 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name BELVIDERE (L.301), TORTILLA (L.536), NAHMINT Mining Division Alberni
BCGS Map 092F005
Status Showing NTS Map 092F03E
Latitude 049º 02' 24'' UTM 10 (NAD 83)
Longitude 125º 01' 08'' Northing 5433866
Easting 352456
Commodities Copper, Silver Deposit Types K : SKARN
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Belvidere (L.301) and Tortilla (L.536) occurrences are located approximately 2 kilometres north of the mouth of a creek flowing into Snug Basin.

The area is underlain by a narrow north trending band of Upper Triassic Quatsino Formation (Vancouver Group) limestone. The band is in contact on the west with Karmutsen volcanics (Vancouver Group), and on the east with Lower Jurassic volcanics (Bonanza Group). The strata is intruded by diorite and granodiorite of the Early to Middle Jurassic Island Plutonic Suite.

At the Belvidere (L.301) occurrence a 0.05 metre thick, rusty and vuggy copper skarn vein, oriented at 305 degrees strike and dipping 70 degrees northwest, is exposed over 10 metres length. The skarn is hosted by a felsic intrusive and contains chalcopyrite and pyrite with garnet. In 2007, a select outcrop grab sample (362657) assayed 1.52 per cent copper and 5 grams per tonne silver (Assessment Report 29574).

At the Tortilla (L.536) occurrence, located approximately 200 metres north, a 1.5 metre thick, foliated, fractured and vuggy iron-copper skarn zone, oriented at 155 degrees strike and 60 degrees dip to the south west, is exposed over a 15 to 25 metre strike length. The skarn zone is hosted by a mafic intrusive and contains magnetite with sulphide fractures and in-fillings including pyrite, chalcopyrite with garnet and epidote. In 2007, a select outcrop grab sample (362658) assayed 3.42 per cent copper and 3.5 grams per tonne silver (Assessment Report 29574).

The area was originally explored in 1899 and 1916. An old adit occurs on the Tortilla (L. 536) crown grant from this time. In 1965, Alberni Mines completed a program of geological mapping, geochemical sampling and a ground magnetometer survey. In 1967, Mt. Agnes Mines completed a ground magnetometer survey on the area. In 1969 and 1970, Nootka Explorations completed a program of rock and soil sampling, geological mapping and a ground magnetometer survey on the area as the Henderson property.

In 2007 through 2013, Nahminto Resources completed a program of prospecting, geological mapping, geochemical sampling, a ground magnetometer survey and airborne geophysical surveys on the area as the TJM claims, part of the Nahmint property.

Bibliography
EMPR ASS RPT 777, 2856, 29252, *29574, 29660, 30799, 31248, 31708, 32603, 33092
EMPR FIELDWORK 1988, pp. 61-74
EMPR GEM 1971-233
GSC BULL 172
GSC MAP 17-1968; 1386A
GSC OF 463
GSC P 68-50; 71-36; 72-44
Carson, D.J.T. (1968): Metallogenic Study of Vancouver Island With Emphasis on the Relationships of Mineral Deposits to Plutonic Rocks, Unpublished Ph.D. Thesis, Carleton University
Houle, J. (2009-02-09): Technical Report on The Nahmint Property
Houle, J. (2013-11-30): Technical Report on the Nahmint Property

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