British Columbia Ministry of Energy, Mines and Natural Gas and Responsible for Housing
News | The Premier Online | Ministries & Organizations | Job Opportunities | Main Index

MINFILE Home page  ARIS Home page  MINFILE Search page  Property File Search
Help Help
File Created: 16-Feb-2026 by Karl A. Flower (KAF)
Last Edit:  14-Mar-2026 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name SOLLY NORTH, NORTH GRID Mining Division Victoria
BCGS Map 092B081
Status Showing NTS Map 092B13W
Latitude 048º 53' 10'' UTM 10 (NAD 83)
Longitude 123º 53' 54'' Northing 5415194
Easting 434151
Commodities Copper, Lead, Zinc, Silver, Gold Deposit Types G06 : Noranda/Kuroko massive sulphide Cu-Pb-Zn
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Solly North occurrence is located from approximately 720 to 820 metres elevation on a southwest-facing slope, northeast of Solly Creek and approximately 3.9 kilometres south-southwest of Mount Hall. The Lara (MINFILE 092B 192) developed prosect is located approximately 700 metres to the southwest.

Regionally, the area is underlain by chert, siliceous argillite and siliciclastic rocks of the Mississippian to Pennsylvanian Fourth Lake Formation (Buttle Lake Group) and volcanic rocks of the Middel to Upper Devonian McLaughlin Ridge Formation (Sicker Group), which have been intruded by gabbroic bodies (called the Mount Hall Gabbro) that are coeval with the Upper Triassic Karmutsen Formation (Vancouver Group). See the Lara (MINFILE 092B 129) occurrence for a larger discussion of the regional geology.

Locally, a moderately spaced grouping of drillholes has identified weak to moderate polymetallic mineralization similar to that of the nearby Randy North (MINFILE 092B 128) and Lara (MINFILE 092B 129) occurrences.

In 1987, diamond drilling yielded intercepts including 0.240 per cent copper, 0.100 per cent lead and 0.525 per cent zinc over 1.54 metres (67.44 to 68.98 metres down hole) from a quartz eye tuff and cherty tuff hosting quartz veins and veinlets with sphalerite and chalcopyrite in hole 87-177; 0.400 per cent copper over 0.32 and 1.57 metres, each, (542.88 to 543.40 and 577.52 to 579.08 metres down hole, respectively) from a volcaniclastic sequence with crystal lithic tuff hosting disseminations and stringers of chalcopyrite, pyrite and pyrrhotite in hole 87-210; 0.076 per cent copper, 0.240 per cent lead, 0.480 per cent zinc, 3.0 grams per tonne silver and 0.380 gram per tonne gold over 0.31 metre (60.96 to 61.27 metres down hole) from a quartz eye crystal tuff hosting quartz veins with pyrite, sphalerite and chalcopyrite in hole 87-211; 0.550 per cent copper over 1.22 metres (104.87 to 106.09 metres down hole) from an andesite lapilli tuff hosting veinlets and blebs of pyrite and chalcopyrite in hole 87-213; 1.066 per cent zinc over 1.55 metres (21.81 to 23.36 metres down hole) from a lithic tuff hosting sphalerite in hole 87-214; 0.131 per cent copper, 0.257 per cent lead, 0.674 per cent zinc, 3.7 grams per tonne silver and 0.222 gram per tonne gold over 0.70 metre (217.86 to 218.56 metres down hole) from a rhyolite quartz eye tuff hosting pyrite with minor chalcopyrite, sphalerite and trace galena and tetrahedrite and 0.640 gram per tonne gold over the following 1.60 metres (218.56 to 220.16 metres down hole) from a rhyolite dust tuff hosting pyrite blebs with trace chalcopyrite in hole 87-216 (Assessment Report 17857).

Work History

The area has been explored in conjunction with the nearby Lara (MINFILE 092B 129) occurrence, and a complete exploration history of the area can be found there.

Bibliography
EMPR ASS RPT 936, 7384, 11123, 13655, 14492, 15504, 15737
*17857, 19806, 19807, 20980, 20981, 26021, 29840, 31578,
35428, 37716
EMPR EXPL 1977-E105; 1978-E122; 1979-122
EMPR FIELDWORK 1982, p. 46; 1987, pp. 81-91
EMPR OF 1988-8; 1999-2
GSC MAP 42A; 1386A; 1553A
GSC MEM 13; 96
GSC OF 463
GSC P 1972-44; 1975-1A, p. 23; 1979-30
PERS COMM Massey, N.W.D., 1991
Carson, D.J.T. (1968): Metallogenic Study of Vancouver Island with Emphasis on the Relationship of Plutonic Rocks and Mineral Deposits, Ph.D. Thesis, Carleton University
Holbek, P. (1980): Geology and Geochronometry of the Sharron Volcanogenic Prospect, Mt. Brenton Area, Southwestern B.C., B.Sc. Thesis, University of British Columbia
Kelso, L. (2007-11-15): Independent Technical Report and Mineral Resource Estimation – Lara Polymetallic Property
Kelso, L. (2008-04-02): Independent Technical Report and Mineral Resource Estimation – Lara Polymetallic Property

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY