The Merritt map area contains 191 recorded mineral occurrences and is
in the Intermontane tectonic belt dominated by Quesnellia terrane rocks and numerous
faults.The Highland Valley porphyry copper district occupies
the western portion of the map where copper deposits lie within the Late Triassic Guichon
Creek batholith. The batholith intrudes sedimentary and volcanic strata of the
Mississippian to Triassic Cache Creek and Upper Triassic Nicola groups and is
unconformably overlain by sedimentary and volcanic strata ranging in age from Lower
Jurassic to Middle Tertiary. Two major past producing mines include Bethlehem
(092ISE001) and Highmont
(092ISE013). Nearby, the JA
deposit (092ISE149) has measured geological reserves of 286 million tonnes grading
0.43 per cent copper and 0.017 per cent molybdenum.
The remainder of the map area is predominantly underlain by Nicola Group
volcanic, sedimentary and intrusive rocks overlain by extensive Quaternary cover. Numerous
copper occurrences are predominant in the Nicola Group.
The Swakum Mountain area is noted for polymetallic skarn-type mineralization,
lead-zinc-silver bearing quartz veins and replacements, and polymetallic-precious metal
quartz veins in Nicola Group rocks. Limited past production has been recorded at the Lucky
Mike (092ISE027), Old
Alameada (092ISE094) and Thelma
(092ISE101). In the Stump Lake area Nicola Group rocks host numerous polymetallic-precious
metal quartz veins (Enterprise
(092ISE028), Joshua
(092ISE109)) which have also received limited past production.
In the Merritt area, the Merritt
Coalfield (092ISE058) occurs in Eocene Coldwater Formation sediments.
The area is a past producer and hosts an estimated 18 million tonnes of high volatile
bituminous B rank coal.
Skarn-type mineralization is also prevalent where Craigmont
Mines (092ISE035) milled 34 million tonnes of copper-iron ore before
closing in 1982. Recent exploration is focussed on epithermal-style mineralization (Redbird
(092ISE179)) in Nicola Group volcanics.
Industrial mineral occurrences have also been identified: bentonite at Quilchena
(092ISE) and Coutlee
(092ISE); gypsum at Merritt
Gypsum (092ISE); and limestone at Promontory
(092ISE144) and Nicola
Lake (092ISE145).

BC Geological Survey Publications for
NTS 092I
