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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  03-Nov-1994 by Garry J. Payie (GJP)

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NMI
Name YOLA CREEK Mining Division New Westminster
BCGS Map 092H023
Status Showing NTS Map 092H03W
Latitude 049º 12' 54'' UTM 10 (NAD 83)
Longitude 121º 24' 31'' Northing 5452576
Easting 615894
Commodities Copper Deposit Types K : SKARN
Tectonic Belt Coast Crystalline Terrane Undivided Metamorphic Assembl., Plutonic Rocks
Capsule Geology

Pyrrhotite and chalcopyrite in lime silicate rock (skarn) occur within granite gneiss of the Custer Gneiss complex. The Custer Gneiss is derived mainly from lower Mesozoic and possibly Paleozoic and Precambrian rocks, and metamorphosed in the Late Cretaceous or early Tertiary.

Two mineral showings are indicated on the north side of the Yola Creek valley about 1 kilometre downstream from where Cantelon Creek enters, possibly at about 2000 and 2500 metres elevation (GSC Summary Report 1923 Part A, Map 2023).

It is reported to be very similar to the Hinton 1,2 occurrence (092HSW100).

Bibliography
GSC MAP 737A; 1069A; 12-1969; 41-1989
GSC P 69-47
GSC SUM RPT *1923A, p. 72 (Map 2023)
EMPR PFD 673300

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