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File Created: 22-Mar-2012 by Karl A. Flower (KAF)
Last Edit:  05-Mar-2020 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name CLUTCH 1-4, CLUTCH, JR, 716, 766 Mining Division Kamloops, Vernon
BCGS Map 082L033
Status Showing NTS Map 082L05E
Latitude 050º 23' 08'' UTM 11 (NAD 83)
Longitude 119º 35' 43'' Northing 5584720
Easting 315507
Commodities Opal, Agate, Gemstones, Diatomite Deposit Types Q11 : Volcanic-hosted opal
Q03 : Agate
Tectonic Belt Intermontane Terrane Quesnel, Overlap Assemblage
Capsule Geology

The Clutch 1-4 (JR) occurrence is situated in the headwaters of Ewer Creek, approximately 12.5 kilometres south of Falkland.

Regionally the area is underlain by volcanics, mudstone, siltstone, shale and fine clastic sedimentary rocks of the Devonian to Triassic Harper Ranch and(?) Nicola groups, which are intruded by Middle Jurassic granitic rocks. Extensive volcanic and sedimentary rocks of the Eocene Kamloops and Penticton groups overlie the older units and include waterlain clast- and matrix- supported lahars and ash to lapilli tuffs that host common opal, agate and a variety of zeolite minerals.

Locally, at the JR zone, precious opal and facet-grade opal were discovered in a red lahar layer of a basaltic andesite. Opal occurs in an agate-rich zone within the lahar. Individual precious opal and facet-grade opal grains are generally fine grained; the largest grain seen was approximately 1.5 centimetres long. The precious opal is clear to greyish translucent with bright play of colours including green, blue, pink and orange. The facet-grade opal shows pale salmon pink to orange to gold colour in whitish slightly translucent grains. Common opal occurs as vesicle filling throughout the agate-rich rocks. Fine free gold associated with quartz vein/agate and opalized material has possibly been identified from the JR zone.

Two other zones (716 and 766) of common opal, agate and diatomaceous earth are reported approximately 650 metres to the southwest of the main (JR) zone. Common opal, agate and minor pyrite mineralization occur as north-trending fracture fillings, whereas at the 716 zone a white diatomaceous earth layer varies from approximately 10 to 15 centimetres thick.

In 1997, a single large grain of dark bluish-grey translucent opal 4 centimetres in diameter was observed in a piece of lahar rubble (Assessment Report 25214).

In 1993, the Clutch 1-4 claims were staked to cover an area of abundant agate mineralization and a program of geological mapping and prospecting was performed through 1997 for precious opal.

In 2017 and 2018, Opal Resources Canada Inc. conducted programs of prospecting, geological mapping, geochemical sampling and trenching on the area as the Klinker/Ewer property. This work was centred on the JR, 716 and 766 zones.

Bibliography
EMPR ASS RPT 23574, 25214, 37376, *38166
EMPR FIELDWORK 1982, pp. 89-92; 1987, pp. 55-58; 1988, pp. 355-363
EMPR MAP 37, 5214G, 7216G
EMPR OF 1989-5, 1990-30
EMPR RGS 1976
GSC MEM 296
GSC MISC RPT *8, p. 65, 67
GSC OF 637, 736, 2167
GSC P 89-1E pp. 51-60

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