Okanagan Landscape
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Metamorphic Rocks

Updated 14 February 2014

The east side of the Okanagan Valley is dominated by metamorphic and plutonic (igneous intrusive) rocks. The north Okanagan is dominated by the Monashee Gneiss, at more than 2 billion years old, is some of the oldest rock in the southern interior. The south Okanagan is dominated by Okanagan Metamorphic Complex rocks. These rocks are typically mylonitic gneiss, which are highly fractured and broken due to high pressures in the Okanagan fault zone. 

Nice exposures of metamorphic rocks can be found along Naramata Creek below the falls, along Naramata Road, the cliffs to the East of Vaseaux Lake and McIntyre Bluff. Below are a few photos of metamorphic rocks found in the region.

References

Brown, S, Gibson, D and Thorkelson, D. 2010. Geology of the southern Okanagan Valley shear zone. Unpublished field trip guide. http://gac.esd.mun.ca/sgtd/page3/page40/assets/ctg2010.pdf 

Roed, MA and Fulton, RJ (eds.) 2011. Okanagan Geology South. Okanagan Geology Committee. 238p. 

Okulitch, AV. 2013. Geology, Okanagan Watershed, British Columbia (3 sheets). Geological Survey of Canada, Open File 6389. http://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan/fulle.web&search1=R=292220

Picture
Simplified bedrock geology of the south Okanagan. Polygons with metamorphic rocks labelled with "M". Map based on information from DataBC overlayed on Google Earth.
Picture
Small S-fold and fault within Okanagan Complex metamorphic rock (mylonite). Garnet Fire trail, Penticton (Photo: T Redding)
Picture
Okanagan Complex mylonitic gneiss with large porphyroclasts. (Photo: T. Redding)
Picture
Foliated (light-dark bands) metamorphic rock in the parking lot at Munson Mountain. (Photo: T. Redding)
Picture
Cliff of Okanagan Complex metamorphic rock above Vaseaux Lake. (Photo: T. Redding)
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