Ecstall Greenstone Belt
The Ecstall Greenstone Belt is a north-northwest trending
Kitimat, in the vicinity of the Ecstall River. This 80 km (50 mi) long and 3 to 20 km (1.9 to 12.4 mi) wide geologic feature forms a small portion of the 2,000 km (1,200 mi) long Central Gneiss Complex, which ranges from Proterozoic-to-Paleozoic age. Metavolcanic and metasedimentary rocks as well as quartzite and layered gneiss comprise the Ecstall Greenstone Belt.[1]
See also
References
- ^ Alldrick, D.J.; Friedman, R.M.; Childe, F.C. (2000), "Age and Geologic History of the Ecstall Greenstone Belt, Northwest British Columbia", Geological Fieldwork 2000, no. 2001–1, British Columbia Geological Survey
 | This article about a location on the Coast of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
 | This article about a specific Canadian geological feature is a stub. You can help Wikipedia by expanding it. |