Surficial geology of the Shawnigan Lake area. by H.E. Blyth [and others]

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Ministry of Energy, Mines and Petroleum Resources , Victoria
Geology - British Col
The Physical Object
Pagination1 map Scale 1:50,000
ID Numbers
Open LibraryOL22021683M

Details Surficial geology of the Shawnigan Lake area. by H.E. Blyth [and others] EPUB

The Geomorphology of Vancouver Island is a series of nine based thematic maps that collectively describe the physical nature of Vancouver : Richard Guthrie. Katich, P. J., Jr.,Cretaceous and early Tertiary stratigraphy of central and south-central Utah with emphasis on the Wasatch Plateau area, in Geology of portions of the high plateaus and adjacent canyon lands, central and south-central Utah: Intermountain Assoc.

Petroleum Geologists Guidebook 5th Ann. Field Conf.,p.

Description Surficial geology of the Shawnigan Lake area. by H.E. Blyth [and others] FB2

Reconnaissance geology of northern Toobally Lake (95D/8), southeast Yukon. All content in this area was uploaded by Robert B. MacNaughton. ex pose d a proba ble ol istolit h (e xotic blo ck.

Download Surficial geology of the Shawnigan Lake area. by H.E. Blyth [and others] FB2

Full text of "Regional geology of the southern Lake Erie (Ohio) bottom: a seismic reflection and vibracore study" See other formats. A Canyon is a deep, steep-sided valley formed by weathering and erosion. Explanation; -Canyon are deep, steep-walled, V-shaped valley cut by a river through resistant rock.

Such valleys often occur in the upper courses of rivers, where the stream has a strong, swift current that digs its valley relatively rapidly. The Guano-Guayes property, in the Pelly Mountains of the Yukon Territory, covers a rare earth element (REE) bearing contact metamorphic aureole which developed around a syenite stock during Mississippian time ( ± 10 Ma phlogopite K-Ar date, ± 10 Ma Rb-Sr skarn mineral isochron).

Sedimentary rocks consist of several hundred metres of Ordovician dark gray shale which are faulted .