Last edited by Faushura
Thursday, July 16, 2020 | History

2 edition of Geology of the Straw Lake Area found in the catalog.

Geology of the Straw Lake Area

Ontario Geological Survey.

Geology of the Straw Lake Area

Districts of Kenora and Rainy River.

by Ontario Geological Survey.

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Published by s.n in S.l .
Written in English


Edition Notes

1

SeriesOntario Geological Survey report -- 222
ContributionsEdwards, G.
ID Numbers
Open LibraryOL21808131M

Geology of the Chewelah-Loon Lake area, Stevens and Spokane counties, Washington, with a section on potassium-argon ages of the plutonic rocks Professional Paper By: Fred K. Miller, Lorin Delbert Clark, and J.C. Engels. GEOLOGY. The underlying bedrock of Michigan is mostly hidden from view by unconsolidated material deposited during continental glaciation. However, there are a number of places in the Lower Peninsula where the bedrock can be seen such as in rock quarries and in outcrops along rivers and lakes.

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Geology of the Straw Lake Area by Ontario Geological Survey. Download PDF EPUB FB2

T he geologic story of the landscape surrounding lakes Mead and Mohave began more than a billion years ago when this area was a shallow sea. Sediments from this ancient ocean were invaded and contorted by molten rock, some of which made it to the surface as lava flows.

The mix of molten rock, sediments and lava cooled to become the billion-year-old gneiss, schist, and granite. Additional Physical Format: Online version: Edwards, Geniana R., Geology of the Straw Lake area, districts of Kenora and Rainy River. Toronto, Ont.: Ontario Ministry of Natural Resources,   This book is for San Francisco Bay Area residents and visitors who want to explore the geologic world of this spectacular area, to learn about its shapes, colors, and rocky foundations.

Doris Sloan illuminates the colorful geologic mosaic that surrounds San Francisco Bay and lucidly explains the complex and fascinating processes that have Cited by: The geology of England's Lake District is dominated by sedimentary and volcanic rocks of mainly Ordovician age underpinned by large granitic r sedimentary sequences outcrop on the edges of the Lake District area, with Silurian to the south, Carboniferous to the north, east and west and Permo-Triassic to the west and east.

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