|Contributions||Fitzgerald, D.M., Rosen, P.S.|
|LC Classifications||GB 582 G57 1987|
|The Physical Object|
|Number of Pages||364|
Glaciated Coasts Paperback – Novem by Duncan M. Fitzgerald (Editor) See all 3 formats and editions Hide other formats and editions. Price New from Used from Kindle "Please retry" $ — — Hardcover "Please retry" $ $ $ Paperback "Please retry" $ $ Format: Paperback. Glaciated Coasts is a collection of articles that deals with shoreline morphologies of glaciated coasts and the processes that formed these coastlines in North America. This book examines nonsandy shorelines and covers a range of geologic and geographic coastal settings in a Book Edition: 1. ISBN: OCLC Number: Description: xv, pages: illustrations ; 24 cm: Contents: Geomorphology of a tectonically active, glaciated coast, South-Central Alaska / Larry G. Ward, Thomas F. Moslow, and Kenneth Finkelstein --Fjord sedimentation in Northern British Columbia / S.B. McCann and R.A. Kostaschuk --Coarse-grained beach sedimentation under paraglacial. Glaciated coasts. San Diego: Academic Press, © (DLC) (OCoLC) Material Type: Document, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: Duncan M FitzGerald; Peter S Rosen.
Glaciated coasts are dominated or closely affected by glaciers and glacier processes. They include: (1) modern systems in direct contact with glacial ice; (2) proglacial systems, in front of or adjacent to active glaciers; and (3) paraglacial coasts, formerly glaciated systems that are controlled by glacial geomorphology, sediment sources, and/or isostatic responses. There are a wide variety of glaciated coasts, usually with both erosional and depositional features. Coasts may be actively glaciated systems, such as Antarctica, southeastern Alaska, and Greenland, or formerly glaciated regions such as Scandinavia, Scotland, northeastern Canada and New England, the Pacific Northwest, and southern Chile. Past Glacial Environments, Second Edition, presents a revised and updated version of the very successful first edition of Menzies’ book, covering a breadth of topics with a focus on the recognition and analysis of former glacial environments, including the pre-Quaternary glaciations. The book is made up of chapters written by various geological experts from across the world, with the editor. 2. New Jersey's outer coast is made up of mostly barrier islands, while Maine's is mostly bedrock. Why does the coast of New Jersey differ so much from Maine? a) New Jersey has fewer freezing days; b) Maine's coastline is higher than New Jerseys; c) A subduction zone is slowly forming off the Maine coast; d) Maine's coast was glaciated, New.
Peter Duncan: free download. Ebooks library. On-line books store on Z-Library | B–OK. Download books for free. Find books. Peter S Rosen Duncan Fitzgerald Boston Harbor Island shorelines have formed from the submergence and erosion of drumlins,which provided sediment to form connected spits, or tom bolos. Tourism in glaciated areas: The French Alps - Chamonix Chamonix is located on the North-Western part of the French Alps, 15 km from the Swiss border and 15km from the Italian border. The area is dominated by Mont Blanc which stands at 4,m tall and attracts . Beaches and Coasts Richard A. Davis Jr and Duncan M. FitzGerald BACA01 12/03/ Page i. BACA01 12/03/ Page xii. 17 Glaciated coasts 18 Rocky coasts 19 Reef coasts 20 Coastal erosion 21 Human interaction with coastal dynamics Glossary File Size: 1MB.