The Mid-Oceanic Ridges: Mountains Below Sea Level

The existing oceans are geologically relatively young. They formed when a large supercontinent (Pangaea) broke apart some 150 Ma ago. The mid-oceanic ridges are narrow belts of submarine mountains marking the boundaries between plates which are moving apart, with new oceanic crust being created at the same time. Under the continents oceanic crust is subducted. The ocean bottom is an ideal location to study recent geodynamic processes on Earth. Of special interest for the reader will be the combination of the most recent oceanographic data with ophiolites, representing fossil ocean crust, obducted onto the continents by tectonic processes. The book is mainly written for students, teachers and scientists in the broad field of geosciences. In addition, it will be of interest to a broad readership since the text is accompanied by figures, most in color, of excellent quality and significance.

"1114935204"
The Mid-Oceanic Ridges: Mountains Below Sea Level

The existing oceans are geologically relatively young. They formed when a large supercontinent (Pangaea) broke apart some 150 Ma ago. The mid-oceanic ridges are narrow belts of submarine mountains marking the boundaries between plates which are moving apart, with new oceanic crust being created at the same time. Under the continents oceanic crust is subducted. The ocean bottom is an ideal location to study recent geodynamic processes on Earth. Of special interest for the reader will be the combination of the most recent oceanographic data with ophiolites, representing fossil ocean crust, obducted onto the continents by tectonic processes. The book is mainly written for students, teachers and scientists in the broad field of geosciences. In addition, it will be of interest to a broad readership since the text is accompanied by figures, most in color, of excellent quality and significance.

54.99 In Stock
The Mid-Oceanic Ridges: Mountains Below Sea Level

The Mid-Oceanic Ridges: Mountains Below Sea Level

The Mid-Oceanic Ridges: Mountains Below Sea Level

The Mid-Oceanic Ridges: Mountains Below Sea Level

Paperback(1995)

$54.99 
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Overview

The existing oceans are geologically relatively young. They formed when a large supercontinent (Pangaea) broke apart some 150 Ma ago. The mid-oceanic ridges are narrow belts of submarine mountains marking the boundaries between plates which are moving apart, with new oceanic crust being created at the same time. Under the continents oceanic crust is subducted. The ocean bottom is an ideal location to study recent geodynamic processes on Earth. Of special interest for the reader will be the combination of the most recent oceanographic data with ophiolites, representing fossil ocean crust, obducted onto the continents by tectonic processes. The book is mainly written for students, teachers and scientists in the broad field of geosciences. In addition, it will be of interest to a broad readership since the text is accompanied by figures, most in color, of excellent quality and significance.


Product Details

ISBN-13: 9783540573807
Publisher: Springer Berlin Heidelberg
Publication date: 02/17/1995
Edition description: 1995
Pages: 201
Product dimensions: 6.10(w) x 9.25(h) x 0.02(d)

Table of Contents

1 Young and Living Oceans.- 2 The Earth, a Heat Engine.- 3 The Ridges — Cradles of the Ocean.- 4 Submarine Exploration.- 5 Ophiolites — or in Search of Lost Oceans.- 6 Mantle Metallurgy.- 7 The Forges of Vulcan in the Kingdom of Neptune.- 8 From Rifts to Fast-Spreading Ridges.- 9 The Major Pulsations of the Earth.- Source of Illustrations.
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