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The explosion of interest, effort, and information about the ocean since about 1950 has produced many thousand scientific articles and many hun dred books. In fact, the outpouring has been so large that authors have been unable to read much of what has been published, so they have tended to concentrate their own work within smaller and smaller subfields of oceanog raphy. Summaries of information published in books have taken two main paths. One is the grouping of separately authored chapters into symposia type books, with their inevitable overlaps and gaps between chapters. The other is production of lightly researched books containing drawings and tables from previous pUblications, with due...
The Atlantic is also relatively deeper and less cumbered with islands than the Pacific, which has the higher ridges near its shores, constituting what some visitors to the Pacific coast of America have not inaptly called the "back of the world," while the wider slopes face the narrower ocean, into which for this reason the greater part of the drainage of the land is poured... a) What has at first determined the position and form of the Atlantic ocean? b) What changes has it experienced in the lapse of geological time? c) What relations have these changes borne to the development of life on the land and in the water? d) What is its probable future?
The study of the topography and structure of the ocean floor is one of the most important stages in ascertaining the geological structure and history of development of the Earth's oceanic crust. This, in its turn, provides a means for purposeful, scientifically-substantiated prospecting, exploration and development of the mineral resources of the ocean. The Atlantic Ocean has been geologically and geophysically studied to a great extent and many years of investigating its floor have revealed the laws governing the structure of the major forms of its submarine relief (e. g. , the continental shelf, the continental slope, the transition zones, the ocean bed, and the Mid-Oceanic Ridge). The bas...
An account of some aspects of marine geology and marine geophysics, comprehensible to those at an early stage in their study of geology and to scientists who are not specialists in these fields. There are many biologists, chemists, mathematicians or physicists who work in the laboratory or on board ship with geologists and geophysicists and this book will help them to understand the aims of their colleages' experiments. Wherever possible, without a loss of necessary precision, terminology is deliberately simplified.
Foreword by C.S. Piggot, general introduction by W.H. Bradley.-- pt. 1. Lithology and geologic interpretations.-- pt. 2. Foraminifera. (1 v.)-- pt. 3. Diatomaceae -- pt. 4. Ostracoda -- pt. 5. Mollusca -- pt. 6. Echinodermata -- pt. 7. Miscellaneous fossils and significance of faunal distribution -- pt. 8. Organic matter content.-- pt. 9. Selenium content and chemical analysis -- [pt. 10]. Index.
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