Lingua: Inglese
Editore: Geological Society of Amer, 1993
ISBN 10: 0813722780 ISBN 13: 9780813722788
Da: ThriftBooks-Dallas, Dallas, TX, U.S.A.
Paperback. Condizione: Very Good. No Jacket. Former library book; May have limited writing in cover pages. Pages are unmarked. ~ ThriftBooks: Read More, Spend Less.
Lingua: Inglese
Editore: Geological Society of America., Boulder, Colorado, U.S.A., 1993
ISBN 10: 0813722780 ISBN 13: 9780813722788
Da: Eryops Books, Stephenville, TX, U.S.A.
Soft cover. Condizione: Very Good. Softcovers; ex-corporate library; light creasing of corners of covers and a few leaves; o/w in very good condition. Book.
EUR 18,72
Quantità: Più di 20 disponibili
Aggiungi al carrelloCondizione: As New. Unread book in perfect condition.
EUR 20,57
Quantità: Più di 20 disponibili
Aggiungi al carrelloCondizione: New.
EUR 42,82
Quantità: 1 disponibili
Aggiungi al carrelloPaperback. Condizione: Brand New. 128 pages. 8.25x6.50x0.50 inches. In Stock.
Editore: The Geological Society of America, Boulder, Colorado, 2021
ISBN 10: 0813725496 ISBN 13: 9780813725499
Da: Joseph Burridge Books, Dagenham, Regno Unito
EUR 59,44
Quantità: 1 disponibili
Aggiungi al carrellovi, 128 pages : illustrations, maps ; 28 cm. Emergence and Evolution of Barbados is a three-part analysis of the Quaternary geologic and geomorphologic evolution of the island of Barbados in the southeastern Caribbean. "Geology of Southeastern Barbados" assembles and integrates detailed observations into a complex 700 k.y. history of marine sculpting and riverine flooding processes. "Marine Terrace Evolution of Windward Barbados" revises the Quaternary stratigraphy of the island, describes the tec-tonics of emergence, and demonstrates that uplift rates vary by location. "Active Emergence, Chronology, and Limestone Facies in Southeastern Windward Barbados" is the first com-prehensive study to integrate marine erosion and deposition with tectonic uplift rates. Major findings of this work are that Barbados' Central Highlands are an erosional remnant, and that terraces originated principally by marine erosion rather than by reef construction.