Robert c speed hai cheng (2 risultati)

Autore: 
Perfeziona con la Ricerca avanzata

Perfeziona la tua ricerca

  • Libri (2)

a

Fascia di prezzo personalizzata (EUR)

a

  • Editore: Geological Society of America, 2021

    0813795494 / 9780813795492

    • Brossura

    Da: RiLaoghaire, Knoxville, TN, U.S.A.RiLaoghaire

    Venditore con 5 stelle
    Contatta il venditore

    Condizione: Usato - Buono

    EUR 4,54

    EUR 4,32 spedizione 
    Spedito in U.S.A.

    Quantità: 1 disponibile

    Soft cover. Condizione: Good. 128 numbered pages; light wear to corners and edges of cover; a couple minor creases to cover; minor rub to cover; a few minor dings to cover; weighs 14.3 ounces; measures 10.9 by 8.4 by .4 inches; 112025.

  • Editore: The Geological Society of America, Boulder, Colorado, 2021

    0813725496 / 9780813725499

    • Brossura

    Da: Joseph Burridge Books, Dagenham, Regno UnitoJoseph Burridge Books

    Venditore con 5 stelle
    Contatta il venditore

    Condizione: Nuovo

    EUR 60,08

    EUR 31,50 spedizione 
    Spedito da Regno Unito a U.S.A.

    Quantità: 1 disponibile

    Soft cover. Condizione: New. vi, 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.…