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  • af Frederick Richard Cowper Reed
    178,95 - 323,95 kr.

  • af Frederick Richard Cowper Reed
    294,95 kr.

    This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work was reproduced from the original artifact, and remains as true to the original work as possible. Therefore, you will see the original copyright references, library stamps (as most of these works have been housed in our most important libraries around the world), and other notations in the work.This work is in the public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work.As a reproduction of a historical artifact, this work may contain missing or blurred pages, poor pictures, errant marks, etc. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.

  • af Frederick Richard Cowper Reed
    341,95 kr.

  • af Frederick Richard Cowper Reed
    451,95 kr.

    Beneath Cambridgeshire's towns, villages, farmland, hills, fens and waterways lie the rocks that display a variety of geological landscapes. Basement rocks are buried under sandy deposits from ancient tropical seas. The rising and tilting of the land due to large-scale movements permitted water flows that produced gradual alterations. Glaciation, erosion and dramatic variations in climate all wrought more rapid changes. The consequences of these processes are revealed in this scholarly 1897 account of the geology of Cambridgeshire, which integrated the latest research then available. Proceeding from the most ancient to the most recent beds, systematic consideration is given to the features, distribution and modes of formation, as well as the economic implications of the various strata. Discussions of palaeontology, including detailed lists of site-specific fossils, and of water supply are also provided. An appendix, lists, maps, memoirs and other publications of H.M. Geological Survey from 1814 to 1897 are included.

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