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The Configuration of the Rock Floor of Greater New York

Om The Configuration of the Rock Floor of Greater New York

This geology text offers a detailed study of the composition and structure of the bedrock underlying the city of New York and its environs. Hobbs' observations help explain the geologic processes that shaped the region and inform the engineering of its buildings and infrastructure. An essential resource for geologists, engineers, and anyone interested in the geology of the New York City area. 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 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. 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.

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  • Språk:
  • Engelska
  • ISBN:
  • 9781022527324
  • Format:
  • Häftad
  • Utgiven:
  • 18. juli 2023
  • Mått:
  • 156x234x25 mm.
  • Vikt:
  • 676 g.
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Leveranstid: 2-4 veckor
Förväntad leverans: 6. februari 2025

Beskrivning av The Configuration of the Rock Floor of Greater New York

This geology text offers a detailed study of the composition and structure of the bedrock underlying the city of New York and its environs. Hobbs' observations help explain the geologic processes that shaped the region and inform the engineering of its buildings and infrastructure. An essential resource for geologists, engineers, and anyone interested in the geology of the New York City area.
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 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.
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.

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