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The Faults In The Triassic Formation Near Meriden, Connecticut - William Morris Davis - Bog

Bag om The Faults In The Triassic Formation Near Meriden, Connecticut

This detailed geological study of the Triassic rocks of Connecticut is a groundbreaking work that established William Morris Davis as one of the founders of modern geology. Filled with precise observations, meticulous drawings, and insightful analysis, The Faults in the Triassic Formation Near Meriden, Connecticut is an important contribution to the scientific literature of the late 19th century. 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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  • Sprog:
  • Engelsk
  • ISBN:
  • 9781022340787
  • Indbinding:
  • Paperback
  • Udgivet:
  • 18. Juli 2023
  • Størrelse:
  • 156x234x3 mm.
  • Vægt:
  • 77 g.
Leveringstid: 2-3 uger
Forventet levering: 28. Maj 2024

Beskrivelse af The Faults In The Triassic Formation Near Meriden, Connecticut

This detailed geological study of the Triassic rocks of Connecticut is a groundbreaking work that established William Morris Davis as one of the founders of modern geology. Filled with precise observations, meticulous drawings, and insightful analysis, The Faults in the Triassic Formation Near Meriden, Connecticut is an important contribution to the scientific literature of the late 19th century.
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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