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On The Tertiary Fluvio-marine Formation Of The Isle Of Wight

Bag om On The Tertiary Fluvio-marine Formation Of The Isle Of Wight

Edward Forbes's scientific article provides an in-depth analysis of the geological formations found on the Isle of Wight. From the flora and fauna to the geological strata, this article is a must-read for anyone interested in geology and the natural world. Forbes's attention to detail and scientific rigor make this article a valuable resource for scholars and experts in the field of geology. 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:
  • 9781019644928
  • Indbinding:
  • Hardback
  • Udgivet:
  • 18. juli 2023
  • Størrelse:
  • 156x234x13 mm.
  • Vægt:
  • 467 g.
Leveringstid: 2-3 uger
Forventet levering: 22. januar 2025
Forlænget returret til d. 31. januar 2025
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Beskrivelse af On The Tertiary Fluvio-marine Formation Of The Isle Of Wight

Edward Forbes's scientific article provides an in-depth analysis of the geological formations found on the Isle of Wight. From the flora and fauna to the geological strata, this article is a must-read for anyone interested in geology and the natural world. Forbes's attention to detail and scientific rigor make this article a valuable resource for scholars and experts in the field of geology.
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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