Bulletin of the Museum of Comparative Zoology (Volume 28)
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Bulletin of the Museum of Comparative Zoology (Volume 28)

Bulletin of the Museum of Comparative Zoology (Volume 28)


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1898. Excerpt: ... the low base level swamps which indent the valleys of the Eio Grande aud border the coast of Panama, the residual clays present the same laminated structure. The laminated red clays can be continuously traced from Culebra as far north as Gorgona, everywhere overlying the massive igneous rocks and some of the igneous boulder formations, and I am inclined to think that some of them, with the exception of the swamp levels, are the residuum of the Tertiary sediments. PART III. The Pacific Coast from Panama to Punta Arenas, Costa Rica. Leaving the island of Naos in the Bay of Panama at night, we reached Cape Mala, the outer point of the Gulf, the next morning. After turning the point of the cape, we sail close alongside the straight shore line between Cape Mala and Mariato Point. Here the Pacific breaks abruptly against what is perhaps the widest portion of the Isthmian mainland. The accompanying sketches (Figs. 17-21) will convey an idea of the general topography of this region. From the steamer's deck nearly all the details of the coast topography can be seen. The interior consists of an east and west line of high conical summits rising to a height of at least 2,000 feet, between which and the coast were successively lower hills. The higher summits are more elevated in general than along the line of the Panama Railway section, but they present the same type of configuration. At the water's edge the coast shows in many places low vertical bluffs from 20 to 100 feet, which are being attacked by the washing of the waves. Sailing parallel to these bluffs and within a half mile of them we could make out the same familiar red clay so universal in the Isthmian region. Sometimes there were beds which were apparently stratified and not of igneous origin. Again the ma...


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Product Details
  • ISBN-13: 9781235678677
  • Publisher: General Books
  • Publisher Imprint: General Books
  • Height: 246 mm
  • No of Pages: 112
  • Spine Width: 6 mm
  • Width: 189 mm
  • ISBN-10: 1235678679
  • Publisher Date: 01 Feb 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 213 gr


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