A Preliminary Report on the Geology of the Eastern Desert of Egypt Between Latitude 22 N. and 25 N. Volume 1
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A Preliminary Report on the Geology of the Eastern Desert of Egypt Between Latitude 22 N. and 25 N. Volume 1

A Preliminary Report on the Geology of the Eastern Desert of Egypt Between Latitude 22 N. and 25 N. Volume 1


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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. 1907 Excerpt: ...schists forming a harder well marked band. At the next bend to the north coarse hornblende-gneisses come in strongly, also having an apparent southward dip of 60, these being in their turn followed by a lighter micaceous variety much resembling a typical biotite-granite, except for the foliation. Dark bands are also occasionally present, and quartz veins are conspicuous, the latter sometimes having distinct copper staining. These types form the whole of the low country south of Wadi Hafafit, and are remarkably veined by pegmatite dykes, having a NE--SW trend. Speaking generallv, the country south of the Wadi Abu Had and Hafafit junction is biotite-gneixs, and to the north is a very dark closegrained variety penetrated by an immense number of pegmatite dykes which seam the rocks in all directions, smaller veins branching from them along the foliation planes. The red range north of Hafafit again differs, the rock composing it being a red i/neiss, having strong affinities to a pegmatite. At the mouth of Wadi Nugrus a change takes place, the mica-and talc-schists of Sikait lying to the east, and the true gneiss of Wadi Gemal to the west. Gneiss forms the prominent mountain range of Gebel Migif and probably also the main portion of the long straight range of Gebel Hafafit. Similar rocks have also been observed on the southern, and to a less extent on the northern side of Khrug. The gneiss was subsequently traced down Wadi Gemal, where it assumes a hornblendic character and becomes almost a diorite-gneiss, while to the SE., in Wadi Um Sueh it became associated with an acid variety whose characters suggest a granitic and intrusive origin. It, in fact, generally presents this duplicate dioritic and granitoid character. It was finally seen in its typical character n...


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Product Details
  • ISBN-13: 9781130215373
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 28
  • Spine Width: 2 mm
  • Width: 189 mm
  • ISBN-10: 1130215377
  • Publisher Date: 01 Mar 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 68 gr


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A Preliminary Report on the Geology of the Eastern Desert of Egypt Between Latitude 22 N. and 25 N. Volume 1
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