File:The Quarterly journal of the Geological Society of London (1904) (14781876091).jpg

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Identifier: quarterlyjourna601904geol (find matches)
Title: The Quarterly journal of the Geological Society of London
Year: 1845 (1840s)
Authors: Geological Society of London
Subjects: Geology
Publisher: London (etc.)
Contributing Library: Smithsonian Institution Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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dM ■ Fig. I.-View of Mount Owen, the Linda Valley, and the Gormanston Moraine, from the Razorback
Text Appearing After Image:
Fig. 2.—View of Mount Owen, the Gormanston Gap, and the pi aned surface of the Gormanston Moraine, from the hill beside the Mount-Lyell Mine Offices Vol. 60.) GLACIAL GEOLOGY OF TASMANIA. 53 EXPLANATION OF PLATES VII & VIII. Plate VII. Sketch-map of the glaciated area around Mount Lyell, including the Gorman-ston Moraine in the Linda Valley, on the scale of If miles to the inch. Plate VIII. Fig. 1. View of Mount Owen, the Linda Valley, and the Gormanston Moraine,from the Eazorback : showing the glaciated aspect of the lowernorthern slopes of Mount Owen.2. View of Mount Owen, the Gormanston Gap, and the planed surface ofthe Gormanston Moraine, from the hill beside the Mount-Lvell MineOffices. Discussion. Dr. \V. T. Blanfoed called attention to the fact that the Authorsclear account of the Pleistocene glacial evidence in the Tasmanianlowlands was an important addition to our knowledge of therecords left by the Glacial Period in the Southern Hemisphere ;for instance, in New Zealand

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