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EARTH SCIENCE

18 images Created 20 Jul 2014

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  • Middle Eocene Silcrete Fossil Leaf (Malvaceae brachychiton) - South Australia
    0245 16 Sep 2012 .JPG
  • Geologist Andrew Ezzy observes sedimentary structures in Triassic Sandstone at Buckland, Tasmania, Australia
    9815 20 Jul 2014 .jpg
  • Iron Staining Lamination in Triassic Sandstone - Tasmania, Australia
    9774 20 Jul 2014 .jpg
  • Iron Staining Lamination in Triassic Sandstone - Tasmania, Australia
    9775 20 Jul 2014 .jpg
  • Iron Nodules in Triassic Sandstone - Tasmania, Australia
    9781 20 Jul 2014 .jpg
  • Iron Staining Lamination and Nodule Formation - Tasmania, Australia
    9788 20 Jul 2014 .jpg
  • Middle Eocene Silcrete Fossil Leaf - South Australia
    00095 16 Sep 2012 .JPG
  • Middle Eocene Silcrete Fossil Leaf - South Australia
    0107 15 Sep 2012 .JPG
  • Iron Staining Lamination in Triassic Sandstone - Tasmania, Australia
    9785 20 Jul 2014 .jpg
  • Tessellated Pavement - Tasmania
    anaspides-idw-9677-27-nov-2006.jpg
  • Sand Ripples - South Australia
    anaspides-idw-4909-10-sep-2007.jpg
  • Slate and Lichen - South Australia
    anaspides-idw-5112-14-sep-2007.jpg
  • Slate  - South Australia
    anaspides-idw-5119-14-sep-2007.jpg
  • Bicheno Blowhole, Bicheno - Tasmania
    anaspides-idw-3492-21-feb-2010-.jpg
  • Thrombolites are living fossils from the Archean Period that are partly responsible for the oxygen in the atmosphere.  These Thrombolites are roughly 2000 years old
    7263 09 Sep 2013 .jpg
  • Glacial tarns and lakes are common in the High Sierras and are formed during glacial and periglacial conditions.  Ice has tremendous power when under pressure and carves the underlying rock as glaciers move towards lower elevations.  Glacial lakes and alpine tarns can be formed at the upper edge of a glacier
    0833 07 Jul 2009.JPG
  • A glacial erratic lies along the edge of a an alpine tarn in the Cathedral Range in the High Sierras in Yosemite National Park.  Glacial erratics are large rocks that have been transported from their original place of origin by being entrained within glaciers
    1960 13 Jul 2009.JPG
  • Vogelsang High Camp located in the High Sierras in the Cathedral Range in Yosemite National Park.  A glacial erratic can be observed in the foreground.  Erratics are large boulders that have been moved and deposited away from their origin by glacial activity
    0970 08 Jul 2009.JPG
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ANASPIDES PHOTOGRAPHY Iain D. Williams

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