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  • Racing Stream, British Columbia - Canada
    anaspides-idw-4419-16-sep-2008.jpg
  • Boulder or rock streams are produced during geological periods of frost and thaw
    3130a 13 Jan 2011.JPG
  • Many streams begin their passage to the ocean from the High Sierras as this one located near Vogelsang Peak in the Cathedral Range in Yosemite National Park
    0724 07 Jul 2009.JPG
  • Meandering Stream, British Columbia - Canada
    anaspides-idw-1085-17-sep-2008.jpg
  • Racing Stream, Liffey Forest Reserve - Tasmania
    anaspides-idw-8941-30-sep-2007.jpg
  • Sunrise.  Indian paint bush grows along a high mountain stream adjacent to Vogelsang Peak in the Cathedral Range of Yosemite National Park in the High Sierras
    0946 07 Jul 2009.JPG
  • Salmon Swimming River To Spawn, Canada
    anaspides-idw-4526-17-sep-2008.jpg
  • Salmon Swimming River To Spawn, Canada
    anaspides-idw-4508-17-sep-2008.jpg
  • anaspides-idw-4990-27-aug-2008.jpg
  • Brown Bear (Ursus arctos), Katmai - Alaska
    anaspides-idw-2555-30-aug-2008.jpg
  • Brown Bear (Ursus arctos), Katmai - Alaska
    anaspides-idw-2309-29-aug-2008.jpg
  • Sunrise, British Columbia - Canada
    anaspides-idw-1083-17-sep-2008.jpg
  • Temperate Rainforest, British Columbia - Canada
    anaspides-idw-0952-14-sep-2008.jpg
  • Forest Cascade - Tasmania
    anaspides-idw-0893-14-may-2006.jpg
  • Prograding Dolerite Spires, Mount Wellington - Tasmania..Physical, chemical erosion and periglacial freeze and thaw cause boulders to move downslope.  As the boulders move they lift up as they reach the edge a slope.  Often this process causes mountain boulder streams.
    anaspides-idw-0100-28-nov-2005.jpg
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ANASPIDES PHOTOGRAPHY Iain D. Williams

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