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  • 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
  • The grandeur of the Cathedral Range in the High Sierras in Yosemite National Park can be appreciated when the sun, low to the horizon causes the mountains to be bathed in warm light.  A summer storm, common in the High Sierras, is forming in the background
    1991 13 Jul 2009.JPG
  • Marmots are quite common the high country and on a warm day can be seen basking on the granitic rocks that make up the basement rock of the High Sierras
    0812 07 Jul 2009.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
  • A stars and stripes lantern adorns a conifer tree in the High Sierras during 4th of July celebrations at Vogelsang High Camp in Yosemite National Park
    0935 07 Jul 2009.JPG
  • The tannin stained water of a glacial alpine tarn in the Cathedral Range in the High Sierras in Yosemite National Park
    1851 13 Jul 2009.JPG
  • Alpine cabbage grows in moist areas in the High Sierras along the Cathedral Range in Yosemite National Park
    1131 08 Jul 2009.JPG
  • The remains of an extensive snow and ice field in the High Sierras in Yosemite National Park.  Summer temperatures have all but melted the field leaving small areas of ice that have been eroded beneath by flowing water
    1098 08 Jul 2009.JPG
  • The sun is captured in a star burst photograph of a dead conifer tree in the High Sierras
    0910 07 Jul 2009.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 National Parks rescue helicopter lands in a clearing in the High Sierras in preparation to extract an injured rock climber
    0647 06 Jul 2009.JPG
  • A National Parks rescue helicopter lands in a clearing in the High Sierras in preparation to extract an injured rock climber
    0543 06 Jul 2009.JPG
  • A walker in the Cathedral Range in the High Sierras  admires wildflowers that have flowered in the wake of winter.  Wildflowers inhabit many of the scree slopes and edges of moist alpine tarns in Yosemite National Park
    1104 08 Jul 2009.JPG
  • Snow drifts and small ice fields are common in the High Sierras and often cover sections of hiking trails.  Care must be taken when crossing such drifts as they can be quite deep in places and the ice can be slippery
    0894 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
  • Snow drifts and small ice fields are common in the High Sierras and usually can be found in summer months in the lee of hills and boulders where the summer warmth is minimal.  A jet contrail can be seen in the sky
    1075 08 Jul 2009.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
  • Sunrise over Vogelsang Peak n the Cathedral Range in Yosemite National Park
    0996 08 Jul 2009.JPG
  • Sunrise over Vogelsang Peak in the Cathedral Range in Yosemite National Park
    1041 08 Jul 2009.JPG
  • Evening stars pin point the sky on a clear evening in the Cathedral Range in Yosemite National Park
    2044 13 Jul 2009.JPG
  • Yosemite National Park is a place of mountains that have been eroded by glaciers to appear as skeletons of their former selves
    2113 14 Jul 2009.JPG
  • Reflection of Vogelsang Peak at sunrise in a glacial tarn in Yosemite National Park
    1139 08 Jul 2009.JPG
  • Large cracks in the granite base rock indicate that internal geological forces are occurring.  The cracks are caused by the granite swelling (isotactic adjustment) as overburden and rock is removed by glacial action
    2119 14 Jul 2009.JPG
  • Young volunteer staff rangers ply their way along walking trails using hand tools to maintain the tracks in Yosemite National Park
    0466 06 Jul 2009.JPG
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ANASPIDES PHOTOGRAPHY Iain D. Williams

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