Kip Evans Photography

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  • Mono Lake, Eastern Sierra California, eastern sierra, yosemite, tuffas, lake
    Mono Lake Tufas.jpg
  • Aerial view of Soda Lake, a shallow, ephemeral, alkali lake, in the Carrizo Plain in southeastern San Luis Obispo County, California. Internal drainage of the Carrizo Plain and the formation of Soda Lake began during Pliocene-Pleistocene time when tectonic deformation associated with the San Andreas Fault defeated a stream that once drained the valley. An originally fresh to brackish water lake probably persisted through much of the Pleistocene during which coastal California was wetter and cooler than now. Diminished Holocene precipitation and a higher evaporation rate led to shrinkage of the ancestral lake and associated increased salinity which set the stage for clay dune formation (wiki 2009)
    Soda Lake_3592.jpg
  • Rainbow over the Painted Desert - Arizona.
    Painted Desert.jpg
  • Grand Canyon National Park, north rim.
    Moon Over Spire Grand Canyon.jpg
  • Rocks in the desert. Death valley National Park
    DesertRocks1188.jpg
  • Mesa Verde Canyon - Arizona.
    Mesa Verde Canyon.jpg
  • Slot Canyon
    Slot Canyon (c)Kip Evans.jpg
  • Aerial view of Soda Lake, a shallow, ephemeral, alkali lake, in the Carrizo Plain in southeastern San Luis Obispo County, California.
    Soda Lake_3594.jpg
  • Aerial view of Soda Lake, a shallow, ephemeral, alkali lake, in the Carrizo Plain in southeastern San Luis Obispo County, California.
    Soda Lake_3593.jpg
  • Tufa is a calcium carbonate (CaCO3) deposit that forms by chemical precipitation from bodies of water with a high dissolved calcium content. Tufa is common in many parts of the world. There are some prominent towers of tufa at Mono Lake and Trona Pinnacles in California, USA, formed by precipitation from calcium-bearing spring water flowing into an alkaline lake (wiki 2009)
    Mono Lake Tuffas_MG_5503.jpg