Kip Evans Photography

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  • Carrizo Grassland
    Carrizo Grassland-Kip-2379.jpg
  • Pronghorn Antelope (Antilocapra americana), Carrizo Plain, California
    Pronghorn Antelope-Kip-2491.jpg
  • A herd of Tule Elk, Carrizo Plain California
    Tule Elk-Kip-2374.jpg
  • Antelope Ground Squirrel, Carrizo Plain, CA.
    Antelope Ground Squirrel-Kip-2381.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
  • 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
  • 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 the San Andreas Fault in the Carrizo Plain. The San Andreas Fault is a continental transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate (wiki 2009)
    San Andreas Fault_3591.jpg
  • Aerial view of the San Andreas Fault in the Carrizo Plain. The San Andreas Fault is a continental transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate (wiki 2009)
    San Andreas Fault_3589.jpg
  • Aerial view of the San Andreas Fault in the Carrizo Plain. The San Andreas Fault is a continental transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate (wiki 2009)
    San Andreas Fault_3590.jpg
  • Aerial view of the San Andreas Fault in the Carrizo Plain. The San Andreas Fault is a continental transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate (wiki 2009)
    San Andreas Fault_3587.jpg
  • Aerial view of the San Andreas Fault in the Carrizo Plain. The San Andreas Fault is a continental transform fault that runs a length of roughly 800 miles (1,300 km) through California in the United States. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate (wiki 2009)
    San Andreas Fault_3588.jpg
  • Pronghorns live primarily in grasslands but also in brushland and deserts. They eat a wide variety of plant foods, often including plants that are unpalatable or toxic to domestic livestock.
    Pronghorn antelope_O2R1242.jpg
  • A male Tarantula  Aphonopelma sp.
    Tarantula_O2R1439.jpg