Death Valley - Geologie Des Death Valley, Death-Valley-Nationalpark, Koso, Death Valley Junction, Wandernde Felsen, Badwater, Telescope Peak (English, German, Paperback)

Kapitel: Geologie Des Death Valley, Death-Valley-Nationalpark, Koso, Death Valley Junction, Wandernde Felsen, Badwater, Telescope Peak, Amargosa, Christian Brevoort Zabriskie, Lake Manly, Zabriskie Point, Devil's Hole, Ubehebe Crater. Aus Wikipedia. Nicht dargestellt. Auszug: Zabriskie Point is a part of Amargosa Range located in east of Death Valley in Death Valley National Park in the United States noted for its erosional landscape. It is composed of sediments from Furnace Creek Lake, which dried up 5 million years ago - long before Death Valley came into existence. Panoramic view from Zabriskie Point, looking back over Furnace Creek; Death Valley, California Portrait of Christian Brevoort Zabriskie, on an interpretive sign at the Zabriskie Point site in Death Valley National ParkThe location was named after Christian Brevoort Zabriskie, vice-president and general manager of the Pacific Coast Borax Company in the early 20th century. The company's famous, iconic twenty-mule teams were used to transport borax from its mining operations in Death Valley. Eroded badlands at Zabriskie Point Badland formations at Zabriskie PointMillions of years prior to the actual sinking and widening of Death Valley and the existence of Lake Manly (see Geology of the Death Valley area), another lake covered a large portion of Death Valley including the area around Zabriskie Point. This ancient lake began forming approximately nine million years ago. During several million years of the lake's existence, sediments were collecting at the bottom in the form of saline muds, gravels from nearby mountains, and ashfalls from the then-active Black Mountain volcanic field. These sediments combined to form what we today call the Furnace Creek Formation. The climate along Furnace Creek Lake was dry, but not nearly as dry as in the present. Camels, mastodons, horses, carnivores, and birds left tracks in the lakeshore muds, along with fossilized grass and re...http: //booksllc.net/?l=de