History of Death Valley National Park

 Landscape

Death Valley National Park is the lowest point in North America and one of the hottest places in the world. It is also a vast geological museum, containing examples of most of the earth's geological eras. Death Valley National Park includes all of Death Valley, a 130-mile-long north/south-trending trough that formed between two major block-faulted mountain ranges: the Amargosa Range on the east and the Panamint Range on the west. Telescope Peak, the highest peak in the Park and in the Panamint Mountains, rises 11,049 feet above sea level and lies only 15 miles from the lowest point in the United States in the Bad water Basin salt pan, 282 feet below sea level. The California Desert Protection Act added most of the Saline, Eureka, northern Panamint, and Green water valleys to the Park.

Flora and fauna

Animal life is varied, and numerous species of reptiles, birds and mammals populate Death Valley, adapting well to the desert environment. However, many of these animals have a nocturnal lifestyle in order to escape the searing climate and can be difficult to spot.

The largest native mammal in the area, and perhaps the best studied member of the fauna, is the desert bighorn sheep. Small herds of sheep are most commonly found in the mountains surrounding Death Valley but at least occasionally visit the valley floor. Look for these animals near the springs and seeps that can be found throughout the park.

Over 350 species of birds are now known to inhabit or visit the area. And