Death Valley National Park is a national park in the U.S. states of California and Nevada located east of the Sierra Nevada, occupying an interface zone between the arid Great Basin and Mojave deserts in the United States. The park protects the northwest corner of the Mojave Desert and contains a diverse desert environment of salt-flats, sand dunes, badlands, valleys, canyons, and mountains. It is the largest national park in the lower 48 states and has been declared an International Biosphere Reserve. Approximately 95% of the park is a designated wilderness area. It is the hottest and driest of the national parks in the United States.

The second-lowest point in the Western Hemisphere is in Badwater Basin, which is 282 feet (86 m) below sea level. The park is home to many species of plants and animals that have adapted to this harsh desert environment. Some examples include creosote bush, Bighorn Sheep, Coyote, and the Death Valley Pupfish, a survivor of much wetter times.

A series of Native American groups inhabited the area from as early as 7000 BC, most recently the Timbisha around 1000 AD who migrated between winter camps in the valleys and summer grounds in the mountains. A group of European-Americans that became stuck in the valley in 1849 while looking for a shortcut to the gold fields of California gave the valley its name, even though only one of their group died there. Several short-lived boom towns sprang up during the late 19th and early 20th centuries to mine gold and silver. The only long-term profitable ore to be mined was borax, which was transported out of the valley with twenty-mule teams. (Interesting visit to be done to the Furnace Creek museum.)

The valley later became the subject of books, radio programs, television series, and movies. Tourism blossomed in the 1920s, when resorts were built around Stovepipe Wells and Furnace Creek. Death Valley National Monument was declared in 1933 and the park was substantially expanded and became a national park in 1994.

The natural environment of the area has been shaped largely by its geology. The valley itself is actually a graben. The oldest rocks are extensively metamorphosed and at least 1.7 billion years old. Ancient, warm, shallow seas deposited marine sediments until rifting opened the Pacific Ocean. Additional sedimentation occurred until a subduction zone formed off the coast. This uplifted the region out of the sea and created a line of volcanoes. Later the crust started to pull apart, creating the current Basin and Range landform. Valleys filled with sediment and, during the wet times of glacial periods, with lakes, such as Lake Manly.

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GALLERY IN PROCESS... GALERIE EN CONSTRUCTION...

Between the 13th of May and the 3rd of June 2013 we spent 3 wonderful weeks in the west part of USA. It was our first trip in this part of USA, and each day was full of surprises, with countless breathtaking landscapes.
After 3 days in San Francisco, Sausalito, and on the north coast, we made a flight to Las Vegas, to began our long road trip (3.000 miles i.e. 4.800 km and more than 70 hours driving on the wonderful scenic roads from one park to another). We had the pleasure to discover the following sites :

- Grand Canyon National Park, (the south rim part only)
- the Colorado canyon at Lees Ferry, the Vermillion Cliffs on the road to Cliff Dwellers
- the area of the city of Page (with the visit of the 2 Antelope Canyons Navajo Tribal Parks, the Lake Powell, and Horseshoe Bend,
- Monument valley NP (with an afternoon spent in the Mystery Valley trails with a Navajo guide driving a Jeep Wrangler)
- Arches NP
- Canyonlands NP
- Bryce canyon NP
- Zion NP
- Death Valley NP
- Bodie State Historic Park
- Mono Lake
- Yosemite NP and Maropisa Grove NP near Wawona
- the Napa valley with a visit of the Newton winery (LVMH group)
- we did a balloon flight over the vineyards
- and we stayed 2 mores days in San Francisco before leaving this great city to go back to France.

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