It's organic to live in places people to visit to find peace, a sense of wonder or return to time when vast tracks of our country was wilderness wild and free. This nostalgic isn't only for Americans but people all over the world. During the summer Europeans, Eastern Europe flock here to "experience" the heat of the desert and this vast landscape of 3.3 million acres. It is never what they expected. The Basin Range topography of this area is several stories of long ago oceans, constant fault activity of the Pacific Plate, the Furnace Creek Fault system located in the northern part of the park and the Southern Death Valley Fault system both move with a right-lateral offset along strike-slip faults; these types of faults rub past each other so that a theoretical observer standing on one side facing the other side sees it move right. Both fault systems run parallel to and at the base of the ranges.Much of the extra local stretching in Death Valley that is responsible for its lower depth and wider valley floor is caused by left lateral strike-slip movement along the Garlock Fault south of the park (the Garlock Fault separates the Sierra Nevada range from the Mojave Desert). This particular fault is pulling the Panamint Range westward, causing the Death Valley graben to slip downward along the Furnace Creek Fault system at the foot of the Black Mountains.[22] It is a lot to take in isn't it. This place is a geologist wonderland. However if you just like great sunsets and backcountry roads that lead to some great hiking trips and family campouts we have that too. Death Valley National Park is very much alive. Come on down or up and check us out.
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