On the Eastern border of California, and near the Western border of Nevada, is an area that is full of mystery, wilderness, and desert solitude. This area is Death Valley National Park. The name alone “Death Valley” transcends time and space, and for hundreds of years has been a beacon to prospectors, explorers, adventurers, and today, casual visitors. While Death Valley is, as its name suggests – a fundamentally hostile environment, with temperatures regularly soaring over 100 degrees from April through October, it is more than a flat wasteland. In reality, Death Valley is one of the most geologically diverse environments on the planet, where the remains of glacial Lake Manly are laid bare, and the effects of active volcanism and erosion are easily visible. Within the confines of Death Valley, one can find tall, uplifted mountains, year-round waterfalls, volcanic craters, sand dunes, eroded canyons, and the lowest spot in North America.
Badwater Basin
Of the fifty-nine National Parks in the United States, Death Valley is the most infamous, and the least well known. Most people assume that Death Valley is an inhospitable wasteland, with nothing of interest to see or do. However, outdoorspeople, geologists, and adventurers know that Death Valley is a location with interesting geologic features, mining history, tall mountains, sand dunes, volcanic activity, historic structures, and much more. Even if it did not have all of these things and more, Death Valley is a notable location to visit because of Badwater Basin.
Shorty's Mine
While most of the mines in the park have been sealed by the National Park Service for the public’s protection, some of the mines in the more remote areas of the park can be found and explored by intrepid visitors. Such exploration is not for the faint-hearted: as the above sign states, abandoned mines carry a plethora of hazards. If those physical dangers aren’t enough of a deterrent, the Panamint Range of the park is rumored to harbor a series of large underground caverns containing strange creatures and even stranger relics. If you are interested in exploring a Death Valley mines safely, or just seeing an open Death Valley mine, despite the above listed hazards, the easiest mine to see in the backcountry is Shorty’s Mine.
The Salt/Saline Pools of the Devil’s Golf Course
The Devil's Golf Course is an area of Death Valley that is close to Badwater. While it is not quite as far below sea level as Badwater, this is an area that is also below sea level. But like Badwater, it shares a common geologic past. Over twenty thousand years ago, the valley floor of Death Valley was not barren and desolate - but instead was covered with water - a large body of water known to geologists and historians as Lake Manly. Lake Manly was full of minerals from the surrounding terrain; and over the course of time, as it evaporated, it left those minerals - and sedimentary rocks behind. Today, what remains are salt crystals from the bottom of the lake - and borax crystal formations. These crystals have grown into an extensive – and hard network of structures. As you can see from the pictures above, the crystal formations have covered the area in a network of sharp formations that are between one to two feet high and are close together. As the area is difficult to traverse on foot, one can only imagine the difficulty one would have attempting to play any sort of golf game (hence the name). While the crystals are spectacular, where myth and fact meet are with the secret pools of water that remain interspersed among the formations.