Information AboutKelso Dunes |
| CATEGORIES ABOUT KELSO DUNES | |
| landforms of california | |
| mojave desert | |
| protected areas of the mojave desert | |
| san bernardino county, california | |
| dunes | |
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Kelso Dunes, also known as the '''Kelso Dune Field''', is the largest field of Eolian Sand deposits in the Mojave Desert . The region is protected by the Mojave National Preserve and is located near the town of Baker , San Bernardino County , California . The dune field covers 115 square kilometers (45 square miles) and includes migrating dunes, vegetation-stabilized dunes, sand sheets, and sand ramps. The tallest dunes rise up to 200 meters (656 feet) above the surrounding terrain. The dunes are composed predominantly of light-colored Quartz and Feldspar , most likely Eroded from the Granitics of the San Bernardino Mountains to the south. Magnetite and Amphibole can also be found, often accumulating at the dune crests. Kelso Dunes represent part of a much larger sand transport system, which includes the nearby Devil's Playground region. The composition and morphology of the sand grains indicate that most originated from the Mojave River sink near Afton Canyon , which lies to the west of the dunes' current location. The sand has accumulated at the southeastern end of the Soda Lake-Kelso basin, where the Granite Mountains and Providence Mountains form a barrier to prevailing winds. At present, only the area around the Mojave River sink and the westernmost parts of Devil's Playground are receiving new sand through this system; sand is no longer accumulating at Kelso Dunes itself. The Kelso Dunes are composed of five stacked sets of dunes, each set corresponding to a period of climate change over the last 25,000 years. During dry climate episodes, a decrease in stabilizing vegetation exposed surface sand to wind Erosion , which ultimately brought the sand to the dunes. (Most of the eastern part of the Kelso dunes was formed when nearby Soda Lake and Silver Lake dried into their current Playa s.) However, once the sand was emplaced, vegetation began to grow, locking much of it into place. The Kelso Dunes are also notable for the phenomenon known as Singing Sand , or "booming dunes". Enthusiasts typically climb to the top of the dunes and slide down slowly, generating a low-frequency rumble that can be both felt and heard. This effect has also been noted at the Eureka Dunes in California, Sand Mountain in Nevada , and the Booming Dunes in the Namib Desert , Africa . Endemic to the Kelso dunes are seven species of Insect , including the Kelso Dunes Giant Sand Treader (''Macrobaenetes kelsoensis'', a species of camel Cricket ), the Kelso Dunes Jerusalem Cricket (''Ammopelmatus kelsoensis''), and the Kelso Dunes Shieldback Katydid (''Eremopedes kelsoensi''). Although not endemic, several plant and Reptile species are rare outside of these dunes. One example is the Mojave Fringe-toed Lizard (''Uma scoparia''), which is specialized in its ability to "swim" under sand. Kelso Dunes are closed to off-road vehicles, but are open to hikers. The trailhead is at the end of a three mile graded dirt road splitting from Kelbaker Road. This road can be accessed from both Interstate 15 (at Baker) and Interstate 40 (east of Barstow ). The dunes themselves lay just north of the Kelso Ghost Town . |
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