Wildrose Wash Endangered Desert Legacy

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Wildrose Wash Endangered Desert Legacy Location: The Wildrose Wash area is located in the Mojave Desert, in Inyo County, about 25 miles north of the town of Trona. The area is located south of Death Valley National Park and east of the Argus Range Wilderness. It abuts or lies very near to the western edge of Surprise Canyon Wilderness. The southern portion of the area lies to the east of Trona Wildrose Road, while the northern portion lies to the north/northwest of Trona Wildrose Road. Management Agency: Bureau of Land Management, Ridgecrest Field Office Description: The Wildrose Wash area lies within the Panamint Valley, an expansive internally-drained closed basin that retains water and does not allow outflow to the ocean or other external bodies of water. Panamint Valley contains several ephemeral lakes that hold water after big rains. The beautiful, multicolored Argus Range can be seen to the west and the Panamint Range to the east. Wildlife and Plants: Species that make this area their home include the endangered Inyo California Towhee, and the protected desert bighorn sheep (photo above). Other species that make this area home include Townsend’s Big- eared bat, prairie falcon, Pallid bat, Panamint alligator lizard, Antioch multilid wasp, Pinyon rockcress, Panamint dudleya, Panamint Mountains lupine, Hoffmann’s buckwheat, Amargosa beardtongue, American badger, Death Valley round-leaved phacelia, Pinyon Mesa buckwheat, Mormon needle grass, Death Valley sandpaper-plant, and polished blazing-star. This area has ten distinct plant communities, including Mojave Riparian Forest and Mesquite Bosque. The rare Panamint Daisy can also be found in this area (photo above). Activities: Many people visit this area, including nature enthusiasts, equestrians, photographers, star-gazers, and hunters. Rockhounds visit nearby mines to collect onyx. In the spring, wildflower viewers flock to this area. Campers enjoy staying at nearby Wildrose Campground located within Death Valley National Park. Hikers, back packers and peak-baggers trek the nearby trails to Wildrose Peak and Telescope Peak, also within Death Valley National Park. Telescope Peak, with an elevation of 11,043 feet is the highest peak in Death Valley National Park. Off-roaders enjoy the nearby 28-mile Nadeau National Recreation Trail. Desert Renewable Energy Conservation Plan – California Wilderness Coalition Like us on facebook For more information contact: Linda Castro, 760.221.4895, [email protected] to get involved .

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Upper Neogene Stratigraphy and Tectonics of Death Valley — a Review
Earth-Science Reviews 73 (2005) 245–270 www.elsevier.com/locate/earscirev Upper Neogene stratigraphy and tectonics of Death Valley — a review J.R. Knott a,*, A.M. Sarna-Wojcicki b, M.N. Machette c, R.E. Klinger d aDepartment of Geological Sciences, California State University Fullerton, Fullerton, CA 92834, United States bU. S. Geological Survey, MS 975, 345 Middlefield Road, Menlo Park, CA 94025, United States cU. S. Geological Survey, MS 966, Box 25046, Denver, CO 80225-0046, United States dTechnical Service Center, U. S. Bureau of Reclamation, P. O. Box 25007, D-8530, Denver, CO 80225-0007, United States Abstract New tephrochronologic, soil-stratigraphic and radiometric-dating studies over the last 10 years have generated a robust numerical stratigraphy for Upper Neogene sedimentary deposits throughout Death Valley. Critical to this improved stratigraphy are correlated or radiometrically-dated tephra beds and tuffs that range in age from N3.58 Ma to b1.1 ka. These tephra beds and tuffs establish relations among the Upper Pliocene to Middle Pleistocene sedimentary deposits at Furnace Creek basin, Nova basin, Ubehebe–Lake Rogers basin, Copper Canyon, Artists Drive, Kit Fox Hills, and Confidence Hills. New geologic formations have been described in the Confidence Hills and at Mormon Point. This new geochronology also establishes maximum and minimum ages for Quaternary alluvial fans and Lake Manly deposits. Facies associated with the tephra beds show that ~3.3 Ma the Furnace Creek basin was a northwest–southeast-trending lake flanked by alluvial fans. This paleolake extended from the Furnace Creek to Ubehebe. Based on the new stratigraphy, the Death Valley fault system can be divided into four main fault zones: the dextral, Quaternary-age Northern Death Valley fault zone; the dextral, pre-Quaternary Furnace Creek fault zone; the oblique–normal Black Mountains fault zone; and the dextral Southern Death Valley fault zone.
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