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Geology of Amargosa Valley

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Geology of Amargosa Valley, Nevada

IN PHOTOS

The Amargosa Valley lies astride the California-Nevada border, just east of Death Valley. It begins in the vicinity of Beatty, Nevada and continues some 100 miles southward to Tecopa, California where it ends at the Sperry Hills. The Amargosa River, however, an ephemeral stream that drains the Amargosa valley, issues from wetlands at Ash Meadows some 50 miles south of Beatty, and then cuts through the Sperry Hills in Amargosa Canyon. From there, it flows to the north side of the Avawatz Mountains and then bends westward and northward to empty into Death Valley.

Southward views of Amargosa Valley in the vicinity of Eagle Mountain. Eagle Mountain lies just south of Ash Meadows, where the Amargosa River gets its start. Aerial view of Eagle Mountain, a tilted fault block, in the center of the Amargosa Valley. Here, the Amargosa River empties out of a large playa.

Mojave Desert, California (Pan)

Evaporite deposits in Amargosa Valley near Tecopa, CA (Image ID# 5566)
View southward over Eagle Mtn.

Tilted fault block, SE California.

Aerial view of Eagle Mountain, a tilted fault block, in the center of the Amargosa Valley. Here, the Amargosa River empties out of a large playa. (SrF-02)
Desert River. Amargosa River, SE California.

Desert River, Mojave Desert, California

The Amargosa River, frequently dry, carries water after a storm in the Amargosa Valley, California. (Dep-40)

Flooded playa, Mojave Desert, California

Flooded playa, Amargosa Valley, California. In the background lies the Resting Spring Range. Parts of the valley floor frequently becomes flooded during wet winters. The white hills in the middle ground are part of the Plio-Pleistocene Tecopa Lake Beds. (101230-44)
Paleozoic rock between the Cambrian Cararra and the Cambrian Bonanza King Formation.

Paleozoic Rock, Mojave Desert, CA

Paleozoic Rock of the Resting Spring Range as seen from the Amargosa Valley. The red-brown colored strata near the base of the photo belong to the Cambrian Cararra Formation while the overlying gray limestone belongs to the Cambrian Bonanza King Formation. (Image ID# 101218-38)
View of Tecopa Basin, the south end of the Amargosa Valley. From the top of Tecopa Peak, one gets a wonderful view of the south end of the Amargosa Valley. In the middleground lies Lake Tecopa, surrounded by Plio-Pliestocene lake bed deposits. The mountains in the background are the Resting Spring Range (closest) and the Nopah Range. Both consist of predominantly Cambrian rock that has been tilted and faulted during crustal extension.

Lake Tecopa, a playa in southern CA

Salt-covered playa of Lake Tecopa,Mojave Desert, California. (IMG_5517)
View of eroded lake beds of China Ranch. Just beyond the southern edge of the Amargosa Valley, the Amargosa River cuts a canyon through the Sperry Hills. Here lies China Ranch, an oasis that now hosts a date palm plantation. Surrounding China Ranch are the eroded badlands of the Miocene China Ranch Basin.

Badlands eroded into lakebeds, Mojave Desert, California

Badlands eroded into Miocene China Ranch Lakebeds, Mojave Desert, California (5D-9549)
View of eroded lake beds of China Ranch. Just beyond the southern edge of the Amargosa Valley, the Amargosa River cuts a canyon through the Sperry Hills. Here lies China Ranch, an oasis that now hosts a date palm plantation. Surrounding China Ranch are the eroded badlands of the Miocene China Ranch Basin.

Badlands, Mojave Desert, California

Badlands eroded into Miocene China Ranch Lakebeds, Mojave Desert, California (5D-9547)

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Geology of Death Valley, CaliforniaView southwestward over San Andreas fault to Pinnacles National Monument. The fault runs along the base of the hills in the middle ground. Pinnacles consist of 23.5 Ma felsic and intermediate volcanic rock; it is visible as the north tilted layers near the center of the photo. Similar rock is found in only one other place on the other side of the fault: 315 km to the south in the "Neenach Volcanic field".Geology of San Andreas Fault, California
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