Digital-Desert : Mojave Desert Visit us on Facebook -- Desert Gazette -- Desert Link
Introduction:: Nature:: Map:: Points of Interest:: Roads & Trails:: People & History:: Ghosts & Gold:: Communities:: BLOG:: :?:: glossary

Joshua Tree National Park - Mojave Ecozone:
Geology Tour Road:

Stop #13

Pleasant Valley Dry Lake


Looking south across the playa

The upheaval of the Hexie Mountains with subsidence of the area north of the southern fault line, created a low area in which a periodic lake existed during a wetter climate. Sediments made of clays and sand were carried from nearby slopes and alluvial fans to be deposited at depths of several hundred feet. As time went on, and the lakebed rose, the slope extending from the canyons and alluvial deposits lessened. With this, finer silts and dissolved salts drying began to level the bottom of the valley creating what we see now as a dry lake, or playa. Although salt deposits here are not as obvious as in other desert dry lakes (where extremely few, or, no plants grow), evidence of the salt content can be seen in the presence of salt-tolerant plants species. Interestingly, after heavy rains, many dry lakes become temporary "wet" lakes.


Looking west across the playa

PREVIOUS - NEXT

GLOSSARY > alluvial fan, dry lake, fault, playa, sediments

Dry Lakes of the Mojave

In desert basins, where rivers merge but do not drain, a dry lake bed or playa may ...
Clickable map


Introduction:: Nature:: Map:: Points of Interest:: Roads & Trails:: People & History:: Ghosts & Gold:: Communities:: BLOG:: :?:: glossary
Country Life Realty
Wrightwood, Ca.
Mountain Hardware
Wrightwood, Ca.
Canyon Cartography
DesertLink
Links to Desert Museums

Grizzly Cafe
Family Dining


Custom Search

Abraxas Engineering
privacy
Copyright ©Walter Feller. All rights reserved.