Home Archived Aug 4, 2016
(i)

Geology of the National Parks - Death Valley

 

Death Valley geology field trip

Death Valley field trip button

Devil's Golf Course

View of Devil's Golf Course
The lumpy salts you see here are the residue of Death Valley's last significant lake, which had evaporated by 2000 years ago. Photo by Marli Miller

Mineral music

It's an early summer morning. The temperature is rising fast. The air is completely still and the quiet is profound. But, listen carefully and you'll hear a sounds like tiny pops and pings. Bend your ear to the ground and the sound grows louder. The musical sound of literally billions of tiny salt crystals bursting apart as they expand and contract in the heat provides the backdrop for this salty story.

Lakeside property

Not long ago, about 2000-4000 years ago during the Holocene, the climate was quite a bit wetter than today. It was so wet that water gradually filled Death Valley to a depth of almost 30 feet. The ancient peoples of Death Valley must have enjoyed centuries of abundant food in their lakeside homes.
Salt pinnacle close-up Jagged salt pinnacles. Photo from NPS archives.

The desert returns

These good times didn't last, however. The climate warmed, rainfall declined, and the shallow lakes began to dry up. Minerals dissolved in the lake became increasingly concentrated as water evaporated. Eventually, only a briny soup remained, forming salty pools on the lowest parts of Death Valley's floor. Salts (95% table salt - NaCl) began to crystallize, coating the muddy lakebed with a three to five feet thick crust of salt.
Salt pinnacle close-up
Close-up of delicate lacework edges decorating salt pinnacles. Photo by Ray Nordeen, NPS.

Pinnacles

While the saltpan at Badwater periodically floods, then dries, Devil's Golf Course lies in a part of the Death Valley salt pan that is several feet above flood level. Without the smoothing effects of flood waters, the silty salt at Devil's Golf Course grows into fantastic, intricately detailed pinnacles. The pinnacles form when salty water rises up from underlying muds. Capillary action draws the water upward where it quickly evaporates, leaving a salty residue behind. The pinnacles grow very slowly, perhaps as little as an inch in 35 years. Wind and rain continually work to erode and sculpt the salty spires into an amazing array of shapes.
Devil's Golf Course in time
geologic time scale
Dig deeper... On to next stop If you're going... Split Cinder Cone image gallery
| Death Valley Geology Home | | Virtual Field Trip | | Geologic History |
| Image gallery | | Geologist's page | | Death Valley National Park

Accessibility FOIA Privacy Policies and Notices

Take Pride in America logo USA.gov logo U.S. Department of the Interior | U.S. Geological Survey
URL: http://geomaps.wr.usgs.gov/parks/deva/ftdev1.html
Page Contact Information: G & G Webmasters
Page Last Modified: 01-Mar-2016@10:08