The Devil’s Golf Course in Death Valley… An Interlude

The sun beats down on the Devil’s Golf Course in Death Valley.

Only the Devil could play golf here.” 1934 National Park guide book.

Peggy and I are playing hooky, extending our seemingly endless time away from home. One would think that backpacking the PCT, visiting Puerto Vallarta, and spending over a month with our kids in Florida and North Carolina would satisfy our wandering needs for a while. But no, here we are in Las Vegas, or Lost Wages, as I like to call it, ensconced in a comfortable suite at the very southern tip of Las Vegas Boulevard, the infamous Strip. Or is that famous?

Few people who visit this city venture outside of its mecca of gambling and entertainment pleasure palaces. Peggy and I always do. There is much to see and do. There is a desert on its doorstep, and it is a desert of rare beauty. Death Valley National Park is a prime example. It is a mere two hours away and Peggy and I drove out there on Sunday. To us, it’s like seeing an old friend; we have been there many times.

It is a geologist’s dream— there are rocks everywhere, and the rocks all have stories to tell. It’s a story of ancient seas and lakes and volcanic activities and clashing, mountain-building plates. Death Valley is a rift valley, or a graben in technical terms, formed along a fault zone between two mountain ranges. As the mountains were thrust up by tectonic forces, the valley dropped between them, several thousand feet. The two mountain ranges have since filled the valley up with eroded debris.

The shallow Lake Manly filled the basin a few thousand years ago. As the climate of the area changed and became more desert like, the lake dried up. Its briny waters left a deep deposit of salt behind, which brings us to today’s post. The Devil’s Golf Course is located a short 10 miles away from Bad Water Basin, which, at 282 feet below sea level, is the lowest point on the North American continent. Water that drains into the Basin melts the salt and becomes undrinkable, thus the name. The Devil’s Golf Course is several feet higher and avoids the melting water. Instead, capillary action pulls salty subsurface water up creating the crystalline structures that the area is famous for.

Peggy and I caught the area at a particularly good time for photography, which surprised me, given the location of the overhead sun. Anyway, here are the results.

This close up provides a view of the crystalline structures developed by the capillary action. BTW, they are composed of 95% table salt. (Photo by Peggy Mekemson.)
I took this photo looking east toward the Amargosa Range.
Looking southwest along the Panamint Range.
Peggy photographing the Devil’s Golf Course provides a perspective on the size of the crystalline structures.
A final shot of the Devil’s Golf Course backed up by the Panamint Range. (Photo by Peggy Mekemson.)

NEXT POST: A ghostly reminder of Death Valley’s past, and more.