After exploring Scotty’s Castle, Ubehebe Crater and some of Titus Canyon on our third day at Death Valley National Park we stopped at the Mesquite Sand Dunes on the way back to camp.
The sand is a product of erosion from the Cottonwood Mountains to the west and northwest and is made up of light colored grains of quartz and dark grains of magnetite.
The evenly spaced ripples forming perpendicular to the wind are made up of the larger grains that fall behind.
I don’t know who’s who. Do you?
There is evidence of creatures that venture onto the sand like the sidewinder rattlesnake, desert kangaroo rat, kit fox, lizards and beetles.
The day waned.
taken by Jeremy
This was Jeremy and my last night camping in Death Valley and we were rewarded by a full moon. The next day he started his long journey back to the Chicago area and I headed back to my winter home in Yarnell, Arizona
The sand is a product of erosion from the Cottonwood Mountains to the west and northwest and is made up of light colored grains of quartz and dark grains of magnetite.
The evenly spaced ripples forming perpendicular to the wind are made up of the larger grains that fall behind.
I don’t know who’s who. Do you?
There is evidence of creatures that venture onto the sand like the sidewinder rattlesnake, desert kangaroo rat, kit fox, lizards and beetles.
The day waned.
taken by Jeremy
This was Jeremy and my last night camping in Death Valley and we were rewarded by a full moon. The next day he started his long journey back to the Chicago area and I headed back to my winter home in Yarnell, Arizona