Canyon dune. Sand anchored on debris-flow fan, Paymaster Ridge, Great Basin Desert, NV
Slip face. Active dune overtakes its parent, Paymaster Ridge, Great Basin Desert, NV
Generations. Aeolian dune migration overtakes its sand source, Paymaster Ridge, Great Basin Desert, NV
Wind runs. Barchan forms in Clayton Valley, Paymaster Ridge, Great Basin Desert, NV
Siliciosity. Reflective tilted beds in the Paymaster Ridge, Great Basin Desert, NV
Please respect the natural and cultural resources of our public lands. #naturefirst #keepgoing
