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By nature, ergs are very active. Smaller dunes form and migrate along the flanks of the larger dunes and sand ridges. Occasional precipitation fills basins formed by the dunes; as the water evaporates, salt deposits are left behind. Individual dunes in ergs typically have widths, lengths, or both dimensions greater than 500 m (1,600 ft). [2]
Monahans Sandhills State Park near Odessa, Texas. Beaver Dunes State Park near Beaver, Oklahoma. The Killpecker sand dunes of the Red Desert in southwestern Wyoming. Jockey's Ridge State Park – on the Outer Banks, North Carolina. The Great Dune found in Cape Henlopen State Park in Lewes, Delaware.
As barchan dunes migrate, smaller dunes outpace larger dunes, catching-up the rear of the larger dune and eventually appear to punch through the large dune to appear on the other side. The process appears superficially similar to waves of light, sound, or water that pass directly through each other, but the detailed mechanism is very different.
Steamboat Mountain, overlooking the Killpecker Sand Dunes, provides habitat for desert elk. The Killpecker Sand Dunes stretch 55 miles (89 km) east from the Green River Basin across the Continental Divide into the Great Divide Basin and encompass approximately 109,000 acres (440 km 2). [5] These living dunes, one of North America's largest ...
The Santa Anas are katabatic winds (Greek for "flowing downhill") arising in higher altitudes and blowing down towards sea level. [7] The National Weather Service defines Santa Ana winds as "a weather condition [in southern California] in which strong, hot, dust-bearing winds descend to the Pacific Coast around Los Angeles from inland desert regions".
Make like a nomad on a caravan camping trip in the vast Erg Chigaga desert of southern Morocco.. Several outfitters offer multi-day camel-trekking trips that feature tent camping among the dunes ...
Monahans Sandhills State Park is noted for the presence of sand dunes up to 70 feet (21 m) high. Although desert-like, the Monahans Sandhills are not a desert; they are a part of a semi-arid ecosystem (average annual rainfall 12.3 inches (310 mm)) characterized by the presence of both groundwater and relatively nutrient-poor windblown sand.
Giant current ripples (GCRs), also known as giant gravel bars or giant gravel dunes, [1] are a form of subaqueous dune. They are active channel topographic forms up to 20 m high, which occur within near- thalweg areas of the main outflow routes created by glacial lake outburst floods . [ 2 ]