Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12520
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12521
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12522
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12523
Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12524
Checkerboard Mesa, a good example of crossbedding (horizontal lines) and vertical cracks caused by thermal expansion/contraction. Navajo sandstone forms the cliffs and walls of Zion National Park. The sandstone reaches a thickness of 2300 feet and consists of ancient cemented desert sand dunes. Horizontal lines, commonly called crossbedding, represent layers of wind-blown sand that built up into sand dunes. These dunes were then buried, and the sand grains glued together by calcite and iron oxide to form sandstone.
Location: Zion National Park, Utah
Image ID: 12526
Ripples in sand dunes at sunset, California. Winds reshape the dunes each day. Early morning walks among the dunes can yield a look at sidewinder and kangaroo rats tracks the nocturnal desert animals leave behind.
Location: Stovepipe Wells, Death Valley National Park, California
Image ID: 15604
Ripples in sand dunes at sunset, California. Winds reshape the dunes each day. Early morning walks among the dunes can yield a look at sidewinder and kangaroo rats tracks the nocturnal desert animals leave behind.
Location: Stovepipe Wells, Death Valley National Park, California
Image ID: 15605
Ripples in sand dunes at sunset, California. Winds reshape the dunes each day. Early morning walks among the dunes can yield a look at sidewinder and kangaroo rats tracks the nocturnal desert animals leave behind.
Location: Stovepipe Wells, Death Valley National Park, California
Image ID: 15607
Ripples in sand dunes at sunset, California. Winds reshape the dunes each day. Early morning walks among the dunes can yield a look at sidewinder and kangaroo rats tracks the nocturnal desert animals leave behind.
Location: Stovepipe Wells, Death Valley National Park, California
Image ID: 15630
Ripples in sand dunes at sunset, California. Winds reshape the dunes each day. Early morning walks among the dunes can yield a look at sidewinder and kangaroo rats tracks the nocturnal desert animals leave behind.
Location: Stovepipe Wells, Death Valley National Park, California
Image ID: 15631