Water rushes through a narrow crack, in the red sandstone of Zion National Park, with fallen autumn leaves.
Location: Zion National Park, Utah
Image ID: 26100
Water rushes through a narrow crack, in the red sandstone of Zion National Park, with fallen autumn leaves.
Location: Zion National Park, Utah
Image ID: 26138
Water rushes through a narrow crack, in the red sandstone of Zion National Park, with fallen autumn leaves.
Location: Zion National Park, Utah
Image ID: 26113
Water rushes through a narrow crack, in the red sandstone of Zion National Park, with fallen autumn leaves.
Location: Zion National Park, Utah
Image ID: 26137
Water rushes through a narrow crack, in the red sandstone of Zion National Park, with fallen autumn leaves.
Location: Zion National Park, Utah
Image ID: 26143
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25654
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25741
Brain rocks. Sandstone is curiously eroded through the forces water and wind acting over eons. Cracks and joints arise when water freezes and expands repeatedly, braking apart the soft sandstone.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20747
Water rushes through a narrow crack, in the red sandstone of Zion National Park, with fallen autumn leaves.
Location: Zion National Park, Utah
Image ID: 26396
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25671
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25738
Sandstone joints. These cracks and joints are formed in the sandstone by water that seeps into spaces and is then frozen at night, expanding and cracking the sandstone into geometric forms.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20748
Brain rocks. Sandstone is curiously eroded through the forces water and wind acting over eons. Cracks and joints arise when water freezes and expands repeatedly, braking apart the soft sandstone.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20750
Brain rocks. Sandstone is curiously eroded through the forces water and wind acting over eons. Cracks and joints arise when water freezes and expands repeatedly, braking apart the soft sandstone.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20754
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25655
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25672
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25740
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25742
A glacier fractures and cracks, as the leading of a glacier fractures and cracks as it reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25743
A glacier fractures and cracks, as the leading edge reaches the ocean. The pieces will float away to become icebergs.
Location: Neko Harbor, Antarctic Peninsula, Antarctica
Image ID: 25739
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