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Panoramic view from Panorama Point, Badlands National Park, about an hour before sunset.
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Castle Rock is an erosional remnant of Upper Cretaceous Niobrara Formation (Smoky Hill member) chalk, located in southeastern Gove County, Kansas. The chalk badlands at this locality owe their preservation to a caprock of Ogallala Formation conglomerates, visible atop the cliff at left and in boulders on the slope.
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The "Snake" shot.
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Two small normal faults are visible in these erosional remnants of the Cretaceous Smoky Hill Chalk in southeastern Gove County, Kansas.
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This panorama offers a fantastic view of the typical Badlands landscape. You can find numerous erosion features, paleosols, evidence for ecological edge effects and explore the White River Group.
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Castle Rock badlands from atop the Smoky Hill Chalk.
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A view of the erosional features of the White River Badlands in eastern Badlands National Park, near Interior, South Dakota. There's a remarkably high contrast between the shadows and the sunlight, but I did my best with the exposure.
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The view from the parking lot near the east entrance to Badlands National Park.
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This 360 degree sunset pano is from a lookout at the Park's entrance. The dinosaur fossils for which the Park is named are exposed as soil erodes from these cliffs. Tens of millions of years underground and they show up now; what are the odds? Presumably, if one examines the cliffs in this pano one might find a newly ...
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