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A more detailed version of a panorama that I posted yesterday, this one previously failed to properly stitch, but seems to be okay this time.
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Another rangefront panorama...
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When I framed this GigaPan the clouds formed a nice large halo directly centered on Muleshoe Mound. Unfortunately by the time the robot got over to the clouds they had drifted a bit. It's not often I can complain about having too much blue sky. :-P
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Climbers arise and prepare to break camp at the Devils Tower National Monument Campground.
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Three large slabs of sandstone displaying remarkably well preserved interference ripple marks.
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The Lower Mississippian Muleshoe Mound is one of the best studied Waulsortian mounds, a type of bioherm or reef composed largely of lime mud and all sorts of Late Paleozoic critters (crinoids, brachiopods, etc. but not coral).
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- Loess by Ron Schott
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Loess is a wind-blown sediment that is predominantly in the clay size range. It makes for very fertile soils and there's a significant portion of western Kansas that has a fairly thick mantling of it. During the Dust Bowl Era this was the Dust.
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From the Devil Canyon overlook, looking north along the main channel of Bighorn Canyon. If I remember the stratigraphy correctly, the top layer of the canyon is formed from the Madison Limestone, which is over 350 million years ago - same age and similar in appearance to the Redwall Limestone that makes up part of t...
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That's the name given to this particular overlook along Rte. 12 in southern Utah. Large expanses of Navajo Sandstone make up the majority of the foreground rocks - these were once (millions of years ago) a vast expanse of sand dunes. The remnants of the dunes are found in structures called cross beds, where layers of...
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The view from the parking lot near the east entrance to Badlands National Park.
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