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View 3 of 3. For comparison with this same scene in full flood: gigapan.com/gigapans/129569
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- 40
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May 14, 2013. View 2 of 3 For a version of this same view, but with flood waters raging, see this GigaPan: gigapan.com/gigapans/129543
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- 76
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- 36
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May 14, 2013. View 1 of 3 Compare with this one (from the same exact site), taken during the flood: gigapan.com/gigapans/129490
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- 100
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- 72
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Kilbourne Hole is a maar crater in southern New Mexico. Compare with this non-annotated view: gigapan.com/gigapans/129481
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- 164
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- 31
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Kilbourne Hole is a maar crater in southern New Mexico. Compare with this non-annotated view: gigapan.com/gigapans/129419
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- 93
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- 30
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The Boquillas, Fort Hancock, and Camp Rice formations are exposed here in a classic example of an angular unconformity. This annotated GigaPan is intended as a complement to the 'raw' image here: gigapan.com/gigapans/129421
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- 99
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- 42
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The Baraboo Quartzite, before metamorphism, was laid down as sand ~1.7 billion years ago. Here, the bedding is tilted up to vertical due to a large synclinal fold that forms the Baraboo Hills of Wisconsin. You're actually looking at the underside of the layers here-- making it effectively a cast of the ripples that exi...
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- 56
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- 51
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This rock, named after geologist Charles Van Hise, is a National Historic Landmark. Between two layers of quartzite - vertical here - is a layer of phyllite that has been sheared because of its sandwiched position. As the entire unit of rock folded into a large syncline, the stronger quartzite layers slid past each oth...
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- 130
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- 42
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A zone of breccia exists parallel to bedding in this location. The red rock is the quartzite, which is surrounded by a matrix of quartz. The breccia is thought to be related to hydrothermal activity, not faulting.
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- 59
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- 58
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This outcrop of the Baraboo Quartzite shows both gorgeous cross-bedding and ripple surfaces.
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- 54
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- 49