Haughton Tour: Thomas Payne Canyon

As you can see from these pictures, the layers of rock near the tops of the canyon walls are nearly all horizontal. They are sedimentary rocks, primarily limestones. These rocks were laid down approximately 380-450 million years ago when the region was covered by shallow tropical seas. The rocks approximately 15 kilometers to the west of this location were also horizontal when the impact occurred 23 million years ago. Keep this in mind as we go from stop to stop on our Haughton tour. If you notice any rocks that are NOT horizontal, then its safe to assume that these rocks were deformed and moved around by the impact event.

Tour Stops

Haughton: BasecampHaughton: DirectionsHaughton: Thomas Payne Canyon
Haughton: Stop 1Haughton: Stop 2Haughton: Stop 3
Haughton: Stop 4Haughton: Stop 5Haughton: Stop 6
Haughton: Stop 7Haughton: Stop 8Haughton: Stop 9
Haughton: Stop 10Haughton: Stop 11Haughton: Stop 12
Haughton: Stop 13Haughton: Stop 14Haughton: Stop 15
Haughton: Stop 16Haughton: Stop 17
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