Photo 5-1 A river floor in Chu-Tzu Keng
About 100 m southwest of the factory of photo 1. The river bed was bended and uplifted by the faulting, which is striking NE.
An example of no jumping of gravels
No. 2
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Photo 5-1 A river floor in Chu-Tzu Keng About 100 m southwest of the factory of photo 1. The river bed was bended and uplifted by the faulting, which is striking NE. |
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Photo 5-2 A view from the top of the fault scarp in the above photo. There is a pond due to the uplift and depression behind the buldge. The gravels on the buldge showed no trace of jumping. |