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The Rock Cycle and Tectonics. One drives the other. The Rock Cycle. Fig. 1.21. Two tectonic episodes recorded. Convergent Tectonics. Horizontal compressional forces - old ocean crust destroyed - reverse dip-slip faults, folds formed - new mountains created (continental collision).
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The Rock Cycle and Tectonics One drives the other.
The Rock Cycle Fig. 1.21
Convergent Tectonics Horizontal compressional forces - old ocean crust destroyed - reverse dip-slip faults, folds formed - new mountains created (continental collision)
Convergent Tectonics +time +time example: Himalayan Mountains
Divergent Tectonics Horizontal tensional forces - normal dip-slip faults - new ocean crust created
Divergent Tectonics Horizontal tensional forces - normal dip-slip faults - new ocean crust created
Transform Tectonics Horizontal shearing forces - strike-slip faults - no crust created or destroyed
The Rock Cycle Fig. 1.21