Source: Koshy Koshy via Flickr (CC BY 2.0)
Last
November, my daughter and I visited the Himalayan Mountains', as soon as she laid
eyes on the beautiful complex convergent continental plate boundary, she could
tell that this mountain range was profoundly special. As we joked, I begin to
listen to her explain, that the Himalayas were probably form under a lot of
compressional stresses, due to the degree of the thrust fault formations. These
apparent asymmetric extreme angled anticline-synclines of this fold belt are
metamorphic rock due to its dark appearance. She notes, that the propagation
folds are dramatically uplifting the continental crust as the younger rocks are
forced over the older rocks.
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