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Published byJulie Webb Modified over 8 years ago
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Mountain Building By : Thais, Jahod, Nick, and Dennisja
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Folded Mountains The Folded Mountains form when rock layers are squeezed together, and pushed upward. An example of a Folded Mountain range that formed at a convergent boundary. Other examples of mountain ranges that consist of very and complex folds are the Alps in central Europe, the Ural Mountains in Russia, and the Himalayas.
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Fault-Block Mountains Fault-Block Mountains forms when this tensions causes large blocks of the Earths crust to drop down relative to other blocks. When sedimentary rock layers are tilting up by faulting, they can produce mountains that have sharp, jagged peaks. For example, the Tentons in western Wyoming are a spectacular of the Fault-blocking Mountains.
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Volcanic Mountains Volcanic Mountains are rocks that is melted in subduction zones form magma, which rises to the Earths surface and erupts. Volcanic Mountains can also form under the sea, which sometimes rises above the ocean surface to become islands/land. Volcanic Mountains on the Earth have formed around the tectonically active rim of the Pacific Ocean.
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