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Mountain Building Processes Year 7 Geography What are mountains? The dictionary defines a mountain as that which is ‘higher and steeper than a hill’. It is a landform that extends above the surrounding terrain in a limited area. Mountains usually have steep, sloping sides and sharp or slightly rounded ridges and peaks. Generally, mountains are landforms that rise above 2000 feet. Mountains exist on every continent and even beneath our great oceans. Formed through varying causes, there are several distinct types of mountains. Types of mountains There are five basic kinds of mountains: dome, fold, fault-block, volcanic, and plateau mountains. Dome mountains Dome mountains are the result of a great amount of melted rock pushing its way up under the earth Fold mountains Fold mountains are formed when two plates collided head on, and their edges crumbled, much the same way as a piece of paper folds when pushed together. Fault-block mountains These mountains form when faults or cracks in the earth's crush force some materials or blocks of rock up and others down. Volcanic mountains Volcanic Mountains are formed when molten rock, or magma deep within the earth, erupts, and piles upon the surface. Plateau mountains These are mountains that are really plateaus that have worn down from erosion. How mountains form? The Earth's crust is made up of 6 huge slabs called plates, which fit together like a jigsaw puzzle. When two slabs of the Earth's crust smash into each other the land can be pushed upwards, forming mountains. Many of the greatest mountain ranges of the world have formed because of enormous collisions between continents. http://www.classzone.com/books/earth_science/terc/content/visualization s/es1105/es1105page01.cfm?chapter_no=visualization http://www.seed.slb.com/en/scictr/watch/living_planet/mountains.ht m