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Mountain Building
Processes
Year 7 Geography
What are mountains?
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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
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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
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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
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