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Continents Collide and grind against one another,
while hot, molten rock bubbles beneath earth’s surface.
these powerful forces thrust up mountains reaching as
high as 5 miles (8 km). Many mountains are still growing,
and those that formed long ago are slowly wearing
away. some mountains are volcanoes, made of layers
of so lid i fied lava that build up as the volcano erupts.
there are mountains under the oceans and on other
planets. the highest known mountain is on Mars;
it is three times as high as Mount everest.
earth has two vast mountain ranges. the Rocky
Mountains and the Andes run through north
and south America; the mighty Himalayas,
Alps, and Atlas Mountains stretch across Asia,
europe, and north Africa. these mountains
are “young”: they formed during the last 50
million years. other ranges, such as the Urals
in Russia, are much older and lower. the
forces of erosion have worn them down
since they were first formed more
than 200 million
years ago.
MoUnt eveRest
the world’s highest
mountain is Mount everest,
on the border of China and
nepal. it rises to 29,029 ft
(8,848 m). Above are
edmund Hillary of new
Zealand (left) and tenzing
norgay of nepal, who first
climbed everest in 1953.
AvAlAnCHe
snow and ice can
suddenly crash down a steep
mountainside. this is called an
avalanche, and it often occurs
in the spring as the snow melts.
MoUntAin CliMbing
Mountain climbing
requires special
equipment, such
as ropes to prevent
falls, and crampons—
steel spikes attached
to mountaineers’
boots that
grip ice.
eRosion
ice, wind, and running water break
up rock, slowly wearing it away over
millions of years. this process of
erosion carves out deep valleys and
creates high peaks. Continuing
erosion wears away the peaks, so
that the mountains become
lower and more rounded.
MoUntAin Zones
A high mountain has several zones, or
regions, containing different kinds of plants.
Forests cover the mountain’s lower reaches.
Farther up is a zone of small, low-lying
plants. snow covers the summit, which is
bare of plant life. Zones occur because the
air becomes colder higher up the mountain.
Forests of broad-
leaved trees and a wide
range of other vegetation
grow at the base of
the mountain.
FAUlting And Folding
As the continents move, they
squeeze layers of rock. these
movements produce huge
cracks, or faults, and push
up blocks of rock that
form block mountains. the
movements also make earth’s
surface buckle, form ing fold
mountains. dome mountains
appear when molten granite
pushes the rock above it into
a huge hump.
Formation of
block mountains
High on the
mountaintop it
is so cold that
plants cannot
grow. There
is only snow
and bare
rock.
Formation of fold
Mountains
Mountains
Block wears away
over many years to
produce a mountain.
Squeezing action
pushes up
blocks of rock.
The rocks then
crack and
wear away at
the top of the
curve, forming
jagged mountains.
As layers of rock
are squeezed, they
form zigzag folds.
Find out more
Continents
glaciers and ice caps
Mountain wildlife
oceans and seas
volcanoes
Higher still, only
plants that are
adapted to the cold
are able to grow.
Forests of pine
trees grow higher
up the mountain
where it is colder.
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