·
The plateaus cover about 18%
of the earth’s surface.
·
This landform has a large
elevated area on its top unlike a mountain and has nearly even surface out
there.
·
Very often rivers or streams
cut out deep valleys and gorges in a plateau region.
·
In place of its original
smooth topography, it then changes into a disected plateau.
·
Though normally 600 metres
above sea level, there are plateau of Tibet and Bolivia, more than 3600 metres
above sea level.
CLASSIFICATION OF PLATEAUS :
On the basis of their
geographical location and structure of rocks, the plateaus can be classified
as:
(a) Intermontane Plateaus
(b) Piedmont Plateaus
(c) Continental Plateaus
(a) Intermontane Plateau :
·
The plateau which are
bordering the fold mountain range or are partly or fully enclosed within them
are the intermontane plateaus .
·
Vertical movements raise this
extensive landforms of nearly horizontal rocks to thousands of metres above sea
level.
·
The extensive and over 4500
metres high plateau of Tibet is one such example.
·
It is surrounded by folded
mountains like Himalaya, Karakoram, Kunlun, Tien Shah on its two sides.
·
The plateau of Colorado is
another well known example, over one km high into which rivers have cut the
Grand Canyon and a series of gorges.
·
The plateau of Mexico,
Bolivia and Iran are all other examples of this type.
(b) Piedmont Plateau :
·
The plateaus that are
situated at the foot of the mountains and are bounded on other sides by a plain
or an ocean are called piedmount plateau.
·
The plateau of Malwa in India, those of Patagonia facing the Atlantic ocean and the
Appallachian situated between the Appalachian Mountain and the Atlantic Coastal
Plain in U.S.A are their examples.
·
In their case, the areas once
high have now been reduced by various agents of erosion.
·
For this reason, these are
also called the plateaus of denudation.
(c) Continental plateau :
·
These are formed either by
an extensive continental uplift or by the spread of horizontal basic lava
sheets completely covering the original topography to a great depth.
·
The volcanic lava covered
plateau of Maharashtra in India, Snake River Plateau in
North West USA are the examples of this type.
·
These are also, called the ptateau of accumulation.
·
All continental plateaus show
an abrupt elevation in contrast to the nearby lowland or the sea .
·
As compared to other, these
plateaus, cover a vast area like the Great Indian Plateau and those of Arabia,
Spain, Greenland, Africa and Australia.
·
They may be tilted on one
side without any disturbance in the horizontal nature of underlying rock strata
as in the case of Great Indian plateau.
·
Due to continuous erosion of
their surface, we observe the prevalence of a patchy or the slow development of
agriculture and building of roads on the plateaus.
Nevertheless plateaus are extremely useful to mankind in the
following ways:
(1) Storehouse of Minerals :
·
Most of the minerals in the
world are found in the plateaus.
·
Besides, the extraction of
minerals is relatively easier on plateaus.
·
We get gold from the Plateau
of Western Australia; copper, diamonds and gold from the Plateaus of Africa and
coal, iron, manganese and mica from the Chota Nagpur Plateau in India.
(2) Generation of
Hydel-power :
·
Rivers falling down the edges
of plateaus form water-falls.
·
These waterfalls provide
ideal sites for generating hydel-power.
(3) Cool Climate :
·
The higher parts of the
plateaus even in tropical and sub-tropical regions have cool climate.
·
Hence they have attracted
Europeans to settle there and develop their economy e.g. South and East Africa.
(4) Useful for
Animal-rearing and Agriculture :
·
Plateaus have large grassland
areas suitable for animal-rearing specially sheep, goat and cattle.
·
They provide a veriety of
products such as wool, milk, meat and hides and skin.
·
The lava plateaus as compared
to all other plateau are richer in agriculture since their soil is very fertile.
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