KERALA PSC / PHYSICAL GEOGRAPHY / CLASSIFICATION OF
LANDFORMS / PLATEAUS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL
KNOWLEDGE
KERALA PSC / PHYSICAL GEOGRAPHY / CLASSIFICATION OF LANDFORMS / PLATEAUS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE
PLATEAUS
·
A
plateau is an elevated area generally in contrast to the nearby areas.
·
It
has a large area on its top unlike a mountain and has an extensively even or
undulating surface.
·
The
rocks of the plateau are layered with sandstones, shales and limestones.
·
But
an inclined or tilted strata may also become flat through continuous wearing
down. The great Deccan Plateau with its slope towards east is a tilted plateau
in our country.
·
Very
often, rivers and streams cut out deep valleys and canyons in a plateau region.
·
The plateaus are famous for minerals. Plateaus
have cooler climates than those of plains. The plateaus are of four types on
the basis of their situation:
Ø
Intermontane
plateaus
Ø
Continental
plateaus
Ø
Piedmont
plateaus
Ø
Lava
plateaus
INTERMONTANE
PLATEAUS
·
The
plateaus which are partly or fully enclosed by mountains are known as Intermontane
Plateaus.
·
The
highest and extensive plateaus of the world such as Tibet, Bolivia and Mexico
are of this category.
·
These
are the results of the mountain-building process which was accompanied by a
vertical uplift of the adjoining enclosed lands.
PIEDMONT PLATEAUS
·
Situated
at the foot of a mountain, they are bounded on the opposite side by a plain or
an ocean.
·
The
plateau of Malwa in India, Those of Patagonia in Argentina and the Appalachian
in US are some of the examples. Eg: Appalchian plateau, Patagonian plateau
CONTINENTAL
PLATEAUS
·
They
rise abruptly from the lowlands or from the sea
·
They
are the result of a continental uplift producing large tablelands like the
plateaus of Brazil, South Africa, West Australia, Chotanagpur and Shillong.
Their heights vary from 600-1500 metres.
·
Sometimes
a plain or a low-lying area is vertically uplifted and gives rise to a plateau.
·
In
India plateaus of Kaimur, Rohtas, Ranchi and Karnataka are of this type.
LAVA PLATEAUS
·
When
lava spreads out to cover the pre-existing land surface, a lava plateau is
formed which is also called a plateau of accumulation.
·
The
horizontal sheets of lava flow have trapped the original topography varying in
depth from 1200-1500 meters over large parts of Maharashtra and the adjoining
areas in Deccan. Eg : Columbia plateau (USA), Mahabaleshwar plateau
KERALA PSC / PHYSICAL GEOGRAPHY / CLASSIFICATION OF LANDFORMS / PLATEAUS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

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