Hey Guys, What’s up? Let’s study about Volcanoes and its landform today.
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Volcanoes
– a place where gases, ashes and/or molten rock
material-lava-escape to the ground.
(This picture must
have reminded most of you about your childhood science project where you or
your friends have actually made volcano, yes these are the ones we are
discussing today. See UPSC is all about General Knowledge and basic Common
Sense)
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Types of
Volcanoes :-
o Shield Volcanoes – 2nd largest after basalt flows Eg Hawaiian volcano, made of
basalt – very fluid lava, not steep, explosive only if water enters.
o Composite
volcanoes – like mountains, more
viscous lava; along with lava large quantities of pyroclastic materials &
ashes find their way to the ground.
o Caldera – most explosive, collapsed on themselves, collapsed depressions called
caldera.
o Flood Basalt Provinces – highly fluid lava flows for long distances. Eg.
Deccan Trap, Maharashtra.
o Mid-Ocean Ridge Volcanoes- volcanoes in oceanic areas. Length more than 70,000
kms stretching through all oceans.
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Volcanic
Landforms
§ Lava released during volcanic eruptions on cooling,
forms igneous rocks.
§ Cooling may take place on surface or inside surface.
§ Depending on location of cooling, igneous rocks –
·
Plutonic
(cooling beneath surface)
·
Volcanic
(cooling at the surface)
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Intrusive
Landforms – lava cooling beneath surface.
o
Batholiths
– large dome shaped
o Lacoliths – large dome shaped with a level base & connected by a pipe-like
conduit from below. Eg. Karnataka Plateau spotted with domal hills of granite
rocks.
o
Lapolith-
Saucer shaped, concave to sky body.
o
Phacoliths-
wavy material
o Sill or sheet – horizontal bodies; thinner ones are sheets & thicker ones are sills.
o
Dykes – perpendicular to ground. Eg. West Maharashtra areas.
This was about the Volcanoes and its
landforms. In the next article, we will learn about Ocean & Continent distribution.
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Thankyou
ReplyDeleteThank you sir
ReplyDeletethank you sir
ReplyDeletereally nice and understandable
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