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sci lesspn 1 : introduction to volcanoes and their types
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geomorphology
: the study of the relief features of the earths crust
diastrophism
: vertical and horizontal movement of the crust, caused by the movement of the plates
erosion
: physical removal of rock by weathering, water, ice, or wind
diastrophism can occur due to
internal pressure
erosion
are caused by forces outside the earths crust
vulcanism
: also called as
volcanicity
, phenomenon related to various processes associated with the surface discharge of magma
geyser
: phenomenon on the surface where the ground water beneath the shallow surface is heated up
fumaroles
: emit mixtures of steam and other gases
fumaroles are fed by
conduits
fumaroles are responsible for
intense chemical activities
hot springs occur in many
geothermal
areas where the
surfce
of the earth intersects the
water table
volcano is an example of
extrusive
volcano
volcano
: cone-shaped hill or mountain form by the extrusion of lava
vulcano, an islan of sicily named after the roman god of fire,
vulcan
859
active volcanoes
75
% of them are located in the ring of fire
ring of fire
: belt of the volcanoes that rings the pacific ocean
Paricutin
: located near the town of san juan, mexico
paricutin
: an active volcano as violent explosion were seen during the past
five
years
paricutin cone grew
336m
+
88m
for another
8
yrs
types of volcanoes
cinder cones
composite volcanoes
shield volcanoes
volcanic domes
supervolcanoes
submarine volcanoes
subglacial volcanoes
cinder cones is also known as
scoria cone
cinder cones
: the simplest type of volcano
cinder cones
are steep conical hill, commonly found on flanks and in the calderas of hawaii
250m
in height
composite volcanoes are also called as
stratovolcano
composite volcanoes are made of alternating layers of
pyroclastic materials
and
solidified lava flows
composite volcanoes essential flows is
conduit system
shield volcanoes
are broad gently sloping landform built by many layers of low-viscous lava flows
shield volcanoes eruptions on this type are relatively
non-violent
mauna loa
is the largest shield volcano in the world and is located in
hawaii
stands at 13,677 ft above sea level
28,000
ft avove
volcanic domes also known as
lava domes
volcanic domes
are rounded, steep-sided mound that is formed by small, bulging masses of lava
supervolcanoes
are made to produce largest eruptions on earth
vei meaning -
volcanic explosivity index
VEI scale is created my
christopher g. newhall
in the us and
stephen self
at the university of hawaii in
1982
volumes of tephra
are usually obtained by mapping the distribution and thickness of the tephra
submarine volcanoes
are created when magma erupts in the underwater fissures of the earth.
submarine volcanoes
are found near ocean ridges, shallow water
pillow lava
characterized by thick sequence of discontinuous pillow-shaped masses
hydrothermal vents are commonly found in
submarine volcanoes
subglacial volcanoes
are also called
glaciovolcano
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