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Diastrophism
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Diastrophism
Large scale movement causing deformation of earth's surface
Continental drift theory
Theory proposed by
Alfred Wegener
in
1912
that there was once a supercontinent called
Pangaea
which started to
break up
and form
smaller masses
Alfred Wegener
was a
German
geologist
Plate tectonic theory
Theory that the lithosphere is broken into plates that move on the asthenosphere (molten upper mantle)
Asthenosphere
Molten upper mantle
Plate
tectonic
theory
Oceanic
and
continental crust
interact to form
ridges
,
rifts
,
trenches
, and
mountains
Major tectonic plates
North American
South American
Eurasian
Pacific
African
Indo-Australian
Antarctic
Plate
boundaries
Where plates meet
Types of plate boundaries
Divergent
/
spreading
Convergent
/
colliding
Transform fault
Stress
A force that can compress, pull apart, and deform a rock
Types of stress
Compression
Tension
Shear
Folding
Bending of rock without breakage
Types of folds
Monocline
Anticline
Syncline
Fault
A fracture in the earth's crust
Main groups of faults
Normal
Thrust
(
reverse
)
Strike-slip
Hanging wall
Rock above the fault
Footwall
Rock below the fault
Diastrophism
Large scale movement
causing
deformation
of
earth surface
Continental drift theory
Theory proposed by
Alfred Wegener
in
1912
that there was once a supercontinent called
Pangaea
which started to
break up
and form
smaller masses
Alfred Wegener
was a German geologist
Plate tectonic theory
The
lithosphere
is broken into
plates
that move on the
asthenosphere
Oceanic
and
continental crust
interact to form
ridges
,
rifts
,
trenches
, and
mountains
Major tectonic plates
North American plate
South American plate
Eurasian plate
Pacific plate
African plate
Indo-Australian plate
Antarctic plate
Plate boundaries
Where plates
meet
Types of plate boundaries
Divergent
/
spreading
(move away from each other)
Convergent
/
colliding
(two plates bump each other, creating volcanoes and trenches)
Transform fault
(two plates rub/slip horizontally)
Stress
A force that can compress, pull apart, and deform a rock
Types of stress
Compression
(squeezes rock causing folding)
Tension
(stretches causing lengthening/breaking apart)
Shear
(slippage and translation)
Folding
Bending of rock without breakage
Types of folds
Monocline
(one-sided slight bend)
Anticline
(symmetrical arch-shaped fold)
Syncline
(rock below pushed up into V or U shape)
Fault
Fracture in the earth's crust
Types of faults
Normal
(pulling/tension moves rock up and down)
Thrust
/
reverse
(squeezing/compression)
Strike-slip
(shearing horizontal movement)
Hanging wall
Rock above the fault
Footwall
Rock below the fault