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G11 SEM1 Q2
EARTH SCIE 2Q
L4 | STRESS AND STRAIN
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Cards (30)
STRESS
force
applied to an object.
force per unit area that is placed on a rock.
4 TYPES OF
STRESSES
:
CONFINING
TENSION
COMPRESSION
SHEAR
CONFINING
deeply buried rock is pushed down by the weight of all the material above it
TENSION
Rocks are pulled
apart
Force acting
perpendicular
to and
away
fro a surface
Major type of stress at
divergent
plate
COMPRESSION
Pushed
together
SHEAR
Parallel
but in
opposite
direction
Force acting parallel to a surface
Most common stress at
transform
plate boundary
STRAIN
Deformation
Change in solid’s shape caused by the application of
stress
2 KINDS OF
DEFORMATION
ELASTIC
DEFORMATION
PLASTIC
DEFORMATION
ELASTIC DEFORMATION
the rock returns to its
original
shape when the
stress
is removed.
PLASTIC DEFORMATION
rock
does
not
return to its
original
shape when the
stress
is removed.
FRACTURE
Happens when rock
breaks
FOLDS
Bend in the rock in response to
compressional
forces
Noticeable in rocks with
stratification
3 TYPES OF
FOLD
:
MONOCLINE
ANTICLINE
SYNCLINE
MONOCLINE
Bend in the rock layer so that they are no longer
horizontal
ANTICLINE
Folding of rock into
arch-like
shape
Oldest
beds
SYNCLINE
Fold that bends
downward
3 TYPES OF FOLD
A)
MONOCLINE
B)
ANTICLINE
C)
SYNCLINE
3
FAULT
Fracture
or
zone
of fractures between 2
blocks
of rock
Allows the block to move
relative
to each other
3 TYPES OF
FAULT
:
NORMAL FAULTING
REVERSE FAULTING
STRIKE
-
SLIP
FAULTING
NORMAL
FAULTING
Crust is being pulled apart in which the overlying block moves down with respect to the lower block.
REVERSE
FAULTING
Crust is being compressed in which the hanging wall block moves up and over the footwall block
STRIKE-SLIP
FAULT
Dip-slip fault in which the dip of the plane is vertical
Result from
shear
stress
3 MAIN TYPES OF FAULT:
A)
NORMAL FAULT
B)
REVERSE FAULT
C)
STRIKE-SLIP FAULT
3
3 STAGES OF DEFORMATION:
FRACTURE
DEFORMATION
ELASTIC
DEFORMATION
DUCTILE
DEFORMATION
FRACTURE
DEFORMATION
irreversible
strain
, rock breaks because it is
brittle
DUCTILE
DEFORMATION
strain is
irreversible
changes in its shape are
permanent
, and the material is no longer able to
revert
to its original shape
SLIP
distance that rocks move sideways a fault
can be up or down the fault plane
DIP SLIP FAULT
fault's dip is inclined relative to the
horizontal
surface
OBLIQUE
SLIP
FAULT
fault which has components of
dip
slip
and
strike
slip
TYPES OF STRESS
A)
CONFINING
B)
TENSION
C)
COMPRESSION
D)
SHEAR
4