Internal Processes / Landforms - Solid Tectonic Processes
Folding
existing rocks are bent, tilted, folded, or fractures by pressure
not igneous processes
sedimentary rocks - once laid horizontally now tilted or folded
California Coast Range
and Transverse Range (So. Calif.)
compressional forces
over time deform rock
wrinkle
Earth's crust
tablecloth
example
Appalacian
Mountains
/ Coast Range
simple folds
- wavy like, with symmetrical folds
syncline
or synclinal trough or valley
anticline
or anticlinal ridge (like an ant hill)
often
exposed
by erosion
Waterpocket fold
, Utah and
other folds
Faulting
Tensional stress or lateral forces
often associated with faulting
rigid rocks rupture instead of fold
vertical displacement
earthquakes - ground shaking
also: landslides, liquefaction, and even tsunamis
Normal fault
- tensional stresses
one block slides down
Strike-slip
fault - lateral movement
one block slides past another block
San Andreas fault
Fault-Block Mountain Ranges
(also called
tilted fault-block
Mtns.)
gentle fronts slope
, steep back-side escarpment
massive displacement
of rocks
exposing
deeply-formed rocks
Sierra Nevada,
Grand Tetons
Horst & Graben Landforms
- tensional stress
Parallel faults
drop block known as
graben
Great Basin
(basin & range region)
Death Valley -
half-graben
Physical Index