Internal Processes / Landforms - Solid Tectonic Processes
Folding
existing rocks are bent, tilted, folded, or fractures by pressure
sedimentary rocks - once laid horizontally now tilted or folded
compressional forces
over time deform rock
wrinkle
Earth's crust
simple folds
- wavy like, with symmetrical folds
syncline
or synclinal trough
Faulting
tensional or lateral forces
often associated with faulting
Normal fault
- tensional forces drop block
one block rises, the other slips downward
Grand Tetons
, Sierra Nevada, Great Basn
Strike-slip
fault - lateral movement
one block slides past another block
San Andreas fault
Fault Block Mountain Ranges
(also called
Fault-Scarp
Mtns.)
gentle fronts slope, steep back-side escarpment
massive displacement of rocks
exposing
deeply-formed rocks
characteristic of the American West
Horst & Graben Landforms
- tensional forces
Parallel faults
drop block known as
graben
characteristic of the
Great Basin
Physical Index