- strike-slip and dip-slip. In a
strike-slip
fault (also
known as a
wrench fault, tear
fault or
transcurrent fault), the
fault surface (plane) is
usually near...
-
subduction zone. A
transform fault is a
special case of a
strike-slip
fault that also
forms a
plate boundary. Most such
faults are
found in
oceanic crust...
- Enriquillo–Plantain
Garden fault zone (EPGFZ or EPGZ) is a
system of
active coaxial left lateral-moving
strike slip
faults which runs
along the southern...
- The
North Anatolian Fault (NAF) (Turkish:
Kuzey Anadolu Fay Hattı) is an
active right-lateral
strike-slip
fault in
northern Anatolia, and is the transform...
- The
Marikina Valley fault system, also
known as the
Valley fault system (VFS), is a
dominantly right-lateral
strike-slip
fault system in Luzon, Philippines...
-
uplifted on the
fault over the last 12
million years in a
series of earthquakes. However, most of the
motion on the
fault is
strike-slip (side to side)...
- The San
Andreas Fault is a
continental right-lateral
strike-slip
transform fault that
extends roughly 1,200
kilometers (750 mi)
through the U.S. state...
- The Septentrional–Orient
fault zone (SOFZ) is a
system of
active coaxial left lateral-moving
strike slip
faults that runs
along the
northern side of the...
- The
Great Glen
Fault is a
strike-slip
fault that runs
through the
Great Glen in Scotland.
Occasional moderate tremors have been
recorded over the past...
- four
types of
faults classified by
geologists today, Anderson's
fault theory focuses on the
explanation of three: normal, reverse, and
strike-slip. Slip...