the oblique slip fault is a movement that has a combination of normal and strike-slip fault
An oblique slip fault is a type of fault where the movement is a combination of both strike-slip and dip-slip motion. This means that the fault moves both horizontally and vertically. Oblique slip faults are common in areas where different stresses are acting on the Earth's crust, causing complex fault movements.
A fault that is a combination of dip-slip and strike-slip movements
There are 6 types of fault lines. Strike-slip faults, dip-slip faults, oblique- slip faults, listric faults, ring faults, and synthetic and antithetic faults.
internal oblique opposes the external oblique
Oblique lines:
oblique rectangular
Oblique means at an angle.
Slanting. A slash (/) is oblique
Oblique means slanted or at an angle.
Oblique-slip faults are found along the San Andreas Fault in California, USA. Strike-slip faults can be found along the North Anatolian Fault in Turkey. Normal faults are common in the East African Rift Valley. Reverse faults can be seen in the Himalayas in Asia.
The inguinal ligament runs deep to the external oblique muscle.
One's a triangle.