The hanging wall slides down relative to the footwall.
Hanging wall moves down relative to football.
Occurs when the hanging wall moves down relative to the footwall.
Normal faults usually form where tectonic plate motions cause tension.
A dip slip fault in which the upper block above the fault plane moves up and over the.
Along a normal fault the hanging wall moves down relative to the footwall.
Occurs when the hanging wall moves down relative to the foot wall reverse fault.
A n fault forms when the hanging wall moves up relative to the footwall.
The theory that continents move apart from each other.
When the hanging wall moves down in relative to the footwall it is called a fault.
An upthrown block between two normal faults dipping away from each other is a horst.
When the hanging wall moves up in relative to the footwall it is called a fault.
These usually occur when tectonic forces cause tension that pulls rocks apart.
Normal faults are common.
In a normal fault the hanging wall moves downward relative to the footwall.
Tension is stress that pulls rocks apart.
In a fault the hanging wall block moves down relative to the footwall block.
Occurs when opposing when the hanging forces cause rock to break and move horizonally.
A map symbol similar to the letter t is used to record on a map.
A downthrown block between two normal faults dipping towards each other is a graben.
The hanging wall moves down relative to the foot wall.
Since there is thicker crust in the himalayas it is heavier and pushes the crust down farther into the mantle aesthenosphere.
Dip either east or west.
Low angle normal faults with regional tectonic significance may be designated detachment faults.
They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins of tectonic plates.
A dip slip fault in which the block above the fault has moved downward relative to the block below.
This type of faulting occurs in response to extension.
The layer of earths that has the most mass.