A map symbol similar to the letter t is used to record on a map.
Hanging wall moves down relative to football.
Occurs when the hanging wall moves down relative to the footwall.
Rift valleys are formed by the sliding of the hanging walls downward many thousands of metres where they then become the valley floors.
In a normal fault the hanging wall moves downward relative to the footwall.
In a fault the hanging wall block moves down relative to the footwall block.
A downthrown block between two normal faults dipping towards each other is a graben.
The hanging wall moves down relative to the foot wall.
Occurs when opposing when the hanging forces cause rock to break and move horizonally.
This type of faulting occurs in response to extension.
The layer of earths that has the most mass.
Normal faults are common.
Formed by tensional stress rocks are stretched away from each other.
When the hanging wall moves up in relative to the footwall it is called a fault.
The hanging wall slides down relative to the footwall.
Since there is thicker crust in the himalayas it is heavier and pushes the crust down farther into the mantle aesthenosphere.
They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins of tectonic plates.
Dip either east or west.
Tension is stress that pulls rocks apart.
A dip slip fault in which the block above the fault has moved downward relative to the block below.
Occurs when the hanging wall moves down relative to the foot wall reverse fault.
When the hanging wall moves down in relative to the footwall it is called a fault.
The theory that continents move apart from each other.
If a bed strikes north it must.
A n fault forms when the hanging wall moves up relative to the footwall.
Low angle normal faults with regional tectonic significance may be designated detachment faults.
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.