A n fault forms when the hanging wall moves up relative to the footwall.
Hanging wall moves down relative to football.
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.
Tension is stress that pulls rocks apart.
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 upper block above the fault plane moves up and over the.
Low angle normal faults with regional tectonic significance may be designated detachment faults.
Dip either east or west.
If a bed strikes north it must.
Formed by tensional stress rocks are stretched away from each other.
In a normal fault the hanging wall moves downward relative to the footwall.
When the hanging wall moves down in relative to the footwall it is called a fault.
The hanging wall slides down relative to the footwall.
In a fault the hanging wall block moves down relative to the footwall block.
These usually occur when tectonic forces cause tension that pulls rocks apart.
Along a normal fault the hanging wall moves down relative to the footwall.
Occurs when opposing when the hanging forces cause rock to break and move horizonally.
Rift valleys are formed by the sliding of the hanging walls downward many thousands of metres where they then become the valley floors.
Occurs when the hanging wall moves down relative to the footwall.
An upthrown block between two normal faults dipping away from each other is a horst.
Occurs when the hanging wall moves down relative to the foot wall reverse fault.
Normal faults usually form where tectonic plate motions cause tension.
A downthrown block between two normal faults dipping towards each other is a graben.
The theory that continents move apart from each other.
When the hanging wall moves up in relative to the footwall it is called a fault.
The layer of earths that has the most mass.
Normal faults are common.