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The term that describes down-dropped blocks of crust bounded by steeply dipping normal faults is "graben." Graben formations occur when tectonic forces cause the crust to extend and fracture, leading to the subsidence of these blocks. They are often found in rift valleys and are characterized by their steep sides and a lower elevation compared to the surrounding terrain.

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What term describes down dropped blocks of crust bounded by steeply dipping normal faults?

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Which term describes down-dropped blocks of crust bounded by steeply dipping normal faults?

The term that describes down-dropped blocks of crust bounded by steeply dipping normal faults is "graben." Graben formations occur as a result of tectonic forces pulling the Earth's crust apart, leading to the subsidence of the block between the faults. This process is often associated with extensional tectonics and can create distinct geological features.


What term describes down-dropped blocks of crust bounded by steeply dipping normal faults?

These down-dropped blocks of crust are called grabens. Grabens are formed by the extensional forces that cause the crust to stretch and create space for the down-dropped blocks between the steeply dipping normal faults.


A graben is bounded on each side by?

A graben is bounded on each side by normal faults and upthrown crustal blocks known as horsts.


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A fault-block mountain is the type of mountain that is bounded by faults, where blocks of the Earth's crust are pushed up or dropped down along fault lines, creating mountain ranges with steep, rugged edges.


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