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A type of lake that forms in the depression of the earth's crust between two parallel faults is known as
Question

A type of lake that forms in the depression of the earth's crust between two parallel faults is known as

A.

Grade lake

B.

Surface lake

C.

Graben lake

D.

Glacial lake

Correct option is C

Introduction
· Lakes are inland bodies of water that occupy depressions on the Earth's surface, formed through various geological, tectonic, or glacial processes.
· Tectonic lakes, in particular, are created by the movements of the Earth's crust, such as tilting, folding, or faulting, which create significant natural basins.
· Understanding the geomorphology of lake basins is essential in environmental science for studying sedimentation patterns and long-term ecosystem stability.

Information Booster
· Graben lake is the correct answer because it specifically refers to a lake formed within a "Graben," which is a depressed block of the Earth's crust bordered by parallel normal faults.
· These lakes are often characterized by being very deep, long, and narrow, as they occupy the floor of rift valleys created by tectonic divergence or crustal stretching.
· A classic example of such a formation is Lake Baikal in Siberia or the various lakes found within the East African Rift Valley, such as Lake Tanganyika.
· The downward displacement of the central fault block (the graben) creates a natural catchment area where water accumulates over geological timescales.
· Because of their tectonic origin, these lakes are often among the oldest and deepest freshwater bodies on the planet.

Additional Knowledge
· Grade lake is not a standard geological term for a lake type; however, "graded" usually refers to a stream or slope that has achieved a state of equilibrium between erosion and deposition.
· Surface lake is a general descriptive term for any body of water on the Earth's exterior but does not specify a particular geological formation process or tectonic origin.
· Glacial lake refers to a lake formed by the action of glaciers, such as those created by glacial erosion (cirque lakes) or by the damming of water by glacial debris like moraines.
· Horst and Graben structures often occur together, where the "Horst" is the uplifted block between faults and the "Graben" is the sunken block that eventually becomes the lake bed.

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