Angle of repose is the maximum slope angle at which given unconsolidated material is stable. O a mixed flow of rock, sediment, vegetation and other materials.

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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Angle of repose is
the maximum slope angle at which given
unconsolidated material is stable.
a mixed flow of rock, sediment,
vegetation and other materials.
the space (usually measured in degrees)
between two intersecting lines or
surfaces at or close to the point where
they meet.
the down slope movement of material
due to gravity.
Transcribed Image Text:Angle of repose is the maximum slope angle at which given unconsolidated material is stable. a mixed flow of rock, sediment, vegetation and other materials. the space (usually measured in degrees) between two intersecting lines or surfaces at or close to the point where they meet. the down slope movement of material due to gravity.
The very slow, downhill movement of soil
caused by freezing and thawing is called
O creep.
O mudflow.
O inching.
O slump.
Transcribed Image Text:The very slow, downhill movement of soil caused by freezing and thawing is called O creep. O mudflow. O inching. O slump.
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