A normal stream's longitudinal profile tends to be convex-upward in shape. (A) Convex-downward B) Concave-downward Concave-upward (D) True Potholes are formed by quarrying. (A) Stream velocity B) Capacity C) Abrasion (D) True

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
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A normal stream's longitudinal profile tends to be convex-upward in shape.
(A) Convex-downward
B) Concave-downward
(c) Concave-upward
(D) True
Potholes are formed by quarrying.
(A) Stream velocity
B) Capacity
C) Abrasion
D) True
Transcribed Image Text:A normal stream's longitudinal profile tends to be convex-upward in shape. (A) Convex-downward B) Concave-downward (c) Concave-upward (D) True Potholes are formed by quarrying. (A) Stream velocity B) Capacity C) Abrasion D) True
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