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
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
Section: Chapter Questions
Problem 1LR
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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](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F40f53177-3384-4137-b434-2de94c9c5cd4%2F2c95bc9c-62b4-461b-95db-c1fcc29d9a98%2Fgre6hx_processed.png&w=3840&q=75)
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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