in the following table to summarize the characteristics of sediment deposited by the transporting agents listed. Agent of transportation Textural feature Streams Wind Glaciers Grain size Sorting Grain shape

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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6.5 INTERPRETING CLASTIC SEDIMENTARY TEXTU
EXERCISE 6.7
Recognizing Sediment Deposited by Streams, Wind, and Glaciers
Name:
Section:
Course:
Date:
Fill in the following table to summarize the characteristics of sediment deposited by the transporting agents listed.
Agent of transportation
Textural feature
Streams
Wind
Glaciers
Grain size
Sorting
Grain shape
called sediment maturity: the degree to which a sediment has changed during tran
portation and deposition. The changes it can undergo include changes in gra
size and shape by the physical processes described above as well as the loss of casi
Transcribed Image Text:6.5 INTERPRETING CLASTIC SEDIMENTARY TEXTU EXERCISE 6.7 Recognizing Sediment Deposited by Streams, Wind, and Glaciers Name: Section: Course: Date: Fill in the following table to summarize the characteristics of sediment deposited by the transporting agents listed. Agent of transportation Textural feature Streams Wind Glaciers Grain size Sorting Grain shape called sediment maturity: the degree to which a sediment has changed during tran portation and deposition. The changes it can undergo include changes in gra size and shape by the physical processes described above as well as the loss of casi
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