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2. Tributary stream just downslope from rockfall deposit (Photo C). a. The large sedimentary grains that can be seen in the stream channel are generally less than ~1.5 m in diameter. Judging from the turbulence of the mountain stream, what grain sizes do you expect

2. Tributary stream just downslope from rockfall deposit (Photo C). a. The large sedimentary grains that can be seen in the stream channel are generally less than ~1.5 m in diameter. Judging from the turbulence of the mountain stream, what grain sizes do you expect

Applications and Investigations in Earth Science (9th Edition)
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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2. Tributary stream just downslope from rockfall deposit (Photo C). a. The large sedimentary grains that can be seen in the stream channel are generally less than ~1.5 m in diameter. Judging from the turbulence of the mountain stream, what grain sizes do you expect to be carried (suspended) in the water? b. What grain sizes do you expect to be rolling, sliding, or resting on the bottom of the channel, including those that you can see? c. How would you describe the shape of the sedimentary grains you can see in or near this stream channel (Fig. 6.16B)?
Transcribed Image Text:2. Tributary stream just downslope from rockfall deposit (Photo C). a. The large sedimentary grains that can be seen in the stream channel are generally less than ~1.5 m in diameter. Judging from the turbulence of the mountain stream, what grain sizes do you expect to be carried (suspended) in the water? b. What grain sizes do you expect to be rolling, sliding, or resting on the bottom of the channel, including those that you can see? c. How would you describe the shape of the sedimentary grains you can see in or near this stream channel (Fig. 6.16B)?
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