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4. The picture below shows a river in Washington discharging to the ocean in a hyperpycnal state, which means the density of the fluid travelling through the channel is greater than that of sea water due to very high suspended sediment concentrations. The density of a debris flow travelling in a channel can be even higher, in some cases approaching that of sediment. Explain how the size of grains entrained from the bed of a channel would be different under flow conditions ranging from just water, to hyperpycnal flow, to debris flow.

4. The picture below shows a river in Washington discharging to the ocean in a hyperpycnal state, which means the density of the fluid travelling through the channel is greater than that of sea water due to very high suspended sediment concentrations. The density of a debris flow travelling in a channel can be even higher, in some cases approaching that of sediment. Explain how the size of grains entrained from the bed of a channel would be different under flow conditions ranging from just water, to hyperpycnal flow, to debris flow.

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
Problem 1LR
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4. The picture below shows a river in Washington discharging to the ocean in a hyperpycnal state, which means the density of the fluid travelling through the channel is greater than that of sea water due to very high suspended sediment concentrations. The density of a debris flow travelling in a channel can be even higher, in some cases approaching that of sediment. Explain how the size of grains entrained from the bed of a channel would be different under flow conditions ranging from just water, to hyperpycnal flow, to debris flow.
Transcribed Image Text:4. The picture below shows a river in Washington discharging to the ocean in a hyperpycnal state, which means the density of the fluid travelling through the channel is greater than that of sea water due to very high suspended sediment concentrations. The density of a debris flow travelling in a channel can be even higher, in some cases approaching that of sediment. Explain how the size of grains entrained from the bed of a channel would be different under flow conditions ranging from just water, to hyperpycnal flow, to debris flow.
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