Mountain Streams and V-Shaped Valleys

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12 Questions

How is discharge calculated?

By multiplying the cross-sectional area of the stream by its average velocity

What happens to the velocity if the cross-sectional area of a stream increases?

Velocity decreases

What are floodplains?

Flat areas adjacent to river channels that are occasionally flooded

How are oxbow lakes formed?

When a meander loop is cut off from the main channel

What is a drainage basin?

The entire land area that contributes water to a specific stream or river system

What does recurrence interval refer to in relation to floods?

The average time between floods of a certain magnitude

What is one factor contributing to the formation of deep, V-shaped valleys in mountain streams?

Limited vegetation exposing rock to erosive force

What does the angle of repose refer to in relation to loose material on a slope?

The steepest angle without material collapsing

What happens to the gradient (slope) of a stream as it flows downstream?

It decreases, resulting in a slower flow rate

How does the channel width change as a stream flows downstream?

It increases as downcutting decreases and flow rate slows

What is lateral erosion in the context of stream dynamics?

Erosion that widens the valley by removing material from its sides

How does limited vegetation at high altitudes impact stream dynamics?

It minimizes soil stabilization and exposes rock to erosive forces

Learn about the factors that contribute to the formation of V-shaped valleys by mountain streams, including steep gradient, downcutting, limited vegetation, and weathering. Understand how these processes shape the landscape in mountainous regions.

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