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In a typical stream where the gradient is steep the discharge is small.
In a typical stream where the gradient is steep the discharge is small.
In a typical stream where the gradient is steep the discharge is small.
A steep gradient will force the water to flow downhill faster.
The topsoil in a typical soil profile is usually around 2 to 8 inches deep.
A river beginning high up in the mountains will fall sharply until the gradient levels out in the valleys. A river beginning in lower hills will naturally have a less steep gradient over all. Therefore, each river's longitudinal gradient will be different and there is no definitive answer.
Apple Computers (in the beginning)
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
Normally a picture, your age the city/state u live in. It depends on if your talking like on facebook instagram or a private profile