A glacier-eroded valley will typically have a U-shape with steep sides and a flat bottom, while a stream-eroded valley usually has a V-shape with a narrow channel and wider floodplain. Glacier-eroded valleys are often much larger in scale and can be sculpted by the movement of thick ice over long periods of time, whereas stream-eroded valleys are shaped by the gradual erosion caused by flowing water.
A glaciated mountain valley typically has a U-shaped profile with a broad, flat bottom and steep, straight sides, formed by the movement of glaciers. In contrast, a mountain valley formed through other natural processes, such as erosion from rivers or tectonic activity, may have a V-shaped profile with a narrower bottom and more irregular slopes.
narmada valley is an example of a rift valley
The bottom of a valley is called the valley floor. It is typically the lowest point in the valley and where most of the water and sediment accumulates.
Some examples of valleys around the world include Death Valley in California, USA; Kathmandu Valley in Nepal; and Napa Valley in California, USA. Other well-known valleys include Yosemite Valley in California, USA, and the Rift Valley in East Africa.
You would likely experience a valley breeze, where cooler air from higher elevations flows downhill towards the valley floor during the night and morning. This flow reverses during the day, with warmer air rising up the valley slopes as a valley wind.
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Because it is planned and Houston they just knock down tress to build what they want and the indus valley they had what they wanted!
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Both civilizations were very structured. However, the Tigris and Euphrates were much less predictable than the Nile was and flooding was not as able to be as planned for in the Tigris-Euphrates Valley as it was in the Nile River.
A glaciated mountain valley typically has a U-shaped profile with steep, smooth walls and a flat bottom due to the scouring action of the glacier. In contrast, a mountain valley that was not glaciated usually has a V-shaped profile with more rugged and uneven walls, shaped primarily by flowing water and tectonic forces.
Life in the Chang Jiang Valley was characterized by more stable and predictable flooding from the river, leading to fertile land for agriculture. In contrast, life in the Huang He Valley was marked by unpredictable and devastating floods, which made agriculture more challenging. The Chang Jiang Valley had a milder climate and more diverse crops, while the Huang He Valley had harsher conditions and relied more on flood control and irrigation systems.
By having actors offstage speak the characters' lines
A glaciated mountain valley will likely have a U-shaped profile with a broad, flat floor and steep, often striated walls due to the erosion by the glacier. In contrast, a mountain valley that was not glaciated will typically have a V-shaped profile with a narrower, more gently sloping floor and less steep walls shaped primarily by the natural erosional processes of water and weathering.
The Aryan society didn't move their herds of cattle when they travel ,also they would stop at a place build a civilization unlike the Harappans.
A glaciated mountain valley typically has a U-shaped profile with a broad, flat bottom and steep, straight sides, formed by the movement of glaciers. In contrast, a mountain valley formed through other natural processes, such as erosion from rivers or tectonic activity, may have a V-shaped profile with a narrower bottom and more irregular slopes.