A narrow v-shaped valley
A narrow v-shaped valley
Narrow valley.
mass wasting on the valley sides
A 'V' shaped valley is typically formed by the erosion of a river or stream cutting through elevated land over time. The flowing water carves out the valley by gradually wearing away the surrounding rock and soil, creating steep, sloping sides that converge at the bottom in a V shape.
A Misfit Stream is formed when water melted from the mountains flow into a U-shaped valley. Then because the stream is too small for the valley it is then called a misfit valley.
A stream valley is usually 'V' shaped, formed by erosion from a stream. A glacial valley is usually 'U' shaped, formed by the action of a glacier.
A stream shaped valley is usually 'V' shaped. A glacier formed valley is usually 'U' shaped.
Rapids and numerous whitewater are characteristics of downcutting and a youthful stage of valley evolution. Other characteristics include rough or irregular channels and V-shaped valleys.
Rapids and lots of whitewater
Oversteepened slopes are first formed when a stream undercuts a valley wall or waves pound against the base of a cliff.
The address of the Valley Stream Historical Society is: 143 Hendrickson Ave, Valley Stream, NY 11580
A 'V' shaped valley is formed by streams and water action. A 'U' shaped valley is formed by the gouging out of the valley walls by a glacier. A hanging valley is where side valleys are cut across by the main glacier. Hanging valleys often have waterfalls that fall into the main valley over a cliff.