Narrow valley.
A narrow v-shaped valley
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 wide stream valley has gently sloping sides and a broad, flat floor due to erosion over time by a large volume of water. In contrast, a narrow stream valley has steep, V-shaped sides and a narrow floor formed by fast-flowing water cutting through the landscape.
A stream shaped valley is usually 'V' shaped. A glacier formed valley is usually 'U' shaped.
A narrow v-shaped valley
Oversteepened slopes are first formed when a stream undercuts a valley wall or waves pound against the base of a cliff.
Yosemite Valley in California is a well-known example of a v-shaped valley. It was formed by the erosive action of glaciers over thousands of years, resulting in steep valley walls that come together to form a V shape.
A Rift Valley
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.
V-shape
The address of the Valley Stream Historical Society is: 143 Hendrickson Ave, Valley Stream, NY 11580