A stream widens its valley primarily through the processes of erosion and sediment transport. As water flows, it erodes the banks and bed of the stream, particularly during periods of high flow or flooding, which increases its lateral and vertical dimensions. This erosion is often enhanced by the composition of the surrounding materials, as softer rocks and soils are more easily worn away. Over time, the continuous action of water reshapes the valley, creating a wider and often more U-shaped profile.
a stream is most likely widen by erosion
The address of the Valley Stream Historical Society is: 143 Hendrickson Ave, Valley Stream, NY 11580
The stream valley will likely have a V-shaped profile characterized by steep sides and a narrow channel due to the primary work of downward erosion cutting towards base level. This shape results from the stream's ability to efficiently remove material through hydraulic action, abrasion, and corrosion. As the stream continues to erode downwards, the valley may deepen and widen over time.
A stream valley forms through the process of erosion, where flowing water carves out the landscape, creating a channel and shaping the surrounding terrain. The depth of downcutting depends on factors such as the stream's velocity, sediment load, and the geology of the area; streams in soft rock may create deeper valleys than those in harder rock. Over time, the valley may widen and evolve through various processes, including lateral erosion and sediment deposition. Ultimately, the depth and profile of a stream valley can vary significantly based on these environmental factors.
The phone number of the Valley Stream Historical Society is: 516-872-4159.
Providence is about 180 miles from Valley Stream.
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 shaped valley is usually 'V' shaped. A glacier formed valley is usually 'U' shaped.
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.
No, Valley Stream is not in any of the five boroughs. Valley Stream is a village in Nassau County, on Long Island, New York. However, Nassau County borders the New York City borough/county of Queens on its east side, and Valley Stream is located right next to the Queens/Nassau border. So Valley Stream is almost in Queens, but not quite.
Young Stream or Young River whichever works
Narrow valley.