The Velocity
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 landform is the most common result of erosion by flowing water over a long period of time. Water shapes the land by cutting through rock and soil, creating a valley with a stream or river running through it.
The address of the Valley Stream Historical Society is: 143 Hendrickson Ave, Valley Stream, NY 11580
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.
The 'Water of Leith' is the principal stream, and North East Valley Stream joins that at the Gardens. There is also the Kaikorai Stream as well.
I think its a river!
The phone number of the Valley Stream Historical Society is: 516-872-4159.
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.
During a flood, the area of the stream valley that is covered by water is typically the floodplain, which includes the low-lying regions adjacent to the stream or river. This area is designed to absorb excess water when the stream overflows its banks. Additionally, the water may cover parts of the channel and surrounding terrain that are normally dry. Floodwaters can extend further into adjacent areas, depending on the severity of the flood.
Providence is about 180 miles from Valley Stream.
A stream valley typically has a V-shape, while a glacial valley has a U-shape. This difference in shape is due to the different erosional processes involved. Stream valleys are eroded mainly by flowing water, while glacial valleys are shaped by the movement of glaciers that scrape and pluck rock and sediment.
if you're talking about a stream like body its called a fjord.