A canyon
A deep valley with high steep slopes that often has a stream running through it is called a canyon. Canyons are typically formed by the erosion of water over time, creating a distinctive geological feature.
A valley is a stretch of lowland located between hills and mountains formed by erosion. It usually contains a river or stream running through it.
A stream shaped valley is usually 'V' shaped. A glacier formed valley is usually 'U' shaped.
The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, at least with respect of the cross section of the slopes or hillsides. A valley formed by flowing water, or river valley, is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. A valley carved by glaciers, or glacial valley, is normally U-shaped. The valley becomes visible upon the recession of the glacier that forms it.
Contour lines will bend and point upstream to form a "V" shape when crossing a stream valley on a topographic map. The V-shape indicates the direction of the stream flow and shows the gradual slope of the valley.
A valley breeze typically occurs during the daytime when the sun heats up the valley floor, causing air to rise and flow up the valley slopes. This breeze is usually strongest in the afternoon.
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 river running through rock wear it down into deep valley with the steep sides what is it called
The valleys and mountains were very beautiful.
A narrow valley between hills or mountains, with steep rocky walls and possibly a stream running through
A valley is a stretch of lowland located between hills and mountains formed by erosion. It usually contains a river or stream running through it.
Oversteepened slopes are first formed when a stream undercuts a valley wall or waves pound against the base of a cliff.
The space inclosed between ranges of hills or mountains; the strip of land at the bottom of the depressions intersecting a country, including usually the bed of a stream, with frequently broad alluvial plains on one or both sides of the stream. Also used figuratively., The place of meeting of two slopes of a roof, which have their plates running in different directions, and form on the plan a reentrant angle., The depression formed by the meeting of two slopes on a flat roof.
Young Stream or Young River whichever works
Canyon
The address of the Valley Stream Historical Society is: 143 Hendrickson Ave, Valley Stream, NY 11580
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.
Valley.