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According to Merriam-Webster, a ravine is "a small, narrow, steep-sided valley that is larger than a gully and smaller than a canyon and that is usually worn by running water". [1] Some societies and languages do not differentiate between a gully and ravine; in others, there is a distinction, particularly when concerning environmental ...
A crevasse is a deep crack that forms in a glacier or ice sheet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces.
In southern Louisiana the word coulée (also spelled coolie) originally meant a gully or ravine usually dry or intermittent but becoming sizable during rainy weather. As stream channels were dredged or canalized, the term was increasingly applied to perennial streams, generally smaller than bayous. The term is also used for small ditches or ...
Nidd Gorge makes up a section of the River Nidd in North Yorkshire, England, in which the river enters a deep ravine with sheer tree-covered valley sides. The river as a whole flows from its source near Great Whernside in Nidderdale (part of the Yorkshire Dales ), to its confluence with the River Ouse near Nun Monkton .
The river flows to the north before heading west. Rising on the eastern side of the mountains of Gilead, it runs a course of about 105 kilometers (65 mi) in a wild and deep ravine before flowing into the Jordan River between the Sea of Galilee and the Dead Sea, at a point 1,090 meters (3,576 ft) below its origin. [13]
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After this point the river flows to Dikchu through a deep ravine and drops to a height of 550 metres (1,800 ft). Then it cambers and reaches Singtam , which is at a height of 200 metres (660 ft). After Rangpo , the Teesta widens and meets the River Rangeet at Melli Bazaar.
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