What is wind gap ?

Mayank Mishra

A wind gap is a geographic feature that occurs when a river or stream changes its course or cuts through a mountain range, leaving a narrow gap or pass between two mountainous areas. It is typically formed by the erosive action of a river that gradually erodes the land and cuts through the rock layers, creating a gap. Wind gaps are also known as dry valleys. They are shallow notches in the crest of a mountain ridge. Wind gaps are different from water gaps, which are similar features but still contain a waterway. Water gaps and wind gaps often provide routes that are suitable for trails, roads, and railroads through mountainous terrain. Some examples of wind gaps are the Cumberland Gap in the Appalachian Mountains of the United States, the Thal Ghat in the Western Ghats of India, and the Brenner Pass in the Alps of Europe. Source: (1) The phenomena of wind gap is associated with: - Testbook.com. https://testbook.com/question-answer/the-phenomena-of-wind-gap-is-associated-with--61f01f008494db74e48f79c8. (2) . https://bing.com/search?q=wind+gap+in+earth+science. (3) Wind gap | geology | Britannica. https://www.britannica.com/science/wind-gap. (4) Climate - Wind Patterns, Air Pressure, Jet Streams | Britannica. https://www.britannica.com/science/climate-meteorology/Wind. (5) undefined. https://en.wikipedia.org/wiki/Wind_gap. (6) undefined. https://www.britannica.com/science/wind. (7) undefined. https://courses.lumenlearning.com/earthscienceck12/chapter/wind-erosion-and-deposition/.