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A box canyon is a small canyon that is generally shorter and narrower than a river canyon, with steep walls on three sides, allowing access and egress only through the mouth of the canyon. Box canyons were frequently used in the western United States as convenient corrals, with their entrances fenced.
Diastrophic eustasy is the change in sea level due to variation in capacity of ocean basins, whereas glacio-eustasy is the change in sea level due to withdrawal or return of water into the oceans, due to the accumulation or melting of successive ice sheets. Eustatic rejuvenation relocates the mouth of the stream.
Many archaeological sites have been discovered in the gorge that show that people have been dwelling in the canyon for at least 10,000 years. Prior to the completion of Hales Bar Dam in 1913 and the subsequent raising of the water level, the stretch of the Tennessee River flowing through the gorge was notorious for its navigational hazards, whirlpools, eddies, shoals, and one huge rock.
Niagara Gorge is an 11 km (6.8 mi) long canyon carved by the Niagara River along the Canada–United States border, between the U.S. state of New York and the Canadian province of Ontario. [1] It begins at the base of Niagara Falls and ends downriver at the edge of the geological formation known as the Niagara Escarpment near Queenston, Ontario ...
This is a non-diffusing subcategory of Category:Canyons and gorges of Utah. It includes canyons and gorgess that can also be found in the parent category, or in diffusing subcategories of the parent. This is a container category .