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The Yungui Plateau is a large mountainous region with rugged terrain including steep karst peaks and deep gorges. [5] The plateau is buttressed by the large Hengduan Mountains to the northwest and by lowland regions to the north, east, and southeast. Other major mountain ranges cross or surround portions of the Yungui Plateau.
[3] The upper valley of the Dordogne is a series of deep gorges. The cliffs, steep banks, fast flowing water and high bridges attract both walkers and drivers. In several places the river is dammed to form long, deep lakes. Camp sites and holiday homes have proliferated wherever the valley floor is wide enough to accommodate them.
Mountains and deep gorges The Genfel is a river of northern Ethiopia . Rising on the foot of the Atsbi horst at 2,253 metres above sea level, it flows southwestward to Giba River which empties finally in the Tekezé River . [ 2 ]
Gooya, Goya or Gòoya is an archaeological site, ancient city and a mountainous valley with many hollows, caves and gorges found in Fika local government area, Yobe State, Nigeria. [ 1 ] [ 2 ] [ 3 ] It is considered one of the tourists attraction sites in Yobe and the deepest gorge valley in Nigeria.
The Grand Canyon, Arizona, at the confluence of the Colorado River and Little Colorado River.. A canyon (from Spanish: cañón; archaic British English spelling: cañon), [1] gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. [2]
Kaaterskill Clove. Kaaterskill Clove is a deep gorge, or valley, in New York's eastern Catskill Mountains, lying just west of the village of Palenville and in Haines Falls. . The clove was formed by Kaaterskill Creek, a tributary of Catskill Creek rising west of North Mountain, and is estimated by geologists to be as much as 1 million years old
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Rio Grande Gorge Bridge. Geologically, the Rio Grande Gorge is a canyon, [1] carved out by erosion over the last several million years. [2] The Rio Grande Gorge and its river follow a topographical low within the larger Rio Grande Rift; a mixture of volcanic activity, shifting tectonic plates, and erosion of layers of gravels and lava yielded the recognizable narrow, deep gorge visible today.
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