Precipices in the context of "Trango Towers"

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⭐ Core Definition: Precipices

In geography and geology, a cliff or rock face is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs.

An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers.

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Precipices in the context of Llogara National Park

Llogara National Park (Albanian: Parku Kombëtar i Llogarasë/Llogorasë) is a national park centered on the Ceraunian Mountains along the Albanian Riviera in southwestern Albania, spanning a surface area of 1,769 ha (17.69 km). The park's terrain includes large alpine meadows, vertical rock faces, precipices and dense forests. Most area of the park is covered by forests and was established in 1966 to protect several ecosystems and biodiversity of national importance. The International Union for Conservation of Nature (IUCN) has listed the park as Category II. The region has been recognised as an important Bird and Plant Area, supporting significant number of species.

The park features outstanding diversity with the landscape ranging from the alpine peaks of the Ceraunian Mountains covered with snow in winter to the sunny Albanian Ionian Sea Coast in summer. At 1,027 m (3,369 ft), the Llogara Pass provides a striking scenery, with tall mountains overlooking the Albanian Riviera and several islands in the sea. The region experiences a mediterranean climate. This means that the summers are hot and the winters generally dry to warm to cool. Despite the vicinity to the mediterranean climatic region, an alpine climate prevails at the Maja e Çikës. Geomorphologically, carbonate rocks occupy most of the area, while the mountains are composed of limestones and dolomites.

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