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A ''Steilhang'' (pl: ''Steilhänge'') is a geoscientific term for a steep mountainside or hillside (or a part thereof), the average slope of which is greater than 1:2 or 30°. Leser defines a ''steilhang'' as a mountainside with an incline of between 16° and 60°, slopes of between 30° and 60° being described as "very steep" (''übersteil'') and anything over 60° being a rock face (''Wand'').〔 The term is German for "steep slope/mountainside/hillside", "escarpment"〔Leser, Hartmut, ed. (2005). ''Wörterbuch Allgemeine Geographie'', 13th ed., dtv, Munich, p. 893. ISBN 978-3-423-03422-7.〕 or "steep face".〔 The word ''Hang'' in this compound may be similar in origin to the English word "hangar" used to mean woods on steep hillsides e.g. for the East Hampshire Hangers. == Geology == The formation of slopes of different gradients depends on the one hand on the type of underlying rock of the mountain or hill - and this may result in slopes varying from those on the other side of a mountain, hill or valley – and on the other hand on its local hardness, and circumstances of its deposition (sedimentation, stratigraphy, bedding or jointing), on its resistance to erosion and not least on the water flow and local climatic conditions. From a geomorphological standpoint, there is a distinction made between ''steilhänge'' not simply on the basis of their gradient and rock type, but especially on their aspect (i.e. their orientation), their rotundity or roughness (small shapes, flexion, steps, terraces, drainage etc.), the vegetation on the mountainsides or hillsides and the soil formation. For example, the soil type known as ''ranker'' gets its name from the word ''Ranker'' which is commonly used in Western Austria to mean ''steilhang''. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Steilhang」の詳細全文を読む スポンサード リンク
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