Himalaya

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Contesto di Himalaya

L'Himalaya (AFI: /iˈmalaja/ o, meno precisamente, /imaˈlaja/; in sanscrito हिमालय [ɦɪˈmɑːlɐjɐ], "dimora delle nevi", dall'unione di hima, "neve", e ālaia, "dimora"), adattato talvolta in italiano come Imalaia, è un sistema montuoso dell'Asia meridionale, che si innalza a settentrione del bassopiano indo-gangetico e a meridione dell'altopiano del Tibet, e che forma un gigantesco arco diretto da nord-ovest a sud-est con la convessità rivolta a sud e compreso all'incirca tra 73° e 95° di long. e...Leggi tutto

L'Himalaya (AFI: /iˈmalaja/ o, meno precisamente, /imaˈlaja/; in sanscrito हिमालय [ɦɪˈmɑːlɐjɐ], "dimora delle nevi", dall'unione di hima, "neve", e ālaia, "dimora"), adattato talvolta in italiano come Imalaia, è un sistema montuoso dell'Asia meridionale, che si innalza a settentrione del bassopiano indo-gangetico e a meridione dell'altopiano del Tibet, e che forma un gigantesco arco diretto da nord-ovest a sud-est con la convessità rivolta a sud e compreso all'incirca tra 73° e 95° di long. est e 27° e 36° di lat. nord.

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