翻訳と辞書 Words near each other ・ Neomordellistena lestradei ・ Neomordellistena maculipennis ・ Neomordellistena notatipennis ・ Neomordellistena palpalis ・ Neomordellistena parvula ・ Neomordellistena picicolor ・ Neomordellistena roeri ・ Neomordellistena ruficeps ・ Neomordellistena rufopygidialis ・ Neomordellistena suturalis ・ Neomordellistena testacea ・ Neolithic long house ・ Neolithic Revolution ・ Neolithic signs in China ・ Neolithic sites in Kosovo ・ Neolithic Subpluvial ・ Neolithic Tibet ・ Neolithic tomb ・ Neolithocolletis ・ Neolithocolletis hikomonticola ・ Neolithocolletis kangarensis ・ Neolithocolletis mayumbe ・ Neolithocolletis nsengai ・ Neolithocolletis pentadesma ・ Neolithodes grimaldii ・ Neolitsea ・ Neolitsea aciculata ・ Neolitsea australiensis ・ Neolitsea cassia ・ Neolitsea daibuensis Dictionary Lists mini英和辞書 mini和英辞書 Webster 1913 Latin-English FOLDOC Wikipedia English ウィキペディア

翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Neolithic Subpluvial ： ウィキペディア英語版 Neolithic Subpluvial The Neolithic Subpluvial, or the Holocene Wet Phase, was an extended period (from about 7500–7000 BCE to about 3500–3000 BCE) of wet and rainy conditions in the climate history of northern Africa. It was both preceded and followed by much drier periods. The Neolithic Subpluvial was the most recent of a number of periods of "Wet Sahara" or "Green Sahara", during which the Sahara region was much more moist and supported a richer biota and human population than the present-day desert. == Date ranges == The Neolithic Subpluvial began during the 7th millennium BC and was strong for about 2,000 years; it waned over time and ended after the 5.9 kiloyear event (3900 BCE). Then the drier conditions that prevailed prior to the Neolithic Subpluvial returned; desertification advanced, and the Sahara Desert formed (or re-formed). Arid conditions have continued through to the present day.〔Sources differ on specific date ranges, which necessarily varied over such a wide geographic expanse. One (Bard, Kathryn A. (1999), ed. ''Encyclopedia of the Archaeology of Ancient Egypt.'' London, Routledge, pg 863) gives "9000–5000 BP," or 7000–3000 BCE, for the duration of the subpluvial. Another (Wilkinson, Toby A. H. (1999), ''Early Dynastic Egypt.'' London, Routledge, pg 372) places the end of the subpluvial c. 3300 BCE.〕 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「Neolithic Subpluvial」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.