{"title":"关于l’hydrogéomorphologie anthropisation密集型城市空间的网站:Nı̂my更新世(Languedoc)法国大于古代;撞击后","authors":"Guilhem Fabre , Martial Monteil","doi":"10.1016/S1251-8050(01)01664-0","DOIUrl":null,"url":null,"abstract":"<div><p>Hydrogeomorphological, archaeological and geohistorical integrated studies of the very urbanised Nı̂mes area attest of piedmont slopes and torrential alluvial fan existence from the beginning of digging of the Vistre valley since the end of the ancient Pleistocene. The urbanisation is situated on top of a major superior Pleistocene–Holocene alluvial fan. This fan existed during the old Antiquity, and has been widely truncated by the anthropisation during the High Empire. This fan is connected to other little ones, and becomes a colluvial–alluvial fan landform connected to the present flood plain of the Vistre River. It is still functioning now, as during the recent flash flood disaster of 3 October 1988.</p></div>","PeriodicalId":100301,"journal":{"name":"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science","volume":"333 8","pages":"Pages 435-440"},"PeriodicalIF":0.0000,"publicationDate":"2001-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1251-8050(01)01664-0","citationCount":"3","resultStr":"{\"title\":\"Sur l'hydrogéomorphologie d'un espace à forte anthropisation urbaine : le site de Nı̂mes (Languedoc, France) du Pléistocène supérieur à l'Antiquité ; impacts postérieurs\",\"authors\":\"Guilhem Fabre , Martial Monteil\",\"doi\":\"10.1016/S1251-8050(01)01664-0\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Hydrogeomorphological, archaeological and geohistorical integrated studies of the very urbanised Nı̂mes area attest of piedmont slopes and torrential alluvial fan existence from the beginning of digging of the Vistre valley since the end of the ancient Pleistocene. The urbanisation is situated on top of a major superior Pleistocene–Holocene alluvial fan. This fan existed during the old Antiquity, and has been widely truncated by the anthropisation during the High Empire. This fan is connected to other little ones, and becomes a colluvial–alluvial fan landform connected to the present flood plain of the Vistre River. It is still functioning now, as during the recent flash flood disaster of 3 October 1988.</p></div>\",\"PeriodicalId\":100301,\"journal\":{\"name\":\"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science\",\"volume\":\"333 8\",\"pages\":\"Pages 435-440\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-10-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1251-8050(01)01664-0\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1251805001016640\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1251805001016640","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Sur l'hydrogéomorphologie d'un espace à forte anthropisation urbaine : le site de Nı̂mes (Languedoc, France) du Pléistocène supérieur à l'Antiquité ; impacts postérieurs
Hydrogeomorphological, archaeological and geohistorical integrated studies of the very urbanised Nı̂mes area attest of piedmont slopes and torrential alluvial fan existence from the beginning of digging of the Vistre valley since the end of the ancient Pleistocene. The urbanisation is situated on top of a major superior Pleistocene–Holocene alluvial fan. This fan existed during the old Antiquity, and has been widely truncated by the anthropisation during the High Empire. This fan is connected to other little ones, and becomes a colluvial–alluvial fan landform connected to the present flood plain of the Vistre River. It is still functioning now, as during the recent flash flood disaster of 3 October 1988.
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