首页> 外文OA文献 >Contribution a la connaissance des vallons élémentaires du nord de la France : l'exemple de la Creuse des Fosses ( Authieule, plateau picard) Contribution to the knowledge of the elementary valleys of the north of France : the example of the Creuse des Fosses (Authieule, plateau picard )
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Contribution a la connaissance des vallons élémentaires du nord de la France : l'exemple de la Creuse des Fosses ( Authieule, plateau picard) Contribution to the knowledge of the elementary valleys of the north of France : the example of the Creuse des Fosses (Authieule, plateau picard )

机译:对法国北部基本山谷的知识的贡献:以弗雷塞斯(Creuse des Fosses)为例(对法国北部基本山谷的知识的贡献:以弗雷塞斯(Creuse des Fosses)为例。 Authieule,皮卡德高原)

摘要

The survey deals with the morphodynamic evolution of a creuse. It is a ravine-like landform of kilometnc length that often cut the bottom of the small elementary valleys incised into the chalky plateaus of the Artois and Picardy. The morphosedimentary analysis takes into account the data (stratigraphy, micromorphological analysis) of 3 cross-sections distributed along a 500 m section and replaced in their geomorphological context (cartography based on a DTM, longitudinal profile). The recognition of characteristic deposits (bedded loess, palaeosol) and of medieval artefacts allows to set a chronology of the events since 30 000 BP Stratigraphie and landform analyses demonstrate the fluvial character of the creuse. Two main phases of incision, locally associated to a sinuous channel pattern, are described. Phases of infilling, probably of medieval age for the last one, correspond to episodic and violent floods of torrential type. Valley sides play an important role, delivering in abundance loess that infilled the creuse in present time.
机译:该调查研究了皱纹的形态动力学演变。这是一条长达千米的沟壑状地形,经常切开切入阿尔托瓦斯和皮卡第白垩高原的小基本河谷的底部。形态沉积分析考虑了沿500 m剖面分布并在其地貌背景下被替换的3个剖面的数据(地层学,微观形态分析)(基于DTM的制图,纵向剖面)。自3万个BP地层学以来,对特征性沉积物(层状黄土,古土壤)和中世纪人工制品的认识使得能够确定事件的年代顺序,而地形分析证明了该皱纹的河流特征。描述了切口的两个主要阶段,其局部地与弯曲的通道模式相关。填充阶段可能是中世纪的最后阶段,对应于洪流式的暴发性洪水。山谷两侧起着重要的作用,提供了丰富的黄土,填补了当前的皱纹。

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