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Geomorphologie-Relief Processus Environnement最新文献

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Le paléoenvironnement de l’Escaut moyen sur le site de Kerkhove Stuw (Flandre Occidentale, Belgique) au cours de l’Holocène inférieure 全新世晚期Kerkhove Stuw遗址(比利时西佛兰德斯)中scheldt古环境
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-12-30 DOI: 10.4000/geomorphologie.15954
F. Cruz, Annelies Storme, L. Allemeersch, Joris Sergant, Hans Vandendriessche, Kim Aluwé, Mathieu Boudin, Jari Mikkelsen, P. Crombé
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引用次数: 2
Un géomorphologue lettré : Jean-Jacques DUFAURE (1932-2020) - De la néotectonique à la géoarchéologie et à la géomorphologie humaine 一位受过教育的地貌学家:Jean-Jacques DUFAURE(1932-2020)——从新构造学到地质考古学和人类地貌学
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-12-30 DOI: 10.4000/geomorphologie.16057
Christian Giusti, Bruno Comentale, É. Fouache, L. Lespez, Michel Rasse, Jean-Pierre Peulvast, M. Calvet, Marie-Françoise André
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引用次数: 0
Hommage collectif à Jean Nicod (1923-2021) 向Jean Nicod致敬(1923-2021)
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-12-30 DOI: 10.4000/geomorphologie.16050
A. Marre, J. Delannoy
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引用次数: 0
Altération hydrogéomorphologique et qualité écologique de trois petites rivières périurbaines de la métropole parisienne 巴黎郊区三条小河的水文地貌变化和生态质量
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-10-26 DOI: 10.4000/geomorphologie.15739
Lucile de Milleville, F. Gob, É. Tales, L. Lespez
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引用次数: 1
The unique topography from Obanul Mare (Mangalia, SE Romania): remnant of a maze cave 奥巴努尔海(罗马尼亚东南部曼加利亚)的独特地形:迷宫洞穴的遗迹
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-10-26 DOI: 10.4000/geomorphologie.15794
V. Drăgușin, L. Tîrlă, S. Covaliov, N. Cruceru, I. Mirea, I. Şandric
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引用次数: 1
Geochemical studies and lacustrine geomorphology of Lake Yakhi basin in eastern Mongolia 蒙古东部雅基湖盆地地球化学与湖泊地貌研究
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-10-26 DOI: 10.4000/geomorphologie.15873
A. Orkhonselenge, Odmaa Bulgan
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引用次数: 0
Évolution historique contemporaine de l’ensablement de la plateforme d’érosion du littoral à falaises de Seine-Maritime 塞纳河海崖海岸侵蚀平台淤积的当代历史演变
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-10-26 DOI: 10.4000/geomorphologie.15684
Bastien Peuziat, S. Costa, B. Tessier
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引用次数: 0
Scotland’s Mountain Landscapes. A geomorphological perspective 苏格兰的山地景观。地貌学的观点
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-06-30 DOI: 10.4000/geomorphologie.15505
D. Mercier
Colin Kerr Ballantyne, professeur emerite de geographie physique a l’Universite de St‑Andrews et fin connaisseur de l’Ecosse, propose un ouvrage de geomorphologie a mi-chemin entre la vulgarisation grand public et les articles scientifiques de tres haut niveau dont il est coutumier. Il vient utilement completer la bibliotheque des passionnes des milieux froids et des amoureux de l’Ecosse, dans laquelle l’ouvrage de 1967 The evolution of Scotland’s Scenery de Brian Sissons, recemment decede, t...
圣安德鲁斯大学(St Andrews university)自然地理学名誉教授、苏格兰专家科林·克尔·巴兰坦(Colin Kerr Ballantyne)提出了一本地形学著作,介于大众通俗读物和他所习惯的高水平科学文章之间。它有效地补充了寒冷环境的爱好者和苏格兰爱好者的图书馆,其中布莱恩·西森(Brian Sissons) 1967年出版的《苏格兰风景的演变》(The evolution of Scotland’s Scenery)最近去世。
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引用次数: 0
Hommage collectif - Yvette DEWOLF – une géomorphologue de terrain passionnée 集体致敬- Yvette DEWOLF -一个充满激情的地形地貌学家
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-06-30 DOI: 10.4000/geomorphologie.15588
M. Fort, Marie-Françoise André, Mekki Ben Salem, G. Bourrié, Y. Callot, J. Coutard, Françoise Duraffour, Mustapha El Hannani, B. Deffontaines, Charles Le Cœur, Eliane Leterrier, Cl. Martin, Mario Panizza, A. Simonin, A. Taïbi, E. Verrecchia
Monique Fort (Pr. Emerite, Universite de Paris, UMR 8586 PRODIG CNRS) Yvette Dewolf nous a quittes le 5 avril 2021. Nee en 1928, elle debuta sa carriere a l’Universite de Caen dans l’equipe d’Andre Journaux, et elle s’investit tres vite au Centre de Geomorphologie ou elle participa, entre autres avec Jean-Pierre Lautridou et Jean-Pierre Coutard, aux experiences sur les milieux periglaciaires et la cryoclastie. Nommee a Paris en 1965, elle co-dirigea, avec F. Durand-Dastes et sous la Direction...
Monique Fort(名誉教授,巴黎大学,UMR 8586 PRODIG CNRS) Yvette Dewolf于2021年4月5日去世。她出生于1928年,在andre期刊的团队中开始了她的职业生涯,并很快进入地貌中心,在那里她与Jean-Pierre Lautridou和Jean-Pierre Coutard一起参与了冰周围环境和低温裂化的实验。1965年,她被任命到巴黎,与F. Durand-Dastes共同指导……
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引用次数: 0
Geoarchaeology of the middle Herault valley (southern France) since the Bronze Age: cartographic approach 青铜器时代以来埃罗河谷中部(法国南部)的地理考古学:制图方法
IF 0.6 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Pub Date : 2021-06-30 DOI: 10.4000/geomorphologie.15510
Ambrine Bouchène, Benoît Devillers
While the concept of the Anthropocene is still debated, it seems crucial to deepen our knowledge of the interactions taking place between human societies and their environment. Occupied for at least the Bronze Age, the middle Herault valley offers a territory suitable for the analysis of these interactions thanks to the wealth of archaeological data uncovered and their proximity to river activity. In order to do this, we determined the nature of the hydromorphological evolution of the Herault River and their impact on the fluvial landscape, through a comparative analysis of the cartographic data, making it possible to identify the morphogenic capacities of the river. By crossing the results of geomorphological, hydromorphometric, palaeogeographic and archaeological analysis, we were able to define three sections in the floodplain, each characterised by its own dynamics. The first section is distinguished by the flow of the river in a deep channel and the poor development of the Holocene terrace. The palaeogeographic analysis revealed a relative conservation of the fluvial hydrography. Consequently, on this section, the hydrological functioning of the river has little impact on the evolution of the alluvial landscape. The second section particularly stood out from the rest of the valley following the analysis of the hydromorphometric data. The frequency and amplitude of the meanders on this section is 3.7 times greater than the average observed over the entire middle valley. Consequently, the fluvial landscape of this section is characterized by a greater instability. Finally, the third section was characterised by the narrowing of the channel, a decrease in its depth and a vast expansion of the Holocene terrace, reflecting a strong dynamic of alluviation.
虽然人类世的概念仍有争议,但加深我们对人类社会与其环境之间相互作用的了解似乎至关重要。埃罗河谷中部至少在青铜时代就被占领了,由于发现了丰富的考古数据,而且靠近河流活动,因此它提供了一个适合分析这些相互作用的领域。为了做到这一点,我们确定了埃罗特河的水文形态演变的性质及其对河流景观的影响,通过对地图数据的比较分析,使确定河流的形态形成能力成为可能。通过综合地貌学、水文形态测量学、古地理和考古分析的结果,我们确定了洪泛区的三个部分,每个部分都有自己的动态特征。第一部分的特点是河道较深,全新世阶地发育较差。古地理分析揭示了河流水文的相对保存。因此,在这一段,河流的水文功能对冲积景观的演变影响不大。在对水文形态测量数据进行分析后,第二部分在山谷的其他部分中尤为突出。这一段曲流的频率和幅度是整个中部山谷平均值的3.7倍。因此,这一段的河流景观具有较大的不稳定性。最后,第三段的特点是河道变窄,深度减少,全新世阶地大面积扩张,反映出强烈的冲积动力。
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引用次数: 0
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Geomorphologie-Relief Processus Environnement
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