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Taylor Joyal, Alexander K. Fremier and Jan Boll
In the humid tropics, forest conversion and climate change threaten the hydrological function and stationarity of watersheds, particularly in steep terrain. As climate change intensifies, shifting precipitation patterns and expanding agricultural and pas...
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Yanrong Liu, Guonian Lu, Zhongqiu Meng, Dashu Guo, Di Hu, Lei Zhu and Handong He
A structural landform is defined by its surface morphology, controlled by tectonics, lithology (arrangement and resistance), and folded structures, and demonstrated by the characteristics and relationships between geological and geomorphic elements. It i...
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Vasileios A. Tzanakakis, Aikaterini Pavlaki, Emmanouil Lekkas, Emmanouil A. Varouchakis, Nikolaos V. Paranychianakis, Giorgos Fasarakis and Andreas N. Angelakis
Sfakia is a mountainous municipality located in the southwestern area of the island of Crete, including the southern part of the Lefka Ori Mountain, with an elevation ranging from sea level to over 2400 m. The mountainous massif mainly consists of carbon...
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Guido S. Mariani and Andrea Zerboni
The attention to deep-seated gravitational slope deformations (DSGSDs) has steadily increased in the last few decades, because such features are ubiquitous in mountain areas. Their geomorphological surface expression, especially when related to the effec...
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Grzegorz Wierzbicki, Mateusz Grygoruk, Maria Grodzka-Lukaszewska, Piotr Bartold and Tomasz Okruszko
The advances and retreats of ice sheets during Pleistocene significantly changed high- and mid-latitude landscapes and hydrological systems, albeit differently, in North America and Europe. On the southern margin of the Last Glacial Maximum (LGM) in the ...
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Alessandra Ascione, Sergio Nardò and Stefano Mazzoli
The MS 6.9, 1980 Irpinia earthquake occurred in the southern Apennines, a fold and thrust belt that has been undergoing post-orogenic extension since ca. 400 kyr. The strongly anisotropic structure of fold and thrust belts like the Apennines, including l...
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Jose M. Araos,Jacobus P. Le Roux,Michael R. Kaplan,Matteo Spagnolo
Pág. 357 - 378
The Sierra Baguales Mountain Range, forming the eastern foothills of the Southern Patagonian Andes, has well-developed alpine-glaciated landforms which present an ideal opportunity to study climatic and non-climatic factors that control cirque developmen...
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Marjan Temovski, Balázs Madarász, Zoltán Kern, Ivica Milevski and Zsófia Ruszkiczay-Rüdiger
Although glacial landforms on the Balkan Peninsula have been studied since the 19th century, only scarce data are available about the extent of the former glaciations in the Central Balkan Peninsula, the transition zone between the Mediterranean and Cent...
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Aditya Saputra, Christopher Gomez, Ioannis Delikostidis, Peyman Zawar-Reza, Danang Sri Hadmoko, Junun Sartohadi and Muhammad Anggri Setiawan
Located approximately a hundred kilometres north of Java Subduction Zone, Java Island has a complicated geology and geomorphology. The north zone is dominated by the folded area, the centre is dominated by the active volcanic arc and the south of Java in...
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