Titlebook: Ciomadul (Csomád), The Youngest Volcano in the Carpathians; Volcanism, Palaeoenv Dávid Karátson,Daniel Veres,Ulrich Hambach Book 2022 The E

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Hydroclimate Variability and Pollution History of the Moho? Peatbogomposition of peat layers, we can infer the paleoenvironmental conditions recorded in the bog, such as the input of atmospheric dust, providing important information about prevailing wind changes and other climatic changes through time. The Moho? bog dust record clearly captures the formation of the

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脫水

The Palaeolithic in the Karst Area of Varghi? (Vargyas) Gorgesndard geochronometers are ambiguous. An example of this are the caves in the Varghi? (Vargyas) Gorges, close to the volcanic massif of Ciomadul (Csomád) where human presence has been documented since the Middle Palaeolithic. Here, the chronology offered by tephra occurrences can be corroborated with

Magnificent

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genuine

Landscape History, Land Use, and Tourism of the Ciomadul–Balvanyos Regionring settlements; L?z?re?ti (Lázárfalva), Tu?nad (Tusnád), B?ile Tu?nad (Tusnádfürd?), Bixad (Sepsibükszád) and Turia (Torja), which are all related to the range of hills dominating the region, but which had been developed and managed independently. The region has a rich heritage of local, national

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https://doi.org/10.1007/978-3-030-89140-4Quaternary volcanoes; Carpathian-Pannonian region; Andscape evolution; St; Ana crater; lava domes; Calima

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978-3-030-89142-8The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl

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