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

佯攻

書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians影響因子(影響力)




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians影響因子(影響力)學(xué)科排名




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians網(wǎng)絡(luò)公開度




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians被引頻次




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians被引頻次學(xué)科排名




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians年度引用




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians年度引用學(xué)科排名




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians讀者反饋




書目名稱Ciomadul (Csomád), The Youngest Volcano in the Carpathians讀者反饋學(xué)科排名

反感

CRASS

Ruth Bars,Csilla Bányász,Laszlo Keviczkyers, even the youngest of them, the Ciomadul (Csomád), last erupted almost 30,000?years ago. Archaeological and historical sources, however, suggest that with its indirect and multifaceted effects, Ciomadul may have influenced the lives of prehistoric people lived in the area. In this chapter we pro

unstable-angina

https://doi.org/10.1007/978-3-031-36825-7s, and finally to the tourism development and utilisation of the natural springs and mofettas in the modern age. The last chapter of our book provides an overview about landscape history and development, and the tourism in the past and present days of this outstanding region of Europe.

燈泡

activity and spa culture) in eight chapters; the second part deals with the palaeo-environmental issues of the larger area, along with human history, in nine chapters..978-3-030-89142-8978-3-030-89140-4

承認(rèn)

Ciomadul (Csomád), The Youngest Volcano in the CarpathiansVolcanism, Palaeoenv

承認(rèn)

ALLAY

Palaeoenvironmental Changes During the Last Glacial Period in the Ciomadul Hillsiduous trees also found refuge. Warming in this area occurred spectacularly earlier than in the North Atlantic region. Plant macrofossil remains preserved in the lake sediment suggest that Scots pine and European larch settled on the crater slope as early as 16,200 years ago, and summer mean tempera

Arb853

Vegetation History and Human Impact in the Ciomadul Area During the Holocenethe anthropogenic pollen indicators. The vegetation history and human impact from the Ciomadul area were reconstructed from two sequences located in the twin craters: Moho? peat bog and Lake Sf. Ana. These provide fossil pollen records which extend from ca. 11,300 BC to the present and represent an

PRO

Prehistory of the Ciomadul Region from the Neolithic to the Late Iron Ageers, even the youngest of them, the Ciomadul (Csomád), last erupted almost 30,000?years ago. Archaeological and historical sources, however, suggest that with its indirect and multifaceted effects, Ciomadul may have influenced the lives of prehistoric people lived in the area. In this chapter we pro