Titlebook: Glaciokarsts; Márton Veress,Tamás Telbisz,Jaroslav M. Gutak Book 2019 Springer Nature Switzerland AG 2019 Glaciokarst.Karstification.Glaci

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書目名稱Glaciokarsts影響因子(影響力)




書目名稱Glaciokarsts影響因子(影響力)學(xué)科排名




書目名稱Glaciokarsts網(wǎng)絡(luò)公開度




書目名稱Glaciokarsts網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Glaciokarsts被引頻次




書目名稱Glaciokarsts被引頻次學(xué)科排名




書目名稱Glaciokarsts年度引用




書目名稱Glaciokarsts年度引用學(xué)科排名




書目名稱Glaciokarsts讀者反饋




書目名稱Glaciokarsts讀者反饋學(xué)科排名

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終端

https://doi.org/10.1007/978-3-658-43236-2morphic action of glaciers is discussed with a focus on karst. On karst, glacial erosion is characteristic in karst depressions, in stratified limestone, as well as in troughs which developed on similar rocks. As regards depressions, the denudation of slopes the inclination of which is identical wit

Oligarchy

Just Give Me Narcan and Let Me Got terrains, and the deepest caves are almost all found in glaciokarsts. On the other hand, as for the volume of cave chambers and passage dimensions, glaciokarst caves are not among the largest ones. One of the most important questions about glaciokarst speleogenesis is whether subglacial cave devel

發(fā)牢騷

Health Disparities in Allergic Diseasesn. The recent karstification and pattern of the areas of former cirque glaciers, valley glaciers, ice caps, ice sheets and piedmont glaciers are presented. The recent karstic pattern and development of the karst of glaciokarst types (plateau glaciokarst, semi-plateau glaciokarst, mountain glaciokars

花束

Optimal Health Insurance Contracts, concealed karst and allogenic karst, then in light of them, the landscape evolution in the area of various glacial erosional surfaces and landforms will be outlined. The future geomorphic evolution of glacial erosional surfaces are also touched upon.

花束

Health Economics from Theory to Practicees deal with the sample sites of the Alps (Northern Calcareous Alps, Julian Alps and Bernese Alps). One area is situated in the Durmitor (Dinarides), while the fifth area is a special site. It is a subarctic karst in the southern part of Patagonia developing under extreme climatic circumstances.

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