Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia | Zendy

Janina Wrzak-Tomic | Zendy; Andrzej Manecki | Zendy

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Hydrothermal phenomena in Risovaca cave and within Vencac massif Shumadies, Serbia

Author(s) -

Janina Wrzak-Tomic,

Andrzej Manecki

Publication year - 2004

Publication title -

journal of the geographical institute jovan cvijic sasa

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 0.16

H-Index - 2

eISSN - 1821-2808

pISSN - 0350-7599

DOI - 10.2298/ijgi0453027w

Subject(s) - karst , cave , massif , geology , hydrothermal circulation , geochemistry , ornaments , earth science , paleontology , archaeology , geography , style (visual arts)

In the Risovaca cave are found, for the karst, atypical alteration in the limestones structure. Also, morphogenesis of the object can not be logically interpret. Those differences are result of hydrothermal process in initial phase of karstic cycle. And then activity of hot water and hot emanations brought up to the metasomatism and destruction of rock, enormous excrete of ornaments and later, ceiling collapse and fill up of cave room

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