Hypogenic origin of Provalata Cave, Republic of Macedonia: a distinct case of successive thermal carbonic and sulfuric acid speleogenesis

Authors

Marjan Temovski, Graduate School, University of Nova Gorica, Vipavska 13, 5000 Nova Gorica, SloveniaFollow
Philippe Audra, Polytech Nice - Sophia, Engineering School of Nice - Sophia Antipolis University, 930 Route des Colles 06903 Sophia-Antipolis, IMREDD, FranceFollow
Andrej Mihevc, Karst Research Institute ZRC SAZU, Titov trg 2, 6230 Postojna, SloveniaFollow
Jorge E. Spangenberg, Institute of Earth Sciences, University of Lausanne, Géopolis, 1015 Lausanne, SwitzerlandFollow
Victor Polyak, Earth and Planetary Sciences, University of New Mexico, 200 Yale Blvd, Northrop Hall, Albuqueque, NM 87109, USAFollow
William McIntosh, New Mexico Bureau of Geology and Mineral Resources, New Mexico Tech, 801 Leroy Place, Socorro, NM 87801, USAFollow
Jean-Yves Bigot, French Association of KarstologyFollow

Abstract

Provalata Cave (Republic of Macedonia) is a small but remarkable hypogenic cave, developed in Cambrian marbles by successive thermal carbonic and sulfuric acid speleogenesis. The cave has a thick partly corroded calcite crust, abundant gypsum deposits, with cupolas, ceiling and wall channels, feeders and replacement pockets as some of the most characteristic morphological features. Distribution of morphology and deposits suggest a hypogenic origin in two distinct speleogenetic phases: the first by thermal CO₂ rich waters, the second by sulfuric acid dissolution, which were separated by complete infilling of cave passages with pyroclastic-derived clays. In the first phase of speleogenesis, cave passages were formed by dissolution along fractures due to cooling of rising carbonated thermal waters. These phreatic morphologies were later covered with a thick calcite crust deposited in a shallow phreatic environment. In Early Pleistocene the cave was completely filled with clays due to deposition of pyroclastic rocks in a lacustrine environment in the nearby Mariovo Basin. Mariovo Lake sediments were later incised by the Buturica River, which cut down into Cambrian marbles, creating its superimposed valley. Incision lowered the water table and allowed removal of the clay deposits in Provalata Cave. The second phase of speleogenesis started after introduction of H₂S associated with rising thermal waters. Oxidation produced sulfuric acid, which rapidly dissolved first calcite crust, then marble host rock. Condensation-corrosion by sulfuric vapors replaced carbonate rock with gypsum producing replacement pockets as well as second generation of pockets and cupolas. The contact of sulfuric acid with the clay deposits formed alunite, jarosite, and natroalunite. ⁴⁰Ar/³⁹Ar dating gave maximum ages of 1.6 Ma (alunite) and 1.46 Ma (jarosite) for this last stage of speleogenesis, thus making it the second ⁴⁰Ar/³⁹Ar dating of a sulfuric cave in Europe (after Kraushöhle in Austria), and the first dated cave in the Republic of Macedonia.

DOI

http://dx.doi.org/10.5038/1827-806X.42.3.7

Recommended Citation

Temovski, Marjan; Philippe Audra; Andrej Mihevc; Jorge E. Spangenberg; Victor Polyak; William McIntosh; and Jean-Yves Bigot. 2013. Hypogenic origin of Provalata Cave, Republic of Macedonia: a distinct case of successive thermal carbonic and sulfuric acid speleogenesis. International Journal of Speleology, 42: 235-246.
Available at: https://digitalcommons.usf.edu/ijs/vol42/iss3/7