BÁBEK, Ondřej, Jiří FAIMON, Milan GERŠL and Ondřej ŠRÁČEK. Can the Hranice Abyss, the Deepest Underwater Cave in the World, Really Reach 1 km Depth? A Comment on the Paper by Klanica et al. (2020). JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE. WASHINGTON: AMER GEOPHYSICAL UNION, 2021, vol. 126, No 4, p. 1-5. ISSN 2169-9003. Available from: https://dx.doi.org/10.1029/2020JF005916.
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Basic information
Original name Can the Hranice Abyss, the Deepest Underwater Cave in the World, Really Reach 1 km Depth? A Comment on the Paper by Klanica et al. (2020)
Name in Czech Can the Hranice Abyss, the Deepest Underwater Cave in the World, Really Reach 1 km Depth? A Comment on the Paper by Klanica et al. (2020)
Authors BÁBEK, Ondřej, Jiří FAIMON, Milan GERŠL and Ondřej ŠRÁČEK.
Edition JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, WASHINGTON, AMER GEOPHYSICAL UNION, 2021, 2169-9003.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher United States of America
Confidentiality degree is not subject to a state or trade secret
WWW Journal pages
Impact factor Impact factor: 4.418
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1029/2020JF005916
UT WoS 000645002100024
Keywords (in Czech) Article Comment; Hranice Abyss; geophysical data; epigenic/hypogenic origin; hydrogeochemistry
Keywords in English Article Comment; Hranice Abyss; geophysical data; epigenic/hypogenic origin; hydrogeochemistry
Tags RIV ne
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 17/3/2023 09:13.
Abstract
Based on shallow geophysical data, Klanica et al. (2020, ) argued that the deepest undewater cave in the world, the Hranice Abyss (HA) had formed by epigenic karstification related to mid-Miocene opening of similar to 1 km deep Carpathian Foredeep (CF) and, hence, could be similar to 1 km deep. However, the CF subsided and the abyss was uplifted due to post mid-Miocene faulting with at least 460 m vertical offset, which makes the depth estimate of Klanica et al. (2020, ) invalid. It remains unclear under which geological circumstances the HA, if formed by epigenic karstification, could be backfilled with water column reaching similar to 400 m of height.
Abstract (in Czech)
Based on shallow geophysical data, Klanica et al. (2020, ) argued that the deepest undewater cave in the world, the Hranice Abyss (HA) had formed by epigenic karstification related to mid-Miocene opening of similar to 1 km deep Carpathian Foredeep (CF) and, hence, could be similar to 1 km deep. However, the CF subsided and the abyss was uplifted due to post mid-Miocene faulting with at least 460 m vertical offset, which makes the depth estimate of Klanica et al. (2020, ) invalid. It remains unclear under which geological circumstances the HA, if formed by epigenic karstification, could be backfilled with water column reaching similar to 400 m of height.
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