{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,7,30]],"date-time":"2025-07-30T10:30:52Z","timestamp":1753871452648,"version":"3.41.2"},"reference-count":18,"publisher":"American Geophysical Union (AGU)","issue":"4","license":[{"start":{"date-parts":[[2021,4,4]],"date-time":"2021-04-04T00:00:00Z","timestamp":1617494400000},"content-version":"vor","delay-in-days":3,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":["agupubs.onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["JGR Earth Surface"],"published-print":{"date-parts":[[2021,4]]},"abstract":"<jats:title>Abstract<\/jats:title><jats:p>Based on shallow geophysical data, Klanica et\u00a0al. (2020, <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1029\/2020JF005663\">https:\/\/doi.org\/10.1029\/2020JF005663<\/jats:ext-link>) argued that the deepest undewater cave in the world, the Hranice Abyss (HA) had formed by epigenic karstification related to mid\u2010Miocene opening of \u223c1\u00a0km deep Carpathian Foredeep (CF) and, hence, could be \u223c1\u00a0km deep. However, the CF subsided and the abyss was uplifted due to post mid\u2010Miocene faulting with at least 460\u00a0m vertical offset, which makes the depth estimate of Klanica et\u00a0al. (2020, <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1029\/2020JF005663\">https:\/\/doi.org\/10.1029\/2020JF005663<\/jats:ext-link>) invalid. It remains unclear under which geological circumstances the HA, if formed by epigenic karstification, could be backfilled with water column reaching \u223c400\u00a0m of height.<\/jats:p>","DOI":"10.1029\/2020jf005916","type":"journal-article","created":{"date-parts":[[2021,3,8]],"date-time":"2021-03-08T06:31:02Z","timestamp":1615185062000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":1,"title":["Can the Hranice Abyss, the Deepest Underwater Cave in the World, Really Reach 1\u00a0km Depth? A Comment on the Paper by Klanica et\u00a0al. (2020)"],"prefix":"10.1029","volume":"126","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-4673-3341","authenticated-orcid":false,"given":"O.","family":"B\u00e1bek","sequence":"first","affiliation":[{"name":"Department of Geology Faculty of Science Palacky University  Olomouc Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"J.","family":"Faimon","sequence":"additional","affiliation":[{"name":"Department of Geology Faculty of Science Palacky University  Olomouc Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"M.","family":"Ger\u0161l","sequence":"additional","affiliation":[{"name":"Department of Agricultural, Food and Environmental Engineering Mendel University  Brno Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"O.","family":"Sracek","sequence":"additional","affiliation":[{"name":"Department of Geology Faculty of Science Palacky University  Olomouc Czech Republic"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"13","published-online":{"date-parts":[[2021,4,4]]},"reference":[{"key":"e_1_2_8_2_1","doi-asserted-by":"publisher","DOI":"10.3166\/ga.17.389-400"},{"key":"e_1_2_8_3_1","unstructured":"Brzobohat\u00fd R. &Cicha I.(1993).Carpathian Foredeep. 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