{"id":27027,"date":"2021-09-14T14:18:23","date_gmt":"2021-09-14T12:18:23","guid":{"rendered":"https:\/\/pecs.hu\/nyugat-mecsek-karsztjelensegei\/"},"modified":"2022-12-01T09:29:27","modified_gmt":"2022-12-01T08:29:27","slug":"karst-formations-in-western-mecsek","status":"publish","type":"post","link":"https:\/\/pecs.hu\/en\/karst-formations-in-western-mecsek\/","title":{"rendered":"Karst formations in Western Mecsek"},"content":{"rendered":"<section id=\"downloads-block_ad304be0985c0fdc7ae112357476d75f\"class=\"block block-downloads align\" >\n  \n  <div class=\"container-md\">\n          <div class=\"tinymce mb-40px\">\n        <p>The total area of Mecsek mountain range with its varied geological makeup is approximately 500 km<sup>2<\/sup>. It contains rocks from different geological eras from crystalline rocks as old as hundreds of millions of years to calc-tufa still forming today. In the Western part of the mountain, an area of about 50 km<sup>2<\/sup> is suitable for karst formation mostly containing limestone and dolomite, but also containing small amounts of marl variations. Carbonite substrates overlap and border southward the sandstones and aleurites of Jakab-Mountain (Jakab-hegy) providing a large water source to the karst. The resulting alluvium\u2019s abrasive force may play an important role in the formation of caves with flowing streams in Mecsek.<\/p>\n<p>Ponors and sinkholes are typically found at the bottom of North-South ancient valleys. The Mecsek karst region can be divided into the drainage basins of eight karst springs including Tettye-, V\u00edzf\u0151-, K\u0151lyuk-, Paplika (Abaligeti-), and Kispaplika spring, and the M\u00e9lyv\u00f6lgyi-, M\u00e9sz\u00e9get\u0151-, and Melegm\u00e1nyi springs.<\/p>\n<p>The longest cave of the karst region is Abaliget Cave. The total length of the cave is 1750 metres out of which a 500-metre section of the main corridor can be visited by tourists. The minor corridors of the cave can only be accessed by speleologists. The deepest cave of the region is Spiral Hole (Spir\u00e1l-nyel\u0151) that has been excavated up to 96 metres depth reaching the main corridor with a stream at the level of karst water.<\/p>\n<p>The surface of the karst region is characterized by potholes and deep sinkholes of 10-20-30 metres deep. Shorter and longer sections of active cave streams have become known in streams at the foot of the mountain (V\u00edzf\u0151-, Kispaplika-, M\u00e9sz\u00e9get\u0151-, Melegm\u00e1nyi streams) that end in uncharted siphons. Rare formations in the karst region are T\u00f6r\u00f6kpince Sinkhole Cave and the Ak\u00e1cos Hole connected to Abaliget Cave and the syngenetic tufa caverns that formed within Tettye Tufa Cave (Tettyei M\u00e9sztufa Barlang). Mecsek is rich in various ground-level karst formations as well including fully-fledged ponors, sinkholes, or the tufa steps of Melegm\u00e1ny and Nagym\u00e9lyv\u00f6lgy.<\/p>\n\n      <\/div>\n        <div class=\"downloads\">\n                                <a href=\"https:\/\/pecs.hu\/app\/uploads\/2021\/09\/13hat4-term.pdf\" target=\"_blank\" class=\"file\" download>\n            <em class=\"icon-file\"><\/em>\n            <span>\n            <span class=\"filename\">Cultural heritage  &#8211; 4\/2013. (12.06.)<\/span>\n            <span class=\"filesize\">25.7 KB<\/span>\n          <\/span>\n          <\/a>\n                  <\/div>\n  <\/div>\n<\/section>\n\n\n\n<p>Source of photo: <a href=\"https:\/\/magyarmezogazdasag.hu\/\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/magyarmezogazdasag.hu\/<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Source of photo: https:\/\/magyarmezogazdasag.hu\/<\/p>\n","protected":false},"author":13,"featured_media":7470,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[1566,1847,1850],"tags":[1572],"usertype":[52],"class_list":["post-27027","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-our-values-culture-en","category-pecs-values","category-respiratory-of-values","tag-pecsiseg-en","usertype-local","post-variant","post-variant--saffron"],"acf":[],"publishpress_future_action":{"enabled":false,"date":"2026-04-24 04:36:14","action":"change-status","newStatus":"draft","terms":[],"taxonomy":"category","extraData":[]},"publishpress_future_workflow_manual_trigger":{"enabledWorkflows":[]},"_links":{"self":[{"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/posts\/27027","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/users\/13"}],"replies":[{"embeddable":true,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/comments?post=27027"}],"version-history":[{"count":3,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/posts\/27027\/revisions"}],"predecessor-version":[{"id":33201,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/posts\/27027\/revisions\/33201"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/media\/7470"}],"wp:attachment":[{"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/media?parent=27027"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/categories?post=27027"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/tags?post=27027"},{"taxonomy":"usertype","embeddable":true,"href":"https:\/\/pecs.hu\/en\/wp-json\/wp\/v2\/usertype?post=27027"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}