{"id":213,"date":"2026-03-03T20:10:48","date_gmt":"2026-03-03T19:10:48","guid":{"rendered":"https:\/\/www.bchs.sk\/?p=213"},"modified":"2026-03-03T20:10:48","modified_gmt":"2026-03-03T19:10:48","slug":"banictvo-vo-vernari","status":"publish","type":"post","link":"https:\/\/www.bchs.sk\/?p=213","title":{"rendered":"Ban\u00edctvo vo Vern\u00e1ri"},"content":{"rendered":"\n<p class=\"wp-block-paragraph\">O prvopo\u010diatkoch ban\u00edctva v chot\u00e1ri obce nie s\u00fa zachovan\u00e9 \u017eiadne p\u00edsomn\u00e9 doklady. M\u00f4\u017eeme len predpoklada\u0165, \u017ee osada Vern\u00e1r, ktor\u00e1 bola zalo\u017een\u00e1 v r. 1295, bola zalo\u017een\u00e1 pr\u00e1ve kv\u00f4li v\u00fdskytu r\u00fad, tak ako aj \u010fal\u0161ie, dnes u\u017e zaniknut\u00e9 osady v okol\u00ed (Obr.1). Boli to Hincava \u2013 zalo\u017een\u00e1 v r. 1294, Falkenstein (Fal\u0161t\u00edn) v r. 1310 a Borzov zalo\u017een\u00fd v r. 1320. P\u00f4vodne st\u00e1l Vern\u00e1r v doline Mlynn\u00e1.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Na SV svahoch k\u00f3ty Barbolica, v lokalite Studni\u010dky sa nach\u00e1dzaj\u00fa najstar\u0161ie kutacie pr\u00e1ce v \u017eilnom telese dioritu. Boli n\u00e1jden\u00e9 limonitov\u00e9 h\u013euzy, \u017eilky a povlaky spolu s drobn\u00fdmi zrnkami malachitu a azuritu.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">V potoku Mlynn\u00e1 pri ly\u017eiarskom stredisku Studni\u010dky bolo n\u00e1jden\u00fdch nieko\u013eko kusov r\u00f4znych typov trosky z tavby \u017eeleznej rudy. Ako palivo v peciach sa pou\u017e\u00edvalo dreven\u00e9 uhlie. \u010ealej, asi 150 m od bufetu ved\u013ea cesty sa nach\u00e1dza zavalen\u00e9 \u00fastie \u0161t\u00f4lne v ktorej sa \u0165a\u017eili \u017eelezn\u00e9 rudy &#8211; hematit a limonit. Halda je vidite\u013en\u00e1 v \u0161\u00edrke cca 20 m s maxim\u00e1lnou mocnos\u0165ou do 1,5 m.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"> Na lokalite Brestov\u00e1 jama sa nach\u00e1dza pingov\u00e9 pole a mno\u017estvo kutac\u00edch j\u00e1m a r\u00fdh. Z mineraliz\u00e1cie v slabo metamorfovan\u00fdch zlepencoch a pieskovcoch bol zisten\u00fd limonit a hematit.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">V z\u00e1vere doliny Mlynn\u00e1 sa nach\u00e1dzala e\u0161te v 90. rokoch 20. stor. \u0161t\u00f4l\u0148a, ktorej \u00fastie u\u017e s\u00edce bolo zavalen\u00e9, ale vytekala z nej voda. V bl\u00edzkosti tejto \u0161t\u00f4lne sa nach\u00e1dzaj\u00fa e\u0161te \u010fal\u0161ie kutacie pr\u00e1ce men\u0161ieho rozsahu. (Obr.2)<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Na hrebeni k\u00f3ty Skalica sa e\u0161te v 70. rokoch 20. stor. nach\u00e1dzala \u0161achtica rozmerov 1,0 x 1.0 m s nezistenou h\u013abkou. \u0160achtica bola ne\u010faleko od okraja skaln\u00e9ho mas\u00edvu, ktor\u00fd sa zosunul. Hlavn\u00fdm miner\u00e1lom je limonit hnedej a\u017e tehlovo\u010dervenej farby. Na hrebeni sa okrem uvedenej \u0161achtice nach\u00e1dza e\u0161te minim\u00e1lne 8 kutac\u00edch j\u00e1m a jeden objekt obd\u013a\u017enikov\u00e9ho tvaru by mohol by\u0165 ban\u00edcky dom\u010dek, tzv. kr\u00e1m. (Obr.3)<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Na juhov\u00fdchodn\u00fdch svahoch lokality Borzov sa nach\u00e1dza men\u0161ie lo\u017eisko Cu r\u00fad v barytovej, resp. kremennej \u017eilovine. Rudn\u00e9 miner\u00e1ly tvor\u00ed preva\u017ene tetraedrit, chalkopyrit a anhydrit, zo sekund\u00e1rnych miner\u00e1lov je tu malachit, azurit a limonit. Nach\u00e1dzaj\u00fa sa tu v hojnom po\u010dte pingy, kutacie jamy, \u0161achtice s rozr\u00e1\u017ekami (Obr.4) a obrys ban\u00edckeho dom\u010deka.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">V lokalite Nad vajdov\u00fdm jarkom (Pr\u00edslopok) sa nach\u00e1dza doteraz n\u00e1jden\u00e9 najrozsiahlej\u0161ie bansk\u00e9 dielo v katastri obce Vern\u00e1r. Pod\u013ea ve\u013ekosti haldy sa jedn\u00e1 o \u0161t\u00f4l\u0148u s celkovou d\u013a\u017ekou do 500 m, ktor\u00e1 je razen\u00e1 v svetlosiv\u00fdch triasov\u00fdch kremencoch. D\u013a\u017eka pr\u00edstupnej \u010dasti ru\u010dne razenej \u0161t\u00f4lne, tzv. kresanice dosahuje 70 m s prev\u00fd\u0161en\u00edm 5 m. Predmetom \u0165a\u017eby boli ankerit a limonit. (Obr.5 a 6)<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Intenz\u00edvna bansk\u00e1 \u010dinnos\u0165 je vidite\u013en\u00e1 aj na lokalite Potoky. Nach\u00e1dza sa tu ve\u013ek\u00e9 mno\u017estvo kutac\u00edch j\u00e1m a jedna halda na ploche cca 200 m2 (Obr.7), z \u010doho sa d\u00e1 us\u00fadi\u0165, \u017ee sa tu nach\u00e1dza vy\u0161e 150 m chodieb. Hlavn\u00fdm rudn\u00fdm miner\u00e1lom je hematit &#8211; odroda spekularit, pri povrchu limonitizovan\u00fd.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Najvy\u0161\u0161ie n\u00e1jden\u00fdmi bansk\u00fdmi dielami s\u00fa kutacie jamy a pingy tesne pod vrcholom Prednej hole vo v\u00fd\u0161ke 1540 m n.m. Nach\u00e1dza sa tu 8 kruhov\u00fdch kutac\u00edch j\u00e1m, resp. zavalen\u00fdch p\u00edng. Tie\u017e sa tu nach\u00e1dza aj jedna ve\u013emi dobre zachovan\u00e1 pinga rozmerov 1,0 x 2,5 m s h\u013abkou 5,0 m (Obr.8). \u0164a\u017een\u00fdmi miner\u00e1lmi boli spekularit a limonit.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Autor: Slavom\u00edr Kyse\u013ea<\/p>\n","protected":false},"excerpt":{"rendered":"<p>O prvopo\u010diatkoch ban\u00edctva v chot\u00e1ri obce nie s\u00fa zachovan\u00e9 \u017eiadne p\u00edsomn\u00e9 doklady. M\u00f4\u017eeme len predpoklada\u0165, \u017ee osada Vern\u00e1r, ktor\u00e1 bola zalo\u017een\u00e1 v r. 1295, bola zalo\u017een\u00e1 pr\u00e1ve kv\u00f4li v\u00fdskytu r\u00fad, tak ako aj \u010fal\u0161ie, dnes u\u017e zaniknut\u00e9 osady v okol\u00ed (Obr.1). Boli to Hincava \u2013 zalo\u017een\u00e1 v r. 1294, Falkenstein (Fal\u0161t\u00edn) v r. 1310 a <a class=\"read-more\" href=\"https:\/\/www.bchs.sk\/?p=213\">READ MORE<\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-213","post","type-post","status-publish","format-standard","hentry","category-nezaradene"],"_links":{"self":[{"href":"https:\/\/www.bchs.sk\/index.php?rest_route=\/wp\/v2\/posts\/213","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.bchs.sk\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.bchs.sk\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.bchs.sk\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.bchs.sk\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=213"}],"version-history":[{"count":1,"href":"https:\/\/www.bchs.sk\/index.php?rest_route=\/wp\/v2\/posts\/213\/revisions"}],"predecessor-version":[{"id":214,"href":"https:\/\/www.bchs.sk\/index.php?rest_route=\/wp\/v2\/posts\/213\/revisions\/214"}],"wp:attachment":[{"href":"https:\/\/www.bchs.sk\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=213"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.bchs.sk\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=213"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.bchs.sk\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=213"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}