. . "Rypl, Ji\u0159\u00ED" . "1"^^ . . . . "1"^^ . . "7"^^ . . "12410" . . "[D39AA6F34586]" . . "\u017Dof\u00EDnsk\u00E1 hornatina je geomorfologick\u00FDm okrskem Poho\u0159sk\u00E9 hornatiny, kter\u00E1 je geomorfologick\u00FDm podcelkem Novohradsk\u00FDch hor. \u017Dof\u00EDnsk\u00E1 hornatina se nach\u00E1z\u00ED ve v\u00FDchodn\u00ED \u010D\u00E1sti Novohradsk\u00FDch hor. Nejzaj\u00EDmav\u011Bj\u0161\u00ED lokality jsou situov\u00E1ny na severu p\u0159i hranici se Stropnickou pahorkatinou. Mezi nejzaj\u00EDmav\u011Bj\u0161\u00ED geomorfologick\u00E9 lokality pat\u0159\u00ED Krav\u00ED hora, Kun\u00ED hora a Vysok\u00E1. Tyto lokality jsou odd\u011Bleny od Stropnick\u00E9 pahorkatiny 300 metr\u016F vysok\u00FDm tektonick\u00FDm svahem a vytv\u00E1\u0159\u00ED vysok\u00E9 exfolia\u010Dn\u00ED klenby. N\u00EDzk\u00E9 exfolia\u010Dn\u00ED klenby se tak\u00E9 vyskytuj\u00ED na svaz\u00EDch. Mrazov\u00E9 zv\u011Btr\u00E1v\u00E1n\u00ED b\u011Bhem Pleistocenu m\u011Blo velk\u00FD vliv na formov\u00E1n\u00ED mezoforem reli\u00E9fu. Jednotliv\u00E9 periglaci\u00E1ln\u00ED formy reli\u00E9fu (nap\u0159. Napoleonova hlava) pat\u0159\u00ED mezi nejzaj\u00EDmav\u011Bj\u0161\u00ED a nejd\u016Fle\u017Eit\u011Bj\u0161\u00ED formy reli\u00E9fu v t\u00E9to \u010D\u00E1sti Novohradsk\u00FDch hor." . "V" . "\u010Cesk\u00E1 geografie v evropsk\u00E9m prostoru XXI. sjezd \u010Cesk\u00E9 geografick\u00E9 spole\u010Dnosti" . "\u017Dof\u00EDnsk\u00E1 hornatina je geomorfologick\u00FDm okrskem Poho\u0159sk\u00E9 hornatiny, kter\u00E1 je geomorfologick\u00FDm podcelkem Novohradsk\u00FDch hor. \u017Dof\u00EDnsk\u00E1 hornatina se nach\u00E1z\u00ED ve v\u00FDchodn\u00ED \u010D\u00E1sti Novohradsk\u00FDch hor. Nejzaj\u00EDmav\u011Bj\u0161\u00ED lokality jsou situov\u00E1ny na severu p\u0159i hranici se Stropnickou pahorkatinou. Mezi nejzaj\u00EDmav\u011Bj\u0161\u00ED geomorfologick\u00E9 lokality pat\u0159\u00ED Krav\u00ED hora, Kun\u00ED hora a Vysok\u00E1. Tyto lokality jsou odd\u011Bleny od Stropnick\u00E9 pahorkatiny 300 metr\u016F vysok\u00FDm tektonick\u00FDm svahem a vytv\u00E1\u0159\u00ED vysok\u00E9 exfolia\u010Dn\u00ED klenby. N\u00EDzk\u00E9 exfolia\u010Dn\u00ED klenby se tak\u00E9 vyskytuj\u00ED na svaz\u00EDch. Mrazov\u00E9 zv\u011Btr\u00E1v\u00E1n\u00ED b\u011Bhem Pleistocenu m\u011Blo velk\u00FD vliv na formov\u00E1n\u00ED mezoforem reli\u00E9fu. Jednotliv\u00E9 periglaci\u00E1ln\u00ED formy reli\u00E9fu (nap\u0159. Napoleonova hlava) pat\u0159\u00ED mezi nejzaj\u00EDmav\u011Bj\u0161\u00ED a nejd\u016Fle\u017Eit\u011Bj\u0161\u00ED formy reli\u00E9fu v t\u00E9to \u010D\u00E1sti Novohradsk\u00FDch hor."@cs . "Jiho\u010Desk\u00E1 univerzita v \u010Cesk\u00FDch Bud\u011Bjovic\u00EDch. Pedagogick\u00E1 fakulta" . . "Vysok\u00E1, Krav\u00ED hora, Kun\u00ED hora ? geomorfologicky zaj\u00EDmav\u00E9 lokality Novohradsk\u00FDch hor"@cs . "Vysok\u00E1, Krav\u00ED Mountain, Kun\u00ED Mountain ? the interesting geomorphological localities of the Novohradsk\u00E9 Mountains"@en . "Vysok\u00E1, Krav\u00ED hora, Kun\u00ED hora ? geomorfologicky zaj\u00EDmav\u00E9 lokality Novohradsk\u00FDch hor" . "The \u017Dof\u00EDnsk\u00E1 Mountains are the geomorfological region of the Poho\u0159sk\u00E1 Mountains which is a geomorphological subunit of the Novohradsk\u00E9 Mountains. \u017Dof\u00EDnsk\u00E1 Mountains are situated in the eastern part of the Poho\u0159sk\u00E1 Mountains and so in the eastern part of the Novohradsk\u00E9 Mountains. The most interesting localities of the \u017Dof\u00EDnsk\u00E1 Mountains are situated in the north, along the border with the Stropnick\u00E1 Upland. Vysok\u00E1, Krav\u00ED Mountain and Kun\u00ED Mountain are ranked among the most interesting geomorphological localities of the \u017Dof\u00EDnsk\u00E1 Mountains. These localities are separated from the Stropnick\u00E1 Upland approximately 300 meters high tectonic slope and creates bornhardts. Ruwares are also occuring on the slopes. The frost disintegration during the cool period of the Pleistocen played an important role in formation of the mezoforms relief. The individual periglacial forms of relief (eg. the Napoleon Head) are ranked among the most interesting and the most important forms in this part of the Novohradsk\u00E9 Mount"@en . "\u010Cesk\u00E9 Bud\u011Bjovice" . "Vysok\u00E1, Krav\u00ED Mountain, Kun\u00ED Mountain ? the interesting geomorphological localities of the Novohradsk\u00E9 Mountains"@en . "Vysok\u00E1, Krav\u00ED hora, Kun\u00ED hora ? geomorfologicky zaj\u00EDmav\u00E9 lokality Novohradsk\u00FDch hor"@cs . "RIV/60076658:12410/07:00010608" . "RIV/60076658:12410/07:00010608!RIV10-MSM-12410___" . . "frost disintegration; \u017Dof\u00EDnsk\u00E1 Mountains"@en . "459796" . . "Vysok\u00E1, Krav\u00ED hora, Kun\u00ED hora ? geomorfologicky zaj\u00EDmav\u00E9 lokality Novohradsk\u00FDch hor" . . "978-80-7040-986-2" .