. . . . . . "\u0160umavsk\u00E9 slat\u011B"@cs . . "14869463"^^ . . . . . . "32"^^ . "Slat\u011B je n\u00E1zev pro ra\u0161elini\u0161t\u011B v centr\u00E1ln\u00ED \u010D\u00E1sti \u0160umavy. Pro vznik slat\u00ED na \u0160umav\u011B existovaly tak\u0159ka ide\u00E1ln\u00ED podm\u00EDnky, tedy m\u011Blk\u00E9 p\u00E1nve, sedla, m\u00EDrn\u00E9 svahy, n\u00E1horn\u00ED roviny, pl\u00E1n\u011B. D\u00E1le tak\u00E9 \u0161irok\u00E1, m\u011Blk\u00E1 \u00FAdol\u00ED potok\u016F a jej\u00EDch n\u011Bkter\u00FDch p\u0159\u00EDtok\u016F."@cs . . "Slat\u011B je n\u00E1zev pro ra\u0161elini\u0161t\u011B v centr\u00E1ln\u00ED \u010D\u00E1sti \u0160umavy. Pro vznik slat\u00ED na \u0160umav\u011B existovaly tak\u0159ka ide\u00E1ln\u00ED podm\u00EDnky, tedy m\u011Blk\u00E9 p\u00E1nve, sedla, m\u00EDrn\u00E9 svahy, n\u00E1horn\u00ED roviny, pl\u00E1n\u011B. D\u00E1le tak\u00E9 \u0161irok\u00E1, m\u011Blk\u00E1 \u00FAdol\u00ED potok\u016F a jej\u00EDch n\u011Bkter\u00FDch p\u0159\u00EDtok\u016F. Podneb\u00ED je zde velmi chladn\u00E9 a vlhk\u00E9, prameni\u0161\u0165 je dostatek a horninov\u00FD podklad pod zv\u011Btralinov\u00FDm pl\u00E1\u0161t\u011Bm nen\u00ED pro vodu p\u0159\u00EDli\u0161 propustn\u00FD.Spojen\u00EDm v\u00EDce jez\u00EDrek rozr\u016Fstaj\u00EDc\u00EDmi se porosty ra\u0161elin\u00EDk\u016F vznikly velk\u00E9, mnohdy n\u011Bkolikasethektarov\u00E9 komplexy \u0161umavsk\u00FDch ra\u0161elini\u0161\u0165 s mnoha jez\u00EDrky uprost\u0159ed. Komplex cel\u00E9ho ra\u0161elini\u0161t\u011B (tvo\u0159en\u00E9ho zejm\u00E9na ra\u0161elin\u00EDky) zadr\u017Euje velk\u00E9 mno\u017Estv\u00ED vody, m\u00E1 tedy d\u016Fle\u017Eitou hydrologickou funkci. Zp\u011Btn\u011B p\u0159\u00EDzniv\u011B ovliv\u0148uje mikroklima a mezoklima nejbli\u017E\u0161\u00EDho okol\u00ED."@cs . . . . . . . . . . . . . "99883"^^ . . "4549"^^ . . . . . . . . . . . . . "\u0160umavsk\u00E9 slat\u011B"@cs . .