{"id":6995,"date":"2020-05-05T08:46:43","date_gmt":"2020-05-05T06:46:43","guid":{"rendered":"https:\/\/www.hausamstrom.de\/udoli-dunaje-2\/zemepis\/geologie-v-bavorskem-lese-a-v-udoli-dunaje\/"},"modified":"2020-05-05T08:46:43","modified_gmt":"2020-05-05T06:46:43","slug":"geologie-v-bavorskem-lese-a-v-udoli-dunaje","status":"publish","type":"page","link":"https:\/\/www.hausamstrom.de\/cs\/udoli-dunaje-2\/zemepis\/geologie-v-bavorskem-lese-a-v-udoli-dunaje\/","title":{"rendered":"Geologie v Bavorsk\u00e9m lese a v \u00fadol\u00ed Dunaje"},"content":{"rendered":"

Historie Donauengtales za\u010d\u00edn\u00e1 pozvednut\u00ed \u010cesk\u00e9ho hmoty ji\u017e p\u0159ed 17-18 miliony let v t\u0159etihor\u00e1ch. Dokonce i po\u010d\u00e1tkem zemsk\u00e9 Precambrian p\u0159ed 1000 milion\u016f let, kter\u00e9 nyn\u00ed vytvo\u0159en\u00fdch p\u0159i stavb\u011b horsk\u00fdch rozpoznateln\u00fdch struktur a sm\u011bry.<\/p>\n

Na obou stran\u00e1ch \u00fadol\u00ed star\u00e9 krystalick\u00e9 horniny je vytvo\u0159en, kter\u00e9 se li\u0161\u00ed v rule a \u017eula rula lassen.Die p\u0159edstavuje sk\u00e1ly deformov\u00e1n tlaku a tepla, mohou b\u00fdt pou\u017eity do dvou skupin. Tak zvan\u00e1 \u201emonot\u00f3nn\u00ed skupina\u201c, kter\u00fd p\u0159em\u011bna p\u0159em\u011bn\u011bn\u00e1 stonky p\u00edskovec, j\u00edlu nebo opuky a (nap\u0159 grafitu b\u0159idlice v prostoru horn\u00ed bu\u0148ky) jsou za\u0159azeny do skupiny \u201eBunte\u201c, kter\u00e1 je proniknuta sope\u010dn\u00fdch usazenin.<\/p>\n

B\u011bhem vr\u00e1sn\u011bn\u00ed Variscan v karbonu, v n\u011bm\u017e dosp\u011bla k zapojen\u00ed \u017eul, Bavorsk\u00fd les vyvinula do vysok\u00e9 hory. Tvorba p\u00f3lu (nap\u0159 Aicha-Halser hromada strana Iggensbach do Pasova), je dusac\u00ed n\u00e1pl\u0148 sloupce spad\u00e1 do tohoto obdob\u00ed.<\/p>\n

V n\u00e1sleduj\u00edc\u00edch geologick\u00fdch v\u011bk\u016f permu a triasu vysok\u00e9 hory odkl\u00edz\u00ed hlubok\u00e9 eroze na trupu hor. V dob\u011b Jura z\u016fstal jen \u201e\u010desk\u00fd ostrov\u201c, byl obklopen m\u011blk\u00fdch mo\u0159\u00edch a kor\u00e1lov\u00fdch \u00fates\u016f, p\u0159es.<\/p>\n

Tvorba Alp vyroben po\u010d\u00e1te\u010dn\u00edm sr\u00e1\u017ece africk\u00e9 a evropsk\u00e9 desky, co\u017e vedlo k pozvednut\u00ed \u010cesk\u00e9ho masivu, bemerkbar.Mehrfache mo\u0159sk\u00e9 z\u00e1plavy v povod\u00ed p\u0159ed rozv\u00edjej\u00edc\u00edch Alp zaznamen\u00e1v\u00e1ny ani podlo\u017e\u00ed. Zbytky t\u011bchto mo\u0159sk\u00fdch usazenin, jsou nyn\u00ed zn\u00e1m\u00e9 jako melasa a to i na z\u00e1kladn\u00ed horninov\u00fd masiv score.The m\u00edstnost tahem tektonick\u00fdch poruch hraj\u00ed d\u016fle\u017eitou roli v toku Dunaje.<\/p>\n

Rozbit\u00ed okraj Dunaj, li\u0161\u00edc\u00edch se v Hofkirchen jih je linie lomu, p\u0159i kter\u00e9 suter\u00e9n m na v\u00edce ne\u017e 1000, vzta\u017eeno na ji\u017en\u00ed terci\u00e1rn\u00ed p\u0159\u00edb\u0159e\u017e\u00ed zv\u00fd\u0161il wurde.Ein prekurzor starov\u011bk\u00fdch Dunaj m\u00e1 pravd\u011bpodobn\u011b dal\u0161\u00ed sn\u00ed\u017een\u00ed \u00fadol\u00ed na z\u00e1pad\u011b retrogr\u00e1dn\u00ed eroze a tak aktu\u00e1ln\u00ed Donau p\u0159edm\u011btu ur\u010deno.<\/p>\n

ale k tomuto \u00fa\u010delu existuj\u00ed i \u200b\u200bjin\u00e9 Theorien.Wohl teprve na konci t\u0159etihor Dunaj byl pak jeho sou\u010dasn\u00fd Bett.Unterhalb Pasov dnes n\u00e1sleduje po Dunaji nepo\u0159\u00e1dek Donauleiten v p\u0159\u00edm\u00e9m pokra\u010dov\u00e1n\u00ed hrani\u010dn\u00ed poruchy Dunaje a Aicha-Halser-Nebenpfahles.W\u00e4hrend ledov\u00e1 shodoval s stoupaj\u00edc\u00ed z hor, prohlouben\u00ed \u00fadol\u00ed, kter\u00e9 p\u0159isp\u011bly ke vzniku dne\u0161n\u00ed \u00fadol\u00ed Dunaje.<\/p>\n

Verebnungsfl\u00e4chen kde byl ulo\u017een \u0159eka \u0161t\u011brky a p\u00edsky, jsou d\u016fle\u017eit\u00fdmi obytn\u00e9 z\u00f3ny, stejn\u011b jako d\u016fle\u017eit\u00e9 n\u00e1dr\u017ee podzemn\u00ed vody.<\/p>\n","protected":false},"excerpt":{"rendered":"

Historie Donauengtales za\u010d\u00edn\u00e1 pozvednut\u00ed \u010cesk\u00e9ho hmoty ji\u017e p\u0159ed 17-18 miliony let v t\u0159etihor\u00e1ch. Dokonce i po\u010d\u00e1tkem zemsk\u00e9 Precambrian p\u0159ed 1000 milion\u016f let, kter\u00e9 nyn\u00ed vytvo\u0159en\u00fdch p\u0159i stavb\u011b horsk\u00fdch rozpoznateln\u00fdch struktur a sm\u011bry. Na obou stran\u00e1ch \u00fadol\u00ed star\u00e9 krystalick\u00e9 horniny je vytvo\u0159en, kter\u00e9 se li\u0161\u00ed v rule a \u017eula rula lassen.Die p\u0159edstavuje sk\u00e1ly deformov\u00e1n tlaku a […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":6962,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-6995","page","type-page","status-publish","hentry"],"yoast_head":"\nGeologie v Bavorsk\u00e9m lese a v \u00fadol\u00ed Dunaje - Haus am Strom<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.hausamstrom.de\/cs\/udoli-dunaje-2\/zemepis\/geologie-v-bavorskem-lese-a-v-udoli-dunaje\/\" \/>\n<meta property=\"og:locale\" content=\"cs_CZ\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Geologie v Bavorsk\u00e9m lese a v \u00fadol\u00ed Dunaje - Haus am Strom\" \/>\n<meta property=\"og:description\" content=\"Historie Donauengtales za\u010d\u00edn\u00e1 pozvednut\u00ed \u010cesk\u00e9ho hmoty ji\u017e p\u0159ed 17-18 miliony let v t\u0159etihor\u00e1ch. 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