[{"@context":"https:\/\/schema.org\/","@type":"Article","@id":"https:\/\/www.starweg.cz\/jak-funguje-tektonika\/#Article","mainEntityOfPage":"https:\/\/www.starweg.cz\/jak-funguje-tektonika\/","headline":"Jak funguje tektonika","name":"Jak funguje tektonika","description":"Ji\u017e od prad\u00e1vn\u00fdch dob se lid\u00e9 zaj\u00edmali o to, jak\u00e9 jsou p\u0159\u00ed\u010diny zem\u011bt\u0159esen\u00ed \u010di nap\u0159\u00edklad vulkanick\u00e9 \u010dinnosti. To v\u0161e bylo nejprve p\u0159isuzov\u00e1no nejr\u016fzn\u011bj\u0161\u00edm boh\u016fm, av\u0161ak jak na\u0161e porozum\u011bn\u00ed rostlo, pochopili jsme, \u017ee p\u0159\u00ed\u010diny t\u011bchto v\u011bc\u00ed jsou naprosto p\u0159irozen\u00e9. \u00a0 Jedn\u00edm z\u00a0nejz\u00e1sadn\u011bj\u0161\u00edch objev\u016f byl v\u00a0tomto ohledu objev litosf\u00e9rick\u00fdch desek. Tato teorie se pak stala \u0161iroce p\u0159ij\u00edmanou […]","datePublished":"2023-09-28","dateModified":"2023-09-28","author":{"@type":"Person","@id":"https:\/\/www.starweg.cz\/author\/devene\/#Person","name":"devene","url":"https:\/\/www.starweg.cz\/author\/devene\/","identifier":1,"image":{"@type":"ImageObject","@id":"https:\/\/secure.gravatar.com\/avatar\/014a645f9f16d49aceddb25e316448c724bd78e7db0ee7a34c29417d5ca39ef1?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/014a645f9f16d49aceddb25e316448c724bd78e7db0ee7a34c29417d5ca39ef1?s=96&d=mm&r=g","height":96,"width":96}},"publisher":{"@type":"Organization","name":"starweg.cz","logo":{"@type":"ImageObject","@id":"\/logo.png","url":"\/logo.png","width":600,"height":60}},"image":{"@type":"ImageObject","@id":"https:\/\/www.starweg.cz\/wp-content\/uploads\/tektonika1.png","url":"https:\/\/www.starweg.cz\/wp-content\/uploads\/tektonika1.png","height":0,"width":0},"url":"https:\/\/www.starweg.cz\/jak-funguje-tektonika\/","about":["V\u011bda"],"wordCount":450,"articleBody":"Ji\u017e od prad\u00e1vn\u00fdch dob se lid\u00e9 zaj\u00edmali o to, jak\u00e9 jsou p\u0159\u00ed\u010diny zem\u011bt\u0159esen\u00ed \u010di nap\u0159\u00edklad vulkanick\u00e9 \u010dinnosti. To v\u0161e bylo nejprve p\u0159isuzov\u00e1no nejr\u016fzn\u011bj\u0161\u00edm boh\u016fm, av\u0161ak jak na\u0161e porozum\u011bn\u00ed rostlo, pochopili jsme, \u017ee p\u0159\u00ed\u010diny t\u011bchto v\u011bc\u00ed jsou naprosto p\u0159irozen\u00e9.\u00a0Jedn\u00edm z\u00a0nejz\u00e1sadn\u011bj\u0161\u00edch objev\u016f byl v\u00a0tomto ohledu objev litosf\u00e9rick\u00fdch desek. Tato teorie se pak stala \u0161iroce p\u0159ij\u00edmanou a dnes se v\u011b\u0159\u00ed, \u017ee je skute\u010dn\u011b t\u00edm spr\u00e1vn\u00fdm vysv\u011btlen\u00edm nejr\u016fzn\u011bj\u0161\u00edch p\u0159\u00edrodn\u00edch jev\u016f, kter\u00e9 m\u016f\u017eeme pozorovat.\u00a0\u00a0Zakl\u00e1d\u00e1 se na tom, \u017ee na\u0161e planeta, \u010di sp\u00ed\u0161e jej\u00ed k\u016fra, je rozd\u011blena na n\u011bkolik r\u016fzn\u00fdch desek odli\u0161n\u00fdch rozm\u011br\u016f, kter\u00e9 se pohybuj\u00ed po zemsk\u00e9m magmatu. Tento pohyb je skute\u010dn\u011b velice pomal\u00fd, ani ne jeden centimetr za rok, av\u0161ak m\u016f\u017ee m\u00edt skute\u010dn\u011b dalekos\u00e1hl\u00e9 n\u00e1sledky.\u00a0Zdaleka nejv\u011bt\u0161\u00ed probl\u00e9my p\u016fsob\u00ed, kdy\u017e se jedna z\u00a0t\u011bchto desek podsune pod druhou, p\u0159\u00edpadn\u011b se od sebe vzd\u00e1l\u00ed. V\u00a0takov\u00e9m p\u0159\u00edpad\u011b doch\u00e1z\u00ed k\u00a0zem\u011bt\u0159esen\u00edm, m\u011bn\u00ed se tak\u00e9 reli\u00e9f krajiny. T\u00edmto zp\u016fsobem tak\u00e9 mimo jin\u00e9 vznikaj\u00ed mnoh\u00e1 poho\u0159\u00ed \u010di naopak p\u0159\u00edkopy. T\u00edm zdaleka nejzn\u00e1m\u011bj\u0161\u00edm jsou potom Himal\u00e1je, kter\u00e9 vznikly, kdy\u017e se Indick\u00e1 deska posunula pod Euroasijskou. To je tak\u00e9 d\u016fvod, pro\u010d i na vrcholc\u00edch hor nach\u00e1z\u00edme fos\u00edlie mo\u0159sk\u00fdch \u017eivo\u010dich\u016f.\u00a0\u00a0V\u00a0p\u0159\u00edpad\u011b, \u017ee se od sebe desky vzd\u00e1l\u00ed, samoz\u0159ejm\u011b m\u016f\u017ee magma vytrysknout na povrch. Takto naopak vznikaly mnoh\u00e9 ostrovy, z\u00a0nich\u017e mnoh\u00e9 vid\u00edme dodnes. D\u016fkazem je to, \u017ee maj\u00ed z\u00e1klad ze sope\u010dn\u00e9 horniny, a tak\u00e9 \u017ee se na nich velmi \u010dasto nach\u00e1z\u00ed sopky. Zde je typick\u00fdm p\u0159\u00edkladem Havaj.\u00a0Bohu\u017eel, pohyb t\u011bchto desek a s\u00a0nimi i cel\u00fdch kontinent\u016f nem\u016f\u017eeme nijak kontrolovat ani korigovat. \u017de k\u00a0n\u011bmu doch\u00e1z\u00ed, m\u016f\u017eeme vid\u011bt i na tom, \u017ee z\u00e1padn\u00ed pob\u0159e\u017e\u00ed Madagaskaru je prakticky toto\u017en\u00e9 s\u00a0v\u00fdchodn\u00edm pob\u0159e\u017e\u00edm Afriky a naopak z\u00e1padn\u00ed pob\u0159e\u017e\u00ed Afriky velmi dob\u0159e pasuje na ji\u017en\u00ed Ameriku.\u00a0Jeden z\u00a0t\u011bchto p\u0159\u00edrodn\u00edch zlom\u016f se pak nach\u00e1z\u00ed i v\u00a0z\u00e1padn\u00ed \u010d\u00e1sti \u010cesk\u00e9 republiky, a je p\u0159\u00ed\u010dinou toho, pro\u010d zde ob\u010das doch\u00e1z\u00ed k, by\u0165 m\u00edrn\u00fdm, zem\u011bt\u0159esen\u00edm. O tom, zda nezes\u00edl\u00ed, v\u0161ak zat\u00edm nelze nic \u0159\u00edci.                                                                                                                                                                                                                                                                                                                                                                                        3.5\/5 - (6 votes)        "},{"@context":"https:\/\/schema.org\/","@type":"BreadcrumbList","itemListElement":[{"@type":"ListItem","position":1,"name":"Jak funguje tektonika","item":"https:\/\/www.starweg.cz\/jak-funguje-tektonika\/#breadcrumbitem"}]}]