{"id":173,"date":"2017-03-12T13:32:29","date_gmt":"2017-03-12T12:32:29","guid":{"rendered":"http:\/\/pages.pedf.cuni.cz\/sc25\/?page_id=173"},"modified":"2020-02-19T12:49:15","modified_gmt":"2020-02-19T11:49:15","slug":"zemepis","status":"publish","type":"page","link":"https:\/\/pages.pedf.cuni.cz\/sc25\/zemepis\/","title":{"rendered":"Zem\u011bpis"},"content":{"rendered":"

Pr\u016f\u0159ezov\u00e1 t\u00e9mata v Zem\u011bpisu
\n<\/strong><\/p>\n

U\u010ditel si vyb\u00edr\u00e1 3 t\u00e9mata z jednoho p\u0159edm\u011btu (z organiza\u010dn\u00edch d\u016fvod\u016f nen\u00ed mo\u017en\u00fd v\u00fdb\u011br t\u00e9mat nap\u0159\u00ed\u010d p\u0159edm\u011bty).<\/p>\n

1. Ur\u010dujeme zem\u011bpisnou polohu a \u010das<\/strong>
\nUr\u010dov\u00e1n\u00ed absolutn\u00ed a relativn\u00ed zem\u011bpisn\u00e9 polohy, popis\/vysv\u011btlen\u00ed cesty z bodu A do bodu B. Ur\u010den\u00ed polohy nejen podle p\u0159\u00edstroj\u016f a mapy, ale tak\u00e9 um\u011bt se zeptat na cestu a druh\u00e9mu ji poradit\/vysv\u011btlit. Podle z\u00edskan\u00fdch informac\u00ed se n\u00e1sledn\u011b dok\u00e1zat v dan\u00e9m prostoru orientovat. V kterou dobu je mo\u017en\u00e9 u n\u00e1s ve st\u0159edn\u00ed Evrop\u011b sledovat p\u0159\u00edm\u00e9 p\u0159enosy sportovn\u00edch akc\u00ed ze vzd\u00e1len\u00fdch lokalit sv\u011bta (nap\u0159. Severn\u00ed a Ji\u017en\u00ed Ameriky, Asie \u010di Austr\u00e1lie).<\/p>\n

2. Kontinent\u00e1ln\u00ed drift a litosf\u00e9rick\u00e9 (tektonick\u00e9) desky<\/strong>
\nKontinent\u00e1ln\u00ed drift a tektonick\u00e9 desky vytv\u00e1\u0159\u00ed \u201etektonickou\u201c mapu sv\u011bta, ze kter\u00e9 lze vy\u010d\u00edst\/vysv\u011btlit oblasti s horotvornou (vr\u00e1sov\u00e1, sope\u010dn\u00e1 a kern\u00e1 poho\u0159\u00ed) a sope\u010dnou \u010dinnost\u00ed, rizikov\u00e9 z\u00f3ny zem\u011bt\u0159esen\u00ed a vln tsunami. Znalosti a dovednosti, jak se chovat v oblastech p\u0159\u00edrodn\u00edch rizik (sope\u010dn\u00e1 erupce, zem\u011bt\u0159esn\u00ed, tsunami). V\u0161echny tyto procesy maj\u00ed p\u016fvod ve vnit\u0159n\u00edch geomorfologick\u00fdch sil\u00e1ch Zem\u011b.<\/p>\n

3. Vn\u011bj\u0161\u00ed geomorfologick\u00e9 procesy ovliv\u0148uj\u00edc\u00ed charakter krajiny<\/strong>
\nZalo\u017eeno na erozn\u00edm cyklu, p\u0159i n\u011bm\u017e se st\u0159\u00edd\u00e1 eroze (vn\u011bj\u0161\u00ed geomorfologick\u00e9 procesy) se zdvihem povrchu (vnit\u0159n\u00ed geomorfologick\u00e9 procesy). Objasnit rozd\u00edl mezi rovinou a n\u00ed\u017einou. Proti vnit\u0159n\u00edm geomorfologick\u00fdm sil\u00e1m p\u016fsob\u00ed vn\u011bj\u0161\u00ed geomorfologick\u00e9 s\u00edly (v\u011btrn\u00e1, vodn\u00ed, mrazov\u00e1 eroze atd.) a vytv\u00e1\u0159\u00ed charakteristick\u00e9 rysy reli\u00e9fu (krajiny). Interpretace p\u0159\u00ed\u010dn\u00e9ho a pod\u00e9ln\u00e9ho profilu reli\u00e9fem, p\u0159\u00edpadn\u011b vodn\u00edm tokem.<\/p>\n

4. P\u0159\u00edstrojov\u00e1 m\u011b\u0159en\u00ed ve fyzick\u00e9 geografii<\/strong>
\nP\u0159\u00edstrojov\u00e1 m\u011b\u0159en\u00ed ve fyzick\u00e9 geografii implementuj\u00ed prvky badatelsky orientovan\u00e9ho vyu\u010dov\u00e1n\u00ed do hodin zem\u011bpisu. Touto formou je mo\u017en\u00e9 ov\u011b\u0159ovat r\u016fzn\u00e9 \u00falohy (m\u011b\u0159en\u00ed rychlosti v\u011btru, m\u011b\u0159en\u00ed pr\u016ftoku vodn\u00edho toku, zji\u0161\u0165ov\u00e1n\u00ed p\u016fdn\u00edho typu atd.) z d\u00edl\u010d\u00edch discipl\u00edn fyzick\u00e9 geografie (meteorologie a klimatologie, hydrologie, pedogeografie atd.) p\u0159i pr\u00e1ci v ter\u00e9nu. Mo\u017en\u00e9 jsou d\u00edl\u010d\u00ed experimenty k ov\u011b\u0159ov\u00e1n\u00ed vzniku r\u016fzn\u00fdch fyzicko-geografick\u00fdch jev\u016f.<\/p>\n

5. Dopady lidsk\u00e9 \u010dinnosti na \u017eivotn\u00ed prost\u0159ed\u00ed<\/strong>
\nV p\u0159\u00edrod\u011b funguj\u00ed vztahy akce a reakce (determinismus). \u010cinnost \u010dlov\u011bka vyvol\u00e1v\u00e1 zm\u011bny v prost\u0159ed\u00ed, kter\u00e9 jsou v\u011bdecky p\u0159edpov\u011bditeln\u00e9 (nap\u0159. zne\u010di\u0161\u0165ov\u00e1n\u00ed ovzdu\u0161\u00ed, vody, eroze p\u016fd). Odezva p\u0159\u00edrodn\u00edch proces\u016f na \u010dinnost \u010dlov\u011bka \u2013 smog, splavov\u00e1n\u00ed\/sm\u00fdv\u00e1n\u00ed p\u016fdy atd. Zm\u011bna chov\u00e1n\u00ed \u010dlov\u011bka \u2013 sni\u017eov\u00e1n\u00ed zdroj\u016f zne\u010di\u0161t\u011bn\u00ed, zm\u011bna technologie p\u0159i obd\u011bl\u00e1v\u00e1n\u00ed p\u016fd \u010di vyu\u017e\u00edv\u00e1n\u00ed plodin na orn\u00e9 p\u016fd\u011b, kter\u00e9 zabra\u0148uj\u00ed odnosu p\u016fdy aj.<\/p>\n

6. Podle nosa pozn\u00e1\u0161 kosa<\/strong>
\nV\u00a0r\u00e1mci programu d\u011bt\u00ed objev\u00ed \u017eivot velmi pestr\u00e9 skupiny zv\u00ed\u0159at, kter\u00e1 se d\u016fvtipn\u011b p\u0159izp\u016fsobila p\u0159\u00edrodn\u00edm podm\u00ednk\u00e1m po cel\u00e9m sv\u011bt\u011b. \u017d\u00e1ci se dozv\u011bd\u00ed, jak\u00fdm zp\u016fsobem se pt\u00e1ci p\u0159izp\u016fsobili \u017eivotu ve vzduchu a d\u00edky kter\u00fdm letov\u00fdm adaptac\u00edm se z\u00a0nich stali kosmopolitn\u00ed \u017eivo\u010dichov\u00e9. Uk\u00e1\u017eeme jim, co kryje povrch t\u011bla pt\u00e1ku a z\u00a0\u010deho se skl\u00e1d\u00e1. \u017d\u00e1ci na z\u00e1klad\u011b praktick\u00e9 dovednosti odvod\u00ed, nev\u0161edn\u00ed originalitu a n\u00e1paditost, se kterou pt\u00e1ci vy\u0159e\u0161ili z\u00edsk\u00e1v\u00e1n\u00ed potravy v\u00a0rozli\u010dn\u00fdch, biogeografick\u00fdch are\u00e1lech sv\u011bta. D\u00edky tomu pt\u00e1ci p\u0159izp\u016fsobili sv\u016fj \u017eivota v\u00a0dan\u00fdch p\u0159\u00edrodn\u00edch podm\u00ednk\u00e1ch. \u017d\u00e1ci si v\u0161e budou moci vyzkou\u0161et na vlastn\u00ed zob\u00e1k.<\/p>\n

Ov\u011b\u0159ov\u00e1n\u00ed n\u011bkter\u00fdch z\u00a0t\u011bchto t\u00e9mat je sou\u010d\u00e1st\u00ed v\u00fdstup\u016f projektu, dostupn\u00e9 zde<\/a><\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"

Pr\u016f\u0159ezov\u00e1 t\u00e9mata v Zem\u011bpisu U\u010ditel si vyb\u00edr\u00e1 3 t\u00e9mata z jednoho p\u0159edm\u011btu (z organiza\u010dn\u00edch d\u016fvod\u016f nen\u00ed mo\u017en\u00fd v\u00fdb\u011br t\u00e9mat nap\u0159\u00ed\u010d p\u0159edm\u011bty). 1. Ur\u010dujeme zem\u011bpisnou polohu a \u010das Ur\u010dov\u00e1n\u00ed absolutn\u00ed a relativn\u00ed zem\u011bpisn\u00e9 polohy, popis\/vysv\u011btlen\u00ed cesty z bodu A do bodu B. Ur\u010den\u00ed polohy nejen podle p\u0159\u00edstroj\u016f a mapy, ale tak\u00e9 um\u011bt se zeptat na cestu … Continue reading →<\/span><\/a><\/p>\n","protected":false},"author":465,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-173","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/pages\/173","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/users\/465"}],"replies":[{"embeddable":true,"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/comments?post=173"}],"version-history":[{"count":8,"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/pages\/173\/revisions"}],"predecessor-version":[{"id":1533,"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/pages\/173\/revisions\/1533"}],"wp:attachment":[{"href":"https:\/\/pages.pedf.cuni.cz\/sc25\/wp-json\/wp\/v2\/media?parent=173"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}