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Vonkajšie činitele

Vonkajšie činitele. biogénny reliéf eolický reliéf glaciálny reliíef činnosť vody na morskom dne. Denisa Hladová, I.C. Biogénny reliéf. a. mravenisko. c. rašeliniská. b. termitiská. d. koralové ostrovy- atoly (Austrália). e. koralové útesy pri Austrálii. Eolický reliéf.

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Vonkajšie činitele

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  1. Vonkajšie činitele • biogénny reliéf • eolický reliéf • glaciálny reliíef • činnosť vody na morskom dne Denisa Hladová, I.C

  2. Biogénny reliéf a. mravenisko c. rašeliniská b. termitiská

  3. d. koralové ostrovy- atoly (Austrália) e. koralové útesy pri Austrálii

  4. Eolický reliéf a. kamenité púšte b. duny

  5. c.,d. veterná erózia e. dôsledok veternej erózie

  6. Glaciálny reliéf c. ľadovcová dolina tvaru U

  7. d. ľadovcový splaz e. ľadovcový kotol- kar f. ľadovcová dolina- tróg

  8. Činnosť vody na morskom dne a. prehľad morského prostredia

  9. c. podmorské kaňóny b. podmorské kaňóny a hlbokomorské deltové vejáre

  10. Použité zdroje • 1. Biogénny reliéf • a • http://www.google.sk/imgres?q=mravenisko&start=20&num=10&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=cboTlKIAT4WOqM:&imgrefurl=http://zivot.lesk.cas.sk/clanok/9488/mravcom-mozeme-zavidiet-priatelske-spolunazivanie.html&docid=XAtqJJigDaaiKM&imgurl=http://img.cas.sk/img/12/gallery/922589_hmyz-mravce-mravenisko.jpg&w=450&h=300&ei=NAyET42tNoLltQbCsNSaCA&zoom=1&iact=rc&dur=183&sig=107362323721404292849&page=2&tbnh=151&tbnw=218&ndsp=26&ved=1t:429,r:3,s:20,i:11&tx=67&ty=96 • b • http://www.google.sk/imgres?q=termitisko&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=s6NlY17rNWu8QM:&imgrefurl=http://infovekacik.infovek.sk/2010-oktober/priroda-predstavujeme.php&docid=izDQHCs89mqHeM&imgurl=http://infovekacik.infovek.sk/2010-oktober/priroda/termitisko.jpg&w=350&h=233&ei=cAyET9WUGMXhtQbJwOTGBg&zoom=1&iact=hc&vpx=647&vpy=202&dur=169&hovh=183&hovw=275&tx=164&ty=119&sig=107362323721404292849&page=1&tbnh=143&tbnw=207&start=0&ndsp=22&ved=1t:429,r:2,s:0,i:69 • c • http://www.google.sk/imgres?q=ra%C5%A1elinisko&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=3dOjEHo-oRak6M:&imgrefurl=http://pochyly.blog.sme.sk/c/113232/Finsko-NP-Rokua-a-NP-Salamajarvi.html&docid=RvcE5RlEk3_JKM&imgurl=http://blog.sme.sk/blog/1238/113232/DSCN3243.JPG&w=532&h=399&ei=UAyET53qKtHmtQbosuCvBg&zoom=1&iact=rc&dur=351&sig=107362323721404292849&page=2&tbnh=152&tbnw=203&start=20&ndsp=27&ved=1t:429,r:14,s:20,i:142&tx=106&ty=102 • d • http://www.google.sk/imgres?q=koralov%C3%A9+ostrovy&um=1&hl=cs&sa=N&biw=1280&bih=866&tbm=isch&tbnid=8VmfcwyTJWNG2M:&imgrefurl=http://www.infoglobe.cz/zajimavosti/velky-barierovy-utes/&docid=d_G9doL5gknLNM&imgurl=http://www.infoglobe.cz/res/data/190/021873_56_270448.jpg%253Fseek%253D1282701406&w=300&h=401&ei=KJqNT4G5JMHVtAaSl4G6CQ&zoom=1&iact=rc&dur=301&sig=107362323721404292849&page=1&tbnh=168&tbnw=132&start=0&ndsp=20&ved=1t:429,r:16,s:0,i:100&tx=42&ty=82 • e • http://www.google.sk/imgres?q=koralov%C3%A9+%C3%BAtesy&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=MKKJRtPzgBvrDM:&imgrefurl=http://www.drom.sk/clanky/hudba-a-kultura/dokumentarny-film-home-domov&docid=Ntvxc_WzO1IISM&imgurl=http://img.drom.sk/others/clanky/home-domov/koralove-utesy-home-movie-domov-film.jpg&w=600&h=338&ei=ywuET-TJMInJsga7-ZHfBg&zoom=1&iact=hc&vpx=372&vpy=462&dur=29&hovh=168&hovw=299&tx=190&ty=104&sig=107362323721404292849&page=3&tbnh=109&tbnw=193&start=45&ndsp=25&ved=1t:429,r:1,s:45,i:170

  11. 2. Eolický reliéf • a • http://www.google.sk/imgres?q=kamenit%C3%A9+p%C3%BA%C5%A1te&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=heL6rA9RSxE6DM:&imgrefurl=http://www.janmiklin.cz/clanek-nazca-a-ica/&docid=A-x4thrOfcEdVM&imgurl=http://www.janmiklin.cz/soubory/images/clanky/73_582.jpg&w=750&h=422&ei=2gmET8GON9GSswbM5qXLBg&zoom=1&iact=rc&dur=411&sig=107362323721404292849&page=3&tbnh=107&tbnw=190&start=46&ndsp=27&ved=1t:429,r:15,s:46,i:202&tx=84&ty=57 • b • http://www.google.sk/imgres?q=pieso%C4%8Dn%C3%A9+presypy-duny&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=8N41pw-rhgdN1M:&imgrefurl=http://www.infoglobe.sk/zaujimavosti/pyla-pobrezie-piesocnych-presypov/&docid=IRxyBgesy4yeOM&imgurl=http://www.infoglobe.sk/res/data/195/022429_56_241883.jpg%253Fseek%253D1282697644&w=500&h=470&ei=sAqET7-dItDKsgbtlYnXBg&zoom=1&iact=hc&vpx=506&vpy=316&dur=3593&hovh=218&hovw=232&tx=160&ty=113&sig=107362323721404292849&page=1&tbnh=155&tbnw=159&start=0&ndsp=24&ved=1t:429,r:8,s:0,i:80 • c • http://www.google.sk/imgres?q=vetern%C3%A1+erozia&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=nmlR7H8MTkn_wM:&imgrefurl=http://www.agroserver.sk/news/veterna-erozia-a-jej-skodlivost/&docid=voE7X5_f1qLNoM&imgurl=http://www.agroserver.sk/media/2459/large/veterna-erozia.jpg&w=800&h=600&ei=NwuET4G4HtH2sgaKvZzyBg&zoom=1&iact=rc&dur=266&sig=107362323721404292849&page=1&tbnh=149&tbnw=194&start=0&ndsp=20&ved=1t:429,r:8,s:0,i:80&tx=97&ty=75 • d • http://www.google.sk/imgres?q=vetern%C3%A1+er%C3%B3zia&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=RbGMFG47RiHgvM:&imgrefurl=http://sk.wikipedikia.org/wiki/Er%25C3%25B3zia&docid=nusLJhvM8xp8GM&itg=1&imgurl=http://upload.wikimedia.org/wikipedia/commons/thumb/d/de/Saltation-mechanics.gif/220px-Saltation-mechanics.gif&w=220&h=143&ei=fguET53JIJHUsgbC8OnGBg&zoom=1&iact=rc&dur=256&sig=107362323721404292849&page=2&tbnh=114&tbnw=176&start=20&ndsp=25&ved=1t:429,r:13,s:20,i:140&tx=108&ty=48 • e • http://www.google.sk/imgres?q=vetern%C3%A1+erozia&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=w11ly0vK__4ToM:&imgrefurl=http://fidler.blog.sme.sk/c/130410/a-co-tu-po-nas-zostane-I.html&docid=sRYSy5ttjRm0qM&imgurl=http://blog.sme.sk/blog/8444/130410/vjoneonre.jpg&w=400&h=266&ei=NwuET4G4HtH2sgaKvZzyBg&zoom=1&iact=rc&dur=283&sig=107362323721404292849&page=1&tbnh=149&tbnw=194&start=0&ndsp=20&ved=1t:429,r:6,s:0,i:76&tx=98&ty=51

  12. 3. Glaciálny reliéf • a,b • http://www.google.sk/imgres?q=glaci%C3%A1ln%C3%AD+geomorfologick%C3%A9+procesy&um=1&hl=cs&sa=N&biw=1280&bih=866&tbm=isch&tbnid=ZkSQVQZFimR7MM:&imgrefurl=http://geologie.vsb.cz/geologie/KAPITOLY/9_reli%25C3%25A9f/9_typy_tvary_reli%25C3%25A9fu.htm&docid=_pfhMIEJ0htNtM&imgurl=http://geologie.vsb.cz/geologie/KAPITOLY/9_reli%2525C3%2525A9f/9_typy_tvary_reli%2525C3%2525A9fu_soubory/image043.jpg&w=1751&h=820&ei=Dg2ET7qYJM7NswaHyPjKBg&zoom=1&iact=hc&vpx=546&vpy=351&dur=420&hovh=153&hovw=328&tx=199&ty=95&sig=107362323721404292849&page=1&tbnh=95&tbnw=202&start=0&ndsp=20&ved=1t:429,r:7,s:0,i:80 • c • http://www.google.sk/imgres?q=glaci%C3%A1ln%C3%AD+geomorfologick%C3%A9+procesy&um=1&hl=cs&sa=N&biw=1280&bih=866&tbm=isch&tbnid=7q537L1W8enU_M:&imgrefurl=http://www.geocaching.com/seek/cache_details.aspx%3Fguid%3D57c06f5b-7979-4f18-9938-5c80dd32dce4&docid=UlKda2A9oVAPVM&imgurl=http://img.geocaching.com/cache/de1f43a8-515f-46f7-aa1b-40f0d21c004d.jpg&w=424&h=499&ei=Dg2ET7qYJM7NswaHyPjKBg&zoom=1&iact=hc&vpx=188&vpy=280&dur=6669&hovh=244&hovw=207&tx=122&ty=127&sig=107362323721404292849&page=1&tbnh=163&tbnw=139&start=0&ndsp=20&ved=1t:429,r:15,s:0,i:98 • d • http://www.google.sk/imgres?q=mor%C3%A9ny&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=8H_CKeJ_qxx6NM:&imgrefurl=http://www.horyinfo.cz/rservice.php%3Fakce%3Dtisk%26cisloclanku%3D2008100012&docid=CzoM30cXwASB9M&imgurl=http://www.horyinfo.cz/image/gallery_clanky_cesty/200810181931_Obr116.jpg&w=500&h=302&ei=Ew-ET5_zBsKSswa-qJHIBg&zoom=1&iact=hc&vpx=586&vpy=340&dur=4880&hovh=174&hovw=289&tx=141&ty=81&sig=107362323721404292849&page=1&tbnh=121&tbnw=201&start=0&ndsp=20&ved=1t:429,r:7,s:0,i:78 • e • http://www.google.sk/imgres?q=%C4%BEadovcov%C3%BD+kotol+kar&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=qsqL3RPHDlA9gM:&imgrefurl=http://www.infoglobe.sk/horske-jazera/plesne-jazero/&docid=WZ9NAcqHlDFLKM&imgurl=http://www.infoglobe.sk/res/data/255/029695_56_307065.jpg%253Fseek%253D1282708406&w=325&h=450&ei=Lw6ET_rIOYzmtQagzom2Bg&zoom=1&iact=rc&dur=286&sig=107362323721404292849&page=1&tbnh=158&tbnw=115&start=0&ndsp=20&ved=1t:429,r:1,s:0,i:65&tx=14&ty=71 • f • http://www.google.sk/imgres?q=%C4%BEadovcov%C3%BD+kotol+kar&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=-HKZi20hZ-lqMM:&imgrefurl=http://www.mineraly.sk/files/lok/401-500/468_slovgeo_geomor_vyvin_stvrtohory_1.htm&docid=VKqKY6XwDxN1KM&imgurl=http://www.mineraly.sk/files/lok/401-500/468.jpg&w=300&h=279&ei=Lw6ET_rIOYzmtQagzom2Bg&zoom=1&iact=hc&vpx=402&vpy=318&dur=2180&hovh=216&hovw=233&tx=140&ty=113&sig=107362323721404292849&page=1&tbnh=153&tbnw=165&start=0&ndsp=20&ved=1t:429,r:6,s:0,i:76

  13. 4. Činnosť vody na morskom dne • a,b • http://geologie.vsb.cz/Sedimentologie/textova%20cast/sedimentacni%20prostr/Hlubokomo%C5%99sk%C3%A9%20sedimenty.htm • c • http://www.google.sk/imgres?q=podmorsk%C3%A9+ka%C5%88%C3%B3ny&um=1&hl=cs&biw=1280&bih=866&tbm=isch&tbnid=-FUFUu26CvcbSM:&imgrefurl=http://geologie.vsb.cz/geomorfologie/Prednasky/7_kapitola.htm&docid=_ggoDC6eSvezbM&imgurl=http://geologie.vsb.cz/geomorfologie/Prednasky/7_obrazky/7_5_Offshore.jpg&w=671&h=550&ei=yA-ET_iSH47mtQbvqs3hCg&zoom=1&iact=rc&dur=297&sig=107362323721404292849&page=1&tbnh=149&tbnw=182&start=0&ndsp=20&ved=1t:429,r:0,s:0,i:63&tx=77&ty=74

  14. Oceňujem pozorné obecenstvo

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