Klif

Klifovi su poglavito strme obale nastale djelovanjem abrazije. Klifovi mogu biti i tektonskog postanka.

Procesi abrazije se ponavljanju, i klif postupno uzmiče, usporedno s tim razrušena stjenovita građa se taloži, stvarajući strmu vanjsku obalu.

 Vanjski linkovi 
 https://web.archive.org/web/20060521223224/http://www.guinnessworldrecords.com/content_pages/record.asp?recordid=54819
 https://web.archive.org/web/20051127032740/http://www.guinnessworldrecords.com/content_pages/record.asp?recordid=47602
 http://books.google.co.uk/books?id=Yuc2Aro6ukkC&pg=PA177&lpg=PA176
 http://www.planetfear.co.uk/articles/Greenland_New_Route_on_Thumbnail_926.html 
 https://web.archive.org/web/20120928053846/http://www.ts2.pl/en/News/1/56
 http://www.bigwall.dk/galleri/klatring/tasermiu/pages-uk/uk05keti.htm
 https://web.archive.org/web/20081217084704/http://www.americanalpineclub.org/AAJO/pdfs/1986/175_canada_greenland_aaj1986.pdf
 http://www.eoearth.org/article/Abiotic_factor?topic=49461

Kategorija:Geomorfologija
Kategorija:Fluvijalni oblici reljefa