Klif
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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
[uredi | uredi izvor]- https://web.archive.org/web/20060521223224/https://www.guinnessworldrecords.com/content_pages/record.asp?recordid=54819
- https://web.archive.org/web/20051127032740/https://www.guinnessworldrecords.com/content_pages/record.asp?recordid=47602
- https://books.google.co.uk/books?id=Yuc2Aro6ukkC&pg=PA177&lpg=PA176
- https://www.planetfear.co.uk/articles/Greenland_New_Route_on_Thumbnail_926.html Arhivirano 26. 3. 2012. na Wayback Machine
- https://web.archive.org/web/20120928053846/https://www.ts2.pl/en/News/1/56
- https://www.bigwall.dk/galleri/klatring/tasermiu/pages-uk/uk05keti.htm
- https://web.archive.org/web/20081217084704/https://www.americanalpineclub.org/AAJO/pdfs/1986/175_canada_greenland_aaj1986.pdf
- https://www.eoearth.org/article/Abiotic_factor?topic=49461
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