Raznovrstnost kraških površinskih reliefnih oblik na karbonatnem krasu
DOI:
https://doi.org/10.3986/ac.v50i2-3.10082Ključne besede:
kras geografskih pasov, visokogorski kras, majhna reliefna kraška oblika, velika reliefna kraška oblika, raznovrstnostPovzetek
V prispevku je opisana raznovrstnost majhnih, srednjih in velikih korozijskih reliefnih oblik, v krasu različnih geografskih pasov in v visokogorskem krasu. Upoštevano je bilo, kako se raznovrstnost spreminja glede na oddaljenost od ekvatorja pri majhnih, srednjih in velikih reliefnih oblikah v različnih geografskih pasovih ter kako se spreminja glede na spreminjanje nadmorske višine pri škrapljah (drobne oblike) na visokogorskem krasu. Ugotoviti je mogoče, da se raznovrstnost kraških reliefnih oblik zmanjšuje glede na oddaljenost od ekvatorja (neodvisno od velikosti teh oblik), v visokogorju pa se raznovrstnost škrapelj z višanjem nadmorske višine sprva povečuje, nato pa se zmanjšuje. Zmanjševanje raznovrstnosti srednjih in velikih reliefnih oblik, značilno za čedalje večjo oddaljenost od ekvatorja, je mogoče pojasniti z zmanjševanjem intenzivnosti raztapljanja. Spreminjanje raznovrstnosti škrapelj pa kaže povezavo z raznovrstnostjo naklona pobočja, na katerem nastajajo. Na območjih tropskega krasa in na srednje visokih območjih visokogorja (1600–2100 m), kjer se pojavljajo obsežna gola pobočja z različnim naklonom pobočja, je raznovrstnost škrapelj zelo velika. Na tropskem krasu so pobočja z različnim naklonom nastala z zakrasevanjem, v visokogorju pa z ledeniško erozijo.
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