APA 6th Edition Surić, M. (2005). Submerged Karst – Dead or Alive? Examples from the Eastern Adriatic Coast (Croatia). Geoadria, 10 (1), 5-19. https://doi.org/10.15291/geoadria.71
MLA 8th Edition Surić, Maša. "Submerged Karst – Dead or Alive? Examples from the Eastern Adriatic Coast (Croatia)." Geoadria, vol. 10, br. 1, 2005, str. 5-19. https://doi.org/10.15291/geoadria.71. Citirano 14.04.2021.
Chicago 17th Edition Surić, Maša. "Submerged Karst – Dead or Alive? Examples from the Eastern Adriatic Coast (Croatia)." Geoadria 10, br. 1 (2005): 5-19. https://doi.org/10.15291/geoadria.71
Harvard Surić, M. (2005). 'Submerged Karst – Dead or Alive? Examples from the Eastern Adriatic Coast (Croatia)', Geoadria, 10(1), str. 5-19. https://doi.org/10.15291/geoadria.71
Vancouver Surić M. Submerged Karst – Dead or Alive? Examples from the Eastern Adriatic Coast (Croatia). Geoadria [Internet]. 2005 [pristupljeno 14.04.2021.];10(1):5-19. https://doi.org/10.15291/geoadria.71
IEEE M. Surić, "Submerged Karst – Dead or Alive? Examples from the Eastern Adriatic Coast (Croatia)", Geoadria, vol.10, br. 1, str. 5-19, 2005. [Online]. https://doi.org/10.15291/geoadria.71
Sažetak Numerous karst features submerged by the Late Pleistocene-Holocene transgression are found along the Eastern Adriatic (Croatian) coast. Generally, most of karstification processes cease at the base level, that is, in case of coastal karst, the sea level. However, evidence of continued karstification (corrosion) and related processes (mechanical erosion and bioerosion), as well as remarkable change in hydrogeological settings of some hydrological systems, are quite common in Croatian submarine and coastal area.