Pregled bibliografske jedinice broj: 538369
Plitvice Lakes – a hydrogeologic phenomenon
Plitvice Lakes – a hydrogeologic phenomenon // SOWAEUMED Case Study I: Monitoring of Water and Lake Sediment Quality in Natural Environment: Programme and Abstracts / Krajcar Bronić ; Ines ; Obelić ; Bogomil (ur.).
Zagreb: Institut Ruđer Bošković, 2011. str. 10-10 (predavanje, nije recenziran, sažetak, stručni)
CROSBI ID: 538369 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Plitvice Lakes – a hydrogeologic phenomenon
Autori
Juračić, Mladen ; Felja, Igor
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, stručni
Izvornik
SOWAEUMED Case Study I: Monitoring of Water and Lake Sediment Quality in Natural Environment: Programme and Abstracts
/ Krajcar Bronić ; Ines ; Obelić ; Bogomil - Zagreb : Institut Ruđer Bošković, 2011, 10-10
Skup
SOWAEUMED - Case Study I : Monitoring of water and lake sediment quality in natural environment
Mjesto i datum
NP Plitvička jezera, Hrvatska, 29.05.2011. - 01.06.2011
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Nije recenziran
Ključne riječi
karst; freshwater lakes
Sažetak
In the presentation an explanation for the existence of freshwater Plitvice Lakes in Dinaric karst will be presented. Formerly the existence of the Plitvice lakes was considered a “miracle” due to the fact that generally in the high karst region underground water flow prevails. The area where Plitvice Lakes are located is built of carbonate rocks of Mesozoic age. There is a thick series of dolomite and limestone rocks (3500 – 4000 m) that were deposited from Upper Triassic (T3 “Hauptdolomit”) to Upper Cretaceous (K2 rudist limestone and marly (clayey) limestone). In the upper part (below Upper Lakes) this Triassic dolomite covers older impermeable clastic rocks, and the formation of surface flow is easily explained. However, the Lower Lakes are formed in Upper Cretaceous well karstified limestone with a number of caves in the canyon flanks. The only plausible explanation is that a series of marly (clayey) limestone of Turonian age (K22) represents a barrier for underground flow. Therefore, the litholology could explain the existence of the surface water flow. The existence of the lakes is, however, the consequence of intense deposition of calc tufa within the water flow. Mechanisms, chemistry and biogeochemistry of calc tufa deposition are important topic of the ongoing research in the world.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119-1191152-1169 - Recentni sedimenti i fosilni okoliši jadranskog priobalja (Juračić, Mladen, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Mladen Juračić
(autor)