2007
DOI: 10.1016/j.jhydrol.2006.10.029
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The Aggitis karst system, Eastern Macedonia, Greece: Hydrologic functioning and development of the karst structure

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Cited by 22 publications
(6 citation statements)
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“…It was also found that the very good drainage of the aquifers corresponds to a developed karst system. (c) The karst system hosted in the marbles of Aggitis presented similar results regarding the autocorrelation and cross-correlation functions, and thus similar characteristics with the above-mentioned systems [13]. The lag time of 50 days for the autocorrelation function was attributed to the system's long memory, corresponding to an increased storage, which could explain the huge water reserves that were calculated by the recharge area of the springs.…”
Section: The Role and Presence Of The Epikarstic Zone In General Andsupporting
confidence: 56%
See 1 more Smart Citation
“…It was also found that the very good drainage of the aquifers corresponds to a developed karst system. (c) The karst system hosted in the marbles of Aggitis presented similar results regarding the autocorrelation and cross-correlation functions, and thus similar characteristics with the above-mentioned systems [13]. The lag time of 50 days for the autocorrelation function was attributed to the system's long memory, corresponding to an increased storage, which could explain the huge water reserves that were calculated by the recharge area of the springs.…”
Section: The Role and Presence Of The Epikarstic Zone In General Andsupporting
confidence: 56%
“…The most well-known studies focus on the central Peloponnese and Western Greece, where the carbonate formations of the Ionian, Gavrovo-Tripolis, and Olonos-Pindos zones are mainly developed. Additionally, individual studies provide important information for other areas, for example [8] for the Pre-Apulian zone, [9,10] for the Parnassos-Giona zone, [11] for the Pelagonian and Attico-Cycladic zones, [12] for the Koziakas Mountain, [13] for the crystalline limestones of the Rhodope massif, and others [14].…”
Section: The Hellenic Karstmentioning
confidence: 99%
“…Long‐term isolation is also supported by the occurrence of the endemic fish Cobitis punctilineata Economidis & Nalbant and the endemic lamprey Eudontomyzon hellenicus Vladykov, Renaud, Kott & Economidis in the Aggitis River. The Aggitis Spring is part of a well developed and complex karst network, which has existed at least since Pliocene (Novel et al , 2007) and is characterized by constant conditions that seem to have supported fish populations long enough to develop a pronounced divergence from other populations.…”
Section: Discussionmentioning
confidence: 99%
“…During the last decades, The river flow is generated by water inputs of an extensive underground karst system, and flows as an underground river at Aggitis (or Maara) Cave [45]. The Aggitis springs are located at the outlet of the cave [46]. The river crosses the plain of Drama Prefecture along with other major streams, then flows through a small gorge "Aggitis Gorge" near Alistrati Cave, and finally contributes to Strymonas River which ends in Strymonikos Gulf in the North Aegean Sea [47,48].…”
Section: Introductionmentioning
confidence: 99%