Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Jovan Zoto"'
Publikováno v:
Acque Sotterranee, Vol 6, Iss 1 (2017)
Karst aquifers are characterized by high heterogeneity of groundwater flow. The classical study methods such as boreholes, pumping tests, and point observations give important data but cannot be extended to the entire aquifer. However the environment
Externí odkaz:
https://doaj.org/article/f7323cfc49a44ff8817e008dcd315924
Publikováno v:
Acque Sotterranee, Vol 6, Iss 1 (2017)
Karst aquifers are characterized by high heterogeneity of groundwater flow. The classical study methods such as boreholes, pumping tests, and point observations give important data but cannot be extended to the entire aquifer. However the environment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::98e00bcddedfdec5bd7b561a7cc45271
https://doi.org/10.7343/as-2017-257
https://doi.org/10.7343/as-2017-257
Autor:
Romeo Eftimi, Alqiviadis Stamos, Sokrat Amataj, Jovan Zoto, Ioannis Leontiadis, Ralf Benischke, Laurence Gourcy, Eftim Micevski, Todor Anovski, Liliana Kola
Publikováno v:
Environmental Geology. 51:749-753
Prespa Lake and Ohrid Lake constitute a hydraulic system shared between Albania, FYR of Macedonia and Greece. Karst rocks separate both lakes. The elevation of Prespa Lake is about 150 m higher than that of Ohrid Lake. Considering these facts, Cvijic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ac4a6a4b52f7d799bf9144d30671fdd
https://doi.org/10.1007/s00254-006-0388-9
https://doi.org/10.1007/s00254-006-0388-9
Publikováno v:
Geologica Balcanica. 32:43-49
Two big lakes are located in southeastern Albania, near the border with Former Yugoslav Republic of Macedonia (FYROM), Prespa Lake at elevation 850 m above sea level (a.s.l.), and Ohrid Lake at elevation 695 m a.s.l. Mali Thate – Galichica Mountain
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d448948187611f074fb22c57152816f
https://doi.org/10.52321/geolbalc.32.1.43
https://doi.org/10.52321/geolbalc.32.1.43