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dc.contributor.authorKostiuk, Uliana
dc.contributor.authorPopiuk, Yana
dc.contributor.authorRidush, Bogdan
dc.date.accessioned2023-11-14T07:41:40Z
dc.date.available2023-11-14T07:41:40Z
dc.date.issued2023-09-14
dc.identifier.citationKostiuk U., Popiuk Ya., Ridush B. The development of gypsum karst in Northern Bukovyna in Late Pleistocene – Holocene. The 7th Conference on Regional Climate and Environmental Dynamics: GEOSCIENCE IN THE CARPATHIAN AND BLACK SEA REGION (GCBS 2023) VATRA DORNEI, SUCEAVA COUNTY, ROMANIA, 14-17 SEPTEMBER 2023 INQUA REGIONAL MEETING. P. 43-45.uk_UA
dc.identifier.urihttps://archer.chnu.edu.ua/xmlui/handle/123456789/7626
dc.description.abstractKarst development in the northern part of Northern Bukovyna is controlled by lithology, geology, and tectonic settings, as well as cycles of chemically active water. We can determine the signs of karst development by the morphology of the cave passages, as well as by the available cave deposits (paleogeographic sights). Also, karst development is influenced by human economic activity, which has been started in this region at least since the Neolithic. The development of epigenic karst and karst denudation is still active in the territory, but its history in Late Pleistocene and Holocene should be traced after the karst sediments research. At present, it is enhanced by anthropogenic factors, in particular, economic development of the territory (ploughing, reduction of forests cove, runoff regulation etc.).uk_UA
dc.language.isoenuk_UA
dc.publisherThe 7th Conference on Regional Climate and Environmental Dynamics: GEOSCIENCE IN THE CARPATHIAN AND BLACK SEA REGION (GCBS 2023) VATRA DORNEI, SUCEAVA COUNTY, ROMANIA, 14-17 SEPTEMBER 2023 INQUA REGIONAL MEETINGuk_UA
dc.subjectGypsum, karst, Holocene, cave, Chornyi Valley, Balamutivka villageuk_UA
dc.titleThe development of gypsum karst in Northern Bukovyna in Late Pleistocene – Holoceneuk_UA
dc.typeThesisuk_UA


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