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Photogrammetry and Remote Sensing2020

DYNAMIC BALANCE OF THE LANDSCAPE MORPHOLOGICAL PATTERN OF ALLUVIAL PLAINS: THE QUANTITATIVE ASPECT

A. S. Victorov, Maria Archipova, O. N. Trapeznikova · SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 20th International Multidisciplinary Scientific GeoConference Proceedings SGEM 2020, Informatics, Geoinformatics and Remote Sensing

DOImathematical morphology of landscapesalluvial plainsthe morphological pattern of landscapedynamic balance of morphological pattern
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Hydrogeology, Engineering Geology and Geotechnics2017

IMPACT OF THE RIVER LEVEL REGIME ON THE GROUNDWATER DYNAMICS AND PHYSICOCHEMICAL CHARACTERISTICS OF THE ALLUVIAL AQUIFER IN THE OGOSTA VALLEY

Peter Gerginov · SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 17th International Multidisciplinary Scientific GeoConference SGEM2017, Science and Technologies in Geology, Exploration and Mining

DOIgroundwater - surface water interactiongroundwater levelregimealluvial aquiferOgosta River
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Ecology and Environmental Protection2017

SIGNIFICANCE OF RELIEF-FORMING ACTIVITIES BY CASTOR FIBER L. FOR THE EVOLUTION OF HOLOCENE FLOODPLAINS OF SMALL RIVER VALLEYS (RESULTS OF STUDIES CONDUCTED IN POLAND)

Snieszko Zbigniew, Miroslaw Rurek, Mariusz Rzetala · SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 17th International Multidisciplinary Scientific GeoConference SGEM2017, Science and Technologies in Geology, Exploration and Mining

DOIalluviasedimentspeatsbeaverssmall riversponds+2 keywords
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Hydrogeology, Engineering Geology and Geotechnics2011

APPLIED POTENTIAL OF SATELLITE DATA IN THE DETERMINATION OF GROUNDWATER RESOURCES IN DAMBOVICIOARA AREA, ROMANIA

Mădălina Nicoleta Frînculeasa · SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; SGEM2011 11th International Multidisciplinary Scientific GeoConference

DOIRemote sensingliniamentsgroundwaterstructural-tectonic elements 1. LOCALIZATIO1 Situated in a transitional area between the flysch zone of the Oriental Carpathians and the crystalline zone of the Southern Carpathiansthe DГўmbovicioara Corridor appears as a large depressionshaped as a parallelogr am+264 keywords
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