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Dynamicky orientovaný hierarchický geomorfologický informačný systém (prípadová štúdia Ľubietová)
Názov Dynamicky orientovaný hierarchický geomorfologický informačný systém (prípadová štúdia Ľubietová) Podnázov dizertačná práca Aut.údaje Alžbeta Medveďová; školiteľ: Jozef Minár Autor Medveďová Alžbeta 1971- (100%) UMBFP01 - Katedra geografie a geológie
Ďalší autori Minár Jozef (Školiteľ (konzultant))
Korp. Vyd.údaje Bratislava : Univerzita Komenského, Prírodovedecká fakulta, Katedra fyzickej geografie a geoekológie , 2010. - 138 s. Kľúč.slová geomorphological information system (GmIS) morphodynamic phenomena geomorphological database Heslá geogr. Ľubietová (Slovensko) Jazyk dok. slovenčina Krajina Slovenská republika Systematika 550 Anotácia Geomorhpological information system (GmIS) is a special type of GIS suitable for collection, elaboration and presentation of geomorphological data. GmIS is an excellent tool for efficient storage and generating new geomorphological information as well as for visualization of outputs. In our contribution the build-up of a tool for complex (temporal and spatial) study of gravitational deformations in the Ľubietová territory is presented. The hierarchical system approach is applied to the investigation of one of the most active subsystems in the context of the whole supersystem. In our case the basic system corresponds to a paradynamic gravity-fluvial system (Hutná stream with its tributaries and neighboring slopes), its most active subsystem is the system of the gravitational deformation (i.e. the last landslide activated in 1977), and the supersystem refers to a higher-order system, i.e. to the neotectonical system of the territory. All dynamic processes have certain temporal and spatial hierarchy. Neotectonics are considered as a processes of several million years time-scale described within the spatial scale of 1:50 000. Gravity-fluvial system is studied in the scale of 1:10 000 in the range of 105 – 106 years. The most detailed temporal (few decades) and spatial (1:5 000) scales are used for the subsystem of the active landslide. The vertical scale (in our case expressed in meters to kilometers) plays also an important role in the study of landslide processes. Both spatial hierarchies are mutually related (not deterministically) – processes of smaller extent are described in the larger scale. The dynamically oriented hierarchic GmIS focuses on morphodynamic phenomena as well as on the multilevel hierarchy of geomorphological database. Geomorphological data can be digitally stored as a powerful database with thematic layers and attribute tables. ESRI ArcGIS is suggested to manage the geomorphological data. Kategória publikačnej činnosti DAI Číslo archívnej kópie 18218 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ 
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