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Studie současné úrovně a možností dalšího doplnění zeleně v mikroregionu IvančickoHoffmannová, Eva January 2010 (has links)
No description available.
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Rozvojový potenciál vybraného venkovského mikroregionu: případová studie Dolní KouniceHladká, Dana January 2012 (has links)
No description available.
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Veřejná prostranství malých městHošková, Veronika January 2013 (has links)
No description available.
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Zhodnocení potenciálu viničních tratí v mikroregionu Dolní KouniceKárník, Pavel January 2013 (has links)
No description available.
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Posouzení druhového zastoupení obojživelníků (Amphibia) na různě antropogenně ovlivněných biotopechKrejčová, Veronika January 2013 (has links)
No description available.
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Sledování druhového a početního zastoupení obojživelníků (Amphibia) a plazů (Reptilia) v oblasti Dolní MarkloviceNytra, Lukáš January 2010 (has links)
No description available.
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Návrh úprav v nivě toku Šporka v k.ú. Česká LípaPytloun, Miroslav January 2008 (has links)
No description available.
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Rizika těžby a úpravy uranových rud v ČR na modelovém území ložisek Rožná a Stráž pod RalskemJuřička, David January 2012 (has links)
No description available.
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Studium fluidních inkluzí v pegmatitech ze Skalska u Jílového a z Dolních Borů / Fluid inclusion study of pegmatites from Skalsko near Jílové and Dolní BoryFenclová, Kateřina January 2010 (has links)
Fluid inclusions of pegmatites from two localities in the Moldanubina Zone were studied in order to constrain P-T conditions of their crystallization and enstablish composition and properties of fluids associated with pegmatite formation. The first locality Skalsko (near Jílové u Prahy) is located within the Central Bohemian Plutonic Complex (CBPC) of Variscian age.Pegmatitic dykes represent the late stage of magmatic evolution of the CBPC. Pegmatite is hosted by biotite-granodiorite of the "Požáry" and "Sázava" types and probably belongs to the muscovite class of the pegmatites. The other locality, Dolní Bory, is located within the Bory granullite Massif ( metamorphism is dated to about 340 Ma). Following types of pegmatite occur in this district: 1. barren to less evolved pegmatites; 2. more evolved phosphate-bearing pegmatites and 3. Li-complex, the most evolved pegmatites. The studied material comes from an andalusite-diaspore nodule hosted by blocky quartz of the barren pegmatite (pegmatite dike No. 3). Fluid inclusions were studied mostly in quartz (Skalsko, Dolní Bory), andalusite and diaspore (Dolní Bory). Fluids trapped in samples from Skalsko correspond to H2O-CO2 and H2O types. The H2O-CO2 fluid had relatively low salinity (4,1-5,9 wt.% NaCleq), contained from 20 to 5 mol.% CO2 and its...
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Marketingové zhodnocení lyžařského areáluHuňková, Lenka January 2014 (has links)
My thesis is focused on the marketing evaluation of the visitors of Dolni Morava Relax & Sport Resort during the winter season. The main content of the thesis is the description of the current state and consequent evaluation of satisfaction with offered service. Identification of the client is also important. The thesis includes theoretical part which defines basic terms related to marketing, services and tourism and of practical part which consists of the characteristics of the resort, description of the service and results of a survey. The conclusion is dedicated to suggestions and recommendations.
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