From the viewpoints of regional and agrarian geography and regional planning the author systematically analyze all main natural features and many regional social factors of the municipality of ...Moravče: bedrock, type of relief, altitude, inclination, water conditions (including flood conditions), climate conditions (particularly insolation), soil and vegetation, land use, population, settlements, and economy. On the basis of the analysis, a detailed partition of the municipality into small homogenous units is made, three in the valley and four in the hills. The book also deals with the evaluation of the landscape from the viewpoint of individual types of agricultural land use~determines the suitability of areas for cultivated fields, meadows, and orchards~and considers the quality of locations from the viewpoint of settlement. The book concludes with recommendations for the most suitable land use and a survey of the current irrational use of land.The synthetic maps and theme maps showing individual natural factors can be used to advantage in regional planning. Emphasis is placed on determining the interdependence of landscape factors and their joint influences, on the laws and causes governing individual phenomena, and on the comparison of microregions.
Moravče je mjesto u sesvetskome Prigorju; u suvremenoj administrativnoj podjeli dio je Grada Zagreba, na njegovu krajnjem sjeveroistočnom rubu. Kajkavski govor Moravča prema Ivšićevoj podjeli pripada ...konzervativnoj zagorsko-međimurskoj skupini, što znači da se u njemu u velikoj mjeri čuva tzv. osnovna kajkavska akcentuacija, odnosno da nije zahvaćen naglasnim inovacijama u pogledu intonacije dugih naglasaka ili pomicanja naglasnoga mjesta. Time to rubno prigorsko mjesto pokazuje neke osnovne akcenatske karakteristike koje velikim dijelom obilježavaju govore središnjega dijela Hrvatskoga zagorja. Govor je troakcenatski, bez nenaglašenih dužina (uz jednu iznimku) i bez oksitoneze. Sekundarno naglašeni predzadnji slogovi, jednako oni s polaznom dužinom kao i oni s polaznom kračinom, naglašeni su akutom (pere 'pero', im. petạ 'peta'). Akut je u zadnjem ili jedinom slogu zamijenjen cirkumfleksom. Inventar dugih naglašenih samoglasnika broji devet fonema; taj je broj rezultat vokalsko-akcenatskog razvoja u kojem je došlo do duženja sekundarno naglašenoga polazno kratkog sloga, pri čemu se u dijelu vokala naknadno produženi samoglasnici razlikuju od polazno dugih.
Govor je u radu analiziran prvenstveno s gledišta fonologije, a donose se i neki osnovni morfološki podaci.
Provider: - Institution: - Data provided by Europeana Collections- Moravče – trg s spomenikom Jurija Vege. Razglednica ni bila odposlana.- All metadata published by Europeana are available free of ...restriction under the Creative Commons CC0 1.0 Universal Public Domain Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Provider: - Institution: - Data provided by Europeana Collections- All metadata published by Europeana are available free of restriction under the Creative Commons CC0 1.0 Universal Public Domain ...Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
The Komjatice depression, situated on the Danube Basin’s northern margin, represents a sub-basin of the Neogene epicontinental Central Paratethys Sea and Lake Pannon. The paper provides an insight ...into the character of sediment provenance evolution by study of well cores (ZM-1, IV-1, MOJ-1, VR-1 wells). A modern combination of provenance, sedimentology and biostratigraphy together with the reported redefinition of Pannonian formations resulted in a new lithostratigraphy of the study area. Moreover, newly published volcanic rock age data were used for calibration of biostratigraphy. The overall age span of the sedimentary fill is occupied only by late Badenian–Sarmatian (Serravallian) to Pannonian (Tortonian–Messinian) strata: 1) the basal alluvial sediments of the newly defined Zlaté Moravce Formation; 2) late Badenian–Sarmatian (Serravalian) marine sediments of the Vráble-Pozba Fm., connected with tectonic opening of the depression; 3) Pannonian (Tortonian) coarse grained sediments of the Nemčiňany Fm. with an erosional base; 4) Pannonian (Tortonian–Messinian) predominantly fine-grained, basin floor to slope Ivanka Fm., sandy deltaic Beladice Fm. and predominantly muddy, alluvial Volkovce Fm. In the middle Miocene provenance is situated in Paleozoic sequences and Neogene volcanic rocks occurring currently in the NE. During the late Miocene, provenance is changed to the NNW (Tribeč Mts.), although the transport from the NE also remained.
The microseismic survey method was applied to the study of the geological structures in the region around the Mochovce nuclear power plant. The previous geological and geophysical investigations ...considered a contact between the Miocene volcanites and sediments as a neotectonic fault. The results of the microseismic investigations allow us to interpret the zone of a supposed neotectonic fault as a transgressive contact of the sediments and the volcanic rocks without a tectonic disruption.
Provider: - Institution: - Data provided by Europeana Collections- All metadata published by Europeana are available free of restriction under the Creative Commons CC0 1.0 Universal Public Domain ...Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
Provider: - Institution: - Data provided by Europeana Collections- All metadata published by Europeana are available free of restriction under the Creative Commons CC0 1.0 Universal Public Domain ...Dedication. However, Europeana requests that you actively acknowledge and give attribution to all metadata sources including Europeana
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