315 research outputs found
Az optikai lumineszcens kormeghatĂĄrozĂĄs pontossĂĄgĂĄnak növelĂ©se futĂłhomok-terĂŒletekrĆl szĂĄrmazĂł mintĂĄk esetĂ©ben = Increasing the accuracy of optical dating on fixed sand dune areas
KutatĂĄsaink sorĂĄn hazĂĄnk legnagyobb fĂ©lig kötött futĂłhomok-terĂŒleteinek holocĂ©n eolikus fejlĆdĂ©sĂ©t vizsgĂĄltuk 11 mintaterĂŒleten gyƱjtött mintegy 100 db minta lumineszcens kormeghatĂĄrozĂĄsĂĄval. Kimutattuk, hogy a klimatikusan vezĂ©relt preboreĂĄlis eolikus tevĂ©kenysĂ©gen tĂșl lokĂĄlisan ârĂ©szben emberi hatĂĄsraâ szinte bĂĄrmelyik holocĂ©n fĂĄzisban megindulhatott a homok. KirajzolĂłdtak azok az idĆszakok is, amikor tĂ©rben Ă©s idĆben is gyakoribbak lehettek az eolikus esemĂ©nyek. Ăgy a NyĂrsĂ©gben Ă©s BelsĆ-Somogyban az atlantikus fĂĄzisban talĂĄltunk bizonyĂtĂ©kokat a homokmozgĂĄsra, ami a neolitikum emberĂ©nek Ă©getĂ©ses talajvĂĄltĂł gazdĂĄlkodĂĄsĂĄra vezethetĆ vissza. A Duna-Tisza közĂ©n ellenben kĂ©sĆbb, a szubboreĂĄlis fĂĄzisban azonosĂthatĂł jelentĆsebb eolikus tevĂ©kenysĂ©g, ami fĆkĂ©nt a bronzkori nagyĂĄllat-tartĂĄsnak Ă©s legeltetĂ©snek tudhatĂł be. Szinte minden mintaterĂŒleten markĂĄnsan jelentkeztek a nĂ©pvĂĄndorlĂĄs Ă©s honfoglalĂĄs kori homokmozgĂĄsok ĂŒledĂ©kei, ami az elĆzĆeknĂ©l nagyobb âakĂĄr regionĂĄlis kiterjedĂ©sƱâ a szĂĄrazabb klĂma Ă©s a legeltetĂ©ses terĂŒlethasznĂĄlat ĂĄltal egyĂŒttesen vezĂ©relt eolikus tevĂ©kenysĂ©get feltĂ©telez. VĂ©gĂŒl rĂĄmutattunk, hogy a 18.-19. szĂĄzadi homokverĂ©sek sorĂĄn a Duna-Tisza köze központi terĂŒletein jelentĆs mĂ©retƱ, 5-8 m magas garmadĂĄk alakultak ki nĂ©hĂĄny Ă©vtized leforgĂĄsa alatt. KutatĂĄsaink tovĂĄbbi hozadĂ©ka, hogy a mĂłdszert fluviĂĄlis ĂŒledĂ©keken is teszteltĂŒk, valamint megteremtettĂŒk MagyarorszĂĄgon a lumineszcens kormeghatĂĄrozĂĄs rĂ©gĂ©szeti-archeometriai alkalmazĂĄsĂĄnak feltĂ©teleit. | We investigated Holocene aeolian activity on the largest stabilised sand dune areas of Hungary by dating almost 100 sand samples from 11 study sites. It has been shown that following Preboreal climate driven events local deflation could occur practically at any time during the Holocene as a consequence of human disturbance. We have identified however those periods when these local events were more frequent both in temporal and spatial terms. Thus, both the NyĂrsĂ©g and the Somogy Alluvial Fan provided evidence for Atlantic Phase blown sand formation, which can probably be traced back to the slash and burn agricultural practice of Neolithic people. On the Danube-Tisza Interfluve nevertheless, these evidence were missing and Subboreal events were identified, referring to significant Bronze Age disturbance by the extensive grazing of livestock. Migration Period blown sand deposits were found in great abundance nearly at all sites, suggesting a more general âsometimes regionalâ aeolian activity, which was driven thus both by climate and contemporary agricultural practice. Finally we determined the intensity of aeolian accumulation in the 18-19th c. and found that 5-8 m high dunes could develop in a matter of a few years on the central parts of the Danube-Tisza Interfluve. Additional achievements during the research period were the investigation of fluvial sediments and the establishment of the basis of archaeological-archaeometrical application of luminescence dating in Hungary
Effect of climate change on the hydrological character of River Maros, Hungary-Romania : Effect of climate change on the hydrological character of river Maros, Hungary-Romania
Identification and characterization of a novel circadian clock mutant in Arabidopsis thaliana
Changes of cross-sectional morphology and channel capacity during an extreme flood event, lower Tisza and Maros rivers, Hungary
When examining the characteristics of individual floods Hungarian researchers primarily investigate hydrological and hydraulic processes, whilst the relation between flood events and morphological changes of the river-bed are widely ignored. The present research quantifies the morphological changes of two cross-sections of the lowland reaches of the River Tisza and its tributary, the River Maros, during a high magni-tude flood which occurred in spring 2000. During the flood several key morphological cross-section variables (mean depth, channel bed eleva-tion, maximum depth, cross-sectional area and channel capacity) were monitored. Relationships between these data and daily river stage height series of the flood and specific stream power were determined. Results suggest that the identified morphological changes highly affect the channel capacity of the two cross-sections during the flood event. The channel capacity changes (9-10%) were almost identical for both study sites. However, different morphological processes characterised the two cross-sections. We found that morphological parameters de-pend not only on the actual stream power, but the available amount of sediment for transport, the rate of stage and stream power change
An Enigmatic Funnel Find of the SomogyvĂĄr-Vinkovci Culture from BalatonĆszöd-TemetĆi dƱlĆ in Transdanubia, Hungary
A small section of an Early Bronze Age settlement made up of pits was uncovered at the prehistoric,
multi-period site of BalatonĆszöd-TemetĆi dƱlĆ. In addition to ceramics of the SomogyvĂĄr-Vinkovci
culture, the finds from Pit 2563 included an enigmatic artefact of baked clay. Despite the fact that
analogous archaeological finds and various archaeometric analyses have provided several clues for
a conclusive determination of its function, comparable finds nonetheless suggest that it might in all
probability be associated with dairying or metalworking
Geomorphological processes along the lowland sections of the Maros/MureĆ and Körös/CriĆ Rivers
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