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Wyświetlanie 1-2 z 2
Tytuł:
Correlation of genetic and morphometric types of Šventoji River catchment relief (north-east Lithuania)
Autorzy:
Česnulevičius, A.
Morkunaite, R.
Powiązania:
https://bibliotekanauki.pl/articles/2059179.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Šventoji catchment
relief genesis
morphometric types of relief
Opis:
The Šventoji is a river of the Baltic Upland. The catchment of the Šventoji is teardrop-shaped up to 50–60 km wide, and 160 km long. Most of the catchment is situated in the Aukštaičiai Upland and the Western Aukštaičiai Plateau. The surface of the catchment was formed by Quaternary ice sheets that deposited a moraine layer 100–200 m, the thick topographic relief dating to the late Nemunas (Weichselian) Glaciation phases. The eastern part of catchment was formed in the East Lithuanian Phase, the middle part in the South Lithuanian Phase and the western part in the Middle Lithuanian Phase. The catchment surface is composed of three different genetic relief types: the ice-marginal deposits of the East Lithuanian Phase, represented by small hills; the middle part of the Šventoji catchment, transected by a few ice-marginal ridges of the South Lithuanian Phase which form small hills; and the western part of the catchment is transected by a few asymmetric ridges of the Middle Lithuanian Phase. The eastern part dominantly comprises ice-marginal deposits with glaciolacustrine and glaciofluvial intercalation; the middle part comprises variable glaciolacustrine, basal moraine and ice-marginal deposits; the western part by basal moraine and ice-marginal deposits.
Źródło:
Geological Quarterly; 2003, 47, 2; 149-154
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Changes in quantitative parameters of active wind dunes on the south-east Baltic Sea coast during the last decade (Curonian Spit, Lithuania)
Autorzy:
Morkūnaitė, R.
Bautrėnas, A.
Česnulevičius, A.
Dobrotin, N.
Baubinienė, A.
Jankauskaitė, M.
Kalesnikas, A.
Mačiulevičiūtė-Turlienė, N.
Powiązania:
https://bibliotekanauki.pl/articles/2059357.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Curonian Spit
aeolian processes
coastal dunes
penetrating radar
GPR
dynamics
Opis:
The Curonian Spit is one of the largest Holocene sand accumulation forms, stretching along the Baltic Sea coast and belonging to the Baltic sand belt. This article deals with the dynamics of the Curonian Spit dunes in the context of global climate change. Investigations were carried out in the environs of two high dunes (Parnidis Dune and Naglis Dune) over a period of 10 years (2003-2014). Levelling of cross-sections was performed using modern geodesic devices. Wind velocities and directions were measured at meteorological stations of Klaipeda and Nida. The wind regime (number of days with winds >15 m/s) was almost at the multiannual average during the study period. Sand moisture was measured in both dunes studied, and groundwater level was measured in the environs of the Naglis Dune by using ground penetrating radar (GPR). The Naglis Dune experienced a more significant lowering (by 4-6 m) compared with the Parnidis Dune over the study period, while sand deficit was greater in the Parnidis Dune (~10,000 m3). Compared with other European sand dune systems, the Curonian Spit dunes have undergone strong degradation. The article highlights possible degradation reasons and indicates the necessity of additional investigations. Only long-term investigations can contribute to disclosing the main processes both as natural background and due to anthropogenic activities, and the devising of protection measures.
Źródło:
Geological Quarterly; 2018, 62, 1; 38--47
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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