Temat: Orłowo Cliff - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Morpholithodynamical changes of the beach and the nearshore zone under the impact of submerged breakwaters — a case study (Orłowo Cliff, the Southern Baltic)
Autorzy:: Kubowicz-Grajewska, A.
Powiązania:: https://bibliotekanauki.pl/articles/49145.pdf
Data publikacji:: 2015
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: breakwater
beach
morpholithodynamics
Orlowo Cliff
Southern Baltic
Polish coast
nearshore zone
Źródło:: Oceanologia; 2015, 57, 2
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Tytuł:: Cementacja węglanowa osadów piaszczystych klifu w Gdyni-Orłowie
Carbonate cementation of sandy sediments on the cliff in Gdynia-Orłowo
Autorzy:: Ciborowski, T.
Jankowski, M.
Powiązania:: https://bibliotekanauki.pl/articles/2074554.pdf
Data publikacji:: 2007
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: cementacja węglanowa
osady piaszczyste
klif w Gdyni-Orłowie
Zatoka Gdańska
carbonate cementation
sandy sediments
Orłowo Cliff
Gulf of Gdansk
Opis:: Carbonate cementation of sandy sediments is most common in tropical and subtropical climate, and quite rare in temperate climate. About 20 sites where carbonate cemented sandstones occur are known throughout the Polish Lowlands. A new outcrop of carbonate cemented sandstone was found near Gdynia-Orłowo (coast of the Gulf of Gdańsk). Field studies and microscopic analyses [optical microscopy and SEM] let to recognise the pattern of cementation of sandy sediments. Origin of the sandstones is connected with infiltration of rain water into glacial till (partially cracked). This till is the source of calcium carbonate transported by water into underlying fluvioglacial sands. Because of different sediments porosity and resulting degassing of CO2, CaCO3 precipitated. Additionally, elevated temperature and evaporation of water may also create favorable condition for precipitation. The process of cementation is related to the exposition of fluvioglacial sands layer caused by cliff abrasion (about 1 m per year). The best geochemical conditions for precipitation of CaCO3 are in the zone of contact with atmosphere, so this cementation seems to be recent. Carbonate cemented sandstones formed below the glacial till fall down and may be found in the colluvium of the cliff slope.
Źródło:: Przegląd Geologiczny; 2007, 55, 2; 140-145
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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Tytuł:: Budowa geologiczna i glacitektonika klifu orłowskiego w Gdyni
Geology and glaciotectonics of the Orłowo Cliff in Gdynia, northern Poland
Autorzy:: Kaulbarsz, D.
Powiązania:: https://bibliotekanauki.pl/articles/2074343.pdf
Data publikacji:: 2005
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: Klif orłowski
analiza strukturalna
deformacja glacitektoniczna
geneza glin zwałowych
zlodowacenie Wisły
zlodowacenie Odry
stadiał świecia
Orłowo Cliff
Baltic shore
glaciotectonic deformations
structural analysis
Odranian Glaciation
Warthanian Glaciation
Vistulian glaciation
Świecie Stadial
Main Stadial
Opis:: The Orłowo Cliff is built of glacial and fluvioglacial deposits, Middle Polish Glaciations (possibly Odranian and Warthanian) and Vistulian Glaciation. Deposits are heavily deformed glaciotectonically. In the northern part of the cliff, Miocene sediments are exposed. It is possible, that the Miocene sediments were dislo-cated from their primary position. There were observed overthrusts and intermingling with Pleistocene material in the lower part of the exposure. The Orłowo Headland is built of glacial tills. It is probably a part of fold, similar in pattern to the structure of overthrust folds present in silty-sandy-grained deposits in the southern part of the cliff. Apart from folds and overthrusts there are many faults and the boudinage. Structural analysis of glaciotectonic deformations in conjunction with origin of deposits and statigraphic research enabled the recognition of several stages of development of deformations. Two local directions of glaciotectonic transport were marked clearly: from the north-east, which was connected with glacier invasion in the OEwiecie Stadial of the Vistulian Glaciation, and direction from north-west (north north-west), related to the Main Stadial of the Vistulian Glaciation.
Źródło:: Przegląd Geologiczny; 2005, 53, 7; 572--581
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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