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Wyświetlanie 1-10 z 17
Tytuł:
Late Quaternary evolution of the Tjörn Valley, Wedel Jarlsberg Land, Spitsbergen
Autorzy:
Szczęsny, Ryszard
Powiązania:
https://bibliotekanauki.pl/articles/2053251.pdf
Data publikacji:
1987
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Spitsbergen
Quaternary glaciations
Źródło:
Polish Polar Research; 1987, 8, 3; 243-250
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pre-Quatemary glaciations of West Antarctica: evidence from the South Shetland Islands
Autorzy:
Birkenmajer, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/2057378.pdf
Data publikacji:
1984
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctica
pre-Quaternary glaciations
Źródło:
Polish Polar Research; 1984, 5, 3-4; 319-329
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Glacial and marine episodes in Kaffioyra, northwestern Spitsbergen, during the Vistulian and the Holocene
Autorzy:
Niewiarowski, Władysław
Pazdur, Mieczysław F.
Sinkiewicz, Mieczysław
Powiązania:
https://bibliotekanauki.pl/articles/2052726.pdf
Data publikacji:
1993
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Spitsbergen
Kaffioyra
Quaternary
glaciations
marine transgressions
Źródło:
Polish Polar Research; 1993, 14, 3; 243-258
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Glacial landforms as geodiversity resources for geotourism in Tierra del Fuego, Argentina
Autorzy:
Coronato, Andrea
Schwarz, Soledad
Flores Barrera, Flavia
Powiązania:
https://bibliotekanauki.pl/articles/2054570.pdf
Data publikacji:
2022-03-31
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
glaciations
landscape
georesources
geodidactic potential
tourist attractions
Opis:
The southern extreme location and the natural landscapes, highly modelled by glaciers during the Quaternary period, give Tierra del Fuego a unique opportunity to attract visitors worldwide. Its glacial landforms are geodiversity resources that are witness to global climate changes as natural processes. Therefore, this study aims to highlight different glacial landforms considering their geodidactic potential for educational information in terms of geographical study. Sixteen georesources connected by routes are analysed, using bibliographic research, fieldwork and a datasheet designed ad-hoc. Four of them were formed during middle Pleistocene glaciations and the other twelve during the Last Glacial Maximum (LGM), out of which two also represent the Holocene, which happens to be the youngest glaciation.
Źródło:
Quaestiones Geographicae; 2022, 41, 1; 5-24
0137-477X
2081-6383
Pojawia się w:
Quaestiones Geographicae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The age of the oldest Scandinavian glaciations in mid-eastern Poland and southwestern Belarus
Autorzy:
Lindner, L.
Marciniak, B.
Sanko, A. F.
Khursevich, G. K.
Powiązania:
https://bibliotekanauki.pl/articles/2059317.pdf
Data publikacji:
2001
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polska
Belarus
Early Pleistocene
Scandinavian glaciations
stratigraphic correlation
Opis:
Analysis of type localities of Pleistocene deposits from mid-eastern Poland (Kozi Grzbiet, Łuków, Biała Podlaska and Wilczyn) and southwestern Belarus (Smolarka and Postolovo) has provided a new view on the age, limits and correlation of the oldest Scandinavian glaciations in the area. Integration of palaeontological data with determination of the Brunhes/Matuyama boundary (780 ka) at Kozi Grzbiet and Smolarka suggests that the first glaciation (Narevian) preceded this boundary and had a slightly smaller extent in SW Belarus than hitherto considered. The second glaciation (Nidanian) occurred slightly above or at this palaeomagnetic boundary. In Poland it is the first South Polish Glaciation, a till of which can be traced as far as the Holy Cross Mts. In SW Belarus it is represented by a till to the south of Brest and Bereza, and connected there with the oldest glaciation.
Źródło:
Geological Quarterly; 2001, 45, 4; 373-396
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The extent of Pleistocene glaciations in the western part of the Campo Imperatore (Gran Sasso Massif, Central Italy)
Autorzy:
Bisci, C.
Gentili, B.
Ciccacci, S.
Dramis, F.
Kotarba, A.
Powiązania:
https://bibliotekanauki.pl/articles/294813.pdf
Data publikacji:
1999
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
glacial morphology
stagnant ice topography
Pleistocene glaciations
Central Apennines
Opis:
The Campo Imperatore is a virtually undrained tectonic depression located in the inner part of the Gran Sasso Massif, the highest relief within the Apennines (2,912 m a.s.l. at Corno Grande). This paper reports some major géomorphologie features of the western part of this depression, which   represents a specific and very fine example of glaciated mountain landscape, where landforms typical of glacial erosion are commonplace over l ,800 m a.s.l. Most of the glacial cirques are characterized by karstified bedrock topography, in places covered with thin drift deposits. Distinct recessional moraines are also present at various altitudes (i.e. around 2,250; 2,180; 2,000 and 1,740 m a.s.l). However, the most typical landforms on the floor of the main depression are those due to glacial deposition. There, at altitudes ranging around 1,640—1,590 m a.s.l., stagnant ice déglaciation patterns dominate in the form of a wide lobate moraine system which rises 25—30 m above an outwash plain covered by glaciofluvial, lacustrine and alluvial deposits. Within the latter, small (less than 10 m high) hills, comprising glacial drift, protrude from the flat valley floor. The remnants of these strongly degraded, transformed and laterally-eroded moraines denote the maximum extent of an older glaciation, some 1.5 km remote from the main system.
Źródło:
Landform Analysis; 1999, 2; 37-43
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Nowe spojrzenie na liczbę, wiek i zasięgi zlodowaceń środkowopolskich w południowej części środkowowschodniej Polski
A new look at the number, age and extent of the Middle Polish Glaciations in the southern part of central- eastern Poland
Autorzy:
Lindner, L.
Powiązania:
https://bibliotekanauki.pl/articles/2074381.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
zlodowacenie środkowopolskie
chronostratygrafia
central-eastern Poland
Middle Polish Glaciations
chronostratigraphy
Opis:
An overview of the existing opinions combined with new geomorphological, geological, palaeopedological and TL data allow a new look at the number, age and ranges of the three Middle Polish (Saalian, Dnieperian) Glaciations in central-eastern Poland. During the first of these glaciations (Liviecian), correlated with the 10 oxygen isotope stage in deep-marine deposits (400–360 ka), the Scandinavian ice-sheet advanced in form of a rather narrow lobe, reaching only several tens of kilometres south of Warsaw. During the second glaciation (Krznanian), correlated with the 8 oxygen isotope stage (330–320 ka), it advanced in form of a wider lobe down to the northern margin of the Małopolska and Lublin uplands. In turn, during the third glaciation (Odranian), correlated with the 6 oxygen isotope stage (210–130 ka), the range of the Scandinavian ice-sheet was the largest. It stopped at the elevations of the Quaternary basement in the northern and western part of the Małopolska and Lublin uplands, reaching 330–280 m above sea level. In the study area the discussed glaciations are separated by two interglacials (Zbójnian, Lublinian = Lubavian), correlated with the Reinsdorf and Schöningen interglacials in Germany and Landos and Le Bouchet interglacials in France. The analysed data indicate that within the Odranian Glaciation, its maximum (Kamienna = Drenthe) and postmaximum stadials (Warta = Warthe), as well as two younger recessive stadials (Wkra, Mławka) should be distinguished. Due to the rather wide eastward distribution of the Scandinavian ice-sheets during the two younger glaciations, an attempt has been made to correlate them with the two Dnieperian glaciations in the Ukraine.
Źródło:
Przegląd Geologiczny; 2005, 53, 2; 145--150
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Uwagi o plejstoceńskich glacjałach i interglacjałach
Problem of Pleistocene interglacials and glaciations — general remarks.
Autorzy:
Winter, H.
Powiązania:
https://bibliotekanauki.pl/articles/2074473.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
plejstocen
klimatostratygrafia
palinostratygrafia
interglacjał
lodowacenie
Pleistocene
climatostratigraphy
palinostratigraphy
interglacials
glaciations
Opis:
The paper discusses issues of the distinguishing mono-interglacials (Eemian, Mazovian and Zbojnian ones) and bi-interglacials (Ferdynandovian and Augustovian ones) pollen successions as well as a problem of cooling/glaciation within Ferdynandovian and Augustovian pollen successions. Division of the Ferdynandovian and Augustovian pollen successions into two separated interglacials each (FI and FII, AI and A II, respectivaly) and the glaciation sensu lato (F I/II and A I/II) between these interglacials from the climatostratigraphical point of view is proposed.
Źródło:
Przegląd Geologiczny; 2006, 54, 2; 142-144
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Main climatic changes in the Quaternary of Poland, Belarus and Ukraine
Autorzy:
Lindner, L.
Gozhik, P.
Marciniak, B.
Mars, L.
Yelovicheva, Y.
Powiązania:
https://bibliotekanauki.pl/articles/2058786.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Polska
Belarus
Ukraine
Quaternary
glaciations and coolings
interglacials and warmings
loess
palaeosols
Opis:
26 units are described and correlated, representing the main climatic episodes during the Quaternary in Poland, Belarus and Ukraine. They comprise 13 cool and 13 warm intervals. The four oldest ones are Różcian (Olkhovskian, Siver), Ponurzycian (Grushevskian, Beregovo), Otwockian (Vselubskian, Berezan) and Celestynovian (Yelenynskian, Kryzhaniv); these correspond to Praetiglian, Tiglian, Eburonian and Menapian, respectively of the Early Pleistocene in the Netherlands. In Poland this part of the Quaternary is named the Pre-Glacial or the Pre-Pleistocene. The Mid and Late Quaternary (the glacial epoch in Europe) comprises 11 glaciations or global coolings, namely the Narevian in Poland (Zhlobynskian, Ilyichivsk), the younger pre-Augustovian (Rogachevian 1/2, Shirokino 1/2), Augustovian 1/2 (Rogachevian 2/3, Shirokino 2/3), Nidanian (Narevian in Belarus, Pryazovsk), Sanian 1 (Servetskian, Sula), Ferdynandovian 1/2 (Belovezhian 1/2, Lubny 1/2), Sanian 2 (Berezinian, Tiligul), Liviecian (Orel), Krznanian (Dnieper 1), Odranian+Wartanian (Dnieperian+Sozhian, Dnieper 2 = Tyasmyn), Vistulian (Poozerian, Valday); and 10 interglacials or global warmings: early pre-Augustovian (Rogachevian 1, Shirokino 1), Augustovian 1 (Rogachevian 2, Shirokino 2), Augustovian 2 (Rogachevian 3, Shirokino 3) ,Małopolanian (Korchevian,Martonosha), Ferdynandovian 1 (Belovezhian 1, Lubny 1), Ferdynandovian 2 (Belovezhian 2, Lubny 2), Mazovian (Alexandrian, Zavadivka), Zbójnian (Smolenskian, Potagaylivka), Lubavian (Shklovian, Kaydaky), Eemian (Muravian, Pryluky) and Holocene. All these units are correlated with oxygen isotope stages identified in deep-sea sediments, shown relative to the palaeomagnetic epochs and correlated with main cool and warm stratigraphic units of Western Europe. Particular attention was placed on correlation of glacial and lake deposits, loesses and palaeosols.
Źródło:
Geological Quarterly; 2004, 48, 2; 97--114
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
O podziale klimatostratygraficznym kompleksu środkowopolskiego w plejstocenie Polski
Climatostratigraphic subdivision of the Pleistocene Middle Polish Complex in Poland
Autorzy:
Lindner, L.
Marks, L.
Powiązania:
https://bibliotekanauki.pl/articles/2074906.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
pleistocen
kompleksu środkowopolski
zlodowacenia
interglacjał
Polska
Pleistocene
Middle Polish Complex
glaciations
interglacials
Polska
Opis:
The term Middle Polish Complex was introduced by the authors in 2007 as an informal superstage of the younger Middle Pleistocene in Poland. It replaced a previous inconsistent term of Middle Polish Glaciations, composed both of glaciations and interglacials. The Middle Polish Complex comprises deposits of 3 glaciations (Liwiecian, Krznanian and Odranian) and 3 interglacials (Mazovian, Zbójnian and Lublinian). Glacial and lake-marshy deposits of the complex correspond with loess sequences and separating palaeosols. Their common superposition in Poland and recorded palaeomagnetic episodes Emperor, Chegan, Jamaica and Blake of the Brunhes epoch verify a chronology of climatic changes and climatostratigraphic subdivision of the complex. Mutual relation of climate changes and their reference to glacial-interglacial and loessy-palaeosol cycles in neighbouring countries support usefulness to more specified correlations. Successive interglacials and glaciations of the Middle Polish Complex correspond to rhythmic global climate changes reflected by oxygen isotope stages in deep-sea boreholes (MIS11-6)
Źródło:
Przegląd Geologiczny; 2012, 60, 1; 36-45
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-10 z 17

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