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Tytuł:
Geneza i transformacja rzeźby morenowej w północno-zachodniej części Garbu Lubawskiego (Polska północna)
Origin and transformation of morainic landscape in NW part of Lubawa Upland Origin and transformation of morainic landscape in NW part of Lubawa Upland
Autorzy:
Tylmann, K.
Wysota, W.
Powiązania:
https://bibliotekanauki.pl/articles/2074836.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
subglacial processes
landscape transformation
Lubawa Upland
north Poland
Opis:
The paper presents the investigation results concerning the origin and transformation of the morainic landscape in the northwest part of Lubawa Upland. Detailed sedimentological studies of the sediments within the morainic hill in Rożental and the reconstruction of their depositional and deformational processes are presented. We proposed a model of landscape formation and transformation in examined area. The reconstruction of the palaeogeographical conditions which have been prevailed during the late Pleistocene is also proposed. Collected data show that morainic landscape in the northwestern part of Lubawa Upland reveal landforms of an older origin. It is suggested that relief of examined area consist some features of "palimpsest landscape". The older glacial landforms, formed before the last ice advance, can exist here.
Źródło:
Przegląd Geologiczny; 2011, 59, 11; 739-750
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Społeczność pochodzenia ukraińskiego a Warmii i Mazurach po 1947 roku. Jej wpływ na rozwój kulturalny regionu północno-wschodniej Polski
Community of Ukrainian origin in Warmia and Mazury region after 1947. Its influence on the cultural development f north-eastern region of Poland
Autorzy:
Wrzosek, Paweł
Powiązania:
https://bibliotekanauki.pl/articles/481397.pdf
Data publikacji:
2006-12-01
Wydawca:
Uniwersytet Warmińsko-Mazurski w Olsztynie
Tematy:
North-Eastern Poland
Ukrainian minority
culture
Opis:
The community of Ukrainian origin in Warmia and Mazury is not often the object of research due to the fact that it is strongly involved in ideology and politics, which makes it difficult to draw a boundary between propaganda and its actual problems. What contributed to the transformation of the Ukrainian culture into the North-East Poland were activities of those Ukrainian communities that migrated into this region in the course of „Wisła” action in 1947. The research that the author conducted in a group of Ukrainian teenagers in 2004 casts a new light onto the community, making it possible to characterize the continuously evolving problems of its existence. The approach to this topic highlights the way in which the Ukrainian minority, tom apart from its original environment, deals with its problems and is gradually integrating into the new reality. It also focuses on the analysis of differences concerning mutual relations. In time. the awareness of the Ukrainian community members has lost its demanding nature, and has become filled with invention and initiative, thus resembling the awareness that the hosts of their new motherland should display. It is very interesting to notice that the Poles are often participants in the cultural events organized by the Ukrainians.
Źródło:
Acta Polono-Ruthenica; 2006, 1, XI; 117-124
1427-549X
Pojawia się w:
Acta Polono-Ruthenica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
O słowniczku wyrazów ludowych Antoniego Wagi
On the glossary of Antoni Wagas folk words
Autorzy:
Nowowiejski, Bogusław
Powiązania:
https://bibliotekanauki.pl/articles/2118339.pdf
Data publikacji:
2014-12-30
Wydawca:
Uniwersytet w Białymstoku. Wydawnictwo Uniwersytetu w Białymstoku
Tematy:
folk dialects
North-Eastern Poland
dictionaries
Opis:
The article contains the characteristics of one the nineteenth century sources of "Słownik gwar polskich" [Dictionary of Polish Dialects] by Jan Karłowicz, i.e., the dictionary written by Antoni Waga titled "Abecadłowy spis wyrazów ludowego języka w okolicach Łomży, Wizny i przyległych" [Alphabetic List of Words of Folk Language from Łomża, Wizna and the neighborhood] published in the second volume of a scientific journal “Warsaw Library” for 1860.
Źródło:
Białostockie Archiwum Językowe; 2014, 14; 81-98
1641-6961
Pojawia się w:
Białostockie Archiwum Językowe
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Naturalne i antropogeniczne przemiany krajobrazów delty Wisły
Natural and man-made changes in the delta of Vistula river
Autorzy:
Plit, Joanna
Powiązania:
https://bibliotekanauki.pl/articles/88272.pdf
Data publikacji:
2010
Wydawca:
Polskie Towarzystwo Geograficzne
Tematy:
rozwój delty
zmiany zagospodarowania
Żuławy
delta evolution
changes of management
north Poland
Opis:
Akumulacji osadów w płytkich wodach Zalewu Wiślanego, od neolitu aż do średniowiecza podlegała niemal wyłącznie naturalnym procesom przyrodniczym. Proces był ciągły, acz powolny. Natomiast od średniowiecza przyrost lądu był bardzo szybki. Antropogeniczne wylesianie zlewni Wisły, rolnicze zagospodarowanie gruntów spowodowało wzmożenie erozji w dorzeczu i osadzanie materiału skalnego w delcie. W X-XVI wieku rzeka dobudowała deltę u ujścia północnych odnóg Szkarpawy i Leniwki. Od renesansu główny nurt Wisły skierowany został Nogatem i tam rzeka osadzała najwięcej aluwiów. Mieszkańcy Żuław przyspieszali proces powiększanie lądu. Sypali wały, tworzyli poldery. Począwszy od końca XIX wieku w wyniku przekopania nowego ujścia i skierowania 90% wód Wisły bezpośrednio do morza, przyrost delty jest znacznie wolniejszy. Jest on głównie wynikiem akumulacji obumarłych części organicznych.
Accumulation of the deposits in the Vistula Lagoon was continuous, even though quite slow. Starting with the Middle Ages the increments of land have been rather quick. Deforestation of the Vistula river basin and agricultural land development triggered off erosion. The rocky material was deposited in the delta. Initially, the river had been building the delta at the mouth of the northern branches of Szkarpawa and Leniwka. In the period of Renaissance the main current was directed through the Nogat channel and it is there that the river deposited most of the alluvia. The inhabitants of Zulawy delta lowlands accelerated themselves the process of land extension. They built walls and established polders. Starting with the end of the 19th century, due to the digging of the new river channel and the fact that thereby 90% of discharge was directed straight to the sea, the increase of the delta has been much slower. It is primarily the effect of accumulation of the dead organic parts.
Źródło:
Prace Komisji Krajobrazu Kulturowego; 2010, 13; 13-28
1896-1460
2391-5293
Pojawia się w:
Prace Komisji Krajobrazu Kulturowego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New location of the well-known Ordovician trilobite Asaphus expansus (Wahlenberg, 1821) from north-western Poland
Autorzy:
Borowski, Tomasz
Daniszewski, Piotr
Powiązania:
https://bibliotekanauki.pl/articles/1031283.pdf
Data publikacji:
2021
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Asaphus expansus
Ordovician
Paleozoic
Wahlenberg
north-western Poland
trilobite
Opis:
This report documents the new location of the representative Ordovician trilobite Asaphus expansus. This well-known trilobite was discovered in the “Storkowo” Mining Plant in the central part of the West Pomeranian Province in Poland.
Źródło:
World News of Natural Sciences; 2021, 34; 82-87
2543-5426
Pojawia się w:
World News of Natural Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petrographic Garden in Moryń : a new geotouristic attraction in western Poland
Autorzy:
Górska-Zabielska, M.
Dobracki, R.
Powiązania:
https://bibliotekanauki.pl/articles/294938.pdf
Data publikacji:
2015
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
erratic
petrographic garden
geodiversity
geological heritage
geotourism
north-western Poland
Opis:
A new petrographic garden was established in 2012 in Moryń, north-western Poland. Thirty five erratics, derived from adjacent till moraines, witness local geological heritage and form a new geotouristic attraction. Together with other geovalues of this region, the petrographic garden is a cornerstone of the Polish-German geopark “Glacial Land over the Odra River” (Ger. Geopark Eiszeitland am Oderrand).
Źródło:
Landform Analysis; 2015, 29; 73-80
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geotourism potential of the Drawskie Lake District as a support for the planned geopark named postglacial land of the Drawa and Dębnica Rivers
Autorzy:
Górska-Zabielska, Maria
Kamieńska, Katarzyna
Powiązania:
https://bibliotekanauki.pl/articles/1052505.pdf
Data publikacji:
2017-03-15
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
geodiversity
geotourism
geoconservation
geopark
Drawskie Lake District
north-western Poland
Opis:
The geotourism potential of ten geosites, occurring within the Drawskie Lake District, north-western Poland, was evaluated to demonstrate the need for the establishment of a geopark named “Postglacial land of the Drawa and Dębnica rivers”. Each site was investigated in respect of its scientific (geological and geomorphological), educational, economic, conservation, and added values. It has been found that two geosites, being also cultural heritage sites (Drahim Castle and Pottery Settlement in Sikory), have the greatest geotourism potential. Different aspects of inanimate nature are promoted in both geosites. Thanks to the existence of such objects there is a good chance for the successful development of geotourism, which is a tool for the sustainable socio-economic development of the region.
Źródło:
Quaestiones Geographicae; 2017, 36, 1; 15-31
0137-477X
2081-6383
Pojawia się w:
Quaestiones Geographicae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Heavy Metal Content in Water of Miedwie Lake (North-West Poland)
Autorzy:
Daniszewski, P
Konieczny, R.
Powiązania:
https://bibliotekanauki.pl/articles/411796.pdf
Data publikacji:
2013
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Toxic Heavy Metals
lake water
Lake of Miedwie (North-West Poland)
Opis:
The present research work deals with the quantification of toxic heavy metals in the water samples collected from Lake of Miedwie (North-West Poland). While the annual average concentration of Cadmium was calculated as 0.45 ppm in 2008 of the year and 0.29 ppm in 2009 of the year. The values obtained were found to be below the permissible limit of 2.0 ppm set for inland surface water. While the annual average concentration of Chromium was calculated as 2.78 ppm in 2008 of the year and 2.50 ppm in 2009 of the year. Which was very much above the permissible limit of 0.1 ppm set for inland surface water. The observed annual average concentration of Copper in the water was 0.06 ppm in 2008 of the year and 0.05 ppm in 2009 of the year, which was below the permissible limit of 3.0 ppm set for inland surface water. While the annual average concentration of Mercury was calculated as 0.04 ppm in 2008 of the year and 0.04 ppm in 2009 of the year, which was very much above the maximum limit of 0.01 ppm set for inland surface water. The annual average concentration of Nickel in the water samples was observed to be 2.19 ppm in 2008 of the year and 2.42 ppm in 2009 of the year, which is close to the limit of 3.0 ppm set for inland surface water. The annual average concentration of Lead in the water samples was observed to be 0.06 ppm in 2008 of the year and 0.05 ppm in 2009 of the year, which is above the permissible limit of 0.1 ppm set for inland surface water. The results of the present investigation indicate that the annual average concentration of Zinc in water samples was 3.25 ppm in 2008 of the year and 2.95 ppm in 2009 of the year, which is above the permissible limit of 5.0 ppm set for inland surface water.
Źródło:
International Letters of Chemistry, Physics and Astronomy; 2013, 10, 2; 218-226
2299-3843
Pojawia się w:
International Letters of Chemistry, Physics and Astronomy
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
In the footsteps of the ice sheet in the area of the planned geopark postglacial land of the Drawa and Dębnica rivers (the Drawskie Lakeland, Poland)
Autorzy:
Górska-Zabielska, Maria
Powiązania:
https://bibliotekanauki.pl/articles/2129070.pdf
Data publikacji:
2022
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
geosite
geodiversity
geotourism
geopark
glaciomarginal zone
Drawskie Lakeland
north-western Poland
Opis:
The article presents 20 geosites located on five geotourist paths and their closest vicinity, constituting the initial part of the planned geopark Postglacial land of Drawa and Dębnica. Geosites represent the most valuable abiotic resources, proving the large geodiversity of the studied area. These are: 1. glacial and fluvioglacial accumulation forms (e.g.: terminal end-moraine of the Parsęta lobe, undulating moraine uplands, glacial deposits including erratic border boulders, esker ridges), 2. glacial and fluvioglacial erosive forms (e.g.: channel and melt-out-depressions), 3. other (like e.g.: deep erosive and erosional-denudation valleys, erosive forms of groundwater or 1st order watershed between the Odra and Parsęta catchments). The purpose of the geosites characteristics in this paper is to support the development of geotourism in the peripheral tourist area.
Źródło:
Landform Analysis; 2021, 40; 37--56
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Heavy Metal Content in Water of Resko Lake (North-West Poland)
Autorzy:
Daniszewski, P.
Konieczny, R.
Powiązania:
https://bibliotekanauki.pl/articles/412339.pdf
Data publikacji:
2013
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Toxic Heavy Metals
lake water
Lake of Resko (North-West Poland)
Opis:
The present research work deals with the quantification of toxic heavy metals in the water samples collected from Lake of Resko (North-West Poland). While the annual average concentration of Cadmium was calculated as 0.34 ppm in 2008 of the year and 0.28 ppm in 2009 of the year. The values obtained were found to be below the permissible limit of 2.0 ppm set for inland surface water. While the annual average concentration of Chromium was calculated as 1,75 ppm in 2008 of the year and 1.97 ppm in 2009 of the year. Which was very much above the permissible limit of 0.1 ppm set for inland surface water. The observed annual average concentration of Copper in the water was 0.05 ppm in 2008 of the year and 0.06 ppm in 2009 of the year, which was below the permissible limit of 3.0 ppm set for inland surface water. While the annual average concentration of Mercury was calculated as 0.03 ppm in 2008 of the year and 0.04 ppm in 2009 of the year, which was very much above the maximum limit of 0.01 ppm set for inland surface water. The annual average concentration of Nickel in the water samples was observed to be 2.07 ppm in 2008 of the year and 2.09 ppm in 2009 of the year, which is close to the limit of 3.0 ppm set for inland surface water. The annual average concentration of Pb in the water samples was observed to be 0.07 ppm in 2008 of the year and 0.05 ppm in 2009 of the year, which is above the permissible limit of 0.1 ppm set for inland surface water. The results of the present investigation indicate that the annual average concentration of Zn in water samples was 3.02 ppm in 2008 of the year and 2.74 ppm in 2009 of the year, which is above the permissible limit of 5.0 ppm set for inland surface water.
Źródło:
International Letters of Chemistry, Physics and Astronomy; 2013, 8, 3; 279-287
2299-3843
Pojawia się w:
International Letters of Chemistry, Physics and Astronomy
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dependence of air quality conditions in cities in north-western Poland on the direction of air inflow
Autorzy:
Kicińska, Bożena
Mikulska, Małgorzata
Powiązania:
https://bibliotekanauki.pl/articles/2032475.pdf
Data publikacji:
2006-06-01
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
North-western Poland
air pollution
sulphur dioxide
nitrogen dioxide
wind direction
Opis:
This paper presents the dependence of air pollution with sulphur dioxide and nitrogen dioxide on wind direction in Szczecin, Łeba, Elbląg and Zielona Góra in the period 19931999. It has been shown that the most disadvantageous air quality conditions in the cities listed above are on the days with air inflow from south-east, and the most advantageous on the days with advection from north-west. This dependence is particularly evident in the case of pollution with sulphur dioxide, especially in the cold half-year.
Źródło:
Miscellanea Geographica. Regional Studies on Development; 2006, 12; 81-86
0867-6046
2084-6118
Pojawia się w:
Miscellanea Geographica. Regional Studies on Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The maximum ice sheet limit of the Vistulian Glaciation in northeastern Poland and neighbouring areas
Autorzy:
Krzywicki, T.
Powiązania:
https://bibliotekanauki.pl/articles/2059933.pdf
Data publikacji:
2002
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
north-eastern Poland
Vistulian glaciation
Eemian Interglacial
ice sheet limit
tills
Opis:
This paper outlines a new approach to reconstructing Vistulian ice sheet limits in NE Poland and adjacent areas of Lithuania and Belarus. It is based on geological investigations of landforms and deposits either of a hypothetical boundary to the Vistulian ice sheet limits. The main conclusions are: 1 - the area was covered twice by the Vistulian ice sheet; the first time during the Świecie Stadial (67-50 ka BP) and the second time during the Main Stadial (24-12 ka BP); 2 - the limit of the older stadial was farther to the south a that of the younger one; 3 - due to covering of the Eemian sediments by the ice sheet of the Świecie Stadial the limit of the Vistulian Glaciation has moved about 15-20 km southwards.
Źródło:
Geological Quarterly; 2002, 46, 2; 165-188
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A Hirnantian deep-water refuge for warm-water ostracods in Baltoscandia
Autorzy:
Truuver, K.
Meidla, T.
Powiązania:
https://bibliotekanauki.pl/articles/2059998.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Upper Ordovician
Baltic Palaeobasin
ostracods
north-eastern Poland
Kętrzyn IG1 borehole
Opis:
The latest Ordovician is marked by a severe climate change, the Hirnantian glaciation. This climatic event affected many marine taxa including ostracods. Rich and abundant ostracod assemblages of the Baltic Palaeobasin were severly impoverished. Many of the typical pre-Hirnatian warm-water ostracod species died out, but also some distinct, cold-water species appeared. Two very different but likely coeval latest Ordovician ostracod assemblages are recorded in the Baltic countries and north-eastern Poland. The latest Ordovician Estonian Shelf (inner ramp) is characterized by the Medianella aequa association whilst sections in the Livonian Basin (middle to outer ramp) reveal the Harpabollia harparum association that is thought to represent a cold-water assemblage belonging to the Dalmanitina-Hirnantia Fauna sensu lato. A transitional assemblage composed of a “species mixture” of typical Hirnantian cold-water and some pre-Hirnantian warm-water ostracod species is described for the first time from the Kętrzyn IG1 borehole, north-eastern Poland. The assemblage is dominated by Cryptophyllus pius sp. n. The genus Cryptophyllus is rare in the two other well-known assemblages. The discovery suggests that marginal parts of the Baltic Palaeobasin could serve as a kind of refuge for the last representatives of the ostracod faunas of the inner shelf of Baltic Palaeobasin. The Hirnantian assemblage is replaced by the low-diversity recovery assemblage that is dated as late Hirnantian-Silurian in Estonia and other areas. This suggests that the position of the systemic boundary in the Kętrzyn borehole and elsewhere in north-eastern Poland should be re-evaluated.
Źródło:
Geological Quarterly; 2015, 59, 4; 738--749
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pollen and diatom stratigraphy of the lacustrine-fluvial-swamp deposits from the profile at Domuraty, NE Poland
Autorzy:
Winter, H.
Khursevich, G.
Fedenya, S.
Powiązania:
https://bibliotekanauki.pl/articles/2060215.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
north-eastern Poland
Cromerian Complex Stage
Małopolanian Interglacial
pollen analysis
diatom analysis
Opis:
Fluvio-lacustrine deposits from a boring core drilled at Domuraty, NE Poland have been examined by pollen and diatom analyses. These studies allow characterization of the development of vegetation in a long pollen sequence, and of palaeoenvironmental changes in the former basin based on quantitative and qualitative changes in diatom assemblages along the profile studied. The pollen record shows a sequence of phases with forest communities separated by phases of open vegetation. It demonstrates the impact of rapid, of lesser climate changes, as well as climatic fluctuations on terrestrial ecosystems. The age of the succession can be related to the Cromerian Complex Stages.l. (early Mid dle Pleistocene). Stage s.l. (early Mid dle Pleis to cene).
Źródło:
Geological Quarterly; 2008, 52, 3; 269-269
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petrographic analyses and indicator erratics of gravels of the Odra lobe
Autorzy:
Górska-Zabielska, Maria
Zabielski, Ryszard
Powiązania:
https://bibliotekanauki.pl/articles/2026730.pdf
Data publikacji:
2010
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
petrography of glacial gravels
Scandinavian erratics
Pomeranian phase
Odra lobe
north-eastern Germany
north-western Poland
Opis:
Fennoscandinavian er rat ics found in the gla cial de pos its till and in the glaciofluvial sed i ments within the main limit of the Odra gla cier lobe (NW Po land and NE Ger many), have been ex am ined in two frac tions: of 4–10 mm and 20–60 mm. The most nu mer ous in the frac tion of 4–10 mm are: crys tal line rocks (Cr; 35–40%) orig i nat ing in the Pro terozoic Bal tic Shield as well as Lower Palaeozoic lime stones (LPL; 35–40%) – from the sed i men tary sheet cov er ing the Pro tero zoic Bal tic Shield in the area of cen tral Bal tic Sea. Per cent age of sand stones (S) amounts to 10–15%. The remain ing rock types (sev eral per cent each) are: Palaeozoic shales (PS), the out crops of which are lo cal ized in Scania (Sk¯ne) and on Born holm, Cre ta ceous lime stones (CL) and flintstones (F) orig i nat ing from the west ern part of the south ern Bal tic Sea as well as quartz (Q), milk quartz (MQ) and iso lated grains of De vo nian dolomites (DD). From the anal y sis of in di ca tor er rat ics, which was car ried out in the 20–60 mm frac tion, it ap pears that mainly the out -crops lo cal ized in Sm¯land (e.g. red and grey Växjö gran ites, P¯skallavik por phy ries or Tessini and Kalmarsund sand - stones) as well as in Scania (Höör and Hardeberga sand stones) and Re gion Blekinge–Born holm (e.g. Karlshamn and Halen gran ites as well as NexÝ and Bavnodde sand stones) had been sub jected to the gla cial pluck ing. The o ret i cal boul der cen tres (TBC, Ger man: TGZ das Theoretische Geschiebezentrum, Lüttig 1958), which were cal cu lated for 23 sam ples, are lo cal ized mostly in a small area in Sm¯land, be tween 15°E–16°E and 56.5°N–58.5°N. Apart from in di ca - tor er rat ics the sta tis ti cal ones are nu mer ous, that are first of all grey and red Lower Palaeozoic lime stones with their out crops lo cal ized at the bot tom of the cen tral Bal tic Sea. Tak ing into ac count the TBC val ues of in di ca tor er rat ics as well as high per cent age of sta tis ti cal er rat ics it can be pro nounced that the sec tion of cen tral and west ern Bal tic Sea as well as the one of south-east ern Swe den had been sub jected to the heavi est gla cial pluck ing by that part of the Pleis to - cene ice-sheet which reached the stud ied area dur ing the Pom er a nian Phase.
Źródło:
Studia Quaternaria; 2010, 27; 17-25
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
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