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    Tytuł:
    Późnoplejstoceński rozwój doliny Niemna w rejonie Grodna na Białorusi
    Late Pleistocene evolution of the Niemen River valley near Grodno in Belarus. Prz. Geol.
    Autorzy:
    Lindner, L.
    Sańko, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074560.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Białoruś
    dolina rzeki Niemen
    zlodowacenie poozierskie
    Belarus
    Niemen River valley
    Poozerian Glaciation
    river terraces
    Opis:
    Based on geological and paleobotanic data, the oldest valley system of the Niemen River is linked in the study area with a river located southward of Grodno, within a parallel valley from the Alexandrian (Mazovian) Interglacial. The foundations of the present-day, almost meridian course of the Niemen River valley, are connected with a system of post-glacial lakes from the Sozhian (Wartanian) Stadial of the Pripethian (Odranian) Glaciation, later filled with organic deposits of the Muravian (Eemian) Interglacial. Analysis of six sites with these deposits (Pyszki, Rumlówka, Poniemuń, Żukiewicze, Bohatyrowicze and Kniażewodce) indicates that they represent three lakes located at different altitudes. During the maximal range of the Dvinian (Main) Stadial of the Poozerian (Vistulian) Glaciation, the lakes were beyond the range of the ice-sheet. At this time, the highest located deposits of the Poniemuń-Żukiewicze lake were covered by sander sediments, whereas the Bohatyrowicze-Kniażewodce and Pyszki-Rumlówka lakes that were located at lower levels, were covered by fluvio-periglacial deposits and varved clays of the Skidel ice-dammed lake. Retreat of the ice-sheet of the Dvinian Stadial, resulting in outflow of water from the Skidel ice-dammed lake through the area with the two lower interglacial lakes, triggered the formation of a system of the Niemen River supra-flood terraces above them. Accumulation of the highest of these terraces (VI), during the first phase of the Skidel lake outflow, marks the beginning of the present-day Niemen River valley formation that probably began in the younger phases of the Dvinian ice-sheet retreat. Further evolution of the valley is linked with the Late Glacial formation of the middle (III-V) supra-flood terraces and with the Holocene formation of the lower (II, I) supra-flood terraces.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 1; 73-80
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Morfologia, struktury sedymentacyjne, cechy uziarnienia i geneza wstęg piaszczystych równiny zalewowej doliny dolnej Wisły między Górskiem i Szynychem
    Morphology, sedimentary structures, granulometric properties and origin of sandy ribbons developed on the lower Vistula River valley floodplain between Górsk and Szynych
    Autorzy:
    Kordowski, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074558.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    równina zalewowa
    Dolina Dolnej Wisły
    floodplain
    sandy ribbons
    lower Vistula river valley
    Opis:
    The paper presents the results of morphometric, structural and granulometric analyses carried out on sandy ribbons developed on the lower Vistula river floodplain in the Torun and Unisław Basins. The landforms identified were classified in respect to their shape, sedimentary structures and degree of preservation. Their origin and relation to other flood deposits were described and illustrated in the map of thickness and extent of sandy flood deposits in the Świecie Basin.
    Źródło:
    Przegląd Geologiczny; 2007, 55, 9; 785-794
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Kompleksowe badania osuwisk w dolinie Brdy w Koronowie k. Bydgoszczy
    Complex investigations of landslides in the Brda river valley in Koronowo near Bydgoszcz
    Autorzy:
    Zabuski, L.
    Mrozek, T.
    Świdziński, W.
    Kulczykowski, M.
    Laskowicz, I.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075162.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    landslides
    monitoring
    Brda river valley in Koronowo
    osuwiska
    dolina Brdy w Koronowie
    Opis:
    In the recentyears intensified landslidingwas observed in the surroundings and in the town of Koronowo near Bydgoszcz. (Krajeñskie Lake District). The gently undulated moraine upland, a wide valley of the Brda river, its relatively steep valleysides and incised valleys of tributaries are morphologicfeatures related to modeling by North Polish Glaciation. Quaternary tills alternated with fluvioglacial sands and gravels are underalined by Miocene clay and mud with brown coal intercalations. Due to such morphologic and geologic setting the study area isprone to slope instability. Failure apt soil massifs were assigned to 4 groups. Out of 32 identified landslides, 9 were selected for detailed examination. To register a nature and rate of failures a complex monitoring system was installed on slopes where the selected landslides resulted in severe damages to municipal infrastructure. The system was facilitated with inclinometers andpiezometers, supported by a network of GPS-RTK geodetic benchmarks as well as with a recording weather station. The performed examination revealed that the most unfavourable arrangement of the layers is, when under a non-cohesive soil (e.g. sand, gravel) lies a cohesive impermeable layer (e.g. clay, loam). The landslides are rather shallow ones (except 2 incidents) with slow rate of displacement of an order offew mm/year. The landslide triggeringfactor is water originatingfrom precipitation and snow melting. Influence of water was especially significant in early Spring 2011, due to the combined effect ofsnow melting and infiltration of thawing water originating from the former, exceptionally high rainfalls. The influence of hydrologic conditions on slope deformations is complex. There is a significant timelag between a movement initiation and unfavourable hydrometeorological conditions. That is exemplified with the landslide that was initiated in February-March 2011 in consequence of atmospheric conditions of November-December 2010. The obtained results formed the background for inventing engineering treatment measures aiming at current remedial stabilization of slopes and mitigation ofpossible landsliding in the future.
    Źródło:
    Przegląd Geologiczny; 2014, 62, 9; 472--480
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Związek akumulacji metali ciężkich w osadach facji powodziowej z morfologią doliny Wisły na odcinku od Annopola do Gołębia
    Relationship between the heavy metal accumulation in flood deposits and the morphology of the Vistula River Valley between Annopol and Gołąb
    Autorzy:
    Falkowska, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074355.pdf
    Data publikacji:
    2005
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    metale ciężkie
    osad powodziowy
    dolina Wisły
    Vistula river valley
    heavy metal
    flood deposits
    Opis:
    A distinct zonality as shown in the occurrence of trace elements accumulated in the flood facies of the Vistula River between Annopol and Gołąb. Their amount may be linked with the character and dynamics of river flow in its particular stretches because the nature of the fluvial processes influences on the lithological composition of deposits. Thus the content of these elements in the deposits is related to the geomorphologic conditions of the valley evolution, such as the occurrence of gorge zones and zones with free channel development. The highest concentrations have been noted in flood deposits occurring as intercalations within the channel facies and deposited in the widest parts of the river valley. The lowest concentrations of the trace elements have been observed in the gorge zones of the valley. These are places where the flow is most dynamic, enabling only the formation of low and medium cohesive silty flood deposits with low contents of organic matter, iron oxides and calcium carbonate.
    Źródło:
    Przegląd Geologiczny; 2005, 53, 8; 681--686
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    O potrzebie badań geologiczno-inżynierskich wałów przeciwpowodziowych na obszarze wschodniej części Niżu Środkowoeuropejskiego
    About a necessity of geological-engineering investigations on flood banks of the east Mid-European Lowland
    Autorzy:
    Kołodziejczyk, U.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074340.pdf
    Data publikacji:
    2005
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    dolina rzeczna
    fala powodziowa
    wał przeciwpowodziowy
    river valley
    flooding
    flood bank
    preventing natural disasters
    Opis:
    Throughout history, many times did floods in the river valleys of the East Mid-European Lowland occur. They brought about material losses and frequently hazards to human health and life as well. For centuries now, human communities have been building up flood banks in order to protect themselves against the negative impact of floods. However, the old flood banks were never investigated. First time in Poland they were surveyed after the flood in 1997. The results of investigations into the flood banks along the Odra/Oder River, which were conducted during and after the great flood of the year 1997, point out to the necessity of their renovation. The outcome of the research work carried out in Poland may be useful for the renovation and reconstruction of old flood banks and for the construction of new ones in the whole area of the East Mid-European Lowland.
    Źródło:
    Przegląd Geologiczny; 2005, 53, 7; 582--585
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Iły krakowieckie jako wskaźnik litostratygrafii w dolinie rzeki Sopot na Roztoczu
    The Krakowiec Clays as an indicator of lithostratigraphy in the Sopot River valley in the Roztocze Region (estern Poland)
    Autorzy:
    Janiec, B.
    Czarnecka, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074422.pdf
    Data publikacji:
    2006
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    iły krakowieckie
    mikrofauna
    paleontologia
    litostratygrafia
    Roztocze
    Krakowiec clays
    microfauna
    paleontology
    residuum
    lithostratigraphy
    river valley
    Roztocze region
    SE Poland
    Opis:
    The results of micropaleonthological studies of the Sarmatian (upper Miocene) Krakowiec Clays from primary deposit as well as re-deposited ones were applied to the analysis of the stratigraphic profile of the Sopot valley fills. The study site was at the break section of the Sopot River valley in a contact zone of southern escarpment between the central part of the Roztocze and Sandomierz Basin regions (SE Poland). Species of fossil microfauna (foraminiferans, radiolarians), sponges and mollusks, as well as residual deposits were used. The documented, even if apparently small change in the lithostatigraphic profile of the Sopot valley fills, i.e., the presence of pre-Pleistocene deposits in its floor, is very important for the valley history and for interpreting other problems of river breaks and the Roztocze escarpment zone itself, e.g., sclae of the Holocene movements elevating the Roztocze Region, and their effect on expected intensity of deep fluvial erosion. In the sub-scarp zone of the Tomaszów Roztocze subregion the Krakowiec Clays occur rather shallowly. In the Sopot valley (‘Czartowe Pole’landscape preserve) they are in contact with calcareous formations. In two levels of natural clays’exposures, a dozen or so foraminiferan taxa were found. They were also below the primary deposit on the floor levels of the Sopot valley fills. The residuum of the studied strata consists of glauconite and pre-Pleistocene quartz sands, without silicate and alumosilicate, typical for postglacial formations. The Sarmatian clays present in residue were redeposited at least in the pre-Pleistocene. From the clays top up to the surface of valley fills, are Holocene deposits. The study revealed that: (1) during the Holocene and earlier the Sopot valley fills were not removed completely; (2) the floor of the valley is made not of the youngest, Holocene strata, but much older; (3) the presence of the Sarmatian microfauna in the alluvia allows to date the studied deposits as pre-Pleistocene (Pliocene?); (4) fine quartz sands and glauconite (a specific form of hydromica) both forming the residuum of the studied valley fill levels, together with the absence of other silicates and alumosilicates that are common in the Pleistocene formations, exclude the studied Krakowiec Clays from the group of glacial or fluvioglacial (Pleistocene) formations; (5) the youngest (latest Pleistocene –Holocene) movements elevating the Roztocze Region and the resulting deep fluvial erosion do not correspond with shallow occurrence of the pre-Pleistocene valley fills; this requires further discussion.
    Źródło:
    Przegląd Geologiczny; 2006, 54, 10; 913-918
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Analiza powtarzalności wydzieleń geologiczno-inżynierskich w dolinie rzecznej
    Repeatability analysis of geoengineering layers in river valley
    Autorzy:
    Wierzbicki, J.
    Smaga, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074257.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    sondowanie statystyczne
    dolina Warty
    wydzielenia geologiczno-inżynierskie
    analiza statystyczna
    cone penetration tests
    Warta River valley
    geoengineering layers
    statistical analysis
    Opis:
    The paper presents results of geotechnical and geological investigation on flood plain of the Warta River, below the Jeziorsko reservoir. It is the section of the river, where the intensive erosion process of the river bed occurs. To stop this process thresholds are built. Their efficiency depends of ground conditions, especially spatial variability of geotechnical parameters. To describe the subsoil cone penetration tests were carried out. Subsequently Authors used statistical techniques to analyze variations of geotechnical parameters. Most of all, k-means method was applied. This well known cluster analysis is one of analysis which makes dividing subsoil into relatively homogeneous layers in different part of the river valley possible. However, Authors observed that in case of river alluvial 20% of variation of parameters values in layer is necessary to accept.
    Źródło:
    Przegląd Geologiczny; 2014, 62, 10/2; 721--726
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rzeźba i osady równiny aluwialnej dolnego biegu Przemszy (Wyżyna Śląska) jako wskaźnik zmian środowiska przyrodniczego
    Relief and alluvial plain sediments of the lower Przemsza River valley as indicators of environmental changes (Oświęcim Basin, South Poland)
    Autorzy:
    Panek, I.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074587.pdf
    Data publikacji:
    2008
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    paleogeografia
    sedymentologia
    dolny bieg Przemszy
    Kotlina Oświęcimska
    Polska Południowa
    paleogeography
    sedimentology
    lower Przemsza River valley
    Oświęcim Basin
    South Poland
    Opis:
    Paleogeography of the lower Przemsza River valley was studied in detail. By means of sedimentological methods, C.exp.14 dating and analysis of archival cartographic sources, the chronology of environmental events has been established, along with the types of the sedimentological processes and indirectly the role of neotectonics in the shaping of the valley. The lower Przemsza River section turned out to be the area where the fluvial processes of the Vistula and Przemsza Rivers took place, which can be seen in the formation of two different lithological types of the overbank facies. These types are of key importance in distinguishing between climatic and anthropogenic phases in the upper Vistula River valley.
    Źródło:
    Przegląd Geologiczny; 2008, 56, 2; 124-130
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Pochodzenie sfosfatyzowanych gąbek z warstwy dańskiego piaskowca glaukonitowego z Nasiłowa (dolina środkowej Wisły)
    The origin of phosphatized sponges from the Danian glauconitic sandstone from Nasi3ów (central Poland, Vistula River valley
    Autorzy:
    Świerczewska-Gładysz, E.
    Olszewska-Nejbert, D.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074484.pdf
    Data publikacji:
    2006
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    gąbki
    fauna gąbkowa
    sfosfatyzowane gąbki
    badania paleontologiczne
    mastrycht/dan
    Dolina Środkowej Wisły
    sponges
    phosphatization
    redeposition
    Maastrichtian/Danian
    Vistula river valley
    Opis:
    The sponge fauna from the Danian glauconitic sandstone as exposed at Nasiłów, contains all species known from the underlying Upper Maastrichtian siliceous chalk and, additionally, some species not documented hitherto from the latter unit. The stratigraphic ranges of the all studied sponges indicate their Late Maastrichtian age; there are no Danian sponges in the glauconitic sandstone. Two assemblages of sponges may be distinguished in the glauconitic sandstone, based on the analysis of the infilling of their interspicular space: 1) sponges infilled with phosphatized siliceous chalk and 2) sponges infilled with phosphatized glauconitic siliceous chalk. Petrographic study indicates that the host deposit of the first assemblage was a siliceous chalk. The second type originated from a glauconitic siliceous chalk unit, probably equivalent to the so-called Żyrzyn Beds of Late Maastrichtian age. The glauconitic chalk orginally overlain the siliceous chalk at Nasiłów, but has been subsequently eroded. Detailed analysis of the relations between two types of infillings allows to distinguish a latest Maastrichtian stage of erosion after deposition of the siliceous chalk, not recognised by previous authors. In this erosional stage, phosphatized sponges originally embedded in siliceous chalk were re-exposed and subsequently buried during the deposition of the glauconitic siliceous chalk unit.
    Źródło:
    Przegląd Geologiczny; 2006, 54, 8; 710-719
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rozmieszczenie i geneza form osuwiskowych w przełomowej dolinie Bobru w okolicach Wlenia (Sudety Zachodnie)
    Distribution and origin of landslide forms in the Bóbr river valley near Wleń (Western Sudetes)
    Autorzy:
    Kowalski, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075690.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    ruchy masowe
    geomorfometria
    analiza DEM LiDAR
    dolina rzeki Bóbr
    Sudety Zachodnie
    mass movements
    geomorphometry
    LIDAR DEMs analysis
    Bóbr River Valley
    Western Sudetes
    Opis:
    The paper presents results of field mapping and geomorphometric LiDAR DEM-based analysis of the Bóbr river valley (Izerskie Foothills, Western Sudetes), between Wleń and Nielestno, where a number of individual landslides and their groups were recognized in 2015-2016. The area affected by mass-movements is located within the Wleń Graben - a regional geological unit that constitutes the south-eastern prolongation of the North-Sudetic Synclinorium. The Wleń Graben is a NW-SE trending, elongated morphological and structural depression composed of sedimentary and volcanic rocks of Late Carboniferous, Permian, Triassic and Cretaceous age. The specific geological structure of the graben is reflected in geomorphic features of the study area. Based on mass movement classifications, the forms are considered as: (i) deep-seated rotational landslides (Świerkowa Dolina and Czerwony Wąwóz landslides); (ii) shallow slides and flows of weathered material and rock blocks (headwater areas in the south-western slopes of Gniazdo Hill, "Izerskie Gołoborza” locality), and (iii) complex landslide forms (deep-seated and shallow landslides on the south-eastern slopes of Gniazdo Hill). The studies confirmed the usefulness of geomorphometric analysis based on LiDAR-derived DEMs combined with field investigations. The landslides are located mainly in heavily forested mountainous areas. It was probably the main reason they had not been identified in the past.
    Źródło:
    Przegląd Geologiczny; 2017, 65, 10/1; 629--641
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ocena infiltracji efektywnej we fragmencie doliny Bugu k. Dręszewa z wykorzystaniem metody wskaźnikowej i modelowania hydrodynamicznego
    The evaluation of effective recharge in the Bug River Valley near the village of Dręszew (central Poland) using an index method and hydrodynamic modelling
    Autorzy:
    Szczypczyk, Angelika
    Powiązania:
    https://bibliotekanauki.pl/articles/20200506.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    efektywne zasilanie
    metoda indeksowa
    modelowanie hydrodynamiczne
    ArcGIS
    VisualMODFLOW
    Dolina Bugu
    woj. mazowieckie
    effective recharge
    index method
    hydrodynamic modelling
    Bug River Valley
    Masovian Voivodeship
    Opis:
    The research question undertaken in this paper is the evaluation of recharging infiltration in the vicinity of Dręszew. This village is located about 40 kilometres north of Warsaw. The research area is located in the Bug River Valley. Determination of effective infiltration is very important as it is largely responsible for recharging the aquifer. Currently, many methods and tools exist for determining infiltration. However, it is necessary to make the selection of the method dependent on the purpose, the scope of the study, and the scale of the study area, but also the temporal aspect should be taken into account. Two methods were used to assess groundwater recharge. The first one is an index method based on the calculation formula proposed by Witczak (2011). The calculations were performed using ArcGIS v. 10.3. software. The second recharging infiltration assessment method was used to solve the reverse of the hydrodynamic model. A numerical groundwater flow model was built using the VisualMODFLOW program. Two methods were used to ensure mutual verifiability. In excess of this, the choice of the indicator method along with the mathematical modelling method was related to the fact that both assume the influence of the presence of a shallow groundwater table, from which evaporation is possible, sometimes exceeding recharge.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 11; 816-825
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Osady rzeczne i roślinność interpleniglacjału zlodowacenia Wisły w dolinie Wisłoka między Rzeszowem a Lańcutem
    Alluvial deposits and vegetation of the Interpleniglacial period of the Vistulian Glaciation in the Wisłok River valley between Rzeszów and Łańcut (Sub-Carpathian Trough)
    Autorzy:
    Szczepanek, K.
    Kalinowicz, N.
    Gębica, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074524.pdf
    Data publikacji:
    2007
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    osady aluwialne
    dolina Wisłoka
    analiza pyłkowa i głębokich skamieniałości
    zlodowacenie Wisły
    alluvial sediments
    Wisłok river valley
    pollen and macrofossil analyses
    Middle Plenivistulian (Interpleniglaciał)
    Opis:
    The paper presents the results of geomorphological studies and pollen analysis performed for alluvial deposits at 2 sites situated in the Wisłok River valley. The deposits consist of thin layers of organic muds filling palaeochannels or thermo-karst lakes of the Wisłok River, dated at the Interpleniglacial (Grudziądz Interstadial) of the Vistulian Glaciation. These deposits build the lower part of a sand terrace, 8-12 m high, and outliers of this terrace buried by overbank alluvial sediments within a floodplain. The samples for pollen analysis were taken from a natural undercut in the Wisłok River channel and from a sand pit dug to a greater depth. The pollen diagrams prove the existence of trees (forest-steppe) including primarily Pinus sylvestris, Betula t. alba, Pinus cembra and Larix. The diagrams do not show a clear tendency of a plant succession and thus of any distinct climate changes. The sedimentation took place under cool, boreal climate conditions. The occurrence of several layers of organic and sand deposits in the sections does not reflect rhythmic warm/cold climatic oscillations documented in the Interpleniglacial alluvial sequences in Western European rivers, but is a result of vertical channel fluctuations and facies changes.
    Źródło:
    Przegląd Geologiczny; 2007, 55, 7; 595-600
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Uwarunkowania rozwoju pogrązów w aluwiach doliny Wisłoka w okolicach Rzeszowa (południowo-wschodnia Polska)
    Conditions for the development of load-cast structures in alluvial sedi- ments of the Wisłok River valley near Rzeszów (south-eastern Poland)
    Autorzy:
    Superson, J.
    Brzezińska-Wójcik, T.
    Gębica, P.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075041.pdf
    Data publikacji:
    2013
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    load-cast structures
    alluvial sediments
    Wislok river valley
    Weichselian glaciation
    south-eastern Poland
    pogrązowe struktury
    osady aluwialne
    dolina Wisłoka
    zlodowacenie Wisły
    południowo-wschodnia Polska
    Opis:
    The article presents the results of geological and geomorphological research concerning load-cast structures outcropping in the alluvial terrace sediments of theWisłok River in the Fore-Carpathian Erosional Valley. Given the large dimensions of these structures, reaching 1.5 m in some places, as well as their strong accumulation and diversity (i.e. drop-like and pocket-like structures), the authors attempted to establish the environmental factors that had determined the development of the structures in periglacial deposits of the Weichselian Glaciation. The structures were analysed in two accessible outcrops where sediments are represented by flood rhythmite and organic deposits, overlain by channel sands. Sandy load-cast structures occur in flood rhythmite and loamy deposits. The formation of load-cast structures probably started due to earthquakes in the Upper Pleniglacial period. The various shapes of load-cast structures were constrained by the various physical properties of the sediments and the escape of water during the deformation process.
    Źródło:
    Przegląd Geologiczny; 2013, 61, 2; 127--132
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Charakterystyka litologiczno-petrograficzna osadów czwartorzędowych w dolinie Warty (stanowisko Koźmin-Północ)
    The lithological and petrographic features of the Quaternary deposits in the Warta River valley (Kozmin-North site)
    Autorzy:
    Czubla, P.
    Forysiak, J.
    Petera-Zganiacz, J.
    Grajoszek, M.
    Wiśniewska, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075046.pdf
    Data publikacji:
    2013
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Quaternary deposits
    structural and textural features
    indicator erratics
    lithostratigraphy
    middle Warta River valley
    osady czwartorzędowe
    cechy strukturalne i teksturalne
    wskaźnik eratyków
    litostratygrafia
    Dolina Środkowej Warty
    Opis:
    The investigated area is located in the middle section of the Warta River valley, where the Neogen deposits with lignite series occur within the Adamów tectonic graben. In the Kozmin-North excavation, opened for extraction in 2008 and belonging to the "Adamów"Lignite Mine, the Neogene deposits are covered with an about 30-m thick Quaternary series. The research was carried out to identify the origin and age of the Quaternary sediments. As a result, four sandy series and three till series were identified, which were deposited during the South Polish Glaciations and Middle Polish Glaciations. North Polish Glaciations sediments developed in extraglacial conditions.
    Źródło:
    Przegląd Geologiczny; 2013, 61, 2; 120--126
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Subglacjalne pochodzenie przełomowych dolin zachodniej części progu środkowotriasowego i ciągu pagórów okolic Gogolina
    Subglacial origin of gorge valleys in western part of the Middle Triassic Ridge and the row of the hills near the Gogolin
    Autorzy:
    Salamon, T.
    Powiązania:
    https://bibliotekanauki.pl/articles/2074686.pdf
    Data publikacji:
    2009
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    rynna subglacjalna
    żwiry polodowcowe
    przełomowe doliny Odry
    próg środkowotriasowy
    tunnel channel
    eskers
    subglacial drainage
    gorge valley of the Odra River
    Middle Triassic Ridge
    Opis:
    The western part of the Middle Triassic Ridge is cut by two narrow gorges. At present the Odra River is running through the western gorge in the vicinity of Krapkowice and a small stream, right-bank tributary of this river, through the eastern one, passing 1–2 km to the east of the former. These erosive forms were hitherto interpreted as epigenetic gorges of the Odra. A row of elongated hills built of gravel and sands is found at southeasterly prologation of the eastern erosive gorge. The field study carried out at a site located at one of these hills indicates direct connections and subglacial origin of these erosive forms and hills. Most probably the eastern gorge represents a fragment of a subglacial tunnel valley, which continues northwards into the zone of the present-day Odra channel. The hills located at prolongation of the gorges are interpreted as eskers. Because of the high similarity, the western gorge valley is most probably also of subglacial origin. The studied part of the subglacial drainage system most probably originated in result of an outburst flood of subglacial water temporarily stored at the bottom of the ice-sheet. The tunnel valley and eskars were formed during Odranian glaciation.
    Źródło:
    Przegląd Geologiczny; 2009, 57, 3; 243-251
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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