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Tytuł:
Dendrogeomorphological analysis of landslide activity along the planned S-69 road in the Węgierska Górka municipality (Beskid Śląski Mountains, S Poland)
Autorzy:
Wiktorowski, D.
Krąpiec, M.
Lutka, M.
Powiązania:
https://bibliotekanauki.pl/articles/955175.pdf
Data publikacji:
2017
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
landslides
dendrogeomorphology
Beskid Śląski
Polish flysch Carpathians
Opis:
Our dendrogeomorphological analysis was completed for 4 landslides, situated in the municipality of Węgierska Górka in the Beskid Śląski Mountains in Southern Poland. The local landslides pose a direct threat to the newly designed S-69 expressway running through the north-western part of the municipality. The research material consisted of 127 samples, collected with the use of a Pressler increment borer, from three species of coniferous trees (Norway spruce, Scots pine, and Silver fir). The landslide activity periods were identified on the basis of the splitting of the dendrochronological curves representing the upslope and downslope parts of the tree trunks. The largest number of the studied trees indicated reactions to substrate mass movements in 1964, 1971, 1972, 1984, 1994, 1997, 1998, and 2010. The detailed locations of the sampled trees allowed us to reconstruct the activities of particular landslide sections in time. We identified the fact that parts of the landslides located downslope of the planned road S-69 are more active than parts of the same landslides located above it on the slope. Geological conditions in the studied area favour landslide activity while precipitation is the main triggering factor of landslides.
Źródło:
Geology, Geophysics and Environment; 2017, 43, 2; 139-149
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Two ammonites from the Early Cretaceous deep-sea sediments of the Silesian Nappe, Polish Carpathians, and stratigraphic problems resulted from micropalaeontological dating of their sites
Autorzy:
Vašíček, Z.
Gedl, E.
Kędzierski, M.
Uchman, A.
Powiązania:
https://bibliotekanauki.pl/articles/191914.pdf
Data publikacji:
2010
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
ammonites
nannoplankton
dinocysts
biostratigraphy
Lower Cretaceous
flysch Carpathians
Opis:
Two ammonites Teschenites subflucticulus Reboulet and Criosarasinella mandovi Thieuloy have been found for the first time in the Flysch Carpathians. They occur in the so far poorly dated Early Cretaceous flysch deposits of the Silesian Nappe at Poznachowice Dolne, in the Upper Cieszyn Shale and the Hradiště (Grodziszcze) beds lithotypes, respectively. Teschenites subflucticulus points to Late Valanginian (Furcillata Zone), but nanno- plankton points to Late Hauterivian-Late Barremian and dinocysts to Late Hauterivian, all analyzed from the same sample. Criosarasinella mandovi points also to Late Valanginian (Furcillata Zone), what is not in contra-diction with the nannoplankton assemblage (Early Valanginian-Early Barremian) analyzed from the same bed, but dinocysts suggest Late Hauterivian. Preservation of the ammonites and sedimentary features of their host beds exclude redeposition. The difference in age by almost 3 Ma years between the ammonites and microfossils cannot be satisfactorily explained according to the current knowledge on their biostratigraphic meaning; it is left as it is as a dilemma.
Źródło:
Annales Societatis Geologorum Poloniae; 2010, 80, No 1; 25-37
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Peculiar calcite speleothems filling fissures in calcareous sandstones and their palaeohydrological and palaeoclimatic significance: an example from the Polish Carpathians
Autorzy:
Gradziński, M.
Duliński, M.
Hercman, H.
Górny, A.
Przybyszowski, S.
Powiązania:
https://bibliotekanauki.pl/articles/2060492.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
flysch Carpathians
Pleistocene
Holocene
speleothems
stable isotopes
ascending water
Opis:
Peculiar calcite speleothems developed in fissures in the Cergowa Sandstones were found in the Klęczany Quarry (Polish Western Carpathians). They represent flowstone and stalactites, rafts and various sparry crusts. Such speleothems, especially phreatic ones, are uncommon in the Outer Carpathians that are composed mainly of siliciclastic rocks of flysch type, with only limited calcium carbonate content. The speleothems analysed grew in vadose and phreatic conditions as well as at the air-water interface. Phreatic speleothems and thin rafts comprise calcite crystals of eccentric morphology. Based on their stable isotope composition the majority of the speleothems form two clusters. The first is characterized by d18O values between –9.8 and –8.5‰ and of d13C values between –5.7 and –0.6‰ whereas the second cluster of samples yields d18O values between –9.4 and –7.3‰ and d13C values from –11.5 to –9.7‰. Speleothems grew between 230+14–13 ka and Holocene time. Phreatic speleothems, including massive rafts, precipitated from ascending water of deep circulation whereas vadose and water table speleothems crystallized from local infiltration water charged with soil CO2. Mixing of both waters in the shallow phreatic zone is plausible.
Źródło:
Geological Quarterly; 2012, 56, 4; 711--732
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie facjalne wapieni typu sztramberskiego z polskich Karpat fliszowych
Autorzy:
Hoffmann, M.
Kołodziej, B.
Powiązania:
https://bibliotekanauki.pl/articles/183377.pdf
Data publikacji:
2008
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Karpaty fliszowe
wapienie typu sztramberskiego
Stramberk Limestone
flysch Carpathians
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 3/1; 176-177
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Structural control on the initiation and development of the Biała Wisełka Landslide Complex (Silesian Beskid, Outer Carpathians, Southern Poland)
Autorzy:
Sikora, R.
Powiązania:
https://bibliotekanauki.pl/articles/184722.pdf
Data publikacji:
2018
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
landslides
structural geology
lineaments analysis
LiDAR
Silesian Nappe
flysch Carpathians
Opis:
The numerous landslides which have developed in the mostly Cretaceous to Eocene turbiditic rocks of the Silesian Beskid are genetically and geometrically controlled by bedrock structural features, the Biała Wisełka Landslide Complex being no exception. Its location is in the headwater area of the Wisła River, on the slopes of Mt. Barania Góra (1220 m a.s.l.). The bedrock is represented by flysch strata of the Silesian Nappe (Outer Carpathian Fold-and-Thrust Belt), or, more specifically, the Upper Cretaceous turbiditic Upper Godula and Lower Istebna Beds of the Godula Thrust Sheet. The research work consisted in their mapping and structural analysis, facilitated by the use of a high-resolution digital elevation model based on LiDAR data. A comparative analysis enabled the determination of the relationships between landslides and the bedrock structure. The study results point to significant roles being played by the joint network, fault systems, the structural arrangement and the lithology of rock strata in the initiation and evolution of the studied landslide complex. An additional result of the methods applied methods was the identification and characterization of previously unknown fault zones in the study area.
Źródło:
Geology, Geophysics and Environment; 2018, 44, 1; 31-48
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dated landslides in the Gorce Mts. (Polish Outer Carpathians) : preliminary results
Autorzy:
Buczek, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/2058625.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
radiocarbon datings
landslide fen
mass movement activity
Holocene
Flysch Carpathians
Opis:
Preliminary results of dating landslides in the Gorce Mts. (Polish Outer Carpathians) are given, where ages of landslide activity have been poorly constrained. Four landslide zones with minerogenic mires (fens) were selected in order to determine the age of landslide movements, with depositional sequences of six fens being investigated by boreholes. Conventional radiocarbon dating of wood samples from mineral sediments sealing the landslide depressions was carried out to establish the age of landslide formation or rejuvenation. Loss on ignition analyses were obtained at 2.5 cm intervals along the cores to indicate possible delivery of allochthonous material into the peat bogs. Landslide formation in the Gorce Mts. corresponds to phases of mass movement hitherto identified in the Polish Outer Carpathians. Increased mass movements activity in the Gorce Mts. relate to cold and humid periods of the Holocene which occurred: ~11.1 ka cal BP, 8.6-8.0 cal BP; 6.5-5.9 ka cal BP, 4.8-4.5 cal BP, 3.3-2.5 cal BP and 1.75-1.35 cal BP. Loss on ignition analyses revealed changes in sedimentation in the landslide mires such as formation of mineral and illuvial horizons in peat sequences, and mineral covers overlying fens, associated with humid climatic phases of the Holocene.
Źródło:
Geological Quarterly; 2019, 63, 4; 849--860
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Przejawy mineralizacji w odniesieniu do procesów geotektonicznych w Karpatach fliszowych – nowe doniesienia
Mineral accumulations in reference to the geo- tectonic processes in the Flysch Carpathians – new data
Autorzy:
Jarmołowicz-Szulc, Katarzyna
Kleczyński, Piotr
Kozłowski, Adam
Gąsienica, Aleksander
Giro, Leszek
Powiązania:
https://bibliotekanauki.pl/articles/20231630.pdf
Data publikacji:
2023
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Karpaty fliszowe
realgar
gojazyt
paragenezy mineralne
Flysch Carpathians
goyazite
mineral parageneses
Opis:
Thirty rock and mineral samples were collected in the Rabe-Bystre area in the so-called Bystre slice in the Flysch Carpathians. The research concentrated on the mineral occurrence, parageneses and on the relationship to the tectonics. Red mineral realgar displays a pure content of arsenic sulphide. It occurs in veins and aggregates in the most frequent association with quartz. Fluid inclusions in the realgar crystals have been characterized and preliminarily measured, which is a totally new study in the Carpathian area. A new mineral – goyazite SrAl3(PO4)(PO3OH)(OH)6 – has been found as intergrowths in the realgar accumulations, and its characteristics are provided. It seems that the quartz-carbonates-bitumen paragenesis in the study region is related to the distinct tectonic mélange zones, while the ore mineralization should be referred to fault zones and fissures, and/or the mélange zones. It has an epigenetic character, and may be referred to the adjacent potential magmatic body and mineralized waters in the neighbourhood.
Źródło:
Przegląd Geologiczny; 2023, 71, 4; 188-196
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wyznaczenie przemieszczeń powierzchniowych na osuwisku w Kłodnem (gmina Limanowa, południowa Polska)
Determination of surface displacement on the landslide in Kłodne (Limanowa community, southern Poland)
Autorzy:
Ćwiąkała, P.
Stanisz, J.
Wróbel, A.
Kaczmarczyk, R.
Drwal, P.
Grabek, P.
Daroch, M.
Pękala, M.
Świątek, M.
Zierkiewicz, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075554.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Karpaty fliszowe
osuwiska
monitoring geodezyjny
Kłodne
flysch Carpathians
landslides
geodetic monitoring
Opis:
Examination of the landslide in Kłodne was carried out in 2013 and 2014. The work was divided into two parts: geological engineering investigations (mapping of the external borders of the landslide) and geodetic surveying (photogrammetric studies and monitoring of surface movements). The boundaries of the landslide were marked using a Garmin eTrex GPS receiver and a geological compass (Freiberg). The boundaries have not changed and is convergent with previous studies. In the south-western part of the landslide the boundary is blurred as a result of anthropogenic transformation of the area. In the south-eastern part (as at May17, 2014) about 200 m3 of the colluvial material has been moved. Photogrammetric studies were based on the analysis of aerial photos from May 26, 2009 (prior tothe landslide formation) and on the orthophotomap created from images taken in July 2010, after the formation of the landslide. Displacement vectors were determined by comparing the locations of specific terrain details in the pictures taken before and after the mass movements occurred. In the upper part of the landslide the maximum horizontal displacement value was 87.7 m, the minimum was 6.2, and the average – 84.5 m. In the lower part of the landslide the horizontal displacements amounted to 65.5 m, had a minimum value of 10.3, and an average of 54.8 m. In the last stage of the study the base measurement network was created. It consisted of 68 points stabilized in the ground. The measurements were performed using the static GNSS observations method and linear-angular measurements carried out with a precise total station. In 2013, horizontal displacements ranged from 1 to 8.1 mm, and vertical ones ranged from –9.8 to 13.5 mm. In 2014, there were displacements observed in the vicinity of the main slope. They were directed to the south. The horizontal displacement vector has reached values from 2 to 94 mm, and the vertical vector was from –63 to 16 mm.
Źródło:
Przegląd Geologiczny; 2016, 64, 2; 122--130
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
On the origin of chloride waters in the Polish Flysch Carpathians
Autorzy:
Zuber, A.
Chowaniec, J.
Borowiec, M.
Powiązania:
https://bibliotekanauki.pl/articles/2062987.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
chloride waters
ultrafiltration
diagenetic waters
oil-field waters
catagenesis
flysch Carpathians
Opis:
Chloride waters in the Polish Flysch Carpathians are remnants of marine sedimentation water which was chemically and isotopically changed due to ultrafiltration and the release of dehydration water (diagenetic water) during the burial diagenesis of clay minerals. In the western part of the study area, the diagenetic end-member is characterized by δ18O and δ2H values of about +6.5 and –30.0‰, respectively, and Cl– content in the range of 3.8 and 13.8 g/dm3. In some fault areas, such waters migrate to the surface and mix with local meteoric waters as indicated by mixing lines in δ18O–δ2H and δ18O–Cl– graphs. In several wells of the eastern part, waters containing a significant proportion of marine water occur. However, in majority of deep wells, mixtures of diagenetic and meteoric waters of Quaternary and pre-Quaternary climates are present, as deduced from δ18O–Cl– linear relations. In most cases, they do not exhibit linear relations also expected in δ18O–δ2H graphs due to the shifts of δ2H to heavier isotopic values supposedly caused by involvement of water in the generation of hydrocarbons.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2010, 441 Hydrogeologia z. 10; 201--208
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geotourism during excursions in the northeastern part of The Gorce National Park
Geoturystyka podczas spaceru w północno-wschodniej części Gorczańskiego Parku Narodowego
Autorzy:
Barmuta, M.
Powiązania:
https://bibliotekanauki.pl/articles/905901.pdf
Data publikacji:
2011
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
geomorfologia
Karpaty fliszowe
Gorce
geoturystyka
Gorce Mountains
flysch Carpathians
geotourism
geomorhology
Opis:
The Gorce Mountains National Park is located on the southern part of the Małopolska Province in Poland. Despite the lack of spectacular geological attractions it is a very good site to promote Earth Sciences knowledge and especially to educate in geology. The example of the on-day excursion going along the touristic trails within The Gorce Mountains National Park is being described in the presented paper. The author described great diversity of the geological and geomorphological elements, presenting educational values.
Gorczański Park Narodowy znajduje się w południowej części Małopolski. Mimo braku spektakularnych atrakcji geologicznych jest bardzo dobrym miejscem do promowania wiedzy z zakresu nauk o ziemi, a w szczególności geologii. W poniższym artykule opisano przykład jednodniowej wycieczki, przebiegającej wzdłuż szlaków Gorczańskiego Parku Narodowego, w której wykazano dużą różnorodność elementów geologicznych i geomorfologicznych.
Źródło:
Geotourism / Geoturystyka; 2011, 3-4; 51-62
1731-0830
Pojawia się w:
Geotourism / Geoturystyka
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The structural control of the Mroczna Cave development on the slopes of Mt Kornuty (the Flysch Carpathians, Beskid Niski Mts)
Autorzy:
Zatorski, M.
Powiązania:
https://bibliotekanauki.pl/articles/295108.pdf
Data publikacji:
2014
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
mass movements
flysch Carpathians
crevice-type cave
structural control
anisotropic rock massif
Opis:
The Mroczna Cave is one of the longest caves in the Beskid Niski Mts., located on the south-western slopes of Mt Kornuty, along the main scarp of the landslide. According to the geomechanical criterion, it is dilation cave, where extension has played a major role. Morphotectonic analysis indicates that the main gravitational movement was of a toppling nature but there were also rotation around the vertical axis as well as a backward rotation. The relatively large cave depth (15.5 m) and its shape (cross-section of its passages) indicate that it was formed along a new gravitational cutting surface of the rock massif, associated with joint sets.
Źródło:
Landform Analysis; 2014, 27; 55-65
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ryzyko wykorzystania modeli numerycznych do identyfikacji zasobów wodnych w Beskidzie Wyspowym (Karpaty Zewnętrzne)
Problem with the use of computer models in water management In the outher Carpatians (Flysh) – an example of the Kłodne village
Autorzy:
Bar-Michalczyk, D.
Michalczyk, T.
Juśko, K.
Dendys, M.
Powiązania:
https://bibliotekanauki.pl/articles/338072.pdf
Data publikacji:
2015
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
gospodarka wodna
Karpaty fliszowe
modelowanie matematyczne
flysch Carpathians
numerical modelling
water management
Opis:
Badania terenowe przeprowadzono w okresie niskich stanów wód w zlewni częściowej potoku Smolnik, obejmującej zlewnie potoków Kłodnianka i Bukowiec. Skonstruowano jednowarstwowy model filtracji ustalonej lokalnego pola filtracji wód podziemnych metodą różnic skończonych w programie Visual MODFLOW. Wykorzystanie modelowania matematycznego do oceny możliwości zwiększenia eksploatacji zasobów wodnych przysporzyło wielu problemów. Obszar badań cechuje się trudną do odwzorowania, złożoną budową geologiczną. Duża jego część jest aktywnym osuwiskiem. Niewielkie rozpoznanie budowy geologicznej obszaru przekłada się na jakość odwzorowania warunków krążenia wód podziemnych. Problemem wymagającym rozwiązania jest brak wiedzy o wielkości rzeczywistego poboru wód podziemnych z prywatnych studni przyzagrodowych. Celem prac było wyznaczenie obszarów perspektywicznych dla poboru wody pitnej w obszarze działania wodociągu wiejskiego w miejscowości Kłodne.
Numerical modelling is a frequently used tool in the assessment of both available groundwater resources and for optimization of water management in shortage areas. Field studies in the Kłodne and Męcina area were carried out in December 2012, in the period of low water level after a long term drought. Archive and collected data on groundwater levels and flows in streams were the base for creation a one-layer steady state hydrodynamic model of the local area. Possibilities of increasing aquifer exploitation in the study area were evaluated with the finite difference method in Visual MODFLOW V.4.2 package. Modelling the Carpathians gives rise to many problems. First problem with model construction was the description of geological structure, which resulted in low fidelity model. Study area has a complicated geological structure with large part of the active landslide. Flysch Carpathians are characterised by a lack of continuity of aquifer structures but the software allows to characterise only continuous layers in the model. Furthermore, real groundwater intake was burdened by high uncertainty. Specific water use is registered. Problematic was to estimate unregistered exploitation by private farmstead wells fairly widespread in the study area.
Źródło:
Woda-Środowisko-Obszary Wiejskie; 2015, 15, 3; 5-14
1642-8145
Pojawia się w:
Woda-Środowisko-Obszary Wiejskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dendrogeomorphological analysis of the Sawicki Landslide in the Beskid Niski Mountains (S Poland)
Autorzy:
Krąpiec, Marek
Nawrocka, Natalia
Margielewski, Włodzimierz
Szychowska-Krąpiec, Elżbieta
Powiązania:
https://bibliotekanauki.pl/articles/2058623.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
dendrogeomorphological analysis
complementary method
complex-type landslide
Polish Flysch Carpathians
southern Poland
Opis:
We applied dendrochronological analysis to study an extensive (~2.5 km long) complex-type landslide in the Beskid Niski Mountains (Polish Flysch Carpathians), which was rejuvenated in historical time (the earliest transformation occurred in 1913). We used three complementary methods (dating of eccentricity of annual growth rings, eccentricity indices, and analysis of reaction wood), based on seven species of deciduous and coniferous trees. A total of 204 trees were sampled and 408 cores collected using a Pressler increment borer. Based on the dendrochronological analysis, the activity of various parts of the landslide in the past century is presented, which appears to have been diverse and influenced mostly by precipitation. The upper part of the landslide was active from the 1920s until the 1940s. In the middle section of the landslide, intensifications of gravitational movement were repeatedly recorded after intense rainfalls throughout the entirety of the last century. The highest landslide activity was dendrochronologically detected in the 1980s and 1990s. Increasing landslide activity during so-called “dry years” may have been related to quick drying of the bedrock, resulting in changes in rock strength parameters. Our results indicate significant susceptibility of this particular slope-valley geosystem in response to even slight hydrogeological changes (including dryness), which can trigger ground movement.
Źródło:
Geological Quarterly; 2019, 63, 4; 801--810
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rainfall thresholds for the occurrence of shallow landslides determined for slopes in the Nowy Wiśnicz Foothills (Polish Flysch Carpathians)
Autorzy:
Demczuk, Piotr
Zydroń, Tymoteusz
Siłuch, Marcin
Powiązania:
https://bibliotekanauki.pl/articles/2058628.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
landslide
slope stability
rainfall threshold
VADOSE/W
SLOPE/W
Polish Flysch Carpathians
Opis:
Values of rainfall thresholds on selected shallow landslide slopes (Dział, Gwoździec) located in the Nowy Wiśnicz Foothills are determined using a physically-based slope stability model considering a long-term period of analysis (GeoSlope Inc. software). Slope stability analysis included determination of the impact of rainfall on changes of stress state within the soil substrate and their influence on estimation of mass movement risk. The slope stability calculation results have shown that the rainfall threshold values are a function of many variables, primarily the hydraulic properties of soil and rock substratum, temporal distribution of precipitation, and soil moisture content conditions in the period proceeding rainfall. The results of the calculations indicate that, in extreme cases, accumulated rainfall threshold values for the same slope can range from ~100 to 500 mm. Estimated rainfall threshold values were lower than those values reported in the literature for the Polish Carpathians, but are similar to those determined by Guzetti et al. (2007) for Central and Southern Europe.
Źródło:
Geological Quarterly; 2019, 63, 4; 822--838
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zagrożenia osuwiskowe na trasie budowy drogi ekspresowej S-7 na odcinku Lubień–Naprawa (Karpaty fliszowe)
Landslides hazard in the construction of the expressway S-7 on the Lubień-Naprawa section (Flysch Carpathians)
Autorzy:
Wójcik, Antoni
Jurczak, Sebastian
Wnuk, Mariusz
Janik, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/2075953.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ruchy masowe
Karpaty fliszowe
osuwisko
Polska południowa
mass movements
Flysch Carpathians
landslide
Southern Poland
Opis:
Landslide recognition is an important task for designers and contractors during the road construction process. The problems that contractors often face is insufficient recognition of the geological structure (at the design stage), too small area of purchased land under the "ZRiD’'decision, or the inability of fast responding to emerging threats. The studies described in this article shed more light on the complexity of slope deformation as a result of landslide processes. During the constructing of the expressway S-7, the problems related to deep landslide processes occurred, which most probably were associated with poorly recognized old “rocky-weathering material” type of landslide. The geological survey performed during the construction of this road, confirmed the occurrence of deep (>20 m) displacements, recorded by the inclinometer measurements. These deep displacements are linked to a large landslide with a main scarp located in the region of Mt. Cymbalowa Góra.
Źródło:
Przegląd Geologiczny; 2019, 67, 5; 388--396
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł

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