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    Tytuł:
    Zasięg obszarów objętych osuwiskami w Górach Kamiennych (Sudety Środkowe) : porównanie map geologicznych i cyfrowego modelu wysokości z danych LiDAR
    The extent of landslide-affected areas in the Kamienne Mountains (Middle Sudetes) : a comparison of geological maps and a LiDAR based digital elevation model
    Autorzy:
    Migoń, P.
    Jancewicz, K.
    Kasprzak, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075163.pdf
    Data publikacji:
    2014
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    landslides
    digital elevation model (DEM)
    lidar
    geological mapping
    Sudetes
    osuwiska
    cyfrowy model wysokości
    LIDAR
    mapowanie geologiczne
    Sudety
    Opis:
    The east-central part of the Kamienne Mountains in the Sudetes has long been known as an area where landslides occur in abundance. Their extent was shown on first detailed geological maps from the early 20th century and later on Polish geological maps published in the 1970 and 1990. The total landslide area mapped was about 100 ha. The availability of LiDAR data allowed to build digital elevation models of very high resolution and to attempt landslide mapping using diagnostic landform assemblages as guidelines. 30 separate landslides have been mapped, including complex landslide areas involving overlapping landslide bodies oflikely different origin. The total landslide area is at least300 ha, while the largest complexes cover 40-50 ha. LiDAR-based models proved extremely useful in landslide mapping, espe- cially in forested areas.
    Źródło:
    Przegląd Geologiczny; 2014, 62, 9; 463--471
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rzeźba osuwiskowa południowo-wschodniej części Gór Wałbrzyskich, Sudety Środkowe
    Landslide morphology of the south-eastern part of the Wałbrzyskie Mountains, Middle Sudetes
    Autorzy:
    Kotwicka, Wioleta
    Jancewicz, Kacper
    Migoń, Piotr
    Powiązania:
    https://bibliotekanauki.pl/articles/2075893.pdf
    Data publikacji:
    2019
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    osuwiska
    geomorfometria
    LiDAR
    Sudety
    landslides
    geomorphometry
    Sudetes
    Opis:
    The occurrence of landforms induced by large-scale mass movements has never been reported from the SE part of the Wałbrzyskie Mts., despite detailed geological field mapping carried out twice in the 20th century. This paper provides the first description of landslide-affected slopes in this area, recognized through the combination of LiDAR DEM interpretation and field work. Fifteen landslides have been identified, ranging in size from less than 1 ha to 10.44 ha. Morphological signatures suggest that they represent various types, including minor translational slides, larger rotational complexes and valley-confined flowslides. Closed depressions typify several landslides. In a few instances the valley blocking by landslides can be inferred.
    Źródło:
    Przegląd Geologiczny; 2019, 67, 10; 828--836
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Litologiczny wskaźnik przemieszczeń materiału skalnego jako element oceny podatności stoków na osuwanie
    Lithological displacement index as an element of landslide susceptibility assessment
    Autorzy:
    Wódka, Marcin
    Powiązania:
    https://bibliotekanauki.pl/articles/20051858.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    litologiczny wskaźnik przemieszczeń
    osuwisko
    Cyfrowy Model Terenu
    DTM
    wielookresowy LIDAR
    lithological displacement index
    landslide
    Digital Terrain Model
    multi-temporal LIDAR
    Opis:
    The use of multi-temporal LIDAR data in the study of landslides gives many possibilities. The increasing-over-time availability of ALS data encouraged research on development of landslides using Differential Digital Terrain Models. An important passive factor that determines the development of landslides (especially in the Carpathians) is lithology. The author propose a new lithological displacement index, that dscribes the volume of displaced ground (m3 ) per area of 1 m2 of a given lithological unit. The example of the test area of Rożnowskie Lake has shown that lithological displacement index can assess the landslide susceptibility, which is variable and depends on the amount of rainfall. During periods of heavy rainfall, large volumes of displaced rock masses were recorded in the thick-bedded formations. In dry periods, the trend is reversed.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 9; 695-700
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    W jaki sposób struktura podłoża warunkuje rozwój osuwiska translacyjnego? Przykład osuwiska we Włodowicach w Obniżeniu Noworudzkim (Sudety Środkowe)
    How the bedrock structure determines development of translational landslide? An example of the Włodowice landslide in the Nowa Ruda Basin, Central Sudetes
    Autorzy:
    Kowalski, Adam
    Powiązania:
    https://bibliotekanauki.pl/articles/20197001.pdf
    Data publikacji:
    2022
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    ruchy masowe
    osuwisko translacyjne
    analiza LIDAR-DEM
    synklinorium śródsudeckie
    Sudety Środkowe
    mass movements
    translational landslide
    LIDAR DEMs analysis
    Intra-Sudetic Synclinorium
    Central Sudetes
    Opis:
    In this contribution the author presents the results of geological and geomorphological field mapping and structural analyses conducted within the area of a newly recognized landslide situated near Włodowice, in the southern part of the Nowa Ruda Basin (Central Sudetes, SW Poland). The landform is located within the eastern limb of the Intra-Sudetic Synclinorium (Nowa Ruda Monocline) built of Upper Carboniferous to Lower Permian (Rotliegend) sedimentary rocks. Geomorphological characteristics of the landslide are presented, but the greatest attention is paid to the way of transformation of individual structural elements of basement rocks (bedding surfaces, sets of fractures) by mass movements. The study allows recognition and interpretation of landslide type according to failure mechanism - the analysed form represents a typical translational landslide with a flat, structural slip surface related to bedding planes. A model of the development of a translational landslide under specific geological conditions (monoclinal structure built of different lithological varieties of sedimentary rocks with different rheological properties) is presented. Due to the partial exposure of the slip surface in the upper and lower parts of the landslide, the form should be considered unique among the previously identified landslides in the Sudetes Mts. During this study the author repeatedly confirms the usefulness of analyses of LiDAR models in landslide investigations.
    Źródło:
    Przegląd Geologiczny; 2022, 70, 9; 722-732
    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:
    Zastosowanie bezzałogowego statku latającego (UAV) w monitoringu powierzchniowym ruchów masowych na przykładzie osuwiska w Kasince Małej (Beskid Wyspowy, Zewnętrzne Karpaty Zachodnie)
    The application an unnamed aerial vehicle (UAV) in landslides surface monitoring – case study of the Kasinka Mała landslide (Beskid Wyspowy Mts., Outer Carpathians Mts.)
    Autorzy:
    Karwacki, Krzysztof
    Powiązania:
    https://bibliotekanauki.pl/articles/2075943.pdf
    Data publikacji:
    2019
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    monitorowanie osuwisk
    dopasowanie obrazu
    LIDAR
    fotogrametria
    UAV
    landslide monitoring
    image matching
    photogrammetry
    Opis:
    Landslide monitoring is applied in case of a hazard for existing infrastructure located on hazardous landslide. It is the exact case of the Kasinka Mala landslide in the Outher Carpathians which causes a danger for the surrounding infrastructure. In order to measure the terrain deformations caused by landslide movements, the unnamed aerial vehicle equipped with a non-metric camera has been used. As a result of processing of aerial photos, orthophotomaps as well as digital elevation models have been produced. It enabled providing information about vertical and horizontal displacements caused by the landslide. The results of analysis shows that the mass movements occur at a different pace, but also that there are stable areas in the landslide. The application of UAV photogrammetry for landslide monitoring allows getting the information about the displacements in the unvegetated areas.
    Źródło:
    Przegląd Geologiczny; 2019, 67, 5; 339--350
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    O konieczności wykonania drugiej edycji Szczegółowej Mapy Geologicznej Sudetów w skali 1 : 25 000 : przykłady rewizji budowy geologicznej z wykorzystaniem podkładu lidarowego numerycznego modelu powierzchni terenu
    About the need to develop the second edition of the detailed geological map of the Sudetes at the scale of 1 : 25,000 : examples of a revision of the geological pattern using the LIDAR Digital Elevation Models
    Autorzy:
    Wojewoda, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075533.pdf
    Data publikacji:
    2016
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    mapy geologiczne
    weryfikacja danych
    podkład lidarowy
    geological maps
    data revision
    LIDAR DEM
    Opis:
    The currently available map sheets issued under the edition of the Detailed Geological Map of the Sudetes at the scale of1 : 25,000 (SMGS25), and especially those compiled in the 1950s and 1960s, does not meet the requirement of uniformity and accuracy of mapping, and they do not contain some key information that has been acquired as a result of multidisciplinary geological studies in the Sudetes over the last half-century. New research tools, such as LIDAR models of the land surface (DEM), allow for partial migration of data and (or) the implementation of recent research results, however, it should be verified by experienced geologists in the field. This is documented by two examples of their use to different areas in the Sudetes, which are composed primarily of sedimentary rocks.
    Źródło:
    Przegląd Geologiczny; 2016, 64, 9; 597--603
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Geneza i geologiczne uwarunkowania rozwoju form osuwiskowych w środkowej części Obniżenia Noworudzkiego w Sudetach
    Origin and geological constraints for the development of landslide forms in the central part of the Nowa Ruda Basin, Sudetes
    Autorzy:
    Kowalski, Aleksander
    Powiązania:
    https://bibliotekanauki.pl/articles/20028318.pdf
    Data publikacji:
    2021
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    ruchy masowe
    głęboko osadzone osuwiska
    skały osuwiskowe
    analiza LIDAR DEM
    synklinorium śródsudeckie
    Sudety Środkowe
    mass movements
    deep-seated landslides
    rock topple
    LIDAR DEM analysis
    Intra-Sudetic Synclinorium
    Middle Sudetes
    Opis:
    The paper presents the results of field mapping and structural analyses conducted within the landslides situated near Ludwikowice K³odzkie, in the central part of the Nowa Ruda Basin (Middle Sudetes, SW Poland). The area affected by mass movements is located within the eastern limb of the Intra-Sudetic Synclinorium (Głuszyca Monocline) composed of Upper Carboniferous to Lower Permian (Rotliegend) sedimentary rocks. Nine individual landslide forms, ranging in area from 0.5 to 22.7 ha, including two landslide complexes (Sokółka landslides, 49.7 ha in total area) have been identified and described in terms of their origin and geological conditions. Studies of landslide morphology and structural analysis allow recognition of several types of mass movements. They include: (i) rotational landslides (landslides Sokółka 1-3 and 5); (ii) translational slides (landslides Miłków 1-3); (iii) deep-seated, compound landslides (landslide Sokółka 4), and (iv) topple evolving into deep-seated rotational (?) slide (Sławosz landslide). The studies repeatedly confirm the usefulness of analyses of LiDAR digital elevation models coupled with field investigations and structural analyses.
    Źródło:
    Przegląd Geologiczny; 2021, 69, 10; 666-697
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Ruchy masowe a interpretacja budowy geologicznej : przykład osuwiska na górze Drogosz w paśmie Zaworów (Sudety Środkowe)
    Impact of mass movements on geological interpretation : an example of the Drogosz hill landslide within the Zawory Range (Central Sudetes)
    Autorzy:
    Kowalski, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075779.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    osuwiska
    mapowanie geologiczne
    LiDAR
    Sudety
    basen Krzeszów
    landslides
    geological mapping
    Sudetes
    Krzeszów Basin
    Opis:
    Recognition and precise delimitation of landslide-affected areas, especially in the mountains, have been a challenge so far. New opportunities emerged after dissemination of high- resolution Digital Elevation Models generated by Airborne Laser Scanning (ALS), which are also used to processing and visualization of geological data. This paper touches the issue in both aspects mentioned above, and presents results of morphometric analysis of a landslide on the northern slope of the Drogosz hill within the Zawory Range, in the southern part of the Krzeszów Basin (Central Sudetes). Attempts ofreconstruction ofthe slip surface and estimation oftotal volume of the landslide colluvialfill were undertaken. Furthermore, differential maps were compiled. They were a basis for the spatial distribution of thickness evaluation. The Drogosz hill landslide seems to be strictly related to the geological structure of the research area. The Zawory Range is composed of Upper Cretaceous, Lower Triassic (Buntsandstein) and Permian (Rotliegendes) rocks. Lack of recognition of landslide phenomena was probably the main reason of misleading interpretations of the Krzeszów area geology. The paper also provides comments on the existing concepts of the geological structure of the Krzeszów Basin, especially of the Łączna Anticline.
    Źródło:
    Przegląd Geologiczny; 2017, 65, 2; 96--104
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Lotniczy skaning laserowy (LiDAR-ALS) jako źródło danych do obliczeń stateczności skarp na terenach zadrzewionych i zakrzewionych
    Airborne laser scanning (LiDAR-ALS) as a source of data for calculations of escarpment stability in wooded and bushy areas
    Autorzy:
    Piechota, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075700.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    lotniczy skaning laserowy
    ALS
    skaning laserowy
    LiDAR
    globalny system nawigacji satelitarnej
    GNSS
    cyfrowy model terenu
    DTM
    pomiar nachylenia
    kontrola jakości
    Airborne Laser Scanning
    Light Detection And Ranging
    Global Navigation Satellite System
    digital terrain model
    slope measurement
    quality control
    Opis:
    The paper discusses the problem of quick acquire height data for calculation of escarpment stability. In past the slope of profile was obtainedfrom classical land survey methods (like Total Station, GNSS, etc.), carto- metric measurement on maps or measurements based on a Digital Terrain Modelfrom aerial photography. Now we have a new method that is Airborne Laser Scanning (LiDAR-ALS). In 2011-2014 almost all country was measured in this method. The declared accuracy of height measurement on the durable surfaces is about 0.10-0.15 m. Author compared this method with classical method Global Navigation Satellite System - Real Time Network (GNSS-RTN) on two wooded and bushy areas. The comparison was based on the measurement characteristic points on the profiles and acquisition of height data from LiDAR-ALS data. Data in this method were obtained in two ways: from point cloud and from DTM createdfrom this point cloud. In the next step, height differences were calculated and these data were subjected to basic statistical calculations. The result of the study was a mean error of height data from LiDAR-ALS and conclusions about its usefulness in acquire height data for calculation of escarpment stability.
    Źródło:
    Przegląd Geologiczny; 2017, 65, 10/2; 811--816
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-10 z 10

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