Autor: Różycka, M. - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Osuwisko Vajont (Włochy) : przykład katastrofy przyrodniczej wywołanej działaniami człowieka
Vajont landslide (Italy) : an example of a natural disaster induced by human activity
Autorzy:: Różycka, M.
Duszyński, F.
Michniewicz, A.
Powiązania:: https://bibliotekanauki.pl/articles/2075676.pdf
Data publikacji:: 2017
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: osuwisko
zapora Vajont
Longarone
Monte Toc
Dolomity
landslide
Vajont dam
Dolomites
Opis:: Vajont landslide, which affected the northern slope of Monte Toc in the Dolomites (NW Italy), is one of the most famous examples of a natural disaster induced by human activity. A wave, generated by displaced material that filled the Vajont reservoir, overtopped the dam and destroyed a few villages in the nearby Piave valley, resulting in death of approximately 2000people. In this review paper, some facts about the disaster are presented and its triggering factors are discussed. Information related to tourism development in the area is also provided.
Źródło:: Przegląd Geologiczny; 2017, 65, 9; 560--563
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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Tytuł:: The Rogowiec Landslide Complex (Central Sudetes, SW Poland) : a case of a collapsed mountain
Autorzy:: Kasprzak, M.
Duszyński, F.
Jancewicz, K.
Michniewicz, A.
Różycka, M.
Migoń, P.
Powiązania:: https://bibliotekanauki.pl/articles/2059941.pdf
Data publikacji:: 2016
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: landslide
hillslopes
digital terrain model (DTM)
LiDAR
geomorphometry
electrical resistivity tomography
Opis:: The paper focuses on a large relict landslide complex in the northeastern part of the Kamienne Mts. (Sudetes, SW Poland) developed on Carboniferous and Permian volcanic and clastic sedimentary rocks. Whilst the presence of mass movements around Mt. Rogowiec has long been known, no attempts have yet been made to offer a comprehensive analysis. This study is based on recognition of geomorphic features from LiDAR-derived DTM, geomorphometric analysis, field geomorphological mapping, joint measurements at representative exposures, and electrical resistivity tomography. The total area affected by gravitational slope deformation exceeds 40 ha and consists of a few smaller units that show distinctive patterns of displacement. The eastern slopes of the Mt. Rogowiec ridge have been reshaped by large slides involving rigid blocks of trachyandesite in the upper part and deformed sedimentary successions in the middle and lower part. The central part of the area has experienced lateral spreading which resulted in complete disintegration of the volcanic cap. Fresh-looking ridge-top trenches indicate that this process is ongoing. Subsequent movements included flows into pre-existing valleys and rock wall collapses to produce spectacular block streams. The scale and variety of deformation structures at Mt. Rogowiec make this locality unique in the Sudetes.
Źródło:: Geological Quarterly; 2016, 60, 3; 695--713
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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