Complex landslide terrain in the Kamienne Mountains, Middle Sudetes, SW Poland

Geomorphology ◽  
2010 ◽  
Vol 124 (3-4) ◽  
pp. 200-214 ◽  
Author(s):  
Piotr Migoń ◽  
Tomáš Pánek ◽  
Ireneusz Malik ◽  
Jan Hrádecký ◽  
Piotr Owczarek ◽  
...  
Keyword(s):  
Complex Landslide ◽  
Sw Poland ◽  
Landslide Terrain

Geomorphological, pedological and dendrochronological signatures of a relict landslide terrain, Mt Garbatka (Kamienne Mts), SW Poland

Geomorphology ◽  
2014 ◽  
Vol 219 ◽  
pp. 213-231 ◽  
Author(s):  
Piotr Migoń ◽  
Andrzej Kacprzak ◽  
Ireneusz Malik ◽  
Marek Kasprzak ◽  
Piotr Owczarek ◽  
...  
Keyword(s):  
Sw Poland ◽  
Landslide Terrain

Hazard assessment of a complex landslide: the case of Vestea (Abruzzo, Italy)

2016 ◽  
Vol 41 ◽  
pp. 112-115
Author(s):  
>Domenico >Aringoli ◽  
Mattia Ippolito ◽  
Nicola Sciarra ◽  
Bernardino Gentili ◽  
Marco Materazzi ◽  
...  
Keyword(s):  
Hazard Assessment ◽  
Complex Landslide

A new species of lambdarina (rhynchonellida, brachiopoda) from the viséan of central sudetes (Poland) and its phylogenetic position

2014 ◽  
Vol 64 (1) ◽  
pp. 1-12 ◽  
Author(s):  
Jolanta Muszer
Keyword(s):  
New Species ◽  
Full Range ◽  
Morphological Features ◽  
Phylogenetic Position ◽  
Growth Stages ◽  
Tropical Waters ◽  
Marginal Seas ◽  
Sw Poland ◽  
A New Species

Abstract A new species of micromorphic articulate brachiopod (Rhynchonellida) Lambdarina jugowiensis sp. nov., from the upper Visean (Sokolec Beds) of central Sudetes, SW Poland, is described. The studied specimens are calcified, what makes them unique in respect of their state of preservation. The material is represented by a full range of growth stages; from brephic to gerontic. Based on its morphological features and the palaeogeographical distribution of all its known species, two main evolutionary lines are proposed for the genus; the Australian and the European ones. Lambdarina was widely distributed in the equatorial-tropical waters of marginal seas of the Palaeotethys Ocean, mostly during Mississippian time.

Feldspar crystallization under magma-mixing conditions shown by cathodoluminescence and geochemical modelling – a case study from the Karkonosze pluton (SW Poland)

2004 ◽  
Vol 68 (4) ◽  
pp. 561-577 ◽  
Author(s):  
E. Słaby ◽  
J. Götze
Keyword(s):  
Magma Mixing ◽  
Main Tool ◽  
Precise Determination ◽  
Geochemical Modelling ◽  
Magma Evolution ◽  
Sw Poland ◽  
Crystallization Path ◽  
Geochemical Mass Balance

AbstractFeldspars from the Karkonosze pluton (SW Poland) display many features compatible with magma mixing. The mixing hypothesis has been tested using a geochemical mass balance law resulting in two possible paths of magma hybridization. Based on the results of the geochemical calculation, feldspar samples have been chosen along both mixing lines for cathodoluminescence (CL) investigation which was used as the main tool for the reconstruction of their crystallization path. Changes in the conditions of nucleation and crystallization of the feldspars as well as their movement within the magma chamber have been recognized due to different luminescence characteristics. These changes in the conditions of crystallization obtained by CL allow a precise determination of the genetic affinity of the samples to more mafic or more felsic environments.The results of the present study proved CL to be a valuable tool for the study of crystal-growth morphologies in a dynamic, turbulent environment and also as a geochemical tool for the reconstruction of various petrogenetic mechanisms (e.g. magma hybridization). Accordingly, the combination of CL with geochemical modelling provides corresponding information about magma evolution in an open system.

Radon in waters from health resorts of the Sudety mountains (SW Poland)

1997 ◽  
Vol 48 (6) ◽  
pp. 855-856 ◽  
Author(s):  
Wojciech Cie'zkowski ◽  
Tadeusz Andrzej Przylibski
Keyword(s):  
Sw Poland ◽  
Health Resorts ◽  
Sudety Mountains

scholarly journals Quantitative and Qualitative Research on the Waste from the Mining of Rock Raw Materials in Lower Silesia

Minerals ◽  
2018 ◽  
Vol 8 (9) ◽  
pp. 375 ◽  
Author(s):  
Urszula Kaźmierczak ◽  
Jan Blachowski ◽  
Justyna Górniak-Zimroz ◽  
Herbert Wirth
Keyword(s):  
Raw Materials ◽  
Mineral Resources ◽  
Geological Structure ◽  
Mining Activity ◽  
Road Engineering ◽  
Quantitative And Qualitative Research ◽  
Sw Poland ◽  
Natural Aggregates ◽  
Graphical Presentation ◽  
Lower Silesia

The Lower Silesia area in SW Poland is characterized by a geological structure that is conducive to mining activity. The exploitation of rock raw materials plays an important role in this sector of the economy. By the end of 2017, there were in total approximately 400 current concessions for the exploitation of rock raw materials in the analysed area (Polish Geological Institute, MIDAS database—Management and Protection System of Polish Mineral Resources). The conducted mining activity results in waste, which in the greatest amount occurs in the process of obtaining crushed road and construction aggregates, natural aggregates, carbonate raw materials for the cement and lime industry, as well as stone elements for construction and road engineering. At the end of 2016, the mining plants accumulated 26,569,600 Mg of waste. As part of the European Regions Toward Circular Economy (CircE) project, research was conducted on the volume and composition of the mining waste of rock raw materials in the years 2010–2016 within Lower Silesia. This research used the methods of statistical, descriptive and spatial analysis to identify mining plants with the highest potential for using their wastes. In the course of this study, 6 mining plants with the highest potential of using their waste for industrial production purposes were selected. In order to objectively select these plants, the methodology of qualitative multi-criteria analysis was developed, and 7 criteria were selected for assessing the economic potential of using waste from the mining of rock raw materials. An additional result of this research is a database and graphical presentation of changes in the spatial distribution of generated waste in the Lower Silesia region in the years ranging from 2010 to 2016.

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