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Journal articles on the topic 'The Sudetes'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Stojakowska, Wanda. "Myxomycetes of the Sudetes." Acta Mycologica 19, no. 2 (2014): 207–43. http://dx.doi.org/10.5586/am.1983.020.

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A floristic-ecological monograph of the Myxomycetes of the Sudetes is made. In the years 1965-81 on an investigated area 112 species were recorded (104 species in the Western Sudetes, 80 - in the Central Sudetes, 68 - in the Waster Sudetes), among them 3 mountain species (<i>Diderma ochraceum, Cribraria rubiginosa</i> and <i>C. ferruginea</i>) and 37 species new for the Sudetes. <i>Physarum listeri</i> and <i>Reticularia lobata</i> in Poland are known only from this area.

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2

Urban, Grzegorz. "Snow cover and its variability in the Polish Sudetes Mts. and the Sudetic Foreland." Geografie 121, no. 1 (2016): 32–53. http://dx.doi.org/10.37040/geografie2016121010032.

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The paper presents the snow cover characteristics in the vertical profile of the Polish Sudetes Mountains and their foreland during the period of 1965/66–2007/08. The analysis was based on the number of days with snow cover ≥ 1 cm and its depth in a month, winter season (December–February) and entire year (season). Data was collected at 20 weather stations operated by the Institute of Meteorology and Water Management. The maximum depth of snow cover in the foreland and lower parts of the Sudetes Mountains was recorded in January, in higher parts of the mountains in mid-February or in March. On

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3

Aleksandrowski, P., R. Kryza, S. Mazur, C. Pin, and J. A. Zalasiewicz. "The Polish Sudetes: Caledonian or Variscan?" Transactions of the Royal Society of Edinburgh: Earth Sciences 90, no. 2 (1999): 127–46. http://dx.doi.org/10.1017/s0263593300007197.

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AbstractThe Polish Sudetes on the NE margin of the Bohemian Massif comprise a complex mosaic of pre-Permian basement units, traditionally included in the Variscides. A hypothesis of significant Caledonian orogenesis in this area originated in the 1920s, was subsequently rejected, and then was recently revived in models which invoked Early Palaeozoic to Early-Mid Devonian subduction and continental collision along a proposed extension of the Tornquist suture zone. We reassess the evidence invoked in support of the Caledonian orogeny, such as supposed regional pre-Upper Devonian unconformity, Or

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4

Moczydłowska, Małgorzata. "Comments on ‘Evidence for a Caledonian orogeny in Poland’ by J. D. Johnston, J. A. Tait, J. H. Oliver and F. G. Murphy." Transactions of the Royal Society of Edinburgh: Earth Sciences 86, no. 3 (1995): 227–30. http://dx.doi.org/10.1017/s0263593300002236.

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In a recent paper Johnston et al. (1994) have provided an innovative interpretation of the tectonostratigraphic relationships between distinct terranes juxtaposed along the Intra–Sudetic Fault in the Sudetes Mountainsof the Polish Variscides. They identified this fault as a major crustal fracture between Gondwana and Baltica, rramed the Tornquist Suture, resulting from the closure of the Tornquist Sea during the Caledonian orogeny. This interpretation is based on new U/Pb ages on zircon and titanite from igneous and metamorphic rocks (Oliver et al. 1993), field observations and reassessment of

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5

ALEKSANDROWSKI, P., R. KRYZA, S. MAZUR, and J. ŻABA. "Kinematic data on major Variscan strike-slip faults and shear zones in the Polish Sudetes, northeast Bohemian Massif." Geological Magazine 134, no. 5 (1997): 727–39. http://dx.doi.org/10.1017/s0016756897007590.

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The still highly disputable terrane boundaries in the Sudetic segment of the Variscan belt mostly seem to follow major strike-slip faults and shear zones. Their kinematics, expected to place important constraints on the regional structural models, is discussed in some detail. The most conspicuous is the WNW–ESE Intra-Sudetic Fault Zone, separating several different structural units of the West Sudetes. It showed ductile dextral activity and, probably, displacement magnitude of the order of tens to hundreds kilometres, during late Devonian(?) to early Carboniferous times. In the late Carbonifer

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6

Wójcicka-Rosińska, Anna, Dariusz Rosiński, and Ewa Szczęśniak. "Ophrys apifera Huds. (Orchidaceae) on a heap of limestone mine waste – the first population found in the Sudetes and the second in Poland." Biodiversity Research and Conservation 59, no. 1 (2020): 9–14. http://dx.doi.org/10.2478/biorc-2020-0007.

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Abstract The paper reports the finding of a new locality of Ophrys apifera – the first locality of this species in the Sudeten range and the second in Poland. A new population was found in the Kaczawskie Mts. (Western Sudetes). It consists of 23 flowering plants and occurs in an operating limestone quarry. The detailed data on this population and its habitat are included.

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7

Filipiak, Maciej. "Distribution of silver-fir (Abies alba Mill.) in the Sudeten Mts." Biodiversity: Research and Conservation, no. 3-4 (December 30, 2006): 294–99. https://doi.org/10.14746/biorc.2006.3-4.21.

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This paper presents the assessments concerning the vertical distribution, exposure, slope inclination and land relief of silver-fir localities. The current distribution of fir trees suggest that in the past, Abies alba was widespread in the Sudety Mts. at the altitude range 350-800 m. At altitudes of up to 800 m, the number of localities in each zone is often proportional to the total forest area in the zone. Above 800 m, fir trees are now very rare. The studied species is in general similarly frequent in localities with various exposure and degree of slope. It prefers concave landforms (valle

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8

Johnston, J. D., J. A. Tait, G. J. H. Oliver, and F. C. Murphy. "Evidence for a Caledonian orogeny in Poland." Transactions of the Royal Society of Edinburgh: Earth Sciences 85, no. 2 (1994): 131–42. http://dx.doi.org/10.1017/s0263593300003539.

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AbstractThe Lower Palaeozoic tectonic history of central and eastern Europe is poorly understood because of extensive Variscan and/or Alpine reworking. The trace of the Tornquist Sea, the SE arm of the Lower Palaeozoic Iapetus Ocean, extended from NE Britain to Asia Minor. The site of this ocean is constrained by the tectonostratigraphy and faunal provinciality of Lower Palaeozoic inliers in northern Czechoslovakia, and southern Poland. In this paper, the collage of contrasting tectonostratigraphic histories of terranes in the Lower Palaeozoic of Poland is reviewed. Fossil evidence demonstrate

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9

Pielech, Remigiusz, Krzysztof Zając, and Marek Malicki. "Spread of Veronica filiformis (Scrophulariaceae) in the Sudetes." Biodiversity: Research and Conservation 28, no. 1 (2012): 25–28. http://dx.doi.org/10.2478/v10119-012-0025-2.

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Abstract Veronica filiformis is an alien plant species widely distributed, across Central and Western Europe. The first observation of the species in the Sudetes was reported in 1942. Until 2000, only a few scattered sites were known in south-western Poland. During the last decade, V.filiformis was observed more frequently in many ranges of the Sudetes. In 2007, field works intended to discover new sites of the species were conducted as well as a critical revision of herbarium specimens stored in WRSL was performed. The number of known localities totals 37. Almost 65% of them were discovered d

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10

CYMERMAN, Z., M. A. J. PIASECKI, and R. SESTON. "Terranes and terrane boundaries in the Sudetes, northeast Bohemian Massif." Geological Magazine 134, no. 5 (1997): 717–25. http://dx.doi.org/10.1017/s0016756897007255.

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In the Sudetes, seven distinct lithostratigraphic terranes exhibit a symmetric distribution. A central region of basinal/oceanic and ophiolitic rocks, the Central Sudetic terrane is bordered, respectively to the northwest and southeast, by the sialic Saxothuringian and Moldanubian terranes. These exhibit contrasting metasedimentary/metavolcanic successions and tectonic-metamorphic sequences, but both are characterized by Palaeozoic plutonism. These are in turn bordered (again respectively to the northwest and southeast) by the Lusatian and Moravian terranes, which are also sialic, but contain

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11

Lisowska, Ewa, and Krzysztof Jaworski. "8th-10th century hillforts in the Sudetes – exploring current state of research and observations, towards new horizons." Acta Archaeologica Carpathica 56 (December 2021): 335–86. http://dx.doi.org/10.4467/00015229aac.21.012.15353.

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The article presents the latest results of archaeological studies on the 8th-10th century hillforts in the Sudetes. The authors present previously unknown structures, found through the analysis of aerial scans using the ALS method. Excavation and office studies conducted since 2005 in the Sudetes also allowed for correcting the chronology of some previously known hillfort sites. The article also presents a discussion on the structures referred to as ‘quasi-hillforts’ and those considered to be destroyed. The findings are concluded by a summary of changes in the archaeological research of the e

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Lewandowska, Amelia, Krystyna Boratyńska, Katarzyna Marcysiak, et al. "Phenotypic differentiation of Rhododendron ferrugineum populations in European mountains." Dendrobiology 87 (February 17, 2022): 1–12. http://dx.doi.org/10.12657/denbio.087.001.

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Rhododendron ferrugineum occurs in the mountains of the Central Europe with large disjunction in geographic range between Pyrenees and Alps and between Alps and Sudetes. We expect that these discontinuities in the species occurrence should involved their phenotypic differentiation, similar as described on the studies of molecular markers. The aim of the study was verification of phenotypic differences between the species populations from the Pyrenees, Alps and Sudetes. We examined characters of leaves and capsules from 13 populations, each represented by 25–30 individuals, using ANOVA, discr

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13

Gierlasiński, Grzegorz, Tomasz Rutkowski, Dariusz Kojder, and Jarosław Regner. "Nowe dane o rozmieszczeniu pluskwiaków różnoskrzydłych (Hemiptera: Heteroptera) w Sudetach Zachodnich / New data on the distribution of true bugs (Hemiptera: Heteroptera) in Western Sudetes." Heteroptera Poloniae - Acta Faunistica 15 (May 6, 2021): 71–82. https://doi.org/10.5281/zenodo.4739637.

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A list of true-bug species collected in Western Sudetes with 26 species new to the fauna of this region is given. The occurrence in Poland of the rarest of them is discussed. The paper also presents the history of research in this zoogeographical region of Poland. An attempt was also made to estimate the number of true bug species inhabiting the Western Sudetes.

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14

Roland, Dobosz, and Malkiewicz Adam. "Potwierdzenie występowania wielbłądki Puncha ratzeburgi (Brauer, 1876) w Sudetach." Acta entomologica silesiana 28, online004 (2020): 1–4. https://doi.org/10.5281/zenodo.3726752.

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<strong>Confirmation of the occurrence of the snake-flies <em>Puncha ratzeburgi</em> (Brauer, 1876) in the Sudetes.</strong> <em>Puncha ratzeburgi</em> (Brauer, 1876) was again confirmed in the Sudetes, in Wojcieszów after 100 years. The old records, published in 1989, were again analyzed and the exact harvesting locations of two females from Duszniki Zdrój and Srebrna Góra, were identified.

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15

Don, Jerzy, and Andrzej Żelaźniewicz. "The Sudetes — boundaries, subdivision and tectonic position." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 179, no. 2-3 (1990): 121–27. http://dx.doi.org/10.1127/njgpa/179/1990/121.

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16

Golonka, Jan, Maria Barmuta, and Jan Barmuta. "Kaczawa Klippen Belt – geotouristic attraction in the Sudety Mountains, SW Poland." Acta Geoturistica 9, no. 1 (2018): 30–35. http://dx.doi.org/10.1515/agta-2018-0004.

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Abstract In the paper authors present some geological sites from Kaczawa Unit, Sudetes, Poland, and their interpretation in a geotectonic context. All described geosites are important for understanding the evolution of so called Kaczawa Accretionary Prism as well as whole Sudetes. Presented outcrops are easily accessible, well exposed and exhibits high education value. Special attention was given to the Wojcieszów Limestones and their relationship to the surrounding rocks

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17

Furmankiewicz, Marek, Jacek Potocki, and Jan Kazak. "Land-Use Conflicts in the Sudetes, Poland." IOP Conference Series: Materials Science and Engineering 471 (February 23, 2019): 092033. http://dx.doi.org/10.1088/1757-899x/471/9/092033.

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18

Matyszczak, Witold. "Liandratite from Karkonosze pegmatites, Sudetes, Southwestern Poland." Mineralogy and Petrology 112, no. 3 (2017): 357–70. http://dx.doi.org/10.1007/s00710-017-0537-8.

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19

Kowalski, Aleksander. "W jaki sposób struktura podłoża warunkuje rozwój osuwiska translacyjnego? Przykład osuwiska we Włodowicach w Obniżeniu Noworudzkim (Sudety Środkowe)." Przegląd Geologiczny 70, no. 9 (2020): 722–32. http://dx.doi.org/10.7306/2022.26.

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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 ind

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Przylibski, Tadeusz A. "Radon Research in Poland: A Review." Solid State Phenomena 238 (August 2015): 90–115. http://dx.doi.org/10.4028/www.scientific.net/ssp.238.90.

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The article presents the most important results of radon research in Poland. Large-scale research, launched in this country in the early 1950s, was originally linked to using radon dissolved in groundwater in balneotherapy as well as to uranium ore exploration and mining. This early research focused on the area of the Sudetes and nowadays it is also south-western Poland where most radon research is being conducted. This is chiefly due to the geological structure of the Sudetes and the Fore-Sudetic block, which is propitious to radon accumulation in many environments. Radon research in Poland h

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21

Konowalik, Agnieszka, Anna Najbar, Wiesław Babik, Sebastian Steinfartz, and Maria Ogielska. "Genetic structure of the fire salamander Salamandra salamandra in the Polish Sudetes." Amphibia-Reptilia 37, no. 4 (2016): 405–15. http://dx.doi.org/10.1163/15685381-00003071.

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We analysed genetic variation within and differentiation between nineteen populations of the fire salamander Salamandra salamandra inhabiting the north-eastern margin of the species range in the Sudetes Mountains (south-western Poland). The results were compared with those obtained recently for the Polish part of the Carpathians. Variation of 10 nuclear microsatellite loci was analysed in 744 individuals to estimate genetic structure, gene flow, isolation and to test for a geographic gradient of genetic variation. Mitochondrial DNA control region (D-loop) of 252 specimens from all localities w

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22

Wojciechowska, Irena. "Geology of the Kłodzko Metamorphic Unit (Sudetes, Poland)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 179, no. 2-3 (1990): 189–95. http://dx.doi.org/10.1127/njgpa/179/1990/189.

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23

Křížek, Marek, Václav Treml, and Zbyněk Engel. "Lithologic predisposition, morphology, and spatial distribution of patterned ground above alpine timberline in the High Sudetes." Geografie 112, no. 4 (2007): 373–87. http://dx.doi.org/10.37040/geografie2007112040373.

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It is evident that morphology and location of the patterned ground of the High Sudetes are significantly dependent on lithological conditions. Additional impact has also extreme location, respectively extend of its deflation. The occurrence of sorted polygons is dependent particularly on quartzite; earth hummocks prefer rocks offering fine-grained/small-grained waste. Sorted polygons reach the largest horizontal sizes among all kinds of patterned ground, earth hummocks have the smallest horizontal sizes. Many temporary forms among all kinds of patterned ground exist in the High Sudetes which i

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Migoń, Piotr. "Main features of geomorphology of the Sudetes re-assessed in the light of digital elevation model." Geografie 113, no. 4 (2008): 400–416. http://dx.doi.org/10.37040/geografie2008113040400.

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The Sudetes as a geomorphological region are distinguished by complicated spatial pattern of high- and low-altitude terrains and variable mean slope gradients across the range. Several conceptual models have been proposed to account for this variability, emphasizing the significance of planation surfaces, intramontane basins, climate-controlled landform generations, or differential uplift and subsidence. An analysis of a digital elevation model and maps derived from the model have allowed for re-assessment of some of those hypotheses and concepts. It confirms that differential tectonics explai

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Najbar, Anna, Agnieszka Konowalik, Konrad Halupka, Bartłomiej Najbar, and Maria Ogielska. "Body size and life history traits of the fire salamander Salamandra salamandra from Poland." Amphibia-Reptilia 41, no. 1 (2020): 63–74. http://dx.doi.org/10.1163/15685381-20191135.

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Abstract The fire salamander Salamandra salamandra is a widespread taxon in Europe, exhibiting great intraspecific diversity in phenotype and life history traits across its geographical distribution. Here, we studied body size, sexual dimorphism, age, growth rate and condition of fire salamanders from the north-eastern margin of its range. In total, 2,102 individuals from 23 populations representing the Polish parts of the Sudetes and the Carpathian Mountains were sampled between 2004 and 2016. Body traits and age showed significant differences between the western (the Sudetes) and eastern (th

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Pintor Pirzkall, Heike Clara. "Un viaje sin retorno para los Sudetes alemanes." Studia Politicae, no. 44 (November 30, 2018): 97–113. http://dx.doi.org/10.22529/sp.2018.44.05.

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27

Kotula, Piotr. "Stibnite vein from Dębowina near Bardo (polish Sudetes)." Contemporary Trends in Geoscience 2, no. 1 (2013): 28–33. http://dx.doi.org/10.2478/ctg-2014-0004.

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Abstract In the contact zone of the Bardo Structure and Kłodzko-Złoty Stok Intrusion and Kłodzko Metamorphic, metasomatic orebearing quartz-carbonate veins rich in Sb, Zn, Cu, Ag, Au, Pb are present. In 1771 the mine ,,Reiche Silber Gluck” within stibnite vein was founded in Dębowina near Bardo. Its entrance was discovered again in 2007. The stibnite vein is mainly build of stibnite and sphalerite and of quartz and dolomite rich in Mn. Stibnite crystallizes as columnar or forming radiate centres and aciculars. Its crystals reach size to 2 mm. Sphalerite appears as individual anhedral and polym

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Migała, Krzysztof, Józef Liebersbach, and Mieczysław Sobik. "Rime in the Giant Mts. (The Sudetes, Poland)." Atmospheric Research 64, no. 1-4 (2002): 63–73. http://dx.doi.org/10.1016/s0169-8095(02)00080-7.

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Białek, Dawid, Paweł Raczyński, Przemysław Sztajer, and Dominik Zawadzki. "Archaeocyaths from the Kaczawa complex, West Sudetes, Poland." Journal of Earth Science 21, S1 (2010): 18–20. http://dx.doi.org/10.1007/s12583-010-0159-0.

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Adam, Woźniak, and Byk Adam. "Ząbkonóg czarny Accanthopus velikensis (Piller et Mitterpacher, 1783) (Tenebrionidae: Tenebrioninae, Helopini) – "nowy" gatunek dla fauny Polski." Acta entomologica silesiana 27, online010 (2019): 1–5. https://doi.org/10.5281/zenodo.3249827.

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<strong><em>Accanthopus velikensis</em> (Piller et Mitterpacher, 1783) (Tenebrionidae: Tenebrioninae: Helopini) – “new” species for the fauna of Poland.</strong> <em>Accanthopus velikensis</em> (Piller et Mitterpacher, 1783) is recorded from Poland after over 160 years. One specimen of this species was bred from Hazel from the Eastern Sudetes in 2016.

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Szczęśniak, Ewa, Iwona Jędrzejczyk, Edyta M. Gola, Remigiusz Pielech, Kamila Reczyńska, and Krzysztof Świerkosz. "Polypodium Interjectum And P. × Mantoniae (Polypodiaceae) In The Polish Sudetes." Polish Botanical Journal 60, no. 2 (2015): 163–72. http://dx.doi.org/10.1515/pbj-2015-0021.

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AbstractDetailed analyses of micro- and macromorphological features of 247 specimens representing the Polypodium vulgare complex, combined with DNA content measurements, revealed the presence of tetraploid P. vulgare s.str., hexaploid P. interjectum and the pentaploid hybrid P. × mantoniae in the Polish Sudetes. For species identification, sporangium structure (number of indurated and basal annulus cells) was found to be the most stable and thus the most valuable and taxonomically significant character. The size of spores and stomata was related to taxon ploidy level, and helped to differentia

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Mitka, Józef, Piotr Boroń, Ada Wróblewska, and Wojciech Bąba. "AFLP analysis reveals infraspecific phylogenetic relationships and population genetic structure of two species of Aconitum in Central Europe." Acta Societatis Botanicorum Poloniae 84, no. 2 (2015): 267–76. http://dx.doi.org/10.5586/asbp.2015.012.

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The genetic diversity of two <em>Aconitum</em> species endemic to the Carpathian Mountains and Sudetes was studied. A reticulate evolution between them was earlier postulated as an effect of secondary contact. The genetic diversity at the individual and taxonomic levels was examined across the entire geographical ranges of the taxa in 11 populations based on 247 AFLP markers found in 112 individuals in the Sudetes and Western Carpathians. The overall genetic differentiation was greater within the Sudetic <em>A. plicatum</em> (<em>F</em><span><sub&gt

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Dżaluk, Agnieszka, Dariusz Malczewski, Jerzy Żaba, and Maria Dziurowicz. "In situ measurements of natural radioactivity in selected igneous rocks of the Opava Mountain region." Contemporary Trends in Geoscience 3, no. 1 (2014): 5–12. http://dx.doi.org/10.2478/ctg-2014-0017.

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Abstract In situ gamma-ray measurements of four igneous rocks were taken in the Opava Mountains (Eastern Sudetes, Poland). The activity of naturally occurring radionuclides was measured using a portable GX3020 gamma-ray spectrometry workstation. The activity concentrations of 40K varied from 914 ± 17 Bqkg-1 (gneiss, Kamienna Góra) to 2019 ± 37 Bqkg-1 (weathered granite, Sławniowice), while those of 232Th from 7.5 ± 0.6 Bqkg-1 (weathered granite, Sławniowice) to 68 ± 0.9 Bqkg-1 (migmatitic gneiss, Nadziejów). The activities associated with 238U decay series ranged from 10 ± 0.4 Bqkg-1 (weathere

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Kremer, Barbara. "Mat-forming coccoid cyanobacteria from early Silurian marine deposits of Sudetes, Poland." Acta Palaeontologica Polonica 51, no. 1 (2006): 143–54. https://doi.org/10.5281/zenodo.13643645.

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Paweł, Domagała, and Gradowska Paulina. "Metatropis rufescens (Herrich-Schäffer, 1835) (Heteroptera: Berytidae): drugie stanowisko w Sudetach Wschodnich, a zarazem pierwsze w Górach Opawskich." Acta entomologica silesiana 25, online038 (2017): 1. https://doi.org/10.5281/zenodo.1123219.

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Kwiatkowski, Paweł, and František Krahulec. "Disjunct Distribution Patterns in Vascular Flora of the Sudetes." Annales Botanici Fennici 53, no. 1-2 (2016): 91–102. http://dx.doi.org/10.5735/085.053.0217.

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ŻELAŹNIEWICZ, A. "The Sudetes as a Palaeozoic orogen in central Europe." Geological Magazine 134, no. 5 (1997): 691–702. http://dx.doi.org/10.1017/s0016756897007541.

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Two metasedimentary complexes are exposed in the Sudetes Mountains of Poland, Germany and the Czech Republic. Succession I comprises pelites and greywackes of Neoproterozoic–Cambrian age, deformed and metamorphosed prior to intrusion by S-type porphyritic granites at 515–480 Ma. Succession II comprises a sandstone–mudstone–chert sequence and turbidite sequence of Ordovician–early Carboniferous age accompanied by bimodal volcanogenic rocks. Both successions were intruded by late- to post-orogenic granitoid intrusions at 340–300 Ma. The sedimentary rocks of succession II show increasing maturity

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Migoń, Piotr, and Agnieszka Latocha. "Human interactions with the sandstone landscape of central Sudetes." Applied Geography 42 (August 2013): 206–16. http://dx.doi.org/10.1016/j.apgeog.2013.03.015.

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Latocha, Agnieszka. "The depopulated villages in the Sudetes. And what next?" Przegląd Geograficzny 85, no. 3 (2013): 373–96. http://dx.doi.org/10.7163/przg.2013.3.3.

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40

Majdański, Mariusz, Marek Grad, and Aleksander Guterch. "2-D seismic tomographic and ray tracing modelling of the crustal structure across the Sudetes Mountains basing on SUDETES 2003 experiment data." Tectonophysics 413, no. 3-4 (2006): 249–69. http://dx.doi.org/10.1016/j.tecto.2005.10.042.

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Szeląg, Zbigniew. "Hieracium umbellonigritum (Asteraceae), a new hybridogenous species from the Sudetes in Poland." Phytotaxa 589, no. 3 (2023): 289–92. https://doi.org/10.11646/phytotaxa.589.3.8.

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Szeląg, Zbigniew (2023): Hieracium umbellonigritum (Asteraceae), a new hybridogenous species from the Sudetes in Poland. Phytotaxa 589 (3): 289-292, DOI: 10.11646/phytotaxa.589.3.8, URL: http://dx.doi.org/10.11646/phytotaxa.589.3.8

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Szeląg, Zbigniew. "Hieracium purkynei (Asteraceae): an endemic to the Sudetes rediscovered after a century." Phytotaxa 601, no. 1 (2023): 90–96. https://doi.org/10.11646/phytotaxa.601.1.7.

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Szeląg, Zbigniew (2023): Hieracium purkynei (Asteraceae): an endemic to the Sudetes rediscovered after a century. Phytotaxa 601 (1): 90-96, DOI: 10.11646/phytotaxa.601.1.7, URL: http://dx.doi.org/10.11646/phytotaxa.601.1.7

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Danek, Małgorzata, Monika Chuchro, and Adam Walanus. "Tree-Ring Growth of Larch (Larix decidua Mill.) in the Polish Sudetes—The Influence of Altitude and Site-Related Factors on the Climate–Growth Relationship." Forests 9, no. 11 (2018): 663. http://dx.doi.org/10.3390/f9110663.

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In this paper, the first study of a regional character on the influence of climatic factors on the tree-ring growth of European larch (Larix decidua Mill.) growing in the Polish Sudetes is presented. The obtained results indicate the relatively high diversity of the climatic signal observed in the tree rings of larches growing in the Sudetes. The most significant differentiating factor is altitude. The results suggest that the possible influence of local conditions (e.g., summit proximity, soil and bedrock characteristics, and exposure to strong winds) could also be of importance. A positive r

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Botor, Dariusz, Aneta A. Anczkiewicz, Stanisław Mazur, and Tomasz Siwecki. "Post-Variscan thermal history of the Intra-Sudetic Basin (Sudetes, Bohemian Massif) based on apatite fission track analysis." International Journal of Earth Sciences 108, no. 8 (2019): 2561–76. http://dx.doi.org/10.1007/s00531-019-01777-9.

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Abstract The Intra-Sudetic Basin, a ~ 12 km deep Variscan intramontane basin, has the best preserved post-orogenic sedimentary record available at the NE margin of the Bohemian Massif. Apatite fission track (AFT) analyses have been performed on 16 sedimentary and volcanic samples of Carboniferous to Cretaceous age from the Intra-Sudetic Basin to improve understanding of the post-Variscan thermal evolution. AFT central ages range from 50.1 ± 8.8 to 89.1 ± 7.1 Ma (Early Eocene to Coniacian), with 13 of them being Late Cretaceous. The mean track length values range from 12.5 ± 0.4 to 13.8 ± 0.5 (

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Nadolna, Longina, and Marta Żyszkowska. "Characteristics of grasslands in the Polish Sudetes in view of fodder production potential and grassland protection." Journal of Water and Land Development 15, no. 1 (2011): 29–40. http://dx.doi.org/10.2478/v10025-012-0003-2.

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Characteristics of grasslands in the Polish Sudetes in view of fodder production potential and grassland protection Mountain region of the Sudetes has a productive potential that allows for obtaining high quality fodder from grasslands. The potential is facilitated by the fact that 94% of grassland area is situated below the elevation of 700 m a.s.l. and 75% of them on slopes inclined less 9°. Meadows and pastures of the highest economic importance cover an area larger than 50 000 ha, most of them situated in the Kłodzko district. The analysis of ruminant and horse stock in 2008 revealed that

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Andrzejczak, Maria, Adam Bogacz, Klara Tomaszewska, and Magda Podlaska. "Plant communities, properties, and age of organic soils in the post-extraction sites of the Trzcińskie Mokradła Peatland (Sudetes Mts., SW Poland)." Soil Science Annual 67, no. 2 (2016): 79–87. http://dx.doi.org/10.1515/ssa-2016-0011.

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Abstract The aim of the study was to show the impact of the peat extraction on the development and properties of organic soils and plant habitat in post-extraction sites. The study was conducted in the complex of the Trzcińskie Mokradła Peatlands (Sudetes Mts., SW Poland). The Trzcińskie Mokradła Peatlands began to form in Preboreal (10960–9330 ±50BP) so that they are one of the oldest peatlands in the Sudetes. We analyzed 8 soil profiles (42 samples). Peat forming process there is still active in the moderate or strong degree (PtII-PtIII). The floristic composition of the studied areas was ty

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ŁACH, Janusz, and Aneta MAREK. "THE ROLE OF OPEN-AIR CALVARIES IN THE CONTEXT OF LANDSCAPE HERITAGE PROTECTION OF THE EASTERN SUDETES." GeoJournal of Tourism and Geosites 53, no. 2 (2024): 489–501. http://dx.doi.org/10.30892/gtg.53212-1224.

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The article concerns the meaning and landscape functions of Small Calvaries located in the Eastern Sudetes in the border area of the Czech Republic and Poland. The publication aims to indicate the main typological features of this type of calvary, taking into account the current behaviour of residents having a common sarcastic heritage. Due to the subject, interdisciplinary research was undertaken in the direction of valorization as well as environmental interviews. The use of geosociological methodology made it possible to assess the landscape in terms of its contemporary functions and potent

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Pieczka, Adam, Bożena Gołębiowska, and Wοjciech Franus. "Yukonite, a rare Ca-Fe arsenate, from Rçdziny (Sudetes, Poland)." European Journal of Mineralogy 10, no. 6 (1998): 1367–70. http://dx.doi.org/10.1127/ejm/10/6/1367.

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Mierzejewski, Michal P., and Teresa Oberc-Dziedzic. "The Izera-Karkonosze Bkock and its tectonic development (Sudetes, Poland." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 179, no. 2-3 (1990): 197–222. http://dx.doi.org/10.1127/njgpa/179/1990/197.

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Szeląg, Zbigniew. "Hieracium lomniczkianum (Asteraceae), a new species in the H. wiesbaurianum aggregate from the Sudetes in Poland." Phytotaxa 594, no. 4 (2023): 251–55. https://doi.org/10.11646/phytotaxa.594.4.2.

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Szeląg, Zbigniew (2023): Hieracium lomniczkianum (Asteraceae), a new species in the H. wiesbaurianum aggregate from the Sudetes in Poland. Phytotaxa 594 (4): 251-255, DOI: 10.11646/phytotaxa.594.4.2, URL: http://dx.doi.org/10.11646/phytotaxa.594.4.2

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