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48 results for “Western Carpathians”
Figure 3 from: Rudy J, Rendoš M, Ľuptáčik P, Mock A (2018) Terrestrial isopods associated with shallow underground of forested scree slopes in the Western Carpathians (Slovakia). In: Hornung E, Taiti S, Szlavecz K (Eds) Isopods in a Changing World. Title. ZooKeys 801: 323-335. https://doi.org/10.3897/zookeys.801.24113
Figure 3 Depth distribution of Mesoniscusgraniger. Site 1 is out of the species range. Study sites 4 and 5 were not depicted, because whole depth gradient was not represented (see locality description).
Figure 2 from: Rudy J, Rendoš M, Ľuptáčik P, Mock A (2018) Terrestrial isopods associated with shallow underground of forested scree slopes in the Western Carpathians (Slovakia). In: Hornung E, Taiti S, Szlavecz K (Eds) Isopods in a Changing World. Title. ZooKeys 801: 323-335. https://doi.org/10.3897/zookeys.801.24113
Figure 2 Ethylene glycol to formaldehyde ratio of sampled specimens from all study sites, where both fixating solutions were used.
Figure 1 from: Rudy J, Rendoš M, Ľuptáčik P, Mock A (2018) Terrestrial isopods associated with shallow underground of forested scree slopes in the Western Carpathians (Slovakia). In: Hornung E, Taiti S, Szlavecz K (Eds) Isopods in a Changing World. Title. ZooKeys 801: 323-335. https://doi.org/10.3897/zookeys.801.24113
Figure 1 Location of the study sites. 1/ Borinka (Malé Karpaty Mts.), 2/ Belinské skaly (Cerová vrchovina Highlands), 3/ Drienok Valley, 4/ Slope next to the Malá drienčanská Cave, 5/ Collapse above the Veľká drienčanská Cave (three sites are in the Revúcka vrchovina Highlands), 6/ Vysoký vrch Hill, 7/ Doline next to Silická ľadnica Ice Cave (both sites in Slovak Karst), 8/ Malý Ružinok Valley (Čierna hora Mts.).
Figure 4 from: Rudy J, Rendoš M, Ľuptáčik P, Mock A (2018) Terrestrial isopods associated with shallow underground of forested scree slopes in the Western Carpathians (Slovakia). In: Hornung E, Taiti S, Szlavecz K (Eds) Isopods in a Changing World. Title. ZooKeys 801: 323-335. https://doi.org/10.3897/zookeys.801.24113
Figure 4 Comparison of warm and cold period sampling of Mesoniscusgraniger on study sites 2, 3, 6, 7.
Data used in the manuscript entitled: The Curious Case of Short Fault Scarp in the Podhale Basin (Western Carpathians): implications for Late Pleistocene geodynamics
<p><strong>Manuscript Abstract: </strong>Areas with low deformation rates, such as continental interiors or mature orogens like the Western Carpathians, may represent significant seismic hazard zones, albeit still insufficiently recognized. Relatively low-magnitude earthquakes occurring in such regions pose challenges for paleoseismology, despite occasional documented surface fault ruptures. However, all these ruptures fit the empirical displacement-length scaling relationships. This study focuses on a scarp located in the Podhale Basin (Central Western Carpathians) that deviates from these empirical laws. Despite its relatively short length of only 3 km, the scarp, measuring up to 8 m in height, presents several indications of its tectonic origin. Geophysical GPR and ERT surveys revealed a vertical discontinuity directly beneath the scarp. We identified distinct features interpreted as a fault zone in a trench across the scarp. Lacking material suitable for dating, we estimated the age of the fault scarp at 26.3 ± 14.5 ka using simple linear diffusion modeling. However, this result requires caution due to assumptions like scarp formation from a single event. Yet, the consistency of the estimated age with the superposition of the scarp relative to the morphology and weathered covers from the last glaciation is noteworthy. Furthermore, morphological and geological mapping suggests the dextral oblique kinematics of the studied fault. The prevailing trend of NE (NNE) compression across the Podhale and Orava basins and the Tatra Mountains aligns the dextral Brzegi fault with the broader Alpine-Carpathian geodynamic framework. The Brzegi fault, as part of the broader Białka fault zone, provides evidence of far-field effects, serving as an NNW-striking dextral antithetic fault to major sinistral NE-SW striking faults. The recognized pattern indicates the continued post-Miocene Alpine extrusion toward the Carpathians. </p> <p><strong>In this dataset, we make available:</strong></p> <p>iPhone13Pro LiDAR scan of the trench (texture_output)</p> <p>high-resolution orthophotomosaic (Brzegi_trench.tif)</p> <p>PDF file with methods and results of simple linear scarp diffusion modeling</p> <p>PDF file with methods and all geophysical profiles surveyed with electrical resistivity tomography (ERT), induced polarization tomography (IP), and ground-penetrating radar (GPR) </p> <p> </p>
Fig. 1 in Species Composition And Biotopical Distribution Of Blackflies (Diptera, Simuliidae) On The South-Western Macroslope Of The Ukrainian Carpathians
Fig. 1. Correlation of Simuliidae species developing in streams on the south-western macroslope of the Ukrainian Carpathians.
FIGURE 1 in Two new species in Hieracium sect. Alpestria (Asteraceae) from Mt. Babia Góra, Western Carpathians, Poland
FIGURE 1. Distribution of Hieracium babiogorense (yellow dots) and H. besseri (red dots) on Mt. Babia Góra.
FIGURE 4 in Two new species in Hieracium sect. Alpestria (Asteraceae) from Mt. Babia Góra, Western Carpathians, Poland
FIGURE 4. Involucres of: A. Hieracium babiogorense; B. H. besseri (from holotypes).
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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