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Journal articles on the topic 'Frýdek'

Author: Grafiati

Published: 28 June 2021

Last updated: 16 February 2022

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1

Štraub, Daniel. "The Effects of Fare-Free Public Transport: A Lesson from Frýdek-Místek (Czechia)." Sustainability 12, no. 21 (November 2, 2020): 9111. http://dx.doi.org/10.3390/su12219111.

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The fare-free public transport policy (FFPT), the characteristic feature of which is abolishing fares in public transport, influences the transport system in favour of one means of transport. By joining the academic disputes over the outcomes of the FFPT policy, the aim of this paper is to understand the effects of the FFPT on overall mobility strategies and on the dynamics of the transport system where the policy is implemented. To do so, the paper is analysing a concrete example of the FFPT practice in Frýdek-Místek (Czechia) by conducting surveys with the residents and interviews with the city planning authorities. The results show that the FFPT influences mobility strategies and dynamics in the given transport system, which imprints in an increased use of public transport. However, the FFPT does not represent a universal tool of urban and transport planning and its implementation into practice should take place in synergy with other transport (dis)incentives.

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2

Bubík, Miroslav, Juraj Franců, Helena Gilíková, Jiří Otava, and Lilian Švábenická. "Upper Cretaceous to Lower Miocene of the Subsilesian Unit (Western Carpathians, Czech Republic): stratotypes of formations revised." Geologica Carpathica 67, no. 3 (June 1, 2016): 239–59. http://dx.doi.org/10.1515/geoca-2016-0016.

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Abstract Type sections/areas for all four formations distinguished in the sedimentary succession of the Subsilesian Unit on Czech territory were revisited and described. New data on lithology, sedimentology, fossil record, biostratigraphy, heavy-minerals and geochemical proxies are based on observations and analysis of these sections. The historical type section of the Frýdek Formation was destroyed during railway construction in 19th century. Outcrops of Campanian to Maastrichtian marls and sandstones on the southwestern slope of “Castle hill” at Frýdek, are proposed as a new type section. The Ostravice riverbed in Frýdlant nad Ostravicí was originally designated as the type area, not mentioning the particular section. This area, even when supplemented with Sibudov Creek, does not show all typical facies of the formation. The outcrops range from lowermost Eocene to Eocene-Oligocene transition. In the original description of the Menilite Formation Glocker mentioned several localities in the area covering the Ždanice, Subsilesian and Silesian units, not mentioning the principal one. The single sections, each not exceeding a thickness of 2 m, are not sufficient to be a type section. Instead of that, we propose the area between Paršovice and Bystřice pod Hostýnem, covering the historical localities, as the type area. The type locality of the Ženklava Formation is an outcrop in an unnamed creek in Ženklava according to the original definition. It seems to be reasonable to extend the type section to the whole 500 m long section of the creek with the outcrops that better illustrate the lithological variability of the formation. New biostratigraphic data allow assignment to late Egerian (Eggenburgian?).

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3

Havrlant, Jan. "Mining and its lasting effects in the undermined Karviná part of the Ostrava basin." Geografie 102, no. 4 (1997): 279–87. http://dx.doi.org/10.37040/geografie1997102040279.

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The Czech mining industry has undergone a deep transformation and a damping down. In the year 1996, quality black coal is only mined in the Karviná part of the Ostrava basin and in one colliery in the Frýdek-Místek part of the basin. The used caving technology of underground extraction, however, caused a number of ecological and economic problems in the Karviná region. The question of the future of coal mining and the consequent negative effects on the local countryside are connected with numerous factors. A more extensive application of new laws concerning the protection of environment, the prices of imported coal, and other factors come to the fore in the economy of coal mining.

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4

Hudeček, Jiří J. "Probable historical record of the Slender-billed Curlew (Numenius tenuirostris) in the Czech Republic on the Moravian-Silesian territory." Acta Musei Silesiae, Scientiae Naturales 66, no. 3 (December 20, 2017): 281–87. http://dx.doi.org/10.1515/cszma-2017-0031.

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Abstract The Slender-billed Curlew (Numenius tenuirostris) is a worldwide endangered bird species on the brink of extintion. For the last time it nested in Siberia, Russia. It flew trought Europe regulary in the 19th century. Because its records are unrepeatable, each date has a high scientific value. This article describes the historical record probably of the Czech Republic, probably in north-eastern Moravia in the environment of Místek in Lachia, probably between the years 1884 and 1897. This record might come from the collection of J. Bednař from the school in Místek (now Frýdek-Místek). These indirect data are provable and it is not possible to agree with the conclusion of the Czech Faunistic Committee which considers the location and date as unknown.

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5

Marschalko, M., L. Hofrichterová, and H. Lahuta. "Engineering-geological conditions of the effect of a landslide from mining activity." Slovak Journal of Civil Engineering 18, no. 4 (December 1, 2010): 8–16. http://dx.doi.org/10.2478/v10189-010-0017-1.

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Engineering-geological conditions of the effect of a landslide from mining activityThe paper deals with a slope deformation in Řepiště (Paskov), which is located between the towns of Ostrava and Frýdek Místek; Řepiště is situated in the Ostrava-Karviná District within the reach of the effects of mining activity. The deformation involves the Paskov Mine, which is the only active mine in the Ostrava section of the district. The study included mapping complemented with a geophysical survey using resistance tomography; along with the information obtained from the inspection, it provided an overview of the engineering-geological conditions of the slope deformation. The interpretation of the data obtained identified a very complicated structure, including several levels of slip surfaces. The landslide is thus a textbook example of slope movements with a very complicated geological structure occupying an extensive spatial area in the mining landscape and affecting the stability of a road running directly through its body.

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6

Lampartová, Ivana, Kateřina Blažková, and Kristina Somerlíková. "Public Awareness of the Relation between Nature-friendly Watercourse Modifications and Recreation in Cities." Acta Universitatis Agriculturae et Silviculturae Mendelianae Brunensis 64, no. 4 (2016): 1337–44. http://dx.doi.org/10.11118/actaun201664041337.

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The aim of the article is to present the results of a method of public preferences – a questionnaire survey finding an awareness of the relation between the modifications of watercourses and recreation in urban environment. The aquatic ecosystem and the water itself in a landscape are regarded by citizens as a mere source of energy, food, and water used for industry or as a means of transport. However, water elements along with the flora and fauna belonging to this living ecosystem provide a plethora of opportunities for a development of e.g. recreation, tourism, even an entire region. The questionnaire method used has been applied in selected cities in the Czech Republic, e.g. in Frýdek‑Místek, Olomouc, Vlašim, Benátky nad Jizerou and others. The criterion for selecting the cities has mostly been the construction of nature-friendly modifications to watercourse while seeking to increase the recreational potential of the area. The outcome of this article is to present the original results of the public survey which have subsequently served for a further processing of drafts and measures for recreational potential in the selected locations. The most important finding of this research was the minimum level of selected site citizens’ awareness of revitalization and flood modifications, projects that were realized on watercourses in the cities.

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7

Sládeček, V. "Technical Hydrobiology–Biology of Purification Processes. (in Czech.) Collected Papers from a Seminar, September 17–18, 1987 in Frýdek-Místek. Czech Scientific-Technical Society, 1987, p. 245, not on market." Acta Hydrochimica et Hydrobiologica 17, no. 1 (1989): 86. http://dx.doi.org/10.1002/aheh.19890170112.

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8

Tymonová, Markéta. "Kachlové soubory z Frýdku." Archaeologia historica, no. 2 (2016): 415–35. http://dx.doi.org/10.5817/ah2016-2-21.

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9

Rohr, David M., Jiří Frýda, and Robert B. Blodgett. "Alaskodiscus, a new name for the Ordovician bellerophontoidean gastropod Alaskadiscus Rohr, Frýda and Blodgett, 2003." Journal of Paleontology 87, no. 1 (January 2013): 176. http://dx.doi.org/10.1666/12-082.1.

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The Late Ordovician tropidodiscid gastropod Alaskadiscus, known only in two areas in Alaska, was named by Rohr, Frýda, and Blodgett (2003). Peter Wagner and Stephen K. Donovan have pointed out to us that the name was previously used for a Cambrian trilobite, Alaskadiscus Zhang, 1980. We propose the new name Alaskodiscus with the same type species, A. donensis Rohr, Frýda and Blodgett, 2003. We feel the similarity in names is not likely to cause undue confusion since the taxa are widely separated by phyla and age.

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10

Matýsek, Dalibor, Jakub Jirásek, Aneta Minaříková, and Petr Skupien. "Ranciéit a doprovodné minerály z Rychaltic u Frýdku-Místku (Morava, Česká republika)." Bulletin Mineralogie Petrologie 29, no. 1 (2021): 41–48. http://dx.doi.org/10.46861/bmp.29.041.

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Recently described small outcrop of the upper part of the Barnasiówka Formation yielded several manganese oxidic minerals. Outcrop at the bank of the Krnalovice Stream (GPS N 49°38.623’ E 018°14.630’) consists of Lower Turonian greenish to grey-black laminated claystone alternating with grey chert. The whole sequence is a part of the Baška facies of the Silesian Unit, Outer Western Carpathians. In the middle part of the profile occur concretional aggregates containing manganese minerals. The central pale part of these aggregates is composed of quartz (ca. 90 wt.%), albite (ca. 9 wt.%), and muscovite, the darker rim of quartz (ca. 80 wt.%), goethite (ca. 10 wt.%), illite, todorokite, plagioclase, K-feldspar, and pyrite. Occasionally, remains of Mn-rich siderite were preserved in the cores. We suppose that they are in fact weathering products of carbonate-rich silicites. Manganese oxides also enter fissures in form of thin black coatings. Powder X-ray diffraction proved the presence of todorokite, ranciéite, pyrolusite, and possible vernadite. Todorokite forms black coatings with submetallic lustre, often associating with ranciéite. Ranciéite is dark pink to pinkish-brown, with a metallic lustre. Back-scattered electron images reveal its extremely thin tabular, sometimes undulated crystals and hexagonally oriented intergrowths. Powder diffraction data are strongly affected by preferred orientation, with dominating basal reflections of 001 plane at 7.4849 Å and plane 002 at 3.7424 Å. Its average formula from nine WDS spots (Ca0.14Mg0.01Ba0.01K0.01)Σ0.17(Mn4+0.86Si0.02Al0.03Fe0.01)Σ0.92O2.00·0.88H2O (based on 2 anions, water calculated from the ratio of cation sum / H2O in the formula according to Post et al. 2008) and CaO/MnO2 ratio 9 to 12 correspond well to the published data for this phase. Ranciéite is a rather common phyllomanganate from various geological environments, but this locality represents its first unambiguous occurrence in the Czech Republic. It closely resembles the one from Polish flysch Carpathians from Nowa Wieś near Rzesów.

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11

Blodgett, Robert B., Jiří Frýda, and Patrick R. Racheboeuf. "Murchisonia gourvenneci, new name for Muchisonia oehlerti BLODGETT, FRÝDA and RACHEBOEUF, 1999." Geobios 36, no. 5 (September 2003): 503. http://dx.doi.org/10.1016/s0016-6995(03)00059-7.

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12

Dudała, Halina. "[Recenzja]: David Pindur, Svӗtla a stíny barokní církve ve Slezsku. Frýdecké arciknӗžství v letech 1654-1770. Struktury, procesy, lidé, Muzeum Tӗšínska, Český Tӗšín 2015, ss. 407, indeks osobowy, geografi czny i rzeczowy." Archiwa, Biblioteki i Muzea Kościelne 105 (June 1, 2016): 389–92. http://dx.doi.org/10.31743/abmk.12076.

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13

FRÝDA, JIŘÍ, ROBERT B. BLODGETT, ALFRED C. LENZ, and BARBORA FRÝDOVÁ. "Jardamarekia enigma, a new Early Devonian tryblidioidean from Royal Creek area (Yukon Territory, Canada), and paleobiogeography of the Early Devonian of northwestern Canada." Zootaxa 2905, no. 1 (June 3, 2011): 57. http://dx.doi.org/10.11646/zootaxa.2905.1.4.

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The Tryblidia (= Monoplacophora) represents the conchiferan class with the fewest Recent taxa in the phylum Mollusca (Haszprunar 2008) and its phylogeny is still poorly known. This group is known already in Cambrian strata (Early Paleozoic) more than 500 Ma ago. Present-day tryblidian species are known mainly from hadal environments (Schwabe 2008, but see also Wilson et al. 2009) in contrast to Paleozoic species, which have been described only from shallow environments of continental shelves of many paleocontinents (e.g., Horný 1962). A typical feature of fossil as well as living tryblidian species is their rarity. The vast majority of species are known only from several specimens (Haszprunar 2008). Furthermore, description of Paleozoic tryblidian molluscs is strongly underrepresented in the literature, despite the existence of diverse material. This is also true for fossils described in the present study based on a diverse silicified molluscan fauna of mostly gastropods collected from Lower Devonian strata of the Royal Creek area, Yukon Territory (Fig. 1) by Alfred C. Lenz and David G. Perry from 1970–1980. Lists of all hitherto described molluscan species as well as detailed information on their age and locality can be found in Lenz (1977a), Blodgett et al. (2001, 2010) and Frýda et al. (2008). Prior to our studies of the Royal Creek tryblidian and gastropod fauna, no descriptions or illustrations were available for Lower Devonian molluscs of north-western Canada, although a short discussion and faunal lists were provided by Blodgett et al. (1988) for Lower Devonian tryblidians and gastropods from the relatively nearby Delorme Formation of Northwest Territories, and early Emsian (late Early Devonian) tryblidians and gastropods from the Mt. Lloyd George area, northeastern British Columbia. The poor knowledge of Paleozoic tryblidians and gastropods faunas of Laurentia (North America) caused difficulties in the evaluation of Early Devonian paleobiogeography (Blodgett et al. 1999). The present paper is focused on the taxonomy of a new Devonian tryblidian limpet, but it provides also useful data for paleobiogeography and biostratigraphy of the Lower Devonian of western Canada.

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14

Matýsek, Dalibor, and Miroslav Bubík. "FOSFÁT A PELOKARBONÁT Z PELITŮ PODSLEZSKÉ JEDNOTKY NA STAVBĚ SILNICE R48 U FRÝDKU-MÍSTKU, ČESKÁ REPUBLIKA." Geologické výzkumy na Moravě a ve Slezsku 19, no. 1-2 (November 15, 2012). http://dx.doi.org/10.5817/gvms2012-1-2-088.

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Two samples of concretions from Maastrichtian and Paleocene grey clays/claystones of the Subsilesian Unit near Frýdek-Místek two samples of concretions were studied. The sample from the Paleocene/Eocene clays of the Frýdek Formation is phosphate nodule composed of highly prevailing amount of fluorapatite, low content of quartz and small amount of chlorite, muscovite and accessories. The phosphate nodules may be in fact coprolites. The sample from the Maastrichtian Frýdek Formation is sedimentary siderite (pelosiderite) with trace content of calcite.

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15

"Mauerwerk für Sport und Kultur." Bauingenieur 94, no. 05 (2019): A 8. http://dx.doi.org/10.37544/0005-6650-2019-05-8.

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Dass sich mit Mauersteinen aus Blähton außergewöhnliche Sport- und Kulturstätten errichten lassen, zeigt die Multifunktionshalle im tschechischen Frýdek-Místek. Hier tragen die Plansteine zur Ästhetik in der Halle bei.

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16

"Erratum." Fossil Imprint 76, no. 1 (2020): 209. http://dx.doi.org/10.37520/fi.2020.014.

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To the arcticle: Tonarová, P., Vodrážková, S., Hints, O., Männik, P., Kubajko, M., Frýda, J. (2019): Llandovery microfossils and microfacies of the Hýskov section, Prague Basin. – Fossil Imprint, 75(1): 25–43. https://doi.org/10.2478/if-2019-0002

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