Bulletin (Pdf)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Translated by Stan Hanna
AUSTRIA-HUNGARY’S LAST WAR, 1914-1918 (ÖSTERREICH-UNGARNS LETZTER KRIEG, 1914-1918) EDITED BY THE AUSTRIAN FEDERAL MINISTRY OF THE ARMY AND WAR ARCHIVE Under the Direction of Edmund Glaise-Horstenau Edited by Josef Brauner, Eduard Czegka, Jaromir Diakow, Friedrich Franek, Rudolf Kiszling, Eduard Steinitz, and Ernst Wisshaupt Translated by Stan Hanna Vol 2 (1915) FROM THE BATTLE OF LIMANOWA-LAPANOW FINALE TO THE TAKE OF BREST-LITOWSK With 40 leaflets and 36 sketches 1931 Publisher of Military Science Releases Vienna © 2005 Stan Hanna. All Rights Reserved. Austria-Hungary’s Last War, 1914-1918 Vol 2 TABLE OF CONTENTS TO THE SECOND VOLUME (1915) I. The Situation at the End of 1914 and Start of 1915.............1 A. Summary of the Situation on the Various Fronts..........................1 B. Condition of Austria-Hungary's Land Forces..............................6 1. The soldiers and their equipment......................................6 2. The military leadership..............................................22 3. Morale...............................................................29 4. The national make-up of the Army.....................................32 II. THE CARPATHIAN WINTER, 1914-1915.............................53 A. The Pursuit of the Russians after Limanowa-Lapanow.....................53 1. The pursuit on 13 December is unsatisfactory; decisions of theleaders on both sides...........................................................53 2. Operations of 3rd and 4th Aus-Hung. Armies through 17 December.......56 3. The Russian retreat north of the Vistula (15-18 December)............63 B. The Last Actions of 1914...............................................67 1. Events south of the Vistula..........................................67 a. The Russians build a new front; Austro-Hungarian measures on 17 December..............................................................67 b. Actions at Tarnow and the Dunajec (18-20 December).................69 c. 3rd Army's offensive falters (18-20 December)......................72 d. -
Zbiorniki Czorsztyński I Sromowiecki – Położenie, Charakterystyka, Nazwy
Pieniny – Zapora – Zmiany — Monografi e Pienińskie 2: 9–22, 2010 Zbiorniki Czorsztyński i Sromowiecki – położenie, charakterystyka, nazwy The Czorsztyn and Sromowce Reservoirs – location, characteristics and nomenclature ANDRZEJ JAGUŚ1, MARIUSZ RZĘTAŁA2 1 Akademia Techniczno-Humanistyczna, Wydział Nauk o Materiałach i Środowisku, ul. Willowa 2, 43-309 Bielsko-Biała, e-mail: [email protected] 2 Uniwersytet Śląski, Wydział Nauk o Ziemi, ul. Będzińska 60, 41-200 Sosnowiec, e-mail: [email protected] Abstract. This article presents the reservoirs behind the dams constructed on the Dunajec River in the Pieniny Region. The geographical location of the reservoirs as well as their basic morphometric parameters and functions they fulfi l are described. Nomenclature is also discussed and there appears to be signifi cant variation in reservoirs names. A proposal concerning nomenclature is formulated and justifi ed on terminological and linguistic grounds. Key words: geographical names, morphometrics parameters, reservoirs, Pieniny Region WPROWADZENIE tzw. nazw własnych (Grzenia 2002). Nazwy własne odgrywają bardzo ważne znaczenie w codziennej W latach 90. XX wieku, w środowisku geogra- komunikacji, pozwalając wyróżnić określone fi cznym pogranicza Pienin i Gorców, powstały osoby bądź podobne do siebie obiekty w prze- dwa sąsiadujące z sobą zbiorniki zaporowe strzeni geografi cznej. Precyzyjnie i poprawnie (główny i wyrównawczy). Retencjonują one wody sformułowana nazwa własna pozwala nie tylko rzeki Dunajec, spiętrzone zaporami wzniesionymi na jednoznaczną identyfi kację, ale posiada rów- w rejonie miejscowości Niedzica i Sromowce nież bardzo bogatą treść znaczeniową, generującą Wyżne. Budowa zbiorników oraz ich kilkuna- możliwość dokonania szczegółowej charaktery- stoletnie funkcjonowanie przyniosły z sobą wie- styki. W języku potocznym obiekty fi zycznogeo- lokierunkowe przeobrażenia krajobrazu doliny grafi czne (np. -
XVIII INTERNATIONAL MYELOMA WORKSHOP KRAKÓW 2021, POLAND (Proposed Term 14 – 19.09.2021)
APPLICATION FOR ORGANIZATION OF: XVIII INTERNATIONAL MYELOMA WORKSHOP KRAKÓW 2021, POLAND (proposed term 14 – 19.09.2021) Local Congress Organizers MD PhD, Prof. Aleksander B. Skotnicki Head of the Chair and Departament of Hematology Jagiellonian University Collegium Medicum MD PhD, Assoc. Prof . Artur Jurczyszyn Ms. Agnieszka Grzesiak President of the Myeloma Treatment Fundation Centre JORDAN Congress Bureau Chairman of the Krakow Branch Polish Society of Haematology and Blood Transfusion Address: 22/2 Sobieskiego St, 31-136 Krakow Jagiellonian University Medical College Department of Hematology (PCO Professional Congress Organiser) Address: 17, Kopernika St, 31-501 Krakow Address: 22/2 Sobieskiego St, 31-136 Krakow T: + 48 601 53 90 77 T: + 48 341 46 40 , e-mail: [email protected] e-mail: [email protected], http://szpiczak.org/en/ http://kongres.jordan.pl/en International Myeloma Workshop 2021 1 Table of Contents: Kraków 2021 ? Yes, of course ! …………………………..pages 3-4 Traveling to Cracow…………………………..………………..page 5 Scientific Committee and Partners………………………pages 6-7 Congress Venue ICE …………………………………………….page 8 Hotels in Krakow …………………………………………………pages 9-10 Opening and Closing Ceremony…………………………..page 11 Exhibition Space ………………………………………………… pages 12-13 Welcome Reception…………………………………………… page 14 Gala Dinner……………………………………………………….. .pages 15-17 Social Programme……………………………………………….pages 18-22 General Information about Poland…………………….pages 23-25 International Myeloma Workshop 2021 2 Kraków 2021 ? Yes, of course ! KRAKÓW is the second largest and one of the oldest cities in Poland situated on the Vistula river in the south of Poland. For many years Krakow was the royal capital of Poland until 17 th c. Krakow - an architectural pearl amongst Polish cities on the UNESCO World Cultural Heritage list with its architectural complex of the Old City which has survived unchanged since the Middle Age It is still the city where, like ages ago, one can walk along the Royal Route , starting from the city gates and arriving at the Royal Castle Hill . -
E X C U R S I O N I a (19. IX. 1963) the Excursion Was Devoted to The
GUIDE TO THE GEOLOGICAL EXCURSIONS OF THE XXXVI ANNUAL MEETING OF THE GEOLOGICAL SOCIETY OF POLAND, PIEN17NY MOUNTAINS, 1963 by Krzysztof Birkenmajer, Kazimierz Bogacz, Stefan Kozłowski and Stanisław Węcławik Excursion I A (19. IX. 1963) The excursion was devoted to the hydrogeological, geochemical and balneotechnical (as well as balneotherapeutical) problems of mineral waters of Szczawnica. Excursion IB (19. IX. 1963) During the excursion were shown outcrops of andesite dykes of Mt. Bryjarka at Szczawnica, as well as Quaternary terraces of the Grajcarek stream valley. Excursion IC (19. IX. 1963) The members of the excursion visited a clay pit at Krościenko, which exposes Pliocene clays and’ gravels with abundant and well preserved plant remains (references: Szafer 1946-7, 1950, 1954; K l i m a s ze w- s k i 1948; Birkenma j e r 1954a, 1958a). Excursions II A (20. IX) and III A (21. IX. 1963) The programme of the excursions included outcrops of the Podhale — 413 — Palaeogene (flysch) near the southern contact of the Pieniny Klippen Belt at Szaflary, stratigraphy and tectonics of the Pieniny-, Branisko-, and Czorsztyn Series, as well as the problem of the relation of the Upper Senonian Mantle (Jarmuta Beds) to the Klippen Series between the villa ge Szaflary and the Szaflary quarry. Later on, at Krempachy, has been demonstrated a section of the Pieniny Klippen Belt including strongly disturbed tectonically klippes of the Czorsztyn Series, as well as Dogger-, Middle and Upper Cretaceous members of the northern zone of the Klippen Belt, referred now to the Magura Series. Similar problems were also discussed at Dursztyn, where -the excursion had finished. -
Neotectonics of the Polish Carpathians in the Light of Geomorphic Studies: a State of the Art
Acta Geodyn. Geomater., Vol. 6, No. 3 (155), 291-308, 2009 NEOTECTONICS OF THE POLISH CARPATHIANS IN THE LIGHT OF GEOMORPHIC STUDIES: A STATE OF THE ART Witold ZUCHIEWICZ Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, A. Mickiewicza 30, 30-059 Kraków, Poland *Corresponding author‘s e-mail: [email protected] (Received January 2009, accepted March 2009) ABSTRACT Neotectonics of the Carpathians used to be studied extensively, particular attention being paid to the effects of large-scale domal uplifts and open folding above marginal zones of thrusts and imbricated map-scale folds, and rarely to the characteristics of young faulting. Neotectonic faults tend to be associated with the margins of the Orava-Nowy Targ Basin, superposed on the boundary between the Inner and Outer Western Carpathians, as well as with some regions within the Outer Carpathians. The size of Quaternary tilting of the Tatra Mts. on the sub-Tatric fault were estimated at 100 to 300 m, and recent vertical crustal movements of this area detected by repeated precise levelling are in the range of 0.4-1.0 mm/yr in rate. Minor vertical block movements of oscillatory character (0.5-1 mm/yr) were detected along faults cutting the Pieniny Klippen Belt owing to repeated geodetic measurements performed on the Pieniny geodynamic test area. In the western part of the Western Outer Carpathians, middle and late Pleistocene reactivation of early Neogene thrust surfaces was suggested. Differentiated mobility of reactivated as normal Miocene faults (oriented (N-S to NNW-SSE and NNE-SSW) in the medial portion of the Dunajec River drainage basin appears to be indicated by the results of long-profile analyses of deformed straths, usually of early and middle Pleistocene age. -
Estimation of Parametric Flood Hydrograph Determined by Means of Strupczewski Method in the Vistula and Odra Catchments
DOI: 10.1515/jwld-2016-0035 © Polish Academy of Sciences, Committee for Land Reclamation JOURNAL OF WATER AND LAND DEVELOPMENT and Environmental Engineering in Agriculture, 2016 2016, No. 31 (X–XII): 43–51 © Institute of Technology and Life Sciences, 2016 PL ISSN 1429–7426 Available (PDF): http://www.itp.edu.pl/wydawnictwo/journal; http://www.degruyter.com/view/j/jwld Received 05.08.2015 Reviewed 04.12.2015 Accepted 05.01.2016 Estimation of parametric flood hydrograph A – study design B – data collection determined by means of Strupczewski C – statistical analysis D – data interpretation E – manuscript preparation method in the Vistula and Odra catchments F – literature search Wiesław GĄDEK1) ABCDEF, Tamara TOKARCZYK2) ABCDEF, Arkadiusz ŚRODULA3) BCD 1) Cracow University of Technology, Institute of Water Engineering and Water Management, ul. Warszawska 24, 31-155 Kraków, Poland; tel. +48 12-628-28-54; e-mail: [email protected] 2) Institute of Meteorology and Water Management – National Research Institute, Flood and Drought Modeling Centre, Wrocław, Poland; e-mail: [email protected] 3) Arcadis Ltd., Kraków, Poland; e-mail: [email protected] For citation: Gądek W., Tokarczyk T., Środula A. 2016. Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments. Journal of Water and Land Development. No. 31 p. 43–51. DOI: 10.1515/jwld-2016-0035. Abstract While determining theoretical flood hydrographs, different methods of their construction are used depend- ing on the needs of the problem or the scope of the project. It should be remembered that these methods differ mainly with the principle of the waveform averaging, which may be done either according to the flow or time. -
Sytuacja Hydrologiczna 21.01.2021
INFORMACJA O SYTUACJI HYDROLOGICZNO–METEOROLOGICZNEJ W POLSCE z dnia 21 stycznia 2021 r. 1. Ostrzeżenia hydrologiczne W dniu 21 stycznia 2021 r. (na godz. 11:00) nie obowiązują ostrzeżenia hydrologiczne1. 2. Ostrzeżenia meteorologiczne W dniu 21 stycznia 2021 r. (na godz. 11:00) obowiązują ostrzeżenia meteorologiczne1 1 stopnia dotyczące silnego wiatru: - województwo podkarpackie (pow. bieszczadzki, brzozowski, jasielski, krośnieński, przemyski, sanocki, strzyżowski, leski, Krosno, Przemyśl) – od godz. 20:00 dnia 20.01.2021 do godz. 18.00 dnia 22.01.2021; Przewiduje się wystąpienie silnego wiatru o średniej prędkości od 35 km/h do 50 km/h, w porywach do 80 km/h, przejściowo w ciągu dnia 21.01. w porywach do 90 km/h, z południa. - województwo małopolskie (pow. gorlicki, nowosądecki, nowotarski, suski, tatrzański, Nowy Sącz), województwo śląskie (pow. bielski, cieszyński, gliwicki, pszczyński, raciborski, rybnicki, wodzisławski, żywiecki, Bielsko-Biała, Jastrzębie-Zdrój, Rybnik, Żory) – od godz. 12:00 dnia 21.01.2021 do godz. 18.00 dnia 22.01.2021; Przewiduje się wystąpienie silnego wiatru o średniej prędkości od 35 km/h do 45 km/h, w porywach do 80 km/h, z kierunków południowych. 1 Źródłem prezentowanych danych są informacje zbierane i przetwarzane przez państwową służbę hydrologiczno–meteorologiczną, którymi rozporządza „IMGW– PIB”. 3. Przekroczenia stanów alarmowych i ostrzegawczych. W dniu 21 stycznia 2021 (na godz. 11:00) zanotowano przekroczenie stanu ostrzegawczego: na 2 stacjach wodowskazowych na obszarze dorzecza Wisły, na 3 stacjach wodowskazowych na obszarze dorzecza Odry. Stan Stan wody Zmiana Stan ostrz. Nazwa stacji Rzeka Województwo alarm. [cm] stanu/24h [cm] [cm] [cm] KORZEŃSKO Orla dolnośląskie 225 14 220 260 ZAGRODNO Skora dolnośląskie 122 25 120 150 DOROHUSK Bug lubelskie 306 5 290 430 SULEJÓW (KOPALNIA) Pilica łódzkie 238 8 230 260 DĘBE Swędrnia wielkopolskie 209 1 200 250 Nie zanotowano opadów o dużej wydajności. -
Assessment of Natural and Cultural Landscape Capacity to Proposals the Ecological Model of Tourism Development (Case Study for the Area of the Zamagurie Region)
Ekológia (Bratislava) Vol. 36, No. 1, p. 69–87, 2017 DOI:10.1515/eko-2017-0007 Assessment of natural AND cultural landscape capacity to proposals THE ecological model of tourism development (Case study for THE AREA of THE Zamagurie region) MONIKA DRÁBOVÁ-DEGRO, ZDENA KRNÁČOVÁ* Jurská 23, 831 02 Bratislava, Slovak Republic; e-mail: [email protected] Institute of Landscape Ecology of SAS, Štefánikova 3, P.O.Box 254, 814 99 Bratislava, Slovak Republic; e-mail: zdena. [email protected] *Author for correspondence Abstract Drábová-Degro M., Krnáčová Z.: Assessment of natural and cultural landscape capacity to pro- posals the ecological model of tourism development (case study for the area of the Zamagurie region). Ekológia (Bratislava), Vol. 36, No. 1, p. 69–87, 2017. Agricultural and industrial conditions are not favourable in the uphill and mountain areas of the Zamagurie region, and tourism is often the only opportunity to create new jobs, develop the habitation areas and avoid the emigration of local inhabitants. The Walachian and Sholtys colo- nization has transformed the landscape and created unique significant spatial landscape elements that are traditionally utilized for agricultural purposes, and create a unique esthetical landscape preserved till the present times. This case study has been aimed at developing and applying the new quantification methods using GIS tools for evaluation of localizing, selective realization and environmental preconditions of the landscape, representing recreational (cultural) services of the landscape ecological systems, based on selected indicators. To evaluate the localizing precondi- tions of the landscape, we referred to the landscape-ecological complex geo-databases (LEC) (The- matic maps - internal ground document of ZB GIS , 2013), completed with the field survey during the period 2013−2014 and identification of secondary landscape structure elements (SLS) and selected morphometric indicators. -
Prírodné Predpoklady Cestovného Ruchu Národného Parku Pieniny S Dôrazom Na Analýzu Sústavy Natura 2000
MEDZINÁRODNÝ VEDECKÝ ČASOPIS MLADÁ VEDA / YOUNG SCIENCE Jún 2016 (číslo 1) Ročník štvrtý ISSN 1339-3189 Kontakt: [email protected], tel.: +421 908 546 716, www.mladaveda.sk Fotografia na obálke: Obec Kanal (Slovinsko) 2014. © Branislav A. Švorc, foto.branisko.at REDAKČNÁ RADA doc. Ing. Peter Adamišin, PhD.(Katedra environmentálneho manažmentu, Prešovská univerzita, Prešov) doc. Dr. Pavel Chromý, PhD. (Katedra sociální geografie a regionálního rozvoje, Univerzita Karlova, Praha) doc. PaedDr. Peter Čuka, PhD. (Katedra cestovního ruchu, Slezská univerzita v Opavě) prof. Dr. Paul Robert Magocsi (Chair of Ukrainian Studies, University of Toronto; Royal Society of Canada) Ing. Lucia Mikušová, PhD. (Ústav biochémie, výživy a ochrany zdravia, Slovenská technická univerzita, Bratislava) doc. Ing. Peter Skok, CSc. (Ekomos s. r. o., Prešov) prof. Ing. Róbert Štefko, Ph.D. (Katedra marketingu a medzinárodného obchodu, Prešovská univerzita, Prešov) prof. PhDr. Peter Švorc, CSc.,predseda (Inštitút histórie, Prešovská univerzita, Prešov) doc. Ing. Petr Tománek, CSc. (Katedra veřejné ekonomiky, Vysoká škola báňská - Technická univerzita, Ostrava) REDAKCIA PhDr. Magdaléna Barányiová (Fakulta stredoeurópskych štúdií UKF, Nitra) Mgr. Martin Hajduk (Inštitút histórie, Prešovská univerzita, Prešov) Mgr. Richard Nikischer, Ph.D. (Sociologický ústav Akademievěd ČR, Praha) Mgr. Branislav A. Švorc, PhD., šéfredaktor (Vydavateľstvo UNIVERSUM, Prešov) PhDr. Veronika Trstianska, PhD. (Ústav stredoeurópskych jazykov a kultúr FSŠ UKF, Nitra) Mgr. Veronika Zuskáčová -
National and Landscape Parks, Nature Reserves
National and landscape parks, nature reserves MAŁOPOLSKA 14 UNESCO World Heritage List sites 255 attractions on the Wooden Architecture Route Wadowice – town of birth of Pope John Paul II Salt mines in Wieliczka and Bochnia 9 spa resorts 6 national parks 6 geothermal pools Rafting down the Dunajec gorge 2600 km of bicycle trails 3360 km of mountain trails 65 ski stations www.visitmalopolska.pl fb.com/lubiemalopolske The project has been funded by Małopolska Region Rejkiawik IS MAŁOPOLSKA NATIONAL AND LANDSCAPE PARKS, NATURE RESERVES Capital of the region: Kraków MAŁOPOLSKA Major cities: Tarnów, Nowy Sącz, Oświęcim National Parks, Landscape Parks and Nature Reserves Surface area: 15,190 km2 (about 5% of the surface area of Poland) FIN Helsinki Population: 3.4 mil. (about 8% of the population of Poland) N Oslo S Sztokholm Tallin Landscape: EST RUS the tallest peak – Rysy: 2499 m asl Ryga Encounter with Nature LV mountains – Tatras, Beskids, Pieniny, Gorce Dublin DK foothills – Carpathian Foothills IRL Kopenhaga LT Wilno ałopolska is a unique region, especially in GB RUS uplands – Kraków-Częstochowa Upland Mińsk NL terms of its natural diversity. It boasts fanci- lowlands – Vistula valley Londyn BY Amsterdam Berlin ful outliers and hot desert sands, the scenic main rivers – Vistula, Dunajec, Poprad, Raba, Skawa, Biała Bruksela Warszawa D PL ribbon of the Vistula River and the Dunajec water reservoirs – Czorsztyński, Rożnowski, Czchowski, Dobczycki, Klimkówka B Kijów L Praga KRAKÓW MRiver forcing its way between the rocks, -
DRAINAGE BASIN of the BALTIC SEA Chapter 8
216 DRAINAGE BASIN OF THE BALTIC SEA Chapter 8 BALTIC SEA 217 219 TORNE RIVER BASIN 221 KEMIJOKI RIVER BASIN 222 OULUJOKI RIVER BASIN 223 JÄNISJOKI RIVER BASIN 224 KITEENJOKI-TOHMAJOKI RIVER BASINS 224 HIITOLANJOKI RIVER BASIN 226 VUOKSI RIVER BASIN 228 LAKE PYHÄJÄRVI 230 LAKE SAIMAA 232 JUUSTILANJOKI RIVER BASIN 232 LAKE NUIJAMAANJÄRVI 233 RAKKOLANJOKI RIVER BASIN 235 URPALANJOKI RIVER BASIN 235 NARVA RIVER BASIN 237 NARVA RESERVOIR 237 LAKE PEIPSI 238 GAUJA/KOIVA RIVER BASIN 239 DAUGAVA RIVER BASIN 241 LAKE DRISVYATY/ DRUKSHIAI 242 LIELUPE RIVER BASIN 245 VENTA, BARTA/BARTUVA AND SVENTOJI RIVER BASINS 248 NEMAN RIVER BASIN 251 LAKE GALADUS 251 PREGEL RIVER BASIN 254 VISTULA RIVER BASIN 260 ODER RIVER BASIN Chapter 8 218 BALTIC SEA This chapter deals with major transboundary rivers discharging into the Baltic Sea and some of their transboundary tributaries. It also includes lakes located within the basin of the Baltic Sea. TRANSBOUNDARY WATERS IN THE BASIN OF THE BALTIC SEA1 Basin/sub-basin(s) Total area (km²) Recipient Riparian countries Lakes in the basin Torne 40,157 Baltic Sea FI, NO, SE Kemijoki 51,127 Baltic Sea FI, NO, RU Oulujoki 22,841 Baltic Sea FI, RU Jänisjoki 3,861 Lake Ladoga FI, RU Kiteenjoki-Tohmajoki 1,595 Lake Ladoga FI, RU Hiitolanjoki 1,415 Lake Ladoga FI, RU Lake Pyhäjärvi and Vuoksi 68,501 Lake Ladoga FI, RU Lake Saimaa Juustilanjoki 296 Baltic Sea FI, RU Lake Nuijamaanjärvi Rakkonlanjoki 215 Baltic Sea FI, RU Urpanlanjoki 557 Baltic Sea FI, RU Saimaa Canal including 174 Baltic Sea FI, RU Soskuanjoki Tervajoki 204 -
Growth Rate of the Chub (Squalius Cephalus) and the Nase (Chondrostoma Nasus) from Raba, Dunajec, and Poprad River Piotr Epler, Michał Nowak, and Włodzimierz Popek
AACL BIOFLUX Aquaculture, Aquarium, Conservation & Legislation International Journal of the Bioflux Society Growth rate of the chub (Squalius cephalus) and the nase (Chondrostoma nasus) from Raba, Dunajec, and Poprad River Piotr Epler, Michał Nowak, and Włodzimierz Popek Department of Ichthyobiology and Fisheries, University of Agriculture in Kraków, ul. T. Spiczakowa 6, 30-199 Kraków, Poland, EU. Corresponding author: M. Nowak, [email protected] Abstract. In presented study growth rate of the chub Squalius cephalus and nase Chondrostoma nasus from Raba, Dunajec, and Poprad River were investigated using a back-scaling method. A total number of 167 chubs and 186 nases were analysed. Age of these fishes varied from 2 to 12 years. Growth rate of fish analysed was high and similar to other results from upper Vistula River drainage. We consider that artificial fry gained from these rivers may contribute declining populations of these two species in other rivers of upper Vistula drainage. Key Words: growth rate, chub, nase, Raba, Dunajec, Poprad. Strzeszczenie. Celem badań było określenie tempa wzrostu klenia Squalius cephalus oraz świnki Chondrostoma nasus z Raby, Dunajca i Popradu metodą odczytów wstecznych. Przebadano łącznie 167 kleni i 186 świnek w wieku od 2 do 12 lat. Tempo wzrostu obu gatunków w badanych rzekach było wysokie i porównywalne z danymi uzyskanymi podczas badań na innych rzekach w rejonie Górnej Wisły. Można przypuszczać, że materiał zarybieniowy wyprodukowany na bazie klenia i świnki z Raby, Dunajca i Popradu z powodzeniem mógłby zostać użyty do wzmocnienia zagrożonych populacji tych ryb w rejonie Górnej Wisły. Słowa kluczowe: tempo wzrostu, kleń, świnka, Raba, Dunajec, Poprad.