Waterways – in Reference to the Previous Comments
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THE BUG RIVER VALLEY for NATURE LOVERS Eastern Poland with a Difference
THE BUG RIVER VALLEY FOR NATURE LOVERS Eastern Poland with a difference By Olivier Dochy, Belgium From 21st until 25th of June, I got the chance to join a study visit to the valley of the Bug river on the border of Poland and Belarus, in the far east of Poland. The purpose of this visit was tot evaluate local initiatives for sustainable tourism, oriented to "riverside & country- side" tourism. This visit was organized by a Flemish-Polish exchange project with the prov- inces of West-Vlaanderen en Lubelski (Poland), but also the flemish initiative vzw De Boot (www.deboot.be). My task was to evaluate which topics in the region could be interesting for nature-lovers in general and keen nature-specialists in particular, such as birders. Well, there is a lot ! It is not like the wild expanses of the well-known Biebrza valley or the untouched forests of Bia- lowieza, but rather a small-scale (agri)cultural landscape. But it still has all the biodiversity that once flourished in Western-Europe and now all (but) disappeared. Here follow a number of tips voor those who want to visit the region. There is a lot of in- formation great and small on the internet about the region, but you have to surf a lot to find it all. Anyway, there certainly is a lot to discover for naturalists with a pioneer drive ! You can find pictures of our visit here: http://picasaweb.google.com/Odee.fotos/BugRiverPoland?feat=directlink 1 WHERE IS IT ? The province of Lubelski is in the extreme east of Poland. -
Okręg Mazowiecki
OKRĘG MAZOWIECKI Wykaz wód I. Wody nizinne 1. Rzeki, zbiorniki zaporowe, jeziora w obwodach rybackich Nazwa obwodu Położenie Pow. Granice obwodu rybackiego /powiat [ha] Obwód rybacki obejmuje wody: a) rzeki Kosodka (Golda) na odcin- ku od źródeł do granicy BPN, rz. Biebrza b) rzeki Klimaszewnica na odcinku Grajewo 17,0 nr 3 – (Wissa) od źródeł do granicy BPN, c) rzeki Wissa na odcinku od źródeł do granicy BPN (m. Łoje Awissa). Obwód rybacki obejmuje wody: Ostrów Maz. rz. Brok nr 1 a) rzeki Brok od źródeł do jej ujścia Wysokie 43,0 do rzeki Bug. Mazowieckie Obwód rybacki obejmuje wody: a) rzeki Bug na odcinku od ujścia rzeki Nurzec do ujścia rzeki rz. Bug nr 5 Liwiec, 1268 b) zbiornika Sterdyń. Ostrów Maz. Uwaga: Nadbużański Park Krajo- Wyszków brazowy* Obwód rybacki obejmuje wody: a) rzeki Ełk na odcinku od jazu piętrzącego elektrowni w miej- scowości Nowa Wieś Ełcka do granicy Biebrzańskiego Parku Narodowego, Ełk, rz. Ełk nr 45 103 b) Kanału Kuwasy na odcinku od Grajewo osi podłużnej mostu w miejsco- wości Czarna Wieś do rzeki Ełk, c) Kanału Rudzkiego na odcinku od rzeki Ełk do granicy Bie- brzańskiego Parku Narodowego. } 1 Nazwa obwodu Położenie Pow. Granice obwodu rybackiego /powiat [ha] Obwód rybacki obejmuje wody: a) rzeki Jegrznia na odcinku od rz. Jegrznia ujścia cieku Zgniłka do granicy Grajewo 6,00 nr 11 Biebrzańskiego Parku Narodo- wego. Obwód rybacki obejmuje wody: a) rzeki Jeziorka od zbiornika w Głuchowie do jej ujścia do rze- rz. Jeziorka ki Wisła, Grójec, 120 nr 1 b) zbiornika Głuchów, Piaseczno c) zbiornika Osieczek, d) rzeki Kraska od jej źródeł do jej ujścia do rzeki Jeziorka. -
Floods in Poland from 1946 to 2001 — Origin, Territorial Extent and Frequency
Polish Geological Institute Special Papers, 15 (2004): 69–76 Proceedings of the Conference “Risks caused by the geodynamic phenomena in Europe” FLOODS IN POLAND FROM 1946 TO 2001 — ORIGIN, TERRITORIAL EXTENT AND FREQUENCY Andrzej DOBROWOLSKI1, Halina CZARNECKA1, Janusz OSTROWSKI1, Monika ZANIEWSKA1 Abstract. Based on the data concerning floods on the territory of Poland during the period 1946–2001, the reasons generating floods, the number of regional floods in the rivers catchment systems, and sites of local floods occurrence, were defined. Both types of floods: caused by riverbank overflows, and land flooding by rain or snow-melt water, were considered. In the most cases, the floods were caused by rainfall. They were connected with changes in the rainfall structure within Po- land. In each season of the year floods of various origin were observed. When the flood initiating factors appeared simulta- neously, the flood grew into a catastrophic size. In present analysis, for the first time in Poland, a large group of local floods has been distinguished. A special attention has been paid to floods caused by sudden flooding of the land (flash flood), including floods in the urban areas — more and more frequent during the recent years. The results of the analyses have provided important data for the assessment of the flood hazard in Poland, and for the creation of a complex flood control strategy for the whole country and/or for selected regions. Key words: flood, classification of floods, floods territorial extent, frequency of floods occurrence, torrential and rapid rain- fall, threat of life, material losses. Abstrakt. Na podstawie zbioru danych z lat 1946–2001 okreœlono przyczyny wystêpowania powodzi w Polsce, liczbê powodzi re- gionalnych w uk³adzie zlewni rzecznych oraz miejsca wyst¹pieñ powodzi lokalnych. -
Environmental Impact Report
ENVIRONMENTAL IMPACT REPORT SUPPLEMENT TO THE REPORT ON THE ENVIROMENTAL IMPACT OF THE “CONSTRUCTION OF THE KARCINO-SARBIA WIND FARM (17 WIND TURBINES)” OF 2003 Name of the undertaking: KARCINO-SARBIA Wind Farm (under construction) Contractor: AOS Agencja Ochrony Środowiska Sp. z o.o. based in Koszalin Arch. No. 52/OŚ/OOS/06 Koszalin, September 2006 Team: Bogdan Gutkowski, M.Sc.Eng.– Expert for Environmental Impact Assessment Appointed by the Governor of the West Pomerania Province Marek Ziółkowski, M.Sc. Eng. – Environmental Protection Expert of the Ministry of Environmental Protection, Natural Resources and Forestry; Environmental Protection Consultant Dagmara Czajkowska, M.Sc. Eng. – Specialist for Environmental Impact Assessment, Specialist for Environmental Protection and Management Ewa Reszka, M.Sc. – Specialist for the Protection of Water and Land and Protection against Impact of Waste Damian Kołek, M.Sc.Eng. – Environmental Protection Specialist 2 CONTENTS I. INTRODUCTION .................................................................................................................. 5 II. GENERAL INFORMATION ABOUT THE PROJECT ..................................................... 9 1. Location and adjacent facilities....................................................................................................... 9 2. Modifications to the project .......................................................................................................... 10 3. Technical description of the project .............................................................................................. -
The Lower Vistula in the Aspect of the E40 and E70 International Shipping Routes
Ż. Marciniak | Acta Energetica 2/15 (2013) | 153–161 The lower Vistula in the aspect of the E40 and E70 international shipping routes Author Żaneta Marciniak Keywords shipping route, waterways, inland navigation, E40 international waterway, E70 international waterway Abstract Throughout the history of Europe and the world, shipping routes have determined the develop- ment of many civilisations, since it was along them that settlements and commerce developed, goods and people were transported, and later, industry was located. Currently, shipping routes are an important element in inland transport corridors. The European Union puts particular emphasis on the development of inland and rail transport to balance road transport, which is drastically expanding. Development of inland waterway transport routes in Poland has allies in intensely developing sea ports. The allies of the lower Vistula (dolna Wisła) are the ports in Gdańsk and Gdynia, for which construction of inland ports up-country is an opportunity to increase the trans-shipment capacity. Poland uses the potential of international inland waterways poorly when compared to other European Union countries, which results for instance from the bad technical condition of river engineering structures and from years of neglect in water management. The situation is further amplified by the lack of consistent laws regarding inland navigation and water management, as the responsibility for those issues is shared by several ministries, the institutions they are in charge of and local governments. Governments of the voivodeships situated along the planned international waterways E40 between Warsaw and Gdańsk (Mazowieckie, Kujawsko-Pomorskie, Pomorskie voivodeships) and E70 (Lubuskie, Wielkopolskie, Kujawsko-Pomorskie, Warmińsko-Mazurskie, Pomorskie voivode- ships) can see both the transport and the tourism potential of Polish waterways. -
Sediment Yields and Denudation Rates in Poland
Erosion and Sediment Yield: Global and Regional Perspectives (Proceedings of the Exeter Symposium, July 1996). IAHS Publ. no. 236, 1996. 133 Sediment yields and denudation rates in Poland JAN BRAÑSKI Research and Design Office HYDROS, ul. Somleñskiego 16 B m.58, 01 698 Warsaw, Poland KAZIMIERZ BANASIK Department of Hydraulic Structures, Warsaw Agricultural University SGGW, ul. Nowoursynowska 166, 02-787 Warsaw, Poland Abstract In Poland, there are many 40-year records of suspended sedi ment transport. These records have been used to estimate the intensity of denudation processes over the territory of Poland. The denudation index, expressed in t km’2 year’1, was calculated for many river basins, using data from 50 river gauging stations. The results are presented in the form of maps of denudation rates over the territory of Poland for four decades during the period 1951-1990. INTRODUCTION One of the first studies of the intensity of denudation processes in the Vistula river basin was carried out by Jarocki (1957). Based on hydrological measurements at the Tczew gauge during the period 1946-1953, he concluded that the average value of the denuda tion index (i.e. total sediment yield/river basin area) was 81 km’2 year’1. The first maps of the spatial differentiation of the denudation index across Poland were produced indirectly, by using a map of potential soil erosion published by Reniger (1959). Two versions of such maps were produced using this approach by Dçbski (1959) and Skibinski (1959). The results of Skibinski’s investigation, which dealt only with suspended sediment, in contrast to Dçbski’s investigation which also included bed load, showed considerable spatial differentiation of the denudation index, particularly in the zone of the south Polish uplands, with values ranging from ca 10 to 160 t km"2 year’1. -
The Crime of Genocide Committed Against the Poles by the USSR Before and During World War II: an International Legal Study, 45 Case W
Case Western Reserve Journal of International Law Volume 45 | Issue 3 2012 The rC ime of Genocide Committed against the Poles by the USSR before and during World War II: An International Legal Study Karol Karski Follow this and additional works at: https://scholarlycommons.law.case.edu/jil Part of the International Law Commons Recommended Citation Karol Karski, The Crime of Genocide Committed against the Poles by the USSR before and during World War II: An International Legal Study, 45 Case W. Res. J. Int'l L. 703 (2013) Available at: https://scholarlycommons.law.case.edu/jil/vol45/iss3/4 This Article is brought to you for free and open access by the Student Journals at Case Western Reserve University School of Law Scholarly Commons. It has been accepted for inclusion in Case Western Reserve Journal of International Law by an authorized administrator of Case Western Reserve University School of Law Scholarly Commons. Case Western Reserve Journal of International Law Volume 45 Spring 2013 Issue 3 The Crime of Genocide Committed Against the Poles by the USSR Before and During WWII: An International Legal Study Karol Karski Case Western Reserve Journal of International Law·Vol. 45·2013 The Crime of Genocide Committed Against the Poles The Crime of Genocide Committed Against the Poles by the USSR Before and During World War II: An International Legal Study Karol Karski* The USSR’s genocidal activity against the Polish nation started before World War II. For instance, during the NKVD’s “Polish operation” of 1937 and 1938, the Communist regime exterminated about 85,000 Poles living at that time on the pre- war territory of the USSR. -
Advisory and Technical Committee for Communications and Transit
[Distributed to the Council C. 12. M. 7 . 1925. VIII. and the Members of the League.] (C. C. T./C. J./N . I./ist Session P. V.) Geneva, Jan u ary 15th, 1925. LEAGUE OF NATIONS. ADVISORY AND TECHNICAL COMMITTEE FOR COMMUNICATIONS AND TRANSIT. Joint Session of the Legal Committee and the Sub-Committee for Inland Navigation. MINUTES OF THE FIRST SESSION Held at Geneva, November z^th-zbth, 1924. (With Annexes.) The Legal Committee is at present composed as follows : His Excellency Dr. F. J. U r r u t ia (appointed by the Government of Colombia), Envoy Extra ordinary and Minister Plenipotentiary in Switzerland (Chairman). His Excellency Dr. J. G. G u e r r e r o (appointed by the Government of Salvador), Envoy Extra ordinary and Minister Plenipotentiary in France and Switzerland (Vice-Chairman). M. B. W in ia r s k i (appointed b y the Government of Poland), Professor of Lawy at the University of Poznan. Jonkheer W . J. M. v a n E y s in g a , Professor at the University of Leyden. M. J. H o s t ie , former Legal Adviser to the Belgian Department of Marine, Secretary-General of the Central Commission for Rhine Navigation. The Sub-Committee for Inland Navigation is at present composed as follows : M. Silvain D r e y f u s (appointed by the Government of France), Inspector-General of Bridges and Roads, Member of the Central Commission for Rhine Navigation (Chairman). M. G. P o p e sc o (appointed b y the Government of Roumania), Professor, Director-General of the Société nationale de crédit industriel (Vice-Chairman). -
1 Since 1961 Morphological and Geochemical Record of Historical
since 1961 BALTICA Volume 33 Number 1 June 2020: 1–10 https://doi.org/10.5200/baltica.2020.1.1 Morphological and geochemical record of historical erosion on the example of small alluvial and deluvial fans accumulated on the Bug River terraces in the Neple area (Podlasie Lowland, eastern Poland) Piotr Szwarczewski, Anna Rogóż-Matyszczak, Łukasz Zbucki Szwarczewski, P., Rogóż-Matyszczak, A., Zbucki, Ł. 2020. Morphological and geochemical record of historical erosion on the example of small alluvial and deluvial fans accumulated on the Bug River terraces in the Neple area (Podlasie Lowland, eastern Poland). Baltica, 33 (1), 1–10. Vilnius. ISSN 0067-3064. Manuscript submitted 28 January 2019 / Accepted 6 December 2019 / Published online 23 December 2019 © Baltica 2020 Abstract. The gullies in the vicinity of Neple (Podlaska Lowland, eastern Poland) are relatively young and were created due to the land use and climate changes. The aim of the research was to determine the variability of selected alluvial-deluvial fans occurring in the Bug River valley and their age using interdisciplinary meth- ods (e.g. absolute dating, geochemical analyzes, cartographic data). Geological mapping and several drillings (both within the fans, valleys or gullies bottoms and glacial or fluvioglacial plateaus) were done. Historical data dealing with the human economic activity in the region were analyzed. The obtained radiocarbon dating and geochemical features of sediments building the alluvial and deluvial fans proved that these forms are not older than some 500 years. Due to the lateral movement of the Bug River channel only some of the forms are preserved in the area under study. -
Dermacentor Reticulatus and Occurrence of Canine Babesiosis in Poland in 2016–2018 Dorota Dwużnik‑Szarek1*, Ewa J
Dwużnik‑Szarek et al. Parasites Vectors (2021) 14:267 https://doi.org/10.1186/s13071‑021‑04758‑7 Parasites & Vectors RESEARCH Open Access Monitoring the expansion of Dermacentor reticulatus and occurrence of canine babesiosis in Poland in 2016–2018 Dorota Dwużnik‑Szarek1*, Ewa J. Mierzejewska1, Anna Rodo2, Katarzyna Goździk3, Jolanta Behnke‑Borowczyk4, Dorota Kiewra5, Natalia Kartawik4 and Anna Bajer1 Abstract Background: The signifcance of tick‑borne diseases has increased considerably in recent years. Because of the unique distribution of the tick species Dermacentor reticulatus in Poland, comprising two expanding populations, Eastern and Western that are separated by a Dermacentor‑free zone, it is important to conduct studies on the process of tick expansion and emergence of canine babesiosis. The main aim of the current study was to monitor the expan‑ sion of D. reticulatus populations from spring 2016 to autumn 2018 to determine (1) the actual geographical range of this tick species, and (2) and the seasonal/annual shift in range limits and changes in distance between Western and Eastern populations of ticks (the size of the non‑endemic area). Methods: Ticks were collected in spring/autumn during a 3‑year study. From each season and year at least three pairs of sites from the Western and Eastern populations were selected. Then the mean distance between paired sites was calculated for each season and year. We collected and analyzed data from veterinary clinics on the number of canine babesiosis cases treated in the clinic during a whole year (2018). Results: Accordingly, further expansion of the two D. reticulatus populations was recorded, mainly along river basins. -
Malacofauna in Oxbow Lakes of the Bug River Within the Nadbuĩaēski Landscape Park
Teka Kom. Ochr. Kszt. ĝrod. Przyr. – OL PAN, 2013, 10, 132–142 MALACOFAUNA IN OXBOW LAKES OF THE BUG RIVER WITHIN THE NADBUĩAēSKI LANDSCAPE PARK Beata Jakubik, Krzysztof Lewandowski Institute of Biology, Siedlce University of Natural Sciences and Humanities B. Prusa str. 12, 08-110 Siedlce, [email protected], [email protected] Co-financed by National Fund for Environmental Protection and Water Management Summary. Malacofauna was studies in six oxbow lakes situated in the NadbuĪaĔski Landscape Park between the outlets of two confluents of the Bug River – the Liwiec and Nurzec. The water bodies are of different hydrological regime, from throughflow to isolated lakes. From 9 to 18 mollusc taxa were noted there. Oxbow lakes connected with the Bug had a higher species richness than those long ago permanently isolated from the river. Particularly large share in malacofauna of connected oxbow lakes had bivalves of the family Unionidae, Dreissena polymorpha and snails of the family Viviparidae. Protected species were found among studied molluscs. Studies carried out in two periods 2003–2004 and 2007–2011 showed small differences in species composition of malacofauna. Key words: NadbuĪaĔski Landscape Park, oxbow lakes, molluscs INTRODUCTION The NadbuĪaĔski Landscape Park occupies a 120-km long part of natural valley of the Bug River, where a meandering river channel is accompanied by numerous oxbow lakes [Dombrowski et al. 2002]. Ecology of these oxbow lakes was poorly recognised though the interest in such water bodies has markedly increased recently. This pertains mainly to rivers of eastern Poland – the Bug and Narew [see e.g. Górniak 2001, Biesiadka and Pakulnicka 2004, Jurkiewicz- -Karnkowska 2006, 2011, Lewandowski 2006, Strzaáek 2006, GruĪewski 2008]. -
Arkusz TERESPOL (570)
PA Ń STWOWY INSTYTUT GEOLOGICZNY PA Ń STWOWY INSTYTUT BADAWCZY OPRACOWANIE ZAMÓWIONE PRZEZ MINISTRA Ś R O D O W I S K A OBJAŚNIENIA DO MAPY GEOŚRODOWISKOWEJ POLSKI 1:50 000 Arkusz TERESPOL (570) Warszawa, 2011 Autorzy: Marta Chwistek*, Izabela Bojakowska*, Paweł Kwecko*, Jerzy Miecznik*, Barbara Radwanek-Bąk*, Jerzy Król**, Anna Wąsowicz** Główny koordynator MGP: Małgorzata Sikorska-Maykowska* Redaktor regionalny: Bogusław Bąk* Redaktor regionalny planszy B: Anna Gabryś-Godlewska* Redaktor tekstu: Olimpia Kozłowska* * – Państwowy Instytut Geologiczny Państwowy Instytut Badawczy, ul. Rakowiecka 4, 00-975 Warszawa ** – Przedsiębiorstwo Geologiczne we Wrocławiu Proxima SA, ul. Kwidzyńska 71, 51-415 Wrocław ISBN Copyright by PIG–PIB and MŚ, Warszawa, 2011 Spis treści I. Wstęp (M. Chwistek)............................................................................................................ 3 II. Charakterystyka geograficzna i gospodarcza (M. Chwistek)............................................... 4 III. Budowa geologiczna (M. Chwistek).................................................................................. 6 IV. ZłoŜa kopalin (M. Chwistek, B. Radwanek-Bąk )................................................................. 9 V. Górnictwo i przetwórstwo kopalin (M. Chwistek, B. Radwanek-Bą k)................................ 13 VI. Perspektywy i prognozy występowania kopalin (M. Chwistek, B. Radwanek-Bąk )........... 14 VII. Warunki wodne (M. Chwistek) ……..................................................................................