Reproductive Cycle and the Related Spatial and Temporal Distribution Of
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Procesy Aktywizuj¹ce Degradację Wybrze¿A Klifowego Zalewu Puckiego
Przegl¹d Geologiczny, vol. 53, nr 1, 2005 Procesy aktywizuj¹ce degradacjê wybrze¿a klifowego Zalewu Puckiego Leszek Zaleszkiewicz*, Dorota Koszka-Maroñ* Activation processes of degradation of cliff coast of Puck Lagoon. Prz. Geol., 53: 55–62. Summary.Thewestern cliff coast of Puck Lagoon has a lentgh of 7900 m. Its development proceeds as a result of processes of desintegration, denudation and marine erosion. The mass movement getting on depends on kind of sediment, geometry of slope and plant cover. Earth fall and talus accumulation prevail. As an effect of this pro- cesses, the cliff retreats in the form of small wastes. Key words: Puck Lagoon, cliff coast, geodynamical processes, photographic panorama L. Zaleszkiewicz Dotychczasowe badania geologiczne Ogólna charakterystyka obszaru badañ prowadzone na obszarze wybrze¿a Zale- i zarys budowy geologicznej wu Puckiego ogranicza³y siê do ogólnego opisu budowy geologicznej regionu i W wyniku erozyjnego i akumulacyjnego dzia³ania charakterystyki okreœlonych osadów w ostatniego l¹dolodu oraz jego wód roztopowych powsta³y wybranych miejscach (Subotowicz, odizolowane pradolinami P³utnicy i Redy fragmenty 1982; Jankowska & £êczyñski, 1993; wysoczyzn morenowych Kêpy Puckiej i Swarzewskiej. Skompski, 1997, 2001, 2002; Zawadz- Powierzchnie kêp o charakterze równin, maj¹ce w czêœci ka-Kahlau, 1999; Mas³owska i in., 2000, centralnej wysokoœci bezwzglêdne 30,0–40,0 m n.p.m., 2003). W zale¿noœci od budowy geolo- ³agodnie opadaj¹ w kierunku wschodnim. W stosunku do gicznej i procesów geodynamicznych D. Koszka-Maroñ obecnej sytuacji kontynuowa³y siê one na obszarze dzisiej- okreœlano typ klifu i porównywano go na szego Zalewu. Obecnie zachodnie wybrze¿e wysoczyznowe tle ca³ego wybrze¿a. -
Istituto Tecnico Tecnologico Baracca Kaszubskie Liceum
ONLINE EXCHANGE BRESCIA & BRUSY Istituto Tecnico Tecnologico Baracca Kaszubskie Liceum Ogólnokształcące w Brusach 2021 Elisa Lacagnina Thanks to the Etwinning platform I had the possibility to know Ms. Alicja Frymark, English teacher from Kashubian Secondary School (Kaszubskie Liceum Ogólnokształcące) in Brusy, Poland. Since our first online meeting on Skype, we have kept talking, most of all, of our school project called “Online exchange - Brescia & Brusy”. To start, we decided to assign our students a partner to make them work in pairs. Their task was to exchange emails with their friend about the topic given and then, with the information, to write a short article in English. We assigned different topics like Covid 19 and lockdown; traditional food; language uses; interesting facts about the city, the country and the region; school; local tradition. The first part of the project went really well and I was satisfied with the work done. My 5th-year students are enthusiastic about having a “virtual” foreign partner. I decided to start an online exchange because my students felt the need to improve their English speaking and writing skills, as we have only 3 hour English a week. According to me, these opportunities are not only useful to improve the language skills but also to expand your knowledge, to meet new people, to know about the uses and the customs of different countries. Moreover, it was the right moment to start a project of this kind precisely in this difficult period. We have been experiencing a different life, due to Covid 19 home–schooling, restrictions, curfews, prohibitions etc. -
A0 Vertical Poster
Hydrochemical characterization of SGD in the Bay of Puck, Southern Baltic Sea Żaneta Kłostowska1,2*, Beata Szymczycha1, Karol Kuliński1, Monika Lengier1 and Leszek Łęczyński2 1 Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, 81-712 Sopot, Poland 2 Institute of Oceanography, University of Gdańsk, Marszałka Piłsudskiego 46, 81-378 Gdynia, Poland * [email protected] Introduction Submarine groundwater discharge (SGD) is defined as all flow of water from seabed to the water column and is a significant path of both water masses and chemical substances exchange between land and ocean (Burnett et al. 2003). SGD in the Bay of Puck has been recognized as an important source of selected chemical substances in comparison to rivers, atmospheric deposition and point sources (Szymczycha and Pempkowiak 2016). The assumption was made that SGD off Hel is representative for the whole area. As inner and outer part of the Bay of Puck characterizes with different oceanographic conditions there is a need to verify whether SGD composition is similar at both parts. The aim of this study was to identify difference in SGD composition at several sites located in the Inner and Outer part of the Bay of Puck including sites located in Hel Peninsula and mainland. Methods The research was carried out within 2016 and 2017. Three active groundwater discharge areas were identified in Hel Peninsula (Hel, Jurata, Chałupy), and three at inland part of the bay (Puck, Swarzewo and Osłonino) based on in situ salinity measurements (Fig.1.). Samples with Cl- concentration smaller than 1000 mg·dm-3 represented SGD, while samples with Cl- concentration higher than 1000 mg·dm-3 were recognised as seepage water. -
Annual Conference of the International Wader Study Group
The Hel Peninsulais one of the most interestingplaces for Hamburgand Frankfurt, or via Warsaw(6-7 flightsWar- waterbirdsalong the coastof Polandin the non-breedingsea- saw-Gdanska day). In Warsaw,you can alsochange to son.Large flocks of waterfowland gulls occuron migration the expresstrain by taking a direct city busfrom the air- andin winter. The peninsulais alsoused as a leadingline by port to the main railway station.From Gdanskairport, migratingpasserines and birds of prey in springand autumn take the city bus (or taxi) to the railway stationand then and is well known as the best spotfor rarities in the whole continueby local train to Gdynia or directto Jurata.De- country.Species that have been recorded include Pallid Har- tailedinformation on planeconnections can be founde.g. rier Circus macrourus, Lesser Kestrel Falco naumanni, on: http://www.lot.com.pl. Terek SandpiperXenus cinereus, Greater Yellowlegs Tringa by ferry - there are sailingsfrom Sweden(Nynashamn, melanoleuca,Richard's Pipit Anthusnovaeseelandiae and Karlskrona)to Gdanskor Gdynia,from Sweden(Malta6, Olive-backed Pipit Anthus hodgsoni.Wet meadows and Ystad) andfrom Denmark(Copenhagen) to Swinoujscie sandybeaches provide excellentconditions for stopover in the westof Polandand then by trainto Gdynia.Details waders and, in 1983, this attracted the interest of studentsof of ferry connectionscan be found at: theUniversity of Gdansk.Wader ringing started then and has ß http://www.polferries.com.pl and sinceturned into a long-termstudy. Eventually this led to the ß http://www.stenaline.com.pl. establishmentof the Waterbird ResearchGroup KULING, by car - comingfrom any direction,go to the town of which is very pleasedto hostthe Annual Conferenceof the Wladyslawowoat thebase of Hel Peninsulaand then con- InternationalWader StudyGroup in its birthplace. -
The Stages of the Cultural Landscape Transformation of Seaside Resorts in Poland Against the Background of the Evolving Nature of Tourism
Land. 2020, 9, x; doi:10.3390/ S1 of S9 Supplementary Materials: The Stages of the Cultural Landscape Transformation of Seaside Resorts in Poland against the Background of the Evolving Nature of Tourism Wojciech Bal and Magdalena Czalczynska-Podolska (a) (b) (c) (d) (e) (f) Land. 2020, 9, x; doi:10.3390/ S2 of S9 (g) (h) (i) (j) (k) (l) Figure S1. Stage I: Elite resort—architecture and landscape: (a) The beach, Świnoujście (1898–1903); (b) The pier and the Spa House, Kołobrzeg; (c) Promenade, Świnoujście (1908–1913); (d) Żeromskiego Street––the promenade, the view from the beach, Świnoujście (1905); (e) Świnoujście, a panoramic view (1918); (f) The map of Świnoujście (1910–1914); (g) Miramare Hotel, Międzyzdroje (1900); (h) Międzyzdroje, a postcard (1895–1900); (i) Dziwnów, a panoramic view (1900–1910); (j) The Spa House, Dziwnów (1910); (k) The pier, Sopot (1900–1910); (l) The beach, Sopot (1895–1900). Source: Fotopolska.eu. Archival photos. Land. 2020, 9, x; doi:10.3390/ S3 of S9 (a) (b) (c) (d) (e) Land. 2020, 9, x; doi:10.3390/ S4 of S9 (f) (g) Figure S2. Stage II: National resort—architecture and landscape: (a) Lido Hotel, Jurata (1932–1933); (b) One of the guesthouses in Jurata (1918–1939); (c) One of the summer villas in Jurata (1918–1939); (d) Bałtyk Hotel, Jurata (1930); (e) Cassino in Recreational Centre, Cetniewo (1831); (f) Jastrzebia Góra, a postcard (1934); (g) Jastrzebia Góra, a postcard (1934). Source: Fotopolska.eu. Archival photos (a, e–g), The National Digital Archives (b–d). Land. 2020, 9, x; doi:10.3390/ S5 of S9 (a) (b) (c) (d) (e) (f) Land. -
Labidesthes Sicculus
Version 2, 2015 United States Fish and Wildlife Service Lower Great Lakes Fish and Wildlife Conservation Office 1 Atherinidae Atherinidae Sand Smelt Distinguishing Features: — (Atherina boyeri) — Sand Smelt (Non-native) Old World Silversides Old World Silversides Old World (Atherina boyeri) Two widely separated dorsal fins Eye wider than Silver color snout length 39-49 lateral line scales 2 anal spines, 13-15.5 rays Rainbow Smelt (Non -Native) (Osmerus mordax) No dorsal spines Pale green dorsally Single dorsal with adipose fin Coloring: Silver Elongated, pointed snout No anal spines Size: Length: up to 145mm SL Pink/purple/blue iridescence on sides Distinguishing Features: Dorsal spines (total): 7-10 Brook Silverside (Native) 1 spine, 10-11 rays Dorsal soft rays (total): 8-16 (Labidesthes sicculus) 4 spines Anal spines: 2 Anal soft rays: 13-15.5 Eye diameter wider than snout length Habitat: Pelagic in lakes, slow or still waters Similar Species: Rainbow Smelt (Osmerus mordax), 75-80 lateral line scales Brook Silverside (Labidesthes sicculus) Elongated anal fin Images are not to scale 2 3 Centrarchidae Centrarchidae Redear Sunfish Distinguishing Features: (Lepomis microlophus) Redear Sunfish (Non-native) — — Sunfishes (Lepomis microlophus) Sunfishes Red on opercular flap No iridescent lines on cheek Long, pointed pectoral fins Bluegill (Native) Dark blotch at base (Lepomis macrochirus) of dorsal fin No red on opercular flap Coloring: Brownish-green to gray Blue-purple iridescence on cheek Bright red outer margin on opercular flap -
Quantitative Analysis of the Impact of Fishing Ship Traffic Streams on Traffic Streams of Merchant Vessels in Polish Maritime Areas
Scientific Journals Zeszyty Naukowe of the Maritime University of Szczecin Akademii Morskiej w Szczecinie 2018, 53 (125), 93–101 ISSN 1733-8670 (Printed) Received: 24.10.2017 ISSN 2392-0378 (Online) Accepted: 20.02.2018 DOI: 10.17402/270 Published: 16.03.2018 Quantitative analysis of the impact of fishing ship traffic streams on traffic streams of merchant vessels in Polish maritime areas Anna Anczykowska, Paulina Rekowska, Wojciech Ślączka Maritime University of Szczecin, Faculty of Navigation, Maritime Risk Center 1–2 Wały Chrobrego St., 70-500 Szczecin, Poland e-mail: [email protected] corresponding author Key words: fishing vessels, Baltic Sea, traffic streams, merchant vessels, maritime areas, risk Abstract The Baltic Sea is crisscrossed by several dense vessel traffic routes. Growing shipping traffic increases the likelihood of collisions. A quantitative analysis of the impact of fishing vessel traffic streams on streams of merchant vessel traffic aims to identify areas of intense traffic of this type and to assess the potential risks. The identification of intersections of fishing vessel routes and merchant shipping traffic allows us to identify spots of potential collisions. The analysis made use of the IALA IWRAP Mk2 program and AIS data collected from April 1, 2013 to March 31, 2014. Introduction Shipping routes in the South Baltic – state of knowledge The intensity of commercial vessel traffic in the Baltic Sea has been increasing yearly. The observed The Helsinki Commission (HELCOM) conducts growth comprises mainly bulk carriers, container research on the vessel traffic density in the Baltic ships, general cargo vessels and passenger ships. Sea. Traffic streams are recorded via the automatic Since the LNG terminal in Świnoujście was put into identification system (AIS). -
Esox Lucius) Ecological Risk Screening Summary
Northern Pike (Esox lucius) Ecological Risk Screening Summary U.S. Fish & Wildlife Service, February 2019 Web Version, 8/26/2019 Photo: Ryan Hagerty/USFWS. Public Domain – Government Work. Available: https://digitalmedia.fws.gov/digital/collection/natdiglib/id/26990/rec/22. (February 1, 2019). 1 Native Range and Status in the United States Native Range From Froese and Pauly (2019a): “Circumpolar in fresh water. North America: Atlantic, Arctic, Pacific, Great Lakes, and Mississippi River basins from Labrador to Alaska and south to Pennsylvania and Nebraska, USA [Page and Burr 2011]. Eurasia: Caspian, Black, Baltic, White, Barents, Arctic, North and Aral Seas and Atlantic basins, southwest to Adour drainage; Mediterranean basin in Rhône drainage and northern Italy. Widely distributed in central Asia and Siberia easward [sic] to Anadyr drainage (Bering Sea basin). Historically absent from Iberian Peninsula, Mediterranean France, central Italy, southern and western Greece, eastern Adriatic basin, Iceland, western Norway and northern Scotland.” Froese and Pauly (2019a) list Esox lucius as native in Armenia, Azerbaijan, China, Georgia, Iran, Kazakhstan, Mongolia, Turkey, Turkmenistan, Uzbekistan, Albania, Austria, Belgium, Bosnia Herzegovina, Bulgaria, Croatia, Czech Republic, Denmark, Estonia, Finland, France, Germany, Greece, Hungary, Ireland, Italy, Latvia, Lithuania, Luxembourg, Macedonia, Moldova, Monaco, 1 Netherlands, Norway, Poland, Romania, Russia, Serbia, Slovakia, Slovenia, Sweden, Switzerland, United Kingdom, Ukraine, Canada, and the United States (including Alaska). From Froese and Pauly (2019a): “Occurs in Erqishi river and Ulungur lake [in China].” “Known from the Selenge drainage [in Mongolia] [Kottelat 2006].” “[In Turkey:] Known from the European Black Sea watersheds, Anatolian Black Sea watersheds, Central and Western Anatolian lake watersheds, and Gulf watersheds (Firat Nehri, Dicle Nehri). -
Proceedings of the Indiana Academy of Science
Ecology of the Southernmost Sympatric Population of the Brook Stickleback, Culaea inconstans, and the Ninespine Stickleback, Pungitius pungitius, in Crooked Lake, Indiana 1 - 3 Joseph S. Nelson, Indiana University Abstract The southernmost locality where Culaea inconstans, the brook stickle- back, and Pungitius pungitius, the ninespine stickleback, occur in sympatry is Crooked Lake, Indiana. Both species were first found in Crooked Lake in 1966 with rotenone, gillnets, and Plexiglas traps. Culaea and Pungitius occur between Zy2 and 10 m and 5 and 3 m, respectively. The summer range in pH for the two species is 7.6 to 8.6 and 7.4 to 8.6, respectively. The temperature range is between 12 and 24 and 6 and 24, respectively. Both sticklebacks probably spawn in rooted aquatics. Pungitius adults, however, generally occur below the zone of rooted aquatics. Fully ripe eggs were found in the limited number of Culaea adults between June 26 and July 19. Pimgitius with fully ripe eggs were found from April to August. Identifiable young of Culaea and Pungitius, 12 mm standard length, were first collected July 19 and June 15, respectively. The largest Culaea was 38 mm while the largest Pungitius was 59 mm standard length. Culaea was found in the stomachs of Micropterus salmoides and Perca flavescens. Stomachs of the latter two species and of Esox americanus contained Pungitius. Introduction Culaea (—Eucalia) inconstans (Kirtland), the brook stickleback, occurs in lakes, ponds, and streams across northern North America from northeastern British Columbia to New Brunswick and south to Indiana. Pungitius pungitius (Linnaeus), the ninespine stickleback, oc- curs in the freshwaters and along the coastlines of northern Asia, Europe, and northern North America. -
Dowgiallo J., Fraczek E
AN AITEMPT li.T THE INTERPRETATION OF NEW DATA ON THE HEL SPIT HYDROGEOLOGY (POLANDl 2 J.DOWGI~L0 1 , E.FRACZEK 1 tnstytut Nauk Geologicznych PAN, 2wirki i Wigury 93 02-089 Warsza.wa 2 rrzedsi9biorstwo Geologiczne. Berez~aka. 39 03-908 Warazawa l\BSTRACT Chemical and isotopic analyses as well as groundwater level monitoring carried out through the years 1987-1989 supp l ied new data concerning the Pleistocene-Cretaceous aquifer of the Hel Spit. The presence of relic water originating probably from the Late Glacial or Earl~~olocene stage of the Baltic Sea development is t3stified to by 6 0 and .oo values as low _as -14°/oo and -100 /oo, respectlvely. The lncrease of water sal1n1ty dur1ng the summer extraction peak may be an indicator of Baltic water intrusions, although the mobilization of more saline relic wate r could be another explanation for this phenomenon. is a territory• where particularly difficult are being faced. Several settlements and resorts become crowded during the summer season. The first contains some fresh water (Sadurski et al., its vulnerability to surface pollution and to the intrusions as well as its limited water reserves its unreliability. Also another solution of the question, namely water transport from the mainland serious technical problems. The Hel Spit is here and 150m (Fig.l) and Baltic storm waves is imminent. On the other and the highway running along the Spit do not pipeline. from the above that water supply for the growing ation and seasonal visitors should be based on an aquifer deeper than the first one, formed of Such an. -
Piaśnica a Scene of German Crimes in Pomerania in 1939
Piaśnica A scene of German crimes in Pomerania in 1939 Introduction by Monika Tomkiewicz PhD, historian and member of the Regional Commission for Investigation of Crimes Against the Polish Nation in Gdańsk Scientific consultation Prof. dr hab. Bogdan Chrzanowski Text edited by Janosz Józefczyk Mirosław Odyniecki Correction of texts by Mateusz Ihnatowicz, PhD Jacek Pudliszewski, PhD Biographical notes written by Mateusz Ihnatowicz, PhD Cover design by Karol Formela First edition The Stutthof Museum in Sztutowo Wejherowo 2017 ISBN 978-83-946986-5-2 Published by: The Stutthof Museum in Sztutowo for the Branch Office: The Piaśnica Museum in Wejherowo (in organisation) 11/2 Św. Jacka St., 84-200 Wejherowo phone/fax: +48 58 736 11 11 e-mail: [email protected] www.muzeumpiasnickie.pl Table of Contents Introduction. Massacre in Piaśnica ................................................. 4 Piaśnica ......................................................................................... 11 Main Memorial ............................................................................. 13 Crossroads – “Pensive Christ” ...................................................... 14 Grave No. 4 ................................................................................... 15 Grave No. 1 ................................................................................... 16 Grave No. 2 ................................................................................... 17 Monument to Leon Najman – Mirza Kryczyński ......................... 18 Memorial -
Krynica Morska
Stralsund The Association of The Association of Sea Cities Sea Cities and Municipalities and Municipalities Pętla Żuławska Kaliningrad Lauterbach Stepnica Klaipėda A guide Nida to the ports and sea harbours of the South Coast Baltic – Vorpommern, Zachodniopomorskie, Pomorskie, Kaliningrad Region, Klaipėda Region Kołobrzeg Szczecin Gdańsk Ahlbeck Łeba www.southcoastbaltic.eu Gdańsk 2015 Explanation of the pictograms South Coast Baltic – sailing distances (in nautical miles) Additional information Policja All information from „A guide to the ports and sea harbours of the SOUTH COAST BALTIC“ Harbour master Berths for yachts Customs clearance Tourist information Police station ATM Post office Telephone Pharmacy as well as further information on the marketing initiative can also be found in the internet / harbour office on www.soutcoastbaltic.eu. (Rügen) Touristic information on the SOUTH COAST BALTIC regions can be found at: Hospital Café / Restaurant Bar Grocery supplies Gas cylinders Ship equipment Yacht club Accommodation Bicycle rental Vorpommern • Island of Rügen: www.ruegen.de Rostock-Warnemünde Stralsund Greifswald Lauterbach Sassnitz (Rügen) Świnoujście Szczecin Kołobrzeg Darłowo Ustka Władysławowo Gdańsk Baltiysk Kaliningrad Klaipėda Rønne (Bornholm) Kalmar (Sweden) Liepaja (Latvia) • Island of Usedom: www.usedom.de Car rental Toilets Showers Drinking water Electricity Waste disposal Waste oil disposal Effluent disposal Laundry facilities Rostock-Warnemünde x 55 77 79 78 110 147 139 164 179 233 306 285 308 330 108 215 340 at the pier