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Morpholithodynamic conditions of the tip of the Hel Peninsula, the Baltic Sea

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Hel Peninsula is a 35 km long spit that extends into water depths of almost 60 m. Unlike most sandy barriers, the distal end of the Hel Peninsula is prograding into the deep water. This affects unique conditions for the evolution of this section of the Peninsula. The aim of this study is to determine the morpholithodynamic changes on the tip of the Hel Peninsula. Shore studies were performed in 2006-2008 and 2012. Measurements included: beach profiling, determination of shoreline and dune base line positions, and collection of sediment samples. The different nature of the eastern, central and western part of the Hel tip is evident. The eastern part is accumulative, the central part is variable with the general nature of strong and differently directed redeposition and accumulative periods, while the western part is highly erosive.
Rocznik
Strony
181--192
Opis fizyczny
Bibliogr. 43 poz., rys., tab., wykr.
Twórcy
  • Department of Marine Geology, Institute of Oceanography, University of Gdańsk, Al. M. Piłsudskiego 46, 81-378 Gdynia, Poland, ocemrz@ug.edu.pl
autor
  • Maritime Institute in Gdańsk, ul. Długi Targ 41/42, 80-830 Gdańsk, Poland
Bibliografia
  • [1]. Bączyk, J. (1963). The genesis of the Hel Peninsula of the background of the development of the Gdańsk Bay. Geographic documentation 6: 1-176 (in Polish).
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  • [7]. Furmańczyk, K. (1995). Coast changes of the Hel Spit over the last 40 years. Journal of Coastal Research, Spec. Issue 22: 193¬196.
  • [8]. Furmańczyk, K. & Musielak S. (1993). Analysis of the Hel Peninsula coastline changes and risk prognosis in light of remote sensing studies, Marine Engineering and Geotechnics 1: 18-22 (in Polish).
  • [9]. Furmańczyk, K., Musielak S. & Prajs J. (1992) Remote sensing characteristics of the coast dynamics in selected section of the Hel (Jastarnia region). Scientific Papers of the University of Szczecin, Marine Sciences 1(86): 27-46 (in Polish).
  • [10]. Gao, S. & Collins M. (2001) The use of grain size trends in marine sediment dynamics: a review. Chinese Journal of Oceanology and Limnology 19(3): 165-271. DOI:10.1007/BF02850664.
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  • [15]. Jankowski, M. (2005a). Rip-current connected structures on nearshore bottom, Władysławowo harbour region. In J. Cyberski (Ed.), State and the threat of the Hel Peninsula (pp. 269-279), Gdańsk: Gdańsk Scientific Society (in Polish, English summary).
  • [16]. Jankowski, M. (2005b). Sedimentary structures as indicators of lithodynamics of nearshore bottom in southern Baltic. Unpublished doctoral dissertation, University of Gdańsk, Gdynia, (in Polish).
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  • [20]. Leontiew, O.K., Nikiforow L.G. & Safianow G.A. (1982). Geomorphology of the seashores. Warszawa: Geol. Publ. (in Polish).
  • [21]. Łęczyński, L. (2009). Morpholithodynamics of the nearshore bottom of Hel Peninsula. Gdańsk: UG Press (in Polish).
  • [22]. Łęgowski, S. (1925). Changes in the shape of the Hel Peninsula. Geographical Journal 3(1-2): 142-143 (in Polish).
  • [23]. Martins, L.R. & Barboza E. G. (2005). Sand-gravel marine deposits and grain-size properties. GRAVEL 3: 59-70.
  • [24]. McLaren, P. & Bowles D. (1985). The effects of sediment transport on grain-size distributions. Journal of Sedimentary Petrology 55(4): 457-470.
  • [25]. Miętus, M. & Jakusik E. (2005). Wind and wave conditions in the area of the Hel Peninsula headland. In J. Cyberski (Ed.), State and the threat of the Hel Peninsula (pp. 59-76), Gdańsk: Gdańsk Scientific Society (in Polish, English summary).
  • [26]. Mojski, J.E. (1995). Geological Atlas of the Southern Baltic 1:500000. Sopot: Polish Geological Institute.
  • [27]. Mycielska-Dowgiałło, E. (2007). Research methods for textural features of clastic deposits and the significance of interpretational results. In E. Mycielska-Dowgiałło & J. Rutkowski (Eds.), Research into the textural features of Quaternary sediments and some dating methods (pp. 95-180). Warszawa: The Family Alliance School of Higher Education Press (in Polish).
  • [28]. Mycielska-Dowgiałło, E. & Ludwikowska-Kędzia M. (2011). Alternative interpretations of grain-size data from Quaternary deposits. Geologos 17(4): 189-203. D0I:10.2478/ v10118-011-0010-9.
  • [29]. Pawłowski, S. (1922). Morphological characteristics of Polish coast. Poznań: PSS (in Polish).
  • [30]. Pilarski, M., Wójcik R., Biernacik D., Filipiak J., Jakusik E. et al. (2011). Climatic conditions. In M. Miętus & M. Sztobrym (Eds.), The Polish coastal zone of the Baltic Sea - selected environmental issues from 1986-2005 (pp. 31-34). Warszawa: IMWM (in Polish).
  • [31]. Racinowski, R., Szczypek T. & Wach J. (2001). Presentation and interpretation of the research results on the granulation of quaternary sediments. Katowice: Silesia Univ. Publ. (in Polish).
  • [32]. Reading, H.G. & Collinson J.D. (1996). Clastic coasts. In H. G. Reading (Ed.), Sedimentary Environments: processes, facies and stratigraphy (pp. 154-228). Malden/Oxford/Victoria: Blackwell Science.
  • [33]. Rosa, B. (1963). The morphological development of the Polish coast in the light of former coastline forms. Acta Soc. Sci. Torun. 5 (in Polish).
  • [34]. Rucińska-Zjadacz M. & Rudowski S. (2009). Underwater slope relief of Cape Hel. Oceanological and Hydrobiological Studies XXXVIII, Suppl. 1: 111-119.
  • [35]. Rudowski, S. (1962). Microforms of the shore zone. Acta Geologica Polonica 4: 541-579 (in Polish, English summary).
  • [36]. Rudowski, S. & Wodzinowski T. (2005). The bottom and shore structures in the Jastrzebia Góra-Władysławowo region in light of the teledetection registration and a problem of possibility supply of the bed load to Hel Sandbar. In J. Cyberski (Ed.), State and the threat of the Hel Peninsula (pp. 191-198), Gdańsk: Gdańsk Scientific Society (in Polish, English summary).
  • [37]. Rudowski, S., Hac B., Gajewski Ł, Łęczyński L., Nowak J. et al. (2009). Sand barriers: Disappearing resources; the Hel Peninsula case. In Inter. Conf. Climate Change, 25-28 May 2009 (p. 128). Szczecin, Poland.
  • [38]. Stachurska, B. (2012). Analysis of changes in the position of the Baltic-side coast of Hel Peninsula based on aerial photographs from the years 1947-1991. Marine Engineering and Geotechnics 4: 541-552.
  • [39]. Tomczak, A. (1995). Relief, geology and evolution of the Hel Spit. Journal of Coastal Research, Spec. Issue 22: 181-185.
  • [40]. Tomczak, A. (2005). Some problems from the geological past and future of the Hel Peninsula. In J. Cyberski (Ed.), State and the threat of the Hel Peninsula (pp. 13-58), Gdańsk: Gdańsk Scientific Society (in Polish, English summary).
  • [41]. Uścinowicz, Sz. (2003). Relative sea level changes, glacio-isostatic rebound and shoreline displacement in the Southern Baltic. PGI Special Papers 10: 1-79.
  • [42]. Wunche, H. (1904). Studies on the Hel Peninsula. Dresden: C. Heinrich Print (in German).
  • [43]. Zawadzka-Kahlau, E. (1999). Development tendencies of the Polish south Baltic coast. Gdańsk: Gdańsk Scientific Society.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-f8576c4e-a57c-40cb-bec8-1d251e75c0df
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