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Natural and anthropogenic transformations of the natural environment in the "Kępa Redłowska" reserve

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EN
The "Kępa Redłowska" reserve is located in the southern part of Kępa Redłowska. The location of the reserve is quite unique. Its eastern border runs along the coastline of the Baltic Sea, while on the other sides it is surrounded by highly urbanized districts of Gdynia. Its coastal location means that it is exposed to natural factors that operate in the coastal zone, whereas its urban surroundings are a threat to the natural environment through more or less controlled human activity. The landscape of the reserve owes its attractiveness mainly to the cliff coast it encompasses. Diversified geological structure of this area, both in terms of lithology and age, combined with progressive erosion, causes a continuous change in its appearance. It is this part of the reserve that is most exposed to the destructive activity of natural factors, mainly coast erosion as well as aeolian processes. The intensity of these processes is closely related to climate changes over the centuries, e.g. a significant reduction in the number of winters, during which there is ice cover in the shore zone means that cliffs are not protected against erosion by winter storms. A spectacular effect of winter storms in this area was a large landslide in the southern part of the cliff on February 15, 2018. The retreat of cliffs is a common phenomenon, however observations in recent decades clearly indicate its acceleration. The remaining part of the reserve area, not directly connected with the shore zone, is subjected to continuously growing anthropopressure. As mentioned above, the "Kępa Redłowska" reserve is located in Gdynia. The expansion of the Redłowo district has resulted in the housing development being located directly adjacent to the eastern border of the reserve. An additional element of anthropopressure is the creation of interpretive trails and tourist routes within the reserve. On the one hand, this is an attempt to "channel" tourist traffic in this area, on the other hand, it causes an increase in tourist traffic with all the negative phenomena associated with it, mainly for vegetation. Human interference in the reserve began already at the end of the 1930s. At that time, military facilities, such as bunkers and artillery positions, were built there. This process continued uninterrupted until the 1960s. Post-military objects are on the one hand an attraction for tourists, on the other hand they attract the attention of various types of seekers of military remnants who, during their explorations, cause additional damage to the surface of the area and vegetation.
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5--14
Opis fizyczny
Bibliogr. 26 poz., rys.
Twórcy
autor
  • Institute of Geography and Regional Development, Faculty of Earth Sciences and Environmental Management, University of Wrocław, pl. Uniwersytecki 1, 50-137 Wrocław, Poland
Bibliografia
  • Augustowski, B., 1972. Niziny Nadmorskie (Pobrzeże Bałtyckie). In: Galon, R. (Ed.), Geomorfologia Polski, t. 2. PWN, Warszawa, 111–128.
  • Augustowski, B., 1977. Pomorze. PWN Warszawa, 350 pp.
  • Basiński, T., 1963. Protective buildings on the Polish Baltic coast (Budowle ochronne na polskim wybrzeżu Bałtyku). The materials for the monograph of Polish seashore, IBW PAN, Gdańsk, 4–220 (in Polish).
  • Bohdziewicz, L., 1961. Cliff of the isolated moralne plateau at Redowo. In: Galon, R. (Ed.), From the Balic tothe Tatras, part 1, North Poland, PWN Łódź, 56–58.
  • Buliński, M., Przewoźniak, M., 1996. Monograph of the nature reserve “Kępa Redłowska” (Monografia rezerwatu przyrody „Kępa Redłowska”). In: Przewoźniak, M. (Ed.), Coastal nature reserves, Materials for the natural monograph of the Gdańsk region. Wydawnictwo Gdańskie, Gdańsk, 5–77 (in Polish).
  • Dziadziuszko, Z., Malicki, J., 1993. Growth of risk of stormsurge flooding on the Polish coast. Reasons and history of the January and February storm surges. Gazeta Obserwatora IMGW, Warszawa, 4–5, 6–12.
  • Goc, M., 1996. State of fauna, (Stan fauny), Materiały do monografii. In: Przewoźniak, M. (Ed.), Coastal nature reserves, Materials for the natural monograph of the Gdańsk region. Wydawnictwo Gdańskie, Gdańsk, 62–64.
  • Jarosz, E., Kowalewski, M., 1993. The wind waving motion. In: Korzeniewski, K. (Ed.), Zatoka Pucka. Wydawnictwo Uniwersytetu Gdańskiego, 147–159 (in Polish).
  • Kondracki, J., 1998. Geography of Poland (Geografia regionalna Polski). PWN, Warszawa, 464 pp. (in Polish).
  • Mielczarski, A., 1999. Postlitorina. Relative sea-level changes in the Gulf of Gdańsk in the light of new researches. Peribalticum VII. Z problematyki badawczej wybrzeża południowo bałtyckiego. Gdańsk, 21–40.
  • Mojski, J.E. (Ed.), 1988. Zasady polskiej klasyfikacji I terminologii nomenklatury stratygraficznej czwartorzędu. Instrukcje i Metody Badań Geologicznych PIG 47, 3–63.
  • Musielak, S., 1971. The deep-seated Geological Structure of the Region of Gdańsk (Wgłębna budowa geologiczna Regionu Gdańskiego). Zeszyty Naukowe UG. Geografia 1. Wydawnictwo Uniwersytetu Gdańskiego, 95–126 (in Polish).
  • Nowak, P., 2018. The cliff in Orłowo disappears, but it does not die (Klif w Orłowie znika, ale nie ginie). 30 Dni, 1–2, 40–42 (in Polish).
  • Ordinance No 49/2001 of the Pomeranian Governor (Voivod) of 23 March 2001 on the recognition as a nature reserve of the area on Kępa Redłowska in Gdynia (Official Journal of 2001 No 27, point 283) (in Polish).
  • Ordinance of the Pomeranian Governor of 29 July 1938 on the protection of nature formations in the area of Kępa Redłowska in Gdynia (Official Journal No 23, point 271) (in Polish).
  • Pawłowski, S., 1922. Morphological characteristics of the Polish coast (Charakterystyka morfologiczna wybrzeża polskiego), Skład Główny w KsięgarniaGebethnera i Wolffa, Poznań, 25 pp. (in Polish).
  • Pazdro, Z., 1960. Geological structure of the Gdańsk region. Rocznik Polskiego Towarzystwa Geologicznego XXIX, 4, 337–346 (in Polish).
  • Pępek, A., Olszak, I.J., 1995. The Quaternary of the Kępa Redłowska cliffs (Czwartorzęd klifów Kępy Redłowskiej). In: Florek, W. (Ed.), Geologia i geomorfologia pobrzeża i południowego Bałtyku 2. WSP, Słupsk, 153–158 (in Polish).
  • Regulation No 6/2010 of Regional Director for Environmental Protection in Gdańsk of 7 April 2010 on establishing a protection plan for the “Kępa Redłowska” nature reserve (Official journal of 2010 No 97, point 1897).
  • Rosa, B., 1963. Morphological development of the Polish coast in the light of old shore forms, Studia Societatis Scientiarum Torunensis, Sectio C, Toruń, 5 (in Polish with English summary).
  • Rosa B., 1994. On the changes in the level of the Southern Baltic and the urgent need for further studies in the field. In: Rosa, B. (Ed.), Peribalticum VI , GTN Gdańsk, 95–120.
  • Subotowicz, W., 1982. The lithodynamics of the Polish sea coastal cliffs, Wyd. PAN, Wrocław–Warszawa–Kraków–Gdańsk–Łódź, 1–152 (in Polish).
  • Wodziczko, A., 1929. Recognition of the Kępa Redłowska forests as a reserve (Uznanie lasów Kępy Redłowskiej za rezerwat). Ochrona Przyrody 9 (97), 125–127 (in Polish).
  • Woźniakowski, A, 2017. Fortifications of Gdynia and the surrounding area (Fortyfikacje Gdyni i okolic). Tourist map. Wydawnictwo Casamata, Gdynia (in Polish).
  • Zawadzka-Kahlau, E., 1994. Determination of changes of South Balticspits and cliffs. Bulletin Maritime Institute, 21, 41–59.
  • Zawadzka-Kahlau, E., 1999. Trends in South Baltic Coastal Development during the Last Hundred Years. Peribalticum VII, 115–136.
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2020).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-fca098b8-5cf4-45b3-a93d-ce5a6349ef39
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