Effects On The Processes In The Göksu Delta, Mersin-Turkey

The Göksu Delta, located on the Mediterranean coast in the South Anatolia, is the most significant wetland both in Turkey and Eastern Mediterranean region. The delta environments present suitable reproduction and living conditions for large numbers of continental migratory birds and aquatic species under protection. The eastern shoreline of the delta has been retreating for the last fifty years, whereas recent mouth of the delta progrades toward the gorge of the lagoon. In addition, the lagoons are filled by deposits of crevasse splay, dune and barrier islands deposits by aeolian effects. Dynamic processes in the delta environment were investigated in detail, to explain the causes of retrograding and prograding of the shoreline of the delta and to find possible solutions. According to the data obtained, the natural fluvial system, the shoreline dynamics, and the aeolian processes in the delta have been changed by the anthropogenic effects. The persistence of the variation of the shoreline will cause significant ecological disruption of the delta.

___

  • Çetin, H., Bal, Y. and Demirkol, C., 1999. Engineering and environmental effects of coastline changes in Turkey, northeastern Mediterranean. En- vironmental and Engineering Geosciences, Vol. 3 pp. 315-330.
  • Ediger, V., Okyar, M. and Ergin, M., 1993. Seismic stratigraphy of the fault controlled submarine canyon/valley system on the shelf and upper slope of Anamur Bay, northeastern Mediter- ranean Sea. Mar. Geol., 115, 129-142.
  • Erdem, O. 1995 Turkey's bird paradises. Green Series: 5, Publication of the Ministry of Environ- ment, General Directorate of Environmental Protection, Ankara, Turkey.
  • Erinç, S. 1978. Changes in physical environments in Turkey since the end of the last glacial In: (W.C. Brice, Ed.), The environmental History of the Near and Middle East since the last ice Age Academic press, London, pp. 87-108.
  • Erol, O. 1991. Impacts of sea-level rise on Turkey, International Sea-Level Rise Studies Project. Institute of Marine and Coastal Sciences Rutgers-The State University of New Jersey, New Brunswick, USA. , 1993. Türkiye kýyýlarýndaki baðýl deniz düzeyi deðiþmeleri ve bunun Göksu Deltasý ile diðer deltalarýn evrimine etkisi. Uluslararasý Göksu Deltasý Çevresel Kalkýnma Semineri Bildiri Me- tinleri, Doðal Hayat Koruma Derneði, Istanbul.
  • Gedik, A., Birgili, S., Yýlmaz, H. and Yoldaþ, R. 1979. Mut-Ermenek-Silifke yöresinin jeolojisi ve petrol olanaklarý. Türkiye Jeol. Kur. Bült. 22, 7-26.
  • Gökten, E. 1976. Silifke yöresinin temel kaya birimleri ve Miyosen stratigrafisi. Türkiye Jeol. Kur. Bült. 19, 117-126.
  • Gülkal, O. 1992. Göksu Deltasý'nýn doðal ve kültürel potansiyelinin belirlenmesi ve kullanýmlar yö- nünden deðerlendirilmesi. C.U. Fen Bilimleri Enst. Yüksek Lisans tezi (unpublished) Adana- Türkiye.
  • Keçer, M. 2001. Göksu Deltasý'nýn (Mersin) jeomor folojik evrimi ve güncel akarsu-deniz-rüzgar süreçlerinin kýyý çizgisinde yaptýðý deðiþiklikler. MTA Raporu No: 10468. (unpublished) Ankara.
  • Maltby, E. 1991. Wetland management goals: wise use and conservation. Landscape and Urban Planning, 20, 9-18.
  • MTA. 2002. 1/500, 000 ölçekli Türkiye Jeoloji Hari- talarý, Adana Paftasý. Maden Tetkik ve Arama Genel Müdürlüðü yayýnlarý. Ankara, Türkiye
  • Okyar, M. and Ediger, V. 1998. Göksu Deltasý'nýn Kuvaterner jeolojisinin sismik yöntemlerle ince- lenmesi alt projesi sonuç raporu. ODTU Deniz Bilimleri Enst. Erdemli-Ýçel.
  • Uslu, T. 1993. Göksu Delta'sýnda kýyý kumul yönetimi. Uluslararasý Göksu Delta'sý çevresel kalkýnma semineri bildiri metinleri. Doðal Hayatý Koruma Cemiyeti-Ýstanbul.
Maden Tetkik ve Arama Dergisi-Cover
  • ISSN: 0026-4563
  • Yayın Aralığı: Yılda 3 Sayı
  • Başlangıç: 1950
  • Yayıncı: Cahit DÖNMEZ