Environmental monitoring in the Kaklik Cave (Denizli, Turkey)
Affiliation(s)
Department of Biology, Faculty of Sciences and Letters, Celal Bayar University, Manisa, Turkey;.
Department of Biology, Faculty of Sciences and Letters, Celal Bayar University, Manisa, Turkey;.
ABSTRACT
The formation of caves is the special environment of our earth. Caves with dim natural light and lighted hypogean environments, have been found various organism. The Kaklik Cave located tectonic lines and has a very different way of formation when compare with many other same karstic formation caves. The Kaklik Cave is located in the area of Kaklik town in Honaz area and in Denizli province. The cave is one of the 54 cave opened to tourism in Turkey and endanger. In this study the cave climate, hydrol?ogy and biology were studied. The cave has specific species due to this formation, the entrance is wide and open to the sky, that makes the sunlight could go through a very wide area and cause of it is very rich about hydrology, these effects; provide a very high biodiversity to the cave. The cave has very important touristic potential because of the continuously growing travertine, geographical position, availability of access and natural beauties. The wrong artificial lightning badly changes the natural structure of the cave. This artificial lightning causes the biofilm layer and changing on the color of the travertine.
The formation of caves is the special environment of our earth. Caves with dim natural light and lighted hypogean environments, have been found various organism. The Kaklik Cave located tectonic lines and has a very different way of formation when compare with many other same karstic formation caves. The Kaklik Cave is located in the area of Kaklik town in Honaz area and in Denizli province. The cave is one of the 54 cave opened to tourism in Turkey and endanger. In this study the cave climate, hydrol?ogy and biology were studied. The cave has specific species due to this formation, the entrance is wide and open to the sky, that makes the sunlight could go through a very wide area and cause of it is very rich about hydrology, these effects; provide a very high biodiversity to the cave. The cave has very important touristic potential because of the continuously growing travertine, geographical position, availability of access and natural beauties. The wrong artificial lightning badly changes the natural structure of the cave. This artificial lightning causes the biofilm layer and changing on the color of the travertine.
Cite this paper
Ulcay, S. , Kurt, O. , Akcora, C. and Ozturk, M. (2012) Environmental monitoring in the Kaklik Cave (Denizli, Turkey). Natural Science, 4, 159-165. doi: 10.4236/ns.2012.43023.
Ulcay, S. , Kurt, O. , Akcora, C. and Ozturk, M. (2012) Environmental monitoring in the Kaklik Cave (Denizli, Turkey). Natural Science, 4, 159-165. doi: 10.4236/ns.2012.43023.
References
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[1] Ozansoy, C. and Mengi, H. (2006) Ma?ara bilimi ve ma?arac?l?k. Tübitak Popüler Bilim Kitaplar?, Ankara. [2] MTA (GDMRE) (2011) 2011 Y?l? ilk alt? ayl?k faaliyet raporu, Jeoloji Etütleri Dairesi Ba?kanl???, Ankara. [3] Guney, E. (2011) Yerbilimi 2, Jeomorfoloji, Literatür Yay?nlar?, Istanbul. [4] Nazik, L. (2008) Ma?aralar?n ara?t?r?lma, koruma ve kullan?m ilkeleri. MTA, Yerbilimler Kültür Serisi 2, Ankara. [5] Genc, S. and Kutlu, H. (1999) Burdur ?nsuyu ma?aras? mimari ve elektrik projesi, MTA ?zalit Ar?ivi, Ankara. [6] Turkunal, S. and Ozenci, M. (1958) Antalya Alanya Damlata? ma?aras? civar?na ait krokiler, MTA ?zalit Ar?ivi, Ankara. [7] Karadeniz, V., Celikoglu, S. and Akpinar, E. (2009) G?kg?l ma?aras? ve turizm potansiyeli. Turkish Studies Lit- erature and History of Turkish, 4, 1621-1641. [8] Dogu, A.F., Cicek, ?., Gurgen, G. and Tuncel, H. (1999) Ay?ini ma?aras? (Kayseri), Ankara üniversitesi Dil ve Tarih, Ankara, 335-345. [9] Ozbek, O. (2011) ODTü-SAT MADAG Ma?ara dal??? e?itimi program?, Kuru ma?arac?l?k e?itimi, Lecture note. http://www.sat.metu.edu.tr/madagorg/yayinlar/251-onurozbek.pdf [10] Cetin, B. (2007) Kaklik ma?aras?’n?n (Honaz-Denizli) Turizm potansiyeli, Journal of Social Sciences, 7, 225- 239. [11] Nazik, L. (2000) Kaklik ma?aras? Kaklik Denizli Ara?- t?rma Raporu, MTA Rapor Ar?ivi, Ankara. [12] Nazik, L. (2002) Kaklik ma?aras?. http://www.denizce.com/kaklikmagarasi.asp [13] Nazik, L. (2002) Yeralt?ndaki pamukkale: Kaklik ma?aras?. http://www.turkishairlines.com/tr-TR/skylife/archive/tr/2002_7/konu9.htm#1 [14] Dereci, S. (2000) Denizli Kaklik magaras? uygulama projesi, MTA Ozalit Ar?ivi, Ankara. [15] Demirkiran, Z. and Calapkulu F., (2001) Kaklik-Kocaba? (Denizli) travertenlerinin litolojik, morfolojik ?zellikleri ve s?n?flamas?, Türkiye III. Mermer Sempozyumu, Bildiriler Kitab?, Afyon. [16] Ozkul, M., Varol, B. and Alcicek, M. C. (2002) Depositional environments and petrography of Denizli travertines, Mineral Research and Exploration Bulletin, 125, 13-29. [17] Elci, L., Kartal, A.A. and Soylak, M. (2008) Solid phase extraction method for the determination of iron, lead and chromium by atomic absorption spectrometry using Amberite XAD-2000 column in various water samples, Jour- nal of Hazardous Materials, 153, 454-461. doi:10.1016/j.jhazmat.2007.08.075