May 26, 2016 - on Plateau of Bolkar Mountains (Central Taurus). Mustafa Utlu1,Mesut ÅimÅek2, Muhammed Zeynel Ãztürk3. 1İstanbul University, Faculty of Art ...
4th International Geography Symposium 23 - 26 May, 2016 / Kemer, Antalya, TURKEY
Spatial Distribution Characteristic of Karstic Depressions on Plateau of Bolkar Mountains (Central Taurus) Mustafa Utlu1, Mesut Şimşek2, Muhammed Zeynel Öztürk3 1
İstanbul University, Faculty of Art, Department of Geography, İstanbul, TURKEY İstanbul University, Institute of Social Sciences, Department of Physical Geography, İstanbul, TURKEY 3 Niğde University, Faculty of Art and Science, Department of Geography, Niğde, TURKEY 2
Abstract In this study, spatial distribution characteristic of dolines and uvalas developed on plateau composed of Jurassic-Cretase neritic limestone and carbonates where found at west of Bolkar Mountains were analyzed. 30129 karstic depressions were detected in 2558 km2 area through examining of 1/25000 scaled 34 topographic maps. Dolines and uvalas comprise 85.6% and 14.4% of depressions, respectively. All depressions cover 154 km2 areas, in other words 1.17% of the investigation area. Maximum density reach up to 99 depressions/km2 based on 1x1 km grids. 1-5, 5-30, 30 depressions/km2 comprise 30%, 52%, 7% of the investigation area, respectively. Depressions disperse between 1315 m and 2525 m elevations, while 89% of them are located between 1650 and 2350 meters. Correlation between depression density and elevation was found positive (r = 0.96) up to 1900 meters, and a negative correlation (r = -0.91) was found after 1900 meter. A positive correlation (r = 0.86) was also detected between rate of elevation range and number of depression located at same elevation range. However, while rate of elevation range is more than rate of depressions up to 1850 meters and after this altitude level reverse situation is seen. Formation of depression becomes sparse when slope value increases because dolines and uvalas develop on low sloping areas at karstic plateau. For this reason, karstic plateaus covered by dolines and uvalas at The Taurus Mountains are restricted by steep slopes. Negative correlations are found between density and slope value (r= -028) and dissection index (r=-0.29). However, this correlation is not seen on plains covered by alluvium since alluvial cover inhibits superficial dissolution. Key Words: Karstic depression, correlations, spatial distribution, Bolkar Mountains, Central Taurus. Acknowledgements This study was financially supported by the Scientific and Technological Research Council of Turkey (TUBITAK) (Project number: 115Y580).
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4th International Geography Symposium 23 - 26 May, 2016 / Kemer, Antalya, TURKEY
4th International Geography Symposium May 23 - 26, 2016 - Kemer, Antalya, TURKEY
BOOK OF ABSTRACTS ÖZETLER KİTABI
Edited by Recep EFE Isa CUREBAL
ISBN 978-605-66576-0-3
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4th International Geography Symposium 23 - 26 May, 2016 / Kemer, Antalya, TURKEY
International Scientific Advisory Committee Abdalla Abdsalam AHMED - Water Resources, UNESCO Habib AHMAD - Hazara University, Pakistan Mehmet ARSLAN - Al-Farabi Kazakh National University, Kazakhstan Eyüp ARTVİNLİ - Eskişehir Osmangazi University, Turkey Seyed Esmaeil ASGHARPOUR - Islamic Azad University, Iran Ibrahim ATALAY - Mehmet Akif University, Turkey Emin ATASOY - Uludag University, Turkey Dan BALTEANU - Romanian Academy, Romania Gideon BIGER - Tel Aviv University, Israel Stanley D. BRUNN - University of Kentucky, USA Helmut BRÜCKNER - University of Marburg, Germany Eric CORIJN - Vrije Universiteit Brussel, Belgium Andrej ČERNE - University of Ljubljana, Slovenia İsa CUREBAL - Balikesir University, Turkey Tuncer DEMİR - Akdeniz University, Turkey Uğur DOĞAN - Ankara University, Turkey Mimoza DUSHI - University of Pristina, Kosovo Recep EFE - Balikesir University, Turkey A.Evren ERGINAL - Ardahan University, Turkey Abd-Alla GAD - NARSS, Egypt Ibrahim Farida HANUM - Universiti Putra, Malaysia Pua Bar KUTIEL - Ben Gurion University, Israel Darrel MADDY - University of Newcastle, UK Laila MANDI - CNEREE - University Cadi Ayyad, Morocco Lia MATCHAVARIANI- Tbilisi State University, Georgia René MATLOVIČ - University of Presov, Slovakia Ouessar MOHAMED - Institut des Régions Arides, Tunisia Gulnara NYUSSUPOVA - Al-Farabi Kazakh National University, Kazakhstan Takashi OGUCHI - University of Tokyo, Japan Nizar OMRANI - Arid Land Institute, Tunisia Hasan ÖZDEMİR - Istanbul University, Turkey Munir ÖZTURK - Ege University, Turkey Galina N. PARANINA - Herzen State University, Russia Fantina TEDIM - University of Porto, Portugal Aigul TOKBERGENOVA - Al-Farabi Kazakh National University, Kazakhstan Jorge Batlle SALES - University of Valencia, Spain Abdullah SOYKAN - Balıkesir University, Turkey Witold WILCZYNSKI - Pedagogical University of Kraków, Poland
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