Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol. 17, 2008, pp. 497–541. Copyright ©TÜB‹TAK First published online 09 January 2008 Timing of the Quaternary Elaz›¤ Volcanism, Eastern Turkey, and its Significance for Constraining Landscape Evolution and Surface Uplift AL‹ SEYREK1, ROB WESTAWAY2, MALCOLM PRINGLE3, SEMA YURTMEN4, TUNCER DEM‹R5 & GEORGE ROWBOTHAM6 1 Department of Soil Science, Harran University, TR–63300 fianl›urfa, Turkey 2 Faculty of Mathematics and Computing, The Open University, Eldon House, Gosforth, Newcastle-upon-Tyne NE3 3PW, UK (E-mail:
[email protected]) [Also at: School of Civil Engineering and Geosciences, Newcastle University, Newcastle-upon-Tyne NE1 7RU, UK] 3 Scottish Universities’ Environmental Research Centre, Rankine Avenue, East Kilbride, Glasgow G75 0QF, UK [Present address: Laboratory for Noble Gas Geochronology, Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Building 54 TR–1013, Cambridge, MA 02139 TR–4307, USA] 4 Department of Geology, Çukurova University, TR–01330 Adana, Turkey [Present address: 41 Kingsway East, Westlands, Newcastle-under-Lyme, Staffordshire, ST5 5PY, UK] 5 Department of Geography, Harran University, TR–63300 fianl›urfa, Turkey 6 School of Earth Sciences and Geography, Keele University, Keele, Staffordshire ST5 5BG, UK Abstract: The eastern part of the Anatolian plateau in eastern Turkey has experienced dramatic landscape evolution in the Late Cenozoic, surface uplift having been associated with the disruption of former lake basins and the development of the modern high-relief landscape, incised by the upper reaches of the River Euphrates and its major tributary, the Murat. Overall, the altitude of the plateau decreases gradually westward, and it has been assumed that uplift on any given timescale has varied regionally in a similar manner.