@article{oai:nichibun.repo.nii.ac.jp:00000344,
 author = {NARUSE, Toshiro and KITAGAWA, Hiroyuki and MATSUBARA, Hisashi},
 journal = {Nichibunken Japan review : bulletin of the International Research Center for Japanese Studies},
 month = {Jan},
 note = {Alluvial fans developed and lake levels fluctuated several times according to the climatic changes during the last 24,000 years.  Alluvial fans developed in Lake Tuz in the cold, pluvial periods of increasing discharge during the Holocene around 5000 yr BP. and after 3500 yr BP. Lake expansion occurred at 23 ka., 18-20 ka., 14-15 ka., and 11ka. over the last 24,000 years in the Konya Basin.  These expansions, shown by the raised lake terraces and beach ridges, were mainly due to cold and pluvial climatic changes.  The lake level rose in the colder climate during marine oxygen isotope stage 2 and the Younger Dryas period.  The lake level reached its highest level of 1013 to 1014 m during the last Glacial maximum before 18 ka.},
 pages = {173--192},
 title = {<FEATURE ARTICLES: Changes in the Environment and Civilizations in Turkey and Syria>Lake level changes and development of alluvial fans in lake tuz and the konya basin during the last 24,000 years on the anatolian plateau, Turkey},
 volume = {8},
 year = {1997}
}