655 
lated south of first 
)y WNW-ESE and 
t lavas also erupted 
in the second stage, 
ression can be seen, 
formation of south 
ctonic pattern, one 
ind earthquake re- 
t of the area. 
Figure 4. Landsat geological-geomorphological map 
E XPLANATION 
The oldest andesitic rocks (Early Upper Miocene) 
Old basaltic lavas (Late Upper Miocene) 
Relatively middle aged basaltic lavas 
(Pliocene - Pleistocene) 
Recent basaltic lavas (Holosen) 
Neogen Areas 
Quaternary, fluviátil deposits 
Metamorphic rocks of Menderes Massif 
Limestone plateaus in Neogen rocks 
Demirköprü dam lake 
o Young , slightly eroded craters 
o Distinctive volcanic cones 
Older, strongly eroded volcanic centres 
Deep valleys in radial drainage pattern 
Observeble crest lines 
Main streams 
Certain faults (Also proved by the field 
observations) 
Probable faults 
Faults derived by the rows of the craters 
Main settlements 
Direction of the sun illumination 
REFERENCES 
Beekman, H.P. 1964. Geological investigatins near Kula and Borlu: 
MTA report, Ankara. 
Bergo, G. 1964. Kula yoresinin volkanizmasi: MTA raporu, Ankara. 
Bircan, A. et al. 1982. Gediz Graben Sisteminin Jeomorfolojisi ve 
Gen5 Tektonigi: MTA Raporu, Ankara. 
Canet, J. and P. Jaoul. 1946.Geologie de la Region de Manisa— 
Aydm-Kula—Gordes: Rapport de MTA, Ankara. 
Ercan, T. et al. 1977. U§ak yöresinin jeolojisi ve volkanitlerinin 
petrolojisi: MTA Raporu, Ankara. 
Ercan, T. et al. 1980. Kula—Selendi yörelerinin jeolojisi ve volka 
nitlerinin petrolojisi: MTA Raporu, Ankara. 
Erin?, S. 1970. Kula ve Adala arasinda geii9 volkan reliyefi: Ist. 
Üniv. Cog. Ens. Dergisi c. 9, s. 17: 7—22. 
Philippson, A. 1913. Das vulkangebiet von Kula in Lydien, die 
Katakekaummene der Alten: Pet. Georg. Mitt. c.2: 237-241.