The volcano was constructed during the Pleistocene-Holocene age. The mountain has a large caldera, called Lam Teuba. A smaller 8×6 km caldera is within the Lam Teuba caldera. The volcano contains several hills: sedimentary hills, old volcano hills, a volcanic cone and peneplain area. The volcanic cone was formed by lava and pyroclastic flows. There are three craters. The Tanah Cempago crater is easily recognized, while the other two are covered with vegetations.
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