The BT. balirang forms two semi-circular craterwalls, whereas the sekincau is a younger eruption-point. the sekincau does not possess an actual cone - shape; it is rather an irregular dome, concicting of andesitic material.
Ketersediaan
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Pusat Sumber Daya Mineral, Batubara dan Panas Bumi - Jln. Soekarno Hatta No. 444, Bandung, Jawa Barat
PMB