Mount Tangkuban Perahu

 Tangkuban perahu is one of volcano in West Java, 25 kilometers north of Bandung direction of Lembang. Its location is in between Sagalaherang village, Sagalaherang district, Subang regency and Cikole village, Lembang district, Bandung regency. This volcano offers many places to see and explore. It is a popular tourist attraction where tourists can hike or ride to the edge of the crater to view the hot water springs and boiling mud up close, and buy eggs cooked on the hot surface.
When seen from Bandung, Mt. Tangkuban Perahu has a distinctive shape, like an upside down boat.

Tangkuban Perahu means, in fact, "up-turned boat" This peculiar shape has stimulated the fantasy of the Sundanese people from early times as expressed in the Legend of Sangkuriang. Geologically, Mt. Tangkuban Perahu has played a significant role in the development of Parahyangan highlands.
angkuban Perahu is a volcano with three craters into which areas tourists can walk through. These three craters are: Kawah Ratu ("Queen Crater"), Kawah Domas ("Domas Crater"), and Kawah Upas ("Upas Crater")

  

Tourists can go down into the Domas Crater where exist many hot geysers in which they can boil eggs. Though the mountain appears peaceful, mild eruptions occurred in 1969, when Kawah Ratu spewed ash and barrages 500 m high. As recently as September 1992 it was closed to the public for a few days because unusually high seismic activity leads volcanologist to fear a new eruption. On the mountain's northern flank is an area called Death Valley, so named for its frequent accumulation of poisonous gases.

Kawah Ratu, which means "Queen's Crater", is today just a big gray hole which sometimes has a pool of water at its center. Poisonous gases sometimes accumulate in Kawah Ratu, thus making it somewhat of a risk to descend to the crater floor. Beyond the saddled shaped depression on the far side of Kawah Ratu is the still active Kawah Upas, the oldest crater on the mountain. On the very far western cliff you see a spot where all vegetation has been destroyed by constantly rising sulphurous vapors. On the crater walls, note the various layers of material consisting of rock, sand, and pebbles. Overtime, new craters have formed again and again in a rather consistent shift from west to east. The most well known of these is the Domas crater, but also there are other smaller ones in jungle on the mountain's northeastern flank.