Click on the photo to enlarge
Mount Batur (Gunung Batur) is an active volcano located at
the center of two concentric calderas north west of Mount Agung, Bali,
Indonesia
The south east side of the larger 10×13 km caldera contains a
caldera lake
The inner 7.5 kilometer wide caldera, which was formed during
emplacement of the Bali (or Ubud) ignimbrite, has been dated at about 23,670
and 28,500 years ago
The southeast wall of the inner caldera lies beneath Lake
Batur
The Batur stratovolcano has produced vents over
much of the inner caldera, but a NE-SW fissure system has localized the Batur
I, II, and III craters along the summit ridge
Historical eruptions have been
characterized by mild-to-moderate explosive activity
sometimes accompanied by
lava emission
Basaltic lava flows from both summit and flank vents have
reached the caldera floor
and the shores of Lake Batur in historical time
The
caldera contains an active, 700-metre-tall stratovolcano rising
above the
surface of Lake Batur
The first historically documented eruption of Batur was
in 1804, and it has been
frequently active since then
The substantial lava
field from the 1968 eruption is visible today when viewed from Kintamani, a
town that stradles the southwest ridge of the greater caldera
The caldera is
populated and includes the four main villages of Kedisan, Songan,
Trunyan and
Toya Bungkah
The locals largely rely on agriculture for income but tourism has
become increasingly popular due to the relatively straightforward trek to the
summit of the central crater
The lake Danau Batur is the largest crater lake
on the island of Bali
and is a good source of fish
On September 20, 2012
UNESCO has made Mount Batur Caldera
a part of the Global Geopark Network
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