Wolfgang's photos with the keyword: indonesia

The Balinese Legong dancing girl not only move their body but she's "dancing" with her eyes too.

Three young worshippers sitting in front of a temple for celebrating on the Odalan festival. Its a pleasure to join the local people doing their festivals. This photo was captured during my visit on Bali in 2001 with a CANON A-1 camera and a KODAK Ektachrome 50 ASA slidefilm. Scanned with a NIKON CoolScan V ED.

Bali is an island of temples. The Department of Religion has cataloged at least eleven thousand temples - small and large, local and regional. The Balinese call a shrine palinggih, which simply means "place" or "seat" and refers to any sort of temporary or permanent place toward which devotions and offerings are made. In no case is the shrine itself considered sacred; the shrine exists or is built as a residence for sacred, or holy, spirits - either ancestors or Hindu deities. Balinese temples are not closed buildings, but rectangular courtyards open to the sky, with rows of shrines and altars dedicated to various gods and deities. The gods are not thought to be present in the temples except on the dates of the temple's festivals, and therefore the temples are usually left empty. On festival days the congregation of each temple assembles to pray to and entertain the visiting deities.

The historically active Mount Batur (Gunung Batur) is 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 SE wall of the inner caldera lies beneath Lake Batur; Batur cone has been constructed within the inner caldera to a height above the outer caldera rim. 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.