Generated by GPT-5-mini| Mount Agung | |
|---|---|
| Name | Mount Agung |
| Other name | Gunung Agung |
| Elevation m | 3142 |
| Prominence m | 3142 |
| Location | Bali, Indonesia |
| Range | Lesser Sunda Islands |
| Coordinates | 8°20′S 115°30′E |
| Type | Stratovolcano |
| Last eruption | 2017–2019 |
Mount Agung is a high-consequence stratovolcano on the island of Bali in Indonesia, rising to about 3,142 metres. It dominates eastern Bali's skyline near the regency capitals of Karangasem Regency and Gianyar Regency and lies within a complex of volcanic centres on the Lesser Sunda Islands. The mountain's eruptions have shaped Balinese history and prompted large-scale evacuations coordinated by agencies such as the Indonesian National Board for Disaster Management and international aviation authorities including the International Civil Aviation Organization.
Mount Agung sits in eastern Bali close to the towns of Amlapura and Rendang and within sight of the Bali Sea and the island of Lombok. The edifice is a classic stratovolcano composed of interbedded andesitic to dacitic lava flows, pyroclastic deposits and lahars, set upon older volcanic and marine sedimentary units of the Bali Basin. The volcano forms part of the Sunda Arc, a volcanic arc above the subduction of the Australian Plate beneath the Eurasian Plate and is related to the magmatic activity that also produced nearby centres such as Batur Caldera and volcanic provinces across the Lesser Sunda Islands. Geothermal manifestations on and around the mountain include hot springs and fumarolic fields that have been investigated by scientists from institutions like the Volcanological Survey of Indonesia and international research groups from universities such as University of Oxford and Massachusetts Institute of Technology.
Historical eruptions of the volcano include a major 1843–1849 eruptive period and the catastrophic 1963–1964 eruption, which ranks among the deadliest 20th-century volcanic events. The 1963 eruption produced voluminous pyroclastic flows and ashfall that impacted communities across Bali and deposited tephra recorded as far as Jakarta and the Flores Sea. Instrumental and geological records show a cycle of long repose punctuated by explosive eruptions: deposits include fall layers, ignimbrites, block-and-ash flows and lahars. The most recent activity began with unrest in 2017, escalating to eruptive episodes in late 2017 and 2018 that generated ash plumes affecting flight operations monitored by the International Civil Aviation Organization and regional airports such as Ngurah Rai International Airport. Studies by researchers from institutions like the Smithsonian Institution's Global Volcanism Program and the Volcanological Survey of Indonesia have used petrology, geochronology and geophysical monitoring to reconstruct eruption chronology and magma evolution.
Eruptions pose multiple hazards including pyroclastic density currents, ashfall, ballistic projectiles, lava dome collapse and lahars exacerbated by tropical rainfall from systems such as the Australian monsoon and Indian Ocean Dipole. Major societal impacts arise from ash's effects on human health, agriculture and aviation; the 1963 event caused international humanitarian responses involving organizations like the Red Cross and prompted research at institutions including the London School of Hygiene & Tropical Medicine. Monitoring networks employ seismic arrays, geodetic surveys using GPS provided by agencies such as the Agency for the Assessment and Application of Technology (BPPT) and satellite remote sensing from platforms like Landsat and Sentinel-2. Alert levels and evacuations are coordinated by the Volcanological Survey of Indonesia and local administrations in collaboration with the Indonesian National Board for Disaster Management and international partners including the United Nations Office for Disaster Risk Reduction.
The mountain's slopes host montane forest ecosystems with biodiversity affinities to the Wallacea biogeographic region, supporting flora and fauna studied by researchers from Bogor Agricultural University and conservation organizations such as BirdLife International. Soils derived from volcanic deposits support rice terraces and agroforestry around villages like Tirta Gangga and Sidemen, linking livelihood systems to volcanic fertility documented by agricultural scientists at institutions like University of Sydney. Culturally, the volcano is sacred to Balinese Hindu communities; the mother temple of Besakih, known as Pura Besakih, and other shrines on its flanks are focal points for pilgrimages and ceremonies tied to temples such as Pura Luhur Batukaru and festivals observed in regencies including Karangasem Regency. Historical narratives and artistic depictions in sources linked to museums like the National Museum of Indonesia reflect the mountain's central role in Balinese identity and ritual practice.
The volcano attracts climbers, pilgrims and tourists visiting cultural sites like Pura Besakih, natural attractions such as Tirta Gangga water palace and neighbouring volcanoes including Mount Batur. Trekking routes typically start from villages in Kubu and Selat and ascend via trails maintained by local guides organized through cooperatives and agencies registered with the Ministry of Tourism (Indonesia). Access varies with volcanic alert levels; airports including Ngurah Rai International Airport and ferry crossings to Lombok and the Gili Islands serve as gateways for visitors. Research on sustainable tourism management has involved partnerships between regional governments like Provincial Government of Bali and academic groups from Udayana University and international NGOs focused on cultural heritage and conservation.
Category:Volcanoes of Bali Category:Stratovolcanoes Category:Mountains of Indonesia