🌋VolcanoAtlas

Lawu

Stratovolcano in Indonesia

Key Facts

Elevation

3,265 m (10,712 ft)

Type

Stratovolcano

Location

-7.625°, 111.192°

Region

Sunda Volcanic Arc

Rock Type

Andesite / Basaltic Andesite

Tectonic Setting

Subduction zone

Location

Loading map...

Overview

The Lawu volcanic complex includes a deeply eroded volcano to the south joined to a younger edifice to the north considered by van Bemmelen (1949b) to be probably Holocene. No eruptions or dated deposits are known, but it was mapped by Sampurno and Samodra (1997) as Holocene. The southern end of the broad 3-km-long summit of the younger edifice contains eroded crater rims and a lava dome that fed flows 3.

5 km down the S flank. A fumarolic area is also located on the S flank. A small cone with a crater is present on the lower SE flank of the older edifice, ~19 km from the summit.

An event was reported in November 1885 CE, with booms, rumbling sounds, and "ash rain" later in the day; this was similar to a landslide reported in 1978. A major eruption attributed to Lawu in 1752 CE was actually from Kelud volcano.

Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows
  • Lava flows
  • Volcanic bombs and ballistics
  • Lahars and mudflows

Risk Level

Population at RiskModerate
Infrastructure RiskModerate
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Andesite / Basaltic Andesite
Silica Content
Intermediate (57-63% SiO₂)

Tectonic Setting

Subduction zone
Formed by oceanic plate subduction, typically producing explosive eruptions due to water-rich magmas.

Age & Formation

Epoch
Holocene
Evidence
Evidence Uncertain

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent ActivityUnknownHistoricalHistorically active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Normal
No recent activity. Routine monitoring continues.

Nearby Volcanoes in Sunda-Banda Volcanic Regions

Regional Volcanic Activity
The Sunda-Banda Volcanic Regions contains multiple active volcanic systems. Cross-regional magma interactions and tectonic stresses can influence eruption patterns across the entire arc. Monitor regional seismic activity and volcanic alerts.

Quick Info

  • Smithsonian ID: 263260
  • Evidence: Evidence Uncertain
  • Epoch: Holocene

About the Photo

Lawu dominates the skyline east of the city of Surakarta (Solo). This view is from the south, with a white plume rising from a thermal area at the center of the photo. Lawu was constructed to the north of an older complex during the Holocene. A rift valley between the two volcanoes is occupied on the east by several crater lakes.

Photo by J. Matehelumual, 1979 (Volcanological Survey of Indonesia).

Basic Information

This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.