Inielika
Complex in Indonesia
Key Facts
Elevation
1,559 m (5,115 ft)
Type
Complex
Location
-8.730°, 120.980°
Region
Sunda Volcanic Arc
Rock Type
Andesite / Basaltic Andesite
Tectonic Setting
Subduction zone
Location
Loading map...
Overview
Inielika is a broad, low volcano in central Flores Island that was constructed within the Lobobutu caldera. The complex summit contains ten craters, some of which are lake filled, in a 5 km2 area north of the city of Bajawa. The largest of these, Wolo Runu and Wolo Lega North, are 750 m wide.
A phreatic explosion in 1905 formed a new crater, and was the volcano's only eruption during the 20th century. Another eruption took place about a century later, in 2001. A chain of Pleistocene cinder cones, the Bajawa cinder cone complex, extends southward to Inierie.
Volcanic Hazards & Risk Assessment
Primary Hazards
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 25 years ago | Recent | Recently active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in Sunda-Banda Volcanic Regions
Quick Info
- •Smithsonian ID: 264090
- •Evidence: Eruption Observed
- •Epoch: Holocene
About the Photo
Two of the many summit craters of Inielika can be seen in the left foreground. It is a broad, low volcano in central Flores Island that was constructed within the Lobobutu caldera. The complex summit includes ten craters, some of which contain lakes. A phreatic explosion that formed a new crater in 1905 was the volcano's only eruption during the 20th century. Inierie volcano is the prominent peak on the right horizon.
Photo by Volcanological Survey of Indonesia.
Authority Sources
Related Volcanoes
Basic Information
This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.