Karang
Stratovolcano in Indonesia
Key Facts
Elevation
1,768 m (5,801 ft)
Type
Stratovolcano
Location
-6.268°, 106.050°
Region
Sunda Volcanic Arc
Rock Type
Andesite / Basaltic Andesite
Tectonic Setting
Subduction zone
Location
Loading map...
Overview
Gunung Karang volcano in westernmost Java was constructed SE of the 15-km-wide Pleistocene Danau caldera. Two craters, Kawah Welirang and Kawah Haji, display fumarolic activity and are found on the eastern flanks, which may be of Holocene age (Bronto 1995, pers. comm.
). The forested andesitic and basaltic volcano is the highest of a group of stratovolcanoes in the Danau caldera area and lies across a low saddle from Pulosari volcano.
Volcanic Hazards & Risk Assessment
Primary Hazards
- Pyroclastic flows
- Lava flows
- Volcanic bombs and ballistics
- Lahars and mudflows
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 | Unknown | Historical | Historically active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in Sunda-Banda Volcanic Regions
Quick Info
- •Smithsonian ID: 263020
- •Evidence: Evidence Uncertain
- •Epoch: Holocene
About the Photo
Karang is the large, circular, forested volcano below and to the left of the center of this NASA International Space Station image (N is to the upper right) is. It is located to the SE of the 15-km-wide Pleistocene Danau caldera visible above the center of the image. There are two craters on the SE flank of Karang volcano, the highest peak in this volcanic region at the western tip of Java.
NASA International Space Station image ISS004-E-10353, 2002 (http://eol.jsc.nasa.gov/).
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.