Kurub
Shield in Ethiopia
Key Facts
Elevation
625 m (2,051 ft)
Type
Shield
Location
11.880°, 41.208°
Region
Afar Rift Volcanic Province
Rock Type
Basalt / Picro-Basalt
Tectonic Setting
Rift zone
Location
Loading map...
Overview
The small Holocene shield volcano, also known as Kurub Koma, Kurub Koba, or Curub, lies in the Saha Plain, SE of the Manda Hararo complex in the South Danakil region. The easternmost lava flow was potassium-argon dated at about 0. 3 million years.
Wind-blown sand fills the summit crater of the very recent basaltic volcano. Initial subaqueous activity occurred along NNW-trending fissures. Fumarolic activity observed in the 1930s was not seen during field work in the 1970s.
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 | Unknown | Historical | Historically active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in Eastern Africa Volcanic Regions
Quick Info
- •Smithsonian ID: 221120
- •Evidence: Evidence Credible
- •Epoch: Holocene
About the Photo
The dark-colored circular area in the center of this Landsat image is the small Holocene Kurub shield volcano. Kurub lies in the Saha Plain, SE of the Manda Hararo complex, the southern margin of which is visible at the far left. Initial subaqueous activity occurred along NNW-trending fissures cutting the basaltic volcano. Fumarolic activity observed in the 1930s was not seen during field work in the 1970s.
NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology).
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.