Kutum Volcanic Field
Volcanic field in Sudan
Key Facts
Elevation
1,779 m (5,837 ft)
Type
Volcanic field
Location
14.570°, 25.850°
Region
Southeast Sahara Volcanic Province
Rock Type
Basalt / Picro-Basalt
Tectonic Setting
Intraplate
Location
Loading map...
Overview
The basaltic Kutum volcanic field, in the northern Darfur area of western Sudan, is located SW of the larger Meidob volcanic field. As with other Saharan volcanic fields, Kutum (also known as the Tagabo Hills or Berti Hills) contains very well-preserved cones, lava flows, and explosion craters. They were considered to be of late-Pleistocene or even Holocene age (Almond, 1974).
Franz et al. (1997), however, assigned only Tertiary age ranges for rocks from Tagabo Hills.
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 Northern Africa Volcanic Regions
Quick Info
- •Smithsonian ID: 225040
- •Evidence: Evidence Uncertain
- •Epoch: Holocene
About the Photo
The scattered cones of the Kutum basaltic volcanic field (lower left) in the northern Dafur area of western Sudan are located SW of the larger Meidob volcanic field (top). As with other Saharan volcanic fields, Kutum (also known as the Tagabo Hills) contains very well-preserved cones, lava flows, and craters, although their ages are not well constrained.
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.