Mousa Alli

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  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 12.47°N
  • 42.4°E

  • 2028 m
    6652 ft

  • 221123
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Mousa Alli.

The Global Volcanism Program has no Weekly Reports available for Mousa Alli.

The Global Volcanism Program has no Bulletin Reports available for Mousa Alli.

Basic Data

Volcano Number

Last Known Eruption

Elevation

Latitude
Longitude
221123

Unknown - Evidence Credible

2028 m / 6652 ft

12.47°N
42.4°E

Volcano Types

Stratovolcano
Caldera
Lava dome(s)

Rock Types

Major
Rhyolite
Trachyte / Trachyandesite
Basalt / Picro-Basalt

Tectonic Setting

Rift zone
Intermediate crust (15-25 km)

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
132
1,148
11,607
201,977

Geological Summary

The Mousa Alli volcanic complex is a large Holocene stratovolcano constructed along the border between Ethiopia, Eritrea, and Djibouti. The 2028-m-high trachytic-to-rhyolitic volcano is the most prominent topographic feature in this area and towers above its neighbor to the SW, Manda Inakir. Rhyolitic lava domes and lava flows are found in the summit region, which is truncated by a caldera.

References

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography.

CNR-CNRS, 1975. Geological Maps of Afar: 1, Northern Afar (1971); 2, Central and Southern Afar (1975). La Celle St Cloud, France: Geotechnip.

De Fino M, La Volpe L, Lirer L, Varet J, 1973. Geology and petrology of Manda-Inakir range and Moussa Alli volcano, central eastern Afar (Ethiopia and TFAI). Rev Geog Phys Geol Dynam, 15: 373-386.

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Varet J, 1978. Geology of central and southern Afar (Ethiopia and Djibouti Republic). CNRS, Paris, 124 p.

Wiart P, Oppenheimer C, 2005. Large magnitude silicic volcanism in north Afar: the Nabro volcanic range and Ma'alalta volcano. Bull Volc, 67: 99-115.

The Global Volcanism Program is not aware of any Holocene eruptions from Mousa Alli. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Mousa Alli page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.


Synonyms

Moussa Alli | Musa Ali | Mussa-ali

Photo Gallery


The chain of pyroclastic cones and lava flows extending diagonally down from the upper-left portion of this Landsat image is the southern portion of the Mousa Alli volcanic complex. The flanks of its neighbor to the SW, Manda Inakir, are visible at the extreme lower left. Prominent faults at the right cut lava flows of the Pliocene-Pleistocene stratoid series of the Afar region.

NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology).
Mousa Alli volcano dominates the right-hand side of this NASA Landsat image and straddles the border between Ethiopia, Eritrea, and Djibouti. This 2028-m-high trachytic-to-rhyolitic volcano is the most prominent topographic feature in this area and towers above its neighbor to the SW, Manda Inakir, visible at the lower left. Yellow-colored basaltic pyroclastic cones and associated lava flows occupy the SE and NW flanks of the rhyolitic summit massif.

NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology).

Smithsonian Sample Collections Database


A listing of samples from the Smithsonian collections will be available soon.

Affiliated Sites

Large Eruptions of Mousa Alli Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
WOVOdat WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.
EarthChem EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).
MODVOLC - HIGP MODIS Thermal Alert System Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. When one is found the date, time, location, and intensity are recorded. MODIS looks at every square km of the Earth every 48 hours, once during the day and once during the night, and the presence of two MODIS sensors in space allows at least four hot-spot observations every two days. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. There is a drop-down list with volcano names which allow users to 'zoom-in' and examine the distribution of hot-spots at a variety of spatial scales.
MIROVA Middle InfraRed Observation of Volcanic Activity (MIROVA) is a near real time volcanic hot-spot detection system based on the analysis of MODIS (Moderate Resolution Imaging Spectroradiometer) data. In particular, MIROVA uses the Middle InfraRed Radiation (MIR), measured over target volcanoes, in order to detect, locate and measure the heat radiation sourced from volcanic activity.