Nabro

Photo of this volcano
Google Earth icon
  Google Earth Placemark
  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 13.37°N
  • 41.7°E

  • 2218 m
    7275 ft

  • 221101
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

28 September-4 October 2011

According to NASA's Earth Observatory, satellite images of Nabro acquired on 28 September showed heat from the vent in the central crater, and from an area 1.3 km S of the vent that indicated an active lava flow. A small and diffuse plume rose from the vent. A region of seemingly thicker black ash (that completely covered the sparse vegetation) was noted S of the crater and thinner layers of ash (with some areas of visible vegetation) flanked either side of the region.

Source: NASA Earth Observatory

Index of Weekly Reports


2011: June | July | September

Weekly Reports


28 September-4 October 2011

According to NASA's Earth Observatory, satellite images of Nabro acquired on 28 September showed heat from the vent in the central crater, and from an area 1.3 km S of the vent that indicated an active lava flow. A small and diffuse plume rose from the vent. A region of seemingly thicker black ash (that completely covered the sparse vegetation) was noted S of the crater and thinner layers of ash (with some areas of visible vegetation) flanked either side of the region.

Source: NASA Earth Observatory


13 July-19 July 2011

Based on analyses of satellite imagery, the Toulouse VAAC reported that on 16 July an ash plume from Nabro rose to altitudes below 5.5 km (18,000 ft) a.s.l. A weak eruption detected on 17 July decreased through the day then appeared to have stopped.

Source: Toulouse Volcanic Ash Advisory Centre (VAAC)


29 June-5 July 2011

A satellite image of Nabro acquired on 29 June showed a clear view of the caldera and the vent within the active crater near the middle of the caldera. Lava flows to the W, and within the crater (E and S of the vent), continued to be hot. A brown ash plume rose from the vent and drifted S.

Source: NASA Earth Observatory


22 June-28 June 2011

A satellite image of Nabro acquired on 22 June showed a gas-and-ash plume rising from the caldera and drifting W. According to a news article, the eruption resulted in at least seven deaths, injured many, and displaced thousands in Eritrea, and affected about 5,000 Ethiopians living near the border. Two satellite images acquired on 24 June show the erupting vent, plumes and emissions, and lava flows in detail. One false-color image highlighted hot areas throughout the lava flow and flow front, as well as hot material above the vent. Gas emissions rising from the lava flow were also detected. A natural-color image showed fresh but cooled lava flows in the N part of the caldera. A dark ash plume rose from the vent, and at higher altitudes a plume composed of water vapor and sulfur dioxide drifted W and obscured the active lava flow. Black ash deposits covered the landscape to the S and W. During 22-26 June large amounts of sulfur dioxide in the region continued to be detected by satellite images. Based on analyses of satellite imagery, the Toulouse VAAC reported that during 26-27 June plumes rose to altitudes up to 6.1 km (20,000 ft) a.s.l.

Sources: Toulouse Volcanic Ash Advisory Centre (VAAC); NASA Earth Observatory; NASA Global Sulfur Dioxide Monitoring; Sudan Tribune


15 June-21 June 2011

An eruption from Nabro that started on 12 June continued to produce a plume. Based on analyses of satellite imagery, the Toulouse VAAC reported that during 15-20 June plumes comprised mostly of water and sulfur dioxide rose to altitudes of 6.1-7.9 km (20,000-26,000 ft) a.s.l. Ash was occasionally detected near the volcano. Satellite imagery posted on MODIS Web showed a dark brown ash plume fanning out to the SW on 19 June. A thermal satellite image acquired at night on 19 June revealed a 15-km-long lava flow that had traveled NW. A high-altitude plume, likely rich in water vapor, rose from the erupting vents and a diffuse ash-rich plume drifted SW.

News articles stated that ash had covered a well-known mine that produces edible salt, and had contaminated food and water sources. During 15-16 June several airlines cancelled some domestic and international flights, including in and out of Addis Abeba (Ethiopia), neighboring Djibouti, and Khartoum (Sudan).

Sources: Toulouse Volcanic Ash Advisory Centre (VAAC); NASA Earth Observatory; Addis Fortune; Bloomberg; NASA MODIS Rapid Response System


8 June-14 June 2011

According to the USGS Earthquake Hazards Program, an earthquake swarm was detected during the evening of 12 June on the border of Ethiopia and Eritrea, in the vicinity of Nabro, the most prominent of three volcanoes with large summit calderas aligned in a NE-SW direction SW of Dubbi volcano. The swarm began at 1837 with an M 5.1 earthquake. Several more were detected between M 4.3 and 5.1 over the next few hours. Two M 5.7 earthquakes at depths of 10.1 km and 9.9 km were detected at 2332 on 12 June and 0003 on 13 June, respectively.

The Toulouse VAAC reported that an eruption from Nabro (originally attributed to Dubbi) started between 0000 and 0200 on 13 June. An eruption plume initially rose to altitudes of 9.1-13.7 km (30,000-45,000 ft) a.s.l. then was later detected at altitudes of 6.1-10.7 km (20,000-35,000 ft) a.s.l. during 13-14 June. According to the Eritrean Ministry of Information, ashfall covered hundreds of kilometers and the government evacuated area residents. Witnesses noted that the eruption had started at about 2100 on 13 June. Satellite images that same day showed the plume drifting more than 1,000 km NW, over parts of Sudan. On 14 June a detached ash cloud was detected over southern Israel according to news articles. A plume from Nabro was not obvious on satellite imagery.

Sources: US Geological Survey Earthquake Hazards Program; Toulouse Volcanic Ash Advisory Centre (VAAC); NASA MODIS Rapid Response System; Eritrean Ministry of Information; The Jerusalem Post


Index of Monthly Reports

Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.

09/2011 (BGVN 36:09) First historically observed eruption began 13 June 2011


Contents of Monthly Reports

All information contained in these reports is preliminary and subject to change.

All times are local (= UTC + 3 hours)

09/2011 (BGVN 36:09) First historically observed eruption began 13 June 2011

The first documented historical eruption at Nabro began on 13 June 2011. Nabro lies in a belt of active volcanoes that follows the Red Sea and lies in the Afar Triangle in Southern Eritrea near the border with Ethiopia (figure 1). An earthquake swarm began on 12 June 2011. The swarm included an M 5.1 earthquake in the vicinity of Nabro and early the next day, satellite remote sensing revealed a large ash plume. Tensions remain in the war-ravaged border region of Eritrea and Ethopia; despite an official cease fire, access to the region remains limited. Nabro's eruption delivered large and concentrated SO2 plumes, dropped ash over extensive areas, forced thousands of evacuations, and, according to the Eritrean government, led to fatalities.

Figure 1. Nabro's location in Eritrea and with respect to neighboring countries in East Africa. (Inset) The location of Eritrea in Northeastern Africa along the Red Sea.

Nabro lies in the midst of a chain of volcanoes (figure 2; dashed lines indicate trends of volcanic ranges). Each of the three main volcanoes on figure 2 contains a prominent summit crater or caldera (figures 3 and 4).

Figure 2. A regional map showing Nabro in the volcanic range of the same name (Nabro Volcanic Range, NVR). According to the map's authors (Wiart and Oppenheimer, 2005), the NVR trends with a bearing of N26°E and extends 110 km from the SE margin of the Afar depression at Bara' Ale to islands in the Red Sea. Nabro marks the highest point in the NVR (which the map authors state as 2,248 m, some 30 m higher than the value given in our header, above). Taken from Wiart and Oppenheimer (2005).
Figure 3. Satellite image of the Nabro region taken in February 2000 processed to form a shaded-relief map. When viewed in color, the lower elevations are in green, grading through yellow to red to blue at the highest elevations on the rims of the various nested calderas. Elevation data used in this image was acquired by the Shuttle Radar Topography Mission (SRTM) aboard the NASA Space Shuttle Endeavour. The scale is inexact, and the Eritrean-Ethiopian border is approximate. Courtesy of NASA Jet Propulsion Laboratory.
Figure 4. Astronauts on the NASA International Space Station took this photograph of Nabro on 30 January 2011, showing the pre-eruption morphology of Nabro and some smaller volcanic centers to the S. Nabro's outer crater is ~8 km across and opens to the SSW. Centered within that larger caldera lie two much smaller craters, one inside the other. The inner wall of the caldera has steep sides, some as high as 400 m. Courtesy of NASA Earth Observatory.

Seismic precursors. According to an article in the Ethiopian Journal issued on 13 June 2011, a series of moderate earthquakes struck the Eritrea-Ethiopia border region on the evening of 12 June 2011. The U.S. Geological Survey (USGS) reported a total of 14 light-to-moderate earthquakes in the border area, the two strongest being M 5.7, both centered in Eritrea. The series began at 1837 hours when an M 5.1 earthquake struck ~128 km WNW of Assab, a port city in the southern Red Sea region of Eritrea. It occurred at ~10 km depth and was followed by seven smaller ones, between M 4.5 and M 4.8, during the next 2.5 hours. Those were then followed by earthquakes of M 4.7, 4.8, and 5.0. Soon after, at 2332 hours, the first M 5.7 earthquake struck about 123 km WNW of Assab at a depth of 10 km. It was quickly followed by the second M 5.7 earthquake and other smaller earthquakes.

Eruption. The Toulouse Volcanic Ash Advisory Center (VAAC) reported that an eruption from Nabro (originally attributed to Dubbi, ~25 km NNE of Nabro) started between 0300 and 0500 on 13 June 2011. The eruption plume initially rose to altitudes of 9.1-13.7 km; it was detected at altitudes of 6.1-10.7 km during 13-14 June.

According to the Eritrean Ministry of Information, ashfall covered hundreds of square kilometers, and the government evacuated area residents. Eye witnesses first observed the eruption at about 2100 on 13 June. Satellite images that same day showed the plume drifting more than 1,000 km NW, over parts of Sudan. On 14 June 2011 news articles reported that a detached ash cloud was detected over southern Israel. Throughout the eruption, satellite images were nearly the only source of new information about activity.

The Addis Fortune website reported that, although the major eruption took place in Nabro, large quantities of dust from the earthquake occurred in the town of Afambo (~26.5 km N of Nabro). It also reported that the Eritrean government announced that inhabitants had moved to safe areas. The well-known Afdera salt accumulation site in the depression was covered in volcanic ash. The salt, extracted for human and other consumption, had thus become inedible. The ash clouds also caused the cancellation of some domestic and international flights in Eritrea and Ethiopia.

During the week of 15-21 June 2011, Nabro continued to produce plumes. Based on analyses of satellite imagery during that period, the Toulouse VAAC reported that plumes comprised mostly of water and SO2 rose to altitudes of 6.1-7.9 km (figure 5). Ash was occasionally detected near the volcano. Satellite imagery posted on the MODIS/MODVOLC website showed a dark brown ash plume fanning out to the SW on 19 June. By 19 June, the altitude of Nabro's ash plume dropped from a maximum of 14 km to 7.6 km. The ash halted flights in eastern Africa for a time. The eruption killed seven people, according to the Eritrean government, although later reports appeared to discount that. Other reports indicated that thousands were affected in both Eritrea and Ethiopia, though news was sparse.

Figure 5. This large and intense SO2 gas cloud emitted from Nabro was captured by the OMI satellite's spectrometer during the time interval between 1017 and 1159 UTC on 19 June 2011. The SO2 traveled to the S and the W during the period, and some portions of intense gas clearly extended off this image in those directions. The scale at right is in Dobson Units (DU, a unit common in atmospheric research and widely described in text books). The mass of SO2 depicted on this image was ~103 kilotons (kt); the area of cloud was ~591,000 km2; the maximum SO2 values on the image occurred at the location 40.87°N and 13.14°E and reached 68 DU. Courtesy of Simon Carn, and NASA Global Sulfur Dioxide Monitoring Aura/OMI website.

A thermal satellite image acquired at night on 19 June revealed a 15-km-long lava flow that had traveled NW (figure 6). A high-altitude plume, likely rich in water vapor, rose from erupting vents; a diffuse ash-rich plume drifted SW. The more restricted plume on 19 June enabled images to reveal a NW-trending lava flow that extended ~15 km from the summit area, although the area of venting remained obscured by a water-rich plume.

Figure 6. A thermal infrared, false-color image of Nabro on 19 June 2011 taken by the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). Hot areas are bright with new lava flows shown in white, and cold areas are dark. Thermal infrared data were combined with a shaded relief image to show the terrain. Courtesy of NASA Earth Observatory.

On 22 June a report from the Eritrea Ministry of Energy and Mines stated that the ash and lava covered hundreds of square meters. A satellite image acquired that day showed a gas-and-ash plume rising from the caldera and drifting W. An image from 24 June showed the erupting vent, plumes and emissions, and lava flows (figure 7).

Figure 7. A false-color image of Nabro, acquired by the Advanced Land Imager (ALI) aboard the Earth Observing-1 (EO-1) satellite on 24 June 2011, highlighted hot areas throughout the lava flow and flow front, as well as above the vent in the center of the caldera. The bright red portions indicate hot surfaces. To the W, portions of an active lava flow (particularly the flow-front) are also hot. The speckled pattern on upstream portions of the flow is likely due to hardened crust splitting and exposing fluid lava. An ash plume rose from the vent, and at higher altitudes a plume composed of water vapor and SO2 drifted W and obscured the active lava flow. Black ash deposits covered the landscape to the S and W. Courtesy of NASA Earth Observatory.

During 22-26 June large amounts of SO2 in the region continued to be detected by satellite images. Based on analyses of satellite imagery, the Toulouse VAAC reported that during 26-27 June plumes reached altitudes of up to 6.1 km.

An annotated satellite image acquired on 29 June (figure 8) showed a clear view of the eruption. NASA Earth Observatory analysts labeled what they inferred to be the vent, an area in the main caldera's center and likely engulfing both the two inner craters with either very hot lava or with fresh tephra that probably formed cones or other features whose surface cooled quickly. An ash plume rose from the vent and drifted S. Based on analyses of satellite imagery, the Toulouse VAAC reported that on 16 July an ash plume from Nabro rose to altitudes below 5.5 km. A weak eruption detected on 17 July decreased through the day then appeared to stop.

Figure 8. A visible and infrared image of Nabro from the Advanced Land Imager (ALI) on the Earth Observing-1 (EO-1) satellite, taken 29 June 2011. The image shows the still-hot lava flow, fresh ash over the lower half of the photo (dark landscape, accentuated by slanting lines or dashes in the lower portion of the image). A diffuse ash plume rose from the vent. The hottest lava is indicated by orange-red, with cooler zones fading to black. The ~15 km long flow on the W side of the volcano is mottled with black, indicating areas with cooler surfaces. The lava to the E and S of the vent appears to be newer, since little of it has cooled. Image and interpretation of NASA Earth Observatory (with lines and additional labels added).

According to an article by the South Africa Weather and Disaster Information Service (SAWDIS) dated 30 June 2011, a press release from the Eritrean Government disclosed that, though the advancing lava in the nearby village of Sireru had slowed down, a large area of land covered by vegetation was destroyed and river beds were covered within 24 hours.

NASA's Earth Observatory noted that images from 28 September showed heat from the vent in the central crater and from an area 1.3 km S of the vent that indicated an active lava flow. A small and diffuse plume rose from the vent. A region of seemingly thicker black ash (that completely covered the sparse vegetation) was noted S of the crater and thinner layers of ash (with some areas of visible vegetation) flanked either side of the region.

MODVOLC Thermal Alerts. Prior to 12 June 2011 the MODVOLC website indicated that no thermal alerts were measured over at least the past 5 years. The onset of thermal alerts was a 3-pixel area detected at 0115 on 13 June 2011 (2215 on 12 June UTC), followed by nearly daily measurements through 1 September 2011. Since that date, several alerts per week have been measured for Nabro up to 5 November 2011.

Some individual satellite passes measured high numbers of alerts. A 9-pixel alert occurred on 8 September, and as many as 95 pixels were measured for a single satellite pass at 2245 on 17 June. Other single orbital passes during June-August measured alerts of 50 to more than 70 pixels.

Reference. Wiart, P., and Oppenheimer, C., 2005, Large magnitude silicic volcanism in north Afar: the Nabro Volcanic Range and Ma'alalta volcano, Bulletin of Volcanology, v. 67, no. 2, pp. 99-115.

Information Contacts: NASA Earth Observatory (URL: http://earthobservatory.nasa.gov); MODIS/MODVOLC, Hawai'i Institute of Geophysics and Planetology (HIGP) MODVOLC Thermal Alerts System, School of Ocean and Earth Science and Technology (SOEST), Univ. of Hawai'i, 2525 Correa Road, Honolulu, HI (URL: http://hotspot.higp.hawaii.edu/); Toulouse Volcanic Ash Advisory Centre (VAAC) (URL: http://www.ssd.noaa.gov/VAAC/OTH/FR/messages.html); NASA Global Sulfur Dioxide Monitoring (URL: http://SO2.gsfc.nasa.gov/index.php); Jet Propulsion Laboratory (URL: http://photojournal.jpl.nasa.gov); S.A. Weather and Disaster Information Service. (SAWDIS) (URL: http://saweatherobserver.blogspot.com); Ethiopian Journal (URL: http://www.ethjournal.com), Addis Fortune (URL: http://www.addisfortune.com); Simon Carn, Dept of Geological and Mining Engineering and Sciences, Michigan Technological University, 1400 Townsend Dr., Houghton, MI 49931, USA (URL: http://www.volcarno.com/, http://SO2.umbc.edu/omi/).

The 2218-m-high Nabro stratovolcano is the highest volcano in the Danakil depression of northern Ethiopia and Eritrea. Located at the SE end of the Danakil Alps, Nabro lies in the Danakil horst. Nabro is the most prominent and NE-most of three volcanoes with large summit calderas aligned in a NE-SW direction SW of Dubbi volcano. These three volcanoes, along with Sork Ale volcano, collectively comprise the Bidu volcanic complex. The complex Nabro stratovolcano is truncated by nested calderas, 8 and 5 km in diameter. The larger caldera is widely breached to the SW. Nabro was constructed primarily of trachytic lava flows and pyroclastics. Post-caldera rhyolitic obsidian domes and basaltic lava flows were erupted inside the caldera and on its flanks. Some very recent lava flows were erupted from NNW-trending fissures transverse to the trend of the Nabro volcanic range.

Summary of Holocene eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
2011 Jun 13 2012 Jun 3 (?) Confirmed 4 Historical Observations

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
Nabbeo
The large caldera below and to the left of the center of this Space Shuttle photo of the Danakil Alps of Ethiopia is Nabro. The 2218-m-high Nabro stratovolcano is the highest volcano in the Danakil depression and is truncated by nested calderas 10 and 5 km in diameter. The larger caldera is widely breached to the SW. Nabro was constructed primarily of rhyolitic lava flows and pyroclastics. The 8-km-wide Mallahle caldera is at the lower left, and the dark-colored lava flows at the right are from Dubbi volcano.

NASA Space Shuttle image S-61A-36, 1985.

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.

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

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

Katsui Y (ed), 1971. List of the World Active Volcanoes. Volc Soc Japan draft ms, (limited circulation), 160 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.

Wood C A, 1980. . (pers. comm.).

Volcano Types

Stratovolcano
Caldera(s)
Lava dome(s)
Scoria cone(s)

Tectonic Setting

Rift zone
Intermediate crust (15-25 km)

Rock Types

Major
Trachyte / Trachyandesite
Rhyolite
Basalt / Picro-Basalt

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
24
145
2,713
26,881

Affiliated Databases

Large Eruptions of Nabro 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).
Smithsonian Collections Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.