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Mombacho

Photo of this volcano
  • Country
  • Volcanic Region
  • Landform | Volc Type
  • Last Known Eruption
  • 11.826°N
  • 85.968°W

  • 1,344 m
    4,409 ft

  • 344110
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number


Most Recent Bulletin Report: February 2012 (BGVN 37:02) Citation IconCite this Report

Seismicity and fumarole characteristics from 2000 to 2011

Our BGVN reports discussing Mombacho volcano have discussed variable fumarolic gas emissions and characteristics of hot springs since 1980. Data collection from three distinct fumaroles became available by the Instituto Nicaragüense de Estudios Territoriales (INETER) starting in 1994 (BGVN 19:11). Since January 2000, the Geophysics Department of INETER has published "Sismos y Volcanes de Nicaragua," a monthly bulletin for volcanoes throughout Nicaragua. Status and seismicity reports for Mombacho appear as early as December 2000. Here we present a summary of field observations including local seismicity from 2000 to 2010, and thermal measurements from Mombacho's fumaroles from July 2001 to December 2011.

Local seismicity from 2000 through 2010. INETER reported a significant number of earthquake magnitudes and hypocenter locations in 2000 (table 1). A total of 14 events were registered and located during July-October. Few earthquakes were registered after 2000, with the largest magnitudes being ML 2.6-2.7. One seismic station with a radio repeater is located on Mombacho's flanks ~1.5 km to the NW of the summit.

Table 1. Located earthquakes recorded near Mombacho from 2000 through 2010. For each year, the table lists the number of located earthquakes, the range of their local magnitudes (ML), the range of their focal depths, and the average focal depths. Courtesy of INETER.

Year Earthquakes ML Range of focal depths (km) Average focal depths (km)
2000 14 2.1-2.9 0-6 2.9
2002 4 2.3-2.7 2-14 6
2004 2 2.5-2.6 4-18 11
2010 1 2.7 70 70

Fumarole temperature monitoring from 2001 to 2011. There are three well-established fumarole areas near the summit of Mombacho located above 800 m asl (figure 1 in BGVN 19:11). Fumarole temperatures were collected intermittently between July 2001 and December 2011 (table 2). Depending on surface conditions (local rockfalls often covered fumaroles), one to five different point sources were visited during this time period. Temperatures had a wide range and were frequently low; the lowest temperatures were recorded in November 2009 (81°C), March 2011 (61.5°C), and June 2011 (81°C). Temperatures greater than 125°C were rare; the highest measurements of 398°C were measured in August 2009, August 2010, and December 2011. INETER made numerous visits to Mombacho's fumarole fields from 2000 to 2011 however, it wasn't always possible to take measurements. Campaigns to fumarole sites were encumbered by dense vegetation; new trails needed to be cut for each visit, even with a time lapse as small as three months during the dry season. Temperatures were measured at fumaroles with a digital thermometer. INETER observed that landslides frequently covered fumarole sites and reported the extent of debris in their field reports: 19 August 2009, 14 May 2010, July 2010, 19 August 2010, 15 June 2011, 12 December 2011.

Table 2. Fumarole temperature data collected during campaigns to Mombacho sites from 2001 to 2011. Temperatures were measured with a handheld digital thermometer. Courtesy of INETER.

Month Temp. Range °C
Jul 2001 100-110
Feb 2002 100-120
Apr 2003 96.5-120.6
Jul 2003 96.5-121.0
Apr 2005 98.4-110.5
Aug 2007 95.3-123
Nov 2008 96.1-125
Aug 2009 92-398
Nov 2009 81-94
Feb 2010 90-99
May 2010 99-117
Jul 2010 90-112
Aug 2010 92-398
Nov 2010 90-93
Mar 2011 61.5
Jun 2011 81-86
Dec 2011 96-302

Field observations. Field visits from December 2000 to December 2011 by INETER consistently encountered the effects of landslides within Mombacho's southern crater. The steep walls, especially the E and W scarps, shed debris that collected within the crater. Evidence of large rockfalls was typically encountered after major rain events such as Hurricane Keith in September 2000 and a tropical storm in October 2010.

The southern crater is one of two dramatic collapse amphitheaters (figure 2). The collapse scars show up as high relief features in satellite imagery and topographic maps. At least three large-volume debris avalanche deposits have been attributed to Mombacho and resulted from catastrophic flank collapse (Shea and others, 2008). The long runout of the northern deposit reached Lake Nicaragua and formed the arcuate peninsula and cluster of islands, Isletas de Granada, ~11 km NE from Mombacho's summit (close-up photos and captions are available in the GVP Photo Archive).

Figure (see Caption) Figure 2. Satellite image centered on Mombacho using near-, mid-infrared, and infrared bands (Landsat bands 4,5,7). Recent rockfalls and water-poor soils appear cyan; brown-to-red areas indicate moist soils; water is black. Small ponds (irregular black shapes) are found within the Lagunetas de Mecatepe Reserve in an area mapped as debris avalanche deposits (Shea and others, 2008). Three yellow asterisks mark fumarole areas near the summit and local place names note major landmarks in the area including the city of Granada (N of the summit). The three circular features (~400 m diameter) located SW of the city of Granada, are the Granada Fissure Vents, sometimes called the La Joya alignment. Landsat acquired this ETM+ image on 27 January 2000 and it was processed by GVP (NASA Landsat Program, 2003).

Several investigations into the debris avalanche deposits of Mombacho revealed new ideas about the likely factors that led to flank failure. The geologic setting of Mombacho includes the extensive pumice-rich ignimbrite deposits from Apoyo and Las Sierras and potentially lake sediments from Lake Nicaragua (figure 3). These relatively weak units that underlie Mombacho's edifice may have promoted gravitational spreading if the weight of the volcanic edifice caused deformation of the substratum. The near-vertical southern scarp exposes hydrothermally altered rock. This clay-rich material could have contributed to the weakening process that triggered the S-directed collapse. Deposits linked to the S-facing scarp have been mapped to the southernmost edge of the Lagunetas de Mecatepe Nature Reserve (~12 km from the summit).

Figure (see Caption) Figure 3. (A) The top figure is centered on the W coast of Nicaragua where major Quaternary volcanoes are aligned in the Central American Volcanic Front (CAVF). Mombacho (M) is located on the shore of Lake Nicaragua, within the enlarged area of this map, as well as other major sites: Las Sierras (LS), Apoyo (A), and Zapatera (Z). (B) Starting in the NW, the numbers correspond to major volcanic sites: 1 Chiltepe shield (Apoyeque and Jiloa Calderas), 2 Las Sierras caldera complex, 3 Masaya caldera complex, 4 Apoyo caldera, and 5 Mombacho volcano. This composite image is modified from Shea and others (2008) and van Wyk de Vries (1993).

References. NASA Landsat Program (2003) Landsat ETM+ scene 7dt20000127, SLC-Off, USGS, Sioux Falls, Jan. 27, 2000.

Shea, T., van Wyk de Vries, B., and Pilato, M. (2008) Emplacement mechanisms of contrasting debris avalanches at Volcan Mombacho (Nicaragua), provided by structural and facies analysis. Bulletin of Volcanology, v. 70, p. 899-921.

van Wyk de Vries, B. (1993) Tectonics and magma evolution of Nicaraguan volcanic systems. [PhD thesis] Milton Keynes, The Open University, UK.

Information Contacts: Instituto Nicaragüense de Estudios Territoriales (INETER), Apartado Postal 2110, Managua, Nicaragua (URL: http://www.ineter.gob.ni/); Global Land Cover Facility (URL: http://http://www.glcf.umiacs.umd.edu/); Washington Volcanic Ash Advisory Center (VAAC), Satellite Analysis Branch (SAB), NOAA/NESDIS E/SP23, NOAA Science Center Room 401, 5200 Auth Rd, Camp Springs, MD 20746, USA (URL: http://www.ospo.noaa.gov/Products/atmosphere/vaac/).

The Global Volcanism Program has no Weekly Reports available for Mombacho.

Bulletin Reports - Index

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.

12/1980 (SEAN 05:12) Small intermittent plume

03/1982 (SEAN 07:03) Four hot-springs located

01/1988 (SEAN 13:01) Noisy gas emissions from fumarole in collapse crater

02/1991 (BGVN 16:02) Continued gas emission

11/1994 (BGVN 19:11) Venting continues from fumarole in south crater; two other fumarole areas located

02/2012 (BGVN 37:02) Seismicity and fumarole characteristics from 2000 to 2011




Information is preliminary and subject to change. All times are local (unless otherwise noted)


December 1980 (SEAN 05:12) Citation IconCite this Report

Small intermittent plume

In late 1980 a small, intermittent plume was visible, rising from the SE section of the summit.

Information Contacts: R. Stoiber, S. Williams, H.R. Naslund, L. Malinconico, M. Conrad, Dartmouth College; M. Carr, J. Walker, Rutgers Univ.; A. Creusot, Instituto Nicaraguense de Energía.


March 1982 (SEAN 07:03) Citation IconCite this Report

Four hot-springs located

"Paolo Pisani, a consultant to INE, reported finding four previously unknown low-temperature hot springs on the S side of Mombacho. These are not believed to be new, however."

Information Contacts: S. Williams, R. Stoiber, Dartmouth College; I. Menyailov, V. Shapar, IVP, Kamchatka; D. Fajardo B., INETER.


January 1988 (SEAN 13:01) Citation IconCite this Report

Noisy gas emissions from fumarole in collapse crater

A fumarole emitting gas with a loud noise has been seen in the southern collapse crater in 1986 and 1987.

Information Contacts: B. van Wyk de Vries, H. Rymer, and G. Brown, Open Univ; P. Hradecky and H. Taleno, INETER.


February 1991 (BGVN 16:02) Citation IconCite this Report

Continued gas emission

"The fumarole in the S collapse crater continued to emit gas."

Information Contacts: B. van Wyk de Vries, O. Castellón, A. Murales, and V. Tenorio, INETER.


November 1994 (BGVN 19:11) Citation IconCite this Report

Venting continues from fumarole in south crater; two other fumarole areas located

The fumarole that has been active since at least 1986 continued to vent vapor in November and December 1993. A strong sulfur odor was detected even when the wind was blowing towards the fumarole. This observation led to the discovery of two other previously unreported fumarole fields (figure 1). Vapor was seen rising from both, but they were not approached closely; neither appeared to be a new feature.

Figure (see Caption) Figure 1. Map of the Mombacho summit area, showing locations of reported and previously unreported fumarole areas. Courtesy of B. van Wyk de Vries and P. Hernandez.

Information Contacts: B. van Wyk de Vries, Open Univ; Pedro Hernandez, INETER.


February 2012 (BGVN 37:02) Citation IconCite this Report

Seismicity and fumarole characteristics from 2000 to 2011

Our BGVN reports discussing Mombacho volcano have discussed variable fumarolic gas emissions and characteristics of hot springs since 1980. Data collection from three distinct fumaroles became available by the Instituto Nicaragüense de Estudios Territoriales (INETER) starting in 1994 (BGVN 19:11). Since January 2000, the Geophysics Department of INETER has published "Sismos y Volcanes de Nicaragua," a monthly bulletin for volcanoes throughout Nicaragua. Status and seismicity reports for Mombacho appear as early as December 2000. Here we present a summary of field observations including local seismicity from 2000 to 2010, and thermal measurements from Mombacho's fumaroles from July 2001 to December 2011.

Local seismicity from 2000 through 2010. INETER reported a significant number of earthquake magnitudes and hypocenter locations in 2000 (table 1). A total of 14 events were registered and located during July-October. Few earthquakes were registered after 2000, with the largest magnitudes being ML 2.6-2.7. One seismic station with a radio repeater is located on Mombacho's flanks ~1.5 km to the NW of the summit.

Table 1. Located earthquakes recorded near Mombacho from 2000 through 2010. For each year, the table lists the number of located earthquakes, the range of their local magnitudes (ML), the range of their focal depths, and the average focal depths. Courtesy of INETER.

Year Earthquakes ML Range of focal depths (km) Average focal depths (km)
2000 14 2.1-2.9 0-6 2.9
2002 4 2.3-2.7 2-14 6
2004 2 2.5-2.6 4-18 11
2010 1 2.7 70 70

Fumarole temperature monitoring from 2001 to 2011. There are three well-established fumarole areas near the summit of Mombacho located above 800 m asl (figure 1 in BGVN 19:11). Fumarole temperatures were collected intermittently between July 2001 and December 2011 (table 2). Depending on surface conditions (local rockfalls often covered fumaroles), one to five different point sources were visited during this time period. Temperatures had a wide range and were frequently low; the lowest temperatures were recorded in November 2009 (81°C), March 2011 (61.5°C), and June 2011 (81°C). Temperatures greater than 125°C were rare; the highest measurements of 398°C were measured in August 2009, August 2010, and December 2011. INETER made numerous visits to Mombacho's fumarole fields from 2000 to 2011 however, it wasn't always possible to take measurements. Campaigns to fumarole sites were encumbered by dense vegetation; new trails needed to be cut for each visit, even with a time lapse as small as three months during the dry season. Temperatures were measured at fumaroles with a digital thermometer. INETER observed that landslides frequently covered fumarole sites and reported the extent of debris in their field reports: 19 August 2009, 14 May 2010, July 2010, 19 August 2010, 15 June 2011, 12 December 2011.

Table 2. Fumarole temperature data collected during campaigns to Mombacho sites from 2001 to 2011. Temperatures were measured with a handheld digital thermometer. Courtesy of INETER.

Month Temp. Range °C
Jul 2001 100-110
Feb 2002 100-120
Apr 2003 96.5-120.6
Jul 2003 96.5-121.0
Apr 2005 98.4-110.5
Aug 2007 95.3-123
Nov 2008 96.1-125
Aug 2009 92-398
Nov 2009 81-94
Feb 2010 90-99
May 2010 99-117
Jul 2010 90-112
Aug 2010 92-398
Nov 2010 90-93
Mar 2011 61.5
Jun 2011 81-86
Dec 2011 96-302

Field observations. Field visits from December 2000 to December 2011 by INETER consistently encountered the effects of landslides within Mombacho's southern crater. The steep walls, especially the E and W scarps, shed debris that collected within the crater. Evidence of large rockfalls was typically encountered after major rain events such as Hurricane Keith in September 2000 and a tropical storm in October 2010.

The southern crater is one of two dramatic collapse amphitheaters (figure 2). The collapse scars show up as high relief features in satellite imagery and topographic maps. At least three large-volume debris avalanche deposits have been attributed to Mombacho and resulted from catastrophic flank collapse (Shea and others, 2008). The long runout of the northern deposit reached Lake Nicaragua and formed the arcuate peninsula and cluster of islands, Isletas de Granada, ~11 km NE from Mombacho's summit (close-up photos and captions are available in the GVP Photo Archive).

Figure (see Caption) Figure 2. Satellite image centered on Mombacho using near-, mid-infrared, and infrared bands (Landsat bands 4,5,7). Recent rockfalls and water-poor soils appear cyan; brown-to-red areas indicate moist soils; water is black. Small ponds (irregular black shapes) are found within the Lagunetas de Mecatepe Reserve in an area mapped as debris avalanche deposits (Shea and others, 2008). Three yellow asterisks mark fumarole areas near the summit and local place names note major landmarks in the area including the city of Granada (N of the summit). The three circular features (~400 m diameter) located SW of the city of Granada, are the Granada Fissure Vents, sometimes called the La Joya alignment. Landsat acquired this ETM+ image on 27 January 2000 and it was processed by GVP (NASA Landsat Program, 2003).

Several investigations into the debris avalanche deposits of Mombacho revealed new ideas about the likely factors that led to flank failure. The geologic setting of Mombacho includes the extensive pumice-rich ignimbrite deposits from Apoyo and Las Sierras and potentially lake sediments from Lake Nicaragua (figure 3). These relatively weak units that underlie Mombacho's edifice may have promoted gravitational spreading if the weight of the volcanic edifice caused deformation of the substratum. The near-vertical southern scarp exposes hydrothermally altered rock. This clay-rich material could have contributed to the weakening process that triggered the S-directed collapse. Deposits linked to the S-facing scarp have been mapped to the southernmost edge of the Lagunetas de Mecatepe Nature Reserve (~12 km from the summit).

Figure (see Caption) Figure 3. (A) The top figure is centered on the W coast of Nicaragua where major Quaternary volcanoes are aligned in the Central American Volcanic Front (CAVF). Mombacho (M) is located on the shore of Lake Nicaragua, within the enlarged area of this map, as well as other major sites: Las Sierras (LS), Apoyo (A), and Zapatera (Z). (B) Starting in the NW, the numbers correspond to major volcanic sites: 1 Chiltepe shield (Apoyeque and Jiloa Calderas), 2 Las Sierras caldera complex, 3 Masaya caldera complex, 4 Apoyo caldera, and 5 Mombacho volcano. This composite image is modified from Shea and others (2008) and van Wyk de Vries (1993).

References. NASA Landsat Program (2003) Landsat ETM+ scene 7dt20000127, SLC-Off, USGS, Sioux Falls, Jan. 27, 2000.

Shea, T., van Wyk de Vries, B., and Pilato, M. (2008) Emplacement mechanisms of contrasting debris avalanches at Volcan Mombacho (Nicaragua), provided by structural and facies analysis. Bulletin of Volcanology, v. 70, p. 899-921.

van Wyk de Vries, B. (1993) Tectonics and magma evolution of Nicaraguan volcanic systems. [PhD thesis] Milton Keynes, The Open University, UK.

Information Contacts: Instituto Nicaragüense de Estudios Territoriales (INETER), Apartado Postal 2110, Managua, Nicaragua (URL: http://www.ineter.gob.ni/); Global Land Cover Facility (URL: http://http://www.glcf.umiacs.umd.edu/); Washington Volcanic Ash Advisory Center (VAAC), Satellite Analysis Branch (SAB), NOAA/NESDIS E/SP23, NOAA Science Center Room 401, 5200 Auth Rd, Camp Springs, MD 20746, USA (URL: http://www.ospo.noaa.gov/Products/atmosphere/vaac/).

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.

Eruptive History

There is data available for 0 confirmed Holocene eruptive periods.

[ 1850 ] Discredited Eruption

The report of the formation of the the parasitic cone Pilas on the N flank is very doubtful, for it is reported only by Crawford, who probably confused it with the 1850 formation of Cerro Negro on the north side of Las Pilas volcano (CAVW).

[ 1570 ] Uncertain Eruption

Episode 1 | Eruption
1570 - Unknown Evidence from Unknown

List of 6 Events for Episode 1

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion Uncertain
   - - - -    - - - - Avalanche
   - - - -    - - - - Earthquakes (undefined) Time and Type Unknown.
   - - - -    - - - - Edifice Destroyed Collapse/avalanche
   - - - -    - - - - Property Damage
1570    - - - - Fatalities
Deformation History

There is no Deformation History data available for Mombacho.

Emission History

There is no Emissions History data available for Mombacho.

Photo Gallery

The 7-km-wide, lake-filled Apoyo caldera, seen here from the NW with Mombacho volcano in the background, is a large silicic volcanic center immediately SE of Masaya caldera. An early shield volcano constructed of basaltic-to-andesitic lava flows and small rhyodacitic lava domes collapsed following two major dacitic explosive eruptions about 23,000 years ago. Post-caldera ring-fracture eruptions formed the Granada cinder cones and La Joya collapse craters along fracture systems to the east of the caldera. The age of the latest activity is not known.

Photo by Alain Creusot-Eon, courtesy of Jaime Incer, 1968.
Mombacho is a stratovolcano on the shores of Lake Nicaragua that has undergone edifice collapse on several occasions. The NE-flank scarp was the source of a large debris avalanche that produced an arcuate peninsula and the Las Isletas chain of islands in Lake Nicaragua. The only reported historical activity was in 1570, when a debris avalanche destroyed a village on the S side of the volcano.

Photo by Jaime Incer, 1977.
Las Isletas, a group of islands that were created by a large Holocene debris avalanche from Mombacho that swept into Lake Nicaragua. The avalanche traveled at least 12 km. The hummocky debris created an arcuate peninsula that extends into the lake as well as hundreds of small islands. This morphology is common where debris avalanches enter shallow bodies of water.

Photo by Jaime Incer, 1972.
These angular boulders are part of a debris-avalanche deposit that originated from the south side of Mombacho volcano (seen in the background), most likely in 1570 CE. The avalanche traveled 13 km from Mombacho, and destroyed a village, killing 400 people.

Photo by Jaime Incer, 1972.
The south side of Mombacho contains a horseshoe-shaped crater that was the source of a large debris avalanche in 1570 CE that swept over a village south of the volcano, killing 400 people. The avalanche traveled 13 km S; contemporary accounts note that if it had occurred to the north, it would have reached the city of Granada. Contemporary accounts indicate that the volcano "exploded," but eruptive activity associated with the collapse has not been documented.

Photo by Jaime Incer.
The south side of Mombacho volcano is cut by a large horseshoe-shaped depression that left two major summit peaks. Recent landslips scar the face of the higher easternmost peak. The depression was formed during collapse of the volcano, which produced a large debris avalanche that traveled to the south. The 2-km-wide depression merges with a scarp from a NE-flank collapse, which lies on the other side of the notch in the center of the photo.

Photo by Jaime Incer, 1996.
Volcán Mombacho rises above cattle ranches on the plain of Nandaime, south of the volcano. The volcano's irregular summit with two major peaks reaching 1222 and 1333 m resulted from collapse of the top of the volcano, which left the horseshoe-shaped depression in the center of the photo. Mombacho is the centerpiece of the Mombacho Volcano Reserve, whose forested terrain contains exotic orchids, birds and primates.

Photo by Jaime Incer, 1966.
Mombacho volcano in the background collapsed during the late Pleistocene, producing a debris avalanche that swept into Lake Nicaragua, deposting debris that accumulated to form the Aseses Peninsula in the foreground. The surface of the avalanche deposit lies below the lake surface immediately offshore of the mainland, creating the Bay of Aseses in the middle of the photo. Portions of the deposit rise above the lake surface, forming hundreds of small islands.

Photo by Jaime Incer.
Las Isletas, or Isletas de Granada, are a cluster of about 500 small islands flanking the Aseses Peninsula extending into Lake Nicaragua. They were formed when the NE flank of Mombacho volcano collapsed, producing a debris avalanche that swept into the lake. A road leads down the peninsula to the settlement of El Diamante seen above the center of the photo. The peninsula is a resort area visited frequently from the nearby city of Granada. Many of the islands host vacation residences.

Photo by Jaime Incer.
The arcuate Aseses Peninsula extending 5 km into Lake Nicaragua was formed when the NE flank of Mombacho volcano collapsed producing a highly mobile debris avalanche that swept into the lake. Flanking the peninsula are hundreds of small islands, known as Las Isletas, or Isletas de Granada. These are the tops of hummocky terrain formed of debris from the avalanche, which traveled as far as 12 km from the volcano.

Photo by Jaime Incer.
An aerial view of Mombacho from the SW shows the higher eastern summit of the twin-peaked volcano at the right. In the foreground is the southernmost of two large collapse scarps that cut the edifice. The other scarp, out of view on the NE flank beyond the ridge below the summit, was the source of a large debris avalanche that swept into Lake Nicaragua, forming the Aseses Peninsula and Las Isletas at the upper left.

Photo by Franco Penalba (courtesy of Jaime Incer), 1994.
These small forested islands are hummocks of a large debris avalanche from Mombacho volcano that swept into Lake Nicaragua. The horizon is formed by Isla Zapatera volcano, SE of Mombacho.

Photo by Lee Siebert, 1998 (Smithsonian Institution).
A small boat plies the waters of Ensenada de Aseses, with Zapatera Island forming the horizon to the SE. In the middle distance are the small island hummocks of Las Isletas, formed by a debris avalanche from Mombacho volcano, out of view to the right. The conical peak on the distant left horizon is Concepción volcano; the low, rounded peak to its left is Cerro las Banderas, a pyroclastic cone on the NE tip of Zapatera Island.

Photo by Paul Kimberly, 1998 (Smithsonian Institution).
Two major scarps cutting Mombacho volcano (left-center) were the sources of major debris avalanches. The arcuate peninsula and island chain extending into Lake Nicaragua (known as Las Isletas or Isletas de Granada) was produced by collapse of Mombacho to the NE. The island at the right is Zapatera, a small shield volcano and maar complex. The lake at the far left fills late-Pleistocene Apoyo caldera, and the roughly N-S-trending Granada cinder cone alignment lies NNW of Mombacho and east of Lake Apoyo in this NASA Space Shuttle image (with north to the upper left).

NASA Space Shuttle image STS081-742-25, 1997 (http://eol.jsc.nasa.gov/).
Two major flank-collapse scarps on the NE and SW sides of Mombacho are visible in this March 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 25 km across). The islands to the NE are part of the 56.8 km2 Las Isletas debris avalanche deposit; the 49.5 km2 El Crater debris avalanche deposit is to the S. The La Danta debris avalanche deposit is between the two on the SE flank and surrounding area.

Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).
GVP Map Holdings

Maps are not currently available due to technical issues.

The maps shown below have been scanned from the GVP map archives and include the volcano on this page. Clicking on the small images will load the full 300 dpi map. Very small-scale maps (such as world maps) are not included.

Smithsonian Sample Collections Database

There are no samples for Mombacho in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.

External Sites