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Michoacán-Guanajuato

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  • Country
  • Volcanic Region
  • Landform | Volc Type
  • Last Known Eruption
  • 19.85°N
  • 101.75°W
  • 3,860 m
    12,664 ft
  • 341060
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Most Recent Bulletin Report: December 1989 (SEAN 14:12) Citation IconCite this Report

Fumarole temperatures decrease

Geologists visited Ahuan fumarole on 23 November. The fumarole temperature was 305°C, a decrease from 336°C measured in May 1988.

Information Contacts: Kurt Roggensack, Helen Mango, John Lucio, and Half Zantop, Dartmouth College.

The Global Volcanism Program has no Weekly Reports available for Michoacán-Guanajuato.

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.

04/1983 (SEAN 08:04) Fumaroles emit acid gases

11/1985 (SEAN 10:11) Fumarole temperatures increase

11/1986 (SEAN 11:11) Temperature of hottest fumarole declines; HCl-rich gases

05/1988 (SEAN 13:05) Fumarole temperatures decline

12/1989 (SEAN 14:12) Fumarole temperatures decrease



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


April 1983 (SEAN 08:04) Citation IconCite this Report

Fumaroles emit acid gases

"Fumaroles at several localities were emitting small amounts of acid gases but there was no visible plume at the summit or elsewhere when visited 28 April-1 May. Temperatures were mostly less than 150°C but some were much hotter, over 400°C."

Information Contacts: R. Stoiber, L. Benton, C. Connor, D. Douglass, D. Shumway, and J. Swartz, Dartmouth College.


November 1985 (SEAN 10:11) Citation IconCite this Report

Fumarole temperatures increase

"Fumarolic activity persisted at Ahuan vent on the SW flank. When temperatures were measured at Ahuan vent on 29 November, the hottest fumarole was 473°C, 70° higher than in April 1983, when Dartmouth scientists last measured temperatures at Parícutin. Several fumaroles over an area of about 50 m2 were hotter than 300°C. No physical changes in the area were apparent since April 1983."

Information Contacts: C. Connor, B. Gemmell, and R. Stoiber, Dartmouth College.


November 1986 (SEAN 11:11) Citation IconCite this Report

Temperature of hottest fumarole declines; HCl-rich gases

When geologists visited Parícutin 26 November, fumaroles were emitting HCl-dominated gases. The temperature of Ahuan fumarole (on the SW flank) was 375°C, about 100° lower than in November 1985. Other fumaroles remained at about 100°C. No other changes were observed.

Information Contacts: R. Stoiber, C. Connor, and other geologists, Dartmouth College.


May 1988 (SEAN 13:05) Citation IconCite this Report

Fumarole temperatures decline

Geologists mapped fumaroles and measured temperatures on 8 and 16 May. As in previous years, fumaroles were hottest at Ahuan vent (figure 1) but had cooled to 336°C, from 473° in November 1985 and 375° in November 1986. The area seemed morphologically unchanged since April 1983. Fumaroles at Sapichu vent ranged from 186° to 275°C, an increase of as much as 120° since they were last measured in April 1983. Sulfur continued to be deposited around the Sapichu fumaroles. All other fumaroles at Parícutin had temperatures of

Figure (see Caption) Figure 1. Distribution of fumaroles at Parícutin, May 1988. Fumaroles were found in the shaded areas (stipple pattern,100°C). Three vents are labeled: Ahuan (A), the main crater (P), and Sapichu (S). The W and SW margins of lava flows surrounding the cone are indicated by the stippled border.

Information Contacts: C. Connor, James Diaz, and Jorge Corrales, FIU, Miami; Ana Lillian Martin-Del Pozzo, Instituto de Geofísica, UNAM, México.


December 1989 (SEAN 14:12) Citation IconCite this Report

Fumarole temperatures decrease

Geologists visited Ahuan fumarole on 23 November. The fumarole temperature was 305°C, a decrease from 336°C measured in May 1988.

Information Contacts: Kurt Roggensack, Helen Mango, John Lucio, and Half Zantop, Dartmouth College.

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 10 confirmed Holocene eruptive periods.

1943 Feb 20 - 1952 Feb 25 Confirmed Eruption VEI: 4

Episode 1 | Eruption Parícutin
1943 Feb 20 - 1952 Feb 25 Evidence from Observations: Reported

List of 14 Events for Episode 1 at Parícutin

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash
   - - - -    - - - - Lapilli
   - - - -    - - - - Bombs
   - - - -    - - - - Blocks
   - - - -    - - - - Lightning
   - - - -    - - - - Earthquakes (undefined) Before.
   - - - -    - - - - Earthquakes (undefined)
   - - - -    - - - - Property Damage
   - - - -    - - - - Evacuations
1943    - - - - Fatalities
1943 Feb 20    - - - - VEI (Explosivity Index)

1759 Sep 29 - 1774 Confirmed Eruption VEI: 4

Episode 1 | Eruption Jorullo
1759 Sep 29 - 1774 Evidence from Observations: Reported

List of 11 Events for Episode 1 at Jorullo

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Seismicity (volcanic) Before eruption.
   - - - -    - - - - Phreatic activity
   - - - -    - - - - Pyroclastic flow
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash violent, strong, or large
   - - - -    - - - - Lahar or Mudflow
   - - - -    - - - - Property Damage
   - - - -    - - - - Evacuations
1759 Sep 29    - - - - VEI (Explosivity Index)
1764    - - - - VEI (Explosivity Index)

[ 1050 ± 50 years ] Uncertain Eruption

Episode 1 | Eruption Valle de Santiago
1050 ± 50 years - Unknown Evidence from Unknown

List of 2 Events for Episode 1 at Valle de Santiago

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion Uncertain
   - - - -    - - - - Ash Uncertain

1140 BCE ± 865 years Confirmed Eruption  

Episode 1 | Eruption Cerro el Zoyate
1140 BCE ± 865 years - Unknown Evidence from Isotopic: 14C (calibrated)

List of 4 Events for Episode 1 at Cerro el Zoyate

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash

1880 BCE ± 150 years Confirmed Eruption VEI: 3

Episode 1 | Eruption Cerro el Jabalí
1880 BCE ± 150 years - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 6 Events for Episode 1 at Cerro el Jabalí

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash
   - - - -    - - - - Lapilli
1880 BCE ± 150 years    - - - - VEI (Explosivity Index)

2050 BCE (?) Confirmed Eruption  

Episode 1 | Eruption Valle de Santiago (La Alberca)
2050 BCE (?) - Unknown Evidence from Correlation: Anthropology

List of 6 Events for Episode 1 at Valle de Santiago (La Alberca)

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Phreatic activity
   - - - -    - - - - Pyroclastic flow
   - - - -    - - - - Ash
   - - - -    - - - - Lapilli
   - - - -    - - - - Blocks

2750 BCE ± 200 years Confirmed Eruption VEI: 3

Episode 1 | Eruption Cerro el Metate
2750 BCE ± 200 years - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 6 Events for Episode 1 at Cerro el Metate

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash
   - - - -    - - - - Lapilli
2750 BCE ± 200 years    - - - - VEI (Explosivity Index)

4140 BCE ± 300 years Confirmed Eruption  

Episode 1 | Eruption Cerro la Tinaja
4140 BCE ± 300 years - Unknown Evidence from Isotopic: 14C (calibrated)

List of 4 Events for Episode 1 at Cerro la Tinaja

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash

5940 BCE ± 335 years Confirmed Eruption  

Episode 1 | Eruption Cerro Grande?
5940 BCE ± 335 years - Unknown Evidence from Isotopic: 14C (calibrated)

List of 4 Events for Episode 1 at Cerro Grande?

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash

6480 BCE ± 300 years Confirmed Eruption VEI: 3

Episode 1 | Eruption Cerro la Taza
6480 BCE ± 300 years - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 6 Events for Episode 1 at Cerro la Taza

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash
   - - - -    - - - - Lapilli
6480 BCE ± 300 years    - - - - VEI (Explosivity Index)

7350 BCE ± 300 years Confirmed Eruption VEI: 3

Episode 1 | Eruption Hoyo el Huanillo
7350 BCE ± 300 years - Unknown Evidence from Isotopic: 14C (uncalibrated)

List of 6 Events for Episode 1 at Hoyo el Huanillo

Start Date End Date Event Type Event Remarks
   - - - -    - - - - Explosion
   - - - -    - - - - Lava flow
   - - - -    - - - - Cinder Cone
   - - - -    - - - - Ash
   - - - -    - - - - Lapilli
7350 BCE ± 300 years    - - - - VEI (Explosivity Index)
Deformation History

There is data available for 1 deformation periods. Expand each entry for additional details.


Deformation during 2007 - 2011 [Subsidence; Observed by InSAR]

Start Date: 2007 Stop Date: 2011 Direction: Subsidence Method: InSAR
Magnitude: 3.000 cm Spatial Extent: 3.00 km Latitude: Unknown Longitude: Unknown

Remarks: Lava flow subsidence at the base of Paricutin cinder cone

Figure (see Caption)

Averaged 2007?2011 LOS velocity map of the Trans-Mexican Volcanic Belt, from ALOS InSAR. Only pixels with a temporal coherence larger than 0.7 are shown. Red triangles: historically active volcanoes (bold: those active during the survey period). Black triangles: other volcanoes. Black diamonds: major cities near volcanoes. White arrow: relative plate convergence rate at the Cocos Trench. Positive LOS velocities (uplift) are shown in red and negative LOS velocities (subsidence) in blue. Labeled insets: zoomed in for volcanoes showing deformation (Pari?cutin) or volcanoes active during the time period of the survey (Colima and Popocate?petl). These insets have a smaller color scale. Bottom right inset: LOS velocity map of El Chicho?n, volcano located southeast of the area shown.

From: Chaussard et al. 2013.

Reference List: Fournier et al. 2010; Chaussard et al. 2013.

Full References:

Chaussard E, Amelung F, Aoki Y, 2013. Characterization of open and closed volcanic systems in Indonesia and Mexico using InSAR time series. J. Geophys. Res., 118(8), 3957-3969. https://doi.org/10.1002/jgrb.50288

Fournier, T. J., M. E. Pritchard, and S. N. Riddick, 2010. Duration, magnitude, and frequency of subaerial volcano deformation events: New results from Latin America using InSAR and a global synthesis. Geochemistry Geophysics Geosystems, 11: Q01003. https://doi.org/10.1029/2009GC002558

Emission History

There is no Emissions History data available for Michoacán-Guanajuato.

Photo Gallery

This photo shows an ash plume rising above Parícutin on 9 June 1943, seen here from the Uruapan highway to the east. Prevailing winds distribute the ash plume to the south. Other scoria cones appear on the horizon, some of the 1,000-plus scoria cones within the massive Michoacán-Guanajuato volcanic field.

Photo by William Foshag, 1943 (Smithsonian Institution). A roughly 15-second time-exposure during the night shows the incandescent trajectories of ejecta from Parícutin on 1 August 1943, near the start of the 1943-52 eruption. Periodic large explosions of bursting lava bubbles in the vent rapidly ejected incandescent lava spatter.

Photo by Carl Fries, 1943 (U.S. Geological Survey). Parícutin ejects a shower of incandescent lava blocks and bombs and an ash plume in this painting by Dr. Atl, the renowned Mexican artist.

Painting by Dr. Atl (published in Luhr and Simkin, 1993). The tower of the unfinished San Juan Parangaricutiro church rises above the lava flows that surrounded it in 1944. The Taquí lava flow began on 8 January 1944 from the SW base of Parícutin. Renewed lava extrusion on 24 April threatened the town of San Juan Parangaricutiro and impacted it 17 June. The church was surrounded by lava in July. By the time the flow ceased in early August it had a length of 10 km.

Photo by James Allan, 1985 (Smithsonian Institution). Parícutin, the volcano that erupted in cornfield in 1943, is the best-known feature of the Michoacán-Guanajuato volcanic field. The huge field contains over 1,400 vents covering a wide area of Michoacán and Guanajuato states. Scoria cones are the predominant volcanic form, and lava domes, maars, tuff rings, and lava flows are also present. Parícutin is seen here from the NE with Cerro de Tancítaro in the background.

Photo by James Allan, 1985 (Smithsonian Institution). The flat-topped Hoya el Huanillo cinder cone, located about 35 km NE of Parícutin, erupted during the early Holocene about 9300 years ago. It is seen here from the NW with the town of Cherán in the left distance near the Cerro Cucundicata cinder cone. In contrast to many other Michoacán cinder cones, only a small ash-covered lava flow was emitted from Hoya el Huanillo.

Copyrighted photo by Katia and Maurice Krafft, 1981. Parícutin cinder cone, born in a Mexican cornfield in 1943, is perhaps the world's best-known example of a pyroclastic cone. Pyroclastic cones (from the Greek words for "fire" and "broken") are created by the accumulation of explosively ejected fragmental material around a volcanic vent. Depending on the dominant type of ejecta, they are called cinder cones, scoria cones, pumice cones, ash cones, or tuff cones. Pyroclastic cones are typically tens of meters to several hundred meters high and often issue lava flows from vents at their base.

Copyrighted photo by Katia and Maurice Krafft, 1981. The renowned church of San Juan Parangaricutiro was surrounded by lava flows from Parícutin in July 1944. Only one of the two church steeples had been completed prior to the eruption. The interior of the church was dismantled only days before it was overrun by the lava flow. The west margin of the 1944 lava flow appears at the top, with faintly visible abandoned streets of the town beyond.

Copyrighted photo by Katia and Maurice Krafft, 1981 (published in Luhr and Simkin, 1993). An aerial view from the NNW on 5 March 1943, about two weeks after the start of the Parícutin eruption, shows the Quitzocho lava flow advancing to the NE as an ash plume rises from the scoria cone. The flow was about 6-15 m thick as it advanced.

Photo by Ezequiel Ordonez, 1943 (U.S. National Archives). An ash plume rises above the new Parícutin cone on 21 February 1943, the second day of the eruption. The new cone is about 30 m high and is just rising above the treetops in this view from the NE. During this early stage the cone had slope angles of 32 degrees toward the west and lower angles to the east. At this point lava had begun flowing to the east.

Photo by Salvador Ceja, 1943 (U.S. National Archives, published in Luhr and Simkin, 1993). An incandescent lava flow travels down a channel within solidified lava near the SW-flank vents of Parícutin in 1945. Lava flows at this time traveled NW over the site of the village of Parícutin. The Taquí lava flows erupted during 1944-45 and covered about 18 km2. The most striking feature of the Taquí flows was the development of hornitos (rootless vents) when molten lava was ejected through overlying solidified crust.

Photo by Ken Segerstrom, 1945 (U.S. Geological Survey, published in Luhr and Simkin, 1993). An ash plume rises from Parícutin in October 1944. The photo was taken from the north at the outskirts of the town of San Juan Parangaricutiro. Lava flows in the foreground had already buried the town; the church tower seen in many other photos of the Parícutin eruption is hidden behind the small tree to the right.

Photo by Carl Fries, 1945 (U.S. Geological Survey, published in Luhr and Simkin, 1993). An ash plume at Parícutin in 1944 is photographed from the first observatory cabin 1.5 km north, with local resident Celedonio Gutierrez in the foreground. Gutierrez was born in the nearby town of San Juan Parangaricutiro, which was inundated by lava flows, and became actively involved in collaborations with U.S. scientists throughout the eruption.

Photo by Ken Segerstrom, 1944 (U.S. Geological Survey, published in Luhr and Simkin, 1993). The first lava flow from Parícutin, the Quitzocho flow, moves northward over cornfields prepared for planting. An ash plume rises from the new cone, which by the time of this photo on 25 February, the 5th day of the eruption, was already more than 150 m high. Gas plumes rise from the advancing lava flow.

Photo by Instituto de Geología, 1943 (published in Luhr and Simkin, 1993). The steeple of the church of San Juan Parangaricutiro rises above surrounding lava fields in the center of the photo, seen here from the NE. The still-unfinished church was inundated by lava in July 1944, a month after flows began advancing into the town. The unvegetated, steeper-sided lava flows in the background were erupted later during 1944-46.

Photo by Jim Luhr, 1982 (Smithsonian Institution). This nighttime time-exposure of México's Parícutin volcano in 1948 shows a Strombolian eruption ejecting incandescent blocks that then rolled down the slopes of the cone. Parícutin is known as the volcano that erupted in a cornfield in 1943. It grew to a height of more than 150 m within the first week of its appearance and remained active until 1952.

Photo by Carl Fries, 1948 (U.S. Geological Survey). This sketch by Mexican artist Dr. Atl depicts the early moments of the Parícutin eruption in a cornfield near the village from which the volcano was named. A Tarascan farmer, Dionisio Pulido, observed the formation of the eruptive vent in his field about 1630 on 20 February 1943 as he was burning branches.

Sketch by Dr. Atl, 1943 (published in Luhr and Simkin, 1993). On 7 July 1944 a lava flow (left) approaches the church of San Juan Parangaricutiro. Residents had already evacuated the town when lava first entered the town on 17 June. By the time the flow stopped in early August the church was entirely surrounded by lava.

Photo by William Foshag, 1943 (Smithsonian Institution, published in Luhr and Simkin, 1993). In mid-November 1944 lava broke out of the SSW base of the cone, below the south vent in the crater, seen here from the S. The Ahuán flow advanced over the earlier Taquí flows in the foreground. A small lava intrusion was exposed in the flank of the cone a short distance above the vent. Ahuán flows traveled around the east side of the cone and to the north.

Photo by Frank Zierer, 1944 (published in Foshag and González-Reyna, 1956). A villager inspects the roof of a house in the village of Parícutin that was destroyed by heavy ashfall in the first year of the eruption. The village that the volcano was named after was located only 3 km NW of the new cone. Ashfall was particularly intense during the eruption's second to fifth months, and the town's 733 residents were forced to evacuate four months after the eruption began. The Mexican government provided new lands in Caltzontzín, 27 km to the SE.

Photo by Frederick Pough, 1943 (American Museum of Natural History). A vertical aerial photo of Parícutin taken on 26 May 1945 shows the cone at the bottom with the partially buried horseshoe-shaped Sapichu vent on its NE flank. Lava flows, forming the lighter-colored areas in the photo, surround the Quitzocho Ridge in the center of the photo and the older Cerro de Jarátiro scoria cone at the top. Ultimately nearly the entire Quitzocho Ridge was buried by lava flows.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL), 1:25,000, 1945. One of the first photographs taken of the Parícutin eruption shows an ash plume rising from the new volcano at 1800 on 20 February 1943, 1.5 hours after the start of the eruption. The photo was taken near Ticuiro, 5 km NNW of the volcano, with the fields of San Juan Parangaricutiro, later overrun by lava flows, in the foreground. Cerro de Canicjuata is the forested older cone to the right.

Photo by Luis Mora-Garcia, 1943 (published in Foshag and González-Reyna, 1956). A geologist observes an ash plume rising above the crater of Parícutin on 22 March 1944, as seen from 1 km SW at Mesa de Cocjarao. During March 1944 the eruptive activity ranged from small ash plumes accompanied by deep rumbling to large but almost soundless ash plumes, as was true with the plume shown here.

Photo by William Foshag, 1944 (Smithsonian Institution, published in Foshag and Gonzáles-Reyna, 1956). Villagers observe an ash plume rising above Parícutin in 1944 beyond the streets of San Juan Parangaricutiro, soon to be overrun by lava flows. In June and July 1944 lava advanced slowly through the town, which was incrementally evacuated as the flow progressed. Many residents, showing their deep attachment to the land, stayed until the lava overran the last segments of their property.

Photo by William Foshag, 1944 (Smithsonian Institution, published in Luhr and Simkin, 1993). Local Tarascan residents observe Parícutin volcano from Cerro de Equijuata, 2.5 km to the NNE, in March 1944. In this photo taken a little more than a year after the eruption began the Sapichu cone appears at the NE (left-hand) base of Parícutin. The rugged lava flows of June 1943 are visible in the middle of the photo. Heavy ashfall has defoliated trees and a thick ash deposit mantles the landscape.

Photo by Arno Brehme, 1944 (U.S. National Archives, published in Foshag and Gonzáles-Reyna, 1956). An ash plume towers 6 km above Parícutin on 24 March 1943, a little more than a month after the start of the eruption. The photo was taken from 3 km N in Tititzu and shows the advancing front of the Mesa del Corral lava flow in the middle ground, with the rim of the scoria cone behind it.

Photo by William Foshag, 1943 (Smithsonian Institution, published in Foshag and Gonzáles-Reyna, 1956). An ash plume rises from the summit crater of Parícutin sometime during 1946-48. A thick ash deposit covers the foreground. An estimated 4,500 cattle and 550 horses died during the heavy ashfall in the early months of the eruption, devastating the local people who depended on the animals for food, plowing, and transportation. Ashfall was deeper than 15 cm over a 300 km2 area around the volcano and continued with varying intensity throughout the 9-year-long eruption.

Photo by Ray Wilcox (U.S. Geological Survey). The Jorullo cone eruption began in 1759 in the Michoacán-Guanajuato Volcanic Field. In this view from the NW the unvegetated area visible on the center-horizon is the final lobe that flowed north. Volcán del Norte, one of Jorullo's four flank cones visible on the left horizon, produced a lava flow towards the west during the middle stages of the 1759-74 eruption.

Photo by Jim Luhr, 1996 (Smithsonian Institution). The principal vent of Jorullo formed the scoria cone seen here from the SSE that grew to 250 m in height during the first month and a half of the 1759 eruption. Lava flows were erupted at some unknown later time from four flank vents located along a NE-SW fissure cutting through the main cone.

Photo by Jim Luhr, 1996 (Smithsonian Institution). The most recent lava flows of the 1759-74 Jorullo eruption appear in the left and foreground of this view from the north with the sparsely vegetated cone of Jorullo to the upper right. Unlike earlier lava flows that were covered with ashfall from explosive eruptions, this latest does not and remains relatively unvegetated in this 1982 photo. Lava flows were erupted from NE-SW-trending flank vents and covered an area of 9 km2.

Photo by Jim Luhr, 1982 (Smithsonian Institution). Jorullo, a predecessor to Parícutin, was the first cinder cone of the Michoacán-Guanajuato volcanic field to be formed in historical time. The eruption began on September 29, 1759. Pyroclastic flows and mudflows in the first days caused much damage to neighboring haciendas. The first incandescent bombs were observed on October 8, and after October 14 the eruption was dominantly magmatic. By November 13 the cone had reached 250 m height. Major eruptions continued until 1764, and lesser eruptions were reported until 1774.

From the collection of Maurice and Katia Krafft. Lava flows in the western part of the Michoacán-Guanajuato volcanic field are seen here from the north. Cerro el Astillero, a scoria cone near the middle right-hand margin of the photo, was the source of the unvegetated lava flow that extends to the east and then south. Cerro el Pedegral, a cone near the lower left, produced lava flows to the west and south toward the upper part of the photo. This lava field is located near the town of Tancítaro and is among the many Holocene flows in the Michoacán-Guanajuato field.

Photo by Lee Siebert, 1997 (Smithsonian Institution). Since the end of the 1759-1774 eruption the Jorullo crater has been collapsing inward along steep, arcuate faults, increasing its dimensions to 400 x 500 m; its depth was 150 m by 1997.

Photo by Jim Luhr, 1997 (Smithsonian Institution). Jorullo scoria cone of the Michoacán-Guanajuato volcanic field is seen here from the ENE. The eruption began with phreatic and phreatomagmatic activity on 29 September 1759 with wet ashfall and lahars that caused damage to neighboring haciendas. By 13 November the cone had reached 250 m in height, and the eruption episode continued until 1774. The sparsely vegetated lava flow to the right was the produced near the end of the eruption.

Photo by Jim Luhr, 1997 (Smithsonian Institution). Parícutin, the volcano that grew in a cornfield in 1943, is a well-known feature of the Michoacán-Guanajuato volcanic field. The huge field contains over 1,400 vents covering a wide area across the Michoacán and Guanajuato states. Scoria cones are the predominant volcanic landform, and lava domes, maars, tuff rings, and lava flows are also present. Parícutin is seen here from the NE with the Nueva Juatita flank vent in the foreground, the main source of lava during the last five years of the eruption.

Photo by Jim Luhr, 1997 (Smithsonian Institution). By the end of the 9-year-long eruption of Parícutin, the new scoria cone had risen 424 m above the surface of the original cornfield. The 900-m-wide oval-shaped cone is elongated in a NW-SE direction and is truncated by a circular 280-m-wide crater. The western peak (right) is the highest point on the crater rim. The NE-flank peak of Nuevo Juatita is in the foreground with its top covered by white minerals from fumaroles, and was the main source of lava flows during the last five years of the eruption.

Photo by Jim Luhr, 1997 (Smithsonian Institution). The small light-colored spire in the center of the photo is the renowned steeple of the church of San Juan Parangaricutiro, which was surrounded by lava flows from Parícutin volcano in 1944 in this view from the NE. The steep-sided, viscous lava flows in the background were erupted later, during 1944-46. This is one of numerous lava flows within the Michoacan-Guanajuato volcanic field.

Photo by Jim Luhr, 1997 (Smithsonian Institution). The renowned Parícutin scoria cone, which grew from a Mexican cornfield beginning in 1943, is one of the roughly 1,000 cones that form the massive Michoacán-Guanajuato volcanic field in central Mexico. White mineral deposits formed across the top of Nuevo Juatita in the foreground, a NE-flank vent that was the main source of lava flows during the last five years of the 1943-1952 eruption.

Photo by Jim Luhr, 1997 (Smithsonian Institution). The Jorullo cone (right-center) is seen here from the SSW with Cerro la Pilita cone in the foreground. The small, less-vegetated cones immediately to the left are the SW-flank vents that produced lava flows during the middle part of the 1759-1774 eruption. Cerro la Pilita is an older cone that produced pre-historical lava flows along a narrow channel to the SW.

Photo by Jim Luhr, 1997 (Smithsonian Institution). A nighttime Strombolian eruption at Parícutin ejects incandescent blocks and bombs onto the flanks of the scoria cone. Ejecta like this accumulated around the vent to build the cone during February 1943 to February 1952.

Photo by Carl Fries, 1945 (U.S. Geological Survey, published in Luhr and Simkin, 1993). The Valle de Santiago in the NE part of the Michoacán-Guanajuato volcanic field NW of Lake Yuriria contains a group of maars formed by phreatomagmatic eruptions. The maars, four of which are lake-filled, range from 0.8 to 1.8 km in diameter, are 80 to 180 m deep, and are probably Holocene in age. This photo shows the Hoya Rincón de Parangüeo maar at the northern end of the group.

Photo by Jim Luhr, 1982 (Smithsonian Institution). Paracho volcano is one of the many cones of the Michoacán-Guanajuato volcanic field. It is seen here from the west with its summit crater filled by a flat-topped lava dome that is the site of a radio antenna station. The dome fills the upper end of a large erosional valley that extends down the flank from the summit. Edifice collapse has occurred on the eastern side of the volcano, producing a major debris avalanche deposit covering an area of about 175 km2.

Photo by Hugo Delgado, 1991 (Universidad Nacional Autónoma de México). Lava flows from Parícutin (upper center) within the Michoacan-Guanajuato volcanic field cover much of the northern half of this photo. The small white dot immediately NE of the cone is the flank vent of Nuevo Juatita. The latest lava flows that formed during 1952 originated from this vent and form the darker-colored flows that extend to the SE. Cerro Tzirapan is the larger scoria cone near the center, and older cones are to the upper left.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL), 1970. Ashfall from Hoyo el Huanillo scoria cone (lower left) was radiocarbon dated to have formed about 9,300 years ago within the Michoacan-Guanajuato volcanic field. A small ash-covered lava flow extends a short distance to the NW of the cone, which is located 35 km NE of Parícutin. The Cerro Cucundicata scoria cone is to the lower right, and the Cerro Borrego and Cerro Tarucun cones are to the N, NE of the town of Cherán. The eroded Cerro Pacaracua edifice forms much of the upper part of the photo.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL). Jorullo volcano and associated lava flows in the Michoacan-Guanajuato volcanic field are visible in the bottom of this photo. Four NE-SW-trending vents flank the main cone, which erupted during 1759-1774. The 1759-74 lava flows appear in varying shades of gray, with the initial (and largest) flows being lighter in color (due to partial ash cover), and the most recent ash-free lava being darker and extending to the NW and NE. Jorullo lies about 80 km SE of Parícutin.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL). Cerro el Jabalí (upper left) and the adjacent Cerro el Sapien (immediately to the east) of the Michoacan-Guanajuato volcanic field produced the unvegetated lava flow extending across the top of the photo. Ashfall from Cerro el Jabalí scoria cone, located about 15 km SE of Parícutin, erupted about 3,830 years ago. The city of Uruapan is in the right side of the photo, south of the circular Costo (Cerro Cotji) maar.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL). Volcán la Mina is the scoria cone near the center-left margin of the photo with the lava flow emplaced through the collapsed NE crater rim. It formed about 17,170 years ago within the Michoacan-Guanajuato volcanic field, around 90 km ENE of Parícutin. The SW cone containing a crater that also opens to the NE is Volcán el Melón (lower left), which was the source of a lava flow that traveled east to the present-day outskirts of the village of Capula.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL). This aerial photo shows part of the Michoacan-Guanajuato volcanic field. Cerro el Pueblito (upper left), radiocarbon dated to about 29,000 years ago, produced the lava flow that extends eastward across the photo that flowed around the older Cerro las Cabras cone to the right. South of this lava flow is the La Vibor lava flow. Cerro Arena is the cone near the center of the photo.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL). The large forested (dark) area near the center of the photo is Cerro Tecolote, an eroded stratovolcano located roughly 50 km NE of Parícutin within the Michoacan-Guanajuato volcanic field. Cerro las Cabras (upper left) is a scoria cone that produced the lava flow extending across the upper part of the photo. Mexican Highway 15 travels across the flow, which is of Pleistocene age. Cerro Pajarito is one of the scoria cones south of Cerro Tecolote, and another cone is seen here on the SW flank.

Aerial photo by Comisión de Estudios del Territorio Nacional (CETENAL). The Hoya Rincón de Parangüeo maar rises directly above the town of the same name located on the lower southern flank. A brackish lake of seasonally variable size partially fills the floor of the 2-km-wide maar, seen here from its southern rim. The high point on the northern rim rises 450 m above the crater floor. Rincón de Parangueo is part of the Valle de Santiago maar field on the NE side of the Michoacán-Guanajuato volcanic field and is about 7 km NW of the town of Valle de Santiago.

Photo by Jim Luhr, 2002 (Smithsonian Institution). Geologist Todd Housh observes pyroclastic surge deposits in the wall of an abandoned quarry on the north flank of Hoya Estrada maar, directly west of the town of Valle de Santiago. The exposure shows laminar and dune form-bedded surge deposits at the bottom with laminar ashfall layers at the top. The direction that the pyroclastic surges traveled was from right to left.

Photo by Jim Luhr, 2002 (Smithsonian Institution). The walls of a quarry on the SW flank of Hoya Estrada maar close to the city of Valle de Santiago show a spectacular sequence of deposits from the maar-forming eruptions. Most of the outcrop consists of gray-colored dominantly planar pyroclastic surge beds. The three prominent light-colored layers are ashfall deposits. The largest ash layer is about 2 m thick just above the middle of the outcrop in this view looking towards the vent.

Photo by Jim Luhr, 2002 (Smithsonian Institution). A basaltic clast with a light-colored silicic rim from the Hoya Estrada maar. The coin provides scale.

Photo by Jim Luhr, 2002 (Smithsonian Institution). Several maars of the Michoacan-Guanajuato volcanic field are visible in this photo. The 600-m-wide Hoya Solis maar is seen from the SW rim of Hoya Blanca maar, immediately SW of the city of Valle de Santiago. The rim of Hoya de Cintora maar lies beyond Hoya Solis below the far-left horizon.

Photo by Jim Luhr, 2002 (Smithsonian Institution).
GVP Map Holdings

Maps are not currently available due to technical issues.

Smithsonian Sample Collections Database

The following 623 samples associated with this volcano can be found in the Smithsonian's NMNH Department of Mineral Sciences collections, and may be availble for research (contact the Rock and Ore Collections Manager). Catalog number links will open a window with more information.

Catalog Number Sample Description Lava Source Collection Date
NMNH 104717 Sal Ammoniac PARICUTIN --
NMNH 104717-00 Sal Ammoniac -- --
NMNH 104718-00 Sal Ammoniac -- --
NMNH 104718-01 Sal Ammoniac -- --
NMNH 105184-00 Sal Ammoniac -- --
NMNH 105184-01 Sal Ammoniac -- --
NMNH 105184-02 Sal Ammoniac -- --
NMNH 105184-03 Sal Ammoniac -- --
NMNH 105184-04 Sal Ammoniac -- --
NMNH 105184-05 Sal Ammoniac -- --
NMNH 105184-06 Sal Ammoniac -- --
NMNH 105184-07 Sal Ammoniac -- --
NMNH 105184-08 Sal Ammoniac -- --
NMNH 105184-09 Sal Ammoniac -- --
NMNH 105184-10 Sal Ammoniac -- --
NMNH 105184-11 Sal Ammoniac -- --
NMNH 105184-12 Sal Ammoniac -- --
NMNH 106882-00 Sal Ammoniac -- --
NMNH 106882-01 Sal Ammoniac -- --
NMNH 106923 Volcanic Sublimate PARICUTIN --
NMNH 107427 Volcanic Sublimate PARICUTIN --
NMNH 108058 Basalt PARICUTIN, QUITZOCHO FLOW --
NMNH 108059 Basalt PARICUTIN --
NMNH 108060 Basalt PARICUTIN, QUITZOCHO RIDGE, SMALL FLOW --
NMNH 108061 Basalt PARICUTIN --
NMNH 108062 Basalt PARICUTIN --
NMNH 108063 Basalt PARICUTIN --
NMNH 108064 Basalt PARICUTIN --
NMNH 108065 Basalt PARICUTIN --
NMNH 108066 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108067 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108068 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108069 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108070 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108071 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108072 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108072 Basalt PARICUTIN --
NMNH 108073 Basalt PARICUTIN --
NMNH 108074 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108075 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108076 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108077 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108078 Basalt PARICUTIN, SAPICHU VENT --
NMNH 108080 Basalt PARICUTIN, PARANGARICUTIRO TONGUE --
NMNH 108081 Basalt PARICUTIN, PARANGARICUTIRO TONGUE --
NMNH 108082 Basalt PARICUTIN, PARANGARICUTIRO TONGUE --
NMNH 108083 Basalt PARICUTIN --
NMNH 108084-1 Basalt PARICUTIN --
NMNH 108084-2 Basalt PARICUTIN --
NMNH 108085 Basalt PARICUTIN --
NMNH 108086 Basalt PARICUTIN --
NMNH 108087 Basalt PARICUTIN --
NMNH 108088 Basalt PARICUTIN --
NMNH 108089 Basalt PARICUTIN --
NMNH 108090 Basalt PARICUTIN --
NMNH 108091 Basalt PARICUTIN --
NMNH 108092 Basalt PARICUTIN --
NMNH 108093 Basalt PARICUTIN --
NMNH 108094 Basalt PARICUTIN --
NMNH 108095 Basalt PARICUTIN --
NMNH 108096 Basalt PARICUTIN --
NMNH 108097 Basalt PARICUTIN --
NMNH 108098 Basalt PARICUTIN --
NMNH 108098 Basalt PARICUTIN --
NMNH 108099 Basalt PARICUTIN --
NMNH 108100 Basalt PARICUTIN --
NMNH 108100 Basalt PARICUTIN --
NMNH 108101 Basalt PARICUTIN --
NMNH 108102 Basalt PARICUTIN --
NMNH 108103 Basalt PARICUTIN --
NMNH 108104 Basalt PARICUTIN --
NMNH 108105 Basalt PARICUTIN --
NMNH 108106 Basalt PARICUTIN --
NMNH 108108 Basalt PARICUTIN --
NMNH 108109 Basalt PARICUTIN --
NMNH 108110 Basalt PARICUTIN --
NMNH 108112-1 Basalt PARICUTIN --
NMNH 108112-2 Basalt PARICUTIN --
NMNH 108113 Basalt PARICUTIN --
NMNH 108114-1 Basalt PARICUTIN --
NMNH 108114-2 Basalt PARICUTIN --
NMNH 108115 Basalt PARICUTIN --
NMNH 108115 Basalt PARICUTIN --
NMNH 108116 Basalt PARICUTIN --
NMNH 108117 Basalt PARICUTIN --
NMNH 108118 Basalt PARICUTIN --
NMNH 108119 Basalt PARICUTIN --
NMNH 108119 Basalt PARICUTIN --
NMNH 108120 Basalt PARICUTIN --
NMNH 108120-1 Basalt PARICUTIN --
NMNH 108120-2 Basalt PARICUTIN --
NMNH 108121-1 Basalt PARICUTIN --
NMNH 108121-2 Basalt PARICUTIN --
NMNH 108121-3 Basalt PARICUTIN --
NMNH 108122 Basalt PARICUTIN --
NMNH 108122 Basalt PARICUTIN --
NMNH 108123 Basalt PARICUTIN --
NMNH 108124 Basalt PARICUTIN --
NMNH 108125 Basalt PARICUTIN --
NMNH 108126-1 Basalt PARICUTIN --
NMNH 108126-2 Basalt PARICUTIN --
NMNH 108126-3 Basalt PARICUTIN --
NMNH 108127-1 Basalt PARICUTIN --
NMNH 108127-2 Basalt PARICUTIN --
NMNH 108128 Basalt PARICUTIN --
NMNH 108128 Basalt PARICUTIN --
NMNH 108129 Basalt PARICUTIN --
NMNH 108130 Basalt PARICUTIN --
NMNH 108131 Basalt PARICUTIN --
NMNH 108132-1 Basalt PARICUTIN --
NMNH 108132-2 Basalt PARICUTIN --
NMNH 108133-1 Basalt PARICUTIN --
NMNH 108133-2 Basalt PARICUTIN --
NMNH 108134 Volcanic Ash PARICUTIN --
NMNH 108135 Unidentified PARICUTIN --
NMNH 108136 Unidentified PARICUTIN --
NMNH 108137 Unidentified PARICUTIN --
NMNH 108138 Unidentified PARICUTIN --
NMNH 108139 Unidentified PARICUTIN --
NMNH 108140 Volcanic Ash PARICUTIN --
NMNH 108141 Volcanic Ash PARICUTIN --
NMNH 108142 Volcanic Ash PARICUTIN --
NMNH 108143 Volcanic Ash PARICUTIN --
NMNH 108144 Volcanic Ash PARICUTIN --
NMNH 108145 Volcanic Ash PARICUTIN --
NMNH 108146 Volcanic Ash PARICUTIN --
NMNH 108147 Volcanic Ash PARICUTIN --
NMNH 108148 Volcanic Ash PARICUTIN --
NMNH 108149 Volcanic Ash PARICUTIN --
NMNH 108150 Volcanic Ash PARICUTIN --
NMNH 108151 Unidentified PARICUTIN --
NMNH 108152 Volcanic Ash PARICUTIN --
NMNH 108153 Unidentified PARICUTIN --
NMNH 108154 Volcanic Ash PARICUTIN --
NMNH 108155 Unidentified PARICUTIN, SAPICHU VENT --
NMNH 108156 Unidentified PARICUTIN --
NMNH 108157 Volcanic Ash PARICUTIN --
NMNH 108158 Unidentified PARICUTIN --
NMNH 108160-00 Aphthitalite -- --
NMNH 108162-00 Chloraluminite -- --
NMNH 108163 Basalt PARICUTIN --
NMNH 108166-1 Basalt PARICUTIN --
NMNH 108166-2 Basalt PARICUTIN --
NMNH 108166-3 Basalt PARICUTIN --
NMNH 108166-4 Basalt PARICUTIN --
NMNH 108166-5 Basalt PARICUTIN --
NMNH 108166-6 Basalt PARICUTIN --
NMNH 108167 Basalt PARICUTIN --
NMNH 108170-1 Basalt PARICUTIN --
NMNH 108170-2 Basalt PARICUTIN --
NMNH 108171 Basalt PARICUTIN --
NMNH 108172 Basalt PARICUTIN --
NMNH 108173 Volcanic Ash PARICUTIN --
NMNH 108174 Volcanic Ash PARICUTIN --
NMNH 108175 Volcanic Sublimate PARICUTIN --
NMNH 108176 Basalt PARICUTIN --
NMNH 108176 Basalt PARICUTIN --
NMNH 108184 Basalt PARICUTIN --
NMNH 108293 Volcanic Bomb PARICUTIN --
NMNH 108293 Volcanic Bomb PARICUTIN --
NMNH 108294 Volcanic Bomb PARICUTIN --
NMNH 108295 Basalt PARICUTIN --
NMNH 108304 Basalt PARICUTIN --
NMNH 108305 Basalt PARICUTIN --
NMNH 108607 Lava PARICUTIN --
NMNH 108608 Lava PARICUTIN --
NMNH 108609 Basalt PARICUTIN --
NMNH 108795-1 Basalt PARICUTIN --
NMNH 108795-2 Basalt PARICUTIN --
NMNH 108795-3 Basalt PARICUTIN --
NMNH 108795-4 Basalt PARICUTIN --
NMNH 108796 Painting PARICUTIN --
NMNH 108862 Basalt PARICUTIN --
NMNH 108863 Basalt PARICUTIN --
NMNH 108984-1 Lava -- --
NMNH 108986 Basalt PARICUTIN --
NMNH 108987 Basalt PARICUTIN --
NMNH 109064 Basalt PARICUTIN --
NMNH 109089 Basalt PARICUTIN --
NMNH 109353 Basalt PARICUTIN --
NMNH 109354 Basalt PARICUTIN, ZAPICHO CINDER CONE --
NMNH 114709 Volcanic Ash PARICUTIN --
NMNH 114711 Volcanic Rock PARICUTIN --
NMNH 114712 Volcanic Rock PARICUTIN --
NMNH 114713 Volcanic Rock PARICUTIN --
NMNH 114714 Volcanic Rock PARICUTIN --
NMNH 114715 Basalt PARICUTIN --
NMNH 114716 Unidentified PARICUTIN --
NMNH 114717 Volcanic Ash PARICUTIN --
NMNH 114718 Opal PARICUTIN --
NMNH 114719 Opal PARICUTIN --
NMNH 114720 Basalt PARICUTIN --
NMNH 114721 Opal PARICUTIN --
NMNH 114722 Unidentified PARICUTIN --
NMNH 114723 Ammonium Chloride PARICUTIN --
NMNH 114724 Volcanic Sublimate PARICUTIN --
NMNH 114725 Sal Ammoniac PARICUTIN --
NMNH 114726 Unidentified PARICUTIN --
NMNH 114727 Volcanic Ash (?) PARICUTIN --
NMNH 114728 Volcanic Sublimate PARICUTIN --
NMNH 116284-1 Basalt JORULLO 10 Dec 1946
NMNH 116284-10A Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-10B Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-11A Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-11B Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-11C Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-12 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-13A Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-13B Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-14 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-15 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-16 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-17 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-18 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-19 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-1A Basalt JORULLO 10 Dec 1946
NMNH 116284-1B Basalt JORULLO 10 Dec 1946
NMNH 116284-2 Volcanic Ash JORULLO 11 Dec 1946
NMNH 116284-20A Basalt JORULLO 12 Dec 1946
NMNH 116284-20B Basalt JORULLO 12 Dec 1946
NMNH 116284-20C Basalt JORULLO 12 Dec 1946
NMNH 116284-21B Basalt JORULLO 12 Dec 1946
NMNH 116284-21C Basalt JORULLO 12 Dec 1946
NMNH 116284-22 Volcanic Ash JORULLO 12 Dec 1946
NMNH 116284-23 Volcanic Ash JORULLO 12 Dec 1946
NMNH 116284-24 Basalt JORULLO 12 Dec 1946
NMNH 116284-3 Volcanic Ash JORULLO 11 Dec 1946
NMNH 116284-4 Basalt JORULLO 11 Dec 1946
NMNH 116284-5 Volcanic Ash JORULLO 11 Dec 1946
NMNH 116284-6 Volcanic Bomb JORULLO 12 Dec 1946
NMNH 116284-7 Volcanic Bomb JORULLO 12 Dec 1946
NMNH 116284-8 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116284-9 Andesitic Rock JORULLO 12 Dec 1946
NMNH 116289-1 Lava PARICUTIN --
NMNH 116289-10 Lava PARICUTIN, ZAPICHU 10 Jun 1947
NMNH 116289-11 Lava PARICUTIN 5 Sep 1947
NMNH 116289-12 Lava PARICUTIN 30 Nov 1947
NMNH 116289-13 Lava PARICUTIN 2 Sep 1948
NMNH 116289-14 Basaltic Andesite PARICUTIN 19 May 1949
NMNH 116289-15 Basaltic Andesite PARICUTIN 13 Dec 1949
NMNH 116289-16 Basaltic Andesite PARICUTIN 1 Sep 1950
NMNH 116289-17 Basaltic Andesite PARICUTIN 25 May 1951
NMNH 116289-18 Basaltic Andesite PARICUTIN 28 Nov 1951
NMNH 116289-19 Basaltic Andesite PARICUTIN, NUEVO JUATITA 8 Mar 1952
NMNH 116289-2 Lava PARICUTIN --
NMNH 116289-20 Xenolithic Volcanic Bomb PARICUTIN 1 May 1943
NMNH 116289-21 Dacitic Xenolith PARICUTIN 1 Jan 1943
NMNH 116289-22 Xenolith PARICUTIN --
NMNH 116289-23 Granitic Xenolith PARICUTIN --
NMNH 116289-3 Lava PARICUTIN --
NMNH 116289-4 Lava PARICUTIN --
NMNH 116289-5 Lava PARICUTIN --
NMNH 116289-6 Lava PARICUTIN --
NMNH 116289-7 Lava PARICUTIN --
NMNH 116289-8 Lava PARICUTIN, AHUAN VENT --
NMNH 116289-9 Lava PARICUTIN, ZAPICHU 9 Apr 1947
NMNH 116290 Aluminous Basalt PARICUTIN --
NMNH 116291-1 Lava PARICUTIN --
NMNH 116291-2 Lava PARICUTIN --
NMNH 116291-3 Lava PARICUTIN --
NMNH 116291-4 Basaltic Volcanic Bomb PARICUTIN 21 Jun 1943
NMNH 116291-5 Lava PARICUTIN --
NMNH 116292-1 Volcanic Ash PARICUTIN 25 Mar 1943
NMNH 116292-2 Volcanic Ash PARICUTIN 27 Mar 1943
NMNH 116292-3 Lapilli PARICUTIN 18 Jul 1943
NMNH 116292-4 Lava PARICUTIN 16 Jul 1943
NMNH 116292-5 Basaltic Volcanic Bomb PARICUTIN --
NMNH 116292-6 Basaltic Volcanic Bomb PARICUTIN --
NMNH 116292-7 Xenolithic Volcanic Bomb PARICUTIN 4 Feb 1944
NMNH 116292-8 Xenolithic Volcanic Bomb PARICUTIN 4 Feb 1944
NMNH 116292-9 Xenolithic Volcanic Bomb PARICUTIN 4 Feb 1944
NMNH 116293-1 Obsidian Xenolith PARICUTIN 1 Jul 1945
NMNH 116293-1 Pumice PARICUTIN --
NMNH 116293-10 Lava PARICUTIN --
NMNH 116293-11 Volcanic Bomb PARICUTIN --
NMNH 116293-12 Volcanic Bomb PARICUTIN --
NMNH 116293-2 White Xenolith PARICUTIN 1 Mar 1944
NMNH 116293-3 Xenolith PARICUTIN 1 Jan 1943
NMNH 116293-4 Dacitic Xenolith PARICUTIN 1 Jan 1943
NMNH 116293-5 Dacitic Xenolith PARICUTIN --
NMNH 116293-6 Xenolith PARICUTIN --
NMNH 116293-7 Lava PARICUTIN --
NMNH 116293-8 Lava PARICUTIN --
NMNH 116293-9 Lava PARICUTIN --
NMNH 116294-1 Lava PARICUTIN 1 Jan 1945
NMNH 116294-10 Volcanic Bomb PARICUTIN 1 Jan 1945
NMNH 116294-11 Lava PARICUTIN 1 Jan 1945
NMNH 116294-12 Lava PARICUTIN 1 Jan 1945
NMNH 116294-13 Lava PARICUTIN 1 Jan 1945
NMNH 116294-14 Lava PARICUTIN 1 Jan 1945
NMNH 116294-15 Lava PARICUTIN 1 Jan 1945
NMNH 116294-16 Lava PARICUTIN 1 Jan 1945
NMNH 116294-17 Lava PARICUTIN 1 Jan 1945
NMNH 116294-18 Lava PARICUTIN 1 Jan 1945
NMNH 116294-19 Lava PARICUTIN 1 Jan 1945
NMNH 116294-2 Basaltic Volcanic Bomb PARICUTIN 1 Jan 1945
NMNH 116294-20 Lava PARICUTIN 1 Jan 1945
NMNH 116294-21 Lava PARICUTIN 1 Jan 1946
NMNH 116294-22 Xenolith PARICUTIN 1 Jan 1946
NMNH 116294-23 Volcanic Bomb PARICUTIN 1 Jan 1946
NMNH 116294-24 Lava PARICUTIN 7 Feb 1946
NMNH 116294-25 Lava PARICUTIN 1 Jan 1946
NMNH 116294-26 Lava PARICUTIN 1 Jan 1946
NMNH 116294-27 Lava PARICUTIN 1 Jan 1946
NMNH 116294-28 Lava PARICUTIN 1 Jan 1946
NMNH 116294-29 Xenolithic Volcanic Bomb PARICUTIN 31 Jan 1946
NMNH 116294-3 Lava PARICUTIN 1 Jan 1945
NMNH 116294-4 Lava PARICUTIN 1 Jan 1945
NMNH 116294-5 Volcanic Bomb PARICUTIN 1 Jan 1945
NMNH 116294-6 Lava PARICUTIN 1 Jan 1945
NMNH 116294-7 Lava PARICUTIN 1 Jan 1945
NMNH 116294-8 Lava PARICUTIN 1 Jan 1945
NMNH 116294-9 Lava PARICUTIN 1 Jan 1945
NMNH 116295-1 Basalt PARICUTIN 23 Dec 1946
NMNH 116295-10 Lava PARICUTIN, PUERTECITO 25 Feb 1947
NMNH 116295-11 Lava PARICUTIN 30 May 1947
NMNH 116295-12 Xenolith PARICUTIN --
NMNH 116295-13 Volcanic Bomb PARICUTIN 10 Jun 1947
NMNH 116295-14 Volcanic Bomb PARICUTIN 10 Jun 1947
NMNH 116295-16 Volcanic Bomb PARICUTIN 15 Jun 1947
NMNH 116295-17 Lava PARICUTIN, JUATITO 21 Aug 1947
NMNH 116295-18 Lava PARICUTIN, PUERTECITO 28 Aug 1947
NMNH 116295-19 Lava PARICUTIN 28 Aug 1947
NMNH 116295-2 Basalt PARICUTIN 26 Dec 1946
NMNH 116295-20 Lava PARICUTIN 20 Sep 1947
NMNH 116295-21 Lava PARICUTIN 29 Sep 1947
NMNH 116295-22 Lava PARICUTIN 24 Sep 1947
NMNH 116295-23 Lava PARICUTIN 24 Sep 1947
NMNH 116295-24 Lava PARICUTIN 29 Sep 1947
NMNH 116295-25 Lava PARICUTIN 29 Sep 1947
NMNH 116295-26 Lava PARICUTIN 1 Oct 1947
NMNH 116295-27 Lava PARICUTIN 1 Oct 1947
NMNH 116295-28 Volcanic Bomb PARICUTIN 30 Nov 1947
NMNH 116295-29 Basaltic Andesite PARICUTIN 30 Nov 1947
NMNH 116295-3 Lava PARICUTIN 9 Jan 1947
NMNH 116295-30 Lava PARICUTIN 30 Dec 1947
NMNH 116295-31 Volcanic Bomb (?) PARICUTIN --
NMNH 116295-32 Lava PARICUTIN 12 Jan 1948
NMNH 116295-33 Salic Xenolith PARICUTIN, TZINTZUNGO, CERRO DE 22 Jan 1948
NMNH 116295-34 Basaltic Lava PARICUTIN 2 Sep 1948
NMNH 116295-35 Xenolith PARICUTIN, TZINTZUNGO, CERRO DE 1 Apr 1948
NMNH 116295-36 Lava PARICUTIN, PARACHO, CERROS DE 2 Aug 1948
NMNH 116295-37 Lava PARICUTIN 18 Nov 1948
NMNH 116295-4 Lava PARICUTIN 9 Jan 1947
NMNH 116295-5 Lava PARICUTIN 18 Jan 1947
NMNH 116295-6 Lava PARICUTIN 18 Jan 1947
NMNH 116295-7 Lava PARICUTIN, CAPATZIN 18 Jan 1947
NMNH 116295-8 Lava PARICUTIN, AHUAN 20 Feb 1947
NMNH 116295-9 Lava PARICUTIN, PUERTECITO 20 Feb 1947
NMNH 116296-1 Basaltic Andesite PARICUTIN 1 Jan 1949
NMNH 116296-10 Basaltic Andesite PARICUTIN 8 Jul 1950
NMNH 116296-11 Basaltic Andesite PARICUTIN 1 Jan 1950
NMNH 116296-12 Basaltic Andesite PARICUTIN 1 Jan 1950
NMNH 116296-13 Basaltic Andesite PARICUTIN 1 Jan 1947
NMNH 116296-14 Basaltic Andesite PARICUTIN 1 Jan 1950
NMNH 116296-15 Basaltic Andesite PARICUTIN 1 Jan 1950
NMNH 116296-16 Basaltic Andesite PARICUTIN 1 Jan 1950
NMNH 116296-17 Basaltic Andesite PARICUTIN 29 Dec 1950
NMNH 116296-18 Basaltic Andesite PARICUTIN 11 Mar 1951
NMNH 116296-19 Basaltic Andesite PARICUTIN 11 Mar 1951
NMNH 116296-2 Basaltic Andesite PARICUTIN 1 Jan 1949
NMNH 116296-20 Basaltic Andesite PARICUTIN 11 Mar 1951
NMNH 116296-21 Basaltic Andesite PARICUTIN 25 May 1951
NMNH 116296-22 Basaltic Andesite PARICUTIN 11 Jul 1951
NMNH 116296-23 Basaltic Andesite PARICUTIN 11 Jul 1951
NMNH 116296-24 Basaltic Andesite PARICUTIN 11 Jul 1951
NMNH 116296-25 Basaltic Andesite PARICUTIN 12 Jul 1951
NMNH 116296-26 Basaltic Andesite PARICUTIN 11 Jul 1951
NMNH 116296-27 Basaltic Andesite PARICUTIN 15 Oct 1951
NMNH 116296-28 Basaltic Andesite PARICUTIN --
NMNH 116296-29 Volcanic Ash PARICUTIN 29 Jan 1952
NMNH 116296-3 Basaltic Andesite PARICUTIN 17 Oct 1949
NMNH 116296-30 Basaltic (?) Andesite PARICUTIN 1 Jan 1952
NMNH 116296-31 Basaltic (?) Andesite PARICUTIN 30 Apr 1952
NMNH 116296-32 Basaltic Andesite PARICUTIN 30 Apr 1952
NMNH 116296-33 Basaltic Andesite PARICUTIN 31 Jan 1952
NMNH 116296-34 Basaltic Andesite PARICUTIN 30 Apr 1952
NMNH 116296-35 Monzonite (?) PARICUTIN --
NMNH 116296-36 Basaltic Andesite PARICUTIN, NUEVO JUATITA 27 Oct 1952
NMNH 116296-37 Monzonite (?) PARICUTIN --
NMNH 116296-38 Monzonite (?) PARICUTIN --
NMNH 116296-4 Basaltic Andesite PARICUTIN 17 Oct 1949
NMNH 116296-5 Basaltic Andesite PARICUTIN 14 Dec 1949
NMNH 116296-6 Basaltic Andesite PARICUTIN 20 Feb 1950
NMNH 116296-7 Basaltic Andesite PARICUTIN 14 Dec 1949
NMNH 116296-8 Basaltic Andesite PARICUTIN 27 Apr 1950
NMNH 116296-9 Basaltic Andesite PARICUTIN 14 Dec 1949
NMNH 116297-1 Tuff VALLE DE SANTIAGO --
NMNH 116297-2 Tuff VALLE DE SANTIAGO --
NMNH 116297-3 Tuff VALLE DE SANTIAGO --
NMNH 116297-4 Tuff VALLE DE SANTIAGO --
NMNH 116297-5 Tuff VALLE DE SANTIAGO --
NMNH 116300-1 Volcanic Ash PARICUTIN 18 Dec 1946
NMNH 116300-10 Volcanic Ash PARICUTIN 24 Apr 1947
NMNH 116300-11 Volcanic Ash PARICUTIN 2 Nov 1947
NMNH 116300-12 Volcanic Ash PARICUTIN 5 Nov 1947
NMNH 116300-13 Volcanic Ash PARICUTIN 8 Nov 1947
NMNH 116300-14 Volcanic Ash PARICUTIN 12 Nov 1947
NMNH 116300-15 Volcanic Ash PARICUTIN 17 Nov 1947
NMNH 116300-16 Volcanic Ash PARICUTIN 21 Nov 1947
NMNH 116300-17 Volcanic Ash PARICUTIN 22 Nov 1947
NMNH 116300-18 Volcanic Ash PARICUTIN 23 Nov 1947
NMNH 116300-19 Volcanic Ash PARICUTIN 8 Dec 1947
NMNH 116300-2 Volcanic Ash PARICUTIN 3 Jan 1947
NMNH 116300-20 Volcanic Ash PARICUTIN 16 Dec 1947
NMNH 116300-21 Volcanic Ash PARICUTIN 20 Dec 1947
NMNH 116300-22 Volcanic Ash PARICUTIN 25 Dec 1947
NMNH 116300-23 Volcanic Ash PARICUTIN 26 Dec 1947
NMNH 116300-24 Volcanic Ash PARICUTIN 27 Dec 1947
NMNH 116300-25 Volcanic Ash PARICUTIN 30 Dec 1947
NMNH 116300-26 Volcanic Ash PARICUTIN 9 Jan 1947
NMNH 116300-27 Volcanic Ash PARICUTIN 18 Jan 1947
NMNH 116300-28 Volcanic Ash PARICUTIN 27 Jan 1947
NMNH 116300-29 Volcanic Ash PARICUTIN 22 Mar 1947
NMNH 116300-3 Volcanic Ash PARICUTIN 7 Jan 1947
NMNH 116300-30 Volcanic Ash PARICUTIN 24 Oct 1947
NMNH 116300-32 Volcanic Ash PARICUTIN 18 Dec 1947
NMNH 116300-33 Volcanic Ash PARICUTIN 18 Dec 1947
NMNH 116300-34 Volcanic Ash PARICUTIN 19 Dec 1947
NMNH 116300-35 Volcanic Ash PARICUTIN 26 Jan 1948
NMNH 116300-36 Volcanic Ash PARICUTIN 28 Jan 1948
NMNH 116300-37 Volcanic Ash PARICUTIN 21 Feb 1948
NMNH 116300-38 Volcanic Ash PARICUTIN 25 Feb 1948
NMNH 116300-39 Volcanic Ash PARICUTIN 28 Feb 1948
NMNH 116300-4 Volcanic Ash PARICUTIN 13 Jan 1947
NMNH 116300-40 Volcanic Ash PARICUTIN 25 Mar 1948
NMNH 116300-41 Volcanic Ash PARICUTIN 18 May 1948
NMNH 116300-42 Volcanic Ash PARICUTIN 29 Jun 1948
NMNH 116300-43 Volcanic Ash PARICUTIN 29 Sep 1948
NMNH 116300-44 Volcanic Ash PARICUTIN 18 Jan 1947
NMNH 116300-45 Volcanic Ash PARICUTIN 9 Feb 1947
NMNH 116300-46 Volcanic Ash PARICUTIN 10 Feb 1947
NMNH 116300-5 Volcanic Ash PARICUTIN 16 Jan 1947
NMNH 116300-6 Volcanic Ash PARICUTIN 31 Jan 1947
NMNH 116300-7 Volcanic Ash PARICUTIN 5 Feb 1947
NMNH 116300-8 Volcanic Ash PARICUTIN 18 Mar 1947
NMNH 116300-9 Volcanic Ash PARICUTIN 18 Apr 1947
NMNH 116301-1 Volcanic Ash PARICUTIN 20 Jan 1947
NMNH 116301-2 Volcanic Ash PARICUTIN 6 Mar 1948
NMNH 116301-3 Volcanic Ash PARICUTIN 6 Mar 1948
NMNH 116301-4 Volcanic Ash PARICUTIN 31 Mar 1948
NMNH 116302-1 Volcanic Ash PARICUTIN 18 Mar 1948
NMNH 116302-2 Volcanic Ash PARICUTIN 18 Nov 1948
NMNH 116302-3 Volcanic Ash PARICUTIN 18 Nov 1948
NMNH 116325-1 Volcanic Rock PARICUTIN --
NMNH 116325-2 Volcanic Rock PARICUTIN --
NMNH 116595-1 Granite JORULLO --
NMNH 116595-10 Basaltic Andesite JORULLO --
NMNH 116595-11 Basaltic Andesite JORULLO --
NMNH 116595-12 Basaltic Andesite JORULLO --
NMNH 116595-13 Basalt JORULLO --
NMNH 116595-14 Granite JORULLO --
NMNH 116595-15 Granite JORULLO --
NMNH 116595-16 Granite JORULLO --
NMNH 116595-17 Basalt JORULLO --
NMNH 116595-18 Basaltic Andesite JORULLO --
NMNH 116595-19 Basaltic Andesite JORULLO --
NMNH 116595-2 Basaltic Andesite JORULLO --
NMNH 116595-20 Basaltic Andesite JORULLO --
NMNH 116595-21 Basaltic Andesite JORULLO --
NMNH 116595-22 Basalt JORULLO, VOLCAN DEL NORTE --
NMNH 116595-23 Basaltic Andesite JORULLO --
NMNH 116595-24 Granite JORULLO --
NMNH 116595-25 Basaltic Andesite JORULLO --
NMNH 116595-26 Basaltic Andesite JORULLO --
NMNH 116595-27 Basalt JORULLO --
NMNH 116595-28 Basalt JORULLO --
NMNH 116595-29 Basaltic Andesite JORULLO --
NMNH 116595-3 Basaltic Andesite JORULLO --
NMNH 116595-33 Granite Xenolith JORULLO --
NMNH 116595-34 Granite Xenolith JORULLO --
NMNH 116595-35 Granite Xenolith JORULLO --
NMNH 116595-4 Basaltic Andesite JORULLO --
NMNH 116595-5 Basaltic Andesite JORULLO --
NMNH 116595-6 Basaltic Andesite JORULLO --
NMNH 116595-7 Basaltic Andesite JORULLO --
NMNH 116595-8 Altered Basalt JORULLO --
NMNH 116595-9 Basaltic Andesite JORULLO --
NMNH 117253-75 Lava -- --
NMNH 117253-76 Lava -- --
NMNH 117253-77 Lava Hoya Alvarez --
NMNH 117253-78 Lava Hoya Alvarez --
NMNH 117253-79 Lava Hoya Alvarez --
NMNH 117253-80 Lava Hoya Alvarez --
NMNH 117253-81 Lava Hoya Alvarez --
NMNH 117254-113 Lava -- --
NMNH 117628-1 Charcoal Jorullo --
NMNH 117628-10 Basalt Parícutin --
NMNH 117628-100 Scoria La Batea --
NMNH 117628-101 Scoria La Batea --
NMNH 117628-102 Scoria La Batea --
NMNH 117628-103 Basalt -- --
NMNH 117628-104 Scoria Hoya La Cintora --
NMNH 117628-105 Scoria Hoya Solis --
NMNH 117628-106 Basalt Hoya Solis --
NMNH 117628-107 Basalt -- --
NMNH 117628-108 Tuff -- --
NMNH 117628-109 Tuff -- --
NMNH 117628-11 Basalt Parícutin --
NMNH 117628-110 Tuff -- --
NMNH 117628-111 Basalt -- --
NMNH 117628-112 Basalt -- --
NMNH 117628-113 Basalt -- --
NMNH 117628-114 Basalt -- --
NMNH 117628-115 Scoria La Pecina Maar --
NMNH 117628-116 Basalt -- --
NMNH 117628-117 Basalt -- --
NMNH 117628-118 Volcanic Rock -- --
NMNH 117628-119 Basalt -- --
NMNH 117628-12 Basalt Parícutin --
NMNH 117628-120 Scoria -- --
NMNH 117628-121 Scoria -- --
NMNH 117628-122 Scoria -- --
NMNH 117628-123 Scoria -- --
NMNH 117628-124 Scoria -- --
NMNH 117628-125 Plagioclase -- --
NMNH 117628-126 Scoria -- --
NMNH 117628-127 Scoria -- --
NMNH 117628-128 Scoria -- --
NMNH 117628-129 Basalt -- --
NMNH 117628-13 Sal Ammoniac Parícutin --
NMNH 117628-130 Scoria -- --
NMNH 117628-131 Basalt -- --
NMNH 117628-132 Scoria -- --
NMNH 117628-133 Scoria La Joya Maar --
NMNH 117628-134 Scoria La Joya Maar --
NMNH 117628-135 Scoria -- --
NMNH 117628-136 Basalt Volcanes de Zacapu --
NMNH 117628-14 Scoria Parícutin --
NMNH 117628-15 Scoria Parícutin --
NMNH 117628-16 Scoria Parícutin --
NMNH 117628-17 Scoria Parícutin --
NMNH 117628-18 Andesite Rincón de Parangueo --
NMNH 117628-19 Basalt Rincón de Parangueo --
NMNH 117628-2 Basalt Jorullo --
NMNH 117628-20 Dacite Cerro La Mina --
NMNH 117628-21 Basalt Cerro La Mina --
NMNH 117628-22 Basalt Cerro La Mina --
NMNH 117628-23 Basalt Cerro La Mina --
NMNH 117628-24 Basalt Cerro La Mina --
NMNH 117628-25 Scoria -- --
NMNH 117628-26 Scoria -- --
NMNH 117628-27 Scoria -- --
NMNH 117628-28 Scoria -- --
NMNH 117628-29 Scoria -- --
NMNH 117628-3 Ash Jorullo --
NMNH 117628-30 Scoria -- --
NMNH 117628-31 Scoria -- --
NMNH 117628-32 Scoria -- --
NMNH 117628-33 Basalt Maar San Nicolas --
NMNH 117628-34 Scoria Maar San Nicolas --
NMNH 117628-35 Scoria Maar San Nicolas --
NMNH 117628-36 Scoria Maar San Nicolas --
NMNH 117628-37 Scoria Maar San Nicolas --
NMNH 117628-38 Scoria Maar San Nicolas --
NMNH 117628-39 Ash Cerro Buenavista --
NMNH 117628-4 Lapilli Jorullo --
NMNH 117628-40 Basalt Cerro Buenavista --
NMNH 117628-41 Plagioclase Cerro Buenavista --
NMNH 117628-42 Scoria Cerro Buenavista --
NMNH 117628-43 Scoria Cerro Buenavista --
NMNH 117628-44 Basalt Cerro Las Silletas --
NMNH 117628-45 Scoria Cerro Las Silletas --
NMNH 117628-46 Scoria Cerro Las Silletas --
NMNH 117628-47 Basalt Cerro Las Silletas --
NMNH 117628-48 Basalt Hoya Estrada --
NMNH 117628-49 Scoria Hoya Estrada --
NMNH 117628-5 Ash Parícutin --
NMNH 117628-50 Scoria Hoya Estrada --
NMNH 117628-51 Basalt Hoya Estrada --
NMNH 117628-52 Pumice Hoya Estrada --
NMNH 117628-53 Basalt Hoya Estrada --
NMNH 117628-54 Pumice Hoya Estrada --
NMNH 117628-55 Rhyodacite Hoya Estrada --
NMNH 117628-56 Basalt Hoya Estrada --
NMNH 117628-57 Tuff Cerro San Andres --
NMNH 117628-58 Pyroclastic Rock Maar San Nicolas --
NMNH 117628-59 Tuff -- --
NMNH 117628-6 Xenolith Parícutin --
NMNH 117628-60 Scoria Hoya Blanca --
NMNH 117628-61 Tuff Hoya Blanca --
NMNH 117628-62 Basalt Hoya Blanca --
NMNH 117628-63 Basalt Hoya Blanca --
NMNH 117628-64 Tuff Hoya Blanca --
NMNH 117628-65 Tuff Hoya Estrada --
NMNH 117628-66 Tuff -- --
NMNH 117628-67 Tuff -- --
NMNH 117628-68 Scoria -- --
NMNH 117628-69 Scoria -- --
NMNH 117628-7 Xenolith Parícutin --
NMNH 117628-70 Scoria -- --
NMNH 117628-71 Tuff -- --
NMNH 117628-72 Basalt -- --
NMNH 117628-73 Basalt La Batea --
NMNH 117628-74 Basalt La Batea --
NMNH 117628-75 Scoria La Batea --
NMNH 117628-76 Basalt -- --
NMNH 117628-77 Basalt San Vincente Joyuela --
NMNH 117628-78 Basalt Hoya Alvarez --
NMNH 117628-79 Basalt Hoya Alvarez --
NMNH 117628-8 Basalt Parícutin --
NMNH 117628-80 Scoria Hoya Alvarez --
NMNH 117628-81 Scoria Hoya Alvarez --
NMNH 117628-82 Scoria -- --
NMNH 117628-83 Troctolite Xenolith -- --
NMNH 117628-84 Troctolite Xenolith -- --
NMNH 117628-85 Scoria Magdalena Crater --
NMNH 117628-86 Scoria Hoya Alvarez --
NMNH 117628-87 Cinder La Batea --
NMNH 117628-88 Cinder La Batea --
NMNH 117628-89 Basalt Hoya La Cintora --
NMNH 117628-9 Basalt Parícutin --
NMNH 117628-90 Basalt Hoya La Cintora --
NMNH 117628-91 Basalt Hoya La Cintora --
NMNH 117628-92 Basalt Hoya La Alberca --
NMNH 117628-93 Scoria Hoya La Alberca --
NMNH 117628-94 Basalt Hoya La Alberca --
NMNH 117628-95 Tuff Hoya La Alberca --
NMNH 117628-96 Scoria Hoya La Alberca --
NMNH 117628-97 Tuff Hoya La Cintora --
NMNH 117628-98 Tuff -- --
NMNH 117628-99 Scoria Cerro Chupin --
NMNH 117802-18 Basaltic Andesite Paricutin --
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