Skip to main content
Back to map
CompareShow on map

United States · Volcanic field

Red Hill volcanic field

Red Hill-Quemado

Type
Volcanic field
Elevation
2300m
Last eruption
-9450
The Red Hill-Quemado Volcanic Field in New Mexico, USA, contains more than 40 scoria cones, some of which are in the area shown in this August 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 34 km across). There are also phreatomagmatic features including the 2-km-wide Zuni Salt Lake maar at the top of this Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 69 km across).
The Red Hill-Quemado Volcanic Field in New Mexico, USA, contains more than 40 scoria cones, some of which are in the area shown in this August 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 34 km across). There are also phreatomagmatic features including the 2-km-wide Zuni Salt Lake maar at the top of this Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 69 km across). · Photo: Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).
Type
Volcanic field
Country
United States
Region
North America / Basin and Range Volcanic Province
Elevation
2300m
Coordinates
34.250, -108.830
Last eruption
-9450
Tectonic setting
Rift zone / Continental crust (> 25 km)
Landform
Cluster
Major rock type
Basalt / Picro-basalt

Geological summary

The Red Hill-Quemado volcanic field in western New Mexico is across the border from the Springerville volcanic field in Arizona and contains more than 40 cinder cones and maars that were active from the late Miocene to early Holocene.

Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →

From Wikipedia

Red Hill volcanic field, also known as Quemado volcanic field, is a monogenetic volcanic field located in the vicinity of the ghost town of Red Hill in Catron County New Mexico. Red Hill is 24 kilometers (15 mi) east of the larger Springerville volcanic field and includes Zuñi Salt Lake. The area is made up of scoria cone and silicic dome fields. Over 40 volcanic vents have been identified in the field. These erupted basaltic flows, with no other rock types evident in the field.

Wikipedia · CC BY-SA · Read full article →

Eruption history

3 recordedGlossary

Record summary

Confirmed eruptions
3
Uncertain eruptions
0
Span of confirmed record
9850 BCE (±500 yrs) – 9450 BCE
Largest confirmed eruption
No VEI recorded
Confirmed eruptions since 1900
0
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
9850 BCE~9810 BCE · 1 eruptions · max VEI ?9730 BCE~9690 BCE · 1 eruptions · max VEI ?9490 BCE~9450 BCE · 1 eruptions · max VEI ?9850 BCE9770 BCE9650 BCE9570 BCE9490 BCE

Detailed timeline

  1. 9450 BCE (±400 yrs)VEI ?Geological estimate
    9450 BCE – end unknown
    Zuni Salt Lake maar
  2. 9700 BCE (±450 yrs)VEI ?Geological estimate
    9700 BCE – end unknown
    2.5 km radius of Zuni Salt Lake
  3. 9850 BCE (±500 yrs)VEI ?Geological estimate
    9850 BCE – end unknown
    Cerro Pomo?

Nearby volcanoes

External links

⚠ For reference only. Not for emergency response.