Uinkaret Field
Volcanic field in United States
Key Facts
Elevation
1,555 m (5,102 ft)
Type
Volcanic field
Location
36.380°, -113.130°
Region
Basin and Range Volcanic Province
Rock Type
Trachybasalt / Tephrite Basanite
Tectonic Setting
Rift zone
Location
Loading map...
Overview
The Uinkaret volcanic field straddling the Grand Canyon contains cinder cones that have produced lava flows that repeatedly cascaded into the Grand Canyon, forming temporary lava dams up to 200 m high. Two of the most prominent landmarks are Vulcan's Throne, a cinder cone on the north rim, and Vulcan's Forge, a small volcanic neck erupted within the Colorado River, 1000 m below. Most of the field lies north of the Grand Canyon on the Uinkaret Plateau between the Toroweap and Hurricane faults.
It is largely Pleistocene in age, and Vulcan's Throne has a cosmogenic helium age of about 73,000 years. Volcanic activity has continued into the Holocene. One lava flow, from Little Springs, south of Pliocene Mount Trumbull, has a cosmogenic helium age of 1300 +/- 500 years BP.
Pottery sherds dated at between 1050 and 1200 CE were found within the Little Springs lava flow, which occurred about the same time as the Sunset Crater eruption in the San Francisco volcanic field to the SE.
Volcanic Hazards & Risk Assessment
Primary Hazards
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 926 years ago | Historical | Historically active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in North America Volcanic Regions
Quick Info
- •Smithsonian ID: 329010
- •Evidence: Eruption Dated
- •Epoch: Holocene
About the Photo
The small dark-colored pyroclastic cone on the right side of the Grand Canyon at the upper left is Vulcan's Throne, part of the Uinkaret volcanic field, which lies on the north rim of the canyon. Lava flows that originated from the cone can be seen cascading into the Grand Canyon. These flows formed temporary lava dams in the canyon up to 200 m high. Light-colored rocks of the Kaibab Limestone form the steep cliffs bounding the mesa at the right.
Photo by Lee Siebert, 2000 (Smithsonian Institution).
Authority Sources
Related Volcanoes
Basic Information
This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.