Ingakslugwat Hills
Volcanic field in United States
Key Facts
Elevation
190 m (623 ft)
Type
Volcanic field
Location
61.430°, -164.470°
Region
Northern Alaska-Bering Sea Volcanic Province
Rock Type
Basalt / Picro-Basalt
Tectonic Setting
Intraplate
Location
Loading map...
Overview
The Ingakslugwat Hills consist of at least 32 small cinder cones and eight larger craters covering more than 500 km2 in the Yukon-Kuskokwin delta area of SW Alaska. Numerous small spatter cones and cinder cones range from 8 to 190 m in height; many are concentrated in the NW side of the volcanic field. The latest activity was considered to have occurred during the Holocene (Moll-Stalcup, in Wood and Kienle, 1990).
One low cone containing a 400-m-wide lake may be a maar. This dominantly alkali olivine basaltic field also contains basanitic and nephelinitic rocks, some with inclusions of lherzolite and layered gabbro.
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 | Unknown | Historical | Historically active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in North America Volcanic Regions
Quick Info
- •Smithsonian ID: 314030
- •Evidence: Evidence Credible
- •Epoch: Holocene
About the Photo
The Ingakslugwat Hills volcanic field covers an area of more than 500 km2 and contains over 32 scoria cones and 8 larger craters, some of which are seen in this Planet Labs June 2019 satellite image monthly mosaic (N is at the top; image is approximately 40 km across).
Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).
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.