Crow Lagoon

Photo of this volcano
  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 54.7°N
  • 130.23°W

  • 335 m
    1099 ft

  • 320110
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Crow Lagoon.

The Global Volcanism Program has no Weekly Reports available for Crow Lagoon.

The Global Volcanism Program has no Bulletin Reports available for Crow Lagoon.

The Global Volcanism Program is not aware of any Holocene eruptions from Crow Lagoon. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Crow Lagoon page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

The Global Volcanism Program has no synonyms or subfeatures listed for Crow Lagoon.

Photo Gallery


A geologist observes the contact between a basaltic plinian fallout lapilli unit resting on marine clay. This deposit is part of thick beds of basaltic tephra of Holocene age originating from an unknown Quaternary volcanic center found near Crow Lagoon, north of Prince Rupert near the southern tip of the Alaskan panhandle. Ballistically emplaced bombs imply a nearby source, which remains unidentified. The tephra beds are located along the south side of the Khutzeymateen Inlet, about 40 km north of Prince Rupert.

Photo by Jack Souther (Geological Survey of Canada, courtesy of Cathie Hickson).
See title for photo information.

Smithsonian Sample Collections Database


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

Affiliated Sites