Crow Lagoon

Photo of this volcano
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  • 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.

Basic Data

Volcano Number

Last Known Eruption

Elevation

Latitude
Longitude
320110

Unknown - Evidence Credible

335 m / 1099 ft

54.7°N
130.23°W

Volcano Types

Pyroclastic cone

Rock Types

Major
Basalt / Picro-Basalt

Tectonic Setting

Intraplate
Continental crust (> 25 km)

Population

Within 5 km
Within 10 km
Within 30 km
Within 100 km
0
0
456
13,541

Geological Summary

Thick beds of basaltic tephra of Holocene age originating from an unknown Quaternary volcanic center have been 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 (Souther and Weiland, 1993). The tephra beds are located along the south side of the Khutzeymateen Inlet, about 40 km north Prince Rupert.

References

The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography.

Hickson C J, Edwards B R, 2001. Volcanoes and Volcanic Hazards in Canada. In; Brooks G R (ed) {A Synthesis of Geological Hazards in Canada}, Geol Surv Can Bull, 548: 1-248.

Hickson C J, Soos A, Wright R, 1994. Catalogue of Canadian volcanoes. Geol Surv Canada Open-File Rpt.

Souther J G, Weiland I, 1993. Crow Lagoon tephra--new evidence of recent volcanism in west-central British Columbia. Geol Surv Can Pap, 93-1A: 57-62.

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).

Smithsonian Sample Collections Database


A listing of samples from the Smithsonian collections will be available soon.

Affiliated Sites

Large Eruptions of Crow Lagoon Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
WOVOdat WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.
EarthChem EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).
MODVOLC - HIGP MODIS Thermal Alert System Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. When one is found the date, time, location, and intensity are recorded. MODIS looks at every square km of the Earth every 48 hours, once during the day and once during the night, and the presence of two MODIS sensors in space allows at least four hot-spot observations every two days. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. There is a drop-down list with volcano names which allow users to 'zoom-in' and examine the distribution of hot-spots at a variety of spatial scales.
MIROVA Middle InfraRed Observation of Volcanic Activity (MIROVA) is a near real time volcanic hot-spot detection system based on the analysis of MODIS (Moderate Resolution Imaging Spectroradiometer) data. In particular, MIROVA uses the Middle InfraRed Radiation (MIR), measured over target volcanoes, in order to detect, locate and measure the heat radiation sourced from volcanic activity.