Cone 3110


Facts


  • Seismically Monitored: No
  • Color Code: UNASSIGNED
  • Alert Level: UNASSIGNED
  • Elevation: 948m (3110ft)
  • Latitude: 58.5745
  • Longitude: -154.5435
  • Smithsonian VNum:
  • Pronunciation:
  • Nearby Towns:
    • Kokhanok 60.4 mi (97.2 km) N
    • Pope-Vannoy Landing 67.9 mi (109.3 km) N
    • Karluk 69.5 mi (111.8 km) S
    • Aleneva 70.8 mi (114 km) ESE
    • Igiugig 70.9 mi (114.1 km) NW

    Distance from Anchorage: 243.3 mi (391.6 km)

Description

This feature is part of the Savonoski River Cluster of volcanoes, as defined by Hildreth and others (2004) [1] . From Hildreth and others (2004) [1] : "Cone 3110 is a basaltic pile (51% SiO2) about 2 km wide with 675 m of relief that lies a few km NW of Cone 3601. Partly erupted englacially, it consists mostly of massive to sheeted glassy breccia and coarse stratified scoria that dip chaotically and enclose channel fillings of convolutedly columnar glassy lava. The upper third of the cone (235 +/- 30 ka) is coherent lava, columnar to chunky jointed. Products have abundant plagioclase, clinopyroxene, and olivine, with minor orthopyroxene."

Name Origin

Cone 3110 is an informal name given by Hildreth and others (2004).


References Cited

[1] Rear-arc vs. arc-front volcanoes in the Katmai reach of the Alaska Peninsula: a critical apprasial of across-arc compositional variation, 2004

Hildreth, Wes, Fierstein, Judy, Siems, D. F., Budahn, J. R., and Ruiz, Joaquin, 2004, Rear-arc vs. arc-front volcanoes in the Katmai reach of the Alaska Peninsula: a critical apprasial of across-arc compositional variation: Contributions to Mineralogy and Petrology, v. 147, n. 3, p. 243-275.

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