Hayes

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 61.64°N
  • 152.411°W

  • 3034 m
    9952 ft

  • 313050
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Hayes.



 Available Weekly Reports

There are no Weekly Reports available for Hayes.

Summary of eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1200 ± 300 years Unknown Confirmed   Tephrochronology
1550 BCE (?) Unknown Confirmed 5 Tephrochronology
1850 BCE (?) Unknown Confirmed   Tephrochronology

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Miller T P, Smith R L, 1975. Ash flows on the Alaska Peninsula: a preliminary report on their distribution, composition and age (abs). Geol Soc Amer Abs Prog, 7: 1201.

Motyka R J, Liss S A, Nye C J, Moorman M A, 1993. Geothermal resources of the Aleutian arc. Alaska Div Geol Geophys Surv, Prof Rpt, no 114, 17 p and 4 map sheets.

Riehle J R, 1985. A reconnaissance of the major Holocene tephra deposits in the Upper Cook Inlet Region, Alaska. J Volc Geotherm Res, 26: 37-74.

Wood C A, Kienle J (eds), 1990. Volcanoes of North America. Cambridge, England: Cambridge Univ Press, 354 p.

Hayes volcano, located in a remote and rugged part of the Alaska Range NW of Anchorage and north of Mount Gerdine, was not discovered until 1975. It was named after nearby Hayes Glacier and consists of scattered remnants of a largely snow-and-ice covered volcano that has been destroyed by catastrophic eruptions. The most widespread Holocene eruptions in the Cook Inlet area originated from Hayes volcano between about 3800 and 3400 years ago and produced six regional tephra layers with an average volume of 2.4 cu km. The latest known eruption took place about 1000 years ago.