Markagunt Plateau

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 37.58°N
  • 112.67°W

  • 2840 m
    9315 ft

  • 327040
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Markagunt Plateau.



 Available Weekly Reports

There are no Weekly Reports available for Markagunt Plateau.

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

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
[ 1050 (in or before) ] [ Unknown ] Uncertain    

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.

Biek R F, Rowley P D, Anderson J J, Maldonado F, Moore D W, Eaton J G, Hereford R, Matyjasik B, 2012. Interim geologic map of the Panguitch 30 min x 60 min quadrangle, Garfield, Iron, and Kane counties, Utah. Utah Geol Surv Open-File Rep, 599, 3 plates, 1:65,000 scale, 127 p text).

Gregory H E, 1949. Geologic and geographic reconnaissance of Eastern Markagunt Plateau, Utah. Geol Soc Amer Bull, 60: 969-998.

Hatfield S C, Rowley P D, Sable E G, Maxwell D J, Cox B V, McKell M D, Kiel D E, 2003. Geology of Cedar Breaks National Monument, Utah. In: Sprinkel D A, Chidsey T C Jr, Anderson P B (eds) {Geology of Utah's Parks and Monuments}, Utah Geol Assoc Publ, 28: 139-154.

Johnsen R L, Smith I E, Biek R F, 2010. Subalkaline volcanism in the Black Rock Desert and Markagunt Plateau volcanic fields of south-central Utah. In: Carney S M, Tabet D E, Johnson C L (eds), Geology of South-Central Utah {Utah Geol Assoc Pub} 39: 109-150.

Moore D W, Nealey L D, Rowley P D, Harfield S C, Maxwell D J, Mitchell E, 2004. Geologic map of the Navajo Lake quadrangle, Kane and Iron Counties, Utah. Utah Geol Surv, map 199, 2 plates, 1:24,000 scale.

Smith R L, Shaw H R, 1975. Igneous-related geothermal systems. U S Geol Surv Circ, 726: 58-83.

A group of basaltic cinder cones and lava vents on the Markagunt Plateau east of Cedar Breaks National Monument in SW Utah has produced youthful, sparsely vegetated lava flows. Products of an older episode of volcanism producing trachytic, andesitic and rhyolitic lavas were succeeded by basaltic lavas of two different ages. Several lines of NE-SW-trending cinder cones occur within the volcanic field, with the youngest flows being located near Panguitch Lake on the north and Navajo Lake on the south. Navajo Lake formed when a thick, blocky flow from a nearby vent dammed Duck Creek. Young lava flows, many of which are fissure fed, have distinct margins and covered or diverted stream drainages, which have for the most part not been reestablished across the flows. The oldest trees on the youngest flows are about 900 years old (Gregory, 1949) and Southern Paiute legends note "smoking hills" and red-hot lava flows in the Panguitch Lake area, although it is not known if the lava flows are that young.