The geology of Damavand volcano, Alborz Mountains, northern Iran

Jon Davidson, Jamshid Hassanzadeh, Reinis Berzins, Daniel F. Stockli, Behrooz Bashukooh, Brent Turrin, Ali Pandamouz

Research output: Contribution to journalArticle

80 Citations (Scopus)

Abstract

Damavand volcano, located in northern Iran, is a large (>400 km3) composite cone that is currently dormant; it shows fumarolic activity near the summit but no evidence of eruption in the past 1000 yr. The volcano represents an isolated focus of magmatism of uncertain tectonic affinity, although geophysical and geochemical constraints point toward a local hotspot/plume origin, possibly associated with lithospheric delamination, rather than any association with subduction. New (U-Th)/He and 40Ar/39Ar geochronological constraints indicate that the present cone (Young Damavand) has been constructed over ∼600 k.y. on an older, eroded edifice of indistinguishable composition (younger than 1.8 Ma). Damavand activity has been characterized by the eruption of radially directed trachyandesite lava flows, almost exclusively from summit vents. Limited pyroclastic activity has yielded thin fallout pumice lapilli layers and a few pyroclastic flows. Only one significant pyroclastic event is recognized in the remnants of a welded ignimbrite, ponded and preserved along the Haraz River drainage. Relatively short periods of volcanic eruptive activity were interspersed with longer periods of erosion in which volcanic products were transported, particularly as hyperconcentrated flows, into the surrounding drainage systems to be further reworked into epiclastic deposits. Occasional catastrophic events punctuated this interplay between volcanism and erosion. At least one sector collapse is signified by the presence of a large debris avalanche deposit, and the regional drainage systems appear to have been frequently dammed by incursions of volcanic material.

Original languageEnglish (US)
Pages (from-to)16-29
Number of pages14
JournalBulletin of the Geological Society of America
Volume116
Issue number1-2
DOIs
StatePublished - Jan 1 2004

Fingerprint

volcano
volcanic eruption
geology
erosion
debris avalanche
catastrophic event
mountain
pyroclastic flow
delamination
pumice
ignimbrite
fallout
lava flow
magmatism
hot spot
volcanism
subduction
plume
drainage
tectonics

All Science Journal Classification (ASJC) codes

  • Geology

Keywords

  • (U-Th)/He
  • Alborz Mountains
  • Argon-argon
  • Damavand volcano
  • Geochronology
  • Volcanic centers
  • Volcaniclastic rocks

Cite this

Davidson, J., Hassanzadeh, J., Berzins, R., Stockli, D. F., Bashukooh, B., Turrin, B., & Pandamouz, A. (2004). The geology of Damavand volcano, Alborz Mountains, northern Iran. Bulletin of the Geological Society of America, 116(1-2), 16-29. https://doi.org/10.1130/B25344.1
Davidson, Jon ; Hassanzadeh, Jamshid ; Berzins, Reinis ; Stockli, Daniel F. ; Bashukooh, Behrooz ; Turrin, Brent ; Pandamouz, Ali. / The geology of Damavand volcano, Alborz Mountains, northern Iran. In: Bulletin of the Geological Society of America. 2004 ; Vol. 116, No. 1-2. pp. 16-29.
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Davidson, J, Hassanzadeh, J, Berzins, R, Stockli, DF, Bashukooh, B, Turrin, B & Pandamouz, A 2004, 'The geology of Damavand volcano, Alborz Mountains, northern Iran', Bulletin of the Geological Society of America, vol. 116, no. 1-2, pp. 16-29. https://doi.org/10.1130/B25344.1

The geology of Damavand volcano, Alborz Mountains, northern Iran. / Davidson, Jon; Hassanzadeh, Jamshid; Berzins, Reinis; Stockli, Daniel F.; Bashukooh, Behrooz; Turrin, Brent; Pandamouz, Ali.

In: Bulletin of the Geological Society of America, Vol. 116, No. 1-2, 01.01.2004, p. 16-29.

Research output: Contribution to journalArticle

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