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The Global Volcanism Program has no activity reports for Grensdalur.
The Global Volcanism Program has no Weekly Reports available for Grensdalur.
The Global Volcanism Program has no Bulletin Reports available for Grensdalur.
The small Grensdalur volcanic system (also known as the Hveragerdi system) lies at the eastern end of the Reykjanes Peninsula, SE of the Hengill volcanic system and south of the Hrómundartindur volcanic system. Grensdalur is the oldest of the three volcanic systems in the Hengill area and was last active during the Pleistocene. The Hveragerdi geothermal area contains high- and low-temperature geothermal features that include fumaroles, hot springs and pools, mud pots, and geysers, and provide heat to the town of Hveragerdi.
The Global Volcanism Program is not aware of any Holocene eruptions from Grensdalur. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Grensdalur page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Steam plumes, newly formed after a May 2008 earthquake, rise from the Reykir ("smokes" in Icelandic) geothermal area, with the town of Hveragerdi in the background. The Hveragerdi geothermal field lies within the small Grensdalur volcanic system. Grensdalur is the oldest of three volcanic systems in the Hengill area and was last active during the Pleistocene. The Hveragerdi geothermal area include fumaroles, hot springs and pools, mud pots, and geysers, and provides heat to the town of Hveragerdi.
Photo coutesy of the University of Iceland Hvergerdi Research Station, 2008.
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. 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.
Clifton A E, Sigmundsson F, Feigl K L, Gudmundsson G, Arnadottir T, 2002. Surface effects of faulting and deformation resulting from magma accumulation at the Hengill triple junction, SW Iceland, 1994-1998. J Volc Geotherm Res, 115: 233-255.
Hansteen T H, 1991. Multi-stage evolution of the picritic Maelifell rocks, SW Iceland: constraints from mineralogy and inclusions of glass and fluid in olivine. Contr Mineral Petr, 109: 225-239.
Sigmundsson F, Einarsson P, Rognvaldsson S T, Foulger G R, Hodgkinson K M, Gunnar Thorbergsson G , 1997. The 1994-1995 seismicity and deformation at the Hengill triple junction, Iceland: triggering of earthquakes by minor magma injection in a zone of horizontal shear stress . J Geophys Res, 102: 15,151-15,161.
Zhanxue S, Armannsson H, 2000. Gas chemistry and subsurface temperature estimation in the Hveragerdi high-temperature geothermal field, SW-Iceland. Proc World Geotherm Cong, 2000, Kyushy-Tohoku, Japan, May 28-June 10, 2000, p 2235-2240.