Hjartardóttir et al. 2015, p. 8744. Hjartardóttir, Á.R.; Hjaltadóttir, S.; Einarsson, P.; Vogfjörd, K.; Muñoz-Cobo Belart, J. (2015). "Fracturing and earthquake activity within the Prestahnúkur fissure swarm in the Western Volcanic Rift Zone of Iceland". Journal of Geophysical Research: Solid Earth. 120: 8743–8757. doi:10.1002/2015JB012341.
Hjartardóttir et al. 2015, pp. 8745, 8755. Hjartardóttir, Á.R.; Hjaltadóttir, S.; Einarsson, P.; Vogfjörd, K.; Muñoz-Cobo Belart, J. (2015). "Fracturing and earthquake activity within the Prestahnúkur fissure swarm in the Western Volcanic Rift Zone of Iceland". Journal of Geophysical Research: Solid Earth. 120: 8743–8757. doi:10.1002/2015JB012341.
Hjartardóttir et al. 2015, p. 8742. Hjartardóttir, Á.R.; Hjaltadóttir, S.; Einarsson, P.; Vogfjörd, K.; Muñoz-Cobo Belart, J. (2015). "Fracturing and earthquake activity within the Prestahnúkur fissure swarm in the Western Volcanic Rift Zone of Iceland". Journal of Geophysical Research: Solid Earth. 120: 8743–8757. doi:10.1002/2015JB012341.
Hjartardóttir et al. 2015, pp. 8744–8745. Hjartardóttir, Á.R.; Hjaltadóttir, S.; Einarsson, P.; Vogfjörd, K.; Muñoz-Cobo Belart, J. (2015). "Fracturing and earthquake activity within the Prestahnúkur fissure swarm in the Western Volcanic Rift Zone of Iceland". Journal of Geophysical Research: Solid Earth. 120: 8743–8757. doi:10.1002/2015JB012341.
Hjartardóttir et al. 2015, p. 8745. Hjartardóttir, Á.R.; Hjaltadóttir, S.; Einarsson, P.; Vogfjörd, K.; Muñoz-Cobo Belart, J. (2015). "Fracturing and earthquake activity within the Prestahnúkur fissure swarm in the Western Volcanic Rift Zone of Iceland". Journal of Geophysical Research: Solid Earth. 120: 8743–8757. doi:10.1002/2015JB012341.
Hjartardóttir et al. 2015, pp. 8753. Hjartardóttir, Á.R.; Hjaltadóttir, S.; Einarsson, P.; Vogfjörd, K.; Muñoz-Cobo Belart, J. (2015). "Fracturing and earthquake activity within the Prestahnúkur fissure swarm in the Western Volcanic Rift Zone of Iceland". Journal of Geophysical Research: Solid Earth. 120: 8743–8757. doi:10.1002/2015JB012341.
There are multiple possible heights, but used here is the one for the Prestahnúkur peak itself which is without ice/snow cover for some of year. The fissure field to the south has icecap cover with National Landsurvey of Iceland giving a higher spot height currently of 1329 m and a historic height of 1350 m for this region outside the central volcano. Catalogue of Icelandic Volcanoes gives 1383 m in its Central Volcano section which presumably includes the ice of Geitlandsjökull and 1223 m in its Geological setting and tectonic context section on the entry for Prestahnúkur. GVS gives 1385 m which was an icecap height of Geitlandsjökull which has also varied historically downward from 1400 m as the ice has melted. The central volcano height is more correctly that of the terrain under Geitlandsjökull but a referenced height explicitly without the ice needs to be identified.
There are multiple possible heights, but used here is the one for the Prestahnúkur peak itself which is without ice/snow cover for some of year. The fissure field to the south has icecap cover with National Landsurvey of Iceland giving a higher spot height currently of 1329 m and a historic height of 1350 m for this region outside the central volcano. Catalogue of Icelandic Volcanoes gives 1383 m in its Central Volcano section which presumably includes the ice of Geitlandsjökull and 1223 m in its Geological setting and tectonic context section on the entry for Prestahnúkur. GVS gives 1385 m which was an icecap height of Geitlandsjökull which has also varied historically downward from 1400 m as the ice has melted. The central volcano height is more correctly that of the terrain under Geitlandsjökull but a referenced height explicitly without the ice needs to be identified.
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There are multiple possible heights, but used here is the one for the Prestahnúkur peak itself which is without ice/snow cover for some of year. The fissure field to the south has icecap cover with National Landsurvey of Iceland giving a higher spot height currently of 1329 m and a historic height of 1350 m for this region outside the central volcano. Catalogue of Icelandic Volcanoes gives 1383 m in its Central Volcano section which presumably includes the ice of Geitlandsjökull and 1223 m in its Geological setting and tectonic context section on the entry for Prestahnúkur. GVS gives 1385 m which was an icecap height of Geitlandsjökull which has also varied historically downward from 1400 m as the ice has melted. The central volcano height is more correctly that of the terrain under Geitlandsjökull but a referenced height explicitly without the ice needs to be identified.