A magnetic study of the subglacial ridge formed in the 1996 Gjálp eruption
During the 1996 Gjálp eruption an approximately 6 km long subglacial tindar (hyaloclastite ridge) formed in a mostly subglacial fissure eruption beneath the Vatnajökull ice cap. By definition, tindars are composed of hyaloclastite and pillow lava in variable ratios. Hands-on observations on the top...
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| Format: | Thesis |
| Language: | English |
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2018
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| Online Access: | http://hdl.handle.net/1946/30632 |