INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS
In the far north of Iceland, the nine Krafla Fires of 1975 to 1984 produced large volumes of basaltic lava primarily by fissure fed eruptions, which created a variety of volcanic features. Bulbous squeeze-ups, an unusual and previously undescribed lava flow feature, were discovered during a 2015 fie...
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ftmacalestercoll:oai:digitalcommons.macalester.edu:geology_honors-1022 2023-05-15T16:48:43+02:00 INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS Olson, Grady D 2016-01-01T08:00:00Z application/pdf https://digitalcommons.macalester.edu/geology_honors/20 https://digitalcommons.macalester.edu/cgi/viewcontent.cgi?article=1022&context=geology_honors unknown DigitalCommons@Macalester College https://digitalcommons.macalester.edu/geology_honors/20 https://digitalcommons.macalester.edu/cgi/viewcontent.cgi?article=1022&context=geology_honors Geology Honors Projects Iceland Krafla Lava Bulbous Squeeze-up Geochemistry PCA Earth Sciences Geology text 2016 ftmacalestercoll 2021-06-24T12:13:49Z In the far north of Iceland, the nine Krafla Fires of 1975 to 1984 produced large volumes of basaltic lava primarily by fissure fed eruptions, which created a variety of volcanic features. Bulbous squeeze-ups, an unusual and previously undescribed lava flow feature, were discovered during a 2015 field study of an inflated flow field formed during the September 1984 eruption at Krafla. Field studies indicate bulbous squeeze-ups form only on linear pull-apart features, and are likely of high viscosity upon extrusion. The jumbled nature of the flow field surrounding these bulbous squeeze-ups suggests a pulsed, somewhat violent, and rapid emplacement and cooling history. Geochemical and petrographic investigations indicate that bulbous squeeze-ups, elongate squeeze-ups, and pahoehoe plates from the northern flow field are texturally and chemically indistinguishable (e.g., Cohen’s d < 2 for whole rock major and trace element comparisons) suggesting that these features formed from a single, homogenous and unfractionated magma. Principal component analysis (PCA) of major and trace element concentrations further supports this interpretation. The lack of literature describing similar squeeze-up morphologies suggest that the factors that controlled the formation of bulbous squeeze-ups in the northern flow field are somewhat unique to Krafla. Specifically, the formation of bulbous squeeze-ups are largely controlled by pulsed inflation, low slope, high effusion rate, and high viscosity upon extrusion. Importantly, if the manner in which bulbous squeeze-ups form is determined, the identification of this distinctive morphology could be telling of conditions of past eruptions on earth, as well as on other planets with observable lava flows. Text Iceland Macalester College (Minnesota): DigitalCommons@Macalester Krafla ENVELOPE(-16.747,-16.747,65.713,65.713) |
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collection |
Macalester College (Minnesota): DigitalCommons@Macalester |
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ftmacalestercoll |
language |
unknown |
topic |
Iceland Krafla Lava Bulbous Squeeze-up Geochemistry PCA Earth Sciences Geology |
spellingShingle |
Iceland Krafla Lava Bulbous Squeeze-up Geochemistry PCA Earth Sciences Geology Olson, Grady D INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS |
topic_facet |
Iceland Krafla Lava Bulbous Squeeze-up Geochemistry PCA Earth Sciences Geology |
description |
In the far north of Iceland, the nine Krafla Fires of 1975 to 1984 produced large volumes of basaltic lava primarily by fissure fed eruptions, which created a variety of volcanic features. Bulbous squeeze-ups, an unusual and previously undescribed lava flow feature, were discovered during a 2015 field study of an inflated flow field formed during the September 1984 eruption at Krafla. Field studies indicate bulbous squeeze-ups form only on linear pull-apart features, and are likely of high viscosity upon extrusion. The jumbled nature of the flow field surrounding these bulbous squeeze-ups suggests a pulsed, somewhat violent, and rapid emplacement and cooling history. Geochemical and petrographic investigations indicate that bulbous squeeze-ups, elongate squeeze-ups, and pahoehoe plates from the northern flow field are texturally and chemically indistinguishable (e.g., Cohen’s d < 2 for whole rock major and trace element comparisons) suggesting that these features formed from a single, homogenous and unfractionated magma. Principal component analysis (PCA) of major and trace element concentrations further supports this interpretation. The lack of literature describing similar squeeze-up morphologies suggest that the factors that controlled the formation of bulbous squeeze-ups in the northern flow field are somewhat unique to Krafla. Specifically, the formation of bulbous squeeze-ups are largely controlled by pulsed inflation, low slope, high effusion rate, and high viscosity upon extrusion. Importantly, if the manner in which bulbous squeeze-ups form is determined, the identification of this distinctive morphology could be telling of conditions of past eruptions on earth, as well as on other planets with observable lava flows. |
format |
Text |
author |
Olson, Grady D |
author_facet |
Olson, Grady D |
author_sort |
Olson, Grady D |
title |
INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS |
title_short |
INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS |
title_full |
INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS |
title_fullStr |
INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS |
title_full_unstemmed |
INFLATED SHEET FLOWS AND THE OCCURRENCE OF BULBOUS SQUEEZE-UPS |
title_sort |
inflated sheet flows and the occurrence of bulbous squeeze-ups |
publisher |
DigitalCommons@Macalester College |
publishDate |
2016 |
url |
https://digitalcommons.macalester.edu/geology_honors/20 https://digitalcommons.macalester.edu/cgi/viewcontent.cgi?article=1022&context=geology_honors |
long_lat |
ENVELOPE(-16.747,-16.747,65.713,65.713) |
geographic |
Krafla |
geographic_facet |
Krafla |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Geology Honors Projects |
op_relation |
https://digitalcommons.macalester.edu/geology_honors/20 https://digitalcommons.macalester.edu/cgi/viewcontent.cgi?article=1022&context=geology_honors |
_version_ |
1766038803317784576 |