Emplacement and inflation of pahoehoe sheet flows: observations and measurements of active lava flows on Kilauea volcano, Hawaii

Geological Society of America Bulletin
By: , and 

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Abstract

Inflated pahoehoe sheet flows have a distinctive horizontal upper surface, which can be several hundred meters across, and are bounded to steep monoclinal uplifts. The inflated sheet flows studied ranged from 1 to 5 m in thickness, but initially propagated as thin sheets of fluid pahoehoe lava, generally 20-30 cm thick. The morphology of the lava as flow advanced is described. Inflated sheet flows from Kilauea and Mauna Loa are morphologically similar to some thick Icelandic and submarine sheet flows, suggesting a similar mechanism of emplacement. -from Authors
Publication type Article
Publication Subtype Journal Article
Title Emplacement and inflation of pahoehoe sheet flows: observations and measurements of active lava flows on Kilauea volcano, Hawaii
Series title Geological Society of America Bulletin
DOI 10.1130/0016-7606(1994)106<0351:EAIOPS>2.3.CO;2
Volume 106
Issue 3
Year Published 1994
Language English
Contributing office(s) Volcano Hazards Program
Description 20 p.
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Geological Society of America Bulletin
First page 351
Last page 370
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