High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon Rise
The oceanic crust consists mostly of basalt, but more evolved compositions may be far more common than previously thought. To aid in distinguishing rhyolite from basaltic lava and help guide sampling and understand spatial distribution, we constructed a classifier using neural networks and fuzzy inf...
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doaj-d0c5887306e3435187ebf1cfbc1a35692020-11-25T02:10:47ZengMDPI AGGeosciences2076-32632019-06-019624510.3390/geosciences9060245geosciences9060245High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon RiseChristina H. Maschmeyer0Scott M. White1Brian M. Dreyer2David A. Clague3School of the Earth, Ocean and Environment, University of South Carolina, Columbia, SC 29208, USASchool of the Earth, Ocean and Environment, University of South Carolina, Columbia, SC 29208, USAInstitute of Marine Sciences, University of California, Santa Cruz, CA 95064, USAMonterey Bay Aquarium Research Institute, Moss Landing, CA 95039, USAThe oceanic crust consists mostly of basalt, but more evolved compositions may be far more common than previously thought. To aid in distinguishing rhyolite from basaltic lava and help guide sampling and understand spatial distribution, we constructed a classifier using neural networks and fuzzy inference to recognize rhyolite from its lava morphology in sonar data. The Alarcon Rise is ideal to study the relationship between lava flow morphology and composition, because it exhibits a full range of lava compositions in a well-mapped ocean ridge segment. This study shows that the most dramatic geomorphic threshold in submarine lava separates rhyolitic lava from lower-silica compositions. Extremely viscous rhyolite erupts as jagged lobes and lava branches in submarine environments. An automated classification of sonar data is a useful first-order tool to differentiate submarine rhyolite flows from widespread basalts, yielding insights into eruption, emplacement, and architecture of the ocean crust.https://www.mdpi.com/2076-3263/9/6/245seafloor classificationlava morphologyremote sensingmachine learningfuzzy logicoceanic spreading ridge |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Christina H. Maschmeyer Scott M. White Brian M. Dreyer David A. Clague |
spellingShingle |
Christina H. Maschmeyer Scott M. White Brian M. Dreyer David A. Clague High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon Rise Geosciences seafloor classification lava morphology remote sensing machine learning fuzzy logic oceanic spreading ridge |
author_facet |
Christina H. Maschmeyer Scott M. White Brian M. Dreyer David A. Clague |
author_sort |
Christina H. Maschmeyer |
title |
High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon Rise |
title_short |
High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon Rise |
title_full |
High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon Rise |
title_fullStr |
High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon Rise |
title_full_unstemmed |
High-Silica Lava Morphology at Ocean Spreading Ridges: Machine-Learning Seafloor Classification at Alarcon Rise |
title_sort |
high-silica lava morphology at ocean spreading ridges: machine-learning seafloor classification at alarcon rise |
publisher |
MDPI AG |
series |
Geosciences |
issn |
2076-3263 |
publishDate |
2019-06-01 |
description |
The oceanic crust consists mostly of basalt, but more evolved compositions may be far more common than previously thought. To aid in distinguishing rhyolite from basaltic lava and help guide sampling and understand spatial distribution, we constructed a classifier using neural networks and fuzzy inference to recognize rhyolite from its lava morphology in sonar data. The Alarcon Rise is ideal to study the relationship between lava flow morphology and composition, because it exhibits a full range of lava compositions in a well-mapped ocean ridge segment. This study shows that the most dramatic geomorphic threshold in submarine lava separates rhyolitic lava from lower-silica compositions. Extremely viscous rhyolite erupts as jagged lobes and lava branches in submarine environments. An automated classification of sonar data is a useful first-order tool to differentiate submarine rhyolite flows from widespread basalts, yielding insights into eruption, emplacement, and architecture of the ocean crust. |
topic |
seafloor classification lava morphology remote sensing machine learning fuzzy logic oceanic spreading ridge |
url |
https://www.mdpi.com/2076-3263/9/6/245 |
work_keys_str_mv |
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