The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism

<p>The western Arabian Peninsula includes one of the world&rsquo;s most extensive monogenetic volcanic provinces, with dispersed volcanic fields extending from south-eastern T&uuml;rkiye to north-western Yemen. The volcanic fields exhibit significant geological diversity and a magmatic composition r...

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Main Author: Németh, Károly
Format: Book Chapter
Language:English
Published: IntechOpen 2026
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Online Access:https://www.intechopen.com/chapters/1237406
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author Németh, Károly
author_browse Németh, Károly
author_facet Németh, Károly
author_sort Németh, Károly
building IntechOpen
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description <p>The western Arabian Peninsula includes one of the world&rsquo;s most extensive monogenetic volcanic provinces, with dispersed volcanic fields extending from south-eastern T&uuml;rkiye to north-western Yemen. The volcanic fields exhibit significant geological diversity and a magmatic composition ranging from mafic to rare silicic. This province is primarily characterised by relatively small-volume monogenetic volcanoes formed during the Neogene&ndash;Quaternary period, resulting in the creation of over 3,000 volcanic edifices &ndash; more than 90% of which represent typical magmatic explosive and effusive activity. Additionally, the province includes remarkable examples of volcanoes formed by explosive magma&ndash;water interactions, including some of the largest maar volcanoes globally and exceptionally well-preserved phreatomagmatic tuff ring rims. In certain instances, eruptions involving more silicic magmas resulted in brief but intense explosive events triggered by lava dome explosions, in which external water likely contributed to crater formation and the production of characteristic initial eruptive materials. This chapter provides the first comprehensive summary of the fundamental features of the phreatomagmatic eruptive centres within the western Saudi Arabian Neogene&ndash;Quaternary volcanic fields, emphasising their eruptive products, landforms, and the implications for understanding their eruptive environments.</p>
doi_str_mv 10.5772/intechopen.1016928
first_indexed 2026-10-15T21:41:38Z
format Book Chapter
fullrecord <oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><identifier>intech-1237406</identifier><datestamp>2026-07-25</datestamp> <dc:title>The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism</dc:title> <dc:creator>Károly Németh</dc:creator> <dc:subject>Physical Sciences, Engineering and Technology</dc:subject> <dc:description>&lt;p&gt;The western Arabian Peninsula includes one of the world&amp;rsquo;s most extensive monogenetic volcanic provinces, with dispersed volcanic fields extending from south-eastern T&amp;uuml;rkiye to north-western Yemen. The volcanic fields exhibit significant geological diversity and a magmatic composition ranging from mafic to rare silicic. This province is primarily characterised by relatively small-volume monogenetic volcanoes formed during the Neogene&amp;ndash;Quaternary period, resulting in the creation of over 3,000 volcanic edifices &amp;ndash; more than 90% of which represent typical magmatic explosive and effusive activity. Additionally, the province includes remarkable examples of volcanoes formed by explosive magma&amp;ndash;water interactions, including some of the largest maar volcanoes globally and exceptionally well-preserved phreatomagmatic tuff ring rims. In certain instances, eruptions involving more silicic magmas resulted in brief but intense explosive events triggered by lava dome explosions, in which external water likely contributed to crater formation and the production of characteristic initial eruptive materials. This chapter provides the first comprehensive summary of the fundamental features of the phreatomagmatic eruptive centres within the western Saudi Arabian Neogene&amp;ndash;Quaternary volcanic fields, emphasising their eruptive products, landforms, and the implications for understanding their eruptive environments.&lt;/p&gt;</dc:description> <dc:publisher>IntechOpen</dc:publisher> <dc:date>2026-07-25</dc:date> <dc:type>Chapter, Part Of Book</dc:type> <dc:identifier>https://www.intechopen.com/chapters/1237406</dc:identifier> <dc:identifier>doi:10.5772/intechopen.1016928</dc:identifier> <dc:language>en</dc:language> <dc:relation>ISBN:978-1-80631-196-5</dc:relation> <dc:rights>https://creativecommons.org/licenses/by/3.0/</dc:rights> <dc:source>https://www.intechopen.com/books/1005287 ; Latest Advances in Volcanology - Volcanoes as Complex Geosystems</dc:source> </oai_dc:dc>
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spelling intech-12374062026-07-25 The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism Károly Németh Physical Sciences, Engineering and Technology <p>The western Arabian Peninsula includes one of the world&rsquo;s most extensive monogenetic volcanic provinces, with dispersed volcanic fields extending from south-eastern T&uuml;rkiye to north-western Yemen. The volcanic fields exhibit significant geological diversity and a magmatic composition ranging from mafic to rare silicic. This province is primarily characterised by relatively small-volume monogenetic volcanoes formed during the Neogene&ndash;Quaternary period, resulting in the creation of over 3,000 volcanic edifices &ndash; more than 90% of which represent typical magmatic explosive and effusive activity. Additionally, the province includes remarkable examples of volcanoes formed by explosive magma&ndash;water interactions, including some of the largest maar volcanoes globally and exceptionally well-preserved phreatomagmatic tuff ring rims. In certain instances, eruptions involving more silicic magmas resulted in brief but intense explosive events triggered by lava dome explosions, in which external water likely contributed to crater formation and the production of characteristic initial eruptive materials. This chapter provides the first comprehensive summary of the fundamental features of the phreatomagmatic eruptive centres within the western Saudi Arabian Neogene&ndash;Quaternary volcanic fields, emphasising their eruptive products, landforms, and the implications for understanding their eruptive environments.</p> IntechOpen 2026-07-25 Chapter, Part Of Book https://www.intechopen.com/chapters/1237406 doi:10.5772/intechopen.1016928 en ISBN:978-1-80631-196-5 https://creativecommons.org/licenses/by/3.0/ https://www.intechopen.com/books/1005287 ; Latest Advances in Volcanology - Volcanoes as Complex Geosystems
spellingShingle Physical Sciences, Engineering and Technology
Németh, Károly
The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism
title The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism
title_full The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism
title_fullStr The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism
title_full_unstemmed The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism
title_short The Role of Phreatomagmatism in the Saudi Arabian Neogene–Quaternary Intra-plate Monogenetic Volcanism
title_sort role of phreatomagmatism in the saudi arabian neogene quaternary intra plate monogenetic volcanism
topic Physical Sciences, Engineering and Technology
url https://www.intechopen.com/chapters/1237406
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