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Malumalu is a volcanic seamount in American Samoa. Together with Savaii, Upolu and Tutuila, it forms a topographic structure close to the Tonga Trench, which lies about 100 kilometres (62 mi) south. Malumalu lies about 66 kilometres (41 mi) south of Ofu island and is also known as "Southeast Bank". It is about 25 kilometres (16 mi) wide at its base and is part of the Mula ridge, which extends to Tutuila.

Attributes	Values
rdf:type	geo:SpatialThing
rdfs:label	Malumalu (en)
rdfs:comment	Malumalu is a volcanic seamount in American Samoa. Together with Savaii, Upolu and Tutuila, it forms a topographic structure close to the Tonga Trench, which lies about 100 kilometres (62 mi) south. Malumalu lies about 66 kilometres (41 mi) south of Ofu island and is also known as "Southeast Bank". It is about 25 kilometres (16 mi) wide at its base and is part of the Mula ridge, which extends to Tutuila. (en)
geo:lat	-14.607943 (xsd:float)
geo:long	-169.784912 (xsd:float)
dct:subject	Holocene volcanoes Seamounts of the Pacific Ocean Volcanoes of American Samoa
Wikipage page ID	60534311 (xsd:integer)
Wikipage revision ID	1112814983 (xsd:integer)
Link from a Wikipage to another Wikipage	Holocene volcanoes Upolu Vailulu'u Seamount Seamounts of the Pacific Ocean Mantle plume Actinide Tonga Trench Tutuila American Samoa Hawaii Samoa hotspot Volcanoes of American Samoa Ofu-Olosega Slab (geology) Savaii Isotope ratio Ta'u
Link from a Wikipage to an external page	https://darchive.mblwhoilibrary.org/bitstream/1912/24119/1/Reinhard_et_al-2019-Geochemistry%2c_Geophysics%2c_Geosystems.pdf https://ir.uiowa.edu/cgi/viewcontent.cgi%3Farticle=1001&context=geology_pubs
sameAs	Malumalu Malumalu
dbp:wikiPageUsesTemplate	dbt:Cite_journal dbt:Convert dbt:Coord dbt:Refbegin dbt:Refend dbt:Reflist dbt:Sfn dbt:Short_description dbt:Volcanology-stub
georss:point	-14.607943 -169.784919
has abstract	Malumalu is a volcanic seamount in American Samoa. Together with Savaii, Upolu and Tutuila, it forms a topographic structure close to the Tonga Trench, which lies about 100 kilometres (62 mi) south. Malumalu lies about 66 kilometres (41 mi) south of Ofu island and is also known as "Southeast Bank". It is about 25 kilometres (16 mi) wide at its base and is part of the Mula ridge, which extends to Tutuila. The seamount is a young volcano at the eastern end of a lineament that begins on Tutuila. This lineament has been named the "Malu trend" (in contrast to the "Vai trend" farther northeast, which runs between Ofu, Ta'u and Vailulu'u). This is comparable to the "Kea" and "Loa" trends in Hawaii. Malumalu is not much older than Vailulu'u, which has erupted in historical time. Actinide isotope ratios indicate the occurrence of at least three volcanic events in the last 300,000 years, including at least two in the last 150,000 years and at least one in the last 8,000 years. According to one model of the behaviour of the Samoa hotspot, volcanic activity at Malumalu will decline in the next 10,000 - 100,000 years as the mantle plume is pushed farther northeast to Vailulu'u by mantle flow generated by the Tonga slab. (en)
prov:wasDerivedFrom	wikipedia-en:Malumalu?oldid=1112814983&ns=0
page length (characters) of wiki page	5175 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Malumalu
geo:geometry	POINT(-169.78491210938 -14.607942581177)
is Link from a Wikipage to another Wikipage of	List of volcanoes in the United States Malumalu Seamount
is Wikipage redirect of	Malumalu Seamount
is foaf:primaryTopic of	wikipedia-en:Malumalu

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