About: Ingakslugwat Hills

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An Entity of Type : umbel-rc:Mountain, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
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The Ingakslugwat Hills volcanic field is in the Yukon–Kuskokwim Delta in western Alaska. It contains eight large craters and about thirty small pyroclastic cones in an area of some 500 km2. The field contains unusual so-called "Ingakslugwat volcanoes", volcanic ridges up to 7 kilometres (4.3 mi) long and 400 metres (1,300 ft) high which are formed by pyroclastic material. They most likely formed by the interaction of permafrost with magma, seeing as they have a hydrovolcanic nature despite being high above the water table.

Attributes	Values
rdf:type	Thing place dbo:Location schema:Mountain schema:Place natural place Mountain yago:WikicatVolcanoesOfAlaska geo:SpatialThing yago:Abstraction100002137 yago:AmorphousShape113867492 yago:Attribute100024264 yago:Crack109258715 yago:GeologicalFormation109287968 yago:Location100027167 yago:Mountain109359803 yago:NaturalElevation109366317 yago:Object100002684 yago:Opening109379111 yago:PhysicalEntity100001930 yago:YagoGeoEntity yago:YagoLegalActorGeo yago:YagoPermanentlyLocatedEntity Band mountain yago:Shape100027807 yago:Space113910384 yago:Vent109470550 umbel-rc:Mountain
rdfs:label	Ingakslugwat Hills (en)
rdfs:comment	The Ingakslugwat Hills volcanic field is in the Yukon–Kuskokwim Delta in western Alaska. It contains eight large craters and about thirty small pyroclastic cones in an area of some 500 km2. The field contains unusual so-called "Ingakslugwat volcanoes", volcanic ridges up to 7 kilometres (4.3 mi) long and 400 metres (1,300 ft) high which are formed by pyroclastic material. They most likely formed by the interaction of permafrost with magma, seeing as they have a hydrovolcanic nature despite being high above the water table. (en)
foaf:name	Ingakslugwat Hills (en)
name	Ingakslugwat Hills (en)
geo:lat	61.370277 (xsd:float)
geo:long	-163.986938 (xsd:float)
foaf:depiction
dcterms:subject	Landforms of Kusilvak Census Area, Alaska Cinder cones of the United States Landforms of Bethel Census Area, Alaska Volcanoes of Alaska Volcanoes of Unorganized Borough, Alaska
Wikipage page ID	20874576 (xsd:integer)
Wikipage revision ID	1020903245 (xsd:integer)
Link from a Wikipage to another Wikipage	Quaternary Basalt Holocene United States Landforms of Kusilvak Census Area, Alaska List of volcanoes in the United States of America Nephelinite Magma Permafrost Cinder cones of the United States Landforms of Bethel Census Area, Alaska Alaska Volcanoes of Alaska Basanite Cinder cone Volcanic crater Volcanic crater lake Volcanoes of Unorganized Borough, Alaska Baird Inlet Volcanic field Kusilvak Mountains Nelson Island (Alaska) Olivine Yukon–Kuskokwim Delta Pyroclastic cone
Link from a Wikipage to an external page	https://books.google.com/books%3Fid=kkHxAAAAMAAJ&pg=PR8%7Cyear=1988%7Cpublisher=U.S.
sameAs	Ingakslugwat Hills Ingakslugwat Hills Ingakslugwat Hills Ingakslugwat Hills Ingakslugwat Hills Ingakslugwat Hills Ingakslugwat Hills Ingakslugwat Hills
dbp:wikiPageUsesTemplate	dbt:Cite_book dbt:Convert dbt:Coord dbt:Infobox_mountain dbt:Nobreak dbt:Refbegin dbt:Refend dbt:Reflist dbt:Sfn dbt:KusilvakAK-geo-stub dbt:BethelAK-geo-stub
thumbnail	wiki-commons:Special:FilePath/Ingakslugwat_Hills.jpg?width=300
listing	List of volcanoes in the United States of America
age	Holocene
elevation ft	623 (xsd:integer)
location	United States Alaska
photo	Ingakslugwat Hills.jpg (en)
photo caption	Landsat image (en)
type	Cinder cones (en)
georss:point	61.37027777777778 -163.98694444444445
has abstract	The Ingakslugwat Hills volcanic field is in the Yukon–Kuskokwim Delta in western Alaska. It contains eight large craters and about thirty small pyroclastic cones in an area of some 500 km2. The field contains unusual so-called "Ingakslugwat volcanoes", volcanic ridges up to 7 kilometres (4.3 mi) long and 400 metres (1,300 ft) high which are formed by pyroclastic material. They most likely formed by the interaction of permafrost with magma, seeing as they have a hydrovolcanic nature despite being high above the water table. The field is located 35 miles (56 km) north of Baird Inlet. The volcanoes rise 600 feet (180 m) over the surrounding plains and often contain small crater lakes. The height of the cones ranges 8–190 metres (26–623 ft). The volcanoes were active between 1 million and 700,000 years ago, but the latest activity may be of Holocene age. The volcanoes are formed by basaltic rocks. Other Quaternary volcanic centres in the region are Nelson Island and the Kusilvak Mountains. Olivine basalt is the principal volcanic rock but basanite and nephelinite are also found. (en)
last eruption	Unknown (en)

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