The Derwent Hunter Guyot is an extinct volcanic seamount of the Tasmantid Seamount Chain. It is a basaltic volcano that erupted between 12,400,000 and 15,400,000 years ago, with survey data that indicates it rises about 4,000 m (13,000 ft) above the local sea floor to a minimum depth of 323 m (1,060 ft). The sediments deposited on top of the alkali olivine basalt originate from the early Middle Miocene. The Derwent Hunter Guyot appears to be double peaked. It was discovered in 1958 and described as a seamount in 1961.
Attributes | Values |
---|
rdf:type
| |
rdfs:label
| - Derwent Hunter Guyot (en)
|
rdfs:comment
| - The Derwent Hunter Guyot is an extinct volcanic seamount of the Tasmantid Seamount Chain. It is a basaltic volcano that erupted between 12,400,000 and 15,400,000 years ago, with survey data that indicates it rises about 4,000 m (13,000 ft) above the local sea floor to a minimum depth of 323 m (1,060 ft). The sediments deposited on top of the alkali olivine basalt originate from the early Middle Miocene. The Derwent Hunter Guyot appears to be double peaked. It was discovered in 1958 and described as a seamount in 1961. (en)
|
name
| - Derwent Hunter Guyot (en)
|
geo:lat
| |
geo:long
| |
foaf:depiction
| |
dcterms:subject
| |
Wikipage page ID
| |
Wikipage revision ID
| |
Link from a Wikipage to another Wikipage
| |
sameAs
| |
dbp:wikiPageUsesTemplate
| |
thumbnail
| |
discovered
| - Named from the Australian schooner "Derwent Hunter" that discovered it in 1958 (en)
|
group
| |
location
| - To the east of the coast of New South Wales, Australia (en)
|
map caption
| - Location of the Derwent Hunter Guyot (en)
|
map size
| |
pushpin map
| |
type
| |
georss:point
| - -30.865833333333335 156.18916666666667
|
has abstract
| - The Derwent Hunter Guyot is an extinct volcanic seamount of the Tasmantid Seamount Chain. It is a basaltic volcano that erupted between 12,400,000 and 15,400,000 years ago, with survey data that indicates it rises about 4,000 m (13,000 ft) above the local sea floor to a minimum depth of 323 m (1,060 ft). The sediments deposited on top of the alkali olivine basalt originate from the early Middle Miocene. The Derwent Hunter Guyot appears to be double peaked. It was discovered in 1958 and described as a seamount in 1961. The waters above it are incorporated in the Central Eastern Marine Park, an Australian marine park. (en)
|
prov:wasDerivedFrom
| |
page length (characters) of wiki page
| |
foaf:isPrimaryTopicOf
| |
geo:geometry
| - POINT(156.18916320801 -30.865833282471)
|
is Link from a Wikipage to another Wikipage
of | |
is foaf:primaryTopic
of | |