The Kukri Peneplain is a near-horizontal and flat unconformity in the Transantarctic Mountains. The peneplain formed by erosion of the granitic and metamorphic basement rocks during the Paleozoic (Silurian to Devonian). Kukri Peneplain dips gently to the west.
Attributes | Values |
---|---|
rdf:type | |
rdfs:label |
|
rdfs:comment |
|
geo:lat |
|
geo:long |
|
dcterms:subject | |
Wikipage page ID |
|
Wikipage revision ID |
|
Link from a Wikipage to another Wikipage | |
sameAs | |
dbp:wikiPageUsesTemplate | |
georss:point |
|
has abstract |
|
prov:wasDerivedFrom | |
page length (characters) of wiki page |
|
foaf:isPrimaryTopicOf | |
geo:geometry |
|
is Link from a Wikipage to another Wikipage of | |
is foaf:primaryTopic of |