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Statements

Subject Item
dbr:Douglas_Glacier_(West_Coast,_New_Zealand)
rdf:type
geo:SpatialThing
rdfs:label
Douglas Glacier (West Coast, New Zealand)
rdfs:comment
The Douglas Glacier is a glacier in New Zealand's Southern Alps located between Mount Sefton and . It is named after the explorer Charles Edward Douglas. The glacier sits in a valley and is fed by materials consisting of many streams and frequent avalanches which drop from its névé down a cliff face of over 1,000 feet. The glacier itself was approximately 5 miles long in 1908. The glacier has a relatively high rate of moraine materials, consisting of "friable phyllites and schistose grauwackes".
owl:sameAs
n5:2H14L wikidata:Q24189612
geo:lat
-43.68
geo:long
170.0
foaf:depiction
n16:jinglealbumjangle.jpg
dct:subject
dbc:Glaciers_of_New_Zealand dbc:Geography_of_the_West_Coast,_New_Zealand
dbo:wikiPageID
46787014
dbo:wikiPageRevisionID
1013752815
dbo:wikiPageWikiLink
dbr:Névé dbc:Geography_of_the_West_Coast,_New_Zealand dbr:Glacier dbr:Grauwacke dbr:Moraine dbr:Charles_Edward_Douglas dbr:Glacier_recession dbr:Mount_Brunner dbr:Southern_Alps_(New_Zealand) dbr:Douglas_River dbr:Phyllite dbr:Mount_Sefton dbc:Glaciers_of_New_Zealand dbr:Avalanch
dbp:wikiPageUsesTemplate
dbt:Reflist dbt:WestCoastNZ-geo-stub dbt:Westland_landforms dbt:NewZealand-glacier-stub dbt:Coord
georss:point
-43.68 170.0
prov:wasDerivedFrom
wikipedia-en:Douglas_Glacier_(West_Coast,_New_Zealand)?oldid=1013752815&ns=0
dbo:wikiPageLength
1945
dbo:abstract
The Douglas Glacier is a glacier in New Zealand's Southern Alps located between Mount Sefton and . It is named after the explorer Charles Edward Douglas. The glacier sits in a valley and is fed by materials consisting of many streams and frequent avalanches which drop from its névé down a cliff face of over 1,000 feet. The glacier itself was approximately 5 miles long in 1908. The glacier has a relatively high rate of moraine materials, consisting of "friable phyllites and schistose grauwackes". At the foot of the glacier is a lake that was created by glacier recession. Reports from 1892 and 1934 indicated it had "an anomalously slow lake development". The Douglas River (formerly known as the Twain) begins in the lake at the foot of the glacier.
foaf:isPrimaryTopicOf
wikipedia-en:Douglas_Glacier_(West_Coast,_New_Zealand)
geo:geometry
POINT(170 -43.680000305176)