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Statements

Subject Item
dbr:Brau_Kettle
rdf:type
owl:Thing geo:SpatialThing dbo:Work
rdfs:label
Brau Kettle
rdfs:comment
The Brau Kettle is a geological feature known as a karst that is located along the Wallpack Ridge in the Delaware Water Gap National Recreation Area in Sandyston Township, New Jersey. Its name derives from the Dutch for "brewing kettle" or "boiling kettle" which describes how water suddenly bubbles up from the ground. This site is referenced in early French Jesuit and Dutch colonial manuscripts as a landmark near which colonial traders exchanged goods with the Munsee and other local Native American tribes. According to the , the feature looks like a sinkhole in dry times during the year. It is known to flow at random, after periods of precipitation, and is thought to be fed by a that vanishes in the forest roughly 1,800 feet away.
geo:lat
41.13999938964844
geo:long
-74.91300201416016
dct:subject
dbc:Geology_of_New_Jersey dbc:Delaware_Water_Gap_National_Recreation_Area dbc:Sandyston_Township,_New_Jersey dbc:Landforms_of_Sussex_County,_New_Jersey
dbo:wikiPageID
36229902
dbo:wikiPageRevisionID
1114547917
dbo:wikiPageWikiLink
dbr:Sussex_County,_New_Jersey dbr:Lenape dbr:New_Jersey_Geological_Survey dbr:Sinkhole dbc:Sandyston_Township,_New_Jersey dbr:Sinking_stream dbc:Delaware_Water_Gap_National_Recreation_Area dbr:Sandyston_Township,_New_Jersey dbr:Delaware_Water_Gap_National_Recreation_Area dbr:Geology_of_New_Jersey dbr:Karst dbr:Wallpack_Ridge dbc:Geology_of_New_Jersey dbc:Landforms_of_Sussex_County,_New_Jersey
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dbt:Delaware_Water_Gap_National_Recreation_Area dbt:Authority_control dbt:Reflist dbt:Coord
georss:point
41.14 -74.913
dbo:abstract
The Brau Kettle is a geological feature known as a karst that is located along the Wallpack Ridge in the Delaware Water Gap National Recreation Area in Sandyston Township, New Jersey. Its name derives from the Dutch for "brewing kettle" or "boiling kettle" which describes how water suddenly bubbles up from the ground. This site is referenced in early French Jesuit and Dutch colonial manuscripts as a landmark near which colonial traders exchanged goods with the Munsee and other local Native American tribes. According to the , the feature looks like a sinkhole in dry times during the year. It is known to flow at random, after periods of precipitation, and is thought to be fed by a that vanishes in the forest roughly 1,800 feet away.
gold:hypernym
dbr:Feature
prov:wasDerivedFrom
wikipedia-en:Brau_Kettle?oldid=1114547917&ns=0
dbo:wikiPageLength
1694
foaf:isPrimaryTopicOf
wikipedia-en:Brau_Kettle
geo:geometry
POINT(-74.91300201416 41.139999389648)