Karioi

http://dbpedia.org/resource/Karioi an entity of type: Thing

Karioi or Mount Karioi is a 2.4 million year old extinct stratovolcano 8 km (5.0 mi) SW of Raglan in the Waikato region of New Zealand's North Island. It was the earliest of the line of 6 calcalkalic volcanoes, the largest of which is Mount Pirongia (the others are at Kakepuku, Te Kawa, Tokanui, Waikeria and probably Puketotara). Karioi forms a background to many parts of Raglan. Karioi is also a location on the Central Plateau (see article on Karioi railway station). rdf:langString
rdf:langString Karioi
rdf:langString Mount Karioi
rdf:langString Mount Karioi
xsd:float -37.86666488647461
xsd:float 174.8166656494141
xsd:integer 37957571
xsd:integer 1124186850
xsd:integer 300
xsd:integer 756
rdf:langString right
rdf:langString North Island, New Zealand
rdf:langString Mt. Karioi, Raglan and Whaingaroa Harbour.jpg
rdf:langString Mt. Karioi, Raglan and Whaingaroa Harbour
rdf:langString to loiter or idle
rdf:langString Stratovolcano
xsd:string -37.86666666666667 174.81666666666666
rdf:langString Karioi or Mount Karioi is a 2.4 million year old extinct stratovolcano 8 km (5.0 mi) SW of Raglan in the Waikato region of New Zealand's North Island. It was the earliest of the line of 6 calcalkalic volcanoes, the largest of which is Mount Pirongia (the others are at Kakepuku, Te Kawa, Tokanui, Waikeria and probably Puketotara). Karioi forms a background to many parts of Raglan. Karioi was also a Highway Board area around the maunga from 1870 to 1889, when it was absorbed (with Whaingaroa Board area and formed into Karioi Riding) into Raglan County Council. In 1876 it had a population of 112 in 27 houses and in 1889 119 ratepayers, 80 of them absentees. Karioi is also a location on the Central Plateau (see article on Karioi railway station).
rdf:langString from Ruapuke Rd
xsd:nonNegativeInteger 36276
xsd:double 756.0
xsd:string BD32 Raglan
<Geometry> POINT(174.81666564941 -37.866664886475)

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