About: White Ridge Quartzite

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The White Ridge Quartzite is a geologic formation in central New Mexico. It has a maximum age of 1650 million years (Ma), corresponding to the Statherian period.

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dbo:abstract
  • The White Ridge Quartzite is a geologic formation in central New Mexico. It has a maximum age of 1650 million years (Ma), corresponding to the Statherian period. (en)
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  • 1073792372 (xsd:integer)
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dbp:name
  • White Ridge Quartzite (en)
dbp:namedby
  • Stark and Dapples (en)
dbp:namedfor
  • White Ridge (en)
dbp:otherlithology
dbp:overlies
dbp:period
  • Statherian (en)
dbp:prilithology
dbp:region
  • Los Pinos Mountains, New Mexico (en)
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dbp:underlies
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dbp:yearTs
  • 1946 (xsd:integer)
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georss:point
  • 34.383 -106.54
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  • The White Ridge Quartzite is a geologic formation in central New Mexico. It has a maximum age of 1650 million years (Ma), corresponding to the Statherian period. (en)
rdfs:label
  • White Ridge Quartzite (en)
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  • POINT(-106.54000091553 34.382999420166)
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  • 34.382999 (xsd:float)
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  • -106.540001 (xsd:float)
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