The Sphinx is a subglacial mound in the southernmost Coast Mountains of British Columbia, Canada. It is south-east of Garibaldi Lake. The volcano is part of the Garibaldi Volcanic Belt which is a segment of the Cascade Volcanic Arc, but it is not within the geographic boundary of the Cascade Range. It is believed The Sphinx last erupted in the Pleistocene age.

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  • 2402
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dbpedia-owl:elevation
  • 2402
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dbpprop:abstract
  • The Sphinx is a subglacial mound in the southernmost Coast Mountains of British Columbia, Canada. It is south-east of Garibaldi Lake. The volcano is part of the Garibaldi Volcanic Belt which is a segment of the Cascade Volcanic Arc, but it is not within the geographic boundary of the Cascade Range. It is believed The Sphinx last erupted in the Pleistocene age.
dbpprop:caption
  • The Sphinx in July 2001
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dbpprop:elevation
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dbpprop:lastEruption
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dbpprop:name
  • The Sphinx
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  • Mount_Garibaldi_002.JPG
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  • NTS 92G/15
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  • 49.90194444 -122.95138889
  • 49.901944444444 -122.95138888889
rdf:type
rdfs:comment
  • The Sphinx is a subglacial mound in the southernmost Coast Mountains of British Columbia, Canada. It is south-east of Garibaldi Lake. The volcano is part of the Garibaldi Volcanic Belt which is a segment of the Cascade Volcanic Arc, but it is not within the geographic boundary of the Cascade Range. It is believed The Sphinx last erupted in the Pleistocene age.
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  • The Sphinx
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  • 49.901943 (xsd:float)
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  • -122.951385 (xsd:float)
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  • The Sphinx
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