The Gargoyles
http://dbpedia.org/resource/The_Gargoyles an entity of type: Thing
The Gargoyles are two mountain peaks in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. The highest peak has an elevation of 1,823 m (5,981 ft) whereas the lowest peak has an elevation of 1,816 m (5,958 ft). A deeply eroded obsidian dome remnant at The Gargoyles contains 77% silica content and is the only Quaternary high-silica rhyolite identified anywhere in the Cascade Volcanic Arc north of the Three Sisters. The age of this rhyolite is poorly known.
rdf:langString
rdf:langString
The Gargoyles
rdf:langString
The Gargoyles
rdf:langString
The Gargoyles
xsd:float
49.80555725097656
xsd:float
-122.9974975585938
xsd:integer
71674615
xsd:integer
1117845077
xsd:integer
1823
rdf:langString
below
rdf:langString
Location in British Columbia
rdf:langString
Lava Peaks
xsd:string
49.80555555555556 -122.9975
rdf:langString
The Gargoyles are two mountain peaks in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. The highest peak has an elevation of 1,823 m (5,981 ft) whereas the lowest peak has an elevation of 1,816 m (5,958 ft). A deeply eroded obsidian dome remnant at The Gargoyles contains 77% silica content and is the only Quaternary high-silica rhyolite identified anywhere in the Cascade Volcanic Arc north of the Three Sisters. The age of this rhyolite is poorly known. The Gargoyles were originally mapped as the Lava Peaks by William Henry Mathews in 1958. The current name was suggested and adopted in 1978. Another name applied to The Gargoyles is Lava Peak.
xsd:nonNegativeInteger
2716
rdf:langString
Lava Peaks
xsd:double
1823.0
<Geometry>
POINT(-122.99749755859 49.805557250977)