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| Sturgeon Lake Caldera | |
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| Elevation | approx. 455 m (1,493 ft) |
| Location | Ontario, Canada |
| Coordinates | |
| Type | Caldera |
| Volcanic arc/belt | Wabigoon greenstone belt |
| Age of rock | Neoarchean |
| Last eruption | Neoarchean |
| Listing | List of volcanoes in Canada |
Sturgeon Lake Caldera is a large extinct caldera in Kenora District of Northwestern Ontario, Canada. It is one the world's best preserved mineralized Neoarchean caldera complexes, containing well-preserved mafic-intermediate pillow lavas, pillow breccias. hyaloclastite and peperites, submarine lava domes and dome-associated breccia deposits. The complex is some 2.7 billion years old[1] with a minimum strike length of 30 km (19 mi).
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Geology
The Sturgeon Lake Caldera contains a well preserved north facing homoclinal chain of greenschist facies metamorphosed intrusive, volcanic, and sedimentary layers. This piecemeal caldera complex includes nearly 3,000 m (9,843 ft) of major subaqueously deposited intracaldera fill. Episodes of subaerial and subaqueous explosive felsic volcanism created rhyodacitic to rhyolitic tuffs and lapilli tuffs. The caldera complex lies in the Wabigoon greenstone belt.
The Sturgeon Lake Caldera contains volcanic units that outcrop over 30 kilometers from east to west with up to five separate, major ash flow tuff units with thickness ranging from 100 to 1200 meters. The Mattabi pyroclastic flow, with a thickness in excess of 800 m (2,625 ft) and a strike length of at least 30 km (19 mi), is the third and most voluminous eruptive event associated with the Sturgeon Lake Caldera. It hosts the 12-Mt Mattabi massive sulfide deposit which is interpreted to have formed on and below the seafloor, the latter through the processes of pore-space filling and replacement.
See also
References
- ^ Caldera Volcanoes Retrieved on 2007-07-20
External links
