The Springdale Caldera is a large Early Silurian caldera in west-central Newfoundland, Canada. It is at least 60 km (37 mi) long and 35 km (22 mi) wide, covering an area of more than 2,000 km2 (770 sq mi). It is one of the few calderas in Newfoundland that form a large Silurian age volcanic field. Basalt, andesite, rhyolite, pyroclastic rocks, debris flows, breccias and red sandstone are present at the Springdale Caldera.[1]
See also
References
External links
- The Springdale Caldera: A Field Guide for the Annual Field Meeting of the Geological Association of Canada, Newfoundland Branch
- Discordant Silurian paleolatitudes for central Newfoundland: New paleomagnetic evidence from the Springdale Group
- Sulurian Orogeny in the Newfoundland Appalachians
- Discordant Sulrian Paleolatitudes
- Geology, geochemistry and geochronology of the Springdale Group, an early Silurian Caldera in central Newfoundland
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This page was last edited on 28 June 2022, at 22:06