Mount Barrington Explained

Mount Barrington
Other Name:Barrington Volcano
Photo Size:260
Elevation M:1555
Location:Barrington Tops National Park,
New South Wales, Australia
Range:Mount Royal Range
Map:Australia New South Wales
Label Position:left
Map Size:250
Coordinates:-32.05°N 175°W
Type:Shield volcano
Age:Eocene[1]

Mount Barrington, a mountain that is part of the Mount Royal Range, is located on the Barrington Tops plateau in the Mid-Coast Council within New South Wales, Australia and has an elevation of above sea level.

Now the remnants of a volcano, Mount Barrington, formerly the Barrington Volcano, erupted near its present peak between 44 and 54 million years ago. The eruption caused a 700km3 basalt flow, which covered much of the Barrington Tops plateau. The lava was up to thick.

The extensive rainforests in the area grow on much of the resultant red/brown soils.[1] [2] Gemstones such as zircon, sapphire, sapphirine and ruby were formed from the volcano.[3] Nearby Careys Peak is considered a vent in this extinct shield volcano. The surrounding area is covered by sub alpine Snow Gum woodland, with rainforest on the escarpment edge and in fire free gullies.

See also

Notes and References

  1. Book: Johnson. Robert Wallace. Knutson. Jan. Taylor. Stuart Ross. Intraplate Volcanism: In Eastern Australia and New Zealand. 1989. Cambridge University Press. 978-0-521-38083-6. 123.
  2. Book: Adam, Paul. New South Wales Rainforests: The Nomination for the World Heritage List. 1987. 978-0-7305-2075-7. 78.
  3. Sutherland, F. L.. Fanning, C. M.. Gem‐bearing basaltic volcanism. Barrington, New South Wales: Cenozoic evolution, based on basalt K–Ar ages and zircon fission track and U–Pb isotope dating. Australian Journal of Earth Sciences. 48. 2. 2001 . 10.1046/j.1440-0952.2001.00851.x. 221–237. 129043286.