Tweed Volcano

Tweed Volcano
After activity ceased, the volcano rapidly eroded. Pictured here is Mount Warning, a volcanic plug that marks where the summit used to be.
Highest point
Elevation~1,900-2,312 m (6,200-7,586 ft)
Geography
LocationNortheastern New South Wales
Parent rangeGreat Dividing Range
Geology
Age of rockOver 23 Million Years
Mountain typeshield volcano
Last eruption~23 Ma

Tweed Volcano is a partially eroded Early Miocene shield volcano located in northeastern New South Wales, which formed when this region of Australia passed over the East Australia hotspot around 23 million years ago.[1] Mount Warning, Lamington Plateau and the Border Ranges between New South Wales and Queensland are among the remnants of this volcano that was originally over 100 kilometres (62 mi) in diameter and nearly twice the height of Mount Warning today, at 1,156 metres (3,793 ft). Despite its size, Tweed Volcano was not a supervolcano; other shield volcanoes—such as in the Hawaiian Islands—are much larger. In the 23 million years since the volcano was active, erosion has been extensive, forming a large erosion caldera around the volcanic plug of Mount Warning.[2] Its erosion caldera is the largest in the Southern Hemisphere.[3]

  1. ^ Knesel, Kurt M.; Cohen, Benjamin E.; Vasconcelos, Paulo M.; Thiede, David S. (2008). "Rapid change in drift of the Australian plate records collision with Ontong Java plateau". Nature. 454 (7205): 754–757. doi:10.1038/nature07138. PMID 18685705.
  2. ^ "Geological history". Geology of the Tweed. Tweed Regional Museum. Retrieved 3 February 2022.
  3. ^ the Caldera of the Tweed Volcano.

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