Coromandel Volcanic Zone

Coromandel Volcanic Zone
Hochstetter 1859 geological map of the southern part of the then Auckland Province that recognised the Coromandel volcanics of this part of the North Island.
Highest point
Elevation953 m (3,127 ft)
Coordinates37°10′S 175°38′E / 37.16°S 175.64°E / -37.16; 175.64
Geography
Map
Map centred upon the Coromandel Volcanic Zone. Clicking on the map enlarges it, and enables panning and mouseover of volcano name/wikilink and ages before present. Key for the volcanics that are shown with panning is:   basalt (shades of brown/orange),   monogenetic basalts,
  undifferentiated basalts of the Tangihua Complex in Northland Allochthon,
  arc basalts,   arc ring basalts,
  dacite,
  andesite (shades of red),   basaltic andesite,
  rhyolite, (ignimbrite is lighter shades of violet),
and   plutonic. White shading is selected caldera features.
Geology
Rock age(s)Miocene and Pliocene 18–4 Ma
Mountain typeVolcanic area
Rock type(s)Andesite and Rhyolite
Volcanic arcCoromandel Volcanic Zone
Last eruptionc. 2.5 million years ago[1] (subsequent evidence closer to 4 million years ago)[2][3]

The Coromandel Volcanic Zone (CVZ) is an extinct intraplate volcanic arc stretching from Great Barrier Island in the north, through the Coromandel Peninsula, to the Kaimai Range in the south. The area of transition between it and the newer and still active Taupō Volcanic Zone is now usually separated and is called the Tauranga Volcanic Centre. Its volcanic activity was associated with the formation and most active period of the Hauraki Rift.

  1. ^ Cite error: The named reference Briggs et al was invoked but never defined (see the help page).
  2. ^ Cite error: The named reference Pittari2021 was invoked but never defined (see the help page).
  3. ^ Cite error: The named reference Pank2023 was invoked but never defined (see the help page).