Mt Manganuii , Bay of Plenty, Northeastern New Zealand
by Firoz Kadar Badesab, University of Bremen, Germany, Earth sciences, Germany
Mt Maunganui at the entrance of Tauranga Harbour, is a large lava dome formed by the upwelling of rhyolite lava about two to three million years ago. The urban area in the foreground occupies a narrow neck of dune sand called a tombolo that linked Mt Maunganui to the mainland several thousand years ago after sea level rose to its present height.
Categories
- Earth Magnetism & Rock Physics (345)
- Field (2823)
- Geochemistry, Mineralogy, Petrology & Volcanology (944)
- Ocean Sciences (325)
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Image properties
3264 × 2448 px;
image/jpeg; 1.9 MB
Camera:
Sony Cyber-Shot 12.1 Mega Pixels
Taken on 22
February
2010
Submitted on 21 February 2011
Licence
Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)
Credit
Firoz Kadar Badesab (distributed via imaggeo.egu.eu)
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