Tauhara Volcano, Taupo Zone
- 1 March 1968
- journal article
- research article
- Published by Informa UK Limited in New Zealand Journal of Geology and Geophysics
- Vol. 11 (1), 212-224
- https://doi.org/10.1080/00288306.1968.10423686
Abstract
The extinct multiple volcano, Tauhara, of late Pleistocene age, is north-east of Lake Taupo, and consists of five coalescing dacite cumulo-domes. Another dome, Maunganamu N, 3 miles south of Tauhara, is included in the study. The morphology and structure of these domes are described. The internal fan-shaped structure of the flow banding as seen in cross section suggests that each dome was formed from lava continuously extruded from separate vents. The superficial ash deposits of the Taupo ash sequence, which mantle the volcano, are described briefly.Keywords
This publication has 4 references indexed in Scilit:
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- Geological structure and volcanism of the Taupo-Tarawera districtNew Zealand Journal of Geology and Geophysics, 1959
- A macroscopic method of fabric analysisAmerican Journal of Science, 1951
- Structures in the Dacitic Flows at Crater Lake, OregonThe Journal of Geology, 1936