Notes from the New Zealand Geological Survey—5: Age of Rotoiti Breccia
- 1 December 1968
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 11 (5), 1189-1191
- https://doi.org/10.1080/00288306.1968.10420248
Abstract
Rotoiti Breccia forms a submaturely dissected plateau sloping down northwards from the Okataina Rhyolite Centre (Thompson, 1964; Healy, 1964), which lies between Lakes Rotorua and Rotoma. Terrace deposits (H2+1) , correlated with the Last Glaciation (Upper Pleistocene), abut the northern margin of the plateau (Healy, Schofield, Thompson, 1964).Keywords
This publication has 2 references indexed in Scilit:
- Quaternary Volcanism of the Central Volcanic RegionNew Zealand Journal of Geology and Geophysics, 1964
- Volcanic mechanisms in the Taupo Volcanic Zone, New ZealandNew Zealand Journal of Geology and Geophysics, 1964