River terraces and their loessial cover beds, Awatere River valley, South Island, New Zealand
- 1 October 1989
- journal article
- soli science
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 32 (4), 487-497
- https://doi.org/10.1080/00288306.1989.10427556
Abstract
Loessial cover beds on river terraces were examined to determine the age of key terraces and the timing of latest major fluvial events. Six terrace sets or terraces are defined. Loessial cover beds on terraces are named after the terrace sets which represent fonner floodplains that the river occupied during sedimentation of each layer. Volcanic glass from c. 21 000 year old Aokautere Ash (Kawakawa Tephra) found within the loess has been used to date the last major river aggradation, which culminated about 17 000 years ago. A major change in river regimen occurred about 12 000 years ago, in which downcutting succeeded aggradation. This change is considered to mark the end of the Last Glacial.Keywords
This publication has 4 references indexed in Scilit:
- Toward a Comprehensive Upper Quaternary Tephra and Ignimbrite Stratigraphy in New Zealand using Electron Microprobe Analysis of Glass ShardsQuaternary Research, 1983
- New Zealand and Oblique‐Slip Margins: Tectonic Development up to and during the CainozoicPublished by Wiley ,1980
- Rate of Horizontal Fault Displacement in New ZealandNature, 1972
- Analysis of Progressive Fault Displacement During Downcutting at the Branch River Terraces, South Island, New ZealandGSA Bulletin, 1968