Rates of coastal erosion and accretion in New Zealand
- 1 December 1978
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Marine and Freshwater Research
- Vol. 12 (4), 429-456
- https://doi.org/10.1080/00288330.1978.9515770
Abstract
Rates of coastal erosion and accretion for New Zealand are calculated for the period since early European colonization. Methods used for calculating rates from cadastral plans, vertical aerial photographs and field measurements are described, evaluated, and illustrated with examples. The most natural reference line for measurements of shoreline changes and for defining the seaward boundary of land is the seaward limit of land vegetation. Measurements made from air photographs and plans at scales larger than 1:4000 have errors less than .+-.1 m. As scales become small, errors increase proportionately. Along depositional shorelines, erosion and accretion generally occur at 0.5-4.0 m .cntdot. yr-1. Maximum erosion and accretion rates are 25.4 m .cntdot. yr-1 at North Kaipara Head and 68.9 m .cntdot. yr-1 at Farewell Spit, respectively. Cliff recession generally occurs at 0.25-1.0 m .cntdot. yr-1 with maximum rates of 2.25 m .cntdot. yr-1 for mudstone cliffs at Cape Turnagain and 3.46 m .cntdot. yr-1 for conglomerate cliffs at Ngapotiki.This publication has 6 references indexed in Scilit:
- The Evolution of Coastal Landforms of the Wairau ValleyNew Zealand Geographer, 1976
- Coastal changes at Kaikoura, 1942–74, determined from air photographsNew Zealand Journal of Geology and Geophysics, 1975
- Late holocene marine features adjacent to Port Nicholson, Wellington, New ZealandNew Zealand Journal of Geology and Geophysics, 1973
- COASTAL CHANGES AT THE ENTRANCE TO THE KAIPARA HARBOUR 1836–1966New Zealand Geographer, 1969
- Beach Erosion and Coastal Development in the Canterbury BightNew Zealand Geographer, 1969
- Sand movement at Mangatawhiri Spit and Little Omaha BayNew Zealand Journal of Geology and Geophysics, 1967