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Rates and patterns of erosion on inter‐tidal shore platforms, Kaikoura Peninsula, South Island, New Zealand
Author(s) -
Stephenson Wayne J.,
Kirk Robert M.
Publication year - 1998
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/(sici)1096-9837(199812)23:12<1071::aid-esp922>3.0.co;2-u
Subject(s) - subaerial , shore , geology , weathering , erosion , peninsula , coastal erosion , lithology , geomorphology , hydrology (agriculture) , oceanography , geochemistry , geotechnical engineering , archaeology , geography
This paper presents measured rates of erosion on shore platforms at Kaikoura Peninsula, South Island, New Zealand. Surface lowering rates were measured with a micro‐erosion meter and traversing micro‐erosion meter. The mean lowering rate for all shore platforms was 1·130 mm a −1 . Differences in lowering rates were found between different platform types and lithologies. The rate of surface lowering on Type A (sloping) mudstone platforms was 1·983 mm a −1 , and 0·733 mm a −1 on Type B mudstone platforms (subhorizontal). On limestone platforms the lowering rate was 0·875 mm a −1 . A previously reported cross‐shore pattern of surface lowering rates from Kaikoura was not found. Rates were generally higher on the landward margins and decreased in a seaward direction. Season is shown statistically to influence erosion rates, with higher rates during summer than winter. The interpretation given to this is that the erosive process is subaerial weathering in the form of wetting and drying and salt weathering. This is contrary to views of shore platform development that have favoured marine processes over subaerial weathering. Copyright © 1998 John Wiley & Sons, Ltd.