Abstract
Dated historic structures provide a chronological framework for the evaluation of coastal greenschist weathering over periods of up to 450 years. A weathering rate of 0.6 mm a-1, derived by direct methods over a short period, is shown to be valid over a span of centuries. Local variations in aspect, elevation and exposure of the structures influence weathering processes and rates. This paper is a summary of work published in full elsewhere.
| Original language | English |
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| Pages (from-to) | 343-346 |
| Number of pages | 4 |
| Journal | Quarterly Journal of Engineering Geology and Hydrogeology |
| Volume | 31 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - Nov 1998 |