Sedimentary response of Pagham Harbour, Southern England to barrier breaching in AD 1910

Cundy, A. B., Long, A. J., Hill, C. T., Spencer, C. and Croudace, I. W. (2002) Sedimentary response of Pagham Harbour, Southern England to barrier breaching in AD 1910. Geomorphology, 46 (3-4). pp. 163-176. ISSN 0169-555X Available from:

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This paper examines the evolution of Pagham Harbour, southern England following storm-induced breaching of a protective barrier in AD 1910. Stratigraphic studies of sediments collected from intertidal areas show the presence of a distinct stratigraphic horizon in the northeast of Pagham Harbour at ca. 0 to +1.0 m ordnance datum (OD). Radiometric data indicate that this horizon is a ‘reclamation surface’ formed after land claim in AD 1846. Following marine flooding in AD 1910, sediment has accreted relatively rapidly (at a broadly constant rate of between 4 and 8 mm a−1), wave and/or tidal energy have decreased and extensive marshes have developed. An asymptotic reduction in sediment accretion rate through time, as predicted in various theoretical models of salt marsh accretion, is not observed. Over the entire Pagham Harbour area, the period between AD 1948 and AD 1986 has seen an average marsh loss of 0.0087 km2 a−1, which is relatively small in comparison with other more exposed sites in the local area. Historically breached sites such as Pagham Harbour are common around European coasts, and these provide important natural laboratories within which the medium-term (decadal to centennial) coastal response to barrier breaching, and to managed-realignment coastal protection schemes, can be assessed.

Item Type:Article
Uncontrolled Keywords:sea-level rise, 210Pb and 137Cs dating, diatoms, barrier breaching, salt marshes, coastal management
Faculty/Department:Faculty of Environment and Technology > Department of Geography and Environmental Management
ID Code:8948
Deposited By: B. Upload account
Deposited On:15 Jul 2010 12:28
Last Modified:29 Jul 2016 13:55

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