Jrl. Allen et Mj. Duffy, MEDIUM-TERM SEDIMENTATION ON HIGH INTERTIDAL MUDFLATS AND SALT MARSHES IN THE SEVERN ESTUARY, SW BRITAIN - THE ROLE OF WIND AND TIDE, Marine geology, 150(1-4), 1998, pp. 1-27
Six sites monitored monthly on salt marshes and mudflats in the middle
and outer Severn Estuary gave potentially predictive-retrodictive rel
ationships between the vertical response of the sedimentary surface (e
rosion/accretion), a factor reflecting tidal heights, and the wind-wav
e power-supply. The continuing rise of relative sea level in the area,
at the rate of a few millimetres annually, is providing accommodation
space at a pace low enough to permit the continuing vertical build-up
of the salt marshes throughout the estuary. On the mudflats, wind and
tidal conditions during the survey maintained an accretionary regime
in the middle estuary but an erosional one in the outer part. The Seve
rn Estuary is a system in delicate balance which is likely to respond
dramatically to modest changes in the tidal and/or wind regimes. (C) 1
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