Large coefficients indicate important high and low tides major currents and movements usually take place on the sea bed. Identifying the importance of local and regional controls on foreland evolution is difficult, though, as the sensitivity of the foreland to processes operating at different spatial scales may well have changed through time. The following graph shows the progression of the tidal coefficient in the month of July of 2022.These values give us a rough idea of the tidal amplitude in Dungeness, forecast in July. Mon 27 Jun Tue 28 Jun Wed 29 Jun Thu 30 Jun Fri 1 Jul Sat 2 Jul Sun 3 Jul Max Tide Height. may be recorded by the return of marine conditions to Wickmaryholm Pit, breaching of the Dungeness foreland at Rye, and a sudden increase in the altitude of the gravel beaches in Denge Beach. However, evidence for a regional episode of increased storm incidence at ca. No clear relationship is apparent between long-term time/altitude changes in sea level and episodes of foreland development during the last ca. Under periods of high storm incidence, increased northward distal extension of the beach ridges in the study area has occurred, while under calmer conditions reduced distal extension has taken place. Where the change between high tide and low tide is at its smallest a Neap Tide has occurred. It is therefore argued that the alternating gravel and marsh sediments of the study area probably accumulated as a result of changes in storm incidence and gravel supply, and not oscillations in long-term sea level. The graph below shows the tide heights for Dungeness over the next seven days. Please note, the low and high tide times given are not suitable for navigational purposes. An established age/altitude graph of sea-level changes for the region shows that sea level changed little during the period of gravel deposition in the study area (ca. 7 day Dungeness tide chart These tide schedules are estimates based on the most relevant accurate location (Dungeness, Seacamp Dock, Georgia), this is not necessarily the closest tide station and may differ significantly depending on distance. Stratigraphic and diatom data from the marsh sediments in this area indicate that they accumulated under marine/ brackish and brackish tidal channel conditions, while pollen data from a peat bed recorded in the base of Wickmaryholm Pit show a removal and return of the marine influence at ca. The south coast of the foreland, between Jury's Gut and Galloway's Lookout, is characterised by alternating areas of marsh sediments and gravel which have previously been interpreted as evidence for several oscillations in sea level. The Dungeness foreland is located in the eastern part of the English Channel, and consists of over 500 gravel beaches which have accumulated since the mid-Holocene.
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