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Studies of coastal morphodynamics are becoming increasingly more focused on quantification of relationships between processes, form and function of dynamic landform systems because wave climates (e.g., wave height, wave period, seasonality, cyclical patterns) and sediments (i.e., composition, size, and shape) interact in various ways to collectively produce distinctive types of beaches.
Applications of existing and planned methodology to field research will help extend our understanding of the dynamic landform and landscape changes that take place through space and time.
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Orford Ness is one of the most dynamic landforms on the UK coastline and the largest vegetated shingle spit in Europe.
They are dynamic landforms that are prone to abrupt changes on a geomorphological (decades to centuries) time scale, while also being long-term deposition features that preserve sedimentary strata and are sensitive indictors of environmental change.
Notions that climate plays a major dynamic role in landform evolution were in evidence during the first decade of the 20th century but did not emerge in formalized theory until the mid-1900s.
As one of the most dynamic environments, coastal landforms' constant changes are the result of both human activities and physical processes.
Sediment gravity flows are among the most dynamic processes, transforming these landforms.
Again, the result is a dynamic equilibrium in which the landform adjusts to processes acting upon it.
The typical Holocene response of southern Ontario rivers is confounded by numerous distinct glacial landform assemblages and dynamic baselevel histories.
Cosmogenic 10Be and 26Al data together with geomorphic relationships reveal that these landforms are more dynamic and younger than previously suspected.
In this paper, we develop tools to assist in the monitoring of creek network evolution towards dynamic morphological equilibrium, a state of landform stability under current physical forcings.
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