Abstract
The main sediment transport paths in the Bristol Channel and Severn Estuary are briefly described; coarse sediment is transported in a generally westward direction and fine sediment in a generally eastward direction. The concept of differential two-way sediment transport is introduced and applied to the modern Bristol Channel area. This phenomenon is considered to be of significance in interpreting ancient sediment transport patterns and shelf configurations.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
