The Severn Bore

Although not directly related to the geology of the Heritage Coast, the modern-day natural phenomena that is the Severn Bore, does in-part owe its origins to the physical shape of the Bristol Channel and River Severn. And, it is a wonderful physical feature to see and be aware of. The word bore comes from the old Viking word, bára meaning wave.

Wikipedia defines a “Bore” as a tidal phenomenon where by the leading edge of the incoming tide forms a wave(s) that travel up a river against the rivers current, usually where there is a large tidal range. Bores can only ever be generated on Spring Tides when the alignment of the Earth, Moon and Sun causes a gravitational bulge in the seawater leading to a greater volume of water entering an estuary. Bores are bigger around the time of the equinoxes.

Other rivers with bores include the Bay of Fundy in eastern Canada, the Amazon (pororoca) in Brazil, Qiantang River (silver dragon) in China and the Trent (aegir) of England.

The bores physical features become exaggerated as it flows into such funnel-shaped estuaries as The Bristol Channel and River Severn system. The presence of sandbars in the river also enhance the bore. In the open sea the extra volume of water associated with the Spring Tide is un-noticeable as its spread-out across such a vast area of water, with maybe only a mm or so of additional height. However, as that volume of water is pushed into an ever-diminishing space, the extra volume of water has no place to go except upwards (as it is confined by the banks of the channel into which it is flowing). So what start-off as a tiny ripple downstream changes to a wave of a few meters in height as it moves upstream.

Severn Bore taken from near Lydney, Gloucestershire

Because the timing of bores is dependent on the tides, the actual height of a bore depends upon the depth of the river channel and wind direction at the time. If ships frequently navigate up affected rivers the disturbance can deepen the river course thereby diminishing the bore.

Severn Bore taken from Minsterworth, Gloucestershire

The passage of the bore leads to a lot of churning of the water with the wave often having enough energy to rip-up vegetation along the banks of the river. After a bore has passed through the river can be littered with logs and branches. This introduces some danger to those that choose to surf or canoe the bore wave, which is a very popular thing to do! The Severn Bore tends to form a surf-able wave of up to 2m height between Awre almost to the city of Gloucester. The village of Newnham is the most popular location for the public to view the Severn Bore as it the main A48 road passes within feet of the River Severn although Minsterworth higher up the Severn is also a good spot. The longest single surf-run is reported to be 7.6 miles made in 2006.

A timetable of bores expected during 2018 is provided in the link below

http://www.thesevernbore.co.uk/timetable/4594160181

Follow me on :
This entry was posted in Uncategorized by swgt62. Bookmark the permalink.

About swgt62

Kevin Bate holds a B.Sc. in Geology from Aberystwyth University and an M.Sc. in Petroleum Geology from the University of Aberdeen. He has 30 years plus experience as a geologist in the Oil & Gas industry Kevin is a Fellow of the Geological Society of London (FGS) and is a member of the American Association of Petroleum Geologists (AAPG) Kevin has recently been certificated for the WERS2 First Aid course for outdoor instructors together with gaining a Level 3 Award in Education and Training (AOFAQ) Kevin established South Wales GeoTours as an independent business providing fee-based, guided one-day geological tours to tourists and amateur geologists alike in the South Wales area

Leave a Reply

Your email address will not be published. Required fields are marked *

This site uses Akismet to reduce spam. Learn how your comment data is processed.