The Humber is a North Sea inlet on the East coast of England and it is one of the major deepwater estuaries in the U.K. The deepwater channel is 22 miles (35 kms.) long from the open sea at Spurn Point to Kingston Upon Hull. Further upstream at low tide there are many sandbanks that are exposed restricting navigation to smaller vessels.
The Humber starts at the juncture of the River Ouse and the River Trent, and at this point it is approximately 1 mile (1.6km) wide. It increases its width until at its mouth, 37 miles (59 kms.) to the east, it is about 8 miles (13 kms.) wide between North Lincolnshire and Kilnsea, East Yorkshire with Spurn Head jutting out nearly 4 miles (6.4 kms.) into the estuary.
The Humber with its canals and tributaries, (which include the rivers Hull, Ancholme, Derwent, Ouse and Trent) run off an area of 9,550 square miles (24,750 square kms.), which is about 20% of the total land area in England. This provides the largest single output of fresh water from Britain into the North Sea.
The Humber is a large tidal estuary and extremely turbid, the estuary has a brown appearance due to this high turbidity, and is often thought of as a dirty river. This is not so, the Humber is healthy and there are many Nature Conservation areas and important Nature Reserves in and around it.
The waters of the estuary are heavily laden with sediment, which comes from marine and riverine sources and the eroding boulder clay of the Holderness coast.
This sediment keeps extensive inter tidal flats and forms mud and sand bars that make semi-permanent islands along the shores, sand dunes and small lagoons can also be found. At low tide vast expanses of mud flats are exposed. These are one of the Humbers important habitats for millions of invertebrates, that provide a food source for many other species. Further upstream as the salinity decreases extensive reed beds fringe the estuary. Therefore the estuary supports a vast collection of wildlife and natural habitats from salt marsh and samphire beds to sub tidal sandbanks and many species of fish, birds are also a well known feature of the Humber, with many species of International importance using the Estuary.
A creek is usually smaller than a river, especially by length, partly by width and depth.
Vertical erosion is when the depth of the river is greater than the width causing erosion to take place on the bed of the river. This is also when lots of water enters the river but not as much is exiting it.
The motto of Stoke-on-Trent is 'Vis Unita Fortior'.
Wetted width is a term used in fluvial geomorphology. It is the width of a stream at the time of the field measurements indicating the width of the current flow and is generally below bankful width.
The depth depends on so many different things including the state of tributaries that empty into the river. The Army Corps of Engineers has to maintain a 9 ft depth across a 400 ft width of the river, for the barge traffic, but that is by no means the deepest part of the river. The record depths for the Beale Street gage in Memphis is 234.31 feet as the record high with a record low of 173.91 feet. At that gage the river is very narrow compared with up and downstream widths, so it would include the deepest part of the river.
The river Trent
The main river of Nottingham and Staffordshire is the River Trent.
The Yorkshire Ouse is connected to the River Trent by the Trent and Mersey Canal
The river Trent
The river Trent flows into the North Sea.
There's a clue in the name. Stoke-on-Trent lies on the River Trent.
Uh... the Trent?
The River Severn, River Trent and River Thames.
River Severn River Thames River Trent
The River Trent.
The River Trent (Severn and Thames being the first two).
Trent