Where are there meanders on the River Tees?
Where are there meanders on the River Tees?
Middle course As the River Tees starts to erode sideways (lateral erosion ), it forms meanders . These can be identified in the middle course near Barnard Castle.
What is the mouth of the River Tees?
North SeaRiver Tees / MouthThe North Sea is a sea of the Atlantic Ocean between Great Britain, Norway, Denmark, Germany, the Netherlands, Belgium and France. An epeiric sea on the European continental shelf, it connects to the ocean through the English Channel in the south and the Norwegian Sea in the north. Wikipedia
How does the River Tees change from source to mouth?
Teesside: The river Tees enters the North Sea through its estuary. In this area the river has been greatly modified by humans. A large meander (the Mandale Loop) was cut off, shortening the river by 4km, meaning the river flows faster to the sea.
What features can be found along the River Tees?
The River Tees is a fantastic river to study as it contains nearly all of the classic river landforms; V shaped valleys and interlocking spurs, waterfalls, floodplains and levees, meanders and ox bow lakes and an estuary at Tees mouth.
What causes flooding along the Tees?
Within the Tees CFMP area flooding is experienced from a number of sources, high rainfall and snowmelt results in high river flows which causes flooding throughout the catchment. In the estuary high tides can result in flooding in the low lying areas around the estuary.
What happens on the outside of a meander?
Erosion that forms a cut bank occurs at the outside bank of a meander because helicoidal flow of water keeps the bank washed clean of loose sand, silt, and sediment and subjects it to constant erosion. As a result, the meander erodes and migrates in the direction of the outside bend, forming the cut bank.
What causes meanders in rivers?
Meanders are produced when water in the stream channel erodes the sediments of an outer bend of a streambank and deposits this and other sediment on subsequent inner bends downstream. This process reinforces the riffle-pool structure of a stream.
When did the River Tees flood?
On the night of 16/17th November 1771 the North East of England suffered some of the worst and most destructive flooding on record. The river Tees burst its banks in a number of places with Yarm being one of the areas worst affected.
How are River Tees formed?
The source of the River Tees is Cross Fell in the Pennines. In its upper course, the River Tees flows over hard, impermeable rocks. Vertical erosion has formed classic V-shaped valleys.
What are the features of a meander?
A meander is when water flows in a curvy, bendy path, like a snake. As a river makes its way through an area that is relatively flat, it often develops bends as it erodes its way through the path of least resistance. Once a meander starts, it often becomes more and more exaggerated.
Where are meanders formed?
The formation of a meander. As the river erodes laterally, to the right side then the left side, it forms large bends, and then horseshoe-like loops called meanders . The formation of meanders is due to both deposition and erosion and meanders gradually migrate downstream.
Which course of the river does a meander occur?
A meander is a winding curve or bend in a river. They are typical of the middle and lower course of a river. This is because vertical erosion is replaced by a sideways form of erosion called LATERAL erosion, plus deposition within the floodplain.
What are some examples of meanders in nature?
Examples can be found along the River Tees. The River Tees is located in the north of England. The source of the River Tees is located in the Pennines and it flows east to its mouth where the river joins the North Sea. As the River Tees starts to erode sideways (lateral erosion), it forms meanders.
Where are the meanders of the River Tees?
Near Yarm, the meanders in the lower course are much larger, and oxbow lakes have formed. In this area there are also levees which have formed when the river has flooded. The River Tees has a very large estuary with mudflats and sandbanks which supports wildlife in the area. Sites such as Seal Sands are protected areas.
Where does the River Tees start and end?
It flows east from its source in the Pennines to its mouth, on the North Sea coast. The source of the River Tees is Cross Fell in the Pennines. In its upper course, the River Tees flows over hard, impermeable rocks. Vertical erosion has formed classic V-shaped valleys.
What are the characteristics of the River Tees?
High Force waterfall on the River Tees. As the River Tees reaches its middle course lateral erosion overtakes vertical erosion and is evidenced by winding meanders. Meanders in the lower course are much larger.