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River Tees
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Where is the River Tees located?
cross fell, the highest point in Pennine moorland is the source of the river
What is the geology of the upper course on the River Tees?
whinestone (hard) and limestone (soft)
What does the geology of the upper course lead to on the River Tees?
vertical erosion forming V-shaped valleys-high force waterfall found here
What is the geology in the middle course of the River Tees?
lateral (sideways) erosion forming meanders
What is the geology in the lower course of the River Tees?
large estuary, mudflats and sandbanks
What are the landforms present at the River Tees?
high force waterfall, meanders, river tees estuary
What weathering processes occur at the River Tees?
mechanical, biological and chemical
What erosion occurs at the River Tees?
hydraulic action, abrasion, attrition and corrosion
What transport occurs at the River Tees?
traction, saltation, suspension, solution and longshore drift
What management happened at the River Tees in 1810?
river straightening at Stockton-cut across the neck of the Mandale loop
What happened at the River Tees in 1995 and how much did this cost?
Tees barrage was completed and costed £54 million
What did the Tees barrage create?
£500 million of investment in offices, housing and leisure
What did the Yarm flood defence scheme of 1995 do?
-re-enforced concrete walls with 30 metal floodgates and earth embankments
-put in gabions to protect embankments
How much did the Yarm flood defence scheme cost and what did this do?
£2.1 million, discouraged new developments from building on low lying flood prone areas