Teesdale
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Feline Hymnic
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/* Geology */ Accuracy: bedrock->country rock when describing intrusions.
{{Citations missing|date=November 2007}}
:''There is a separate article for the local government district of [[Teesdale (district)|Teesdale]]''.
'''Teesdale''' is a dale, or [[valley]], of the east side of the [[Pennines]] in [[England]]. The [[River Tees]] rises below [[Cross Fell]], the highest hill (2930 feet O.D.) in the Pennines, and its uppermost valley is remote and high. The local climate was scientifically classified as "Sub-Arctic" and snow has sometimes lain on Cross Fell into June.
==Geology==
Unusually for the Pennines, rock of volcanic origin, the [[Whin Sill]], contributes to the surface geology and scenery of Teesdale. Around 295 million years ago upwelling [[magma]] spread through through fissures and between [[stratum|strata]] in the earlier [[Carboniferous limestone]] [[country rock (geology)|country rock]].
More recently, [[Ice Age]] glacial activity shaped the valley, and much of the pre-glacial river course is now buried beneath [[Drift (geology)|glacial drift]].
==Botany==
In places this impervious [[dolerite]] rock, with shallow soil above it, prevented the growth of scrub or trees: this enabled post-glacial Arctic / Alpine plants to survive here when elsewhere they were overgrown. The residual "sugar" limestone once heated by the volcanic rock also meets the requirements of some of these plants. Teesdale is famous among naturalists for the "Teesdale Assemblage" of plants found together here that occur widely separated in other locations, abroad or in the British Isles.
Part of Upper Teesdale near the [[Cow Green Reservoir]] is designated a National Nature Reserve; it contains the unique Teesdale Violet and the blue Spring Gentian as well as more common Pennine flowers such as rockrose, spring sandwort, mountain pansy, bird's-eye primrose and butterwort. Hay meadows in the valley above High Force, some now carefully cultivated to ensure this, contain an extremely rich variety of flowering plants including globe flower, wood cranesbill and Early Purple Orchid. On the south bank of the Tees near High Force can be seen the largest surviving juniper wood in England.
==Geography and history==
Teesdale's principal villages include [[Middleton-in-Teesdale]], [[Mickleton, County Durham|Mickleton]], [[Eggleston]], [[Romaldkirk]], and [[Cotherstone]]. Middleton-in-Teesdale was a lead-mining centre, and plentiful traces of this industry can be seen round the adjoining slopes and side-valleys. On the South side of Teesdale looms the [[Bronze Age]] burial site of [[Kirkcarrion]].
Over ledges in the Whin sill fall the famous waterfalls of [[High Force]] and [[Low Force]] and the cataract of [[Cauldron Snout]].
Teesdale gives its name to the [[Teesdale (district)|Teesdale district]] of [[County Durham]], although the south side of Teesdale lies within the [[Historic counties of England|historic county boundaries]] of the [[North Riding of Yorkshire|North Riding]] of [[Yorkshire]]. Formerly the [[Startforth Rural District]], it was transferred to County Durham for [[metropolitan and non-metropolitan counties of England|administrative]] and [[ceremonial counties of England|ceremonial]] purposes on [[1 April]] [[1974]], under the provisions of the [[Local Government Act 1972]]. All of Teesdale lies within the parliamentary constituency of Bishop Auckland (Co. Durham).
The [[River Tees]] flows through Teesdale before reaching [[Barnard Castle]], thereafter passing to the south of [[Darlington]], reaching the [[North Sea]] south of [[Hartlepool]] after passing [[Stockton-on-Tees]] and [[Middlesbrough]]. Running roughly parallel to Teesdale to the north is [[Weardale]].
{{Durham}}
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[[Category:Geography of North Yorkshire]]
[[Category:Valleys of County Durham]]
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