Everything about Teesdale totally explained
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There is a separate article for the local government district of 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
strata in the earlier
Carboniferous limestone country rock.
More recently,
Ice Age glacial activity shaped the valley, and much of the pre-glacial river course is now buried beneath
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,
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 of
County Durham, although the south side of Teesdale lies within the
historic county boundaries of the
North Riding of
Yorkshire. Formerly the
Startforth Rural District, it was transferred to County Durham for
administrative and
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.
Further Information
Get more info on 'Teesdale'.
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