Teesdale is a dale, or valley, located principally in County Durham, North East England. It is one of the Durham Dales, which are themselves part of the North Pennines, the northernmost part of the Pennine uplands.
| Teesdale | |
|---|---|
.jpg) View over Middleton in Teesdale | |
| Geography | |
| Location | County Durham and Cumbria |
| Country | England |
| Population centers | Middleton in Teesdale, Barnard Castle |
| Borders on | |
| Coordinates | 54°32′42″N 1°55′37″W / 54.545°N 1.927°W |
| Traversed by | Teesdale Way, B6277 road |
| River | Tees, Skerne & Leven |
The dale is named after its principal river, the Tees, which has its source below Cross Fell (890 m (2,930 ft)) in Cumbria.[1] The upper dale is remote and high, but becomes gentler after it enters County Durham shortly downstream. The dale follows the river's south-easterly course to Barnard Castle, at which point the landscape begins to flatten into the Tees Lowlands. The Cumbrian part of Teesdale was historically divided between Cumberland and Westmorland, and the County Durham area between the former and Yorkshire.
Large parts of Teesdale are within the North Pennines national landscape, and Upper Teesdale has been designated a Site of Special Scientific Interest. Parts of the local climate have been scientifically classified as "Sub-Arctic", and snow has sometimes lain on Cross Fell into June.[2][3]
Geology
editUnusually for the Pennines, rock of igneous origin (the Whin Sill) contributes to the surface geology and scenery of Upper Teesdale. Around 295 million years ago upwelling magma spread through fissures and between strata in the earlier Carboniferous Limestone country rock. As it cooled (an event which is believed to have lasted 50 years) the rock contracted and caused itself to split into vertical columns. The heating of the limestone above the rock also caused it to be turned into a crumbly marble known as Sugar Limestone.[4][5]
Economic deposits in Llandovery rocks include soft shales that were previously worked to be used as slate pencils.[6]
More recently, Ice Age glacial activity shaped the valley, and much of the pre-glacial river course is now buried beneath glacial drift.
Botany
edit
In places this impervious dolerite rock, with shallow soil above it, prevented the growth of scrub or trees: this enabled certain post-glacial Arctic / Alpine plants to survive here when elsewhere as a rule they were overgrown. The Sugar Limestone formed by thermal metamorphism of the limestone into which the Whin Sill was intruded 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.[7]
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.[8] 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.[9] On the south bank of the Tees near High Force can be seen the largest surviving juniper wood in England.[10]
Geography
editOver ledges in the Whin Sill fall the famous waterfalls of High Force and Low Force and the cataract of Cauldron Snout.[11] From the source to the Skerne, Teesdale's principal town and most populous settlement is Barnard Castle,[12] a historic market town. The area also includes the small town of Middleton-in-Teesdale and a number of villages, including Mickleton, Eggleston, Romaldkirk and Cotherstone.[12] Middleton was a lead-mining centre,[13] and plentiful traces of this industry can be seen round the adjoining slopes and side-valleys.[14] On the south side of Teesdale is the Bronze Age burial site of Kirkcarrion.[15] The other Durham Dales are on the northern side and to the south is the Yorkshire Dales, Swaledale with Richmond is the closest.
| North | South |
|---|---|
| Source then Middleton-in-Teesdale | N/a |
| Eggleston | Cotherstone |
| Barnard Castle | Startforth |
| Whorlton | Ovington |
| Winston and Gainford | N/a |
| Piercebridge | |
| High Coniscliffe, Merrybent and Low Coniscliffe | Cleasby |
| Darlington | Stapleton |
| Hurworth and Neasham | Croft and Dalton |
| Middleton One Row | Over Dinsdale |
| Aislaby | Low Worsall |
| Egglescliffe | Yarm |
| Preston | Ingleby Barwick |
| Stockton (Bowesfield, town centre and Portrack) | Thornaby |
| Haverton Hill and Port Clarence | Middlesbrough (Old Middlesbrough and North Ormesby) |
| N/a | South Bank then the mouth |
Governance
editThe dale was formerly divided into four with the north in the Darlington and Stockton wards and the south was in the Gilling and Langbaurgh wapentakes.
Both dales gave their names to the former Teesdale district and Weardale district of western County Durham. The south is within the historic county boundaries of the North Riding of Yorkshire, Startforth Rural District, it was transferred to ceremonial County Durham on 1 April 1974, under the Local Government Act 1972. West Teesdale lies within the parliamentary constituency of Bishop Auckland (County Durham).[16]
Uses in local culture
edit- Teesdale (district), County Durham
- Teesdale Allotments, Site of Special Scientific Interest in the Teesdale district
- Teesdale Mercury, newspaper
- Middleton-in-Teesdale
- Forest-in-Teesdale
- Teesdale School, Barnard Castle
- Teesdale Way, path following the river Tees
- Teesdale Iron Works, former name of defunct Head Wrightson large heavy industrial firm based at Thornaby-on-Tees
- Teesdale Business Park, on the site of the former works
- Teesdale Park, Thornaby FC Ground
See also
editReferences
edit- ^ "Great country walks: Cross Fell, Pennine Hills, Cumbria". The Guardian. 26 January 2015. Retrieved 15 February 2017.
- ^ "North Pennines AONB". www.landscapesforlife.org.uk. Archived from the original on 7 March 2017. Retrieved 15 February 2017.
- ^ Gilbert, Joe (27 December 1997). "Skiing: Yad Moss: the St Moritz of the north". The Independent. Archived from the original on 26 May 2022. Retrieved 15 February 2017.
- ^ Cocker, Mark (27 April 2014). "The strange tale of Cronkley Scar, with its chaotic hem of boulder scree". The Guardian. Retrieved 14 February 2017.
- ^ "The Whin Sill" (PDF). northpennines.org.uk. North Pennines AONB. p. 2. Retrieved 14 February 2017.
- ^ Woodward, Horace B (1887). "4: Silurian (Upper Silurian)". The geology of England and Wales: with notes on the physical features of the country. London: G Phillip & Son. pp. 108–109. OCLC 933061775.
- ^ "Upper Teesdale SSSI" (PDF). naturalengland.org. pp. 1–5. Retrieved 14 February 2017.
- ^ "Moor House - Upper Teesdale NNR" (PDF). naturalengland.org. Natural England. 2014. p. 5. Retrieved 15 February 2017.
- ^ "High Force and Bowlees geotrail" (PDF). highforcewaterfall.com. Landscapes for Life. Retrieved 15 February 2017.
- ^ "Saving Teesdale's Juniper Wood". bbc.co.uk. BBC Tees. 13 November 2014. Retrieved 15 February 2017.
- ^ "Cow Green Reservoir – Visit Cumbria". www.visitcumbria.com. Retrieved 15 February 2017.
- ^ a b "Barnard Castle Masterplan Update" (PDF). durham.gov.uk. Durham County Council. December 2016. p. 3. Retrieved 15 February 2017.
- ^ "GENUKI - Middleton-in-Teesdale". joinermarriageindex.co.uk. Retrieved 15 February 2017.
- ^ "Teesdale's industrial heritage". Teesdale Mercury. 27 February 2008. Retrieved 15 February 2017.
- ^ Lloyd, Chris (8 April 2016). "Kirkcarrion keeps its secrets still". The Northern Echo. Retrieved 15 February 2017.
- ^ "History of Barnard Castle". www.barnardcastletowncouncil.gov.uk. Retrieved 15 February 2017.