Teesdale

Valley in Northern England


title: "Teesdale" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["river-tees", "valleys-of-north-yorkshire", "valleys-of-county-durham"] description: "Valley in Northern England" topic_path: "general/river-tees" source: "https://en.wikipedia.org/wiki/Teesdale" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Valley in Northern England ::

::data[format=table title="Infobox valley"]

FieldValue
nameTeesdale
photoPasture south of Middleton in Teesdale (edited, cropped).jpg
photo_captionView over Middleton in Teesdale
locationCounty Durham and Cumbria
countryEngland
townsMiddleton in Teesdale, Barnard Castle
coordinates
traversedTeesdale Way, B6277 road
riverTees, Skerne & Leven
::

::callout[type=note]

::

| name =Teesdale | other_name = | native_name = | native_name_lang = | translation = | photo =Pasture south of Middleton in Teesdale (edited, cropped).jpg | photo_caption =View over Middleton in Teesdale | map = | map_image = | map_caption = | location =County Durham and Cumbria | country =England | towns=Middleton in Teesdale, Barnard Castle | relief = | label = | label_position = | coordinates = | coordinates_ref = | elevation = | elevation_m = | elevation_ft = | elevation_ref = | length = | length_mi = | length_km = | length_orientation = | length_note = | width = | width_mi = | width_km = | width_orientation = | width_note = | area = | area_mi2 = | area_km2 = | depth = | depth_ft = |depth_m = |type = |age = |boundaries=

The dale is named after its principal river, the Tees, which has its source below Cross Fell (2,930 ft) in Cumbria. 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.

Geology

Unusually 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.

Economic deposits in Llandovery rocks include soft shales that were previously worked to be used as slate pencils.

More recently, Ice Age glacial activity shaped the valley, and much of the pre-glacial river course is now buried beneath glacial drift.

Botany

::figure[src="https://upload.wikimedia.org/wikipedia/commons/7/73/Teesdale_violet_at_Langdon_Head_-geograph.org.uk-_5778214.jpg" caption="Teesdale violet"] ::

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.

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

Over ledges in the Whin Sill fall the famous waterfalls of High Force and Low Force and the cataract of Cauldron Snout. From the source to the Skerne, Teesdale's principal town and most populous settlement is Barnard Castle, 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. Middleton 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 is the Bronze Age burial site of Kirkcarrion. The other Durham Dales are on the northern side and to the south is the Yorkshire Dales, Swaledale with Richmond is the closest. ::data[format=table title="Places by the River Tees"]

NorthSouth
Source then Middleton-in-TeesdaleN/a
EgglestonCotherstone
Barnard CastleStartforth
WhorltonOvington
Winston and GainfordN/a
Piercebridge
High Coniscliffe, Merrybent and Low ConiscliffeCleasby
DarlingtonStapleton
Hurworth and NeashamCroft and Dalton
Middleton One RowOver Dinsdale
AislabyLow Worsall
EgglescliffeYarm
PrestonIngleby Barwick
Stockton (Bowesfield, town centre and Portrack)Thornaby
Haverton Hill and Port ClarenceMiddlesbrough (Old Middlesbrough and North Ormesby)
N/aSouth Bank then the mouth
::

Governance

The 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).

Uses in local culture

References

References

  1. (26 January 2015). "Great country walks: Cross Fell, Pennine Hills, Cumbria". The Guardian.
  2. "North Pennines AONB".
  3. Gilbert, Joe. (27 December 1997). "Skiing: Yad Moss: the St Moritz of the north". The Independent.
  4. Cocker, Mark. (27 April 2014). "The strange tale of Cronkley Scar, with its chaotic hem of boulder scree". The Guardian.
  5. "The Whin Sill". North Pennines AONB.
  6. Woodward, Horace B. (1887). "The geology of England and Wales: with notes on the physical features of the country". G Phillip & Son.
  7. "Upper Teesdale SSSI".
  8. (2014). "Moor House - Upper Teesdale NNR". Natural England.
  9. "High Force and Bowlees geotrail". Landscapes for Life.
  10. (13 November 2014). "Saving Teesdale's Juniper Wood". BBC Tees.
  11. "Cow Green Reservoir – Visit Cumbria".
  12. (December 2016). "Barnard Castle Masterplan Update". Durham County Council.
  13. "GENUKI - Middleton-in-Teesdale".
  14. (27 February 2008). "Teesdale's industrial heritage". Teesdale Mercury.
  15. Lloyd, Chris. (8 April 2016). "Kirkcarrion keeps its secrets still". The Northern Echo.
  16. "History of Barnard Castle".

::callout[type=info title="Wikipedia Source"] This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page. ::

river-teesvalleys-of-north-yorkshirevalleys-of-county-durham