Jed Water | |
---|---|
Physical characteristics | |
Source | Carlin Tooth |
• location | 1 mile from England in the Cheviot Hills |
• coordinates | 55°18′55″N2°34′50″W / 55.31528°N 2.58056°W |
Mouth | Jedfoot Bridge |
• location | north of Jedburgh, Scotland |
Length | 21.75 miles (35.00 km) [1] |
Depth | |
• minimum | 0.37 metres (1.2 ft) [2] |
• maximum | 2.33 metres (7.6 ft) (exceptionally 3.5 metres (11 ft)) [2] |
Basin features | |
River system | River Tweed |
The Jed Water is a river and a tributary of the River Teviot in the Borders region of Scotland.
In total the Jed Water is over 21.75 miles (35.00 km) long and it falls 1,375 feet (0.419 km). It flows into the Teviot near Jedfoot Bridge (grid reference NT660243 ) two miles north of Jedburgh. Jed Water rises from a source on Carlin Tooth 55°18′55″N2°34′50″W / 55.31528°N 2.58056°W in the Cheviot Hills where it is first known as Raven Burn. [3]
The river in past times was the main source of water for the monks living in Jedburgh Abbey. It also powered a watermill in the town of Jedburgh although this no longer exists. It gives its name to Jedburgh and Jedforest. In the 1800s it had trout in the river. The Ordnance gazetteer said Jed Water "in the parts immediately above the town of Jedburgh ... more of the elements of fine landscape than during a whole day's ride in the most favourite Scottish haunts of tourists." [1] The guide drew attention to the pure waters, the brisk currents, the steep landscapes and the contrasts which it thought picturesque. [1]
The name Jed is of obscure origin. [4] James has suggested that it may derive from Proto-Indo-European *wei(h1)- d- "a bend, something curved or twisted". [5] He also notes that Scots Gedde- in Jedburgh may have been adopted from Cumbric gwï:δ "a wood", and that the river name may be a back-formation. [5]
In 1787 James Hutton created modern geology when he discovered Hutton's Unconformity at Inchbonny, Jedburgh, in layers of sedimentary rock on the banks of the Jed Water. [6] He later wrote of how he "rejoiced at my good fortune in stumbling upon an object so interesting in the natural history of the earth, and which I had been long looking for in vain". [7]
Jed Water is liable to flood, so the river levels are monitored near the old Canongate Bridge. The depth is usually between 0.37 metres (1.2 ft) and 2.33 metres (7.6 ft) metres deep but it has been as deep as 3.5 metres (11 ft) which it reached in January 2016. [2] In 2020 there was a problem when the flood defences in Jedburgh were breached by debris in one storm just before another storm hit. Luckily repairs were made and serious flooding was avoided. [8]
Jedburgh is a town and former royal burgh in the Scottish Borders and the traditional county town of the historic county of Roxburghshire, the name of which was randomly chosen for Operation Jedburgh in support of the D-Day invasion.
Roxburghshire or the County of Roxburgh is a historic county and registration county in the Southern Uplands of Scotland. It borders Dumfriesshire to the west, Selkirkshire and Midlothian to the northwest, and Berwickshire to the north. To the southwest it borders Cumberland and to the southeast Northumberland, both in England.
The River Teviot, or Teviot Water, is a river of the Scottish Borders area of Scotland, and is the largest tributary of the River Tweed by catchment area. The Teviot is an important river for wildlife, especially the Atlantic salmon, but in recent years has witnessed at least four extreme flooding events.
Nisbet is a small hamlet on the B6400, in Roxburghshire, along the River Teviot, in the Scottish Borders area of Scotland. It is located 5.5 kilometres (3.4 mi) north of Jedburgh and 5 kilometres (3.1 mi) south of Roxburgh.
Jedforest is an historic forest in the Scottish Borders, that has been heavily wooded in the past. It is close to Jed Water and the town of Jedburgh, from which it takes its name.
Eden Water is a tributary of the River Tweed in the Scottish Borders of Scotland. "Water" is the Lowland Scots term for a small river.
Carlin Stone or Carline Stane is the name given to a number of prehistoric standing stones and natural stone or landscape features in Scotland. The significance of the name is unclear, other than its association with old hags, witches, and the legends of the Cailleach.
Minto is a village and parish in the Scottish Borders area of Scotland in Roxburghshire county. It is located 6 miles north-east of Hawick, north of the River Teviot.
Hutton's Unconformity is a name given to various notable geological sites in Scotland identified by the 18th-century Scottish geologist James Hutton as places where the junction between two types of rock formations can be seen. This geological phenomenon marks the location where rock formations created at different times and by different forces adjoin. For Hutton, such an unconformity provided evidence for his Plutonist theories of uniformitarianism and the age of Earth.
Timpendean Tower (tim-pen-deen) or Typenden Castle as it was once known, is a ruined 15th-century tower house near Lanton, around 1.5 miles (2.4 km) north-west of Jedburgh in the Scottish Borders.
The Borders Abbeys Way is a long-distance footpath in the Scottish Borders area of Scotland. It is a circular walkway and is 109 kilometres (68 mi) in length. The theme of the footpath is the ruined Borders abbeys along its way: Kelso Abbey, Jedburgh Abbey, Melrose Abbey and Dryburgh Abbey. These abbeys were homes to monks, who lived there between the 12th and 16th centuries. The route also passes through the towns of Hawick and Selkirk, and close to Abbotsford House, the home of Sir Walter Scott. Along the Borders Abbeys Way there are several rivers: Jed Water, River Teviot, River Tweed, Ale Water, and Rule Water.
Camptown is a small settlement on the A68, in the Scottish Borders area of Scotland, 5m (8 km) south of Jedburgh, and the same distance south to Carter Bar. The village lies on the course of the Jed Water, and the remains of a peel tower are close by at Edgerston.
The Ale Water is a tributary of the River Teviot, in the Scottish Borders area of Scotland. It rises at Henwoodie Hill and flows through Alemoor Loch. It meets the Teviot south of the village of Ancrum, and it runs through Ashkirk and Lilliesleaf. At Ancrum the depth of the water is between 0.26 metres (0.85 ft) and 2.24 metres (7.3 ft), although was as deep at 2.88 metres (9.4 ft) on one occasion in 2002.
Bedrule is a hamlet and civil parish in the historic county of Roxburghshire in the Scottish Borders area of Scotland. The hamlet lies on the east side of the Rule Water, which gave the village its name, about 4 miles west of Jedburgh. It lies south of the A698 between Hawick and Jedburgh. Other local place-names based on the river include Hallrule, Abbotrule, Ruletownhead and Spittal-on-Rule. Larger settlements include Bonchester Bridge and Denholm, as well as Hawick and Jedburgh.
Bonjedward is a hamlet in the Scottish Borders area of Scotland, two miles north of Jedburgh where the Jed Water joins the River Teviot.
The Rule Water is a river in the Scottish Borders area of Scotland, and a tributary of the River Teviot. The Rule Water rises in Wauchope Forest and passes Hobkirk, Bonchester Bridge, Hallrule, Abbotrule, and Bedrule until it joins the River Teviot at Spittal-on-Rule.
Crailing is a village on the A698, in Teviotdale, 4m east of Jedburgh in the Scottish Borders area of Scotland, in the historic county of Roxburghshire.
The Jedburgh Railway was a 9+1⁄2-mile (15 km) single-track branch railway in the Borders, Scotland, built by the Jedburgh Railway Company. It ran from a point south of Roxburgh Junction on the Kelso Line to Jedburgh via three intermediate stations, Kirkbank, Nisbet and Jedfoot.
The Canongate Bridge is a pedestrian bridge in the Scottish Borders town of Jedburgh. It was built as the town's main bridge over the Jed Water in the 16th century. Since 1971 it has been a category A listed building.
Whilst visiting Allar's Mill on the Jed Water, Hutton was delighted to see horizontal bands of red sandstone lying 'unconformably' on top of near vertical and folded bands of rock.