River Goyt

The River Goyt is a tributary of the River Mersey in North West England.

River Goyt
The River Goyt is highlighted in red Coordinates: 53.41420°N 2.15689°W / 53.41420; -2.15689
Location
Country	England
Physical characteristics
Source
• location	Axe Edge Moor, Derbyshire
• elevation	520 m (1,710 ft)
Mouth
• location	River Mersey
• elevation	40 m (130 ft)
Length	48.844 km (30.350 mi)
Basin features
Progression	Mersey—Irish Sea
Tributaries
• left	Todd Brook
• right	Sett, Etherow

River Goyt
Joins River Tame to form the River Mersey A560 Culvert at Stockport Poise Brook at Offerton Torkington Brook A627 at Marple Peak Forest Canal over Marple Aqueduct Sheffield–Manchester Line River Etherow A626 at Marple Bridge Hollywood Brook Mellor Brook Roman Lakes Sheffield–Manchester Line River Sett A6015 at New Mills Shedyard Brook Sheffield–Manchester Line Buxton–Manchester Line Black Brook A6 Peak Forest Canal A5004 at Whaley Bridge Buxton–Manchester Line Toddbrook Reservoir Randal Carr Brook Fernilee Reservoir Errwood Reservoir Source on Axe Edge Moor

Etymology

The name Goyt may be derived from the Middle English gote, meaning "a watercourse, a stream". Derivation from the Welsh gwyth meaning "vein" has been suggested, but described as "doubtful".

Course

The Goyt rises on the moors of Axe Edge, near the River Dane and the Cat and Fiddle Inn. The area is known as the Upper Goyt Valley. The old Cat and Fiddle Road from Buxton to Macclesfield crosses the river just as it turns northwards to flow down its well-known valley. The river then flows under Derbyshire Bridge, which was the old boundary between Derbyshire and Cheshire. Later it reaches an old packhorse bridge that was moved when Errwood reservoir was built in the 1960s (see photo below). Further downstream there is another reservoir, the Fernilee Reservoir, built in 1938. The original line of the Cromford and High Peak Railway can be seen near this point.

The Goyt then passes through Taxal and Horwich End where it is joined by the Todd Brook. Thereafter it passes through Whaley Bridge, New Mills (where it is joined by the River Sett) and Marple Bridge. Having been joined by the River Etherow, the Goyt joins the River Tame at Stockport, forming the River Mersey.

The section of the Goyt valley between Etherow Country Park and Whaley Bridge is followed by the Goyt Way, a 10-mile (16 km) walking route and part of the longer Midshires Way.

The River Goyt is reputedly haunted by the ghost of a girl whose Royalist lover drowned in the river.

Pollution

The river's Environment Agency pollution classification changed from moderate to poor in its lower section from the Etherow to the Mersey in 2016, and in 2015 for the New Mills to Whaley Bridge length. Otherwise the quality is moderate.

Tributaries

• Poise Brook (L)
  • Ochreley Brook (R)
• Torkington Brook (L)
  • Marple Brook (R)
• Padden Brook ?
• St Chad's Brook ?
• River Etherow (R)
• Marple Bridge Brook ? (R)
• Hollywood Brook ? (R)
• Mellor Brook ? (R)
• Linnet Brook ? (R)
• Strines Brook ? (R)
• Higgin's Brook ? (L)
• River Sett (R)
  • River Kinder (R)
    • Upper Brook ? (L)
    • William Brook ? (R)
    • Blackshaws Brook ? (L)
    • Red Brook (L)
• Shedyard Brook ? (R)
• Waterside Brook ? (R)
• Green Botham Brook ? (R)
• Todd Brook (L)
  • Gnathole Brook (L)
  • Carr Brook (R)
• Randal Carr Brook (R)
  • Meveril Brook (L)
    • Brook Houses Brook (R)

Gallery

• 
  The "Roman Bridge" over the River Goyt between New Mills and Marple Bridge is actually 17th century.
• 
  The Goyt (right) meets the Tame in Stockport to form the Mersey.
• 
  Goyts Bridge – the packhorse bridge (see Errwood Reservoir above) was partly broken in 1960, but restored when it was moved.
• 
  River Goyt at Furness Vale (1968) when the colour depended on discharges from the calico print mills in the valley.

See also

List of mills in New Mills area

References

Template:Attached KML/River Goyt

KML is from Wikidata

Further reading

"The Goyt Valley (Fact Sheet: 16)" (PDF). Peak District National Park Authority. Archived from the original (PDF) on 12 May 2013. Retrieved 28 April 2014.