River Blythe: Difference between revisions
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Explained why the site fails to reach the SSSI status of "favourable". Updated link for the SSSI citation. |
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[[File:Brueton Park - geograph.org.uk - 559259.jpg|thumb|left|[[Malvern & Brueton Park|Brueton Park]] Lake, formed by the damming of the River Blythe at [[Solihull]]]] |
[[File:Brueton Park - geograph.org.uk - 559259.jpg|thumb|left|[[Malvern & Brueton Park|Brueton Park]] Lake, formed by the damming of the River Blythe at [[Solihull]]]] |
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The [[river]] rises at various sources near [[Earlswood Lakes]], but the principal tributary is listed as Spring Brook ({{Coord|52.350915|-1.843601|region:GB_type:landmark}}; {{gbmapping|SP107725}}). From here it winds north east, skirting [[Cheswick Green]], towards [[Solihull]]. Here it passes through a local wildlife park, [[Malvern & Brueton Park|Malvern and Brueton Park and Nature Reserve]], where it briefly splits/outpours for approximately 250 metres to form Brueton Park Lake. From here it meanders east, past several old country houses—Old Berry Hall, Ravenshaw Hall and Eastcote Hall—before turning sharply south towards [[Barston]], which is encircled within a large meander of the river. At [[Temple Balsall]] the Cuttle Brook feeds the river, which now arcs north, and again close by Barston. Past [[Hampton in Arden]] the river is fed by ''Shadow Brook'', at ''Diddington Hall''. Travelling further north it passes to the east of [[Coleshill, Warwickshire|Coleshill]], and is fed by the [[River Cole, West Midlands|River Cole]], only a few hundred yards before it itself feeds into the [[River Tame, West Midlands|River Tame]] ({{Coord|52.522317|-1.688242|region:GB_type:landmark}}; {{gbmapping|SP212916}}), at Ladywalk Nature Reserve. |
The [[river]] rises at various sources near [[Earlswood Lakes]], but the principal tributary is listed as Spring Brook<ref name=":0">[https://www.therrc.co.uk/sites/default/files/files/Designated_Rivers/river_blythe_draft_restoration_plan-web_4.pdf "River Blythe Restoration Plan JBA Consulting 2017"] Retrieved 05/04/2022</ref> ({{Coord|52.350915|-1.843601|region:GB_type:landmark}}; {{gbmapping|SP107725}}). From here it winds north east, skirting [[Cheswick Green]], towards [[Solihull]]. Here it passes through a local wildlife park, [[Malvern & Brueton Park|Malvern and Brueton Park and Nature Reserve]], where it briefly splits/outpours for approximately 250 metres to form Brueton Park Lake. From here it meanders east, past several old country houses—Old Berry Hall, Ravenshaw Hall and Eastcote Hall—before turning sharply south towards [[Barston]], which is encircled within a large meander of the river. At [[Temple Balsall]] the Cuttle Brook feeds the river, which now arcs north, and again close by Barston. Past [[Hampton in Arden]] the river is fed by ''Shadow Brook'', at ''Diddington Hall''. Travelling further north it passes to the east of [[Coleshill, Warwickshire|Coleshill]], and is fed by the [[River Cole, West Midlands|River Cole]], only a few hundred yards before it itself feeds into the [[River Tame, West Midlands|River Tame]] ({{Coord|52.522317|-1.688242|region:GB_type:landmark}}; {{gbmapping|SP212916}}), at Ladywalk Nature Reserve. |
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[[File:Blythe Valley - geograph.org.uk - 65387.jpg|thumb|left|Blythe Valley, looking north along the River Blythe near Eastcote]] |
[[File:Blythe Valley - geograph.org.uk - 65387.jpg|thumb|left|Blythe Valley, looking north along the River Blythe near Eastcote]] |
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The river is "a particularly fine example of a lowland river on clay" according to its [[Sites of Special Scientific Interest]] citation. The SSSI was notified in 1989, and includes a {{convert|24|mi|km|adj=on}} stretch of the river from near its source to the point it joins the River Tame.<ref name=en> |
The river is "a particularly fine example of a lowland river on clay" according to its [[Sites of Special Scientific Interest]] citation. The SSSI was notified in 1989, and includes a {{convert|24|mi|km|adj=on}} stretch of the river from near its source to the point it joins the River Tame.<ref name="en">[https://designatedsites.naturalengland.org.uk/PDFsForWeb/Citation/1001772.pdf "English Nature SSSI Citation"] Retrieved 05/04/2022</ref> The Blythe has a wide range of natural geographical features such as riffles, pools, small cliffs and meanders, combined with a high diversity of substrate types ranging from fine silt and clay in the lower reaches to sands and gravels in the upper and middle reaches. The structure of this river is very variable and diverse, and is important as a rare example of such in lowland Britain.<ref name=en /> |
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[[File:The old Packhorse Bridge - geograph.org.uk - 50348.jpg|thumb|left|The old Packhorse Bridge, south of [[Hampton-in-Arden]], crossing the River Blythe]] |
[[File:The old Packhorse Bridge - geograph.org.uk - 50348.jpg|thumb|left|The old Packhorse Bridge, south of [[Hampton-in-Arden]], crossing the River Blythe]] |
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The diverse physical features of the Blythe are matched by its diverse plant communities. Botanically, the Blythe is one of the richest rivers in lowland England, with the most species-rich sections containing as many species as the very richest chalk streams.<ref name=en /> In addition, several damp, unimproved meadows occur along the length of the river; they receive some of their water from annual flooding and are largely dependent upon the river for the maintenance of a high water-table.<ref name=en /> As well as the rich and diverse flora, the river supports a diverse invertebrate community with a wide range of [[molluscs]], [[oligochaetes]] and [[caddisfly|caddisflies]].<ref name=en /> |
The diverse physical features of the Blythe are matched by its diverse plant communities. Botanically, the Blythe is one of the richest rivers in lowland England, with the most species-rich sections containing as many species as the very richest chalk streams.<ref name=en /> In addition, several damp, unimproved meadows occur along the length of the river; they receive some of their water from annual flooding and are largely dependent upon the river for the maintenance of a high water-table.<ref name=en /> As well as the rich and diverse flora, the river supports a diverse invertebrate community with a wide range of [[molluscs]], [[oligochaetes]] and [[caddisfly|caddisflies]].<ref name=en /> |
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However, physical modification to the watercourse and the riparian zone has impacted the functionality of the River Blythe, resulting in the SSSI's condition labelled as "unfavourable no change" in 2017. <ref name=":0" /> The factors leading to this were mainly due to historic management; many sections of the river have been straightened, and the riparian zone modified and disrupted, upsetting the site's ecological health and lowering the overall SSSI status. |
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| ⚫ | The river is popular with anglers along much of its length, although in dry weather it can become shallow in places. Species to be found include [[perch]], [[European chub|chub]] and [[Common Dace|dace]] with occasional summer [[carp]] being caught. The river also holds [[tench]], [[bream]] and [[rudd]] and more recently a small number of [[Barbus barbus|barbel]] have been caught. |
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| ⚫ | The river is popular with anglers along much of its length, although in dry weather it can become shallow in places. Species to be found include [[perch]], [[European chub|chub]] and [[Common Dace|dace]] with occasional summer [[carp]] being caught. The river also holds [[tench]], [[bream]] and [[rudd]] and more recently a small number of [[Barbus barbus|barbel]] have been caught. |
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It is one of the cleanest rivers in England.{{Citation needed|date=September 2009}}. |
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==See also== |
==See also== |
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Revision as of 22:49, 5 April 2022
| River Blythe | |
|---|---|
 The river near Hampton-in-Arden | |
 | |
| Location | |
| Country | England |
| Physical characteristics | |
| Source | |
| • location | Earlswood Lakes, Warwickshire |
| • coordinates | 52°21′58″N 1°50′00″W / 52.366184°N 1.833267°W |
| Mouth | |
• location | Confluence with the Tame at Ladywalk |
• coordinates | 52°28′0″N 1°40′45″W / 52.46667°N 1.67917°W |
| Basin features | |
| Progression | Tame—Trent—Humber—North Sea |
The River Blythe flows through the English Midlands from central Warwickshire, through the Borough of Solihull and on to Coleshill in north Warwickshire. It runs along the Meriden Gap in the Midlands Plateau, is fed by the River Cole and is a tributary of the River Tame beside the West Midland Bird Club's Ladywalk reserve. This then joins the River Trent, whose waters reach the North Sea via the Humber Estuary.
The river rises at various sources near Earlswood Lakes, but the principal tributary is listed as Spring Brook[1] (52°21′03″N 1°50′37″W / 52.350915°N 1.843601°W; grid reference SP107725). From here it winds north east, skirting Cheswick Green, towards Solihull. Here it passes through a local wildlife park, Malvern and Brueton Park and Nature Reserve, where it briefly splits/outpours for approximately 250 metres to form Brueton Park Lake. From here it meanders east, past several old country houses—Old Berry Hall, Ravenshaw Hall and Eastcote Hall—before turning sharply south towards Barston, which is encircled within a large meander of the river. At Temple Balsall the Cuttle Brook feeds the river, which now arcs north, and again close by Barston. Past Hampton in Arden the river is fed by Shadow Brook, at Diddington Hall. Travelling further north it passes to the east of Coleshill, and is fed by the River Cole, only a few hundred yards before it itself feeds into the River Tame (52°31′20″N 1°41′18″W / 52.522317°N 1.688242°W; grid reference SP212916), at Ladywalk Nature Reserve.
The river is "a particularly fine example of a lowland river on clay" according to its Sites of Special Scientific Interest citation. The SSSI was notified in 1989, and includes a 24-mile (39 km) stretch of the river from near its source to the point it joins the River Tame.[2] The Blythe has a wide range of natural geographical features such as riffles, pools, small cliffs and meanders, combined with a high diversity of substrate types ranging from fine silt and clay in the lower reaches to sands and gravels in the upper and middle reaches. The structure of this river is very variable and diverse, and is important as a rare example of such in lowland Britain.[2]
The diverse physical features of the Blythe are matched by its diverse plant communities. Botanically, the Blythe is one of the richest rivers in lowland England, with the most species-rich sections containing as many species as the very richest chalk streams.[2] In addition, several damp, unimproved meadows occur along the length of the river; they receive some of their water from annual flooding and are largely dependent upon the river for the maintenance of a high water-table.[2] As well as the rich and diverse flora, the river supports a diverse invertebrate community with a wide range of molluscs, oligochaetes and caddisflies.[2]
However, physical modification to the watercourse and the riparian zone has impacted the functionality of the River Blythe, resulting in the SSSI's condition labelled as "unfavourable no change" in 2017. [1] The factors leading to this were mainly due to historic management; many sections of the river have been straightened, and the riparian zone modified and disrupted, upsetting the site's ecological health and lowering the overall SSSI status.
The river is popular with anglers along much of its length, although in dry weather it can become shallow in places. Species to be found include perch, chub and dace with occasional summer carp being caught. The river also holds tench, bream and rudd and more recently a small number of barbel have been caught.
See also
References
- ^ a b "River Blythe Restoration Plan JBA Consulting 2017" Retrieved 05/04/2022
- ^ a b c d e "English Nature SSSI Citation" Retrieved 05/04/2022
External links
- River Blythe. Retrieved on 2008-05-24