Lawrence Breakspear
Senior Member
Its also interesting to note that within the JBA consulting document (2013), it states how that the weirs, because of their historical industrial connections are some of the very reasons why the Teme has been given SSI status, it also acknowledges that when weirs have been removed or fell into a state of disrepair the river below the weir has suffered, because of the lack sediment control....and weirs must not be removed purely to put the river back to what it was or what they were:
2.2 Historic Evidence
Historic map evidence and legacy indicators identified during the geomorphological and
ecological audit suggests that the River Teme has been exploited for power generation
purposes for the last 300-400 years. Historic mills are frequent but often their associated weir
structures have been removed or have failed, however it is clear that these once had an
important control on the continuity of the system and influenced the natural sediment regime.
Channel indicators suggest that the bed incision downstream of Ludlow is a response to a
significant change in channel process. This could be attributed to channel reaction associated
with the weirs listed above that have been removed in the past. In combination, these could
have created impounded conditions for a significant length of the River Teme downstream of
Ludlow.
2.2 Historic Evidence
Historic map evidence and legacy indicators identified during the geomorphological and
ecological audit suggests that the River Teme has been exploited for power generation
purposes for the last 300-400 years. Historic mills are frequent but often their associated weir
structures have been removed or have failed, however it is clear that these once had an
important control on the continuity of the system and influenced the natural sediment regime.
Channel indicators suggest that the bed incision downstream of Ludlow is a response to a
significant change in channel process. This could be attributed to channel reaction associated
with the weirs listed above that have been removed in the past. In combination, these could
have created impounded conditions for a significant length of the River Teme downstream of
Ludlow.