January 24th – Chasewater is still in overflow. This fascinates me – there has clearly been a deliberate decision to let the lake overtop the spillway rather than open the valve and let it flow into the canal. This is interesting, as had the water gone into the canal, the canal would have overflowed into the same culvert system, which feeds the Crane Brook. I must take a look at the crane brook when I can to see how it’s affected.
The flow from the breakwater is moving along the floor of the spillway, and into the new culvert system under the Victorian outfall. I guess that’s helping to irrigate the marsh there (as if it needed it, but you never know).
Exactly the same happened this time last year. Perhaps it’s some kind of stress test. It does mean however, that the two narrowboats moored in Anglesey Basin remain quiet on the relatively still canal…
BrownhillsBob's #365daysofbiking 