Observations on October
10, 2005 suggest that stormwater flows on October 7 & 8 had,
indeed, carried significant amounts of sediment downstream from
the Stockwell Manor site. Sediment was visible on the streambed
at the mouth of Burke's Spring Branch (left below), in the channel
in Kirby Park (middle), and in impressive amounts at the downstream
end of the culvert that carries the stream under Kirby Road (right):
The scope of the problem was even more evident upstream of Kirby
Road, on the common land at Brooks Square. New deposits of orangish
sediment were visible below the outlet of the stormwater pond (left,
looking upstream toward the downstream end of the berm/outlet),
and in the area of the stormwater pond itself (middle, looking upstream
from the top of the berm; right, looking back downstream toward
the upstream end of the berm/outlet):
Deposits of orange clay spread thickly over the grass of the stormwater
pond, in places reaching almost 3" deep:
Similar problems could be observed further
upstream, on McLean Greens' common land and beyond.
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