Comments:
Historical straightening appears to be limited to the upper segment from Route 44 down to a pinch in the valley. The valley pinches naturally in the lower segment and the channel planform there was likely straight historically. Many small pieces of LWD, but overall recruitment potential very low. Channel banks are extensively armored, otherwise there would be significantly more erosion and widening (ie, channel locked into stage II). No evidence of significant overbank flow during T.S. Irene except for one bend in segment ~1,000ft downstream of Route 44.
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