Panther Run (a.k.a. Jordan River) is formed by the outlet of Panther Pond in Raymond, Maine (see The Maine Atlas and Gazetteer map 5 C2). The river starts at the dam on Mill Street and flows for one or so convoluted mile towards Jordan Bay in Sebago Lake. The big pool along the retaining wall by the dam is an accessible and popular brook trout fishing hole (click here for details). The river in the immediate vicinity of the dam flows briskly in early spring and has a substrate consisting of coarse sand, gravel and cobbles. In fact, the water flow and substrate composition are such that landlocked Atlantic salmon migrate up from Sebago Lake every fall to lay their eggs in this stretch of the river. But don’t be fooled… The character of the river changes dramatically no more than about 1000 ft downstream of the dam: the current slows down considerably, the banks widen up and become severely eroded, the water deepens in many places, and the substrate is made up entirely of fine white sand. The bottom is also carpeted with branches and other woody debris.
