Fall Creek meanders through the esker fields of the Malloryville Preserve. Here is the view from an abandoned railroad bridge. A major watercourse of the Finger Lakes, throughout the 19th century Fall Creek provided water power for local industry: grain grinding mills, cooperage and furniture. Here the stream bed is wide, flow slow and pacific for a mirrored surface, the effect broken by a single drop from an overhanging tree or, maybe, a fin’s flash.
Pam and I visited Malloryville last weekend to enjoy a “socially distanced” walk with family.
Well formed, sinuous, graded on both sides, eskers can be mistaken for man-made earthen structures, such as railroad embankments. Here is an example, nine-tenths (0.9) of a mile long substantial enough to direct the flow of Fall Creek. On entering the Malloryville esker bed the stream makes a right angle turn.
Here we are at the foot of the primary esker of Malloryville Preserve (it is marked as such on the information placard of this series first post). The slope to the right is the esker. A swamp lies to the right.
This video provides a better feeling for this esker.