Tim Palmer from America by Rivers, "Because of the glaciers' effectiveness in bulldozing soil, bedrock in New England rarely lies more than twenty feet underground and often juts up to the surface. Where rivers intersect these ledges and veins of resistant rock, sharp rapids occur." The far turn downstream from the bridge constitutes a mass of resistant rock, acting as a dam, slowing the water upstream, creating the shallow rapids further down.
Crows haunt the the river.
Deer leave tracks in the center,
then go to the edge.
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