Geography
The river consists of two distinct parts - a flat upper portion that flows between South Watuppa Pond and Troy Street and a steep, rapid section between Troy Street and the Taunton River near Battleship Cove.
The upper, eastern portion of the river was originally a relatively narrow and shallow stream flowing through a flat, wide valley of glacial deposits overlaying a deep granite ridge. Portions of the granite are exposed at the surface near what is today Brayton Avenue and also near Quequechan Street.
The steep, western portion of the river between downtown and the waterfront originally consisted of a series of eight small waterfalls confined within a narrow, rocky bed. In the last half-mile (800 m) the total drop is about 132 feet (40 m). and the average flow is 122 cubic feet per second (3.5 m³/s).
Read more about this topic: Quequechan River
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