Gallery > Features

Particular features at some watersheds account for anticipations about baseflows and observations about water temperatures.

For example, a wood and rock dam about 1.3 mi upstream at Barlow creates a flooded plain that likely assists in the maintenance downstream baseflow.

A beaver dam approximately 2 mi upstream at Scotch likely figures in recharge of its downstream baseflow.

Shading reasonably accounts for the lower and less variable stream temperatures at Priest as compared with temperatures at equivalently high elevations at Slate and Coal.