By: Rhys Hals
Erosion of streambeds is a major threat to the health of our ecosystems. Some erosion over time is natural, but too much too quickly results in soil getting washed away and deposited elsewhere, greatly altering the state of the stream, the biodiversity in it, and the overall aquatic habitat. During intense rain events, water washes over impervious surfaces such as parking lots and driveways and picks up speed as it heads toward a stream. As it makes its way across the land, this water cuts down and through the soil. When the water reaches the stream and has a lot of velocity from heavy rain, it can widen the streambed, or cause erosion near the headwaters of the water body. A deep crevice caused by this kind of erosion near the headwaters of a stream is called a headcut.
Headwaters are the source or origin of a stream or creek, the furthest point from where the steam empties. Headwaters are vital in ecological health1. Yet, despite the importance of these waters, they are disproportionately unmonitored. As runoff from highly developed or agricultural areas empties into headwaters, the stability of the stream is thrown off. The water can become overrun with chemicals and synthetic fertilizers, decreasing water quality and sometimes resulting in algal blooms. Changes in headwaters can go undetected but result in big downstream ecological issues.