“Stream gauge measurements are key to understanding the relationship between precipitation and stream flow (e.g., how quickly stream flow reaches its peak), which can vary significantly depending on the level of watershed development.”
“Streams are dynamic. In a healthy stream system, stream banks move as erosive forces shape and reshape the channel and floodplain. Stream bank and bed mobility is a natural phenomenon. A stream is considered “stable” when the water flow and sediments carried by the channel do not cause excessive changes to the width, depth, cross-sectional area, and slope of the stream.”
"Installed with one end extending out into the river, the structures catch the current to reduce its erosive force. This protects the bank and while providing healthier fish habitats. The newly built floodplain will be able to accommodate higher river flows, allowing floodwaters to slow down and deposit their beneficial sediments."
"Up, up, up it goes in zigzag fashion, following the foaming brook of crystal waters; through open glades, carpeted with beautiful wild flowers of every tint and hue; along the edge of the craggy precipice; up above the timber belt, 3000 feet higher than the city - finally reaching the summit of Point Lookout, and unfolding to your view a panorama worthy of the artist's pencil or the painter's brush."