I own a property with a dug well that has high sulfur content. Just off the corner of this property I have deeded rights to a spring. I have not done
enough exploring to really pinpoint this spring but I know that whole area is fairly soggy through the summer. In the spring there is a ditch just below it that flows like a small waterfall down to the brook. In the summer this ditch is dry but the area by the spring never dries up I am unsure if there is a defined point or if its more of a seepage spring. In the springtime I plan to investigate more. I would like to tap it and measure flow rate through the year to see if it is worth pursuing farther, also get the
water tested for contaminates. By the wording of the deed I believe this spring was likely developed at some point in history (probably late 1800s, no signs of this remain that I have found though) I have been looking into general best practices of how to "develop a spring" This happens to be uphil from anything I would want to
feed with it which is advantageous. My main question right now is the overflow pipe. I cant seem to find an
answer. I have attached a picture of a basic spring plan. I have looked at many pictures but they all are basically this same design. The overflow pipe always just appears to be a pipe from the top of the tank leading to daylight out the hillside. This makes sense except what keeps it from freezing in winter? even if flow was enough to keep the outlet itself from freezing it would be making an ice sheet on the ground in front of it. Eventually I imagine an icicle tower would built up to the height of the outlet at which point flow may be impeded enough to allow freezing. Even if the pipe itself never freezes it sure seems like the ground below and downhill from it would sure be a mess all winter.... Can someone clue me into how this works in cold climates?