Topographic Information
For the United States Geological Survey (USGS), the dam is sourced in the Windsor Windsor quad. The topographic map shows the mountainous terrain of the area. In fact, Windsor County, Vermont is home to a total of 202 mountain summits and peaks. The highest is Gillespie Peak which is at an elevation of 3,343 feet (1,018.95 m) above sea level. The peak flow in the rivers near uneven terrain could fluctuate vastly between periods of high and low precipitation because much of the rainfall flowing down to a discharge rather than infiltrating into the ground first as it would in flat terrain. This flow could cause a large increase in flow rate and river height in a fairly small amount of time. The fact that the Connecticut River was just a few miles away also played a role in this. Because of all this, the timing of opening and closing the dam to regulate flow and produce hydroelectric power was important.
Read more about this topic: Ascutney Mill Dam
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