In the last post, guest writer Robert Wilhelm began telling us the story of Hoopes Reservoir by first relating the tale of the Red Clay Creek reservoir that never was. In this post, he tells us of the background and construction of the reservoir that was created, and a bit of what once stood where the water now is.
-- Researched and written by Robert E. Wilhelm, Jr
An
alternate reservoir location involved Old Mill Stream, a tributary of the Red
Clay Creek in Christiana Hundred and the location of the present day Hoopes
Reservoir and Dam. A dam constructed across
the Old Mill Stream valley could contain water at a higher level (~ 225’ water
surface elevation above sea level) than a dam associated with the Red Clay
Creek Valley (~180’ water surface elevation above sea level if a reservoir was
to remain inside Delaware; 150-160 feet if not impacting Yorklyn). Holding
2-billion gallons of water, an Old Mill Stream reservoir offered greater water
depth at the dam with equivalent storage capacity and less surface area as
compared to a Red Clay water pool.
-- Researched and written by Robert E. Wilhelm, Jr
Hoopes Reservoir, 1933 |
There was little infrastructure
present in the Old Mill Stream valley which was not the case for the Red Clay
Creek Valley. Within most of the 480-acre footprint of the proposed ‘Old Mill Stream
Reservoir’ was the former mill property and farmland belonging to T. Coleman du
Pont including Dupont’s summer home. Once
an operating water-powered stone mill constructed in 1732, du Pont personally converted
the idle mill into a mansion. A smaller stone mill constructed in the 1850s on
the property was in ruins and would remain to succumb to the reservoir’s rising
waters, while du Pont’s home would be demolished leaving only the stone walls
behind.