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Watkins Mill was built in 1859-1860. Watkins built housing for the mill workers nearby, creating one of the first planned communities in North America. The community was effectively self-sufficient, the mill producing yarn and wool cloth. The mill operated at capacity until 1886, two years after Watkins' death.
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The Dillard Mill State Historic Site is a privately owned, state-administered property on Huzzah Creek in Crawford County, Missouri, that preserves a water-powered gristmill. [6] The 132-acre (53 ha) site has been operated as a state historic site by the Missouri Department of Natural Resources under a lease agreement with the L-A-D Foundation ...
The mill was built in 1883, and is a 2 1/2-story, heavy timber frame building sided with vertical boards. Adjacent to the building are paired cylindrical grain storage silos of creek gravel concrete construction. The mill continued to operate until 1969. [2]: 2–4 It was listed on the National Register of Historic Places in 1986. [1]
Walter Klepzig Mill and Farm is a historic farm and sawmill and national historic district located in the Ozark National Scenic Riverways near Eminence, Shannon County, Missouri. The district encompasses three contributing buildings, three contributing sites, and one contributing structure associated with an early-20th century Ozark farm and mill.
With a population of 2,115, this means that Byrnes Mill had 1.8 cases per each person living in the city and collected $205.77 per person in fines. This is the highest amount per person of any municipality in Jefferson County and more than double the amount per person of the next highest municipality, Hillsboro .
Yarrow began in 1847 as Domey's Mill, a grist mill built on the east bank of the Chariton River to serve farmers in southern Adair County, Missouri. This original mill was destroyed by winter ice floes in 1874. However, the demand for services was so great a new mill was up and running on the same location by 1876.
The mill is located where the Zanoni Spring arises from openings in the Roubidoux Formation, an Ordovician unit of mixed sandstone and dolomite. [5] The spring discharges at the base of a ridge above Pine Creek, a tributary of Caney Creek which discharges into Bryant Creek just above its intersection with North Fork River and Norfork Lake . [ 1 ]
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