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Huzzah Creek (locally / ˈ h uː z ɑː /) is a 35.8-mile-long (57.6 km) [3] clear-flowing stream in the southern part of the U.S. state of Missouri. [4] According to the information in the Ramsay Place Names File at the University of Missouri, the creek's name "is evidently derived from" Huzzaus, one of the early French versions of the name of the Osage people.
Courtois Creek (locally / ˈ k oʊ t ə w eɪ /) is a 38.6-mile-long (62.1 km) [7] stream in southern Missouri, United States.It shares its name with the nearby town of Courtois and is in the Courtois Hills region of the Missouri Ozarks.
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 ...
Huzzah Creek is a stream in southern Madison County the U.S. state of Missouri. [1] It is a tributary of the St. Francis River. [2] The stream headwaters arise just south of Missouri Route N and one mile west of US Route 67 at an elevation of about 730 feet. The stream flows southwest then west for a distance of about two miles with the final ...
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Indian Creek is a stream in Crawford and Dent counties in the U.S. state of Missouri. [1] It is a tributary of Huzzah Creek . The stream headwaters arise in northern Dent County at 37°40′28″N 91°17′02″W / 37.67444°N 91.28389°W / 37.67444; -91.28389 at an elevation of 1300
NPS map of the Riverways Rocky Falls on Rocky Creek, a tributary of the Current River. The Ozark National Scenic Riverways is a recreational unit of the National Park Service in the Ozarks of southern Missouri in the U.S. The park was created by an Act of Congress in 1964 to protect the Current and Jacks Fork rivers, and it was formally ...
Meramec Caverns is the collective name for a 4.6-mile (7.4 km) cavern system in the Ozarks, near Stanton, Missouri. [1] The caverns were formed from the erosion of large limestone deposits over millions of years.