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SubTropolis is a business complex located inside of a 55,000,000-square-foot (5,100,000 m 2), 1,260-acre (5.1 km 2) mine in the bluffs north of the Missouri River in Kansas City, Missouri, United States.
Jewell Hall is a historic building located on the campus of William Jewell College at Liberty, Clay County, Missouri. It was built between 1850 and 1853, and is a three-story, modified "H"-plan, Classical Revival style brick and Missouri limestone building. The building measures 120 feet in length and 66 feet in width.
Champion Stone Company, Lueder's Limestone quarry mining from the Lueders Basin outside Abilene, Texas with more than 100 years of Limestone reserves, 14 harvestable layers of limestone and over 12 color options. Tubb Quarry, a shotrock limestone quarry located on the Big Spring Mesa approximately 10 miles south of Big Spring, Texas.
Limestone buildings by country (4 C) C. Limestone churches (3 C, 3 P) H. Hamstone buildings (24 P) Pages in category "Limestone buildings" The following 20 pages are ...
A limestone outcropping on Big Creek west of town gives its name to the Bethany Falls Limestone formation. The falls no longer exist and only a small amount of stone remains exposed. However the formation extends through Kansas City, Missouri and limestone is used extensively in buildings in that city and the formation is the basis for ...
Missouri: The WPA Guide to the 'Show Me' State. St. Louis: Missouri Historical Society Press, 1998. Official Manual of the State of Missouri. St. Louis: Office of the Secretary of State, 1963. Swallow, G.C. First Report of Progress of the Geological Survey of Missouri. Jefferson City, Mo.: James Lusk, Printers, 1855.
Two roughly square lots are shown on map with a light grey background. Buildings are colored brown; plantings, green; water features, blue; and walking paths, off-white.|In this map of Citygarden, the arcing golden limestone wall divides the park's northern zone, while the dark meander wall snakes through the southern zone.
Burlington Limestone is present in nearly all major Mississippian outcrop regions in Missouri. It is known from Iowa to northwestern Arkansas and from western Illinois to western Kansas . It is present throughout Missouri, except in the Ozark uplift, where it has been removed by erosion .