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The Cleveland Museum of Natural History is a natural history museum in University Circle, a district of educational, cultural and medical institutions approximately five miles (8 km) east of Downtown Cleveland, Ohio, United States. The museum was established in 1920 by Cyrus S. Eaton to perform research, education and development of collections ...
Satellite image of Okavango Delta, with national borders added Typical region in the Okavango Delta, with free canals and lakes, swamps and islandsThe Okavango Delta [2] (or Okavango Grassland; formerly spelled "Okovango" or "Okovanggo") in Botswana is a vast inland delta formed where the Okavango River reaches a tectonic trough at an altitude of 930–1,000 metres (3,050–3,280 ft) [3] in ...
Children's Museum of Cleveland: Goodrich–Kirtland Park: Children's Cleveland Grays Armory Museum: Downtown Cleveland: Military History of the Cleveland Grays, a private military company which was founded in 1837, and the military heritage of Greater Cleveland Cleveland History Center: University Circle Multiple
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Wade Park is a park in the University Circle neighborhood of Cleveland, Ohio.Wade Park today largely serves as the campus for the Cleveland Museum of Art, the Cleveland Botanical Garden, and the Cleveland Museum of Natural History, as well as Wade Lagoon, which faces the Museum of Art from the south end of the park.
Cleveland Health Museum, AKA HealthSpace Cleveland, merged in 2007 with the Cleveland Museum of Natural History [279] Degenhart Paperweight and Glass Museum, Cambridge, closed in 2011, portion of the collection relocated to the Museum of American Glass located in Weston, WV [280] Ely Chapman Foundation West African Museum, Marietta [281]
The figure was discovered in a large storage jar during 1937-1938 excavations of the Columned Palace at Ptolemais in Cyrenaica, now part of eastern Libya, according to a statement shared with CNN ...
The Thamalakane River is a river located in Botswana, Africa, at the southern end of the Okavango Delta.It has no well defined beginning and no clear end ().It is the result of the Thamalakane fault - which began to form about two million years ago by the geological process of rifting that is currently splitting Africa apart along the East African Rift.