e/Weaubleau-Osceola structure

Information
has gloss	eng: The Weaubleau-Osceola structure is thought to be a meteorite impact site in western Missouri near the towns of Osceola and Weaubleau. It is believed to have been caused by a 1200-ft (366 m) meteoroid between 310 and 340 million years ago during the late Mississippian period. It is listed by the Impact Field Studies Group as a "probable" impact structure.
lexicalization	eng: Weaubleau-Osceola structure
instance of	(noun) a bowl-shaped depression formed by the impact of a meteorite or bomb crater

Media
geo loc	geographic location 37.983333333333334 -93.63333333333334
media:img	Missouri round rock.jpg
media:img	Weaubleau Structure outline v2.svg
media:img	Weaubleau Structure shaded relief.jpg