The Crater of Diamonds is an Arkansas State Park located in Murfreesboro in Pike County, Arkansas containing the only diamond mine open to the public in the world.
In addition to diamonds, visitors may find semi-precious gems such as amethyst, agate, and jasper or approximately 40 other minerals such as garnet, phlogopite, quartz, barite, and calcite.
The crater itself is a 35 acre (142,000 m2) gravelly open field that is periodically plowed to bring the diamonds and other gemstones to the surface. The remainder of the park consists of a visitor's center, interpretive center, campground, and picnic area. A 1.3 mile (2 km) walking trail along the Little Missouri River is available for hikers.
Murfreesboro is located just south of Hot Springs, Arkansas, the location of Hot Springs National Park. The park is open year round but experienced diamond hunters prefer hunting in the spring when rains wash dirt off of the gemstones and make them easier to spot.
Soon after the original diamond was found, a "diamond rush" turned Murfreesboro into a boomtown for a time. Hotels in Murfreesboro are said to have turned away 10,000 people in the space of a year. These refugees formed a tent city near the mine which was named "Kimberly" in hopeful honor of the famous Kimberley Diamond Mine in South Africa.
From 1952 to 1972 the crater was a privately owned tourist attraction. From 1964 to 1968 Roscoe Johnston leased 49 acres of diamond bearing land adjacent to the crater and operated it as a tourist attraction under the name: "Arkansas Diamond Mine". It was during this time that the "Star of Murfreesboro" and the "Phillips 66" diamonds were found.
In 1972 the State of Arkansas purchased the crater and converted it into the unique state park it is today.
Due in part to the uniqueness of the park (and since Arkansas is the first state where diamonds were found "in situ"), the diamond has come to be associated with the State of Arkansas. The diamond shape on the flag of Arkansas represents this association. The Arkansas State Quarter released in 2003 bears a diamond on its face, and the former seal of Arkansas State University incorporated a multi-faceted diamond.
In ancient times all of Arkansas was under water except for the Ouachita Mountains, which were created by the continental plate riding up over the oceanic plate. About 100 million years ago, these plates began to stabilize. The last movements of the plates caused cracking in the earth's crust, which allowed molten material to rise to the surface. The deep seated lamproite magma brought diamonds to the surface from their upper mantle origin.
Arkansas | Arkansas state parks | Mines in the United States | Diamond mines | Pike County, Arkansas
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