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Crater of Diamonds State Park

Crater of Diamonds State Park is a 911-acre (369 ha) Arkansas state park in Pike County, Arkansas, in the United States. The park has a 37.5-acre (15.2-hectare) plowed field which is one of the few diamond-bearing sites accessible to the public. Diamonds have been discovered in the field continuously since 1906, including the graded-perfect Strawn-Wagner Diamond, found in 1990, and the Uncle Sam, found in 1924, which at over 40 carats is the largest diamond ever found in the United States.

History
, advertising diamonds mining in the early 1900s In 1889, Arkansas state geologist John Branner investigated the site of an 1842 report noting an igneous intrusion amidst sedimentary rock near Murfreesboro. He determined it was kimberlite, but without any associated diamonds. In early 1906, John Wesley Huddleston purchased the area looking for gold. Instead, in August he found two diamonds, 3- and 4.5-carats identified by George Frederick Kunz. Visiting the site with Henry Stephens Washington, Kunz noted of the 140 diamonds collected from the surface, "They are absolutely perfect and are equal to the finest stones [of Africa] or that were ever found in India...Economical extraction [should be entirely] successful." The Arkansas Diamond Company was formed, headed by the Little Rock banker Samuel Reyburn, and Huddleston sold out for $36,000. Kunz and Washington prepared a mining plan for the 73 acre orebody, and initially 1400 diamonds were found in the regolith. Soon ten thousand prospectors started to search the outlying area for diamonds, and for fifty cents a day they could keep any diamonds found on the neighboring Mauney property. The Mauneys also sold lots for the town of Kimberly, which soon contained stores, restaurants, and a hotel. In 1908, the Arkansas Diamond Company hired John Fuller, a former De Beers engineer. Yet money was wasted, and the thousands of diamonds mined were mainly less than half a carat, and the few large ones were industrial grade. In 1912, the mine closed after running out of financial capital. Only a watchman and assistants continued looking for diamonds. In 1912, Austin Q. Millar and his son Howard Millar rented and bought surrounding Murfreesboro properties, including the Mauney place, and established an ore processing system. For the next seven years, they mined thousands of modest stones. On 13 January 1919, the operation ended after arson burned the entire place. ==Geology==
Geology
The Early Cretaceous Prairie Creek Diatreme outcrops include magmatic lamproite, pyroclastic lamproite where diamonds are recovered, and maar epiclastics. According to Howard and Hanson, "Lamproites form from partially melted mantle at depths exceeding 93 miles. The rising material is forced to the surface in volcanic pipes, bringing with it xenoliths and xenocryst diamonds from the harzburgitic peridotite or eclogite mantle regions where diamond formation is stabilized. In the instance of the Arkansas lamproites, the diamonds are of eclogite host origin." In 2002, research by geologist Dennis Dunn (Ph.D. dissertation 2002) found that the diamondiferous epiclastic rocks range from olivine lamproite to phlogopite and olivine-rich tuffs. The chemistry of the mantle xenolith created maximum pressures of around 5 GPa and temperatures of 1000 °C for the upper mantle origin of the lamproitic magma. ==Recreation==
Recreation
Crater of Diamonds State Park is known for its plowed field on which visitors can hunt for diamonds and other semi-precious gems. On average, two diamonds are found per day by park visitors. Diamond mine Crater of Diamonds State Park is situated over an eroded lamproite volcanic pipe. The park is open to the public and, for a small fee, rockhounds and visitors can dig for diamonds and other gemstones. Park visitors find more than 600 diamonds each year of all colors and grades. As of 2015, over 75,000 diamonds had been found in the crater. Visitors may keep any gemstone they find regardless of value. 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, baryte, and calcite. ==Diamonds found==
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