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Mississippi Coliseum

1962 establishments in MississippiBasketball venues in MississippiBuildings and structures in Jackson, MississippiIndoor ice hockey venues in the United StatesSports in Jackson, Mississippi
Sports venues completed in 1962Tourist attractions in Jackson, Mississippi
Mississippi State Fairgrounds December 2018 1 (Mississippi Coliseum)
Mississippi State Fairgrounds December 2018 1 (Mississippi Coliseum)

The Mississippi Coliseum is a 6,500-seat multi-purpose arena in Jackson, Mississippi, built in 1962 and located on the Mississippi State Fairgrounds complex. The arena has 6,812 seats available for basketball, and can be expanded to 10,000 for concerts. It sits 2900 feet (884 meters) atop the extinct Jackson Volcano. In addition to the Coliseum, the Mississippi State Fairgrounds includes: The Mississippi Trade Mart, the A & I agricultural complex and the Kirk Fordice Equine Center. It was home to the Jackson Bandits minor league ice hockey team from 1999 to 2003. The Fairgrounds hosts the Mississippi State Fair each October. Each February, the Mississippi Coliseum and surrounding complex host The Dixie National Rodeo, which is the largest rodeo east of the Mississippi RiverStarting in the 2018–19 basketball season, Mississippi State Bulldogs men's basketball and Ole Miss Rebels men's basketball have played one game at the arena each season.

Excerpt from the Wikipedia article Mississippi Coliseum (License: CC BY-SA 3.0, Authors, Images).

Mississippi Coliseum
Mississippi Street, Jackson

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Wikipedia: Mississippi ColiseumContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 32.300126 ° E -90.172121 °
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Mississippi Coliseum

Mississippi Street
39202 Jackson
Mississippi, United States
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Mississippi State Fairgrounds December 2018 1 (Mississippi Coliseum)
Mississippi State Fairgrounds December 2018 1 (Mississippi Coliseum)
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Jackson Volcano
Jackson Volcano

Jackson Volcano is an extinct volcano 2,900 feet (880 m) beneath the city of Jackson, Mississippi, under the Mississippi Coliseum. The uplifted terrain around the volcano forms the Jackson Dome, an area of dense rock clearly noticeable in local gravity measurements. E.W. Hilgard published his theory of an anticline beneath Jackson in 1860 due to his observations of surface strata. The dome contains relatively pure carbon dioxide which is used in oil production in Gulf Coast oil fields. The noble gas data suggests mantle origins with a date of 70 million years for the Jackson Dome intrusion. Geologists have evidence of repeated uplifts accompanied by dike intrusions and volcanic extrusions, erosion, and sedimentation with one coral reef having developed during a submergence. Much of the oil at the crest of the dome volatilized during a late uplift, but oil production wells numbered over a hundred in 1934. Jackson Volcano is believed to have been extinct for at least 66 million years. A hypothesis states that the Jackson Volcano and related igneous activity in Mississippi were a result of the North America Plate's passage over the Bermuda hotspot 66 million years ago. Alternatively, the volcanism may have been part of a worldwide eruption driven by superplumes, similar to the conditions that created the Deccan Traps and the Siberian Traps.The volcano is one of four inside cities in the United States, Diamond Head in Honolulu, Hawaii, Pilot Butte in Bend, Oregon, and Mount Tabor in Portland, Oregon being the others. The volcano was discovered in 1819.