Strong, Mississippi | |
---|---|
Coordinates: 33°41′43″N88°36′16″W / 33.69528°N 88.60444°W | |
Country | United States |
State | Mississippi |
County | Monroe |
Elevation | 253 ft (77 m) |
Time zone | UTC-6 (Central (CST)) |
• Summer (DST) | UTC-5 (CDT) |
Area code | 662 |
GNIS feature ID | 678365 [1] |
Strong (also known as Strongs or Strongs Station) is an unincorporated community in Monroe County, Mississippi, United States. [1]
Strong is located southwest of Aberdeen.
Strong is located along the Kansas City Southern Railway. [2]
In 1900, Strong had a population of 63. [3]
A post office operated under the name Strongs from 1884 to 1914 and under the name Strong from 1944 to 1963. [4]
The Strong Field is a natural gas field located in Strong. [5]
Ouachita Parish is located in the northern part of the U.S. state of Louisiana. As of the 2020 census, the population was 160,368. The parish seat is Monroe. The parish was formed in 1807.
Jackson–Medgar Wiley Evers International Airport is a city-owned civil-military airport located in Jackson, Mississippi, United States, approximately 6 miles (9.7 km) east of Downtown Jackson across the Pearl River. It is located in Rankin County between the suburbs of Flowood and Pearl, whereas the majority of the city of Jackson is located in Hinds County.
Hamilton is a census-designated place and unincorporated community in Monroe County, Mississippi, United States. As of the 2020 census, it had a population of 404.
Athens is an unincorporated community in Monroe County, Mississippi.
Gibson is an unincorporated community in Monroe County, Mississippi. Gibson is located west of Aberdeen on Mississippi Highway 8.
Greenwood Springs is an unincorporated community in Monroe County, Mississippi. Greenwood Springs is located east of Amory on U.S. Route 278.
Prairie,, is an unincorporated community in Monroe County, Mississippi, United States.
Quincy is an unincorporated community in Monroe County, Mississippi, United States.
Bigbee is an unincorporated community in Monroe County, Mississippi. Bigbee is located northwest of Amory on Mississippi Highway 6 (close to its intersection with Mississippi Highway 371.
Splunge,, is an unincorporated community in Monroe County, Mississippi.
Wren,, is an unincorporated community in Monroe County, Mississippi.
Sipsey Fork is an unincorporated community in Monroe County, Mississippi, United States.
Binford is an unincorporated community in Monroe County, Mississippi. Binford is located southwest of Aberdeen.
Darracott is an unincorporated community in Monroe County, Mississippi. Darracott is located south of Aberdeen.
Parham is an unincorporated community in Monroe County, Mississippi. Parham is located northeast of Hatley and southeast of Smithville.
Wise Gap,, is an unincorporated community in Monroe County, Mississippi, United States.
Riggins is an unincorporated community in Monroe County, Mississippi, United States.
Muldon, also known as Aberdeen Junction, Loohattan, Loohatten and Louhatten, is an unincorporated community in Monroe County, Mississippi. Muldon is located southwest of Aberdeen on Mississippi Highway 25.
Central Grove is an unincorporated community in Monroe County, Mississippi. Central Grove is located west of Amory and south of Nettleton.
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.