Leon County () is a county in the Panhandle of the U.S. state of Florida. It was named after the Spanish explorer Juan Ponce de León. As of the 2020 census, the population was 292,198. The county seat is Tallahassee, which is also the state capital and home to many politicians, lobbyists, jurists, and attorneys. Leon County is included in the Tallahassee metropolitan area. Tallahassee is home to two of Florida's major public universities, Florida State University and Florida A&M University, as well as Tallahassee Community College. Together these institutions have a combined enrollment of more than 70,000 students annually, creating both economic and social effects. History Originally part of Escambia and later Gadsden County, Leon County was created in 1824. It was named after Juan Ponce de León, the Spanish explorer who was the first European to reach Florida. The United States finally acquired this territory in the 19th century. In the 1830s, it attempted to conduct Indian Removal of the Seminole and Creek peoples, who had migrated south to escape European-American encroachment in Georgia and Alabama. After many Seminole were forcibly removed from the area or moved south to the Everglades during the Seminole Wars, planters developed cotton plantations based on enslaved labor. By the 1850s and 1860s, Leon County had become part of the Deep South's "cotton kingdom". It ranked fifth of all Florida and Georgia counties in cotton production from the 20 major plantations. Uniquely among Confederate capitals east of the Mississippi River, in the American Civil War Tallahassee was never captured by Union forces. No Union soldiers set foot in Leon County until the Reconstruction Era. Geography According to the U.S. Census Bureau, the county has an area of , of which are land and (5.0%) are water. Unlike much of Florida, most of Leon County has rolling hills, as part of Florida's Red Hills Region. The highest point is , in the northern part of the county. Geology Leon County encompasses basement rock composed of basalts of the Triassic and Jurassic from ~251 to 145 million years ago interlayered with Mesozoic sedimentary rocks. The layers above the basement are carbonate rock created from dying foraminifera, bryozoa, mollusks, and corals from as early as the Paleocene, a period of ~66—55.8 Ma. During the Eocene (~55.8—33.9 Ma) and Oligocene (~33.9—23 Ma), the Appalachian Mountains began to uplift and the erosion rate increased enough to fill the