Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)
Paper No. 18-1
Presentation Time: 1:00 PM-1:20 PM

KENTUCKY’S LANDSCAPE AND THE CIVIL WAR CAMPAIGNS FOR KENTUCKY, 1861-1862

ANDREWS, William, Kentucky Geological Survey, Univ of Kentucky, 228 Mining and Mineral Resources Building, Lexington, KY 40506-0107, wandrews@uky.edu.

Kentucky was a key border state during the American Civil War (1861-1865). Kentucky’s location along major transportation routes, its agricultural system, and growing manufacturing strength solidified economic ties with both northern and southern states. As such, Kentucky declared itself neutral at the outbreak of war between the two sides. Kentucky’s landscape played a key role in determining the location of strategic transportation routes, as well as the course of campaigns fought along them. The geology of Kentucky is dominated by gently dipping Paleozoic sedimentary strata. Resistant beds have developed gently rolling landscapes and bold cuestas, whereas shaly stratigraphic units have developed more rugged, dissected terrain.

Once the state’s neutrality ended, both sides occupied the state. The Confederates formed a defensive line across southern Kentucky, while Union forces occupied central Kentucky and cities along the Ohio River. Skirmishes occurred along the Knobstone Escarpment as the armies probed enemy positions. In early 1862, key roads, rivers, and escarpments guided the Union advance as its forces outflanked and unhinged the Confederate line, forcing the rebels to withdraw from Kentucky. Notable were the fights at Mill Springs, where the Confederates had their backs to a flooded river, and Fort Donelson, where the Tennessee and Cumberland Rivers provided transportation for Union troops, and a route for Union gunboats to enter the battle.

Federal forces used the mountainous terrain to their advantage when outflanking and capturing the Cumberland Gap in 1862, and likewise used the rugged terrain of eastern Kentucky to shield their subsequent retreat in October 1862. The late 1862 invasion of Kentucky by Confederates and subsequent Perryville Campaign were again guided by topography, transportation routes, and also water supply issues, as the state was in a deep drought at the time. The Perryville Campaign ended Confederate hopes of occupying Kentucky.

Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)
General Information for this Meeting
Session No. 18
Geology and the Civil War II
Hilton McLean Tysons Corner: Ballroom C
1:00 PM-5:00 PM, Thursday, March 25, 2004

Geological Society of America Abstracts with Programs, Vol. 36, No. 2, p. 76

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