The Wayne plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
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Wayne’s center stands about 1,730 ft above sea level. Within three miles the land runs from 1,370 ft to 1,870 ft, a difference of 500 ft: hilly country. The highest named summit within 15 miles is Jackson Hill, about 1,980 ft, 12 miles southeast.
Under the town center the state geologic map shows Corry Sandstone through Riceville Formation, undivided (sandstone, shale), from the Late Devonian, 359 to 384 million years old.
The section below crosses 3 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 27×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Siltstone, conglomerate. Age: Late Devonian, 359 to 384 million years old. About 14 mi of the line.
Sandstone, shale. Age: Late Devonian, 359 to 384 million years old. About 8 mi of the line.
Siltstone, shale. Age: Late Devonian, 359 to 384 million years old. About 2 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR; rock from the USGS State Geologic Map Compilation.
A raindrop that lands in Wayne reaches the Gulf of America by way of Spencer Creek, South Branch French Creek, French Creek, the Allegheny, the Ohio and the Mississippi: about 2,160 river miles.
970 miles of the trip are on the Ohio.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Wayne; river miles along the main stem, rounded.
