The Gibsonia 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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74° on Nov. 11, 2020, the hottest reading for this week of the year since 1905. Next is 70° in 2021.
Gibsonia’s center stands about 1,080 ft above sea level. Within three miles the land runs from 970 ft to 1,340 ft, a difference of 370 ft: rolling country. The highest named summit within 15 miles is Big Knob, about 1,400 ft, 14 miles west-northwest.
The section below crosses 2 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.
Shale. Age: Carboniferous, 299 to 324 million years old. About 15 mi of the line.
Shale, clastic. Age: Carboniferous, 299 to 324 million years old. About 9 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 Gibsonia reaches the Gulf of America by way of Willow Run, Pine Creek, the Allegheny, the Ohio and the Mississippi: about 1,970 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 Gibsonia; river miles along the main stem, rounded.
Gibsonia has a hot-summer humid continental climate. Summer afternoons average 83° in July; winter nights fall to about 19° in January. About 44 inches of rain fall in a normal year.
Normals 1991–2020 and records since 1905 at Acmetonia Lock 3, 10 miles southeast, 330 ft lower. NOAA, through RCC-ACIS.
