The Chinquapin 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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Chinquapin’s center stands about 30 ft above sea level. Within three miles the land runs from 30 ft to 100 ft, a difference of 70 ft: gently rolling country.
Under the town center the state geologic map shows Castle Hayne Formation; Comfort Member and New Hanover Member, undivided (limestone), from the Tertiary, 2.6 to 66 million years old.
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 64×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Limestone. Age: Tertiary, 2.6 to 66 million years old. About 14 mi of the line.
Sand, clay. Age: Cretaceous, 66 to 145 million years old. About 10 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 Chinquapin reaches the Atlantic Ocean by way of the Northeast Cape Fear and the Cape Fear: about 110 river miles.
85 miles of the trip are on the Northeast Cape Fear.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Chinquapin; river miles along the main stem, rounded.
