The Leisure Knoll 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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Leisure Knoll’s center stands about 80 ft above sea level. Within three miles the land runs from 50 ft to 140 ft, a difference of 90 ft: gently rolling country.
Under the town center the state geologic map shows Cohansey Formation (sand), from the Middle Miocene, 12 to 14 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.
Sand. Age: Middle Miocene, 12 to 14 million years old. About 12 mi of the line.
Clay, sand. Age: Early Miocene, 16 to 23 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 Leisure Knoll reaches the Atlantic Ocean by way of Union Branch and the Toms: about 14 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Leisure Knoll; river miles along the main stem, rounded.
