The Bazile Mills 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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Bazile Mills’s center stands about 1,600 ft above sea level. Within three miles the land runs from 1,510 ft to 1,720 ft, a difference of 210 ft: rolling country. The highest named summit within 15 miles is Council Hill, about 1,850 ft, 7 miles south-southwest.
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 42×. 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-mudstone, conglomerate-sandstone. Age: Miocene, 5.3 to 23 million years old. About 14 mi of the line.
Shale. Age: Late Cretaceous, 66 to 100 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 Bazile Mills reaches the Gulf of America by way of Bazile Creek, the Missouri and the Mississippi: about 2,020 river miles.
Lake on the way: Lewis and Clark Lake.
1,170 miles of the trip are on the Mississippi.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Bazile Mills; river miles along the main stem, rounded.
