The Spring Hill 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.
Mostly sunny
Mostly sunny; warmer
Sunny
Sunny
Partly cloudy
Partly cloudy
Chance of showers
80° on Nov. 13, 1999, the hottest reading for this week of the year since 1945. Next is 78° in 1949.
Spring Hill’s center stands about 1,080 ft above sea level. Within three miles the land runs from 940 ft to 1,100 ft, a difference of 160 ft: gently rolling country.
Under the town center the state geologic map shows Lansing Group (shale, limestone), from the Carboniferous, 299 to 324 million years old.
The section below crosses 4 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, shale. Age: Carboniferous, 299 to 324 million years old. About 11 mi of the line.
Shale, limestone. Age: Carboniferous, 299 to 324 million years old. About 10 mi of the line.
Shale, sandstone. Age: Carboniferous, 299 to 324 million years old. About 3 mi of the line.
Sand, silt, clay. Age: Pleistocene to Holocene, less than 2.6 million years old. About 0.5 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 Spring Hill reaches the Gulf of America by way of Spring Creek, Little Bull Creek, Bull Creek, the Marais des Cygnes, the Osage, the Missouri and the Mississippi: about 1,700 river miles.
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 Spring Hill; river miles along the main stem, rounded.
Spring Hill has a hot-summer humid continental climate. Summer afternoons average 89° in July; winter nights fall to about 20° in January. About 38 inches of rain fall in a normal year.
On November 14 Spring Hill normally reaches 55° and falls to 34°. The record high is 78°, in 1964; the record low 9°, in 1959. The most rain on this date, 1.60 in, fell in 1968.
Normals 1991–2020 and records since 1945 at Olathe Johnson County Industrial Airport, 6 miles north-northwest. NOAA, through RCC-ACIS.
