The St. John 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
Partly cloudy
Mostly cloudy
Chance of showers; cooler
Mostly cloudy
Chance of showers
−20° on Nov. 11, 1986, the coldest reading for this week of the year since 1945. Next is −18° in 1959.
St. John’s center stands about 1,960 ft above sea level. Within three miles the land runs from 1,840 ft to 2,150 ft, a difference of 310 ft: rolling country.
Under the town center the state geologic map shows Fox Hills Formation (shale, sandstone), from the Late Cretaceous, 66 to 100 million years old.
The section below crosses 3 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 31×. 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: Late Cretaceous, 66 to 100 million years old. About 10 mi of the line.
Shale, sandstone. Age: Late Cretaceous, 66 to 100 million years old. About 7 mi of the line.
Sandstone, siltstone, claystone. Age: Late Cretaceous, 66 to 100 million years old. About 7 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.
St. John straddles the rim of a basin with no outlet. Rain on the south side runs to Devils Lake; most of the rest goes to Hudson Bay.
From the center of town, a raindrop reaches Hudson Bay by way of the Pembina, the Red River of the North and the Nelson: about 910 river miles. Past the border it runs north through Canada to Hudson Bay. One that lands on the south side reaches Devils Lake by way of Lake Alice and Lake Irvine: about 120 river miles. Devils Lake has no outlet to the sea: the water leaves only by evaporating or soaking into the ground.
Lake on the way: Lake Winnipeg.
400 miles of the trip are on the Nelson.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of St. John; river miles along the main stem, rounded.
St. John has a warm-summer humid continental climate. Summer afternoons average 79° in July; winter nights fall to about −5° in January. About 20 inches of rain fall in a normal year.
On November 14 St. John normally reaches 36° and falls to 16°. The record high is 63°, in 1953; the record low −18°, in 1959. The most rain on this date, 0.12 in, fell in 1960.
Normals 1991–2020 and records since 1945 at Belcourt Keya Radio, 7 miles south-southwest. NOAA, through RCC-ACIS.
