The Englevale 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.
72° on Nov. 16, 2001, the hottest reading for this week of the year since 1903. Next is 70° in 1953.
Englevale’s center stands about 1,340 ft above sea level. Within three miles the land runs from 1,320 ft to 1,410 ft, a difference of 90 ft: gently rolling country.
Under the town center the state geologic map shows Niobrara Formation (shale), from the Late Cretaceous, 66 to 100 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 54×. 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 12 mi of the line.
Shale. Age: Late Cretaceous, 66 to 100 million years old. About 7 mi of the line.
Shale. Age: Late Cretaceous, 66 to 100 million years old. About 5 mi of the line.
Shale. Age: Late Cretaceous, 66 to 100 million years old. About 2 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.
Englevale has a warm-summer humid continental climate. Summer afternoons average 82° in July; winter nights fall to about 0° in January. A normal year brings about 47 inches of snow; with the rain, that comes to about 22 inches of water.
On November 14 Englevale normally reaches 39° and falls to 20°. The record high is 66°, in 2016; the record low −10°, in 1940. The most rain on this date, 0.77 in, fell in 1928.
Normals 1991–2020 and records since 1903 at Lisbon, 11 miles east-northeast, 190 ft lower. NOAA, through RCC-ACIS.