The Owings 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.
82° on Nov. 15, 1993, the hottest reading for this week of the year since 1950. Next is 80° in 1973.
Owings Mills’s center stands about 500 ft above sea level. Within three miles the land runs from 410 ft to 720 ft, a difference of 310 ft: rolling country.
Under the town center the state geologic map shows Wissahickon Formation; Lower Pelitic Schist (biotite-schist), from the Proterozoic, 542 to 2,500 million years old.
The section below crosses 7 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 29×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Muscovite-schist. Age: Proterozoic, 542 to 2,500 million years old. About 7 mi of the line.
Biotite-schist. Age: Proterozoic, 542 to 2,500 million years old. About 6 mi of the line.
Gabbro. Age: Proterozoic to Paleozoic, 252 to 2,500 million years old. About 5 mi of the line.
Gneiss. Age: Precambrian. About 3 mi of the line.
Sand. Age: Cretaceous, 66 to 145 million years old. About 2 mi of the line.
Marble. Age: Proterozoic, 542 to 2,500 million years old. About 1 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale. 1 smaller unit along the line are not listed.
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 Owings Mills reaches Chesapeake Bay and the Atlantic Ocean by way of the Gwynns Falls and the Patapsco: about 35 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Owings Mills; river miles along the main stem, rounded.
Owings Mills has a humid subtropical climate. Summer afternoons average 90° in July; winter nights fall to about 30° in January. About 44 inches of rain fall in a normal year.
On November 14 Owings Mills normally reaches 58° and falls to 43°. The record high is 78°, in 1989; the record low 21°, in 1986. The most rain on this date, 2.46 in, fell in 1972.
Normals 1991–2020 and records since 1950 from the Baltimore Downtown Area threaded record (Maryland Science Center, 13 miles southeast, 480 ft lower). NOAA, through RCC-ACIS.