The Stockton Springs 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.
Partly cloudy
Partly cloudy; warmer
Mostly sunny
Mostly sunny
Mostly sunny
Mostly sunny
Partly cloudy
68° on Nov. 11, 2020, the hottest reading for this week of the year since 1925. Next is 68° in 2022.
Stockton Springs’s center stands about 130 ft above sea level. Within three miles the land runs from 0 ft to 500 ft, a difference of 500 ft: hilly country. Open water lies within three miles. The highest named summit within 15 miles is Mount Waldo, about 1,050 ft, 7 miles north-northwest.
Under the town center the state geologic map shows Penobscot Formation (slate, schist, quartzite), from the Middle Ordovician to Late Ordovician, 450 to 470 million years old.
The section below crosses 5 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 34×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Granite. Age: Devonian, 359 to 422 million years old. About 6 mi of the line.
Sandstone, limestone. Age: Ordovician to Devonian, 359 to 487 million years old. About 5 mi of the line.
Slate, schist, quartzite. Age: Middle Ordovician to Late Ordovician, 450 to 470 million years old. About 3 mi of the line.
Metasedimentary, metavolcanic. Age: Neoproterozoic to Ordovician, 445 to 1,000 million years old. About 0.6 mi of the line.
Calc-silicate-rock. Age: Neoproterozoic to Ordovician, 445 to 1,000 million years old. About 0.4 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.
Rain that falls on Stockton Springs runs only a short way, about 3 miles, to the Atlantic Ocean.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Stockton Springs; river miles along the main stem, rounded.
Stockton Springs has a warm-summer humid continental climate. Summer afternoons average 80° in July; winter nights fall to about 9° in January. A normal year brings about 75 inches of snow; with the rain, that comes to about 42 inches of water.
On November 14 Stockton Springs normally reaches 46° and falls to 30°. The record high is 63°, in 2005; the record low 8°, in 2019. The most rain on this date, 1.56 in, fell in 2006.
Normals 1991–2020 and records since 1925 from the Bangor Area threaded record (Bangor International Airport, 21 miles north). NOAA, through RCC-ACIS.
