The Tolland 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 cloudy
Mostly sunny; warmer
Partly cloudy
Mostly sunny
Mostly sunny
Mostly sunny
Mostly sunny
74° on Nov. 16, 1993, the hottest reading for this week of the year since 1888. Next is 73° in 2020.
Tolland’s center stands about 670 ft above sea level. Within three miles the land runs from 500 ft to 990 ft, a difference of 490 ft: hilly country. The highest named summit within 15 miles is Burley Hill, about 1,320 ft, 13 miles northeast.
Under the town center the state geologic map shows Monson Gneiss (gneiss, amphibolite), from the Early Ordovician to Middle Ordovician, 459 to 487 million years old.
The section below crosses 12 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 20×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Arkose, siltstone. Age: Early Jurassic, 175 to 202 million years old. About 7 mi of the line.
Schist, gneiss. Age: Cambrian to Ordovician, 445 to 542 million years old. About 3 mi of the line.
Granofels, schist. Age: Cambrian to Ordovician, 445 to 542 million years old. About 2 mi of the line.
Gneiss, amphibolite. Age: Early Ordovician to Middle Ordovician, 459 to 487 million years old. About 2 mi of the line.
Granofels, schist. Age: Neoproterozoic, 542 to 1,000 million years old. About 2 mi of the line.
Granofels, schist. Age: Ordovician to Silurian, 422 to 487 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. 6 smaller units 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 Tolland reaches Long Island Sound and the Atlantic Ocean by way of Clough Brook, the Skungamaug, the Hop, the Willimantic, the Shetucket and the Thames: about 65 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Tolland; river miles along the main stem, rounded.
Tolland has a hot-summer humid continental climate. Summer afternoons average 81° in July; winter nights fall to about 19° in January. A normal year brings about 39 inches of snow; with the rain, that comes to about 49 inches of water.
On November 14 Tolland normally reaches 51° and falls to 34°. The record high is 67°, in 1902; the record low 10°, in 1905. The most rain on this date, 2.21 in, fell in 1937.
Normals 1991–2020 and records since 1888 at Storrs, 9 miles southeast. NOAA, through RCC-ACIS.
