The New Lisbon 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.
74° on Nov. 11, 1948, the hottest reading for this week of the year since 1893. Next is 73° in 1956.
New Lisbon’s center stands about 1,250 ft above sea level. Within three miles the land runs from 1,150 ft to 1,810 ft, a difference of 660 ft: hilly country. The highest named summit within 15 miles is Cornish Hill, about 2,230 ft, 15 miles east-northeast.
Under the town center the state geologic map shows Moscow Formation (sandstone, shale), from the Middle Devonian, 384 to 388 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 21×. 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, siltstone, sandstone. Age: Middle Devonian, 384 to 394 million years old. About 12 mi of the line.
Sandstone, shale. Age: Middle Devonian, 384 to 388 million years old. About 6 mi of the line.
Shale, siltstone, sandstone. Age: Middle Devonian, 384 to 394 million years old. About 3 mi of the line.
Shale. Age: Middle Devonian to Late Devonian, 359 to 394 million years old. About 3 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.
A raindrop that lands in New Lisbon reaches Chesapeake Bay and the Atlantic Ocean by way of Stony Creek, Butternut Creek, the Unadilla and the Susquehanna: about 440 river miles.
Lake on the way: Lake Aldred.
360 miles of the trip are on the Susquehanna.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of New Lisbon; river miles along the main stem, rounded.
New Lisbon has a warm-summer humid continental climate. Summer afternoons average 73° in July; winter nights fall to about 14° in January. A normal year brings about 86 inches of snow; with the rain, that comes to about 48 inches of water.
On November 14 New Lisbon normally reaches 40° and falls to 30°. The record high is 70°, in 1989; the record low 9°, in 1939. The most rain on this date, 0.95 in, fell in 1949.
Normals 1991–2020 and records since 1893 at Cooperstown, 16 miles northeast. NOAA, through RCC-ACIS.