The Old Saybrook Center 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.
Old Saybrook Center’s center stands about 30 ft above sea level. Within three miles the land runs from 0 ft to 200 ft, a difference of 200 ft: gently rolling country. Open water lies within three miles. The highest named summit within 15 miles is Tater Hill, about 650 ft, 12 miles north.
Under the town center the state geologic map shows Unknown - Unmapped.
The section below crosses 8 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 32×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
About 4 mi of the line.
Gneiss. Age: Neoproterozoic, 617 to 623 million years old. About 4 mi of the line.
Gneiss. Age: Neoproterozoic, 542 to 1,000 million years old. About 2 mi of the line.
Clay, sand, gravel. Age: Late Cretaceous, 66 to 100 million years old. About 1 mi of the line.
Gneiss, schist. Age: Neoproterozoic, 542 to 1,000 million years old. About 1 mi of the line.
Schist, calc-silicate-rock. Age: Neoproterozoic, 542 to 1,000 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. 2 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 Old Saybrook Center reaches Long Island Sound and the Atlantic Ocean by way of the Connecticut: about 1 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Old Saybrook Center; river miles along the main stem, rounded.