The Essex 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.
Essex’s center stands about 50 ft above sea level. Within three miles the land runs from 0 ft to 320 ft, a difference of 320 ft: rolling country. Open water lies within three miles. The highest named summit within 15 miles is Goose Hill, about 700 ft, 11 miles northwest.
Under the town center the state geologic map shows Rope Ferry Gneiss, from the Neoproterozoic, 617 to 623 million years old.
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.
Schist, gneiss. Age: Cambrian to Ordovician, 445 to 542 million years old. About 5 mi of the line.
Gneiss. Age: Neoproterozoic, 617 to 623 million years old. About 4 mi of the line.
Gneiss, schist. Age: Neoproterozoic, 542 to 1,000 million years old. About 3 mi of the line.
Schist, calc-silicate-rock. Age: Neoproterozoic, 542 to 1,000 million years old. About 2 mi of the line.
About 2 mi of the line.
Gneiss. Age: Neoproterozoic, 542 to 1,000 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. 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 Essex reaches Long Island Sound and the Atlantic Ocean by way of the Falls and the Connecticut: about 11 river miles.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Essex; river miles along the main stem, rounded.