The Russell 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 sunny
Mostly sunny; warmer
Partly cloudy
Partly cloudy
Mostly cloudy
Chance of showers
Showers likely
Russell’s center stands about 880 ft above sea level. Within three miles the land runs from 590 ft to 1,010 ft, a difference of 420 ft: hilly country. The highest named summit within 15 miles is Mount Ashwabay, about 1,340 ft, 12 miles south-southwest.
Under the town center the state geologic map shows Bayfield Group; Chequamegon Sandstone (arkose), from the Mesoproterozoic, 1 to 1.6 billion years old.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 26×. 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. Age: Mesoproterozoic, 1 to 1.6 billion years old. About 12 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 Russell runs straight into Lake Superior. From there it moves on through the Great Lakes, over Niagara Falls and down the St. Lawrence to the Atlantic.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Russell; river miles along the main stem, rounded.
