The Lowman 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.
Lowman’s center stands about 3,780 ft above sea level. Within three miles the land runs from 3,760 ft to 6,160 ft, a difference of 2,400 ft: mountain country. The highest named summit within 15 miles is Wolf Mountain, about 8,760 ft, 13 miles east-southeast.
Under the town center the state geologic map shows Granodiorite and two-mica granite (granodiorite, granite), from the Early Cretaceous to Late Cretaceous, 67 to 107 million years old.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 4×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Granodiorite, granite. Age: Early Cretaceous to Late Cretaceous, 67 to 107 million years old. About 24 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 Lowman reaches the Pacific Ocean by way of the South Fork Payette, the Payette, the Snake and the Columbia: about 790 river miles.
Lakes on the way: Lake Umatilla, Brownlee Reservoir and Hells Canyon Reservoir.
240 miles of the trip are on the Snake.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Lowman; river miles along the main stem, rounded.