The Tygh Valley 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.
Tygh Valley’s center stands about 1,190 ft above sea level. Within three miles the land runs from 1,040 ft to 2,660 ft, a difference of 1,620 ft: steep hill country. The highest named summit within 15 miles is Gordon Butte, about 4,820 ft, 14 miles west-northwest.
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 7×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Basalt. Age: Middle Miocene, 12 to 16 million years old. About 7 mi of the line.
Hypabyssal-rhyolite, hypabyssal-dacite. Age: Miocene, 5.3 to 23 million years old. About 6 mi of the line.
Sandstone, siltstone, mudstone. Age: Miocene to Pliocene, 2.6 to 23 million years old. About 4 mi of the line.
Basalt. Age: Early Miocene to Middle Miocene, 12 to 23 million years old. About 3 mi of the line.
Basalt. Age: Miocene to Pliocene, 2.6 to 23 million years old. About 3 mi of the line.
Clay, silt, sand. Age: Pleistocene, less than 2.6 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 Tygh Valley reaches the Pacific Ocean by way of Tygh Creek, the White River, the Deschutes and the Columbia: about 250 river miles.
200 miles of the trip are on the Columbia.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Tygh Valley; river miles along the main stem, rounded.