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Yosemite Valley rim

Sierra Nevada

A U-shaped valley so deep the rim is a cliff on the map: coincident contours and a spot height at Half Dome.

Yosemite Valley: a wide U-trough with steep granite walls.
A glacial trough in granite. Ice, not a young V-valley.NPS, public domain

Locator · OpenStreetMap / OpenFreeMap · 37.74°, -119.57°

USGS quads make the same spur/valley argument as an OS sheet. The interval is just in feet on older plates. Yosemite Valley is a glacial trough in granite. Hanging valleys dump waterfalls (Yosemite Falls, Bridalveil). El Capitan and Half Dome are the walls. Moraines sit down-valley. Cirques and arêtes sit in the high Sierra above.

The glaciers lab’s U-trough, hanging valley, and truncated spur are this place. The contours lab’s coincident lines are the cliffs. A full Moon over Half Dome is the moon-phases geometry — the same phase as Snowdonia that night, a different rise time because Earth is still rotating.

Ice here is mostly gone as glaciers; the landforms remain. Students should not say ‘Yosemite is a canyon like the Grand Canyon.’ One is ice, one is a river in a plateau. Cross-profile tells them apart.

How would a contour map distinguish Yosemite Valley from a V-shaped river gorge of similar depth?

Teacher hint: U: wide flat floor, steep walls, hanging valleys. V: evenly closing contours to a stream.

  • USGS / NPS Yosemite