butte

butte

butte

French

The isolated flat-topped hills of the American West are called buttes — from French for a mound or hillock — and their dramatic vertical sides are the record of what erosion removed from the surrounding landscape over millions of years.

French butte (mound, small hill, target) came from Old French bout (end, terminal point), related to bouter (to push, to bump). English borrowed the word in the early 19th century for the characteristic isolated hills of the American West — free-standing flat-topped formations rising abruptly from surrounding plains. Monument Valley's mittens, Arizona's Courthouse Butte, Wyoming's Devil's Tower (technically a laccolith, not a butte) — the American West defined the word for English speakers.

A butte forms by differential erosion. A plateau or mesa is capped by a hard, resistant layer of rock (sandstone, basalt, or limestone). The surrounding softer rock erodes faster than the cap rock. Over millions of years, the landscape around the hard cap erodes downward and away, leaving the harder material standing isolated. The butte is not what was built up — it is what remained when everything else was removed.

The Navajo name for Monument Valley's formations is Tsé Biiʼ Ndzisgaii — 'valley within the rocks.' The Navajo Nation's reservation overlaps Monument Valley; the buttes are sacred landscape. John Ford used Monument Valley as the landscape for his Westerns from 1939 onward — Stagecoach, The Searchers, Fort Apache — making it the visual vocabulary of the American frontier film. The butte became a symbol of the West before most Americans had seen one.

Geologists measure a butte's age by the rock layers visible in its sides — a stratigraphic column visible in cross-section. The Redwall limestone visible in Grand Canyon buttes is 340 million years old. The buttes are geological textbooks: what the surrounding landscape used to look like, preserved in rock while everything around it was swept away.

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The butte is what didn't erode. Everything around it was soft enough to be carried away by water, wind, and time. The butte had a hard cap — sandstone, basalt, limestone — that protected what was beneath it. The surrounding landscape descended millions of years into its geological past; the butte kept the old surface level.

John Ford put his camera at the base of Monument Valley's buttes and made them into the visual signature of American mythology. The geological remnants — what survived when everything else was removed — became the symbol of the frontier. The butte is what endures when the softer things are gone.

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