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monadnock

geology
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History

monadnock, isolated hill of bedrock standing conspicuously above the general level of the surrounding area. Monadnocks are left as erosional remnants because of their more resistant rock composition; commonly they consist of quartzite or less jointed massive volcanic rocks. In contrast to inselbergs (island mountains), a similar tropical landform, monadnocks are formed in humid, temperate regions. They take their name from Mt. Monadnock, a solitary mass of rock (3,165 feet [965 metres]) in Monadnock State Park, southeast of Keene, in Cheshire County, southwestern New Hampshire, U.S. A well-known example is Stone Mountain in Georgia, U.S.

This article was most recently revised and updated by John P. Rafferty.