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Hoodoo (geology)

tall, thin spire of rock that protrudes from the bottom of an arid drainage basin or badland

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionSep 5, 2026
Entity authorityQ854550
Source-derived summary

A hoodoo (also called a tent rock, fairy chimney, or earth pyramid) is a tall, thin spire of rock formed by erosion. Hoodoos typically consist of relatively soft rock topped by harder, less easily eroded stone that protects each column from the elements. They generally form within sedimentary rock and volcanic rock formations.

Hoodoos range in size from the height of an average human to heights exceeding a 10-story building. Hoodoo shapes are affected by the erosional patterns of alternating hard and softer rock layers. Minerals deposited within different rock types can cause hoodoos to have different colors throughout their height.

Etymology

In certain regions of western North America these rocky structures are called hoodoos, a name that comes from a Southern Paiute word, oo’doo, which implies something that inspires fear. Hoodoos are featured in some traditional legends of Indigenous peoples of the North American Southwest. For example, hoodoos in Bryce Canyon National Park were considered petrified remains of ancient beings who had been sanctioned for misbehavior. Despite the matching spelling, the term for these rock formations is not related to Hoodoo spirituality.

Editorial summary

The public source identifies “Hoodoo (geology)” as tall, thin spire of rock that protrudes from the bottom of an arid drainage basin or badland. This brief keeps that definition visible, then builds a research path around Hoodoo, geology and tall.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current 183-word lead offers orientation but no explicit four-digit date, so chronology should not be assumed. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Hoodoo, geology and tall providing the first useful test.
Editorial analysis

Why this record matters

A short description can identify a subject without explaining its stakes. For “Hoodoo (geology)”, the useful work is to connect “tall, thin spire of rock that protrudes from the bottom of an arid drainage basin or badland” to the records capable of establishing context and consequence.

Evidence profile

Named sources, stable identifiers and responsible institutions provide the strongest route from overview to verifiable evidence. The source revision retrieved here is dated Sep 5, 2026. The linked authority identifier is Q854550. The Library of Congress control number is sh00006247. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank.

Critical limits

Overview language is designed for orientation and should not be treated as a substitute for the evidence cited beneath it. The lead is largely declarative, so disagreement and counter-evidence require a deliberate search beyond the opening account. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

How to read it

Use the entry as an orientation point, then follow its citations and revision history. Names, dates and institutional relationships should be checked against the original record.

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  2. Expand the search: follow Hoodoo (geology) primary sources, Hoodoo (geology) archive and Hoodoo research across catalogues and specialist indexes.
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Source & attribution

This entry incorporates text from Hoodoo (geology)” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.