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Carrauntoohil

highest mountain in Ireland

Architectural plans, a scale model, maps and brass measuring instruments
Places and architectureInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionSep 6, 2026
Entity authorityQ503368
Source-derived summary

Carrauntoohil, Carrauntoohill or Carrantuohill (, KARR-ən-TOO-əl; Irish: Corrán Tuathail [ˌkɔɾˠaːn̪ˠ ˈt̪ˠuəhəlʲ], meaning "Tuathal's sickle") is the highest mountain in Ireland at 1,038.6 metres (3,407 feet 6 inches). It is on the Iveragh Peninsula in County Kerry, close to the centre of Ireland's highest mountain range, MacGillycuddy's Reeks. Carrauntoohil is composed mainly of sandstone, whose glaciation produced distinctive features on the mountain such as the Eagle's Nest corrie and some deep gullies and sharp arêtes in its east and northeastern faces that are popular with rock and winter climbers.

As Ireland's highest mountain, Carrauntoohil is popular with mountain walkers, who most commonly ascend via the Devil's Ladder route; however, Carrauntoohil is also climbed as part of longer mountain walking routes in the MacGillycuddy's Reeks range, including the 15-kilometre (9+1⁄2 mi) Coomloughra Horseshoe or the 26-kilometre (16 mi) MacGillycuddy's Reeks Ridge Walk of the entire mountain range. Carrauntoohil, and most of the range is held in private ownership and is not part of any Irish national park; however, reasonable access is granted to the public for recreational use.

Geology

Carrauntoohil is composed of sandstone particles of various sizes which are collectively known as Old Red Sandstone. Old Red Sandstone has a purple-reddish colour (stained green in places), and has virtually no fossils; it dates from the Devonian period (410 to 350 million years ago) when Ireland was in a hot equatorial climate. The sedimentary rocks of the Iveragh Peninsula are composed of three layers that are up to 7 kilometres (4+1⁄2 mi) thick (in ascending order): Lough Acoose Formation, Chloritic Sandstone Formation, and the Ballinskelligs Sandstone Formation.

Carrauntoohil was later subject to significant glaciation during the last ice age, the result of which is deep fracturing of the rock, and the surrounding of Carrauntoohil by U-shaped valleys, sharp arêtes, and deep corries.

Geography

Carrauntoohil is the central peak of the MacGillycuddy's Reeks range, and has three major ridges.

Editorial summary

The public source identifies “Carrauntoohil” as highest mountain in Ireland. This brief keeps that definition visible, then builds a research path around Carrauntoohil, highest and mountain.

Editorial reviewA valuable geographic starting point for tracing changing names, boundaries, uses and administrative responsibility. The current 316-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 Carrauntoohil, highest and mountain providing the first useful test.
Editorial analysis

Why this record matters

A short description can identify a subject without explaining its stakes. For “Carrauntoohil”, the useful work is to connect “highest mountain in Ireland” to the records capable of establishing context and consequence.

Evidence profile

Maps, plans, fabric surveys and administrative records can establish how the site’s name, extent and function changed over time. The source revision retrieved here is dated Sep 6, 2026. The linked authority identifier is Q503368. VIAF identifies the subject as 315164007. Authority coordinates are 51.999, -9.743. 1 of 2 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank.

Critical limits

Architectural summaries often privilege surviving fabric and can understate demolished phases, contested use or displaced communities. The source lead contains qualifying language; that uncertainty should survive quotation, summary and reuse. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

How to read it

Treat names, boundaries and functions as historically changeable. Maps, plans, inventories and administrative records can clarify what the place meant at different dates.

Best used for
  • Historic place names
  • Jurisdictional context
  • Routes into maps and plans
Verify next

Contemporary maps, plans, listed-building records, estate papers and the responsible local or national archive.

Three-step research path

  1. Establish the record: confirm the title “Carrauntoohil”, its source revision and the description used here.
  2. Expand the search: follow Carrauntoohil primary sources, Carrauntoohil archive and Carrauntoohil research across catalogues and specialist indexes.
  3. Test the account: compare the strongest cited source with the responsible institution’s current record and note any disagreement.

Questions for further research

  1. Which source most directly establishes the central claim about “Carrauntoohil”?
  2. Which earlier names or jurisdictions may reveal additional records?
  3. What physical evidence or contemporary plan supports the description?
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Source & attribution

This entry incorporates text from Carrauntoohil” 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.