Earth and Environment Atlas

How The Planet Works
Sign In
Text size
100%
Theme
Geological Formation

Liathach

Inselbergs and Crystalline Monoliths

Liathach is a mountain in the Torridon Hills of Scotland's Northwest Highlands, standing between Loch Torridon and the neighboring peak of Beinn Eighe at an elevation of 1,055 meters. It is built of Torridonian sandstone, mostly red and chocolate colored varieties along with arkoses, flagstones and shales, resting on much older Lewisian gneiss, some of whose material was itself weathered into the sandstone above. The rock forms massive, near horizontal strata that create the numerous terraces visible from a distance, a landscape further shaped by heavy glacial and alluvial erosion.

Facts
Classification
Protected Status
Locally or Regionally Protected 1
Protected Status
International Treaty Protected Area 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Liathach

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Liathach
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Liathach
Sources
1. UNEP-WCMC and IUCN: Protected areas at the coordinates of Liathach, World Database on Protected Areas
UNEP-WCMC and IUCN
  • name_eng and desig_eng
    "name_eng": "Loch Maree Complex", "desig_eng": "Emerald Network"
  • desig_eng, designation 4 of the point search
    "name_eng": "Torridon Forest", "desig_eng": "Site of Special Scientific Interest"
View the Source
Wikidata: Liathach
Wikidata Q3064120, class allow-list match (w-wdresolver-0926)View the Source
Comments (0)
No comments yet. Be the first to share a thought.
Reader Challenges (0)
No disputes yet. Spotted an error or a better source? Open the first one.