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Geological Formation

Ritigala

Inselbergs and Crystalline Monoliths

Ritigala is a steep massif of crystalline rock rising from the dry plains of north central Sri Lanka, reaching about 766 meters, roughly 600 meters above the surrounding lowland, and is the highest point in the northern part of the island. Formed from the ancient gneiss and granulite basement that makes up much of Sri Lanka's Precambrian Highland Complex, the massif comprises four peaks separated by a gorge, and its height creates its own wetter microclimate, catching monsoon rain that leaves the surrounding dry-zone plains far drier. Its forested slopes have long sheltered a Buddhist monastic settlement, whose ruins remain scattered across the massif.

Facts
Classification
Protected Status
National Park or Reserve 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: Ritigala

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: Ritigala
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Ritigala
Sources
1. Ritigala (Wikipedia)
Article text
Quote, Article text
Ritigala is a strict nature reserve, covering 1,528 ha (3,780 acres).
View the Source
Wikidata: Ritigala
Wikidata Q19719626, class allow-list match (w-wdresolver-0926)View the Source
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