Sinharaja rainforest has been designated as a UNESCO Natural World Heritage Site, UNESCO Biosphere Reserve and also a Biodiversity Hotspot by the International Union for Conservation of Nature (IUCN). All these titles are highlighting the importance of the forest reserve in terms of its exceptional biodiversity as well as its fragility. Birding in Sinharaja is particularly interesting since it is home to 95% of the endemic birds of Sri Lanka!
Named as a world heritage site in 1989, this lowland evergreen rain forest is steeped in deep legend and mystery. In English 'Sinharaja' translates to Lion (Sinha) King (Raja) alluding to a popular belief according to which the origin of the Sinhala people is from the union between a princess and the lion king who once lived in this forest.
Sinharaja rainforest consists of a series of continuous ridges, aligned approximately in an east-west direction and lies between the tributaries of the Kalu Ganga in the north and the Gin Ganga in the south. The forest lies within the transition zone of two important groups of rock types, the south/western group which consist of metasediments-charnockites and scapolite bearing calc granulites and the highland group comprising khondalites of metamorphosed sediments and charnockites.
The elevation of the Sinharaja reserve ranges from 200m to 1300m. It has a rolling terrain consisting of a series of ridges and valleys, which assumes an east-west trend in the northwestern part of the reserve. In other parts of the reserve, the ridges and valleys assume a north-west/south-east alignment. The peak of Hinipitigala is the tallest, rising up to about 1150m.Other important ridges in the reserve ranges between 550-800m in height NamelyMoulawella (760m), Kosgulana (797m), Sinharaja (742m), Kohilearambe (575m), Dotalugala (769m), and Tibbottagala (904m).
The most significant geological feature of Sinharaja is the presence of a "Sinharaja Basic Zone" which comprises hornblende pyroclasts, basic charnockites pyroxene amphibolites and scapolite.The soils of Sinharaja largely belong to the group of Red Yellow Podzolic soils, with clearly distinguishable horizons of varying soil depths. The soil is well drained with very little accumulation of organic matter.