Geology of Sri Lanka

Sri Lanka is part of a precambian craton, some two billion years old metamorphic rocks. Such rocks were originally sedimentary rocks, but were transformed by a long series of crust muvements, subsidence, high pressure and temperature inside the earth. This craton is a part of the super continent Gondwanaland, and was connected with the craton of the Indian sub continent, until it colldided with the Asian plate and formed the Himalaya some 45 Million years ago. After this collision the small piece which is the base of Sri Lanka was separating from the Indian plate. This separation caused earth quakes and volcanism which created some volcanic rocks on the island.

The geologic history of the island results in a huge amount of metamorphic rocks, but also a small amount of volcanic and sedimentary rocks. The metamorphic rocks are rich in mineral deposits, including iron ore, zinc, mangane, molybdenum, nickle, cobalt, arsene, wolframe, tellurium and gold. There are numerous precious gems found on the island too, rubies, sapphires, topaz and spinell. Unfortunately the history of the country did not result in the development of show mines so far, although it is a popular tourist destination.

There are only very few natural caves in isolated spots of limestone. Most common are erosional caves in all kinds of rocks, created by the erosional forces of the tropic climate. However, they are always of limited depth, more or less overhanging cliff faces and abris. Nevertheless they were used over centuries to create hermit's homes and built temples or buddha statues inside. Several temples in the country are called cave temples.


See also


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