Interesting Site

The Limestone Formation in the Batu Caves
The limestone forming Batu Caves is said to be around 400 million years old. Some of the cave entrances were used as shelters by the indigenous Temuan people (a tribe of Orang Asli).

As early as 1860, Chinese settlers began excavating guano for fertilizing their vegetable patches. However, they became famous only after the limestone hills were recorded by colonial authorities including Daly and Syers as well as American Naturalist, William Hornaday in 1878.

Batu Caves was promoted as a place of worship by K. Thamboosamy Pillai, an Indian trader. He was inspired by the 'vel'-shaped entrance of the main cave and was inspired to dedicate a temple to Lord Muruga within the caves.
History

In 1891, Pillai, who also founded the Sri Mahamariamman Temple, Kuala Lumpur, installed the murti (consecrated statue) of Sri Subramania Swamy in what is today known as the Temple Cave. Since 1892, the Thaipusam festival in the Tamil month of Thai (which falls in late January/early February) has been celebrated there.























The 272 Steps Going Up the Temple Caves
Wooden steps up to the Temple Cave were built in 1920 and have since been replaced by 272 concrete steps. Of the various cave temples that comprise the site, the largest and best known is the Temple or Cathedral Cave, so named because it houses several Hindu shrines beneath its 100 m vaulted ceiling.

















The Macaque Monkeys at the Batu Caves Site
There are various undeveloped caves which contain a diverse range of cave fauna, including some unique species, such as Liphistiidae spiders and Eonycteris and Rousettus fruit bats. The site is also well known for its numerous macaque monkeys, which visitors feed — sometimes involuntarily. These monkeys may also pose a biting hazard to tourists (especially small children) as they can be quite territorial.

















The Dark Cave
Below the Temple Cave is the Dark Cave, with its amazing rock formations and a number of animals found nowhere else. It is a two-kilometer network of relatively untouched caverns. Stalactites jutting from the cave's ceiling and stalagmites rising from the floor form intricate formations such as cave curtains, flow stones, cave pearls and scallops which took thousands of years to form.