Rusa (Gua) [Deer Cave - Garden of Eden Entrance]

Histoire

Survey history Deer Cave was surveyed in 1961 by G. E. Wilford of the British Borneo Geological Survey, who predicted that Mulu would yield many more caves in the future. The cave, which is also known as Gua Payau or Gua Rusa by the local Penan and Berawan people, is said to have received its name because of the deer that go there to lick salt-bearing rocks and shelter themselves. The cave was extensively mapped by a Royal Geographical Society expedition in 1978. They produced measurements of 174 m (571 ft) wide and 122 m (400 ft) high in one section that passed through the mountain for a distance of 1 km (0.62 mi). The next survey in 2009 increased the acknowledged passage length to 4.1 km (2.5 mi) and connected Lang Cave, another show cave within the park, to the Deer Cave System. This survey, made by the Hoffman Institute at Western Kentucky University, revealed the maximum cross-sectional area to be in the large southern passage. This was documented at 169 m wide with a ceiling height of 125 m (410 ft). The northern passage registered the greatest ceiling height at 148 m (486 ft) with a cross-sectional width of 142 m (466 ft). The main entrance of Deer Cave was measured at 146 m (479 ft). Source : * Wikipedia, the Free Encyclopedia > Article "Deer Cave" : en.wikipedia.org/wiki/Deer_Cave BTH - 09/03/2026

Geologic History An explanation of the cave's formation is strongly interconnected with the geological history of the island of Borneo itself. Between 40,000,000 BC and 20,000,000 BC, a 1,500 m (4,900 ft) thick layer of sedimentary rocks known as limestone, composed largely of compressed sea shells, developed in lagoons created by coral reefs. The movement of the Asian and Australian tectonic plates caused the crust to buckle and elevate the land once more, giving birth to the island of Borneo and the Mulu mountains, around five million years ago. Since then, the landscape was hacked by constant erosion from precipitations and winds. The mountain’s surface is composed mostly of limestone, which dissolves when in contact with fresh water, and thus has been slowly sculpted into a karst. Rainwater also infiltrates the porous sedimentary rocks after going through the soil and progressively dissolves the limestone, widening the pores and cracks and creating caves of impressive dimensions such as the Deer Cave. This natural process, which is still working, will cause the cave to widen even more in the future. Source : * Wikipedia, the Free Encyclopedia > Article "Deer Cave" : en.wikipedia.org/wiki/Deer_Cave BTH - 09/03/2026