Until April 2010, when the nearby Ellis Basin cave system was found to be deeper, Nettlebed Cave was thought to be the deepest cave system in the southern hemisphere. It drops 889 metres below its upper entrance (Blizzard Pot) to its lower exit (Pearse Resurgence), and its 24 kilometres of cave passages make it New Zealand's third longest cave.
Nettlebed Cave was first explored by cavers in 1969 through the dry overflow passage of a large spring pouring into the Pearse River. By 1973 1.3 kilometres of passages had been mapped. It was not until 1979 that a flowstone squeeze known as the Hinkle-horn-honking-holes was passed, making further explorations possible. Five successive Christmas expeditions (1979-80 through 1983-84) utilizing an underground camp at Salvation Hall led to the exploration and mapping of a further 20 kilometers.
In 1986 another cave (Blizzard Pot) was connected with Nettlebed Cave, providing an upper entrance to the system.
On 21 March 2007, a team of international cave divers set a New Zealand cave diving record by reaching a depth of 177m (581 feet below ground level) in the Pearse Resurgence.
After a long day underground two cavers negotiate a water filled passage in the Nettlebed cave system.
An enormous passage in Nettlebed Hammer Heights in South Island, New Zealand.
Negotiating the Hinkle-horn-honking-holes, Nettlebed Cave.
Yes, I have seen some beautiful ones, like the one in Carlsbad in New Mexico in the USA, but this one is one of the best!