Devil's Tears is a kilometre of wave-blasted limestone shoreline on Nusa Lembongan's south coast, where Indian Ocean swells funnel into a series of natural blowholes and erupt vertically — the "tears" that give the place its name. From a helicopter, you see the full pattern of eruptions spaced along the cliff as a single swell rolls through, in sequence, which is impossible to take in from any single ground viewpoint.
The place
What is Devil's Tears
The Indonesian name *Pantai Air Mata Iblis* translates literally as "Devil's Tears Beach", though the place is technically a cliff line rather than a beach — a 30-metre vertical limestone wall that takes the brunt of the open-ocean swell with nothing between it and Australia 1,800 km south.
The blowholes are sea caves whose roofs have partially collapsed. When a large swell pushes water into the cave mouth, the trapped air compresses and forces the incoming water back up through the roof opening in a vertical spout that can reach fifteen to twenty metres on a big day. Different blowholes fire at slightly different timings depending on cave shape and depth — which is what creates the cascading visual effect as a swell rolls along the cliff.
The site sits at the south-western tip of Nusa Lembongan, a fifteen-minute scooter ride from the main Jungutbatu village. There is no formal entrance fee and no infrastructure beyond a low rope barrier. The rope exists because tourists are killed here roughly once every two years by waves that overtop the cliff during peak swell — Devil's Tears has the second-highest fatal-accident rate of any beach attraction in the Bali region.
The aerial view
From the air
The helicopter pass over Devil's Tears holds at low altitude along the cliff line, far enough back that the rotor wash doesn't interfere with the spray pattern. At this angle the choreography of the blowholes becomes visible in a way no ground viewpoint can match.
The **full sequence of blowholes** firing along the kilometre of cliff. Ground visitors see one
The **swell lines** approaching the cliff. From altitude you can predict which blowhole will
The **erosion pattern** of the limestone — undercut cliff bases, partially collapsed cave
The **colour gradient** of the water against the cliff — from white spray to turquoise to deep