Tham Luang Cave (Thailand) – Location, Geography, Facts
Tham Luang Cave is a karst limestone cave complex in Thailand, located in Chiang Rai province.

Tham Luang Cave, Thailand.
- Country
- Thailand
- Coordinates
- 20.3812° N, 99.8676° E
Tham Luang Cave overview
Tham Luang Cave is a karst limestone cave complex in Thailand, located in Chiang Rai province. It lies within the formally designated Tham Luang–Khun Nam Nang Non Forest Park and consists of a system of chambers and flooded passages carved into the Doi Nang Non ridge. The cave is significant for its pronounced underground stream and for its role in a widely reported international cave rescue that highlighted the hazards of monsoon-influenced karst systems.
Tham Luang Cave coordinates
Tham Luang Cave is commonly mapped at approximately 20.3812° N, 99.8676° E, or 20.3812, 99.8676 in decimal degrees.
Degrees: 20.3812° N, 99.8676° E
Decimal: 20.3812, 99.8676
Where Tham Luang Cave is located
Tham Luang Cave occupies the western flank of the Doi Nang Non mountain ridge in northern Chiang Rai province, near Thailand’s border with Myanmar. Administratively it falls within the Mae Sai District area and is set inside the forest park that bears its name. The cave entrance opens into mixed deciduous forest on a limestone escarpment, with steep karst topography above and lowland river valleys extending away from the ridge. Local topography concentrates surface runoff toward the cave’s sink points.
Why Tham Luang Cave is important
Tham Luang Cave matters as a large, accessible karst system where an active subterranean stream and extensive karst development coexist close to populated lowlands. Its combination of long, flooded passages and large dry chambers makes it distinctive among caves in northern Thailand. The cave became a focal point for international speleological collaboration and emergency engineering when a trapped group prompted sustained rescue and mapping operations. Scientists and cave divers have used Tham Luang Cave to study rapid hydrological response and speleogenesis in a ridge-scale karst setting.
History of Tham Luang Cave
Tham Luang Cave was produced by the long-term dissolution of limestone in the Doi Nang Non ridge, producing conduits that follow bedding planes and fault zones. Local people have known the cave for generations, and its passages were gradually explored and surveyed by Thai speleologists and visiting cave-diving teams. The site entered broad public attention when a complex, multi-agency rescue effort centered on the cave’s submerged passages and chambers; that operation involved international cave divers, regional authorities, and specialist equipment. Afterward, the cave’s physical mapping and institutional oversight increased, prompting more systematic monitoring of its hydrological behaviour.
Natural features of Tham Luang Cave
The cave consists of a principal entrance that leads into a descending tunnel sequence, several dry chambers, and an active stream passage that becomes submerged in places. The host rock is karstified limestone with calcite formations such as stalactites, stalagmites, and flowstone in the drier galleries. Structural controls on cave development include bedding-plane separation and local faulting in the Doi Nang Non ridge, which guide conduit orientation. Sumps—sections requiring underwater passage—connect otherwise walkable chambers, creating a mixed dry-and-flooded cave morphology.
Environment, protection, and monitoring of Tham Luang Cave
Tham Luang Cave is located inside the Tham Luang–Khun Nam Nang Non Forest Park and is subject to forest-park management and conservation measures administered by Thai conservation authorities and provincial offices. Management priorities emphasize protection of karst landforms, water quality in the underground stream, and monitoring of flood hazards that affect cave safety and structural integrity. Stewardship involves periodic surveys by park staff, collaboration with speleological societies for mapping, and coordination between conservation agencies and emergency services for contingency planning and environmental oversight.
Tham Luang Cave facts
- Tham Luang Cave is part of the Tham Luang–Khun Nam Nang Non Forest Park in Chiang Rai province.
- The cave occupies the limestone ridge known locally as Doi Nang Non, often referred to as the "Sleeping Lady."
- An active underground stream runs through Tham Luang Cave and can flood passages rapidly after heavy surface runoff.
- A multinational rescue effort concentrated on extracting an entrapped youth football team and their coach from inside the cave’s flooded sections.
- Thai and international cave-diving teams conducted detailed underwater mapping and diving operations to chart submerged sections of Tham Luang Cave.
Explore More in Thailand
More in Thailand
Similar places by type or theme
These pages cover places with a similar kind of geography, heritage profile, or thematic tags.
Related places to Tham Luang Cave
Explore nearby pages and closely connected places to keep navigating within the same geography cluster.
Explore Places by Type
Browse structured collections of recently published places by institution, urban role, or transport type.
Frequently Asked Questions
What are the coordinates of Tham Luang Cave?
Tham Luang Cave is commonly mapped at approximately 20.3812° N, 99.8676° E, or 20.3812, 99.8676 in decimal degrees.