page_title: Tebunginako
hierarchical_section_title: Tebunginako
caption_attribution_description: At high tide a handful of houses and the village’s biggest buildings—a Catholic church and giant concrete community hall—are again surrounded by a saltwater moat. ”The contamination of the groundwater started in the late ’70s, and after that erosion started and houses started to fall into the sea,” recalls Mr Aata Maroieta, Village Chief of Tebunginako. ”The force of erosion was stronger than the sea walls and eventually the government said that all we could do was relocate.”
context_page_description: Tebunginako is a village on Abaiang atoll in Kiribati; to its west is Ubanteman, and to its south are Borotiam and Koinawa.
  The settlement had been dealing with seawater inundation and coastal instability since the 1970s, and is being abandoned. A report by the South Pacific Applied Geoscience Commission determined that natural erosion was the primary factor, as the village was located close to the site of a blocked ocean/lagoon channel, however many, including the Kiribati government, suggest that this was due to sea level rise caused by global warming.
  As storm surges becoming more frequent and spring tides more forceful, eventually the erosion was so great that the village had to be abandoned. The remains of about 100 thatched homes and a maneabe are now up to 30 metres offshore. The villagers relocated themselves further inland, with the new village retaining the same name. The sea reaches what was the fishpond creating a peninsula with the Roman Catholic church standing on one side of the bay and the village on the other side.
context_section_description: Tebunginako is a village on Abaiang atoll in Kiribati; to its west is Ubanteman, and to its south are Borotiam and Koinawa.
  The settlement had been dealing with seawater inundation and coastal instability since the 1970s, and is being abandoned. A report by the South Pacific Applied Geoscience Commission determined that natural erosion was the primary factor, as the village was located close to the site of a blocked ocean/lagoon channel, however many, including the Kiribati government, suggest that this was due to sea level rise caused by global warming.
  As storm surges becoming more frequent and spring tides more forceful, eventually the erosion was so great that the village had to be abandoned. The remains of about 100 thatched homes and a maneabe (community meeting hall) are now up to 30 metres offshore. The villagers relocated themselves further inland, with the new village retaining the same name. The sea reaches what was the fishpond creating a peninsula with the Roman Catholic church standing on one side of the bay and the village on the other side.
caption: An abandoned building on Tebunginako, used as a combination church and community hall. Saltwater erosion is visible on the building's concrete foundation.
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