Tongatapu
— — the coral the ocean keeps breathing through.
Not only on a wall.
“The main island of Tonga, flat and coral-built where most Pacific nations rise as volcanoes. Nukuʻalofa sits on the north shore, the royal palace white against the lagoon. On the south coast at Houma the blowholes go off in a long line for five kilometres when the swell is up. The pace is slower than anywhere east of here.
Tongatapu, on ceramic.
Each tile is finished by hand in our Knoxville studio. Artwork is slowly infused into the ceramic surface under high heat and pressure, and rests beneath a thin glossy finish. The colour lives in the surface, not on top of it.
Pick any four 4-inch tiles — National Parks you've been to, a Smokies set, the four seasons of one place. $ for a set of , cork-backed, ready to live on the table.
The place, in three passes.
Tongatapu is the largest island of the Kingdom of Tonga and home to about seventy-five thousand of the country's roughly hundred thousand people. The island covers around two hundred and sixty square kilometres in the South Pacific, raised coral rather than volcanic, which is why it lies flat and green where Samoa and Fiji rise to peaks. Nukuʻalofa, the capital, sits on the north shore facing a sheltered lagoon. The island has been continuously inhabited for nearly three thousand years and remains the seat of the only Polynesian monarchy never colonised.
At the eastern end of the island the Haʻamonga ʻa Maui rises from a clearing: three slabs of coral limestone arranged as a trilithon, each upright weighing about forty tonnes, raised in the early thirteenth century during the reign of Tuʻitātui. It has been called the Stonehenge of the Pacific, though the comparison shortchanges both. In Nukuʻalofa the Royal Palace, a white timber building shipped in pieces from New Zealand in 1867, faces the seafront beneath Norfolk pines. The two together hold eight centuries of Tongan kingship in plain sight.
Along the south coast at Houma the Mapuʻa ʻa Vaea blowholes run for nearly five kilometres of broken coral terrace. When the Pacific swell hits the undercut shelf, seawater shoots through dozens of vents at once, the line of plumes lifting twenty or thirty metres into the trade wind. The display is strongest at high tide with a southerly swell, June through September. Inland, Anahulu Cave at Haveluliku holds a freshwater pool beneath stalactites; swimming there is allowed for a small fee paid to the family that holds the land.