It has never had its own field but has utilized the uneven turf at Onesosopo Park, which is replete with volcanic stubble, water, toads, and sand traps.

In retaliation, the Lei’ato of Fagaʻitua mobilized warriors and launched a dawn raid on ʻAoa, resulting in the deaths and injuries of several villagers.

[7] The geological formation of Fagaʻitua is centered around the Ālōfau volcanic complex, which features a shield-shaped dome composed of thinly layered basaltic lava flows, including both ʻaʻā and pāhoehoe types.

These layers, along with dikes, breccias, and tuffs, create a distinctive structure that spans approximately 2.4 square kilometers on the eastern edge of Fagaʻitua Bay.

The lava deposits, predominantly primitive olivine basalts, are thinly bedded and exhibit a dip of 10 to 20 degrees, radiating away from the village of Ālōfau.

A significant dike complex is visible along the road leading southeast from Fagaʻitua village, providing insight into the subsurface dynamics of the volcano.

The caldera rim, a prominent feature of this volcanic system, descends steeply toward the southwest and extends partially beneath the adjacent offshore waters.