Ballast Island, also known as Barasu Island, is a small uninhabited coral island or cay in the Yaeyama chain off the coast of mainland Japan, located between the islands of Iriomote and Hatoma. The island sits at the center of a coral reef composed primarily of species of the stony coral genus Acropora, most numerously Acropora muricata. At least four goby species have been found at the island, as well as a specimen of the moray eel Gymnothorax ryukyuensis.
Two small islets on the site had formed by the 1960s. A mass bleaching of the reef's corals from July to September 1998 led to the merging of the two islets, accelerated by the impact of several typhoons in 1998 and 1999. Ballast Island reached a maximum land area of around NaNsqm in late 1999, before steadily declining over the following years., the island had a surface area of around NaNsqm, a size it has maintained since 2009. While uninhabited, the island is visited on snorkeling tours departing from Iriomote, allowing access to the surrounding coral reefs.
Ballast Island is a small cay in the Yaeyama Islands, lying at the center of an isolated coral reef. The island measures approximately 200meters in length, and ranges between NaNmeters in width. The island lies south of Hatoma and approximately 2.5km (01.6miles) northeast of the coast of Iriomote. As of 2016, the island measures NaNsqm in area.
The island is primarily composed of more than 90% coral gravel, mainly branch particulates from the stony coral genus Acropora, with fragments reaching sizes of up to 10cm (00inches). The reef on which Ballast Island sits, described as "butterfly-shaped", stretches NaNmeters from Ballast Island's shoreline. The edges of the reef have the greatest density of coral, featuring various Acropora species. On the eastern side of the reef, Acropora muricata covers around 40% of the surface, with smaller amounts covered by the species A. hyacinthus, A. cytherea, and A. intermedia. On the western side of the reef, A. intermedia, A. muricata, and A. aspera make up the majority of reef cover.
Multiple species of fish are known from Ballast Island. A holotype and several paratypes of the goby Gobiodon aoyagii were collected at the island throughout the 1990s, alongside specimens of Gobiodon erythrospilus and Cabillus pexus. A paratype of Eviota filamentosa, the threadfin dwarfgoby, was found at the eastern reef. An individual of the moray eel species Gymnothorax ryukyuensis was found at Ballast Island in 1982.
Local accounts describe islands existing at its present location since at least the 1960s, although subject to considerable changes in shape and terrain due to typhoons and the yearly monsoons. Ballast Island was initially divided into two smaller islets in an east–west arrangement, with a combined land area ranging from NaNsqm. The name Ballast Island refers to the island's gravelly composition, resembling ships' ballast.[1]
A large-scale bleaching event struck the reef's corals from July to September 1998, leading to the accumulation of dead coral over the following seasons. The land area above water rose sharply by early 1999 as two smaller islets coalesced to form Ballast Island. Three typhoons in 1998 and 1999 may have contributed to the rapid accumulation of coral on the island. The island reached its largest size in November 1999, around NaNsqm, before steadily declining in area over the following years. The island had declined to around NaNsqm by 2001, likely due to sediment dispersal in the surrounding water. It maintained an area ranging from NaNsqm throughout the 2000s, before declining to NaNsqm in 2009, remaining around this size since.
Snorkeling tours, departing from Iriomote, take place around Ballast Island and Hatoma.[2]