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A map of Tonga Located in Oceania , Tonga is an archipelago in the South Pacific Ocean , directly south of Samoa and about two-thirds of the way from Hawai'i to New Zealand. Its 171 islands, 45 of them inhabited, [ 1 ] are divided into three main groups – Vava'u, Ha'apai, and Tongatapu – and cover an 800-kilometre (500-mile; 430-nautical ...
The combined efforts of generations of resident and visiting naturalists have helped to make the butterfly fauna of Tobago well known. Some 129 species have been recorded on the island of Tobago that has a land area of only 300 km 2 (116 mi 2 ) and is approximately 42 km long and 10 km wide.
ʻAta is a depopulated island in the far southern end of the Tonga archipelago, situated approximately 160 kilometres (99 mi) south-southwest of Tongatapu. It is distinct from ʻAtā , an uninhabited, low coral island in the string of small atolls along the Piha passage along the north side of Tongatapu .
The town of Janitzio, which means "maize flower" in Purépecha [citation needed], is located atop a hill on the island. Janitzio can only be reached by boats which run regularly back and forth from about 7:30 am to 6 pm, accessible from Pátzcuaro's pier (embarcadero). [2] The boats take approximately 25 minutes to reach the island. [3]
By this time, the island was 1 to 2 km (0.62 to 1.24 mi) wide, 2 km (1.2 mi) long, and 120 m (390 ft) high. [41] [42] The new island had joined with Hunga Haʻapai, and was about 200 m (660 ft) away from joining with Hunga Tonga. [41] [42] Locals visiting the island said seabirds were nesting. [43]
Cyrestis is a butterfly genus in the family Nymphalidae. They are known as map butterflies, so named because the wing-markings of some species resemble the lines of latitude and longitude of a world map. Cyrestis is a widespread genus ranging from Africa to parts of the Indomalayan realm and parts of the Australasian realm .
Tofua caldera. Tofua is a volcanic island in Tonga.Located in the Haʻapai island group, it is a steep-sided composite cone with a summit caldera.It is part of the highly active Kermadec-Tonga subduction zone and its associated volcanic arc, which extends from New Zealand north-northeast to Fiji, and is formed by the subduction of the Pacific Plate under the Indo-Australian Plate. [2]