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Hunga Tonga and Hunga Haʻapai are the only subaerial parts of the volcano. Hunga Tonga is the eastern island, while Hunga Haʻapai is the western one. They are part of Tonga's Haʻapai group of islands, [15] an island arc formed at the convergent boundary where the Pacific Plate subducts under the Indo-Australian Plate. [6] [16] [17]
The Tonga Meteorological Services said a tsunami warning was in effect for all of the archipelago, and data from the Pacific Tsunami Warning Center showed waves of 80 centimeters (2.6 feet) had ...
[22] [23] The government of Tonga issued a tsunami warning to residents, and waves of 30 cm (12 in) were observed in Nuku'alofa. [22] [24] Later in the afternoon, Tongan geologists near the volcano observed explosions and a 5-kilometre-wide (3.1 mi) ash column between 17:00 and 18:30 local time. [25]
Location of Haʻapai District in Tonga. Haʻapai is a group of islands, islets, reefs, and shoals in the central part of Tonga. It has a combined land area of 109.30 square kilometres (42.20 sq mi). The Tongatapu island group lies to its south, and the Vavaʻu group lies to its north. Seventeen of the Haʻapai islands are inhabited.
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]
Most of ʻAta's land is a high plateau 60 to 100 metres (200 to 330 ft) above sea level, with steep cliffs and rocky beaches ringing the shoreline of the entire island. There are three minor peaks: two on the west side and one on the east side of the island, ranging in elevation from 180 metres (590 ft) (eastern) to 307 and 309 metres (1,007 ...
Lea faka-Tonga; Українська ... Volcano F: −40 m (−131 ft) ... Government of Tonga, official 1962 land survey This page was last edited on 5 ...
Climbing down to the beach requires a certain level of mobility. The green sand is more abundant at the bottom of the tuff ring. Papakōlea Beach is located in a bay half circled by Puʻu Mahana, a tuff ring [4] formed over 49,000 years ago [5] and associated with the southwest rift of Mauna Loa.
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