In today's world, Ritter Island is an issue that has become increasingly relevant in society. Since its emergence, Ritter Island has been the subject of debate and interest, generating conflicting opinions and arousing the curiosity of experts and laypeople alike. Whether due to its impact on daily life, its historical relevance or its influence in various areas, Ritter Island has established itself as a topic of global interest. In this article, we will explore the different facets of Ritter Island and discuss its importance in the current context.
Ritter Island | |
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Highest point | |
Elevation | 140 m (460 ft) |
Prominence | 140 m (460 ft) |
Coordinates | 5°31′S 148°07′E / 5.517°S 148.117°E |
Geography | |
Location | Papua New Guinea |
Geology | |
Mountain type | Stratovolcano |
Last eruption | May 2007 |
Ritter Island is a small crescent-shaped volcanic island 100 kilometres (62 mi) north-east of New Guinea, situated between Umboi Island and Sakar Island.
There are several recorded eruptions of this basaltic-andesitic stratovolcano prior to a spectacular lateral collapse which took place in 1888. Before that event, it was a circular conical island about 780 metres (2,560 ft) high.
At about 5:30 am local time on 13 March 1888 a large portion of the island, containing perhaps 5 km3 (1.2 cu mi) of material slid into the sea during a relatively minor, possibly VEI 2, phreatic eruption. Eyewitnesses at Finschhafen, 100 km (62 mi) to the south, heard explosions and observed an almost imperceptible ash fall. Tsunamis 12–15 metres (40–50 ft) high were generated by the collapse and devastated nearby islands and the adjacent New Guinea coast killing around 3,000 people.
The collapse left a 140-metre (460 ft) high, 1,900-metre (6,200 ft) long crescent-shaped island with a steep west-facing escarpment. At least two small eruptions have occurred offshore since 1888, one in 1972 and another in 1974, which have resulted in the construction of a small submarine edifice within the collapse scar.