Lopevi
In the following article we will explore in depth the fascinating world of Lopevi. From its origins to its impact today, we will delve into the multiple aspects that make Lopevi a topic of interest for people of all ages and professions. Throughout these pages, we will discover the importance of Lopevi in modern society and the relevance it has in various areas. Whether you are an expert in the field or are discovering Lopevi for the first time, this article will provide you with a complete and up-to-date overview of this exciting topic.
| Lopevi | |
|---|---|
 A satellite image of the island. | |
| Highest point | |
| Elevation | 1,413 m (4,636 ft)[1] |
| Prominence | 1,413 m (4,636 ft) |
| Listing | Ribu |
| Coordinates | 16°30′24″S 168°20′45″E / 16.50667°S 168.34583°E |
| Geography | |
  Lopevi | |
| Geology | |
| Mountain type | Stratovolcano |
| Last eruption | April to May 2007 |
Lopevi (or Lopévi) is an uninhabited island in Malampa Province, Vanuatu. It lies to the southeast of Ambrym and east of Paama.[2]
Geography
Lopevi consists of the 7-km-wide cone of the active stratovolcano by the same name.[3] It reaches a peak of 1413 m above sea level, the tallest point in central Vanuatu. It has erupted at least 22 times since 1862. The island was formerly inhabited, but in 1960 the population moved to nearby Paama or Epi because of the recurrent danger.
Lopevi is on the New Hebrides Plate, where it lies above the subducted Australian Plate to the west. Because there are no earthquakes between 50 and 200 km below the Earth's surface, it is thought that the subducted plate has fractured, and does not appear between these depths.
References
- ^ "World Ribus – Melanesia". World Ribus. Retrieved 2024-12-25.
- ^ UNEP Islands Directory
- ^ "Lopevi". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-28.
External links
| Authority control databases: Geographic |
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