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In Micronesia, low islands are typically formed from coral reefs and consist mainly of sandy or rocky land with limited elevation, often characterized by lush vegetation and fragile ecosystems. High islands, on the other hand, are volcanic in origin, featuring mountainous terrain and richer soil, which allows for more diverse agriculture and habitats. Examples of low islands include the Marshall Islands, while high islands include locations like Pohnpei and Guam. Both types of islands play crucial roles in the cultural and ecological diversity of the region.

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