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.
The low islands of Micronesia were typically formed by coral reefs growing on the submerged slopes of submerged volcanic mountains, which built up over time to create the islands. Additionally, some low islands in Micronesia were formed by the accumulation of sand and sediment carried by ocean currents and deposited on top of submerged volcanic peaks.
hey i really do not know the answer but can someone help me plz
they are continental, oceanic and tropical.
The Federated States of Micronesia is made up of islands and atolls, which are low-lying coral formations. These islands are scattered across a vast area of the western Pacific Ocean.
if you meant solomon islands, they are high islands:)
small islands...its because theres thousands of islands in micronesia..but only 4 states of FSM
Micronesia is a region in the western Pacific Ocean consisting of thousands of small islands. It is divided into four main island groups: the Caroline Islands, the Gilbert Islands, the Mariana Islands, and the Marshall Islands. The islands are known for their tropical climate, coral reefs, and diverse marine life.
because people like to get high
Acording to wikipedia http://en.wikipedia.org/wiki/List_of_islands_in_the_Pacific_Ocean , high islands.
High islands, low islands, and volcanoes
Micronesia consists of thousands of islands in the Pacific Ocean. They are not politically connected to any continent, but are sometimes associated with Australia.
The islands of Micronesia, Melanesia, and Polynesia can be classified into two main types: volcanic islands and coral islands. Volcanic islands, such as those found in Melanesia, are formed from volcanic activity and typically feature rugged terrains and high elevations. Coral islands, common in Micronesia and parts of Polynesia, are formed from coral reef structures and tend to be flatter and lower in elevation. Both types play crucial roles in the biodiversity and cultural practices of the Pacific island nations.