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A continental island is an island that is geographically close to and geologically connected to a continent. These islands are essentially extensions of the continental landmass. Examples include Great Britain and Greenland.12

In contrast, oceanic islands are typically formed by volcanic activity and do not have a foundation of continental rock. The distinction between continental and oceanic islands is often marked by the Andesite Line in the Pacific Ocean, which separates islands rich in andesite (a type of volcanic rock) from those primarily composed of basalt. The formation and characteristics of islands are closely related to the processes of plate tectonics, including volcanic arcs and island arcs that form at plate boundaries.345

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