
Mainland orphans
Some islands' rocks reveal that they were once part of a continent. Madagascar is a fragment of land that was left behind when the other continents drifted apart. Many offshore islands, such as the British Isles, formed after the last Ice Age. As the climate grew warmer and glaciers melted, sea levels rose. Low-lying areas along Europe's coast were flooded, and the higher elevations remained above water as islands. Then there are barrier islands, which are created as currents steal coastal sand and deposit it offshore in long sandbars. The Atlantic coast of the United States has many islands like these.



