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Lesson 2.3: Islands *Refer to Chapter 13 in your Textbook
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Lesson 2.3 Learning Goals:
Explain how a hotspot forms an island chain. Label the structure of a barrier island. Differentiate between the 3 types of reefs.
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Hot Spots Wilson (1963) Volcanoes can form in the middle of a plate where magma rises upward until it erupts on the sea floor, at what is called a “hot spot” The hotspot will stay still as the plate moves, creating a chain of islands
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Hot Spots
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Barrier Islands Barrier Islands form when a piece of the mainland is broken off and separated by a body of water (lagoon) They can be very large and can be ideal for beaches & hotels, but are also vulnerable to erosion and weather
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Barrier Islands
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Barrier Island Structure
Ocean, Beach, Dune, Flat, Marsh, Lagoon Dune: top of the beach, usually inclining to protect the coastline Barrier flat: thick vegetation Salt marsh: swamp
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Reef Formation Fringing: Most common Form along shoreline of coast or
island The fore side (facing the ocean) has the most biological activity
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Reef Formation Barrier: Forms when island begins to sink or
when there is a rock for the coral to grow on Separated from land by a lagoon Usually much larger than a fringing reef
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Reef Formation Atoll: Forms when island sinks below sea level
The remains of the island are carried away by the tectonic plate, leaving behind a circular reef
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