An island is a piece of land that is completely surrounded by water. Islands can be found in oceans, seas, rivers, and lakes. They come in different sizes, from small islets to large landmasses like Greenland and Australia.
Deposition: Sediments carried by rivers, glaciers, or ocean currents can accumulate and form islands. For example, sandbars and barrier islands are formed through the deposition of sediment by ocean currents.
Tectonic Uplift: Islands can also be formed when tectonic plates shift, causing the land to rise above sea level. This process can create islands like the Galapagos Islands.
Types of Islands
Islands can be classified into different types based on their origins:
Continental Islands: These islands were once part of a continent but were separated by rising sea levels or tectonic activity. Examples include the British Isles and Borneo.
Barrier Islands: Long, narrow islands parallel to the mainland, separated by a lagoon or a bay. They protect the mainland from waves and storm surges.
Coralline Islands: These islands are formed from the accumulation of coral reef and are typically found in tropical waters.
Artificial Islands:Humans can create islands by dredging and piling up sand and rocks. Examples include the Palm Islands in Dubai.
Islands are home to unique ecosystems and species that have evolved in isolation. They often have high levels of endemism, meaning species are found nowhere else on Earth. However, they are also highly vulnerable to human activities and invasive species.
Study Guide
Here are some key points to remember about islands:
Earth's surface changes constantly through a variety of processes and forces. Students can:
Analyze and interpret data identifying ways Earth's surface is constantly changing through a variety of processes and forces such as plate tectonics, erosion, deposition, solar influences, climate, and human activity
Develop and communicate an evidence based scientific explanation around one or more factors that change Earth's surface