Tectonic plates having an area of less than 1 million sq. km are considered minor plates. Microplates on a plate map are generally grouped with the neighboring principal plate. Some examples of microplates include Adriatic Plate, Shetland Plate, Capricorn Plate, Tonga Plate, Panama Plate, Anatolian Plate, Timor Plate, Greenland Plate, Juan de.

A map showing some of the world's major and minor tectonic plates. Tectonic plates are gigantic segments or pieces of the Earth's crust and uppermost mantle that together constitute the Lithosphere. Tectonic Plates are of two types, namely oceanic crust and continental crust that differ in composition.

Earth's thin outer shell is broken into big pieces called tectonic plates. These plates fit together like a puzzle, but they're not stuck in one place. They are floating on Earth's mantle, a really thick layer of hot flowing rock. The flow of the mantle causes tectonic plates to move in different directions. When the edges of plates meet, four.

Tectonic plates Earth’s surface appears to be still, but it is actually constantly on the move. Its outer shell is made up of huge slabs of moving rock called tectonic plates. The plates fit together like puzzle pieces to make up Earth’s surface. Their movements change the planet’s features, depending on how the plates meet.