Plate tectonics

Science, Grade 6


Study Guide

Provides a quick overview of the topic selected!

Flash Cards

Practice and review the topic selected with illustrated flash cards!


Assess students’ understanding of the topic selected!


Print illustrated worksheets!


Engage students with interactive games.

Study Guide Plate tectonics Science, Grade 6

PLATE TECTONICS The Earth is a dynamic planet. Its interior is actually in motion! The crust on its surface is also in motion. It was not until the 20th century that geologists truly began to understand Earth’s dynamic movements. New theories, supported by ever-improving technologies, have made it possible to more clearly understand the forces working within the planet we call home. The Earth’s Interior Sophisticated machines called seismographs are used to understand earthquakes. They measure the strength and arrival times of the different seismic waves produced by an earthquake. Careful study of seismograms has provided a relatively detailed picture of Earth’s interior structure. The Earth is composed of three different layers: the core, the mantle and the crust. The core is composed of two layers, the solid inner core and the liquid outer core. The core is the densest layer of the Earth and is composed of nickel and iron. Convection currents in the liquid outer core, combined with the Coriolis effect created by Earth’s rotation on its axis, are believed to be the source of the Earth’s magnetic field. The mantle is composed of the high-density silicate rock, basalt. Basalt is high in iron and magnesium minerals. Due to intense heat and pressure, the mantle is not solid rock, but a highly viscous liquid rock. Detailed studies have shown that the mantle has a strong lower layer called the mesosphere and a weaker upper layer called the asthenosphere. The mantle is hottest near the core and cools nearer the crust. The hot mantle material rises toward the crust. As it rises it also cools. When it cools, it becomes more dense and then descends © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at
back toward the center of the Earth. This circular motion creates convection cells. Convection cells in the mantle cause the crust to move over the Earth’s surface. Earth’s outermost layer is the crust. There are two different types of crust. Basaltic oceanic crust pours out from the mantle and is found under the oceans. It is the denser of the two types of crust, but it is also the thinner of the two. Continental crust is considerably less dense, but it is also considerably thicker than oceanic crust. The crust moves over the Earth’s surface in large pieces called tectonic plates. Tectonic plates are constructed in layers with crust on the top and a piece of the solid upper mantle below. Geologists call this combination of crust and upper mantle the lithosphere. Lesson Checkpoint: What are the two layers of the Earth’s crust? What Is Continental Drift? In the early 1900’s, Alfred Wegener observed that the boundaries of the continents appeared to look roughly like pieces of a large puzzle. Based on this observation, he theorized that the continents were once together and that some force moved them apart. Studies of fossils on different continents and glacial striations in rocks on different continents supported this theory. © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at
Continental drift is the name given to Wegener’s theory. According to the continental drift theory, all of the continents were together as a large, single landmass. This landmass was given the name Pangaea. About 180 million years ago, the super-continent Pangaea began to split into two smaller continents. Geologists call these two continents Laurasia and Gondwana. For about 50 years, Alfred Wegener’s theory of continental drift was an accepted part of geology. Wegener’s theory has been replaced by the more complete theory of plate tectonics. Lesson Checkpoint: Explain the Continental Drift Theory Sea-Floor Spreading In the middle of the Atlantic Ocean is an immense mountain chain. Here sea-floor spreading occurs. Geologists have determined that at the mid-ocean ridge of the Atlantic Ocean basin, two tectonic plates are pulling away from each other. As they pull away, magma from the Earth’s mantle pours out through the crack onto the ocean floor. © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at
Sea-floor spreading is part of the more comprehensive theory called plate tectonics. The mid-ocean ridge, where the oceanic plates spread apart from one another, is where new oceanic crust is formed. The plates move away from the mid-ocean ridge at a rate of about 1 cm/year. The Theory of Plate Tectonics Alfred Wegener’s theory of continental drift was convincing; however, he could not explain how continental drift occurred. A number of discoveries throughout the 20th century led to a completely new theory, known as plate tectonics. This theory was first proposed in the early 1960’s. As explained above, one piece of the theory is sea-floor spreading. This explains how oceanic crust is formed. Geologists explained the presence of deep ocean trenches at continent-ocean crust boundaries as the region where oceanic crust goes under the continental crust. At this subduction zone, crustal material melts and rises toward the surface, creating volcanoes. The theory of plate tectonics also explained that earthquakes are the result of the energy created by plates pushing toward, pulling away from, and sliding past each other. The strength of the plate tectonic theory is that all of these geologic processes can be explained by the interactions of crustal plates. One piece of the puzzle, so to speak, that was missing was the mechanism that causes plate tectonics to happen in the first place. Geologists are now in agreement that the driving force for the movement of tectonic plates is convection cells of extremely hot, viscous rock in the mantle. In other words, the rising of hot mantle material and its subsequent descent back to the mantle depths is the engine that drives all the actions and interactions in plate tectonics. © Copyright NewPath Learning. All Rights Reserved. Permission is granted for the purchaser to print copies for non-commercial educational purposes only. Visit us at
© Copyright 2012-2020 NewPath Learning. All Rights Reserved. Privacy Notice * Terms of Use