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Deform the ground and change the shape of Earth as they move; very destructive. For this, we need to study body waves so that we can see what Earth's 'body' is like. The lithosphere can't be classified neatly as either crust or mantle because it consists of both. Explanation: Earth's mantle occupies 84% of space. The same thing happens to body waves when they travel through the earth.
How could you adjust your models to show the changes in matter and the different states in each sphere? The inner core is solid because the pressure at that depth is so high that it keeps the core from melting. Interior of the earth worksheet. Here, P waves bend and pick up speed, telling us that the inner core must be solid material because P waves travel faster through solid than liquid. For each layer, add on the depth of that layer to the circle that you've already made, then cut out that new, larger circle. Only able to move through solids. The center of Earth is iron and nickel.
Use different colors of modeling clay to create a half-sphere of the earth. Explain that we can find valuable resources in the crust (oil and minerals). This version of Firefox is no longer supported. 5), which contains garnets. On the top and bottom parts of the mantle, the rock doesn't move very much. Remember that this is never exact. Earth's Interior Structure & Study | What is Inside the Earth? - Video & Lesson Transcript | Study.com. After this time, Earth began to cool allowing layers to form. We know it exists because of how seismic waves change speed as they move through it, but it isn't clear why it's different from the rest of the mantle.
You can use a number of different materials to build a model of the earth. P waves are compressional or longitudinal waves. Surface waves are important, but they don't provide much information about what happens below the surface. This means they retain their frequency as they arrive at the seismic station. Structure of the interior of the earth. P waves can travel through both liquid and solid material, but S waves can only travel through solids. Instruct students to set their egg on their plate and wait for step-by-step directions to be given.
It has a density higher than the crust portion with 10 to 200 km thickness. But, we need body waves to tell us what lies below. S waves are shear waves that shake the ground up and down and side to side. How Did Earth Acquire Its Layered Structure? This means seismic waves travel quicker through solid than liquid. Drilling Into the Earth Worksheet. Tectonic plates sit on the asthenosphere and slide during tectonic activity due to convection currents. DIAGRAM OF INTERIOR OF THE EARTH worksheet. This is where the outer core meets the inner core, and we know that it's solid because the P waves pick up speed yet again. Explain that the Earth is our home, and we need to understand it so we can take good care of it. Submitted by: Laurie Molnar. These recordings made by a seismograph are called seismograms. Date: January 19, 2002. P waves can travel through liquid but much more slowly than through a solid.
Make a circle that represents the core of the earth. Watch the video below to understand the composition of each layer. Worksheet and Answer Key in format; requires free Adobe Acrobat Reader. What do you want to do? Do this for each item in the list above, and you will get an understanding of how thick or thin each layer needs to be. Another pretty significant change occurs at about 1, 900 miles down. While studying seismic waves from earthquakes provided scientists with a lot of information about Earth's interior, much of what we know actually came from nuclear weapons testing during the Cold War. Without a weak asthenosphere, plates would be locked in place, unable to move as they do now. Interior of the earth ppt. The crust is broken into big pieces called tectonic plates and resemble pieces from a jigsaw puzzle. Ask students to write a 1-page paper to address the following questions: Assessment: Observe students during the egg activity. Seismic waves travel at different speeds when they pass through different types of material, so by studying seismograms, scientists can learn a lot about Earth's internal structure.
P waves bend slightly when traveling to different layers. Mineralogy||Studies minerals in Earth's crust as well as lunar and meteorite samples|. We know that the mantle is solid because both P and S waves travel through it. Crust: Up to 25 miles.
Both P and S waves are able to travel through the mantle because the mantle is solid. The mantle is made of mostly that 'liquid' rock that moves like silly putty, but the outer core is an area of mostly liquid iron, which is much denser than the rock in the mantle. This boundary is referred to as the core-mantle boundary. ) As P waves continue through the outer core, they suddenly 'bend' again and pick up speed at a little over 3, 000 miles into Earth's interior. Inner core: 800 miles. One of the ways the United States was able to monitor nuclear testing by the Soviet Union was to study seismic waves that radiated underground from the nuclear tests. S waves suddenly stop as if they have hit a brick wall, and P waves 'bend' and slow down so much that no waves are detected at the surface of Earth. Interior of the earth worksheets. Using colored chalk, draw the layers on the board. I feel like it's a lifeline. Rock samples from Earth provide direct evidence of Earth's interior. Explanation: The crust and the uppermost part of the mantle are known as the lithosphere. Resources created by teachers for teachers.
The mantle is very thick: 1800 miles deep. In the middle of the mantle is the asthenosphere. P waves are compressional or longitudinal waves able to move through any type of material (solid and liquid). The outermost solid part of the Earth is known as ______. It seems like a logical way to get there instead of flying all the way around the globe.
According to scientists, these plates have been moving throughout Earth's history, and they are still moving today at a rate of 3 inches per year. When you put the cake mixes into the pans to bake, try to use the approximate dimensions that you calculated above so that the cake layers will be the correct thickness. Unlock Your Education. To help you understand all of the layers, draw a picture of the size of the different layers. Three types of rocks also help to make up the composition of Earth.
There are two kinds of crust: continental crust, and ocean crust. Rocks higher in the mantle are typically composed of peridotite, a rock dominated by the minerals olivine and pyroxene. List three properties of the mantle. The crust is like a jigsaw puzzle made of approximately 20 huge slabs of rock called tectonic plates.
Seismic waves are sent through the earth during earthquakes, and those energy waves are what cause the ground to shake as they travel through it.