Textbook Notes (362,730)
Canada (158,028)
EESA06H3 (234)
Nick Eyles (205)
Chapter 4

Chapter 4 Notes

4 Pages
Unlock Document

University of Toronto Scarborough
Environmental Science
Nick Eyles

Chapter Four- The Earths Interior WHAT CAN WE LEARN FROM THE STUDY OF SEISMIC WAVES? Seismic reflection-return of some of the energy of seismic waves to the Earths surface after the waves bounce off a rock boundary. Waves reflect off of the boundary between two layers of rocks and reflects back to a recording device called a seismogram. The seismogram measures the amount of time it took the waves to reflect and come back to it to measure the depth of the boundary. Seismic refraction- the bending of seismic waves as they pass from one material to another. As the seismic wave strikes a rock boundary, a lot of the wave travels through I, and changes direction. Seismograph stations receive the direct wave before the refracted one Many different seismographs can be set up in a row to record the velocities and depths of the waves In a thick layer of rock, the increasing pressure with depth changes the wave velocity, making the waves curve. WHAT IS INSIDE THE EARTH The crust is the outer layer of rock which forms a thin skin on the Earth The mantle is a thick shell of rock that separates the crust from the core The core is the centre of the earth made of metals and making the magnetic field THE CRUST Crust is thinner beneath oceans than continents and seismic waves travel faster through oceanic crust (7kmsec) vs 6km per sec through continental. The continental crust is made of granite and other rocks covered in a layer of sedimentary rocks. Felsic-rocks high in feldspar and silicon for the continental crust Mafic-rocks high in magnesium and iron for oceanic crust Mohorovicic discontinuity- the crust that separates the crust from the mantle THE MANTLE Due to the way that the seismic waves travel, it is believed that the mantle is made of solid rock with magma chambers of melted rock in the upper mantle Ultramafic rock is dense igneous rock made up of ferromagnesium minerals. It is believed that this is what the upper mantle is made up of. The crust and uppermost mantle together form the lithosphere that is brittle The lithosphere is the basis of the plate tectonics theory and its lower boundary is marked by the place that the seismic waves slow down. Asthenosphere-the rocks in this zone are closer to melting point than the rocks above or below the zone. Some of the rocks may even be melted, forming a crystal and liquid slush zone. If the rocks are close to their melting point, the zone may be important because it may represent a zone where magma is likely to be generated, and the rocks here may have relatively little strength and therefore are likely to flow. This can cause plasticity between the asthenosphere and mantle rocks. There is argument as to whether the asthenosphere even exists under continental crust as it does in oceanic areas. Scientists think that the chemical make up of the mantle rock is about the same throughout, but www.notesolution.com
More Less

Related notes for EESA06H3

Log In


Don't have an account?

Join OneClass

Access over 10 million pages of study
documents for 1.3 million courses.

Sign up

Join to view


By registering, I agree to the Terms and Privacy Policies
Already have an account?
Just a few more details

So we can recommend you notes for your school.

Reset Password

Please enter below the email address you registered with and we will send you a link to reset your password.

Add your courses

Get notes from the top students in your class.