1 / 5

Unit 6: Dynamic Planet: Plate Tectonics Lecture 3

Earth's Interior. The original surface of the Earth probably looked much as the Moon's surface does today. The Earth was probably composed of the same material from its surface all the way to its center.Objects colliding with Earth helped to cause Earth to grow hot enough that heavy elements such

lilian
Télécharger la présentation

Unit 6: Dynamic Planet: Plate Tectonics Lecture 3

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

    1. Unit 6: Dynamic Planet: Plate Tectonics Lecture 3 Objectives: E3.2C - Describe the differences between oceanic and continental crust (including density, age, composition). E3.r3e - Predict the temperature distribution of the lithosphere as a function of distance from the mid-ocean ridge and how it relates to ocean depth.

    2. Earths Interior

More Related