1 / 8

Lesson 1 - Earth’s Interior

Lesson 1 - Earth’s Interior . Chapter 1 – Inside Earth . Geologists have used two main types of evidence to learn about Earth’s interior: direct evidence from rock samples and indirect evidence from seismic waves. Rocks from inside Earth give geologists clues about Earth’s structure.

bryga
Download Presentation

Lesson 1 - Earth’s Interior

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. Lesson 1 - Earth’s Interior Chapter 1 – Inside Earth

  2. Geologists have used two main types of evidence to learn about Earth’s interior: direct evidence from rock samples and indirect evidence from seismic waves. • Rocks from inside Earth give geologists clues about Earth’s structure. • To study Earth’s interior, geologists also study seismic waves. When earthquakes occur, they produce seismic waves and the paths they take reveal the structure of the planet. Exploring Inside Earth

  3. Using data from seismic waves, geologists have learned that Earth’s interior is made up of several layers. Similar to an onion. • The three main layers of Earth are the crust, the mantle, and the core. These layers vary greatly in size, composition, temperature and pressure.

  4. The high temperatures inside Earth are the result of heat left over from the formation of the planet. In addition, radioactive substances inside Earth release energy. • This further heats the interior. • Pressure results from a force pressing on an area. Pressure inside Earth increases as you go deeper. The deeper you go, the greater the pressure. Temperature & Pressure

  5. The crust is a layer of solid rock that includes both dry land and the ocean floor. • The crust beneath the ocean floor is called the oceanic crust. Oceanic crust consists mostly of rocks such as basalt. • Basalt is a dark rock with a fine texture. • Continental crust forms the continents and consists mainly of rocks such as granite. Granite is light in color and has a coarse texture. The Crust

  6. Earth’s mantle is made up of rock that is very hot, but solid. Scientists divide the mantle into layers based on the physical characteristics of those layers. Overall, the mantle is nearly 3,000 kilometers thick. • Lithosphere • Asthenosphere • The Lower Mantle The Mantle

  7. The core is made mostly of the metals iron and nickel. It consists of two parts – a liquid outer core and a solid inner core. • The outer core is a layer of molten metal that surrounds the inner core. • The inner core is a dense ball of solid metal. • The movements in the liquid outer core creates Earth’s magnetic field. Earth acts like a giant bar magnet. The Core

More Related