1 / 16

The Changing Earth

The Changing Earth. Chapter Thirteen: Formation of Rocks. 13.1 The Composition of Rocks 13.2 Igneous Rocks 13.3 How Rocks Change. Investigation 13A. Mineral Identification. How are minerals identified?. 13.1 The composition of rocks.

tyler
Télécharger la présentation

The Changing Earth

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. The Changing Earth

  2. Chapter Thirteen: Formation of Rocks • 13.1 The Composition of Rocks • 13.2 Igneous Rocks • 13.3 How Rocks Change

  3. Investigation 13A Mineral Identification • How are minerals identified?

  4. 13.1 The composition of rocks • A rockis a naturally-formed solid made of one or more minerals. minerals rock

  5. 13.1 Rocks are made of minerals • A mineralis a solid, inorganic object with a defined chemical composition. • Minerals have atoms arranged into orderly structures called crystals. This cubic mineral is often placed on food. Can you guess what it is?

  6. 13.1 Rocks are made of minerals • Diamonds and graphite are both minerals that are made of carbon, but their crystalline structures are different.

  7. 13.1 Rocks are made of minerals • There are more than 4,000 minerals on Earth. • The two most abundant elements in Earth’s crust, are oxygen and silicon.

  8. 13.1 Common minerals and cleavage planes • Mica is a rock with its minerals stacked like the pages in a book. • A cleavage planeis a surface along which a mineral cleanly splits.

  9. 13.1 Common minerals and cleavage planes • Feldspar is the most abundant mineral in Earth’s crust. • Like feldspar, hornblende has two cleavage planes.

  10. 13.1 Common minerals and cleavage planes • Quartz is the second most abundant mineral in Earth’s crust. • Unlike feldspar, quartz lacks cleavage planes. • When quartz breaks, it does not split along planes.

  11. 13.1 Mohs hardness scale • Mohs hardness scalewas developed in 1812 by Friedrick Mohs (an Austrian mineral expert) as a method to identify minerals. • This scale uses 10 minerals to represent variations in hardness.

  12. 13.1 Groups of rocks • There are three groups of rocks that are formed by the processed in the Earth’s crust. • An igneous rockforms from the cooling and crystallizing of magma or lava. • A sedimentary rockis made of sediments. • A metamorphic rockis a rock that is formed from another rock because of heat and pressure.

  13. 13.1 Groups of rocks • The rock cycle allows material to keep changing form and moving from place to place on Earth.

More Related