Earth’s Interior.   The earlier views of the earth’s processes were viewed by the catastrophic events, and related to gods.  Poseidon was the god of.

Slides:



Advertisements
Similar presentations
The Importance of Earth’s Interior Heat Engine The Core.
Advertisements

Chapter 17 Earth’s interior. Earth’s interior structure Earth is composed of three shells; –Crust –Mantle –Core.
EARTH’S INTERIOR.
Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure.
Chapter 17 Earth’s Interior and Geophysical Properties
Chapter 2 Earth’s Interior
Earth’s Structure Earth is not Jupiter. Introduction We have explored outer space much more extensively than we have explored the inside of our own planet.
How Minerals Form?
How do we know? Rock Samples Seismic Waves 2 ways –Rock Samples –Seismic Waves Holes in the earth up to 12.3 km (7.6 miles) –Brings samples –Gives clues.
Inside the Earth.  At earth’s center is the inner core.  The inner core is composed of nickel and iron in solid form.  The depth from the surface is.
Seismic waves- Earthquake waves travel differently as they move through different materials Through some materials they move straight, while others will.
Earth’s Layered Structure
Catastrophe student summary Evacuate QUESTIONS I can answer…Evidence Scientists work in labs and wear white coats, don’t they? Are teams better than individuals?
IINTRUSIVE VOLCANIC FEATURES
Chapter 3 – Section 2 Igneous Rocks Open your books to page 62 AND take notes over the yellow slides!
Basic Structure of the Earth
Chapter 1 Earth’s Structure
Bellringer List the four layers of Earth, starting with the innermost and moving outward.
-Rocks from inside Earth give geologists clues about earths structure. -This is direct evidence. Something you can physically observe. Geologists.
5 minute thinker… What’s the first thing you think of when you hear the word “Earth”? Write it on your construction paper square as a hashtag. Example:
Intrusive Igneous Activity Plutons result from the cooling and hardening of magma within the earth Exposed at surface after uplift and erosion Pluton refers.
Earth’s Interior p Chapter 5.1 Exploring inside the Earth Since we cannot travel deep inside the Earth scientist use evidence to learn about.
Warm Up 11/18 The broad, slightly dome-shaped volcanoes of Hawaii are ____. a. cinder cone volcanoes c. pyroclastic volcanoes b. composite cone volcanoes d.
Earth’s Interior Earth Science PowerPoint By Mr. Whitmyer.
LAYERS OF THE EARTH Structures of the EARTH By: Adreana Thompson & Victoria Wright.
Chapter 1 book f pg. 6 week 3 of term 2.  Earths surface is constantly changing. It has been lifted up, pushed down, bent, broken, melted and turned.
Earth’s Interior. The Earth’s Core Much of the information scientists have about the Earth’s interior has come not only from complex instruments but also.
Earth’s Interior Chapter 5 Section 1.
Studying Earth’s History. UNIT 7 STUDY GUIDE.  Due to continental drift, tectonic plates move causes Earth’s surface to change. Some effects of this.
The Layers of the Earth © Copyright 2006.  M. J. Krech. All rights reserved.
Chapter Unit F: Plate Tectonics. Layers of the Earth 17.1 The three main layers that make up Earth are -The crust -Mantle -Core The crust is up.
A naturally occurring solid made of minerals or mineral like matter Means that a rock can be made of many minerals or just one mineral. Every mineral is.
Earth’s Structure and Materials
Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure.
Earth’s Interior 6th Grade Earth Science Ms. Mudd.
Earth’s Moving Plates Mr. Perez.
Rocks. Igneous Rock Origin: Magma from within the Earth cools to form igneous rock. Extrusive: Magma that reaches the surface, becomes lava and cools.
EARTH’S INTERIOR. Earth’s Interior Geologists have used two main types of evidence to learn about Earth’s interior: –Direct evidence from rock samples.
The Rock Cycle. Anywhere on Earth…  You may observe processes (such as earthquakes and volcanoes ) changing Earth’s landforms because of processes inside.
Earth’s Interior Earth’s surface has been lifted up, pushed down, bent, and broken therefore it looks much different today than it did millions of years.
BELLWORK: HOW DO GEOLOGISTS LEARN ABOUT EARTH’S INTERIOR?
Earth’s Structure. Introduction We have explored outer space much more extensively than we have explored the inside of our own planet. Why haven’t we.
Earth’s Layers G 103. General Information -Iron,Oxyge, Silicon, & Magnesium - Deepest drill 12 km -Radius of Earth 6371 km - How do we know about the.
TEMPERATURE  The deeper you go, the hotter it gets. & Celsius 4,000° C 4,000 km 2,000 km & kilometers 5,000° C 6,000 km F F mi.
Earth's Interior Summarize the three layers of Earth- crust, mantle, core- on the basis of relative position, density, and composition.
3.1 – Earth’s Interior  Essential Questions: 1. How Do Geologists Learn About Earth’s Interior? 2. What Are the Features of Earth’s Crust, Mantle, and.
Could you watch an island grow? The islands of Hawaii.
Earth’s Interior “Seeing into the Earth”
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
The Layers of the Earth.
7-1 Inside the Earth.
Inside the Earth Earth’s Structure
Chapter 2 Earth’s Interior
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
Chapter 3 Introducing Earth
7-1 Inside the Earth.
Rock A naturally occurring solid made of minerals or mineral like matter Means that a rock can be made of many minerals or just one mineral. Every mineral.
Earth’s Interior Notes.
Today’s Warm-Up Friday, January 10
Earth’s Materials and Processes-Part 8 Investigating Earth’s Interior
Earth Layers and Types of Crust
Earth’s Interior Notes.
Earth’s Interior.
How Do Geologists Learn About Earth’s Interior?
Bell Ringer 1. What physical layer of the Earth makes up all of the crust and the very upper portion of the mantle? 2. The core can be broken up into.
Earth’s Interior.
7-1 Inside the Earth.
Bellringer 8/15/16 What lies on the Earth’s crust? What are the two types?
Earth’s Interior Chapter 5 Section 1.
Earth’s Interior.
Presentation transcript:

Earth’s Interior

  The earlier views of the earth’s processes were viewed by the catastrophic events, and related to gods.  Poseidon was the god of earthquakes  Zeus was the weather god  Vulcan was the god of volcanoes  Earth’s interior was the house of Hades Historical Views

  It has become determined that the earth is an oblique spheroid.  It processes a dipolar magnetic field.  The Earth has a crust with an interior that is composed of different layers  The interior core has a source of heat. Over Time

  The direct evidence of what lies below our feet is quite limited.  Direct evidence refers to actual sample of Earth materials from which composition and density of a certain area of the Earth’s interior can be determined.  The sources  Drilling  Inclusions in igneous rocks  Roots of mountains  Kimberlite pipes The Evidence

  Diamond drill bits have been bored into rock and the cores have been brought to the earth surface.  This technique is limited as the material of the Earth increases in temperature with depth, (called a geothermal gradient) approximately 25ºC per kilometer.  Deepest drill hole to date is 12 km deep, located north of the Arctic Circle in Russia Drilling

  During magmas’ travel to the Earth’s surface pieces of country rock, called inclusions.  With uplifting and erosion at the Earth’s surface the inclusion can provide information about the composition of the Earth at the depth the magma originated Inclusions

  Think of mountain being like an iceberg. To have a high elevation a deep portion or root is needed to balance the structure.  As a mountain erodes over time the deep root of the mountain becomes uplifted and the root is exposed giving direct information about the interior. These depths can be up to 50km Mountain Roots

  Kimberlite pipes are a special intrusive igneous rock formation which develop at great depths (around 600 km) below the surface. These then move upward to the surface.  They are sources of most of the world’s natural diamonds, but they also give clues as to the Earth’s interior. Kimberlite Pipes

 Kimberlite Pipe

  One must remember that the Earth’s radius is over 6300 km, and with direct methods of evidence only going to a depth of maybe 600 km, then much information about the interior is lacking.  To gather the information needed about the interior, indirect methods must be used. Of these most commonly used is seismology. The study of earthquakes Overal