Forces Shaping the Earth

Slides:



Advertisements
Similar presentations
Unit C Chapter 7 Lesson 1 C38 – C45
Advertisements

Forces shaping the earth. Inside the Earth Three layers Core: center of the earth Inner core solid Outer core liquid.
GEOLOGY UNIT REVIEW By Mrs. Susan Dennison
Changes to Earth’s Surface Chapter 9
Mountains,volcanoes, and earthquakes
Unit 1, Section 3 1.  What are the layers of the Earth?  How do Earth’s internal forces change its surface? 2.
Plate Tectonics. Pangea 1912 – Alfred Wegener 1912 – Alfred Wegener Theory: All of the continents Theory: All of the continents were connected as one.
Earth’s Structure Forces on Earth’s Surface Forces Inside Earth
Earth has several layers
 Crust – Rocky surface of the earth  Mantle – A thick layer of rock above the Outer core  Outer Core – Molten lava  Inner Core – Very hot metal.
Chapter 5.  Landform- a physical feature on Earth’s surface.
Bell Ringer Take out a sheet of paper, put your name on it. Write your answer to the questions. 1.What type of tectonic activity made Hawaii? 2.What activity.
The Earth Notes. Water, Land, and Air About 70% of our planet’s surface is water Oceans, lakes, rivers, and other bodies of water make up the hydrosphere.
Volcanoes.
Earth’s Interior and Plate Tectonics Integrated Science Ch 12.
9/11- Geo Engage Write down 3 characteristics of the United States that you enjoy. Think about things that you can do here that you may not be able to.
Journey to the Center of Earth Layers of the Earth Outer Crust Inner Crust Mantle Outer Core Inner Core Crust.
CHAPTER 1 SECTION 1 EARTH’S INTERIOR.
8/26-8/27 Chapter 1, Pgs Most of this is NOT in your book!
FORCES OF CHANGE Chapter 2 Section 2. THINK ABOUT CHANGE…  How has change happening around you influenced your life? How have changes you made within.
The Earth’s Structure. Inside the Earth Age of the Earth- Believed to be 4.6 Billion Years Old! Core: The center of the earth that consists of very hot.
200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300.
Land, Water, and Climate World Geography September 12, 2006.
LandscapesLandscapes Landscape can be thought of as nature’s sculpture of Earth’s surface.
Chapter 2 – A Living Planet Physical Geography The study of the natural aspects of the Earth.
Earth Notes Chapter 2 ~ Section 2 Forces of Change.
1 Hi Guys This term we have 2 more units: Changing Earth Working world For the next 6 weeks it is ‘Changing Earth’
Structure of the Earth & Plate Tectonics. Our Changing Earth The surface of the earth is always changing. What are the two ways in which landform change.
Earth Science 1.2 A View of Earth. Earth’s Major Spheres  Earth is divided into 4 major spheres Hydrosphere Atmosphere Geosphere Biosphere.
Journey to the Center of Earth Layers of the Earth Crust Mantle Outer Core Inner Core.
Internal/External Forces of the Earth. Inner Structure of the Earth 1.Inner Core—dense and solid 2.Outer Core—Molten or liquid Both are mostly hot and.
How Landforms Are Created
Chapter 1 - Lesson 1 Earth’s Landforms How Landforms Came to Be.
Chapter 3 Section 1 The Geosphere.
The Earth and Its Forces Geography2.1. Goals…  Is the Earth’s surface made up of more water or land?  Describe how the Earth’s surface is shaped by.
Chapter 7 Section 1 Pgs Composition of the Earth Divided into 3 layers: Crust Mantle Core Compound – substance made of two or more elements.
How the Layers Formed As earth formed, it was made of hot molten magma and intense gravity. As rocks melted, denser materials sank to the center of the.
L.O.1: To know the structure of the earth. L.O.2: To understand the theories of continental drift and plate tectonics.
Structure of the earth. Inner Core – This is in the centre of the earth where it is hottest. It is solid and consists of Iron and Nickel with temperatures.
Forces Shaping the Earth
Tectonic-plate movement creates landforms
The Earth’s Physical Geography
Chapter 6 Study Guide.
What is the Earth made of?
Plate Tectonics.
landforms mass movement crust weathering erosion mantle inner core
SPHERES OF THE EARTH.
Layers of the Earth, Landforms, and Waterways
Unit D Chapter 1 Lesson 1 Pages D6-D11
Internal/External Forces of the Earth.
Changes to Earth’s Surface Chapter 9
Think about the following questions and be ready to give me an answer when we begin… 1. Why does the earth look the way that it does? 2. Earth vs. people.
EARTH’S STRUCTURE.
Forces of Change Day 3.
Forces Shaping the Earth
Layers of Earth.
The Layers of the Earth!.
The Layers of the Earth.
Earth’s Interior.
BR: D5 Draw a picture of the globe. Then, add and identify the following: The Equator The Prime Meridian The Tropic of Cancer The Tropic of Capricorn The.
The study of the forces that change the Earth’s surface.
Changes Within the Earth
The Earth.
Plate Tectonics The theory that the Earth’s lithosphere is divided into tectonic plates that move around on top of the asthenosphere.
Earth’s Interior.
Earth’s Interior and Plate Tectonics
Chapter 7 Plate Tectonics
Earth’s Interior.
Layers of the Earth Brown Blue.
Inside Earth: Chapter 1 Plate Tectonics.
Presentation transcript:

Forces Shaping the Earth Chapter 1 Day 5 Forces Shaping the Earth

What has made the earth as it is? Mountains, Deserts and other landscapes were formed over millions of years by forces acting below the earths surface. (They are still changing today!)

Inside the Earth Scientists have only been able to actually study the top layer of the Earth. Earth has three layers- the core, the mantle, and the crust. The Earths core is like the center of a cantaloupe where you find the seeds. The mantle is like the part of the fruit you eat. The Crust is like the melons rind.

In the center of the Earth is a dense core out the of hot iron mixed with other metals and rock. The inner core is solid but the outer core is so hot that the metal has melted into liquid.

The Mantle Surrounding the core is the mantle, a layer of rock about 1800 miles thick. Like the core, the mantle also has two parts. The section nearest the core remains solid, but the rock in the outer mantle sometimes melts. This melted rock is called Magma

The Crust The uppermost layer of the Earth, the crust, is relatively thin. This reaches only 31-62 miles deep. The crust is thinnest on the ocean floor.

Forces Beneath the Earths Crust Plate Movement- (Plate Tectonics) This theory states that the crust is not an unbroken shell but consists of plates, or huge slabs of rock, that move. The plates float on top of liquid rock just below the earths crust. Pg. 36 Pangea….

What Happens When Plates Meet? Sometimes through the plates push against each other when this happens one of the three events occurs, depending on what kind of plates are involved. If two continental plates smash into each other the collision produces high mountain ranges. This kind of collision produces the Himilaya in South Asia

If a continental plate and an ocean plate move against each other, the thicker continental plate slides over the thinner ocean plate. The downward force of the lower plate causes molten rock to build up. Then as magma it erupts to form volcanic mountains. The pressure may also cause one plate to move suddenly. The result is an Earthquake.

Undersea Earthquakes can cause huge waves called tsunamis Undersea Earthquakes can cause huge waves called tsunamis. These waves may reach as high as 98 feet. When two plates move alongside each other they create a fault. A fault is a crack in the Earths crust. One of the most famous faults in the United States is the San Andreas Fault in California.

Forces Shaping Landform Weathering is the process of breaking surface rock into boulders, gravel, sand, and soil. Erosion is the process of wearing away or moving weathered material.