Formation of the Universe and Earth’s Interior 1.

Slides:



Advertisements
Similar presentations
Earth’s Layered Structure
Advertisements

Earth’s Interior.
Warm Up 12/4 When does liquefaction occur?
Pg. 25.  After Earth formed, radioactive elements decayed and heat was released  Caused melting of interior  Denser elements sank to core (iron and.
Layers of the Earth. Compositional Layers –Divided by what they are made out of –planetary differentiation – the process of separating out distinct layers.
Earth’s Interior. Contents 1.Evidences of earth’s interior 2.Structure of the earth’s interior.
Journey to the Center of the Earth
Origin of the Universe.
Earth’s Layered Structure
Earth as a System: Earth: A Unique Planet 2.1 and 2.2 Page 27.
Basic Structure of the Earth
Inside the Earth.
Chapter 12 Earth’s Interior
Natural Disasters Earth’s Internal Structure Introduction to Plate Tectonics Earth’s Energy Sources and Systems.
Warm Up 10/21(22) When an earthquake occurs, energy radiates in all directions from its source, which is called the ____. a. fault c. seismic center.
Earth’s Structure and Composition What is geology? What are the characteristics of Earth’s three layers?
Earth's Internal Structure → Layers core mantle crust These are identified using seismic waves p-waves & s-waves.
Nancy Van Wagoner, Acadia University Origin of Earth.
Structure of the Earth. Compositional (Chemical) Layers Crust: Low density High in silicon (Si) and oxygen (O) High in silicon (Si) and oxygen (O) Moho:
Chapter 22.1: The Geosphere Geology = The study of the planet E.’s composition & structure.
The Early Earth “Mr. Montgomery’s Early Earth PowerPoint redefines PowerPoint excellency” - PPTA.
Formation of the Earth In the beginning.
The 4 Earth Sciences. Unique Earth (The blue dot) Earth formed with the birth of our solar system, 4.6 billion years ago. –That’s 4,600,000,000 years.
The 4 Earth Sciences. Geology – Study of the Earth’s surface and interior.
Density and Planetary Differentiation
Star formation (and associated planets) from a nebula.
Inside the Earth Planet Earth All objects on or near Earth are pulled toward Earth’s center by gravity. Earth formed as gravity pulled small particles.

Earth’s Composition.
The Structure of the Earth Internal Structure and Heat.
Earth’s Interior 6th Grade Earth Science Ms. Mudd.
The Earth’s Interior Composed of 4 layers Crust Mantle Outer Core
Earth’s Interior Link for intro animation:
Chapter 12: Earth’s Interior
Chapter 22.1: Earth’s Structure
Philadelphia was the first capital of the United States.
2 The Earth’s Structure series of layers or spheres which differ in density, chemistry (or composition) and physical properties.
Layers of the Earth. The Earth’s Interior Most scientists agree that soon after Earth’s formation, Earth was a large ball of molten (melted) rock. As.
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.
UNIT 1. THE EARTH’S STRUCTURE AND DYNAMICS. THE EARTH’S STRUCTURE.
I. Layers Defined by Composition 8.4 Earth’s Layered Structure  A) Earth’s interior consists of 3 major zones (chemical composition).
The Structure of the Earth
Earth’s Layered Structure. PHENOMENON: What did you observe? What evidence do you have? OBJECTS: Define the system. What objects are interacting? MOTION:
Layers of the Earth The Layers of the Earth are the Inner Core, Outer Core, Mantle and Crust.
Dynamic Earth Ms. Susinno. theory of continental drift In 1915, the German geologist and meteorologist Alfred Wegener first proposed the theory of continental.
Earth’s Interior =mOSpRzW2i_4.
Formation and Structure of the Earth. Standards Recognize that radiometric data indicate that Earth is at least 4 billion years old and that Earth has.
EARTH’S INTERNAL STRUCTURE And processes. What Was Early Earth Like?  Describe what Earth was like right as the Solar System was forming?  Why did earth.
Internal Structure of the Earth Lecture by Dr. Ken Galli, Boston College EESC Environmental Issues and Resources July 7, 2016 Please do not distribute.
Seismicity, Earthquakes & Earth’s Structure. What is an Earthquake? Vibration of the Earth produced by the rapid release of energy. Energy release due.
Learning Objectives I can explain how the solar system formed.
Earthquakes A manifestation of rock deformation
“Window” to the Earth’s Interior
Standard 2 Objective 1 Handout 2
Earth’s Layered Structure
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
What is the earth like inside?
Thursday, 1/29/2015 Objectives: Describe Earth’s interior.
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
Earth’s Layers.
Earth’s Interior Structure
Earth Structure.
Earth’s Interior Chapter 8, pages
Do Now: What is your favorite layered food?
Review Chapter 3 – Earth’s Structure
Earth’s Interior Chapter 8, pages
Mesosaurus: Warm Up: describe what you think this map represents
Dynamic Earth Ms. Susinno.
Earths Interior and Layered Structure
Earth’s Interior Chapter 8, pages
Presentation transcript:

Formation of the Universe and Earth’s Interior 1

Do Now- Think about the following and respond in your journals:  How did the Universe form?  How did early Earth form?  Differentiate the following terms:  Stars  Planets  Sun  Solar system  Galaxy  Universe 2

Big Bang Theory  Inflation & Dark Energy  1929 Edwin Hubble discovered the expansion of the Universe with galaxies moving away from us  This suggested The Universe was born in a single violent event about 14 billion years ago  The Big Bang  Short period of a burst of expansion after the Big Bang  Inflation  Due to an unstable form of energy  Dark Energy  Mathematical models and scientific discoveries support The Big Bang & Inflation Theories  Galaxies are still moving away from Earth

The Earth’s resources were determined when the planet formed. Earth is ~4.6 b.y. old  Formed from gasses (H, He) and cosmic dust  Bombardment of debris from the sun  Early Earth was a hot, molten sphere “magma ocean” that cools from outside-in  Cooling  differentiation into layers based on elemental masses  Heavier elements sank towards center; lighter floated toward the surface…some to the atmosphere  Elements found on earth are as old as the planet; Unevenly distributed  Uneven distribution (concentration in areas) allows us to mine those resources.

Compositional (Chemical) Layers of the Earth  Crust  99% by mass; only 8 elements  O 2, Si, Al, Ca, Mg, Fe, Na, K  50% O 2 ; 25% Si  Silicates (SiO 4 ) Moho- Boundary b/w Crust & Mantle  Mantle  Silicates (SiO 4 )  Primarily Mg, Fe, Ca, Al CMB- Boundary b/w Core & Mantle  Core  Fe-Ni alloy

Physical Layers of the Earth Change in state; Dominated by temperature & pressure  Lithosphere  Brittle solid; Temp  Asthenosphere  Partially molten w/rock; Temp  Mesosphere  Plastic solid; Pressure  Outer core  Liquid; Temp  Inner core  Solid; Pressure There is an interplay of increasing T & P with depth

Layers of the Earth: A Video Recap 7 WwiiOjyfvAU

NOTE to clarify the often incorrect description of mantle: The mantle contains magma in it’s upper region that seeps into the crust and erupts as lava. The mantle itself is a PLASTIC SOLID that behaves as a viscous liquid over geologic time. Therefore, it is the solid mantle that circulates in convection cells, not the magma.

Scale of The Earth’s Layers

Let’s look at the Earths layers…in sing song! *  *Feel free to sing along. This will not adversely affect your grade

Seismic Evidence of Earth’s Layers  Earthquake- energy released by brittle substance (lithosphere);Energy is in the form of waves that radiate  Seismographs & Seismograms  Surface- cause damage at the surface  Body- travel through the Earth  P- Primary; Arrive 1 st ; Compressional (Longitudinal in physics)  S- Secondary; Arrive 2 nd ; Shearing (Transverse in physics)  All waves increase in velocity with increasing density; but s waves can’t penetrate liquids or gasses  Gap between p & s waves tell you how far away the EQ is 12

13 Seismograms generated by seismographs

Evidence for Earth’s internal structure Seen in seismic wave refraction (change in velocity) when traveling from one density layer into a different density layer Seismic waves through undifferentiated planet Seismic waves through differentiated Earth. Animation of seismic waves through undifferentiated and differentiated Earth:

Self-Check: Do you KNOW the Earth’s Interior? You should know the following and be able to give examples where applicable: 1. How did the Earth form? 2. Why did elements become unevenly distributed throughout Earth’s layers? 3. Name & describe the three compositional layers of the Earth % of the Earth’s crust by mass is made up of what 8 elements? 5. How do oceanic and continental crust differ (aside from one being under water)? 6. What are the boundaries that separate the compositional layers and where are they found? 7. Name & describe the five physical layers of the Earth. 8. Explain why the outer core is liquid yet the inner core is solid. 9. Explain “frictional coupling” and identify where it occurs. 10. What data provides the evidence for the Earth’s interior? Explain.