Chapter 8 The Dynamic Planet

Slides:



Advertisements
Similar presentations
MineralsRocksPlate TectonicsEarth quakes Volcanoes
Advertisements

The Living Earth Chapter Nine.
Chapter 1 Minerals: Building Blocks of Rocks. Minerals: Building Blocks of Rocks By definition a mineral is/has Naturally occurring Inorganic solid Ordered.
Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc. Chapter 8 Earth Materials and Plate Tectonics.
Robert W. Christopherson Charlie Thomsen Chapter 11 The Dynamic Planet.
Plate Tectonic Test Review Answers!
Inside Earth Geologists study Earth and the processes that have shaped Earth over time. They study the minerals and rocks that make up Earth, physical.
The Diversity and Cycle of Rocks. Rock Cycle Rock cycle: describes dynamical transformation of rocks between the 3 rock types IGNEOUS, METAMORPHIC, SEDIMENTARY.
CHAPTER 2 Internal Structure of Earth and Plate Tectonics
Robert W. Christopherson Tim Schultz Chapter 11 The Dynamic Planet.
Exam 1 Read chapters 1-4.
The Lithosphere - Tectonics. Geologic Time Scale Figure 8.1.
Introduction to Minerals. Earth Materials Mineral: –Naturally occurring –Solid substance –Orderly crystalline structure –Definite chemical composition.
Chapter 8 The Dynamic Planet
Rocks, Rock Cycle and Layers of the Earth Review
Section 13-1 Review Page #324:1-8.
Minerals: Building Blocks of Rocks Chapter 2
Environmental Geology APES MS LC. Objective 16.1 Understand some basic geologic principles including how tectonic plate movements affect conditions for.
Quiz Question Do you expect that the earthquake in Hawaii was: –Tensionsal (pull-apart movement) –Compressional (push-together movement) –Shear (moving-past.
The Changing Earth Chapter Thirteen: Formation of Rocks 13.1 The Composition of Rocks 13.2 Igneous Rocks 13.3 How Rocks Change.
 Students will know core vocabulary pertaining to minerals.
Earth’s Core By: Diego Gonzalez.
Chapter 1 Minerals: Building Blocks of Rocks
Chapter 1 Earth’s Structure
UNIT SIX: Earth’s Structure  Chapter 18 Earth’s History and Rocks  Chapter 19 Changing Earth  Chapter 20 Earthquakes and Volcanoes.
Geological background 88 elements found in the Earth's crust -- of these, only 8 make up 98%: oxygen, silicon, aluminum, iron, calcium, magnesium, potassium.
Journey to the Center of Earth
The Theory of Plate Tectonics. Earth’s Internal Layers The crust varies in thickness (4-60 km) oxygen, silicon, magnesium and iron The mantle (2885 km)
Processes that shape the planet.. Earth’s Internal Layers The crust (oxygen, silicon, magnesium and iron) The mantle (silicon & oxygen) Outer core (iron.
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 1 Minerals: Building Blocks of Rocks. Minerals: Building Blocks of Rocks By definition a mineral is/has Naturally occurring Inorganic solid Ordered.
 Composition: Silicon, Oxygen, and Aluminum  Types: › Continental Crust: solid & rocky outer layer › Oceanic Crust: thin & dense material.
Earth’s Interior and the Rock Cycle. Earth’s Interior Four Layers Each has a different composition and density (mass/volume).
Rocks and Minerals 4 September 2015.
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.
Integrated Coordinated Science End of Year Review.
Chapter 8 Earth Systems and Resources. Creation of the Earth Earth’s resources are finite and were determined when the planet formed.
Robert W. Christopherson Charlie Thomsen Chapter 11 The Dynamic Planet.
Chapter 11 The Dynamic Planet Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen.
The Earth and it’s layers
Unit 2: Study Guide.
Introduction to Geology, Various Rx and Minerals.
Evidence for Plate Tectonics. Earth’s Interior  By composition  core - Fe & Ni  mantle  crust  By composition  core - Fe & Ni  mantle  crust lithosphere.
The Earth’s Interior Composed of 4 layers Crust Mantle Outer Core
Chapter 1 Minerals: Building Blocks of Rocks
EARTH EDITION Miscellaneous Rocks Minerals Plate Boundaries
Inside Earth Chapter 5 Rocks
Minerals Earthquakes Earth’s Layers Rock Cycle Plate.
Study Guide 6-1 Earth’s Structure.
Jeopardy RocksMineralsPlate Tectonics Plate Tectonics 2 EQs & Volcanoes Q $100 Q $200 Q $300 Q $400 Q $500 Q $100 Q $200 Q $300 Q $400 Q $500 Final Jeopardy.
The Rock Cycle Thinking about relationships among the major rock groups.
Unit II Rocks and Minerals. Earth’s Interior Our Earth consists of four main layers.
Chapter 22 Earth’s Interior
Dynamic Earth Earth Science Jeopardy Layers of Earth Tectonic.
UNIT SIX: Earth’s Structure
Jeopardy Rocks Minerals Plate Tectonics EQs & Volcanoes Q $100 Q $100
Chapter 4.
Navo middle school science
Plate Boundaries Convergent plate boundaries (destructive margins)
AP Environmental Science New England Geology
The Modern Plates.
Integrated Science C Mrs. Brostrom
Plate tectonics.
Minerals: Building Blocks of Rocks
Chapter 8 Earth Systems Friedland and Relyea Environmental Science for AP®, second edition ©2015 W.H. Freeman and Company/BFW AP® is a trademark registered.
Physical Geology Composition of materials, tectonic cycle, Formation and identification of rock types.
Chapter 8 Earth Systems Friedland and Relyea Environmental Science for AP®, second edition ©2015 W.H. Freeman and Company/BFW AP® is a trademark registered.
The Earth presented by Prof. Geller 29 October 2002
Minerals. Minerals Rocks Plate Tectonics Earthquakes.
Presentation transcript:

Chapter 8 The Dynamic Planet Elemental Geosystems 5e Robert W. Christopherson Charles E. Thomsen

The Dynamic Planet The Pace of Change Earth’s Structure and Internal Energy   The Geologic Cycle     Plate Tectonics  

The Pace of Change   Geologic Time Scale Uniformitarianism

Geologic Time Scale Figure 8.1

Earth’s Structure and Internal Energy Earth in Cross Section Earth’s core   Earth’s magnetism Earth’s mantle   Lithosphere and crust  

Earth in Cross Section Figure 8.2

Earth’s Interior Figure 8.2

Earth’s Interior Figure 8.2

Earth’s Interior Figure 8.2

Core to Crust Figure 8.3

Isostatic Adjustment Figure 8.4

The Geologic Cycle The Rock Cycle Igneous processes Sedimentary processes   Metamorphic processes  

The Geologic Cycle Figure 8.5

Minerals: Building Blocks of Rocks By definition a mineral is/has Naturally occurring Inorganic solid Ordered internal molecular structure Definite chemical composition Rock A solid aggregate of minerals

Cubic Crystals of Pyrite Figure 1.7 A

Elemental Abundances in Continental Crust Figure 1.14

Mineral Groups Silicates Most important mineral group Comprise most rock-forming minerals Very abundant due to large % of silicon and oxygen in Earth’s crust Silicon-oxygen tetrahedron Fundamental building block Four oxygen ions surrounding a much smaller silicon ion

Table 1.1

Quartz (SiO2) Exhibits a Variety of Colors

The Rock Cycle Figure 8.6

Igneous Rock Types Figure 8.7

Intrusive and Extrusive Rocks Figure 8.8

Course-Grained Igneous Texture Figure 2.4 B

Sedimentary Rock Types Figure 8.9

Metamorphic Rocks Figure 8.12

Plate Tectonics A Brief History Sea-Floor Spreading and Production of New Crust   Subduction of the Crust   The Formation and Breakup of Pangaea   Plate Boundaries   Earthquake and Volcanic Activity   Hot Spots

Crustal Movements Figure 8.13

Continents Adrift Figure 8.15

Magnetic Reversals Figure 8.14

Ocean Floor Figure 8.17

Earth’s Major Plates Figure 8.16

Earthquakes and Volcanoes Figure 8.18

Hot Spot Tracks Figure 8.19

Elemental Geosystems 5e End of Chapter 8 Elemental Geosystems 5e Robert W. Christopherson Charles E. Thomsen