Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,

Slides:



Advertisements
Similar presentations
Earthquakes.
Advertisements

What is an Earthquake? Chapter 8, Section 1.
Chapter 12 Earthquakes.
Forces in the Earth’s Crust Earth Comm: Understanding Your Environment, pages Earth and Space Science.
Structural Geology Crustal Deformation
Crustal Deformation Earth, 10e - Chapter 10
Prentice Hall EARTH SCIENCE
11.1 Mountain Building : Forces in Earth’s Crust
Inuksuk - Nunavut, Canada
Distribution of Microcracks in Rocks Uniform As in igneous rocks where microcrack density is not related to local structures but rather to a pervasive.
Ch – Forces Within Earth Essential Questions
EARTHQUAKES.
Earthquakes.  Natural vibrations of the ground caused by movement at faults  Faults: Fracture in the Earth’s crust Faults form when rocks break deep.
Lecture-11 1 Lecture #11- Faults and Faulting. Lecture-11 2 Faults Bound the Major Plates.
Dynamic Earth Class February 2005.
Rock Deformation and Geologic Structures
What Are Earthquakes? 7-1 Key Concept:
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
GSC 1530 Chapter 10 Crustal Deformation.
Mountains Chapter 9. Stress and Strain Stress is defined as force per unit area. It has the same units as pressure, and in fact pressure is one special.
Mountains and Mountain Building: Chapter 11. Rock Deformation Deformation is a general term that refers to a change in size or shape of rocks in the earth's.
Rock Deformation Chapter 11, Section 1.
Section 1: How Rock Deforms
 Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.
Crustal Deformation Structural Geology
Unit 1.4 Earthquakes. Where do earthquakes Occur? Earthquakes can occur near the Earth’s surface or far below the surface. Most earthquakes occur at plate.
Section 19.1 Forces Within Earth
Rock Deformation-Structural Geology
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Crust Deformation: Forces, Faults and Folds. Deformation The bending, tilting, and breaking of the earth’s crust major cause of deformation = plate tectonics.
Mountain Building Chapter 11 September 29, Complete the following using Ch. 11 of your textbook (page 308) on your warm up doc: – Define deformation.
Chapter 19.  Most Earthquakes are the result of movement in the Earth’s crust at the tectonic plates.  Rocks in the crust resist movement and build.
Geologic Structure.
Mountain Building Chapter 11 February 28, Announcements Vocabulary for Chapters 9 and 11 is due on TODAY! TEST next Tuesday!
7-4c pgs IN: List and describe the 3 types of rock folding. Put your Worksheet on the box.
Section Review 12-1 Page #300: #1 Describe elastic rebound. The sudden return of deformed rock back.
Chapter 19 - Earthquakes.
Chapter 12, Section 1 Chapter 10, Section 2 Objective 1
1 Folds, Faults and the Deformation of Earth’s Crust Cockscomb structure in Utah.
QUIZ 10/21 1.What are Earthquakes? 2._____ is the deformation of a material caused by stress. 3.Describe tension stress. 4.Faulting causes rock to _________.
Guided Notes for Forces Within Earth
Chapter 19 - Earthquakes Forces within Earth.
Chapter 19 Pg. 526 Earthquakes.
11 CHAPTER 11 Mountain Building. Factors Affecting Deformation 11.1 ROCK DEFORMATION  Factors that influence the strength of a rock and how it will deform.
Chapter 5 section 1 Objective: Determine where earthquakes come from and what causes them Identify different types of earthquakes Describe how earthquakes.
Rock Deformation rock deforms (changes shape) because of stress put on the rock stress is a force that acts on a body (rock in this case) differential.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 3 Earth’s Materials Reference: Chapters 2, 3, 6,
Mountain Building Orogenesis – factors that produce a mountain belt.
Unit 4 Lesson 5 Earthquakes Copyright © Houghton Mifflin Harcourt Publishing Company.
Earthquakes: Earth’s Way of Releasing Stress Chapter 8: Earthquakes.
Earthquakes. earthquakes Earthquakes are natural vibrations of the ground caused by movement along gigantic fractures in Earth’s crust or by volcanic.
Forces In Mountain Building
Mountain Building Folding and Faulting. Stress in the Crust Stress from plate motions causes crustal rocks to deform –Rocks near the surface are cool.
Folds, Faults and the Deformation of Earth’s Crust
11.1 Rock Deformation Factors Affecting Deformation
TOPIC 1:TECTONIC PROCESSES AND HAZARDS
Chapter 7.
Section 1: Forces Within Earth
Let’s Focus What is an earthquake?
What is the Great Shake Out?
Chapter 11.1 Rock Deformation.
Chapter 11: Mountain Building
11.1 – Rock Deformation.
Section 1: Forces Within Earth
Mountain Building Earth Science Ch. 11.
Title: 19.1 Forces Within Earth Page #: Date: 6/6/2013
Mountain construction and destruction
EARTHQUAKES Chapter 16 pg. 426.
Mountains and Mountain Building: Chapter 11
Presentation transcript:

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4, 15, 16, 19; Appendix A & B

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Forces and Factors that affect Deformation Unit 4: Topic 3.1 Focus on...  defining crustal deformation, force, and stress.  outlining and describing three types of deformation.  identifying and describing the forces that cause deformation.  identifying and describing the factors that affect deformation.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Terminology associated with Crustal Deformation: Crustal Deformation is associated with Internal Forces within Earth! Crustal Deformation  General term that refers to all changes that occur to the original form and/or size of a rock body.  It may also produce changes in the location and orientation of rocks.  Most crustal deformation occurs along plate tectonic margins.  Plate motions and the interactions along plate boundaries generate tectonic forces that cause rock units to deform.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Terminology associated with Crustal Deformation: Force  anything that tends to put stationary objects in motion or change the motion of moving bodies. Stress  is defined as the amount of force applied to a given area.  Two types of stress; 1) Uniform – equal stress in all directions. 2) Differential – varying stress in different directions. Strain  causes an irreversible change in the shape and size of a rock body. Original configuration is not retained during deformation.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Types of Crustal Deformation: Differential Stresses: Compressional  stresses that shorten a rock body are compressional in nature Tensional  stresses that elongate a rock body Shear  stresses that cause sections of a rock body or two separate rock bodies to slide past one another

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Types of Crustal Deformation:  When rocks are subjected to stresses greater than their own strength, they begin to deform, usually by folding, flowing, or fracturing. 3 types of deformation: 1)Elastic Deformation - recoverable 2)Brittle Deformation - permanent 3)Ductile Deformation - permanent

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Types of Crustal Deformation: 3 types of deformation: 1)Elastic Deformation  stress is applied gradually and when the stress is removed the rock will return to nearly its original size and shape.  elastic deformation is recoverable after stressing.  earthquakes result from stored elastic energy.  once the elastic limit is reached it either flows (ductile) or fractures (brittle).

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Types of Crustal Deformation: 3 types of deformation: 2)Brittle Deformation  stress is applied gradually and when the rocks strength is exceeded the rock will behave like a brittle solid where it will fracture and the rock will not return to its original size and shape.  occurs near the surface where temperature and confining pressures are lower.  brittle deformation is permanent.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Types of Crustal Deformation: 3 types of deformation: 3)Ductile Deformation  stress is applied gradually and when the rocks strength is exceeded the rock will flow in solid state and produce a change in the original size and shape without fracturing.  occurs at great depths beneath Earth’s surface where temperature and confining pressures are higher.  ductile deformation is permanent.  An example would be similar to a penny placed on a railway track and flattened by a passing train. Metal is permanently changed.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Factors that Affect Crustal Deformation:  The factors that influence the strength of a rock and thus how it will deform include; 1)Temperature 2)Confining Pressure 3)Rock Type 4)Time

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Factors that Affect Crustal Deformation:  The factors that influence the strength of a rock and thus how it will deform include; 1)Temperature  the colder the Earth materials, the more brittle the deformation will be.  the warmer the Earth materials, the more elastic or ductile the deformation will be.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Factors that Affect Crustal Deformation:  The factors that influence the strength of a rock and thus how it will deform include; 2)Confining Pressure  confining pressure will only result in elastic or ductile deformation at varied depths beneath Earth’s surface.  brittle deformation typically occurs on the surface when there is no confining pressure from above.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Factors that Affect Crustal Deformation:  The factors that influence the strength of a rock and thus how it will deform include; 3)Rock Type  all rock types can be deformed.  however, sedimentary rocks could be more easily deformed since they are softer.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Factors that Affect Crustal Deformation:  The factors that influence the strength of a rock and thus how it will deform include; 4)Time  rapid deformation tends to result in brittle deformation.  slower deformation over longer periods of time tends to result in elastic or ductile deformation.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Example 1: Which factors would cause a rock to deform by brittle deformation ? TimeTemperature (A) ShorterColder (B) ShorterWarmer (C) LongerColder (D) Longer Warmer

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Example 2: Which type of stress and faulting occurs at divergent plate boundaries? StressFaulting (A) shearnormal (B) shearreverse (C) tensionnormal (D) tensionreverse

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Your Turn... Take the time and complete the following questions... (Solutions to follow) Question: Which rock type is most easily deformed by stresses in Earth’s crust? (A)igneous plutonic (B)igneous volcanic (C)metamorphic (D)sedimentary

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Solutions... Question: Which rock type is most easily deformed by stresses in Earth’s crust? (A)igneous plutonic (B)igneous volcanic (C)metamorphic (D)sedimentary

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Summary... Overview of Points covered:  Crustal deformation is a direct result of stresses put on rocks.  3 types of stress include; 1) Tensional, 2) Compressional, 3) Shear  3 types of crustal deformation include; 1) Elastic, 2) Brittle, 3) Ductile  Factors affecting crustal deformation include; 1) Temperature, 2) Confining Pressure, 3) Rock Type, 4) Time