Unit 11_Geologic Time Lecture_Note Guide

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Northern Kentucky University *

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Geography

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Feb 20, 2024

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This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. Unit 11: Geologic Time Note Guide Objective (Time is time, right?): We’ve established that the Earth is ~4.6 billion years old. But how do we know this? Why is it 4.6 instead of 2.3 or 8.7? Are the methods scientists use reliable? What are those methods? What parts of the Earth are that old? What parts are younger? How can we tell which rocks are old and which rocks are young without dragging a multi-million dollar TIMS, SIMS, or SHRIMP machine out into the field? One of the major steps in our geologic journey is to establish how we read the rock record and determine geologic time. What is geologic time? Geologic time ** The Principle of Uniformitarianism – physical processes that operate in the modern world also operated in the past, at roughly the same rates, and these processes are responsible for forming the geologic features we observe in the world. ** How do we study the past? o Absolute age dating: o Relative age dating: Relative Age Dating 6 major Principles: 1.) The Principle of Superposition
This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. 2.) The Principle of Original Horizontality 3.) The Principle of Lateral Continuity 4.) The Principle of Cross-Cutting Relationships 5.) The Principle of Inclusions 6.) The Principle of Fossil Succession Index fossils Baked Contacts
This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. Unconformities o Angular unconformity: o Nonconformity: o Disconformity: o Paraconformity: Putting it together: Application of Relative Age Dating Principles
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This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. Rock Correlation o Stratigraphic formation o Geologic contact o Stratigraphic Column Absolute Age Dating Geochronology Radiometric Age Dating o Isotopes o Radioactive decay
This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. o Half-life Case Study: Jack Hills formation, Western Australia The Geologic Time Scale A Brief History of Earth The PreCambrian Hadean
This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. Archean Proterozoic
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This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. The Phanerozoic Eon The Paleozoic Era The Mesozoic Era
This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. The Cenozoic Era
This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. Studying This Unit Apply a Critical Thinking strategy to main concepts (characterize the concept – describe what it is; describe the geological significance – why did we talk about it?; describe the geological context – how does it fit into the larger discussion of Earth?) o Main concepts in this unit: The Principle of Uniformitarianism The 6 Relative Age Dating Principles Unconformities The Geologic Time Scale A Brief History of Earth Determine the sequence of events in the diagram below and answer the accompanying questions. This image is courtesy of the CK-12 Foundation (open access resource for academic use). 1. Put the sequence of events in order from oldest to youngest. 2. What relative age dating principle is used to determine the relative age of unit D? 3. What relative age dating principle is used to determine the relative age of unit B?
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This document is the property of the University System of Georgia and is protected by the USG copyright policy. This document is not to be uploaded to any third-party site. Using this document for anything other than educational purposes among students in this course is a violation of the Academic Integrity policies of this course on behalf of the student and a violation of copyright law on behalf of the third-party site. 4. What type of fault is E? 5. If unit C is 201 Ma and unit A is 145 Ma, then what geologic time period does unit B belong to? What geologic era does this period belong to? One of the best ways to study concepts is to put yourself in the professor’s shoes: how would you teach these concepts to someone else? How would you evaluate someone that you taught these concepts to? Write a set of 5 critical thinking and/or direct application test questions for this unit to help you prepare for potential exam questions.