The Rock Record: Determining Relative Age Chapter 8

Slides:



Advertisements
Similar presentations
Determining Relative Age
Advertisements

GEOLOGIC HISTORY THE RULES OF THE GAME
The relative age of rocks and geological events.
RELATIVE TIME: When the age of rock is compared to the ages of other rocks or events in geological time. Can determine which layers are older than others.
Relative Time: Ages of events are placed in order of occurrence.
Unit 5: Age of the Earth Objective:
Ch 8 Review Jeopardy Unconformi ties Half Lives Laws Relative/ Absolute Age Fossils
Earth’s Story 6.1 & James Hutton Theory of the Earth Uniformitarianism.
Discovering Earth’s History
Bell Ringer What is the theory of evolution? How do fossil records prove this theory? Give two examples of animal fossils found that give evidence to support.
Earth’s History.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix.
Geologic Time Earth’s History.
Key Ideas State the principle of uniformitarianism.
Chapter 8 Section 1 Page 190 #’s 1-6
Relative Dating of Strata. Relative Dating Determining relative ages of rocks or strata compared to another rock or strata. Can say which layer is older.
WELCOME TO CLASS. Agenda TODAY Sequencing Time Rock Record Notes Relative Age activity Hand back tests NEXT TIME Absolute age lab Geologic Time QUIZ.
Discovering Earth’s History Rocks Record Earth’s History 1. Rocks record geological events and changing life forms of the past. 2.Scientists have learned.
Geology Review Game Ready your Mind!. Your teams are your table groups.
Interpreting Earth’s Rocks to Determine Its Past History.
Interpreting Earth’s Rocks to Determine Its Past History.
Dating Rocks Ways to tell the age of a rock. What are relative and absolute Locations?
Determining Relative Age The beginning of modern geology.
We know Earth is 4.6 Billion years old
21.2 – Relative Age Dating How can you tell if one rock layer is older than another? How can you tell if one fossil is older than another? What is an index.
The Rock Record Section 1 Section 1: Determining Relative Age Preview Objectives Uniformitarianism Relative Age Law of Superposition Principle of Original.
Ch. 13 Section 2 Relative Ages of Rocks.
James Hutton proposed the principle of uniformitarianism. This states that the processes occurring on Earth today, have been occurring since Earth first.
Determining geological ages
Stratigraphy Stratigraphy is the branch of geology that deals with the arrangement of rocks in layers.
Relative Time: Ages of events are placed in order of occurrence. No exact date is identified.  Ex. WWI and WWII  Ex. I am the second child in my family.
A Little Bit of History … The history of geologic time begins with the human interest in mining. Interests in rock units began to flourish with commercial.
relative time vs. absolute time
CHAPTER 8-THE ROCK RECORD GRAND CANYON VIDEO GRAND CANYON VIDEO How can we determine ages of rocks and the Earth?
GEOLOGICAL TIME. GEOLOGY NEEDS A TIME SCALE An investigation of the history of Earth Understanding how features of landscape developed and formed Reconstructing.
Geologic History Relative Dating. Birth of Modern Geology Began in the late 1700’s when James Hutton published his Theory of the Earth. He was the first.
Earth’s History How do we know about it?. What is Uniformitarianism? Uniformitarianism: –Is a theory developed by the Scottish geologist, James Hutton,
Chapter 8 Section 1 Pages #’s 1-4 Determining Relative Age.
May 13, 2014 Open up your ISN. Call the next available left side page #84. Title the page “Vocabulary”. Call the following page #85. Title the page “The.
Geology 101 David Brown. James Hutton ( CE) Scottish geologist Scottish geologist Developed the laws of geology Developed the laws of geology.
Uniformitarianism: the processes that act on the Earth’s surface today are the same as the processes that have acted on the Earth’s surface in the past.
Geologic Time. Rocks Record Earth History Rocks record geological events and changing life forms of the past. We have learned that Earth is much older.
The Rock Record Section 1 Section 1: Determining Relative Age Preview Objectives Uniformitarianism Relative Age Law of Superposition Principle of Original.
Interpreting Earth’s Rocks to Determine Its Past History.
Catastrophism vs Uniformitarianism and Relative Age Dating
Earth’s History Introduction: The earth is about 4.6 billion years old. Much of its history is recorded in the rock. Observations of fossils, rock types,
The Rock and Fossil Record II. Relative Dating: Which Came First?
Geologic time Relative dating
21.2 – Relative Age Dating. Interpreting Geology James Hutton, a Scottish geologist who lived in the late 1700s Attempted to explain Earth ’ s history.
“WHO DUNIT?” Activity With your Table Partner, quietly read the case and the list of suspects, examine the evidence, and on your note page…. 1. Name the.
Unit 5: Age of the Earth Objective:
Discovering Earth’s History
Earth History- Table of Contents
Relative Age Quiz.
EARTH’S HISTORY Relative Dating.
Unit 2: Relative Dating - Part 2
Geologic Time Uniformitarianism vs. Catastrophism.
Relative Dating.
Relative Dating.
Discovering Earth’s History
Determining Relative Age
Interpreting Earth’s Rocks to Determine Its Past History
Age of the Earth Objective:
Geologic History Relative Dating.
Relative Dating.
EARTH AND SPACE SCIENCE
Relative Age of Rocks Activity
Chapter 8 section 1 RELATIVE AGE.
Geologic Time.
A Look Back in Geologic Time
Presentation transcript:

The Rock Record: Determining Relative Age Chapter 8

Rocks Tell a Story!!!

How do we know what happened? Relative Dating – tells which one is older, not actual age Absolute Dating – actual age

Determining Relative Age James Hutton discovered that the present is the key to the past. Principle of Uniformitarianism:

Layers of rock called strata tell the story of what came first. A relative age (older vs. younger) can be determined with a few simple laws.

Law of Original Horizontality Sedimentary rocks left undisturbed will remain in horizontal layers.

Law of Inclusions Rock fragments (in another rock) must be older than the rock containing the fragments.

...granite is older. ...sandstone is older.

Law of Crosscutting Relationships A fault or an intrusion is always younger than the rock layers it cuts through.

UNCONFORMITIES Gaps in the geologic record when deposition stopped, rock was eroded away, and then deposition restarted. There are 3 types: 1. Angular Unconformity 2. Disconformity 3. Nonconformity

Angular Unconformity Boundary between a tilted layer and a horizontal layer

Disconformity Nearly horizontal Boundary between layers of rock that have not been deposited continuously A large time gap exists.

Nonconformity Boundary where stratified (layered) rock rests on unstratified rock

Possible Solution 1. Deposition of shale 2 Possible Solution 1. Deposition of shale 2. Deposition of conglomerate 3. Deposition of sandstone 4. Deposition of lithic sandstone 5. Deposition of limestone 6. Deposition of quartz sandstone 7. Deposition of limey shale 8. Deposition of mudstone 9. Intrusion of granite. This may have occurred earlier. However, as granites are emplaced at depth, it is assumed all the sequence was deposited and lithofied prior to emplacement. 10. Uplift and erosion to form current land surface. 11. Deposition of alluvium

Possible Solution 1. Deposition of conglomerate 2 Possible Solution 1. Deposition of conglomerate 2. Deposition of sandstone 3. Deposition of limestone 4. Deposition of shale 5. Deposition of mudstone 6. Faulting 7. Intrusion of gabbro

Possible Solution 1. Deposition of Quarry Shale 2 Possible Solution 1. Deposition of Quarry Shale 2. Deposition of Cave Bluff Limestone 3. Deposition of Redin Sandstone 4. Deposition of Tinely Ashstone 5. Deposition of Clipton Volcanics 6. Folding 7. Intrusion of basalt dyke 8. Faulting

Possible Solution 1. Deposition of Davin Shale 2 Possible Solution 1. Deposition of Davin Shale 2. Deposition of Hutt Ashstone 3. Deposition of Cabin Limestone 4. Deposition of Lower Coal Seam 5. Deposition of Ravin Sandstone 6. Deposition of Blackman Shale 7. Deposition of Fossil Bed Limestone 8. Folding 9. Uplift and erosion (forming unconformity surface) 10. Deposition of Basin Conglomerate 11. Deposition of Log Creek Mudstone 12. Deposition of Loren Shale 13. Deposition of Jackson Sandstone 14. Intrusion of basalt dyke 15. Tilting 16. Erosion to form present landscape.