Fossils and Dating 8-2 notes. What you will learn: The rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers,

Slides:



Advertisements
Similar presentations
Relative and Absolute Age Law of Superposition
Advertisements

Who’s First? What is relative dating?
Unit 2 Lesson 2 Relative Dating
Unit 2 Lesson 2 Relative Dating
Age Dating of Rocks.
Relative and Absolute Dating
Relative Dating : Which Came First?
Sci. 3-2 Relative Dating: Which Came First?
Use answer key to make correction to p. 2 in binder
Chapter 8.  itarianism  A principle that geologic processes that occurred in the past can be explained by current geologic processes.  Volcanism and.
Unit 5: Age of the Earth Objective:
ESS 8.4 Earth’s History.
Finding the Relative age of Rocks
Earth’s History.
Relative Time.
Dating Rock Layers.
Law of Superposition Chapter 8 Lesson 2.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix.
RELATIVE DATING: WHICH CAME FIRST? Brainstorm Questions 1.Why do think the Grand Canyon looks the way it does? 2. Which layers of rock are the oldest?
Absolute vs. Relative Dating of Rocks
Relative Dating By: Thomas Cardona, Cameron Carpenter, Cielo Ruvalcaba, Madison Gasper, Caroline Kelsey, Bryson Probert.
Rock Dating. How old is Earth? What are some tools or methods that scientists could use to figure out the age of Earth? Think About It...
Book G Chapter 4 – Section 1
Geologic Time Rocks record geologic events and the changing life forms of the past. Uniformitarianism: The forces and processes that we observe today have.
fossils Relative age of rocks Radioactive dating Sedimentary Rocks evidence
Earth’s Age + Evidence. WARM UP Update your Table of Contents for today’s activities Get your data folder off the front desk Complete Types of Rock Review.
Geologic Time How can geologists date rocks?. ROCKROCK DATINGDATING.
7.4.c Students know that the rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers, with the oldest generally.
Ch. 13 Section 2 Relative Ages of Rocks.
Sections 8.2 and 8.3 Page  How do geologists determine the relative and absolute ages of rocks?  How are index fossils useful to geologists?
SI. A) Relative age: the age of rock compared to the ages of other rocks above or below it in a sequence of rock layers.
Unit 7 Lesson 2 Relative Dating
Ch 10 Ages of Rocks 10.2/10.3.
EARTH HISTORY UNIT MS. MITCHELL 9 TH GRADE EARTH SCIENCE VICTORIA MITCHELL 1.
Determining Geologic Time  Many geologic events that Earth Scientists study occurred millions of years ago. The ages of these events can be determined.
1 Earth’ s History Unit 6. 2 Vocabulary List 1.Relative Dating 2.Absolute Dating 3.Superposition 4.Cross-cutting relationships 5.Uniformitarianism 6.Original.
I can: describe methods used to assign
2 Types.  Relative Dating  Absolute Dating  1. Law of superposition – youngest layer on top; oldest layer on bottom.
Earth Science With Mr. Thomas. ► Fossils: ► Any evidence of earlier life preserved in rock. ► The study of these fossils is called:
Unit 3 Review Please see pages in your book for more information *This study guide is just to get you started studying– please look at your notes.
How do scientists sequence Earth’s past events to create the geological time scale? Using evidence from rocks and fossils, scientists can determine the.
Geologic Time MMSA Earth-Space Science. -Time scale based upon the fossil record -The fossil record indicates a wide variety of life has existed on Earth.
Age and Movement of Rocks. How old is old? Relative Dating a method of determining if an object is older or younger than another object.
Earth Science Notes Relative Age of Rocks. Objectives I can… Distinguish relative and absolute dating. Describe the 6 laws of relative dating. Use the.
Geological Time Dating Absolute and Relative. Geologic Time B y examining layers of sedimentary rock, geologists developed a time scale for dividing up.
Geological Time Dating Absolute and Relative. Geologic Time B y examining layers of sedimentary rock, geologists developed a time scale for dividing up.
Chapter 8 Science Test Notes Studying Earth’s Past.
The Rock and Fossil Record
Relative Dating: Which Came First?
Unit 2 Lesson 2 Relative Dating
Dating Fossils.
Unit 2 Lesson 2 Relative Dating
How do we know what happened millions of years ago?
Discovering Earth’s History
Relative Vs. Absolute Dating of Rocks
SSA Review 4 – Earth’s History
The History of Earth Chapter 6 Sections 1 and 2.
The History of Earth Chapter 6 Sections 1 and 2.
The History of Earth Chapter 6 Sections 1 and 2.
Rock record Condensed version of complete Rock Record –relative dating portion [See Rock Record to see complete version including more details on Rock.
Relative Age.
Which evidence---a trace fossil, a petrified fossil, a tree ring, or an ice core would be most helpful to a historian studying how the Indians grew food.
Unit 2 Lesson 2 Relative Dating
Relative and Absolute Age Law of Superposition
Geologic Time 1.
Relative Dating Write on RIGHT Side.
BELL-RINGER On a sheet of paper, write the difference between absolute dating and relative dating and give an example of each.
The History of Earth Chapter 6 Sections 1 and 2.
How do we determine the age of rock layers?
Ch. 13 Section 2 Relative Ages of Rocks.
Presentation transcript:

Fossils and Dating 8-2 notes

What you will learn: The rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers, with the oldest generally on the bottom. The rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers, with the oldest generally on the bottom. Radiometric dating can be used to determine how old a rock is and the how old the fossils in the rock are. Radiometric dating can be used to determine how old a rock is and the how old the fossils in the rock are. The Principle of Superposition. The Principle of Superposition.

Imagine that you find this in your back yard while digging….. This is not very likely, but someone had to be the first person to dig up a T-rex. This is not very likely, but someone had to be the first person to dig up a T-rex. How did they explain what it was? How did they explain what it was? How could they determine how old the bones were? How could they determine how old the bones were?

What is relative dating? Compares one rock layer with others in a sequence. Compares one rock layer with others in a sequence. Determining if an object/event is older or younger than another object or event. Determining if an object/event is older or younger than another object or event. This method of dating does not give a # or tell how many years old an object/event is. This method of dating does not give a # or tell how many years old an object/event is.

Principle of Superposition Younger rocks are on top of older rocks in undisturbed layers. Younger rocks are on top of older rocks in undisturbed layers. Fossils found in younger layers must be younger than fossils found in older, lower layers. Fossils found in younger layers must be younger than fossils found in older, lower layers.

Rock Layers

What that looks like in real life…

Not all rocks lay undisturbed… Look at the pictures on page 241. Look at the pictures on page 241. How did the rocks get that way? How did the rocks get that way? Erosion, folding, tilting, faults, and intrusions, are all caused by weathering, plate movement, and magma from below the plates being forced up. Erosion, folding, tilting, faults, and intrusions, are all caused by weathering, plate movement, and magma from below the plates being forced up.

Disturbing the rock layers Folding is the bending of rock layers from stress Folding is the bending of rock layers from stress Tilting happens when the Earth’s forces make the rocks slanted

Gaps in the records - Unconformities Sometimes rock layers are missing. Sometimes rock layers are missing. Never formed Never formed Or washed away by weathering Or washed away by weathering

Fossils A trace or remain of an organism that lived long ago. A trace or remain of an organism that lived long ago. Fossils are mostly found in Sedimentary rock. Fossils are mostly found in Sedimentary rock. There are fossils of freshwater (lake) organisms in Antarctica. What does that tell us about Antarctica? There are fossils of freshwater (lake) organisms in Antarctica. What does that tell us about Antarctica? It used to be much warmer. It used to be much warmer. Trace Fossils are traces that organisms leave behind – like footprints or scat. Trace Fossils are traces that organisms leave behind – like footprints or scat.

Absolute Dating A Method of dating rocks by using radioactive isotopes. Through the absolute dating of meteorites scientist determined that the Earth is 4.6 Billion years old. In one half-life the amount of radioactive material decreases by one-half.

Fossils and Dating Relative dating and Absolute dating of rocks can tell you how long ago a certain fossil was alive. Relative dating and Absolute dating of rocks can tell you how long ago a certain fossil was alive.

What you have learned The layering (order) of rocks will tell you which layers are older than other layers. (Law of Superposition). The layering (order) of rocks will tell you which layers are older than other layers. (Law of Superposition). Relative dating compares 2 items or events to see which one is older. Relative dating compares 2 items or events to see which one is older. Absolute dating uses radioactive decay of certain elements to determine how old rocks are. Absolute dating uses radioactive decay of certain elements to determine how old rocks are.

What to do next: Write a 6 sentence summary: Write a 6 sentence summary: 1. Opening or topic sentence 2. Detail 3. Detail 4. Detail 5. Detail 6. Closing about why the information is important.