Investigation 4: My Sediments Exactly Earth History Grade 6

Slides:



Advertisements
Similar presentations
Relative Dating of Rocks Layers
Advertisements

We know it’s BIG…but HOW do we know that?
FINDING RELATIVE AGE. What is relative age?  1. The age of a rock compared to the ages of other rocks.  Absolute age-the EXACT age of rock (add to your.
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.
 Uniformitarianism- Principle that states that the same geological process shaping the Earth today have been at work throughout Earth’s history.  Examples:
8.1 The Rock Cycle 7.4.a Students know Earth processes today are similar to those that occurred in the past and slow geologic processes have large cumulative.
The scientific method and the foundations of Geology.
GEOLOGIC PRINCIPLES & RELATIVE DATING. HOW OLD IS THE EARTH? The Earth is about 4.6 billion years old Much of its history is recorded in the rocks Observations.
Key Ideas State the principle of uniformitarianism.
1Daily Warm-Up Exercises1 Day 18 What is the difference between erosion and deposition? Erosion is when something like moving water or wind picks up loose.
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.
UNIT 5: GEOLOGIC HISTORY. AT THE END OF THIS UNIT YOU WILL BE ABLE TO  Calculate the absolute age of a substance based on its decay rate  Correlate.
GEOLOGIC TIME DAY 1 October 19. Objectives 10/19 Today I will be able to: - Compare the different ways to establish relative dating - Use the principle.
Interpreting Earth’s Rocks to Determine Its Past History.
Calving Glacier 3VTgIPoGU?rel=0.
LEQ: How do geologists and paleontologists determine the relative age of rocks? Part 2 Key Terms: Uniformitarianism, Original horizontality, cross- cutting.
Pushing the Envelope Observation and Inference. Pushing the Envelope The Principle of Uniformitarianism: The present is the key to the past.
Quick Write: Get the sandstone you made, and create two T-charts as shown. Compare the rocks and complete the T-charts. Include comparisons of grain size,
Interpreting Earth’s Rocks to Determine Its Past History.
Evolution and Change Chapter Fourteen: Earth and Life History 14.1 Evidence from Rocks 14.2 How Earth Changes 14.3 Natural Selection.
Determining Relative Age The beginning of modern geology.
1Daily Warm-Up Exercises1 Day 23 What is the main ingredient in limestone? calcium carbonate What was the purpose of the seawater investigation we did.
Relative Dating and Relative Age
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.
Rocks and the Fossil Record. In 1788 a man named James Hutton wrote Theory of the Earth. In it he hypothesized that all the processes that we observe.
James Hutton proposed the principle of uniformitarianism. This states that the processes occurring on Earth today, have been occurring since Earth first.
Scientific Dating Methods Unit 5. Scientific dating methods of fossils and rock sequences are used to construct a chronology of Earth’s history expressed.
Jump to first page Geologic Time Chapter 34. Jump to first page Dating rocks n Relative dating F Compare events and put them in order based on their sequence.
Entry Task: Get your basin and observe your shale. Record your observations. Create a scientific drawing of your basin. Include a profile-view drawing.
Relative Dating Earth Science What is it? Relative dating is the process of identifying the relative ages of the layers of the Earth. The goal of.
The Geologist as Detective Chapter 6 : Interpreting Geologic History.
Methods of Measurement
Laws of Geologic History. Law of Superposition The oldest layer is at the bottom and the youngest layer is at the top. The oldest layer is at the bottom.
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,
Geologist interpret Earth’s history by studying sedimentary rocks Relative Dating.
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.
Relative Dating. Relative Dating is one of the methods that geologists use to help tell geologic time. It can NOT tell us exactly how old something is,
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.
Earth History: Investigation 4 Sandstone & Shale.
The Rock Record Section 1 Section 1: Determining Relative Age Preview Objectives Uniformitarianism Relative Age Law of Superposition Principle of Original.
Earth History Sandstone & Shale Formation. Basin An area of relative low elevation where water and sediments collect.
Relative-Age Dating. Scientists have not always thought Earth was as old as it is. James Hutton in the late 1700’s was the first geologist to think Earth.
Dating the Earth Chapter 12. A major goal of Geology is to interpret Earth’s History !! A pioneering geologist and 2 nd director of the USGS. Led an expedition.
Homework Review Pg. 190 #1-8, 4 ways to determine absolute age.
Standard 3. Objective 3: Describe how rock and fossil evidence is used to infer Earth’s history. a) Describe how the deposition of rock materials produces.
Interpreting Earth’s Rocks to Determine Its Past History.
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,
How old is old?. Earth Processes take a really, really, really (really) long time….. So, the question is – How do we know how old something is? Especially.
Aim: How do Scientists Read Rocks? Do Now: In your notes, answer the following question. Of the three types of rocks we have discussed (Igneous, Sedimentary.
Geologic time Relative dating
Principles of Geology Mr. Halfen Jan
How is relative age dating like a hamper of clothes?
Discovering Earth’s History
The History of Earth Relative Dating Absolute Dating
Age.
The History of Earth Relative Dating Absolute Dating
Investigation 4: My Sediments Exactly Earth History Grade 6
How Old is Old? Geologic Time.
Here is vocabulary to help you understand the terms to allow you to understand how scientists determine the age of Earth layers and things found in the.
The History of Earth Chapter 6 Sections 1 and 2.
The History of Earth Chapter 6 Sections 1 and 2.
Geologic Time.
The History of Earth Chapter 6 Sections 1 and 2.
FIVE STEPS TO BECOMING A… GEOLOGICAL DETECTIVE!
Science Jeopardy!.
The History of Earth Chapter 6 Sections 1 and 2.
5.1 Principles of Earth’s History
Presentation transcript:

Investigation 4: My Sediments Exactly Earth History Grade 6 Earth’s Layers Investigation 4: My Sediments Exactly Earth History Grade 6

Layers Geologists observed that, usually, when sediments settle in a basin, they form a flat, horizontal layer. Horizontal: level (like a floor), not higher on one side or the other.

Principle of Original Horizontality Each new deposit of sediment forms a new horizontal layer on top of the layers below. Principle of Original Horizontality: layers of sediment are generally deposited in a horizontal or nearly horizontal position.

Uniformitarianism Uniformitarianism: the present is the key to the past. Geologists use the observations they make about processes happening today, such as erosion, deposition, and the formation of sand and clay to infer events that happened in the past, events that they weren’t able to observe.

Uniform The way things happen today is the same way things have always happened. The processes are uniform.