Fossils Chapter 10 Sections 1+2. How a Fossil Forms - Fossils Most fossils form when living things die and are buried by sediment. The sediment slowly.

Slides:



Advertisements
Similar presentations
A trip through geologic time Chapter 10 page 310
Advertisements

A Trip Through Geologic Time
Petrified Remains Hard and rock like Hard and rock like Original material replaced by minerals Original material replaced by minerals Ex. bones, wood.
Fossils Fossil are the preserved remains or traces of living things. They form when living things die and are buried by sediment. They are usually.
FOSSILS UNIT ONE.
Section 4.2  The relative age of a rock is its age compared to the ages of other rocks.  Ex. Mrs. Herrscher is older than her sister and brother. 
The Relative Age of Rocks
Finding the Relative age of Rocks
The Relative Age of Rocks 10-2
Please get out your notebook!!
CH 8 SEC 2 THE RELATIVE AGE OF ROCKS GOAL/PURPOSE STUDENTS KNOW THAT THE ROCK CYCLE INCLUDES THE FORMATION OF NEW SEDIMENT AND ROCKS ARE OFTEN FOUND.
The relative age of rocks
Chapter 9 – 1 FOSSILS.
Table of Contents Fossils The Relative Age of Rocks Radioactive Dating
Fossils & History of the Earth
Chapter 3 Section 4 Looking at Fossils.
Good Morning! 1. Complete your warm-up: What happens at a convergent boundary? Be specific. 2. Have out your Venn Diagram. You may have it pasted in your.
The Relative Age of Rocks
PRESERVED REMAINS OR TRACES OF AN ORGANISM THAT LIVED IN THE PAST
The Relative Age of Rocks
Do Species Change Over Time?
Table of Contents Chapter Preview 8.1 The Rock Cycle
Book G Chapter 4 – Section 1
Fossils. How a Fossil Forms  Most fossils from when living things die and are buried by sediments.  The sediments slowly harden into rock and preserve.
Aim Aim: How do we know the age of the Earth? I. Earth’s History Uniformitarianism A. Uniformitarianism – the principle that most of the geologic events.
Paleontology and Ecology Study Guide Questions & Answers Semester 1 Shiloh Middle School.
fossils Relative age of rocks Radioactive dating Sedimentary Rocks evidence
Paleontology and Ecology Study Guide Questions & Answers.
The Relative Age of Rocks PH Essential Question How does the law of Superpostion help geologists date rocks and what evidence do they use?
Uncovering Earth’s Past Date: 4/3/13 p. 111 in ILL.
Relative Dating and Relative Age
Notes 7-2 and 8-2 Evidence and fossils. Evidence of evolution Similar body structures Patterns of early development Molecular structure Fossils.
How a Fossil Forms - Fossils
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.
Science Earth’s Changing Surface Chapter 4 Section 2.
Bell Ringer How do fossils form? Where are they found and describe each?
What is relative and absolute age? A rock layer’s relative age is its age compared to the ages of other rock layers. Generally (relative) versus specifically.
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?
Chapter 4 A trip Through Geologic Time
4.2 The Relative Age Of Rocks
The Relative Age Of Rocks Chapter 8 Section 2
EARTH SCIENCE.
Fossil/Age of Rock Notes Use the Purple book to get notes for fossils and relative age of rock notes. – Write the word and definition for all of the vocab.
Earth’s History How do we know about it?. What is Uniformitarianism? Uniformitarianism: –Is a theory developed by the Scottish geologist, James Hutton,
How do scientists sequence Earth’s past events to create the geological time scale? Using evidence from rocks and fossils, scientists can determine the.
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.
Fossils Chapter 4 Section 1 Pages Evidence of Ancient Life Fossils- the preserved remains or traces of living things.
The Rock and Fossil Record
(7 th ) Chapter 8-2 Cornell Notes The Relative Age of Rocks.
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.
Jeopardy Fossils Relative Aging Absolute Dating Geologic Time
A Trip Through Geologic Time
A Trip Through Geologic Time
A Trip Through Geologic Time
A Trip Through Geologic Time
Fossils and the Law of Superposition
The Position of Rock Layers
A Trip Through Geologic Time
A Trip Through Geologic Time
The Age of Rocks and Fossils
(7th) Chapter 8-2 Cornell Notes
The History of Earth Chapter 6 Sections 1 and 2.
A Trip Through Geologic Time
Geologic Time.
4/18 - 7th Grade Agenda Learning Objective: Learn about Index Fossils
Fossils and Rock Layers
Finding the Age of Rocks Through Rock Dating
Geologic Time 1.
A Trip Through Geologic Time
Presentation transcript:

Fossils Chapter 10 Sections 1+2

How a Fossil Forms - Fossils Most fossils form when living things die and are buried by sediment. The sediment slowly hardens into rock and preserves the shapes of the organisms.

Changes Over Time - Fossils The fossils record provides evidence about the history of life and past environments on Earth. The fossil record also shows that different groups of organisms have changed over time. Fossils of many different kinds of organisms were formed in this ancient lakeshore environment that existed in Wyoming about 50 million years ago.

Changes Over Time - Fossils From fossils, scientists have reconstructed the paleomastodon. This animal had a short trunk and short tusks on both the upper and lower jaws. The paleomastodon is an ancestor of the modern elephant.

What You Know What You Learned Using Prior Knowledge Before you read, look at the section headings and visuals to see what this section is about. Then write what you know about fossils in a graphic organizer like the one below. As you read, write what you learn. 1.Fossils come from ancient organisms. 2.Fossils are found in hardened rock. 3.Fossils show us how some present-day organisms looked different in the past. 1.Molds and casts are types of fossils. 2.Organisms are also preserved in amber, tar, and ice. 3.Fossils tell us about past climates, changes in Earth’s surface, and how organisms have changed over time. - Fossils

End of Section: Fossils

The Position of Rock Layers According to the law of superposition, in horizontal sedimentary rock layers, the oldest layer is at the bottom. Each higher layer is younger than the layers below it. - The Relative Age of Rocks

Determining Relative Age To determine relative age, geologists also study extrusions and intrusions of igneous rock, faults, and gaps in the geologic record. - The Relative Age of Rocks

Determining Relative Age - The Relative Age of Rocks An unconformity occurs where erosion wears away layers of sedimentary rock. Other rock layers then form on top.

Using Fossils to Date Rocks Index fossils are useful because they tell the relative ages of the rock layers in which they occur. - The Relative Age of Rocks

Index Fossil Activity Click the Active Art button to open a browser window and access Active Art about index fossils. - The Relative Age of Rocks

QuestionAnswer Asking Questions Before you read, preview the red headings. In a graphic organizer like the one below, ask a what or how question for each heading. As you read, write answers to your questions. What does the position of rock layer reveal? The oldest layers—and the oldest fossils—are at the bottom. How do geologists determine the relative age of a rock? They examine the position of rock layer, extrusions and intrusions of igneous rock, faults, and gaps in the geologic record. How are fossils used to date rocks? The age of an index fossil tells the age of the rock layer in which it occurs. - The Relative Age of Rocks

Rock Layers Click the Video button to watch a movie about rock layers. - The Relative Age of Rocks

Index Fossils Click the Video button to watch a movie about index fossils. - The Relative Age of Rocks