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Chapter 16- The Rock & Fossil Record

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Presentation on theme: "Chapter 16- The Rock & Fossil Record"— Presentation transcript:

1 Chapter 16- The Rock & Fossil Record
8th Grade Science Chapter 16- The Rock & Fossil Record © Fall 2005, Pflugerville ISD, 8th Grade

2 Chapter 16- The Rock & Fossil Record
Section 1: Earth’s Story & Those Who First Listened Section 2: When on Earth? Section 3: Looking at Fossils Section 4: Time Marches On Unit 4 : Chapter 16

3 “The present is the key to the past.” -James Hutton
What Do You Think? We study the past because if we don’t, we are doomed to repeat it. But how can studying the present help us understand earth’s history? What are some processes you can see today that also occurred millions of years ago? Unit 4 : Chapter 16 : Section 1

4 Earth’s Story & Those Who Listened
“The present is the key to the past.” Father of modern geology James Hutton Unit 4 : Chapter 16 : Section 1

5 Earth’s Story & Those Who Listened
Hutton knew that Hadrian’s wall was built by the Romans in historical times Hadrian’s Wall, England Unit 4 : Chapter 16 : Section 1

6 Earth’s Story & Those Who Listened
Only 1600 years old, the wall was already starting to weather and erode Hadrian’s Wall, England Unit 4 : Chapter 16 : Section 1

7 Earth’s Story & Those Who Listened
Hutton wondered how long it would take to erode a mountain Arthur’s Seat Volcano, Edinburgh, Scotland Unit 4 : Chapter 16 : Section 1

8 Earth’s Story & Those Who Listened
Hutton decided that it would take millions of years, making the earth very ancient Arthur’s Seat Volcano, Edinburgh, Scotland Unit 4 : Chapter 16 : Section 1

9 Earth’s Story & Those Who Listened
Hutton realized that erosion and deposition have been going on for a long time Arthur’s Seat Volcano, Edinburgh, Scotland Unit 4 : Chapter 16 : Section 1

10 Earth’s Story & Those Who Listened
Uniformitarianism is Hutton’s belief that geologic processes are uniform and do not change over time James Hutton Unit 4 : Chapter 16 : Section 1

11 Earth’s Story & Those Who Listened
Hutton’s views of a billion-year-old earth clashed with most scientists’ belief in catastrophism James Hutton Unit 4 : Chapter 16 : Section 1

12 Earth’s Story & Those Who Listened
Most scientists supported catastrophism, the idea that all geologic change happens quickly Unit 4 : Chapter 16 : Section 1

13 Earth’s Story & Those Who Listened
These scientists used huge floods, eruptions and catastrophes to explain rapid geologic change Unit 4 : Chapter 16 : Section 1

14 Earth’s Story & Those Who Listened
Today, scientists think that sudden events are the cause of some changes in earth’s past Unit 4 : Chapter 16 : Section 1

15 Earth’s Story & Those Who Listened
But they agree that the earth is billions of years old, and that most change is gradual Unit 4 : Chapter 16 : Section 1

16 When on Earth? What Do You Think?
Suppose your friend piles his stuff on his floor and never cleans his room. Under the top layer of clothes, you find a pizza box. Under this is a bunch of CDs then some homework and under this is a ham sandwich. Arrange these four layers from oldest to youngest… Unit 4 : Chapter 16 : Section 2

17 Unit 4 : Chapter 16 : Section 2
When on Earth? The Principle of Superposition states that younger rocks lie over older rocks Grand Canyon Unit 4 : Chapter 16 : Section 2

18 Unit 4 : Chapter 16 : Section 2
When on Earth? The Principle of Superposition is used to find the relative ages of rock layers Grand Canyon Unit 4 : Chapter 16 : Section 2

19 Unit 4 : Chapter 16 : Section 2
When on Earth? The Law of Cross-Cutting Relationships can tell geologists the relative age of a fault or intrusion Unit 4 : Chapter 16 : Section 2

20 Unit 4 : Chapter 16 : Section 2
When on Earth? The dike is the youngest feature, because the other layers were cut by it Unit 4 : Chapter 16 : Section 2

21 Unit 4 : Chapter 16 : Section 2
Relative Dating Use your knowledge to order the layers, faults and intrusions in the next slide from oldest to youngest Unit 4 : Chapter 16 : Section 2

22 Unit 4 : Chapter 16 : Section 2
Relative Dating Unit 4 : Chapter 16 : Section 2

23 Unit 4 : Chapter 16 : Section 1
Relative Dating Geologists can use rock layers from many locations to create a geologic column James Hutton Unit 4 : Chapter 16 : Section 1

24 Unit 4 : Chapter 16 : Section 2
Relative Dating Unit 4 : Chapter 16 : Section 2

25 Unit 4 : Chapter 16 : Section 2
Relative Dating The geologic column is an ideal sequence of rock layers that contains all known rock formations and fossils on Earth Unit 4 : Chapter 16 : Section 2

26 Unit 4 : Chapter 16 : Section 2
When on Earth? An unconformity is a surface that represents a missing part of the geologic column Hutton’s Unconformity Unit 4 : Chapter 16 : Section 2

27 Formation of an Unconformity
Sediment is eroded from a hill and deposited in a valley 30-15 Million Years Ago Unit 4 : Chapter 16 : Section 2

28 Formation of an Unconformity
The area is uplifted and exposed to erosion, then the land surface is eroded away 15-5 Million Years Ago Unit 4 : Chapter 16 : Section 2

29 Formation of an Unconformity
Deposition resumes Can you spot the unconformity? 5 Million Years Ago- Present Unit 4 : Chapter 16 : Section 2

30 Unit 4 : Chapter 16 : Section 2
Absolute Dating When animals eat, they ingest radioactive Carbon-14 Unit 4 : Chapter 16 : Section 2

31 Unit 4 : Chapter 16 : Section 2
Absolute Dating Nitrogen-14 Carbon-14 Carbon-14 decays into Nitrogen-14 Unit 4 : Chapter 16 : Section 2

32 Unit 4 : Chapter 16 : Section 2
Absolute Dating By comparing the amount of C-14 to N-14, geologists can calculate the age of a fossil Unit 4 : Chapter 16 : Section 2

33 Unit 4 : Chapter 16 : Section 2
Absolute Dating Since C-14 has a half-life of only 5730 years, other isotopes are used to date older rocks Unit 4 : Chapter 16 : Section 2

34 Unit 4 : Chapter 16 : Section 1
Absolute Dating The oldest rocks on Earth have been dated to 4.5 billion years, confirming Hutton’s beliefs James Hutton Unit 4 : Chapter 16 : Section 1

35 Unit 4 : Chapter 16 : Section 3
Looking at Fossils What Do You Think? Imagine that a geologist 65 million years from now has unearthed fossils of your life. What would she find? Unit 4 : Chapter 16 : Section 3

36 Unit 4 : Chapter 16 : Section 3
Looking at Fossils A fossil is the remains or physical evidence of an organism preserved by geologic processes Saber-Tooth Cat Fossil Unit 4 : Chapter 16 : Section 3

37 Unit 4 : Chapter 16 : Section 3
Looking at Fossils Fossilized tree sap is called amber Fossil Amber with Insect Inclusions Unit 4 : Chapter 16 : Section 3

38 Unit 4 : Chapter 16 : Section 3
Looking at Fossils Animals caught in amber are perfectly preserved Fossil Amber with Insect Inclusions Unit 4 : Chapter 16 : Section 3

39 Unit 4 : Chapter 16 : Section 3
Looking at Fossils Fossils of mammoths, extinct for 12,000 years, have been found frozen in Arctic ice Woolly Mammoth Unit 4 : Chapter 16 : Section 3

40 Unit 4 : Chapter 16 : Section 3
Looking at Fossils A trace fossil is naturally preserved evidence of animal activity Theropod Track Unit 4 : Chapter 16 : Section 3

41 Unit 4 : Chapter 16 : Section 3
Looking at Fossils This dinosaur track is located in Glen Rose, Texas, in Dinosaur Valley State Park Theropod Track Unit 4 : Chapter 16 : Section 3

42 Unit 4 : Chapter 16 : Section 3
Looking at Fossils A mold is a cavity in rock where a plant or animal was buried Ammonite Fossil Unit 4 : Chapter 16 : Section 3

43 Unit 4 : Chapter 16 : Section 3
Looking at Fossils A cast is an object made when sediment fills a mold and becomes rock Ammonite Fossil Unit 4 : Chapter 16 : Section 3

44 Unit 4 : Chapter 16 : Section 3
Looking at Fossils Unit 4 : Chapter 16 : Section 3

45 Unit 4 : Chapter 16 : Section 3
Looking at Fossils Which of these is the mold and which is the cast? Ammonite Fossil Unit 4 : Chapter 16 : Section 3

46 Unit 4 : Chapter 16 : Section 3
Looking at Fossils Most animals are not buried fast enough to form fossils Whale Bones Unit 4 : Chapter 16 : Section 3

47 Unit 4 : Chapter 16 : Section 3
Looking at Fossils These whale bones will be broken down before they can form fossils Whale Bones Unit 4 : Chapter 16 : Section 3

48 Unit 4 : Chapter 16 : Section 3
Looking at Fossils The trilobite Phacops lived for a short time 400 million years ago Trilobite Fossil Unit 4 : Chapter 16 : Section 3

49 Unit 4 : Chapter 16 : Section 3
Looking at Fossils An index fossil is one found for a short time in rock layers around the world Trilobite Fossil Unit 4 : Chapter 16 : Section 3

50 Unit 4 : Chapter 16 : Section 3
Looking at Fossils If Phacops is found in a rock layer, the rock must be about 400 million years old Trilobite Fossil Unit 4 : Chapter 16 : Section 3

51 Unit 4 : Chapter 16 : Section 4
Time Marches On What Do You Think? If the history of Earth were the length of one calendar year, on what date do you think modern humans arrived? Unit 4 : Chapter 16 : Section 4

52 Unit 4 : Chapter 16 : Section 4
Time Marches On Humans evolved in the last half-hour of New Years Eve! Humans First Arrived Unit 4 : Chapter 16 : Section 4

53 Unit 4 : Chapter 16 : Section 4
Time Marches On The Geologic Time Scale divides Earth’s history into eons, eras, & periods Unit 4 : Chapter 16 : Section 4

54 Unit 4 : Chapter 16 : Section 4
Time Marches On Since most fossils are from the Phanerozoic Eon, this is the eon that is given the most attention Unit 4 : Chapter 16 : Section 4

55 Unit 4 : Chapter 16 : Section 4
Time Marches On The Phanerozoic is actually the shortest of the four eons Unit 4 : Chapter 16 : Section 4

56 Unit 4 : Chapter 16 : Section 4
Time Marches On In the Paleozoic Era, life in the oceans, as well as all major plant groups, flourished Paleozoic Era mya Unit 4 : Chapter 16 : Section 4

57 Unit 4 : Chapter 16 : Section 4
Time Marches On With a mass extinction at the end of the Paleozoic, the remaining reptiles thrived Mesozoic Era mya Unit 4 : Chapter 16 : Section 4

58 Unit 4 : Chapter 16 : Section 4
Time Marches On Known as the Age of Reptiles, birds and small mammals appeared late in the Mesozoic Mesozoic Era mya Unit 4 : Chapter 16 : Section 4

59 Unit 4 : Chapter 16 : Section 4
Time Marches On Mammals flourished after a mass extinction killed the dinosaurs Cenozoic Era 65 mya- Present Unit 4 : Chapter 16 : Section 4

60 Unit 4 : Chapter 16 : Section 4
Time Marches On The Cenozoic is known as the Age of Mammals Cenozoic Era 65 mya- Present Unit 4 : Chapter 16 : Section 4

61 Let’s Review! - 1 - What did James Hutton mean by the comment, “The present is the key to the past”? Unit 4 : Chapter 16

62 How can you tell the age of rocks and fossils?
Let’s Review! - 2 - How can you tell the age of rocks and fossils? Unit 4 : Chapter 16

63 Describe how a geologist would use an index fossil…
Let’s Review! - 3 - How is a fossil created? Describe how a geologist would use an index fossil… Unit 4 : Chapter 16

64 What type of event ended both the Paleozoic and Mesozoic Eras?
Let’s Review! - 4 - What type of event ended both the Paleozoic and Mesozoic Eras? What geologic time period was occurring 200 million years ago? Unit 4 : Chapter 16

65 Web Sites to Visit: . Unit 4 : Chapter 16

66 Pre-AP Extensions Unit 4 : Chapter 16


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