Your SlideShare is downloading. ×
0
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Earth Science 3.2 : Relative Dating : Which Came First?
Upcoming SlideShare
Loading in...5
×

Thanks for flagging this SlideShare!

Oops! An error has occurred.

×
Saving this for later? Get the SlideShare app to save on your phone or tablet. Read anywhere, anytime – even offline.
Text the download link to your phone
Standard text messaging rates apply

Earth Science 3.2 : Relative Dating : Which Came First?

9,855

Published on

Published in: Education, Spiritual, Technology
0 Comments
4 Likes
Statistics
Notes
  • Be the first to comment

No Downloads
Views
Total Views
9,855
On Slideshare
0
From Embeds
0
Number of Embeds
5
Actions
Shares
0
Downloads
96
Comments
0
Likes
4
Embeds 0
No embeds

Report content
Flagged as inappropriate Flag as inappropriate
Flag as inappropriate

Select your reason for flagging this presentation as inappropriate.

Cancel
No notes for slide

Transcript

  • 1. Earth Science Chapter 3.2<br />Relative Dating : Which Came First?<br />
  • 2. Objectives:<br />Explain how relative dating is used in geology.<br />Explain the principle of superposition.<br />Describe how the geologic column is used in relative dating.<br />Identify two events and two features that disrupt rock layers.<br />Explain how physical features are used to determine relative ages.<br />
  • 3. The Principle of Superposition<br />Geologists try to determine the order in which events have happened during Earth’s history. <br />They rely on rocks and fossils to help them in their investigation.<br />Relative dating<br />The process of determining whether an event or object is older or younger than other events or objects.<br />
  • 4. Layers of sedimentary rock, such as the ones shown below, are stacked like pancakes.<br />As you move from the top to the bottom in layers of sedimentary rock, the lower layers are older.<br />Superposition<br />Principle that states that younger rocks lie above older rocks, if the layers have not been disturbed.<br />
  • 5. Disturbing Forces<br />Not all rock sequences are arranged with the oldest layers on the bottom and the youngest layers on top.<br />Some rock sequences have been disturbed by forces within the Earth.<br />These forces can:<br />Push other rocks into a sequence<br />Tilt or fold rock layers<br />Break sequences into moveable parts.<br />
  • 6. The Geologic Column<br />Geologic <br />an ideal sequence of rock layers that contains all the known fossils and rock formations on Earth, arranged from oldest to youngest.<br />Geologists use the geologic column to:<br />Interpret rock sequences <br />Identify the layers in puzzling rock sequences.<br />
  • 7.
  • 8. Disturbed Rock Layers<br />Geologists<br />often find features that cut across existing layers of rock.<br />assign relative ages to the features and the layers.<br />The features must be younger than the rock layers because the rock layers had to be present before the features could cut across them.<br />fault<br />intrusion<br />
  • 9. Events That Disturb Rock Layers<br />Geologists assume that the way sediment is deposited to form rock layers — in horizontal layers — has not changed over time.<br />If rock layers are not horizontal<br />something must have disturbed them after they formed.<br />Four ways that rock layers may become disturbed.<br />A fault<br />break in the Earth’s crust along which blocks of the crust slide relative to one another.<br />An intrusion<br />molten rock from the Earth’s interior that squeezes into existing rock and cools.<br />
  • 10. Folding<br />occurs when rock layers bend and buckle from Earth’s internal forces.<br />Tilting<br />occurs when internal forces in the Earth slant rock layers.<br />
  • 11. Gaps in the Record -- Unconformities<br />Missing Evidence<br />Sometimes, layers of rock are missing, creating a gap in the geologic record.<br />Unconformity<br />break in the geologic record created when rock layers are eroded or when sediment is not deposited for a long period of time.<br />
  • 12. Types of Unconformities<br />Most unconformities form by both erosion and nondeposition, but other factors may be involved.<br />Geologists place them into three major categories: <br />Disconformities<br />Nonconformities<br />Angular unconformities<br />Disconformities exist where part of a sequence of parallel rock layers is missing.<br />
  • 13. Nonconformities<br />exist where sedimentary rock layers lie on top of an eroded surface of nonlayered igneous or metamorphic rock.<br />Angular Unconformities<br />exist between horizontal rock layers and rock layers that are tilted or folded.<br />
  • 14. Rock-Layer Puzzles<br />Rock-layer sequences often have been affected by more than one geological event or feature.<br />For example, intrusions may squeeze into rock layers that contain an unconformity<br />Determining the order events <br />is like solving a jigsaw puzzle.<br />piece together the history of the Earth.<br />

×