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Geologic Time Earth’s History.

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Presentation on theme: "Geologic Time Earth’s History."— Presentation transcript:

1 Geologic Time Earth’s History

2 Uniformitarianism The present is the key to the past
Processes that happen today are the same processes that happened in ancient times Modern Mudcracks Fossilized Ripples Fossilized Mudcracks Modern Ripples

3 Dating – 2 types Relative Dating Absolute Dating
Know order of events but not dates Absolute Dating Know exact age

4 Relative Dating – Key Concepts
Law of Superposition Principle of Original Horizontality Principle of Cross-Cutting Relationships Principle of Inclusions

5 Law of Superposition Each bed is younger than the bed below it.

6 Principle of Original Horizontality
Sedimentary layers are deposited horizontally

7 Principle of Cross-Cutting Relationships
Faults and intrusions are younger than the rocks they cut through

8 Inclusions Fragments of one rock unit that have been enclosed within another are older

9 Relative Dating Youngest  G A B C F D Oldest  E
E is younger than D. Which Principle used? Law of Superposition G is younger than F. Which Principle is used? Principle of Cross-Cutting Relationships

10 Principle of Inclusion
A B Using the Principle of Inclusions, which picture shows the granite intrusion to be the youngest event? B

11 Conformable Beds Beds that have not been disturbed

12 Uncomformities Substantial break or gap in the rock record 3 types
Angular Disconformity Nonconformity

13 Angular Unconformity Older layers have been deformed, eroded, and younger layers deposited above

14 Disconformity Beds are parallel relative to each other but there is a break in sequence Implies a cessation of sedimentation or erosion, but no tilting Hard to recognize

15 Nonconformity Sedimentary layers overlie igneous or metamorphic layers

16 Unconformities Question: Answer: 1. Surface 1 is an example of ?
Nonconformity 2. Surface 2 is an example of ? Angular unconformity 3. Surface 3, 4 and 5? Disconformity 4. Granite is _________ than the Schist. Younger

17 Correlating Rocks Matching rocks of the same age in different locations

18 How do we correlate? Walking out the contact Matching fossils

19 Fossils The remains or traces of prehistoric life

20 Types of Fossils Body fossils Trace fossils Bone, teeth, shells
Record movement

21 Fossilization Hard parts Unaltered

22 Fossilization - Petrified
Turned into stone Petrified Forest, Arizona

23 Fossilization - Replacement
Minerals replace organic matter

24 Fossilization – Molds & Casts
Mold – impression or cavity Cast – deposited material that fills cavity

25 Fossilization - Amber Hardened Resin

26 Conditions favoring Preservation
Rapid burial Possession of hard parts Dies Buried Eroded

27 Fossils and Correlation
William Smith Each rock formation contained fossils unlike the ones above & below Sedimentary strata in widely separated areas could be identified & correlated by their fossil content

28 Principle of Fossil Succession
Fossils occur in a definite, invariable sequence in the geologic record Apply with Law of Superposition and can document evolution of life through time

29 Index Fossils Widespread geographically
Limited to a short span of geologic time

30 Correlating Rocks & Fossils
Igneous rocks are dated radiometrically Ages of fossils can be bracketed Fossils in another area can be correlated containing same fossils Age in another area determined indirectly Doing this repeatedly the geologic time scale established

31 Geologic Time Scale


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