“The Present is the Key to the Past”

Slides:



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

Relative Time.
GEOLOGIC TIME.
Chapter 8 Geologic Time.
Age Dating of Rocks.
Unit 6 – The Geosphere Vocabulary
Earth Science Geologic Time Chapter 11.
Geologic Time Chapter
Geologic time.
Glencoe Earth Science c1999 Chap 12
Earth’s Surface Chapter 4 A Trip Through Geologic Time
Relative and Absolute Dating
Prentice Hall EARTH SCIENCE
Geologic Time (History as told by Rocks)
Are you ready for tomorrow’s quiz? A.YES! The study guide and the practice test helped a ton! B.I think so…but I should look over my notes some more.
Determining Geologic Ages Lab # 8 pg 91
ESS 8.4 Earth’s History.
Chapter 4: A Trip Through Geologic Time
GEOLOGIC TIME.
The History of Earth.
The Rock and Fossil Record – Geology and Time. Earth’s Story Catastrophism (#2) – belief that all geologic change happens suddenly. Rare Mountains, canyons,
Edward J. Tarbuck & Frederick K. Lutgens
Geologic Time Earth’s History.
Table of Contents Chapter Preview 8.1 The Rock Cycle
Paleo Test Review Guide. Hutton’s principal of uniformitarianism states…. Hutton’s principal of uniformitarianism states…. -current geologic processes.
Book G Chapter 4 – Section 1
Earth Science Geologic Time Chapter 12.
Earth’sStoryRelativeDatingAbsoluteDating Looking at Fossils Time Marches On Final Jeopardy Final Jeopardy.
Lecture Outlines Physical Geology, 14/e
THIS IS With Host... Your Modified T/F Modified T/F Multiple Choice Multiple Choice Completion.
Define the following terms at the top of your notes for Ch 21!
The Rock and Fossil Record. Uniformitarianism - proposed by James Hutton - states that Earths landscape is constantly changing due to the same geologic.
Ch. 23.6: Interpreting the Rock Record
Chapter 11 Fossils Fossil: evidence such as the remains, imprints, or traces of once living organisms preserved in rocks Many times dead.
Geologic Time.
© 2012 Pearson Education, Inc. Geologic Time Chapter 11 Stanley C. Hatfield Southwestern Illinois College.
Geologic Time The Geologic Time Scale Geologists have divided the history of the Earth in time units based on fossil evidence. The time units are part.
Fossils +/*0 /210.
Understanding Geologic Time. How old is it? How do we know? Absolute dating – process of assigning a precise numerical age to an organism, object or.
EARTH HISTORY UNIT MS. MITCHELL 9 TH GRADE EARTH SCIENCE VICTORIA MITCHELL 1.
The Relative Age of Rocks
3.4 Earth’s Geologic History
Fossils and the Rock Record
Fossils and the Rock Record The Rock Record  Rocks record geological events and changing life forms of the past  Planet Earth was formed 4.6 billion.
EARTH SCIENCE.
Ch. 12 and 13. Rocks record geological events and changing life forms of the past.
How do scientists sequence Earth’s past events to create the geological time scale? Using evidence from rocks and fossils, scientists can determine the.
The Principle of Uniformitarianism Scientist James Hutton, the author of Theory of the Earth, proposed that geologic processes such as erosion & deposition.
There are different ways geologists can describe the age of rocks & geologic events:
1/28/13 - QOTD In the picture below, where is the oldest rock? A B.
Aging the Earth. a. Using the Fossil Record b. Using the Law of Superposition c. Using Relative Dating d. Using Absolute Dating through Radioactive Decay.
Rock and Fossil Record.   James Hutton: 1788 wrote a book with a big idea  Uniformitarianism -same processes long ago are the same as today  Controversial.
Paleontology and Fossils images.usatoday.com/.../2006/11/07/fossil472.jpg.
Geologic Time. The Geologic Time Scale  A summary of major events in Earth’s past that are preserved in the rock record  Divisions of Geologic Time.
I. History -Earth is believed to be somewhere around 4.6 billion years old. -Geologists use clues recorded in rock to reconstruct the events from the.
Paleontology and Fossils images.usatoday.com/.../2006/11/07/fossil472.jpg.
Earth Science Chapter 6 I. Rocks of the crust provide clues to Earth’s past By analyzing these clues we can infer events from the past.
UNIT 6 HISTORICAL GEOLOGY
Earth History.
CHAPTER 12.1 Discovering Earth’s History
Chapter 12 Geologic Time.
Fossils and the Law of Superposition
CHAPTER 8 GEOLOGIC TIME.
Earth History.
Earth’s History.
The Geologic Time Scale
Geologic Time Earth Science Ch.12.
Geologic Time Notes By studying the characteristics of rocks and the fossils within them geologists can… interpret the environments in which the rocks.
Fossils Preserved remains/traces of living things Clues to the past
Earth’s History Created by Educational Technology Network
Presentation transcript:

“The Present is the Key to the Past” James Hutton, 1700’s

History of Geology The concept and measurement of geologic time has changed through human history. Planet Earth,The Living Machine p1.mp4 7:15 – 8:00 James Ussher (1581-1665) in Ireland calculated the age of Earth based on recorded history and genealogies in Genesis he said that Earth was created on October 22, 4004 B.C. it was considered heresy to say Earth was more than about 6000 years old.

Catastrophism Catastrophism proposed by Georges Cuvier (1769-1832) Huge catastrophies caused major changes to Earth’s geology and biology in a short period of time. six major catastrophes occurred, corresponding to the six days of biblical creation, the last one was the biblical flood.

Uniformitarianism Developed by James Hutton, advocated by Charles Lyell (1797-1875) “The Present is the Key to the Past”, James Hutton, 1700’s What happens today is what happened in the past. Earth changes very slowly. Supports a very old age of Earth. Earth is believed to be about 4.6 billion years old

NeoCatastrophism Blends Uniformitarianism with some Catastrophism. Earth developed and changed at a very slow rate like today, but had some catastrophic event s that caused some sudden changes. Eg: extinction of dinosaurs Asteroid collision, Gamma-ray Bursts . . .

Relative Dating This is not about dating your sister!!  Tells us the sequence in which events occurred in a rock. Which formed 1st, 2nd, etc. . . NOT how long ago they occurred.

Laws and Principles Law of Superposition Youngest Oldest In an undisturbed sedimentary rock, each bed is older than the one above it and younger than the one below it. Youngest Oldest

Laws and Principles Principle of Original Horizontality Layers of sediment are generally deposited in a horizontal position. Rocks that are folded or tilted must have been moved into that position AFTER their formation. What happened first? What happened second? Horizontal deposition Folding

Laws and Principles Principle of Cross-Cutting Relationships When a fault or igneous intrusion cuts through another rock, the fault or intrusion is YOUNGER than rock it cut through. Igneous Intrusion

Laws and Principles Principle of Inclusions Inclusions are pieces of one rock found in another. The rock containing the inclusions is YOUNGER than the rock the inclusions came from. Older Younger Inclusions

Laws and Principles Principle of Unconformities Represents a long period during which deposition is stopped, erosion removed rock and then deposition started again. http://www.wwnorton.com/college/geo/animations/unconformity.htm Angular unconformity The first layers were tilted before the deposition started again. Disconformity When two layers of sedimentary rock are separated by an erosional surface but are still parallel to eachother. Nonconformity Erosional surface separates older igneous rocks from younger sedimentary rocks. http://www.wwnorton.com/college/geo/animations/types_of_unconformity.htm

Principle of Unconformity Which type of Unconformity is which??? Disconformity Angular Unconformity Nonconformity

Relative Dating Place the following layers in order of occurrence from OLDEST to YOUNGEST. Include the Fault and unconformity. 8. 7. 6. 5. 4. 3. 2. H R M Unc Fault F B I Youngest Oldest

Fossils: Evidence of Past Life What is a Fossil? Preserved remains or traces of prehistoric life. The type of fossil formed is determined by the conditions the organism died and was buried.

Fossils: Evidence of Past Life The two conditions necessary for the formation of fossils is: Having HARD parts Rapid BURIAL

Fossils: Evidence of Past Life Forms of Fossilzation Mold and Cast Mold: the hollow shape of the organism left after water dissolved the hard part (shell) Cast: the solid COPY of the shape of the organism Mold Cast

Fossils: Evidence of Past Life Other forms: Petrified: Minerals replace all or part of the organism. Shows interior detail (Quartz) Ex: Petrified Wood Carbon Films: A thin coating of carbon on the rock. The carbon is left from the organism itself. (plants and insects) Impressions: a copy of the surface of organism Trace Fossils: clues that an organism was there. (Foot prints)

Fossils: Evidence of Past Life Fossil Succession Fossils succeed one another in a definite order. (Simpler organisms = older rocks) Any time-period can be recognized by its fossil content. Jurassic Period

Laws and Principles Fossil Correlation Index fossils: Fossils that are Matching similar rock types found in different areas. Index fossils: Fossils that are Widely distributed Lived a short time

Rock Correlation with Fossils Activity Answer Key Unconformity 

Radiometric Dating Radioactive Elements Unstable elements break down or DECAY. Occurs when the Nucleus changes (Protons and Neutrons change). During Radioactive Decay, one element breaks down into another element giving off ENERGY.

Radiometric Dating Occurs in IGNEOUS rocks. The RATE OF DECAY is CONSTANT! Scientists use that rate to determine AGE of a rock.

Radiometric Dating Half-Life The time it takes for half of the radioactive atoms to decay into another element. Parent material = Radioactive Element Daughter product = the stable element the radioactive element decays into. Example: Carbon 14 turns into Nitrogen 14 Carbon 14 = Parent material Nitrogen 14 = Daughter product Carbon-14’s half-life is 5,730 years. (what does that mean?) It takes 5,730 years for half of C14 atoms to decay into N14.

Radiometric Dating Potassium 40 – Argon 40 Dating (K  Ar) (Beta capture) Parent = Potassium 40 Daughter = Argon 40 Half-life = 1.3 billion years. Can be used to date rocks because of its long half-life. Why do you need a LONG half-life to date rocks? Because rocks are old so if half-life is short, there will be NO Parent element in the rock, only the Daughter product. You need Both to determine age.

Carbon-14 Nitrogen-14 Cycle All living things have C-14 in them. This begins to turn to N-14 the moment they die. Can only be used for dating if there is some C14 remaining in the organism

Radiometric Dating Carbon 14 – Nitrogen 14 (C14 – N14): (Beta emission) Called Carbon Dating. Only used for dating things ONCE LIVING. Decay begins when the organism dies. Only works for things YOUNGER than 75,000 yrs. Iceman found in in the European Alps. He died 53,000 years ago.

Radiometric Dating How to determine age of rock using Half-lives Half-life Parent element Daughter product 1 ½ 1/2 2 ¼ ¾ 3 1/8 7/8 4 1/16 15/16 Each Half-life: Parent goes down by ½ Daughter increases by that amount

Radiometric Dating NO This can be done by Percentage too. Half-Life Parent element Daughter product 100% 1 50% 2 25% 75% 3 12.5% 87.5% 4 6.25% 93.75% Mathmatically, does the Daughter product EVER reach 100%? NO

Radiometric Dating 17190 years ago! Now lets add HALF-LIFE YEARS. Parent element (C14) Daughter product (N14) 0 yrs 100% 0% 5730 yrs 50% 11,460 yrs 25% 75% 17190 yrs 12.5% 87.5% 22920 yrs 6.25% 93.75% So if we measured a sample of a mummy and found it to be 12.5% C14 and 87.5% N14, how long ago did he die? 17190 years ago!

Radiometric Dating Importance of Radiometric Dating Provided dates for events in Earth’s History. Supported beliefs of James Hutton, Charles Darwin and others who said Earth is VERY OLD. There has been enough time for major changes to have occurred geologically.

Geologic Time Scale Earth = 4.6 Billion years old (byo) Earth’s time span is SOOOO GREAT, that scientists have divided it into smaller units of time making the “Geologic Time Scale”. This division of time helps people grasp this expanse of time. Scientists used changes in major life-forms and extinctions to divide the time scale. The division of the time scale is broken into 4 sections.

Geologic Time Scale The 4 major divisions are??? Eon Era Period Epoch

Geologic Time Scale 88% of Earth’s History Other 12% PreCambrian Very little evidence of life. Other 12% Phanerozoic Sudden development of life in the oceans. Hard parts developed which increased the fossil record. Visible Life Single-cell

Geologic Time Scale Eras (Divided by major extinctions) Paleozoic (Hard parts developed) Marine animals thrived Pangaea formed Extinction 90% of marine animals became extinct. Mesozoic Dinosaurs developed Pangaea began to break up. Dinosaurs Cenozoic Mammals became dominant Humans evolved Mammals Dinosaur extinction Reptiles (Dino) Marine extinction Water animals Single-cell

Geologic Time Scale Dinosaurs Humans Lived on Earth for 150 million years. Humans Lived on Earth for 100 -200 thousand years. Mammals Dinosaur extinction Reptiles (Dino) Marine extinction Water animals Single-cell

Historical Geology THE END https://www.youtube.com/watch?v=9Ra9lwKn75s