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Interpreting Geologic History
If the history of our planet was condensed to only  one year , when would the “important” events in our history have taken place? Earth’s History  in One Year
[object Object]
 
January to March ,[object Object]
[object Object]
 
April to November ,[object Object],[object Object],[object Object],[object Object]
 
December  ,[object Object],[object Object]
December 6 th ,[object Object],[object Object],[object Object]
December 7 th   ,[object Object],[object Object]
 
December 10 th ,[object Object],[object Object],[object Object],[object Object]
 
December 17 th ,[object Object],[object Object]
December 20 th ,[object Object],[object Object]
It’s snack time!!! AHHH!!!
December 24 th ,[object Object],[object Object]
December 25 th ,[object Object],[object Object],[object Object]
December 28 th   ,[object Object]
December 31 st   ,[object Object],[object Object],[object Object]
 
The Last Hour on December 31 st   ,[object Object],[object Object],[object Object],[object Object]
 
 
The Last Minute of the Year! ,[object Object]
The Last Minute of the Year! ,[object Object]
The Last Second of the Year! ,[object Object]
What Will the New Year Bring?
Welcome Back! Please complete the pre-test when you come in!
The Grand Canyon, AZ Geologic History A Journey Through Time Please take out your Earth's History Notes Packet
Geologic History Intro and Relative Dating Absolute Dating Fossils & Rock Correlations Geologic Time Life and Evolution “Do Now’s” and HW
Who’s Younger? How Do You Know??
“ in a Nutshell” Geologic History of the Earth
Origins of our Solar System Video Clip
[object Object],[object Object],[object Object],Earth’s Formation
Creation of the Earth
 
Earth's first atmosphere 4.6 billion years ago was most likely comprised of hydrogen and helium (two most abundant gases found in the universe!) Through the process of  outgassing, the outpouring of gases from the earth's interior, many other gases were injected into the atmosphere. These include: water vapor (produced rain - rivers, lakes, oceans) carbon dioxidenitrogenAs outgassing occurred over a period of millions of years, the atmosphere evolved to its current state
Life and Evolution Diverse Ordovician Sea-Life Video Clip
[object Object],Variations in Fossils and Environments
[object Object],[object Object],Variations in Fossils and Environments
[object Object],[object Object],Fossils and the Evolution of Life
[object Object]
[object Object],[object Object],[object Object],Rates of Evolution
[object Object],[object Object],Rates of Evolution
[object Object],[object Object],[object Object],Life On Earth Throughout Geologic Time
Stromatolites Formed from the trapping of sediment in layers by  Blue-Green Algae  (Cyanobacteria)
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Life On Earth Throughout Geologic Time
Cambrian Life
Silurian Life
Eurypterid  (Sea Scorpion)  Fossil Largest fossil with human for scale
 
Eurypterid in Action
Devonian Life
Phacops Trilobite of the Devonian
Carboniferous Forests – formed extensive coal deposits
Evolution of Amphibian from Lobe-Finned Fish (Devonian)
 
[object Object],[object Object],[object Object],[object Object],Life On Earth Throughout Geologic Time
Triassic Plateosaurs
 
Iguanodons
 
Cretaceous T-Rex
Impact Event
[object Object],[object Object],[object Object],Life On Earth Throughout Geologic Time
Early Hominids Mastodonts
 
ESRT, p. 8-9
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],How old is the Earth? For example, 10 9  can be read as “one with 9 zeroes after it”  OR 1,000,000,000
 
 
[object Object],[object Object],Birth of Modern Geology
[object Object],[object Object],Principle of Uniformitarianism Hutton's Major Contribution
THE PRINCIPLE OF UNIFORMITY: ,[object Object],Looking  at features  of rocks and rock outcrops
Uniformitarianism (Principle of   ,[object Object],[object Object],Uniformity) Earth’s
[object Object],[object Object],past active ** THE KEY TO THE PAST IS THE PRESENT**
Relative Dating Techniques
[object Object],[object Object],Relative Dating
5 Basic Laws:  ,[object Object],[object Object],[object Object],[object Object],[object Object]
Law of Original Horizontality ,[object Object],[object Object]
Law of Original Horizontality ,[object Object],Grand Canyon Western Iran Steeply Inclined
[object Object],Layer 1 – Siltstone  Layer 2 – Limestone  Layer 3 – Sandstone  Relative Dating Laws
What has happened to this rock strata?
Did it happen before or after the rock had formed? What has happened to this rock strata?
THE LAW OF SUPERPOSITION: ,[object Object],bottom before disturbed uplifted
[object Object],[object Object],[object Object],[object Object],older relative oldest youngest
oldest youngest
Law of Superposition ,[object Object]
[object Object],Relative Dating Laws
 
Younger   Older      Oldest
Grand Canyon,   Sequence of Strata Oldest Youngest Which rock unit is the  youngest? oldest?
Grand Canyon,  Sequence of Strata
 
Older Younger Sheep Rock, Central OR
Law of Inclusions ,[object Object],clast
[object Object],fragments older
Law of Inclusions Which is older the Granite or the Sandstone? In figure A?  In figure B?  Sandstone is older Granite is older
What's the oldest part of this rock? Youngest?
[object Object]
[object Object],Fossils
[object Object],[object Object],[object Object],Sedimentary rock Heat & pressure in  igneous and metamorphic  rock destroys them
FOSSILS GIVE US INFORMATION ABOUT THE ANCIENT ENVIRONMENT  AND CLIMATE
ESRT pp. 8-9
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Gastropods Worthenia
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Mucospirifer Brachiopods
[object Object],[object Object],[object Object],[object Object],Trilobites Phacops
 
[object Object],[object Object],[object Object],[object Object],Nautiloids and Ammonoids
 
[object Object],[object Object],[object Object],[object Object],[object Object],Cnidaria (Corals)
 
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Eurypterids NYS Fossil
                                                                       
 
[object Object],[object Object],Graptolites
[object Object],[object Object],[object Object],[object Object],[object Object],Crinoids
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Bivalves
 
 
 
 
 
 
 
 
 
 
Unconformity ,[object Object]
Rock Fragments  (or Inclusions) that are contained in another rock are  older  than the rocks in which they are found Unconformity
Law of Cross-Cutting Relationships ,[object Object],Igneous rock fault
[object Object],older
Some Processes Include: ,[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],Principle of Cross-Cutting Relationships
Fault Fold Principle of Cross-Cutting Relationships
How does the age of the fault compare  to the age of the rock layers?
Folded Rock Strata
How does the age of the crack compare to the age of the rock?
 
Principle of Cross-Cutting Relationships
Sedimentary layers (the law of original horizontality)
Sedimentary layers
Sedimentary layers
Sedimentary layers
Sedimentary layers
The fault came after  the rock was formed
Sedimentary layers The tilt came after the  the rock was formed
The extrusion came after the rock was formed 1 2 3 4 5 Contact metamorphism
1 2 3 4 5 6 The extrusion came after the lower layers were formed but…. Before the top layer
1 2 3 4 5 This intrusion came after all the layers
 
[object Object],[object Object],[object Object],extrusion
[object Object],extrusion older
[object Object],intrusions magma
[object Object],[object Object],[object Object],Intrusions younger
[object Object],[object Object],Folds folding older younger
 
 
[object Object],[object Object],[object Object],Faults Faults
[object Object],[object Object],[object Object],Faults Faults
[object Object],[object Object],older
[object Object],[object Object],cracks veins natural cement
 
The following diagram represents a cross-sectional view of a portion of Earth’s crust.  What is the relative age of the igneous rock? The igneous rock is older than the … The igneous rock is younger than the …
Law of Original Lateral Continuity ,[object Object],deposition
Folding of strata (rock layers) over upon itself Possible Exceptions to the  Law of Superposition
Strata is displaced by a Fault ( Thrust Fault ) Possible Exceptions to the  Law of Superposition
Law of Original Lateral Continuity
Law of Original Lateral Continuity ,[object Object],erosion
Let’s follow the progression of geological events that formed the sequence below.
Step  One Deposition of rock units A-E
Step  Two Area is uplifted, and is intruded by rock unit D (Sill)
Step  Three Intrusion of rock unit F (Dike)
Step  Four The rock sequence is tilted and then eroded, setting the stage for an angular unconformity
Step  Five Area subsides, followed by the deposition of rock units G-K
Step  Six Area is uplifted and the upper surface begins to undergo erosion
 
That is the story behind this rock sequence
Fossils & Rock Correlations
CORRELATION OF ROCK STRATA: ,[object Object],Matching similar rock strata at different locations  to see  if they formed at the same time
 
[object Object],[object Object],Rock Correlation
[object Object],[object Object],[object Object]
 
Grand Canyon Stratigraphy
 
 
 
 
 
[object Object],Unconformity Fossil Evidence and Rock Correlation
Correlation using Index Fossils
Ways to correlate rock formations: ,[object Object],[object Object],Walking from  end to end
[object Object],continuity
You can match the rock strata in one location with rock strata in more distant locations by Comparing ,  c o l o r texture composition sequence of layers
Time correlation compares ____________ contained in the rock strata index fossils 1 2 3 4 4 5 6 3
The best index fossils: ,[object Object],[object Object],Exist for a brief  period of time are widespread
Which fossil would  make the best index fossil? Found in only 1 layer (short lived) Found in all samples (widespread)
Another way of correlating layers by time is through ___________________ Volcanic ash falls
These ash falls are very ________ events. A single layer of ______ can be   found over a large area, this allows geologists to make a__________________ from one location to another at the position of a common ash fall. brief ash time correlation
Volcanic Eruptions and Rock Correlation ,[object Object],[object Object]
 
Rock Correlation Activity
Rock Correlation Activity
GEOLOGIC TIME SCALE: ,[object Object],formations
[object Object],formations above below
[object Object],[object Object],[object Object],[object Object],relative  time  scale oldest youngest
[object Object],Characteristic  fossil Example: Devon fossil  “ Devonian ”  found in  Devon England
[object Object],[object Object],Geologic  time  scale
[object Object],[object Object],[object Object],Inferred positions of Earth’s Landmasses  Major Geologic Events (ex. Ice ages & Orogenys)
[object Object],Geologic Time
[object Object],[object Object],Orogeny
 
 
GEOLOGIC EVENTS OF THE PAST: ,[object Object],Erosion MISSING LAYERS
[object Object],[object Object],[object Object],Eroded, unconformity
NEW BOTTOM LAYER  APPEARS (EMERGES)
LAYER C IS MISSING EROSION
EROSION
THE UNCONFORMITY IS THE BURIED EROSIONAL SURFACE BETWEEN B AND D
 
 
Who’s Younger? How Do You Know??
Relative vs. Absolute Dating ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Michael Susan Ashley Melanie Anthony
[object Object],[object Object],[object Object],[object Object],[object Object]
What were some of the techniques used to determine absolute time prior to the discovery of radioactivity. Tree Rings Varves
 
[object Object],Modern Absolute Dating Techniques
Mass spectrometer –  instrument used in the detection and study of isotopes
VII. RADIOACTIVE DATING: ,[object Object],relative
Relative Time ,[object Object],[object Object],each other
However,  ,[object Object],geologic absolute radioactivity
[object Object],[object Object],absolute  age
[object Object],isotopes
[object Object],Modern Absolute Dating Techniques
Let’s review the  structure of an  atom The basic building  block of matter Basic Chemistry Review
[object Object],[object Object],[object Object],Basic Chemistry Review
[object Object],[object Object],Basic Chemistry Review
[object Object],[object Object],How can we use radioactive  elements to date things?
ISOTOPE: An unstable element with different number of neutrons than a normal (stable) element.  (Its unstable so wants to change to stable)
EX. C C 6 6 12 14 6 protons  6 protons 6 neutrons Unstable 8 neutrons
EX. C C 6 6 12 14 6 protons  6 protons 6 neutrons  8 neutrons unstable
D. If the nucleus has more or fewer than the normal number of  ____________, the isotope may be  ____________ neutrons radioactive (unstable)
[object Object],[object Object],decay  product
This process is called… Radioactive Decay
RADIOACTIVE DECAY: ,[object Object],DAUGHTER PARENT
[object Object],100
[object Object]
[object Object],fewer
[object Object],older
[object Object],decay product ratio
[object Object],random
[object Object],different
[object Object],half  life
HALF-LIFE: ,[object Object],[object Object],[object Object]
Original=100% Decay product=0% 100/0 Or  1 to 0
Original=50% Decay product=50% 50/50  Or  1 to 1 After one Half-life:
Original=25% Decay product=75% 25/75 Or  1:3  After two Half-lives:
Original=12.5% Decay product=87.5% 12.5/87.5 After three Half-lives:
Original=6.25% Decay product=93.75% 6.25/93.75 After four Half-lives:
[object Object],[object Object],Half-Life
 
[object Object],[object Object],Radioactive Dating
“ Daughter Product” “ Parent Material”
Carbon Dating 0 Half-Life Key Other C 14 N 14
Carbon Dating 1 Half-Life  (5,700 years) Key Other C 14 N 14
Carbon Dating 2 Half-Lives  (11,400 years) Key Other C 14 N 14
Carbon Dating 3 Half-Lives  (17,100 years) Key Other C 14 N 14
Carbon Dating 4 Half-Lives  (22,800 years) Key Other C 14 N 14
Carbon Dating 5 Half-Lives  (28,500 years) Key Other C 14 N 14
Carbon Dating 5 Half-Lives  (28,500 years) Key Other C 14 N 14
(ESRT, pg. 1) Which isotope has the shortest half life? Longest?
1/16  1/32 1/64  22,800 28,500 34,200 Old REGENTS Questions
Do Now How many Potassium-40 half lives have passed if there are 3 times more Argon-40 atoms than Potassium-40 atoms?  What if there are 3 times as many Potassium-40 atoms?
[object Object],[object Object],Can all rocks be dated  using this technique?
[object Object],[object Object],[object Object],[object Object],How does this Technique Work?
Decay of  U-238 If this rock were to be found today, and contained a 1:1 ratio, equal quantities of both U 238  to Pb 206 , it would be concluded that the rock formed 4.5 b.y.   How old would the sample be if it had a 1:3 ratio of U-238 to Pb-206?
[object Object],[object Object],Using Different Isotopes  for Different Studies
Carbon-14 (C 14 ) ,[object Object],[object Object]
Let’s examine the breakdown of Carbon-14
N 14 Ar 40 Pb 206 Sr 87 5.7 x 10 3 1.3 x 10 9 4.5 x 10 9 4.9 x 10 10 Element  Decay Product  Half-life
[object Object],dies wood fire
[object Object],[object Object]
One half life has gone by ,[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],50% 25% 12.5%
[object Object],25% or  2.5 grams 1/4 of the original  amount
I. Selecting the Best Radioactive Element: ,[object Object],[object Object],Use Carbon-14 Use Uranium-238
[object Object],[object Object],[object Object]
State the best isotope to use to discover the age of the individual “caught off guard” in the cartoon below. Why?
DO NOW Please pick up a copy of the  Absolute Dating Lab!
Do Now’s
The following diagram represents a cross-sectional view of a portion of Earth’s crust showing sedimentary rock layers that have not been overturned.  The letters identify the specific layers.  Which rock layer is the oldest? Youngest? DO NOW
What is represented by line A-B?
List the rock layers from oldest to youngest. A D C E B B A, D, C, E, B Do Now Take out your HW!!!
C D E B A G F H I Dating the Lunar Surface
C D E A H I G F B
Do we remember this stuff... What is the evidence that indicates the fault is the most recent geologic event to have occurred in this area?
What is the evidence that indicates rock layer B is younger than layers A and C? Earth Science Review Concepts
How does the age of the igneous intrusion [B]  compare with the age of the shale [F]?
The most apparent buried erosional surface  is found between which rock units?
E D B A C Can you figure this out?
[object Object],[object Object],The time required for half of the atoms in a given mass of a radioactive isotope  to decay Rubidium-87 Spend a moment and look this up...
Do Now Which letter (A,B,C) represents one half-life?
Do Now How much time is represented by letter B?
Take out your HW
Do Now Which isotope (A, B, C, D) has the shortest half-life?
Do Now Which isotope is represented by line B? (use your ESRT, p. 1)
Do Now Take out your HW
DO NOW Please take out your  Absolute Dating Lab
Do Now Clear your desks  and get ready  for the Quest!!!
Decay and Growth Curve of Isotopes Take out your HW! Notes Packet, p. 13 - Radon decays into radioactive solids - Half -Life of 4.5 days - Generated during the decay of Uranium - Inhalation of Radon or decay products may cause lung cancer Radon Facts
Explain how radioactive isotopes are used to  find the absolute age of a rock, bone, fossil?
State the name of the isotopes in the graph.
Which rock layer is the oldest?
Which is older, rock layer F or rock layer D?
What is an unconformity?
[object Object],[object Object],Take out your HW ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],9. 4 10. 3 11. 1 12. 3 13. 2 14. 4 15. 4
Take out your Marsium Lab DO NOW 1 half-life Sample Data
Which rock layer is the oldest? _______  _____
What evidence suggests that rock layer D  is older than layer C?
Which is older, rock layer F or rock layer D?
E D B A C State the age of the rocks in order from oldest to youngest.
How does the age of the igneous intrusion [B]  compare with the age of the shale [F]?
What is represented by line A-B?
What is an unconformity?
What evidence indicates that an unconformity exists between layers A and B?
The most apparent buried erosional surface  is found between which rock units?
Explain why radioactive isotopes are used to  find the absolute age of a rock, bone, fossil? _______  _____
How many half-lives are represented by  letter A, B, & C?
State the name of the isotopes in the graph.
Which isotopes are represented by  the following graphs (A, B, C)? A B C
Ms. Gill’s Baby Picture Clear your desks  and get ready  for the Quest!!!
What is the story here? 1
What is the story here? 2
What is the story here? 3
What is the story here? 4
What is the story here? 5
What is the story here? 6
What is the story here? 7
What is the story here? 8
What is the story here? 9
What is the story here? 10
What is the story here? 11
What are the rules for reading rock layers? ,[object Object],[object Object],[object Object],[object Object],[object Object]
Thanks to the collective resources of ESPRIT for contributing images Design via Threadless
Practice: what happened here?
 
Practice: what happened here?
 
Practice: what happened here?
 
Practice Geologic Profiles Look at the geologic profiles, write down what you think is the correct sequence of events.  Then click the mouse to advance the presentation.  Repeat this process for each of the profiles.
Profile 1 ,[object Object],[object Object],[object Object],[object Object],[object Object],Sequence of Events Remember the law of superposition. Oldest Youngest
Profile 2 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Sequence of Events Faults are younger than the rock they are in. How do you know there is a fault?  Look for the same rock layers. They do not line up.
Profile 3 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Sequence of Events Do you know what this is? An unconformity! These two steps formed it. Remember this a buried erosional surface
Profile 4 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Sequence of Events Intrusions and extrusions are younger than the rock they are in. Metamorphic rock tells you whether you have an intrusion or an extrusion .
Profile 5 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Sequence of Events Magma was forced in between the existing layers of rock to create this formation. You know it is an intrusion because… Metamorphic rock is on all sides.
Exposed volcanic ash layers in Alaska provide an excellent unit for correlation and establishing ages for geologic units and events
Rock Correlation Activity Create a full sequence of strata from these four different outcrops.
Rock Correlation Activity
Rock Correlation Activity
What can you infer happened in this area  based on these footprints (trace fossils)?
Geologic Timeline
[object Object],[object Object],Fossils of organisms that lived for a  short  period of time over a  wide  geographic area Volcanic ash deposits cover a large geographic area in a relatively short period of time You and your neighbor need to be  able to complete these questions.  Use your notes to help (p. 14-15)
_  __
_  __
_  __ Take out your HW Notes, p. 16-17
Take out a pencil, ESRT and calc. QUIZ TIME!
[object Object],[object Object],_  __ Take out your ESRT (p. 8-9) and complete the  following questions with your neighbor... An Era is larger and they are broken up into Periods Quaternary Period, Holocene Epoch
Which geologic period ended with the extinction of many kinds of marine animals, including trilobites? Which orogeny was caused by the collision of North America and Africa along a transform margin creating Pangaea? The Permian Period The Appalachian (Alleghanian) Orogeny _  __ Use your ESRT to complete the following Questions
The Devonian aged siltstone shown in the photograph below occurs as surface bedrock in Hamilton, NY.  What does the presence of the fossil suggest about the environment of Hamilton during the Devonian? _  __
Earth's History Notes Packet, p. 23
_  __ Use your ESRT [p. 8-9] to complete the following question
_  __ Mr. Gill's Baby Picture Please take out your ESRT
The table below gives information about the radioactive decay of carbon-14. Part of the table has been deliberately left blank for student use. After how many years will 1/128 of the original carbon-14 remain?
What is the correct order of development from the original (oldest) stage to the most recent (youngest) stage? DO NOW Work with a partner
Constructed Response Questions State one method used to correlate rock layers… State one piece of evidence why the limestone is the most resistant rock layer in the outcrops. Comparing rock texture / composition, looking for index fossils, examining sequencing of strata The limestone unit extends the furthest out of the outcrop (cliff)
Constructed Response Questions What does the discovery of Ordovician aged fossil corals in the surface bedrock of NYS cause you to infer? Parts of NYS were once in a shallow, warm marine envrionment

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INTERPRETING HISTORY

Notes de l'éditeur

  1. Click to see arrows shoot in one at a time. #1= included fragments #2=intrusion, cross-cutting #3= angular unconformity #4=erosion. This is the outcome of the next slide.
  2. Sediments deposited, sea-level lowered, layers intruded, layers tilted, erosion and deposition under sea, sea-level lowered again. Click arrow to continue.
  3. Click to see arrows shoot in one at a time. #1= included fragments #2=intrusion, cross-cutting #3= angular unconformity #4=erosion. This is the outcome of the next slide.
  4. Sediments deposited, sea-level lowered, layers intruded, layers tilted, erosion and deposition under sea, sea-level lowered again. Click arrow to continue.
  5. Click to see arrows shoot in one at a time. #1= included fragments #2=intrusion, cross-cutting #3= angular unconformity #4=erosion. This is the outcome of the next slide.
  6. Sediments deposited, sea-level lowered, layers intruded, layers tilted, erosion and deposition under sea, sea-level lowered again. Click arrow to continue.