SlideShare una empresa de Scribd logo
1 de 8
Name _________________________________                                 Earth Science
Interpreting Geologic History #1                                       Relative Age



THE PRINCIPLE OF UNIFORMITY:
     Geologists can infer events of the past by ____________________________

     ___________________________________________________________

     Uniformitarianism (Principle of _____________________________)
        states that the forces that acted upon the ______________________
         crust in the__________________ are the same as those that are
     ________________________ today.

****_______________________________________________________________****

Relative Dating Techniques: Five Basic Laws!

        1. Law of _______________________________________________

        2. Law of _______________________________________________

        3. Law of _______________________________________________

        4. Law of _______________________________________________

        5. Law of _______________________________________________

     1. Law of Original Horizontality:
     _________________________________________________________________
     _____________________________________________________________
     If strata are _______________ then they must have suffered some kine of
     disturbance after they were deposited.

     2. Law of Superposition- the principle that the _______________ layers

        in a sequence of rock strata must have been deposited _________________ the

        layers above, unless the rock strata have been ___________ or _____________.

       The __________rocks are found at the bottom. Geologists can date the
     ____________ ages of the strata from __________ to ___________ .
3. Law of Inclusions:
   A rock must first exist in order to be weathered,
   deposited and cemented as a ___________ in another rock.
    Therefore, If rock is composed of _________, the rock fragments must be
    _____________ than the rock in which they are found.




   _______ is older in A.    _____________ is older in B.

     The law of inclusions also applies to fossil preserved in bedrock.
_____________________ are any naturally preserved remains or impressions of
living things.

They are found in ___________________________________, because

_________________________________________________________________
  ______________________________________________________________

    Fossils give us information about
   __________________________________________________.



 4. Law of Cross-Cutting Relationships:
    Any ___________ or ____________ must be younger than ALL the rock through
    which it cuts. Simply put, the body of rock that is cross-cut had to be there first
    in order to be cut by an intruding igneous body or fault.

In general rock is always ____________________ than the process
that changed it.
Some processes include: ________________, ______________,
_________________, __________________ & ________________.

These changes can lead to exceptions to the Law of Superposition:
a. __________________________ is an igneous rock that formed from lava on
         the surface of the crust. An _____________________ must be younger than
         the strata below it, but   _________________ than any layers above.

         b. _____________________ are created when molten rock ( ____________) is

             injected into older rock layers in the crust. ___________ are ____________

                than all the rock layers in contact with them.

         c. ___________________ are bends in rock strata. _____________________
         can overturn

             rock strata so that ______________ rock lies on top of _____________rock.

         d. _________________ are cracks in rock strata. _______________ produce
         offset layers.

      Processes that can change the order of rock strata:

         Rock strata must be _________________ than the process that changed it.

      _________________, _______________ and __________________
      __________________
        are features created after rock or sediment has been deposited.

       5. Law of Original Lateral Continuity: When sediment is dumped by an agent of
erosion, strata extends from the source of deposition until it gradually thins to zero, or until
it reaches the edges of the basin of ____________________. This concept enables
geologists to correlate outcrops of strata that has been dissected by processes of
______________.


CORRELATION OF ROCK STRATA:
    A. Correlation is
       ______________________________________________________________

         ___________________________________________________________

         ______________________________________________________________
B. Ways to correlate rock formations:
        1. “Walking the outcrop” is done by
           ______________________________________________

           This is correlation by _____________________________________.
        2. You can match the rock strata in one location with the rock strata in more
           distant locations by
           ____________________________________________________________
           _______________

        3. Time correlation compares ______________ ________________ contained in
           rock the strata.
        4. The best index fossils:
           a. ______________________________________________________

           b. ______________________________________________________



        5. Another way of correlating layers by time is through
           ________________________________.

           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.

GEOLOGIC TIME SCALE:
Geologists noticed that rock __________________________ could be identified by the
fossils they contained. They also found that certain _____________________ were
consistently located

        _____________________ or ______________________ other formations.

        From these observations they established a
        ___________________ ____________ ___________

        With a sequence of fossil groups from _____________ to ______________each
     of these groups was named for a location where its __________________________
     could be observed in the rocks. Example:___________________________
Further observations from around the world established a
    _________________        ________________ __________________

       based on _______________________________________________

       AND _________________________ex:________________&______________

    An _________________________ is the process of mountain building.

    SEE PAGES 8 & 9 IN YOUR ESRT!!!

GEOLOGIC EVENTS OF THE PAST:

    A. _________________________ causes gaps in the geologic record.

    B. When a new layer of rock is laid down on a surface that has been
       __________________________,

       it forms a buried erosion surface called an
       _________________________________________.

    C. How an unconformity forms:
Name _________________________________                                        Earth Science
Interpreting Geologic History #2                                              Absolute Age

                                RADIOACTIVE DATING:

      Fossils enabled geologists to give __________________________ time,

      Measurements of natural _________________________ in rocks have

      allowed _________________ time scale to be an __________________ time scale.

      The ________________              _______________ of an object is measured in years.

      Chemical elements often have several forms called _________________________.

ISOTOPE:
      ______________________________________________________________

         ______________________________________________________________
Ex.
                      C             C



      If the nucleus has more or fewer than the normal number of ___________________,

      The isotope may be _______________________________.
      Radioactive isotope will break down naturally into a lighter element called

         _____________________                 _______________________.
         Carbon –14                      →
                                        C-14
         Potassium-40               K40 →
                                       →
         Uranium-238                U238 →
         Rubidium-87         Rb87   →

         Example: see front cover of reference table

 The rate of decay of a radioactive element is measured by it’s ___________ _________
HALF-LIFE:
_____________________________________________________________________

Complete the Chart using your Reference Table:

        RADIOACTIVE ELEMENT                 DECAY PRODUCT                HALF-LIFE

1    Carbon-14

2    Potassium-40

3    Uranium-238

4    Rubidium-87



       Calculating the age of a rock:
1. What would be the age of the rock that has equal amounts of
   C-14 and its decay product N-14?




2. What % of the sample is radioactive after the following half-lives,

       After 1 half-life:



       After 2 half-lives:



       After 3 half-lives:

    3. After 11,200 years how much C-14 would remain in a 10 gram sample?

       Selecting the Best Radioactive Element:

      AGE OF SAMPLE                                RADIOACTIVE ELEMENT

1     Under 50,000 (RECENT)

2     Over 50,000 (OLDER)
* Carbon-14 is used for dating: _____________________________________________

                        & _____________________________________________

Más contenido relacionado

Destacado (20)

ttt
tttttt
ttt
 
Presentation1
Presentation1Presentation1
Presentation1
 
9 Things I've Learned About Content While Running A Content Agency
9 Things I've Learned About Content While Running A Content Agency9 Things I've Learned About Content While Running A Content Agency
9 Things I've Learned About Content While Running A Content Agency
 
End child hunger
End child hungerEnd child hunger
End child hunger
 
Rocks of the esrt guide
Rocks of the esrt guideRocks of the esrt guide
Rocks of the esrt guide
 
Fem la mona
Fem la monaFem la mona
Fem la mona
 
Entrepreneurship
EntrepreneurshipEntrepreneurship
Entrepreneurship
 
Gusdur dan papua
Gusdur dan papuaGusdur dan papua
Gusdur dan papua
 
Offscreenparticle
OffscreenparticleOffscreenparticle
Offscreenparticle
 
Masa Depanku Andhika 6 C
Masa Depanku Andhika 6 CMasa Depanku Andhika 6 C
Masa Depanku Andhika 6 C
 
Create a Rain garden
Create a Rain gardenCreate a Rain garden
Create a Rain garden
 
California Budget Crisis
California Budget CrisisCalifornia Budget Crisis
California Budget Crisis
 
7. microsoft excel 1
7. microsoft excel 17. microsoft excel 1
7. microsoft excel 1
 
Ud 2 TectóNica De Placas Proba
Ud 2 TectóNica De Placas ProbaUd 2 TectóNica De Placas Proba
Ud 2 TectóNica De Placas Proba
 
Mobile applications
Mobile applicationsMobile applications
Mobile applications
 
Keyword Research for Pay-Per-Click Marketing
Keyword Research for Pay-Per-Click MarketingKeyword Research for Pay-Per-Click Marketing
Keyword Research for Pay-Per-Click Marketing
 
Good one
Good oneGood one
Good one
 
Contours123
Contours123Contours123
Contours123
 
Citizen Presentation
Citizen PresentationCitizen Presentation
Citizen Presentation
 
Nerva Nevada
Nerva NevadaNerva Nevada
Nerva Nevada
 

Similar a Interpreting geologic history through relative and absolute dating techniques

Similar a Interpreting geologic history through relative and absolute dating techniques (20)

Landscape Outline
Landscape OutlineLandscape Outline
Landscape Outline
 
Dynamic earth
Dynamic earthDynamic earth
Dynamic earth
 
Earth Quake Outline
Earth Quake OutlineEarth Quake Outline
Earth Quake Outline
 
Deposition Outline
Deposition OutlineDeposition Outline
Deposition Outline
 
Np rocks and minerals
Np rocks and mineralsNp rocks and minerals
Np rocks and minerals
 
Interpreting Geologic History Updated
Interpreting Geologic History UpdatedInterpreting Geologic History Updated
Interpreting Geologic History Updated
 
Interpreting geologichistoryupdated2
Interpreting geologichistoryupdated2Interpreting geologichistoryupdated2
Interpreting geologichistoryupdated2
 
Notes Rock Cycle
Notes Rock CycleNotes Rock Cycle
Notes Rock Cycle
 
Notes rock cycle
Notes rock cycleNotes rock cycle
Notes rock cycle
 
Dynamic earth np1
Dynamic earth np1Dynamic earth np1
Dynamic earth np1
 
Dynamic Earth Note Packet
Dynamic Earth Note PacketDynamic Earth Note Packet
Dynamic Earth Note Packet
 
Interpreting Geologic History Power Point
Interpreting Geologic History Power PointInterpreting Geologic History Power Point
Interpreting Geologic History Power Point
 
Weathering Outline
Weathering OutlineWeathering Outline
Weathering Outline
 
Station #4
Station #4Station #4
Station #4
 
Chapter 23 note guide
Chapter 23 note guideChapter 23 note guide
Chapter 23 note guide
 
Ppt cloze notes
Ppt cloze notesPpt cloze notes
Ppt cloze notes
 
Weathering Outline For Sci 8
Weathering Outline For Sci 8Weathering Outline For Sci 8
Weathering Outline For Sci 8
 
Outline: Chapter 16.3: Absolute Age Dating
Outline: Chapter 16.3: Absolute Age DatingOutline: Chapter 16.3: Absolute Age Dating
Outline: Chapter 16.3: Absolute Age Dating
 
Mineral notes
Mineral notesMineral notes
Mineral notes
 
Mountains%2c earthquakes%2c volcanoes notes
Mountains%2c earthquakes%2c volcanoes notesMountains%2c earthquakes%2c volcanoes notes
Mountains%2c earthquakes%2c volcanoes notes
 

Más de West Hollow MS Ms. Gill (20)

Welcome to Regents Earth Science
Welcome to Regents Earth ScienceWelcome to Regents Earth Science
Welcome to Regents Earth Science
 
Syllabus earth science
Syllabus earth scienceSyllabus earth science
Syllabus earth science
 
Prologue pp1 2012
Prologue pp1 2012Prologue pp1 2012
Prologue pp1 2012
 
Prologue np1 2012
Prologue np1 2012Prologue np1 2012
Prologue np1 2012
 
Geologic History Note Packet
Geologic History Note PacketGeologic History Note Packet
Geologic History Note Packet
 
Geologic History Powerpoint Notes
Geologic History Powerpoint NotesGeologic History Powerpoint Notes
Geologic History Powerpoint Notes
 
Earthquakes final
Earthquakes finalEarthquakes final
Earthquakes final
 
Earthquakes final
Earthquakes finalEarthquakes final
Earthquakes final
 
Plates ex2
Plates ex2Plates ex2
Plates ex2
 
Plates Lab
Plates LabPlates Lab
Plates Lab
 
Oceans and Basin Do Now
Oceans and Basin Do NowOceans and Basin Do Now
Oceans and Basin Do Now
 
Pangaea lab
Pangaea labPangaea lab
Pangaea lab
 
Ocean bottom profiles
Ocean bottom profilesOcean bottom profiles
Ocean bottom profiles
 
Global Tectonic Plates HW
Global Tectonic Plates HWGlobal Tectonic Plates HW
Global Tectonic Plates HW
 
Earths Interior Questions HW
Earths Interior Questions HWEarths Interior Questions HW
Earths Interior Questions HW
 
Dynamic Earth
Dynamic EarthDynamic Earth
Dynamic Earth
 
Earths dimension sci 8 ppt np1
Earths dimension sci 8 ppt np1Earths dimension sci 8 ppt np1
Earths dimension sci 8 ppt np1
 
Metamorphic Rocks
Metamorphic RocksMetamorphic Rocks
Metamorphic Rocks
 
Igneous Rocks
Igneous RocksIgneous Rocks
Igneous Rocks
 
Sedimentary rocks of the esrt
Sedimentary rocks of the esrtSedimentary rocks of the esrt
Sedimentary rocks of the esrt
 

Interpreting geologic history through relative and absolute dating techniques

  • 1. Name _________________________________ Earth Science Interpreting Geologic History #1 Relative Age THE PRINCIPLE OF UNIFORMITY: Geologists can infer events of the past by ____________________________ ___________________________________________________________ Uniformitarianism (Principle of _____________________________) states that the forces that acted upon the ______________________ crust in the__________________ are the same as those that are ________________________ today. ****_______________________________________________________________**** Relative Dating Techniques: Five Basic Laws! 1. Law of _______________________________________________ 2. Law of _______________________________________________ 3. Law of _______________________________________________ 4. Law of _______________________________________________ 5. Law of _______________________________________________ 1. Law of Original Horizontality: _________________________________________________________________ _____________________________________________________________ If strata are _______________ then they must have suffered some kine of disturbance after they were deposited. 2. Law of Superposition- the principle that the _______________ layers in a sequence of rock strata must have been deposited _________________ the layers above, unless the rock strata have been ___________ or _____________. The __________rocks are found at the bottom. Geologists can date the ____________ ages of the strata from __________ to ___________ .
  • 2. 3. Law of Inclusions: A rock must first exist in order to be weathered, deposited and cemented as a ___________ in another rock. Therefore, If rock is composed of _________, the rock fragments must be _____________ than the rock in which they are found. _______ is older in A. _____________ is older in B. The law of inclusions also applies to fossil preserved in bedrock. _____________________ are any naturally preserved remains or impressions of living things. They are found in ___________________________________, because _________________________________________________________________ ______________________________________________________________ Fossils give us information about __________________________________________________. 4. Law of Cross-Cutting Relationships: Any ___________ or ____________ must be younger than ALL the rock through which it cuts. Simply put, the body of rock that is cross-cut had to be there first in order to be cut by an intruding igneous body or fault. In general rock is always ____________________ than the process that changed it. Some processes include: ________________, ______________, _________________, __________________ & ________________. These changes can lead to exceptions to the Law of Superposition:
  • 3. a. __________________________ is an igneous rock that formed from lava on the surface of the crust. An _____________________ must be younger than the strata below it, but _________________ than any layers above. b. _____________________ are created when molten rock ( ____________) is injected into older rock layers in the crust. ___________ are ____________ than all the rock layers in contact with them. c. ___________________ are bends in rock strata. _____________________ can overturn rock strata so that ______________ rock lies on top of _____________rock. d. _________________ are cracks in rock strata. _______________ produce offset layers. Processes that can change the order of rock strata: Rock strata must be _________________ than the process that changed it. _________________, _______________ and __________________ __________________ are features created after rock or sediment has been deposited. 5. Law of Original Lateral Continuity: When sediment is dumped by an agent of erosion, strata extends from the source of deposition until it gradually thins to zero, or until it reaches the edges of the basin of ____________________. This concept enables geologists to correlate outcrops of strata that has been dissected by processes of ______________. CORRELATION OF ROCK STRATA: A. Correlation is ______________________________________________________________ ___________________________________________________________ ______________________________________________________________
  • 4. B. Ways to correlate rock formations: 1. “Walking the outcrop” is done by ______________________________________________ This is correlation by _____________________________________. 2. You can match the rock strata in one location with the rock strata in more distant locations by ____________________________________________________________ _______________ 3. Time correlation compares ______________ ________________ contained in rock the strata. 4. The best index fossils: a. ______________________________________________________ b. ______________________________________________________ 5. Another way of correlating layers by time is through ________________________________. 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. GEOLOGIC TIME SCALE: Geologists noticed that rock __________________________ could be identified by the fossils they contained. They also found that certain _____________________ were consistently located _____________________ or ______________________ other formations. From these observations they established a ___________________ ____________ ___________ With a sequence of fossil groups from _____________ to ______________each of these groups was named for a location where its __________________________ could be observed in the rocks. Example:___________________________
  • 5. Further observations from around the world established a _________________ ________________ __________________ based on _______________________________________________ AND _________________________ex:________________&______________ An _________________________ is the process of mountain building. SEE PAGES 8 & 9 IN YOUR ESRT!!! GEOLOGIC EVENTS OF THE PAST: A. _________________________ causes gaps in the geologic record. B. When a new layer of rock is laid down on a surface that has been __________________________, it forms a buried erosion surface called an _________________________________________. C. How an unconformity forms:
  • 6. Name _________________________________ Earth Science Interpreting Geologic History #2 Absolute Age RADIOACTIVE DATING: Fossils enabled geologists to give __________________________ time, Measurements of natural _________________________ in rocks have allowed _________________ time scale to be an __________________ time scale. The ________________ _______________ of an object is measured in years. Chemical elements often have several forms called _________________________. ISOTOPE: ______________________________________________________________ ______________________________________________________________ Ex. C C If the nucleus has more or fewer than the normal number of ___________________, The isotope may be _______________________________. Radioactive isotope will break down naturally into a lighter element called _____________________ _______________________. Carbon –14 → C-14 Potassium-40 K40 → → Uranium-238 U238 → Rubidium-87 Rb87 → Example: see front cover of reference table The rate of decay of a radioactive element is measured by it’s ___________ _________
  • 7. HALF-LIFE: _____________________________________________________________________ Complete the Chart using your Reference Table: RADIOACTIVE ELEMENT DECAY PRODUCT HALF-LIFE 1 Carbon-14 2 Potassium-40 3 Uranium-238 4 Rubidium-87 Calculating the age of a rock: 1. What would be the age of the rock that has equal amounts of C-14 and its decay product N-14? 2. What % of the sample is radioactive after the following half-lives, After 1 half-life: After 2 half-lives: After 3 half-lives: 3. After 11,200 years how much C-14 would remain in a 10 gram sample? Selecting the Best Radioactive Element: AGE OF SAMPLE RADIOACTIVE ELEMENT 1 Under 50,000 (RECENT) 2 Over 50,000 (OLDER)
  • 8. * Carbon-14 is used for dating: _____________________________________________ & _____________________________________________