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earth sci 2nd q
Methods of Knowing the Age of Events in Earth's History
Question | Answer |
---|---|
How old is the universe? | 13.8 billion years old (legal age na sya) |
How old is the Earth? | 4.54 billion years old |
How old is our dear old Luna (moon)? | 4.51 BILLIONYEARS OLD |
How old is organisms? | 3.8 BILLIONYEARS OLD!!! |
How old is man? | 200,000 –300,000YEARS OLD |
***** are recorders of time long before humans invented its concept. It holds the secrets to the past. | Rocks |
Who is the father of modern Geology?(The present is the key to the past) daw | JAMES HUTTON (1700s) |
Earth is approximately 24 – 40million years old -- Who discovered this? | LORD KELVIN(1897) |
Earth is approximately 90 – 100million years old Who discovered this? | JOHN JOLY(1901) |
What are the methods to it? | Relative Dating (oi ano ito) Absolute Dating Fossils |
What is relative dating? | Measures the comparative age of rocks (whichis younger or older) |
Three principles of relative dating? (intawn ano ba bakit relative) | Law of Superposition Law of Cross–Cutting Law of Inclusions |
What is the QUALITATIVE METHOD? | Relative Dating |
What is Law of Superposition? | In an undisturbed sequence of rocks, theOLDEST LAYER is found at the BOTTOM and theYOUNGEST LAYER is found at the TOP. |
What is Law of Cross–Cutting? | When faults / fractures cut through rocks, theevent of faulting / fracturing is always YOUNGERthan the rock it cuts. |
What is Law of Inclusion? | Any rock fragments included / embedded inanother rock is OLDER than the rocksurrounding it. |
What is Absolute Dating? | Determining the numericalage of materials usingradioactive isotopes (thesame elements ofdifferent mass numbers) |
What method is QUANTITATIVE? | Absolute Dating |
What is Isotope? | Atoms of the sameelements withdifferent massnumbers |
What is Radioactive Decay? | is the process ofbreakdown of anucleus to releaseenergy and matter |
Half–Life is? | The amount of timeit takes for half ofthe parent atom todecay into itsdaughter atom |
The third method: Fossils What is it about? | These are the preservedremains or traces oforganisms. This isimportant in determiningpossible age ofsedimentary rocks. |
What are conditions required for fossilization? | •Rapid Burial •Protective cover or medium •Possession of hard part or durable tissues (e.g. teeth, shells, bones) |
Types of Fossilization? | •Preservation without alteration •Preservation with alteration •Ichnofossils or Trace Fossils |
What is Preservation w/o alteration? | no major modificationof the chemistry ofthe remains occurred |
What is Preservation w/ alteration? | chemical composition is altered(PETRIFICATION, RECRYSTALLIZATION,CARBONIZATION) |
Whats petrification? | Replacement ofwoody materialwith minerals(wood becomes arock) |
Whats recrystallization? | Shells of organismsmade from calciumcarbonate becomescalcite. |
Whats carbonization? | Carbon componentof the remains areleft embedded insediments |
What is Ichnofossils or trace fossils: | percentage of organic remains is verysmall (includes molds, casts, etc.) |
Whats carbonization? | Carbon componentof the remains areleft embedded insediments |
What is Ichnofossils or trace fossils: | percentage of organic remains is verysmall (includes molds, casts, etc.) |
Whats carbonization? | Carbon componentof the remains areleft embedded insediments |
What is Ichnofossils or trace fossils: | percentage of organic remains is verysmall (includes molds, casts, etc.) |
What is Ichnofossils or trace fossils: | percentage of organic remains is verysmall (includes molds, casts, etc.) |
What is Preservation w/ alteration? | chemical composition is altered(PETRIFICATION, RECRYSTALLIZATION,CARBONIZATION) |
Whats petrification? | Replacement ofwoody materialwith minerals(wood becomes arock) |
Whats recrystallization? | Shells of organismsmade from calciumcarbonate becomescalcite. |
Whats carbonization? | Carbon componentof the remains areleft embedded insediments |
What is Ichnofossils or trace fossils: | percentage of organic remains is verysmall (includes molds, casts, etc.) |