HISTORY OF EARTH Flashcards

1
Q

THE PRINCIPLE IS THE KEY TO THE PAST QHICH IS BASED ON THE PRINCIPLE THAT NATURALLY LAWS HAVE REMAINED THROUGH OUT TIME

A

UNIFORMITARIANISM

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2
Q

ALSO KNOWN AS THE DOCTRINE OF UNIFORMITY

A

UNIFORMITARIANISM

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3
Q

FORMED IN LAYER, PRIVIDE USEFUL INFORMATION IN RELATIVE DATING

A

SEDIMENTARY ROCKS

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4
Q

THEY ARE FORMED FROM FRAGMENTS OF OTHER TYPES OF ROCKS

A

SEDIMENTARY ROCKS

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5
Q

NEW SEDIMENTARY ROCKS LAYERS ARE ALWAYS _

A

FLAT

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6
Q

USED TO DETERMINE WHETHER AN OBJECT OR EVENT IS OLDER OR YOUNGER THAN OTHER OBJECTS OR EVENTS

A

RELATIVE DATING

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7
Q

ARE DEPOSITED IN THE SEDIMENTARY LAYERS OF ROCKS

A

FOSSILS

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8
Q

LAWS/IDEAS:

A

LAW OF ORIGINAL HORIZONTALLY, LAW OF SUPERPOSITION, PRINCIPLE OF CROSS CUTTING RELATIONS, IDEA OF UNCOMFORMITIES

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9
Q

MEANS THAT SEDIMENTARY ROCKS ARE ORIGINALLY FORMED IN HORIZONTAL LAYER

A

LAW OF ORIGINAL HORIZONTALLY

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10
Q

HORIZONTALLY OCCURS IN AN AREA OF LAND THAT IS FORCES TO BEND, USUALLY FROM FORCES INSIDE THR EARTH PUSHINH ON THEM

A

LAW OF ORIGINAL HORIZONTALLY

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11
Q

STATES THAT IN ANY UNDISTURBED SEQUENCE OF LAYERS OF ROCKS, THE OLDER LAYER WOULD HE AT THE BOTTOM, AND THE YOUNGER WOULD BE ON THE TOP

A

LAW OF SUPERPOSITION

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12
Q

THIS STATES THAT ANY TOCKS OR FAULT THAT CUT ACROSS THE OTHER ROCK IS YOUNGER THAN THOSE IT CUT ACROSS

A

PRINCIPLE OF CROSS CUTTING RELATIONS

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13
Q

ARE SURFACES OF EROSION THAT SEPARATE YOUNGER ROCKS FROM OLDER ONES

A

IDEA OF UNCOMFOMITIES

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14
Q

METHOD OF MEASURING THE ABSOLUTE AGE OF AN EVENT OR OBJECT

A

ABSOLUTE DATING

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15
Q

UNSTABLE RADIOACTIVE ISOTOPE

A

PARENT ISOTOPE

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16
Q

STABLE ISOTOPE PRODUCED BY THE RADIACTIVE DECAY OF THE PARENT ISOTOPE

A

DAUGHTER ISOTOPE

17
Q

TIME NEEDED FOR A HALF A SAMPLE OF RADIACTIVE SUBSTANCE

18
Q

THE RATE OF RADIOACTUVE DECAY IS _

19
Q

ANOTHER DATING METHOD ACHIEVED BY DETERMINING THE ABSOLUTE AGE OF A SAMPLE

A

RADIOMETRIC DATING

20
Q

4 RADIOMETRIC DATING METHODS BASED ON THE ESTIMATED AGE OF AN OBJECT:

A

POTASSIUM-ARGON, URANIUM-LEAD, RUBIDIUM STRONTIUM, CARBON-14

21
Q

=USES POTASSIUM-40
=HALF LIFE OF 1.3 BILLION YEARS GA, IT LEAVSS ITS DAUGHTER MATERIAL, ARGON
=USED MAINLY TO DATE ROCKS OLDER THAN 100000 YEARS

A

POTASSIUM-ARGON METHOD

22
Q

=USES URANIUM-238 HALF LIFE OF 4.5 GA
=URANIUM-238 DECAYS IN A SERIES OF STEPS WHICH BECOMES LEAD-206
=USED TO DATE ROCKS OLDER THAN 10 MILLION YEARS OLD

A

URANIUM-LEAD METHOD

23
Q

=USES RUBIDIUM-87 WHICH FORMS A STABLE DAUGHTER ISOTOPE STRONTIUM-87
=HALF LIFE OF RUBIDIUM IS 49 GA
=USED FOR ROCKS WHICH ARE OLDER THAN 10 MILLION MA

A

RUBIDIUM-STRONTIUM METHOD

24
Q

=USES RADIACTIVE ISOTOPE CARBON-14
=HALF LIFE OF 5730 YEARS
=MAINLY USED FOR DATING THINGS THAT LIVED WITHIN THE LAST 50,000 YEARS

A

CARBON-14 METHOD

25
CONSIDERED A CHAOTI EON MAINLY DUE TO METREORITES THAT CONSTANTLY BOMBARDED EARTH
HADEAN EON
26
HADEAN CAME FROM HADES WHICH MEANS
HELL
27
THE OCEAN AND ATMOSPHERW WERE FORMED AND THE CRUST WAS ALSO STABILIZED
HADEAN EON
28
LASTED FOR 1.3 GA
ARCHEAN EON
29
PERIOD WHEN EARTH BECAME WARM BUT THE ATMOSPHERE CONTAINED OBLY METHANE AND LITTLE TO NO OXYGEN
ARCHEAN EON
30
MILLION OF YEARS
AGE
31
TENS OF MILLION OF YEARS
EPOCH
32
100 MILLION YEARS
PERIOD
33
SEVERAL 100 MILLION YEARS
ERA
34
HALF A BILLION YEARS OR MORE
EON
35
IT IS KNOWN THAT NEW LAYERS CAN BE LAID DOWN ONLY ON TOP OF PREEXISTING OLDER STRATA
PRINCIPLE OF SUPERPOSITION
36
REMNANNT OF ANY ANCIENT ANIMAL OR PLANT THAT HAS BEEN PRESERVED IN CRYSTALLIZED ROCKS
FOSSIL
37
SERVE AS GUIDE OR INDICATORS OF CERTAIN GEOLOGIC PERIODS
INDEX FOSSILS