Relative And Absolute Dating Flashcards

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1
Q

HOW DO WE KNOW THE AGE OF ROCKS?
-Scientists use 2 methods to determine the age of rocks:

A
  1. Relative Dating
  2. Absolute Dating
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2
Q

This results in
deformation of Earth’s crust. There are three types of plate boundaries that makes
the earth’s crust move
3 types:

A
  1. CRUSTAL MOVEMENT the movement of the crust
  2. Convergent Plate Boundaries
  3. Divergent Plate Boundaries
  4. Transform Plate Boundaries
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3
Q

when two
tectonic plates move toward each other and collide. These
boundaries are the site of earthquakes, volcanoes, and other
geological activities.

A

Convergent plate boundaries

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4
Q

exists between two tectonic plates
that are moving away from each other.
within continents initially produce riffs, eventually becomes riff valley.

A

Divergent plate boundaries

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5
Q

where two plates slide past one
another. Most are found in the ocean basin and
connect offsets in the mid-ocean ridges

A

Transform plate boundaries

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6
Q

How do layers of stratified rocks formed?
3 types

A
  1. Crustal Movement
  2. Displacement of soils or soil erosion (remove by human activity = tilting)
  3. Distortion of terrains or weathering
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7
Q

A natural process that occurs as
soil is washed away by running water, blown away by wind, or removed by human
activities such as tilting (inclined).

A

DISPLACEMENT OF SOILS or soil erosion

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8
Q

The breaking down of rocks at the
earth’s surface by the action rain. Rocks, such as lavas, that are quickly buried
beneath other rocks are less vulnerable to weathering and erosion than rocks
that are exposed to agents such as wind and water

A

DISTORTION OF TERRAINS or weathering

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9
Q

What is Dating?

A

When geologists date rocks, they are determining how long ago they formed

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10
Q

is when you give the age of a rock or fossil compared to another rock or fossil.

•Example: Rock A is OLDER than Rock B.
•An actual age in years is not determined.

A

Relative Dating

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11
Q

(RULES OF RELATIVE DATING)

A
  1. Law of Superposition

When sedimentary rock layers are deposited, younger layers are on top of older

  1. Law of Original Horizontality: Sedimentary rock layers are deposited horizontally. If they are tilted, folded, or broken, it happened later.
  2. Law of Cross-Cutting Relationships: If an igneous intrusion or a fault cuts through existing rocks, the intrusion/fault is YOUNGER than the rock it cuts through
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12
Q

●Determining how old something is
●Use numbers (in millions of years, mya)
●Only works for Igneous Rocks
●Determines the specific age of a fossil
●Looks at chemical properties
2 types:

A

Absolute Dating
1. Carbon-14 (radiocarbon)
2. Potassium-Argon

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13
Q

●Also known as Radiocarbon dating
●Used to date organic substances
●Scientists measure the radiocarbon in the fossil to determine its age
●Can only date specimens up to about 60,000 years old

A

Carbon-14 Dating

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14
Q

●Scientists determine the age of the rock surrounding the fossil to determine the fossil’s age.
●Used only for inorganic substances (rocks and minerals)
●Scientists measure the amount of argon in the rock to determine its age
●Dates rock 60,000 years old and older

A

Potassium-Argon Dating

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15
Q

●Absolute Dating
•Helps us determine the age of the earth
•Helps us determine when specific events in the history of the earth happened (ex. Extinction of the dinosaurs)

●Relative Dating
•Can help us estimate the time span between major earthquakes, storms, tsunamis etc
•Can help us determine the order that life forms developed on earth

A
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