Relative Dating vs Absolute Dating (Updated)

Color Me Scientifically
23 Feb 202107:38

Summary

TLDRThis educational script explores the concepts of relative and absolute dating in geology. Relative dating uses the principle of superposition to arrange rock layers or family members from oldest to youngest, without specific ages. Absolute dating, on the other hand, assigns a numeric age to rocks or fossils using radiometric dating. The script explains isotopes and the decay process, exemplified by uranium-lead dating and carbon-14 dating, which help determine the age of rocks and organic materials, respectively.

Takeaways

  • đŸ•°ïž Relative dating involves arranging events or objects in chronological order without specific dates, similar to arranging family members by age.
  • đŸ”ïž In geology, the oldest rock layers are found at the bottom, with younger layers above, following the law of superposition.
  • 🌋 Stratigraphy is the scientific study of rock layers, or strata, which helps in understanding the relative ages of geological formations.
  • đŸœïž The concept of relative dating can be illustrated using a five-layer bean dip, where each layer represents a different age or event.
  • 📊 Absolute dating provides a numeric age of rocks or fossils, as opposed to relative dating which does not include specific dates.
  • 📜 Absolute dating in geology often uses radiometric dating, which measures the ratio of isotopes to determine the age of a rock.
  • ⚗ Radiometric dating involves examining the decay of isotopes, such as uranium to lead dating, to calculate the age of rocks.
  • 🔬 The half-life of an isotope, like uranium-238, is a key factor in radiometric dating, indicating the time it takes for half of the isotope to decay.
  • 📈 Carbon-14 dating is a type of radiometric dating that is used for materials that were once alive and are relatively young, up to about 50,000 years old.
  • đŸ‘” The script humorously compares the reluctance of a grandmother to reveal her age to the use of relative dating in geology.

Q & A

  • What is relative dating?

    -Relative dating is the process of arranging events or objects in chronological order without including actual dates or ages. It is similar to arranging family members by their relative ages from oldest to youngest.

  • How do geologists arrange rock layers in relative dating?

    -In relative dating, geologists arrange rock layers vertically with the oldest at the bottom and the youngest at the top, similar to the layers in a five-layer bean dip.

  • What is stratigraphy?

    -Stratigraphy is the scientific study of layers, particularly in rocks. It involves the observation of the law of superposition, which states that newer layers form on top of previous layers.

  • How does the law of superposition relate to the layers in a five-layer bean dip?

    -The law of superposition in the context of a five-layer bean dip means that the beans, being the oldest layer, are at the bottom, and each subsequent layer (guacamole, salsa, sour cream, cheese) is younger and placed on top of the previous one.

  • What is absolute dating in the context of geology?

    -Absolute dating in geology is the process of determining a numeric age of rocks or fossils using methods like radiometric dating, which provides specific ages in years.

  • What is radiometric dating and how does it work?

    -Radiometric dating is a technique that examines the ratio of one isotope to another in a rock to determine its age. It involves the radioactive decay of isotopes over time, which can be measured to calculate the age of the rock.

  • What are isotopes and how are they used in radiometric dating?

    -Isotopes are forms of the nuclei of atoms of a particular element that have differing numbers of neutrons. In radiometric dating, isotopes like uranium-238 and lead-206 are used to determine the age of rocks by measuring their decay rates.

  • What is the half-life of uranium-238 and how does it relate to dating rocks?

    -The half-life of uranium-238 is 4.5 billion years, which means it takes this long for half of the uranium-238 isotopes to decay into lead-206. By knowing the ratio of uranium to lead in a rock, the age of the rock can be calculated.

  • What is carbon-14 dating and what materials can it be used on?

    -Carbon-14 dating is a type of radiometric dating that uses the radioactive decay of carbon-14 isotopes. It can only be used on materials that were once alive and lived within the last 50,000 years.

  • Why might someone prefer relative dating over absolute dating?

    -Some individuals, like the grandma in the script, might prefer relative dating because it does not require disclosing exact ages in numbers, which can be personally sensitive or simply not known.

  • How does the concept of relative dating apply to the Grand Canyon's exposed layers?

    -In the Grand Canyon, the concept of relative dating is evident as the oldest layers are found at the bottom and the youngest layers are found at the top, indicating a chronological order from oldest to youngest.

Outlines

00:00

📚 Understanding Relative and Absolute Dating

The paragraph introduces the concepts of relative and absolute dating through a family analogy. Relative dating is compared to arranging family members by age without specific years, where the oldest is at the bottom, and the youngest at the top. This is analogous to rock layers, with the oldest at the bottom and the youngest at the top. The paragraph explains stratigraphy, the study of layers in rocks, and the law of superposition, which states that newer layers form on top of older ones. The Grand Canyon is used as an example to illustrate this concept. Absolute dating, on the other hand, involves assigning a numerical age to rocks or fossils, typically using radiometric dating, which is not detailed in this paragraph.

05:01

🔬 Radiometric Dating Techniques

This paragraph delves into radiometric dating, specifically uranium-lead dating and carbon-14 dating. Uranium-lead dating involves measuring the ratio of uranium-238 to lead-206 in a rock to determine its age. The process is illustrated with a simplified animation showing uranium-238 decaying into lead-206 over time. The half-life of uranium-238 is highlighted as 4.5 billion years, which is the time required for half of the uranium atoms to decay into lead. Carbon-14 dating is mentioned as a method applicable to materials that were once alive and have been dead for up to 50,000 years. The paragraph concludes with a personal reflection on the value of learning new things daily.

Mindmap

Keywords

💡Relative Dating

Relative dating is the method of arranging objects or events in chronological order without determining their exact age. In the video, it's compared to ordering family members from oldest to youngest without knowing their actual birth dates. In geology, it involves placing rock layers in order from oldest (bottom) to youngest (top), as seen in the rock strata example.

💡Absolute Dating

Absolute dating is a process that assigns a specific numeric age to an object or event. In the video, it's compared to using birth certificates to determine the ages of family members. In geology, absolute dating uses techniques like radiometric dating to determine the age of rocks or fossils in years.

💡Stratigraphy

Stratigraphy is the scientific study of layers of rocks (strata). In the video, it is introduced alongside the concept of relative dating, explaining that older layers are at the bottom and newer ones are at the top. This concept is exemplified using a five-layer bean dip as an analogy to explain the layers of rock formation.

💡Law of Superposition

The Law of Superposition states that in undisturbed rock layers, the oldest layers are at the bottom and the youngest are at the top. This principle is foundational in stratigraphy and relative dating, allowing geologists to determine the relative ages of different rock layers. The video uses the example of a bean dip to illustrate this concept.

💡Radiometric Dating

Radiometric dating is a technique used to determine the absolute age of rocks by measuring the ratio of isotopes within them. The video explains that scientists use this method, such as uranium-to-lead dating, to calculate the age of a rock by analyzing how long isotopes have been decaying. It highlights the importance of isotopic ratios in determining the age of ancient materials.

💡Isotopes

Isotopes are atoms of the same element that have different numbers of neutrons, and thus different atomic masses. The video explains isotopes like Carbon-12, Carbon-13, and Carbon-14, and how they are used in radiometric dating to determine the age of materials. For example, Carbon-14 is used in dating organic materials within the last 50,000 years.

💡Uranium-238 to Lead-206 Dating

Uranium-238 to Lead-206 dating is a form of radiometric dating used to find the absolute age of rocks. The video explains that uranium-238 decays over billions of years into lead-206, and by measuring the ratio of these isotopes in a rock, scientists can estimate how long the uranium has been decaying. This method is used for dating rocks that are millions to billions of years old.

💡Half-life

Half-life refers to the amount of time it takes for half of the atoms in a radioactive substance to decay. In the video, the concept is used to explain how radiometric dating works, specifically noting that uranium-238 has a half-life of 4.5 billion years. This long half-life is crucial in determining the age of ancient rocks.

💡Carbon-14 Dating

Carbon-14 dating is a method used to determine the age of once-living materials that are up to about 50,000 years old. The video explains that carbon-14 decays into nitrogen over time, and by measuring the remaining carbon-14 in a sample, scientists can estimate its age. This method is contrasted with uranium dating, which is used for much older materials.

💡Strata

Strata are layers of rock that are used in stratigraphy to study the Earth's geological history. The video compares these layers to the layers in a bean dip, with the oldest at the bottom and the youngest at the top. Strata help geologists understand the relative age of fossils and rocks, as each layer represents a different period of time in Earth's history.

Highlights

Relative dating arranges objects or events in chronological order without specific dates.

An analogy of a family's age order demonstrates the concept of relative dating.

In geology, rock layers (strata) are arranged with the oldest at the bottom and the youngest at the top.

Relative dating in geology is aided by the law of superposition, where newer layers form on top of older ones.

Stratigraphy is the scientific study of layers, particularly in rocks.

The Grand Canyon example illustrates how relative dating can be observed in exposed rock layers.

Absolute dating provides numeric ages for rocks or fossils, unlike relative dating.

Radiometric dating is a method used in absolute dating to determine the age of rocks and fossils.

Isotopes, which are variants of elements with different numbers of neutrons, are key in radiometric dating.

Carbon-12, carbon-13, and carbon-14 are isotopes of carbon used in dating methods.

Uranium to lead dating is a well-known radiometric dating method that tracks the decay of uranium-238 into lead-206.

The half-life of uranium-238, which is 4.5 billion years, is crucial for calculating rock ages.

Carbon-14 dating is used for materials that were once alive and are up to 50,000 years old.

The analogy of a five-layer bean dip is used to explain the law of superposition in a relatable way.

The video uses humor and everyday examples to make geological concepts accessible.

The importance of understanding the chronological order in both relative and absolute dating is emphasized.

Transcripts

play00:00

relative dating versus absolute dating

play00:06

what is relative dating well

play00:09

if you look at a family can you put the

play00:12

family members in order from oldest

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to youngest grandma's going to be the

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oldest of course because

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she's the grandma and we're not really

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sure if mom or dad is going to be oldest

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but let's just guess and put dad next

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and then mom and then the older sister

play00:32

and then finally little brother

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we've just arranged the whole family in

play00:37

order from oldest to youngest ages

play00:40

but using relative ages

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if you want to do this like a geologist

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you're going to put the family

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in order vertically the oldest family

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member is going to be at the bottom

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and the youngest family member is going

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to be at the top

play01:00

rock layers do the same thing the oldest

play01:03

rock layers

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are at the bottom just by looking at the

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rock layers we can see that the dark

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orange layer is the oldest

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and the pink layer is younger than the

play01:13

dark orange layer but it's older than

play01:16

the beige layer

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and the sandy layer is the youngest

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layer of them all

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and we know that a fossil that appears

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in the pink layer

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is going to be older than any fossil

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that appears

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in the beige layer and if we were to

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find a fossil in the yellow layer

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that would be the youngest fossil of

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them all

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it's kind of like five layer bean dip

play01:40

it's a tasty treat you might have at a

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party

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if you've never tried it you definitely

play01:44

should so what you do is you put the

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beans at the very bottom

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and that is the oldest layer in the bean

play01:50

dip

play01:51

on top of that you put some guacamole

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and then some salsa

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some sour cream a little cheese on top

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and the cheese is your youngest layer

play02:03

scientists call each one of these layers

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in rocks

play02:06

strata so let's call them strata and our

play02:08

bean dip too why not

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it's a party for scientists stratigraphy

play02:14

is the scientific study of layers and

play02:17

that's usually something that we study

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in rocks

play02:20

and if you want to really impress people

play02:22

at your party

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while you're eating your tasty five

play02:25

layer bean dip

play02:26

you can tell them that this bean dip

play02:29

observes the law of superposition

play02:32

that means that the newer layers form on

play02:34

top of previous layers

play02:36

either way let's eat

play02:40

if you go someplace like the grand

play02:41

canyon where there are a lot of layers

play02:44

in our earth that are exposed

play02:46

you'll see that the oldest layers are

play02:48

found at the bottom

play02:50

and the youngest layers are found at the

play02:52

top

play02:54

so relative dating means putting events

play02:56

or objects in chronological order

play02:58

without including actual dates or ages

play03:03

but absolute dating is a little

play03:05

different

play03:06

let's go back to our family again

play03:11

absolute ages are measured with numbers

play03:14

so if we want to measure the absolute

play03:15

age of each one of these family members

play03:17

we could look at their birth

play03:18

certificates

play03:19

and we'd find that mom is 37

play03:23

and the daughter is 11. the little boy

play03:26

is seven

play03:27

dad's 39 and grandma well she's not

play03:31

going to tell you how old she actually

play03:32

is she prefers relative dating because

play03:36

like a lot of grandmas she doesn't

play03:37

really want to say her age in numbers

play03:41

absolute dating in geology or

play03:43

archaeology

play03:44

is the process of finding a numeric age

play03:46

of rocks or fossils

play03:48

using radiometric dating so what is

play03:51

radiometric dating

play03:55

radiometric dating examines the ratio of

play03:58

one

play03:58

isotope to another in rock to determine

play04:01

its age

play04:02

isotopes are forms of the nuclei of

play04:05

atoms of a particular element

play04:07

that have differing number of neutrons

play04:09

for example

play04:10

carbon atoms always have six protons

play04:14

that's what makes them carbon and

play04:16

usually

play04:17

carbon atoms have six neutrons too

play04:20

this isotope is called carbon-12 because

play04:23

six

play04:24

protons plus six neutrons equals

play04:27

12 as the total number of particles in

play04:29

the nucleus

play04:31

but carbon can also come in other

play04:33

varieties

play04:35

carbon 13 is an isotope that contains

play04:38

six protons and seven neutrons

play04:41

and carbon 14 which you might have heard

play04:44

of

play04:45

has six protons and eight neutrons

play04:48

these are the three stable isotopes of

play04:52

carbon

play04:54

you can use isotopes to find out the age

play04:56

of rock

play04:57

and the most well-known type of

play04:59

radiometric dating

play05:01

is uranium to lead dating this is how it

play05:04

works

play05:04

you take a rock that you know probably

play05:06

has some uranium in it

play05:08

usually in a small crystal called a

play05:09

zircon crystal

play05:11

and as you can see from the screen the

play05:14

process is really complicated uh

play05:17

basically

play05:18

you start with uranium 238 that means

play05:21

there's 238 particles protons and

play05:24

neutrons

play05:24

in the nucleus of this atom and over

play05:27

time

play05:28

this atom loses both protons and

play05:30

neutrons and slowly turns into something

play05:32

completely different

play05:35

so it goes through many steps

play05:39

and eventually it ends up being a

play05:42

stable atom that is lead

play05:45

206 now if you calculate the ratio of

play05:50

uranium-238

play05:51

to lead 206 in the rock you can

play05:54

figure out how long the uranium has been

play05:57

decaying

play05:58

and that gives you the absolute age of

play06:00

the rock

play06:02

here's a simpler way of showing it so

play06:04

the red dots are uranium-238 atoms

play06:07

or isotopes and over time

play06:10

some of them go through that very

play06:12

complicated process

play06:13

and turn into these blue dots which

play06:16

represent

play06:17

lid 206.

play06:21

you've probably heard the term half-life

play06:23

the half-life of uranium-238

play06:26

is 4.5 billion years this just basically

play06:30

tells you it takes a really long time

play06:32

for half of those uranium-238 isotopes

play06:35

to turn in

play06:36

to lead 206 but by knowing how much

play06:40

how much there is of uranium and lid and

play06:43

comparing those amounts

play06:45

you can calculate the age that the rock

play06:47

has been around

play06:49

another type of radiometric dating that

play06:51

you might have heard of is carbon 14

play06:53

dating

play06:55

carbon 14 dating also uses the

play06:58

radioactive decay

play07:00

of carbon 14 isotopes but it can only be

play07:03

used with

play07:04

materials that were once alive and that

play07:06

lived fairly recently

play07:08

within the last 50 000 years

play07:13

now i know you think grandma is old but

play07:16

50 000 years is

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way older than grandma even though

play07:20

she's not going to tell you her age

play07:24

i hope you've learned something from

play07:26

this i learned something new every day

play07:29

thanks a lot

play07:31

[Music]

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Étiquettes Connexes
GeologyRelative DatingAbsolute DatingRadiometric DatingRock LayersFossilsIsotopesSuperpositionStratigraphyCarbon Dating
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