Magnetic Reversals and Sea Floor Spreading

Keith Meldahl
17 Dec 201103:17

Summary

TLDRThis script delves into the Earth's magnetic field and its pivotal role in demonstrating seafloor spreading. It explains how the magnetic field, with its invisible force lines, can reverse polarity, a phenomenon recorded in lava flows. As lava cools, it captures the field's direction, acting as a geological 'tape recorder.' The script vividly describes how alternating stripes of normal and reversed magnetic orientations on the seafloor, formed over time as the Earth's magnetic field flipped, serve as compelling evidence for seafloor spreading. This pattern of magnetic stripes is a testament to the dynamic geological processes shaping our planet.

Takeaways

  • 🧭 The Earth's magnetic field is invisible but can be sensed by a compass needle, which points north because the field lines emerge from the South Magnetic Pole and point toward the North Magnetic Pole.
  • πŸ”„ Magnetic reversals are events where the Earth's magnetic field flips, with north and south poles swapping places, and occur every few million years.
  • πŸŒ‹ Evidence for magnetic reversals comes from lava flows, which contain magnetic minerals that align with the Earth's magnetic field at the time of cooling, preserving the field's direction.
  • 🌊 Seafloor spreading is the process where new oceanic crust is formed at mid-ocean ridges, and it's related to the Earth's magnetic field because the cooling lava there records the field's direction.
  • 🌈 The pattern of magnetic stripes on the seafloor, with alternating normal and reversed polarities, is a direct result of the Earth's magnetic field flipping as new crust is formed during seafloor spreading.
  • 🌎 The symmetrical stripes of magnetized seafloor rock on both sides of mid-ocean ridges provide strong evidence for both seafloor spreading and the Earth's magnetic field reversals.
  • πŸ”¬ By studying the layers of lava and their magnetic orientations, scientists can trace the history of the Earth's magnetic field and understand the timing of its reversals.
  • 🌏 The Earth's magnetic field plays a crucial role in protecting the planet from harmful solar radiation, and understanding its behavior is key to studying Earth's geological and atmospheric processes.
  • πŸ“‰ The animation in the script illustrates how the seafloor's magnetic stripes form, showing the progression of magnetic field reversals and seafloor spreading over time.
  • πŸ” The study of magnetic reversals and seafloor spreading is an interdisciplinary field that combines geology, geophysics, and paleomagnetism to understand Earth's dynamic history.

Q & A

  • What is the Earth's magnetic field?

    -The Earth's magnetic field is an invisible force field that compass needles can sense. It is created by the movement of molten iron in the Earth's outer core and extends from the South Magnetic Pole to the North Magnetic Pole.

  • Why does a compass needle point north?

    -A compass needle points north because the Earth's magnetic field lines emerge from the South Magnetic Pole and wrap around the Earth, pointing toward the North Magnetic Pole.

  • What are magnetic reversals?

    -Magnetic reversals are events where the Earth's magnetic field flips, so that the magnetic north and south poles switch places, causing the field lines to point in the opposite direction.

  • How often do magnetic reversals occur?

    -Magnetic reversals happen irregularly, but on average, they occur every few million years.

  • How do we know about the Earth's magnetic field reversals?

    -We know about magnetic reversals through the study of lava flows. As lava cools, it contains magnetic minerals that align with the Earth's magnetic field at that time, preserving a record of the field's direction.

  • How does the study of lava flows help understand magnetic reversals?

    -By examining the magnetic orientation of minerals in different layers of lava flows, scientists can determine the direction of the Earth's magnetic field at different times in the past, revealing the history of magnetic reversals.

  • What is seafloor spreading and how does it relate to the Earth's magnetic field?

    -Seafloor spreading is the process by which new oceanic crust is formed at mid-ocean ridges as tectonic plates move apart. It relates to the Earth's magnetic field because the new crust that forms records the magnetic field's orientation at the time of its formation.

  • How do the magnetic stripes on the seafloor prove seafloor spreading?

    -The symmetrical stripes of magnetized seafloor rock on either side of mid-ocean ridges, alternating between normal and reversed magnetic orientations, are evidence of seafloor spreading. These patterns match the timing of magnetic reversals, demonstrating that the seafloor has been spreading and recording the Earth's magnetic field changes over time.

  • What is the significance of the magnetic stripes on the seafloor?

    -The magnetic stripes on the seafloor are significant because they provide strong evidence for the theory of plate tectonics and seafloor spreading. They show that the Earth's crust is dynamic and has been changing over geological time.

  • How do the Earth's magnetic field and seafloor spreading contribute to the understanding of Earth's geology?

    -The Earth's magnetic field and seafloor spreading contribute to the understanding of Earth's geology by providing a historical record of the planet's magnetic field changes and crustal movements. This helps scientists reconstruct the geological history and understand the processes that shape the Earth's surface.

  • What is the normal polarity of the Earth's magnetic field?

    -The normal polarity of the Earth's magnetic field is when the magnetic north pole is near the geographic North Pole, and the magnetic south pole is near the geographic South Pole, which is the current state of the Earth's magnetic field.

Outlines

00:00

🌐 Earth's Magnetic Field and Seafloor Spreading

This paragraph introduces the Earth's magnetic field, explaining how it creates invisible force lines that a compass needle can sense. It discusses the concept of magnetic reversals, where the field flips so that the poles switch positions. The evidence for these reversals comes from studying lava flows, which contain magnetic minerals that align with the Earth's magnetic field at the time of cooling. This alignment preserves the direction of the magnetic field, serving as a historical record. The paragraph connects this phenomenon to seafloor spreading, suggesting that as the ocean floor spreads and the magnetic field reverses, the lava that cools on the seafloor records these changes, creating a pattern of magnetic stripes that supports the theory of seafloor spreading.

Mindmap

Keywords

πŸ’‘Earth's magnetic field

The Earth's magnetic field is a magnetic field that extends from the Earth's interior out into space, where it interacts with the solar wind, a stream of charged particles emanating from the Sun. It is generated by the motion of molten iron alloys in the Earth's outer core. In the video, the magnetic field is described as creating invisible lines of force that a compass needle can sense, pointing north because the field lines emerge from the South Magnetic Pole and point toward the North Magnetic Pole.

πŸ’‘Magnetic reversals

Magnetic reversals refer to the phenomenon where the Earth's magnetic field flips, so that the magnetic north and south poles switch places. This is a significant concept in the video as it explains how the field lines that normally emerge from the South Magnetic Pole and point toward the North Magnetic Pole can reverse, causing the compass needle to point in the opposite direction. The video mentions that these reversals occur every few million years.

πŸ’‘Lava flows

Lava flows are streams of lava that solidify on the Earth's surface. They are significant in the context of the video because when lava cools, it contains magnetic minerals that align with the Earth's magnetic field at that time. This alignment preserves a record of the field's direction, either normal or reversed, much like a tape recorder. The video uses the example of a lava flow in Hawaii to illustrate how scientists can study these records to understand the history of the Earth's magnetic field.

πŸ’‘Magnetic minerals

Magnetic minerals are minerals that can become magnetized in the presence of a magnetic field. They are crucial to the video's narrative because they are found in lava and align with the Earth's magnetic field as the lava cools. This alignment allows the minerals to record the direction of the field at the time, providing a historical record that scientists can study to understand past magnetic field orientations.

πŸ’‘Seafloor spreading

Seafloor spreading is a geological process that occurs at mid-ocean ridges where new oceanic crust is formed through volcanic activity and then moves away from the ridge due to tectonic forces. The video explains how this process is related to the Earth's magnetic field, as the new lava that erupts and cools at the mid-ocean ridges records the magnetic field's direction at the time of its formation, creating a pattern of magnetic stripes that serve as evidence for seafloor spreading.

πŸ’‘Mid-ocean ridges

Mid-ocean ridges are underwater mountain ranges, formed by plate tectonics. They are the sites where new oceanic crust is created through volcanic activity. In the video, mid-ocean ridges are highlighted as the areas where lava pours out of the Earth, and as the seafloor spreads, the lava records the magnetic field's direction, creating a pattern of magnetic stripes that serve as evidence for both seafloor spreading and magnetic field reversals.

πŸ’‘Magnetic polarity reversals

Magnetic polarity reversals are changes in the Earth's magnetic field where the north and south magnetic poles switch places. The video discusses how these reversals are recorded in the magnetic minerals within lava flows, with different layers of lava showing either a normal or reversed magnetic field orientation. This record of past magnetic field directions is used as evidence for the occurrence of magnetic polarity reversals.

πŸ’‘Magnetic stripes

Magnetic stripes are alternating bands of normal and reversed magnetization in the oceanic crust, created as new crust forms at mid-ocean ridges during periods of different magnetic field orientations. The video describes how these stripes are symmetrical on both sides of the ridges and are formed as the Earth's magnetic field flips back and forth, with new lava recording the field's direction at the time of its formation.

πŸ’‘Geologic time

Geologic time refers to the vast time scales used in geology to describe the timing and relationships of events that have occurred during Earth's history. The video mentions geologic time in the context of understanding the Earth's magnetic field reversals and seafloor spreading, as these processes occur over millions of years and are studied through the examination of rock layers and their magnetic properties.

πŸ’‘Tectonic forces

Tectonic forces are the forces that cause the movement of Earth's lithosphere, which is broken into several large plates that float on the semi-fluid asthenosphere. In the video, tectonic forces are mentioned as the driving force behind seafloor spreading, where the new oceanic crust formed at mid-ocean ridges is pushed away from the ridge by these forces, recording the magnetic field's direction as it cools and solidifies.

Highlights

Introduction to the Earth's magnetic field and its invisible force lines.

Explanation of why compass needles point north due to the Earth's magnetic field.

Definition and occurrence of magnetic reversals, happening every few million years.

Evidence of magnetic field reversals from lava flows, preserving the Earth's magnetic direction.

Magnetic minerals in lava align with the Earth's magnetic field, recording its direction.

Geologic time evidence of the Earth's magnetic field flipping back and forth.

Connection between seafloor spreading and the Earth's magnetic field reversals.

Visualization of lava pouring out at mid-ocean ridges and recording the magnetic field direction.

Animation of seafloor spreading and magnetic field reversals, illustrating the process.

Description of how new lava gets magnetized in the opposite direction during a magnetic field reversal.

Observation of symmetrical stripes on mid-ocean ridges, indicating alternating magnetic polarity.

The pattern of stripes as evidence for seafloor spreading and magnetic field reversals.

Conclusion that the pattern of magnetic stripes confirms the theory of seafloor spreading.

Emphasis on the stripes as some of the best evidence for the seafloor spreading hypothesis.

Transcripts

play00:00

>> Hi, everyone.

play00:01

We're going to talk

play00:02

about the Earth's magnetic

play00:03

field, and how the reversals

play00:05

in the Earth's magnetic field,

play00:06

revealed that seafloor

play00:08

spreading is happening.

play00:09

The Earth's magnetic field

play00:12

creates lines

play00:12

of invisible force

play00:14

that you can't see

play00:15

but that your compass

play00:17

needle senses.

play00:19

And the reason your needle

play00:20

points north is

play00:21

that these field lines emerge

play00:22

from the South Magnetic Pole

play00:24

and wrap around the Earth

play00:25

and point toward the North

play00:26

Magnetic Pole.

play00:28

Now, we know

play00:29

that the Earth's magnetic

play00:30

field has actually reversed,

play00:31

flipped around,

play00:32

so that these arrows would all

play00:33

point the other direction,

play00:35

coming out of the North Pole

play00:37

and pointing

play00:37

into the South Pole.

play00:38

And these are called

play00:39

MAGNETIC REVERSALS.

play00:40

They happen every few

play00:41

million years.

play00:42

The Earth's magnetic field

play00:43

flips back and forth

play00:44

through time.

play00:46

The reason we know this is

play00:47

from lava flows,

play00:48

like this lava flow on Hawaii.

play00:50

When lava flows

play00:51

out of the Earth,

play00:52

there's little magnetic

play00:54

minerals in the lava.

play00:55

And they line

play00:56

up with the magnetic field

play00:57

at the time

play00:59

and actually preserve,

play01:00

like a tape recorder, the

play01:01

direction of the Earth's

play01:02

magnetic field, whichever way

play01:04

it was pointing, either normal

play01:06

or reversed.

play01:07

So if we go look

play01:08

at a whole series

play01:08

of lava flows, what we'll find

play01:11

if we sample

play01:12

through the lava layers

play01:13

into older and older layers,

play01:14

we'll find some layers

play01:15

oriented

play01:17

with a magnetic field,say,

play01:18

like today,

play01:19

and other older layers

play01:21

that are reversed,

play01:22

and then still older layers

play01:23

that are like today.

play01:24

So through geologic time,

play01:26

the Earth's magnetic field

play01:27

flips back and forth.

play01:28

And we call these magnetic

play01:30

polarity reversals.

play01:32

Now, the way

play01:33

that this all relates

play01:34

to seafloor spreading can be

play01:37

realized by remembering

play01:39

that lava is pouring

play01:40

out of the Earth

play01:40

at mid-ocean ridges.

play01:42

So I want you to imagine

play01:43

that we're going

play01:44

to let this ocean basin spread

play01:46

and we're going

play01:47

to let the Earth's magnetic

play01:48

field flip back and forth

play01:49

as the ocean basin spreads.

play01:51

Remember that when the lava

play01:53

erupts and cools down,

play01:54

it records the direction

play01:55

of the magnetic field

play01:56

at the time,

play01:57

whether it's normal

play01:58

or reversed.

play02:00

play02:00

So we'll start the

play02:01

animation here.

play02:02

We're going to start it

play02:03

at a time when the Earth's

play02:04

magnetic field is like today,

play02:05

what we call normal polarity.

play02:08

And as the seafloor spreads,

play02:10

it's all going

play02:10

to get polarized

play02:12

in the direction

play02:13

of the magnetic field,

play02:14

shown by the blue part

play02:16

of the ocean floor.

play02:17

But now we have a reversal

play02:18

happening, and any new lava

play02:20

that erupts is going

play02:21

to get magnetized

play02:22

in the opposite direction.

play02:23

So you can see the little

play02:24

compass needles here are

play02:25

flipped, showing us

play02:27

that all this new seafloor is

play02:29

recording the direction

play02:30

of the Earth's magnetic field

play02:31

at a time when it

play02:32

was reversed.

play02:34

Now we'll let the Earth's

play02:35

polarity flip again.

play02:37

Any new lava

play02:38

that forms is going

play02:39

to record the polarity

play02:41

of the Earth at that time.

play02:43

So what we see

play02:44

on the mid-ocean ridges

play02:45

of the world today is a series

play02:46

of stripes--

play02:47

symmetrical stripes

play02:48

on both sides of the ridges--

play02:50

of seafloor rock that's

play02:52

magnetized

play02:53

in the same direction

play02:54

as the magnetic field today, then

play02:55

older rock that's reversed, and

play02:57

still older rock that's back

play02:58

to normal.

play03:00

This pattern is impossible

play03:02

to explain

play03:03

if seafloor spreading didn't

play03:04

actually happen

play03:05

and the Earth's magnetic field

play03:07

didn't flip back and forth!

play03:08

So it constitutes some

play03:09

of the best evidence we have

play03:11

that the seafloor is actually

play03:12

spreading over geologic time.

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Related Tags
Magnetic FieldPolarity ReversalsSeafloor SpreadingGeological EventsLava FlowsMagnetic MineralsEarth DynamicsScientific EvidenceOcean BasinsMagnetic Stripes