Plate tectonics

Plate Tectonics

 

 

 

What is it?

How do we know it is happening?

What are the different types of tectonic boundaries?

What are the effects of it?

 

 

Plate tectonics is the theory that plates of Earth's crust are sliding across the surface of Earth.  This theory includes the effects of such movement.

 

But how do we know?  What evidence is there that there are sliding plates?

 

 

Image result for puzzle fit of continents

They look like they fit together...

Continental Drift Biology GIF by PBS Digital Studios - Find & Share on GIPHYPlate Tectonics as Gifs - Space Engine

That man popping up is Alfred Wegener

He looked at this puzzle fit and declared that the continents drift on top of the oceans:

Image result for alfred wegener

And he was vilified for it.

 

But, he predicted that fossile evidence would prove he was right, and it did!

Fossil and rock evidence indicates that they were once together...

Biogeography: Wallace and WegenerPlate tectonics

This further solidified his theory of continental drift.  

But people really did not like the thought of rocks floating on water (continents floating on the oceans) and did not buy in.

 

His theory sat largely un-believed for many years.  Further evidence came to light during WWII.  As we shipped stuff to Europe, we didn't want German U-boats getting under us, so we used strong magnetic detectors as we went back and forth across the Atlantic and discovered something interesting:

We had known that molten rocks, when they solidify, will orient all their iron pointing toward the North Pole.  The sea floor rocks that have magnetic minerals all face north (makes sense), but then we find a section where all of the rocks face south (!???!).  Then another northern section, then southern, and so on.  It made a pattern on the sea floor.  Closer inspection showed the pattern was reflected from the center of the ocean:

 

Seafloor magnetic stripes reconsidered

In this, black is facing North, white is facing South.  This data spans the Atlantic Ocean.

What do you see in this?

What more information would you want?

 

 

This made scientists want to investigate those stripes closer.  They dated them and:

Solved: Normal Reverse Mid-ocean Ridge 100 Km HHHHHHHHHHHH... | Chegg.com

As you can see, scientists then looked at the age of the rocks and found that new rocks were being made at the center and the bands east and west of the center are all dated the same and equal in size to their counterpart.  The newest rocks were in the center and the oldest rocks were on the shores.  So, what does this mean?

 

Image result for age of ocean floor                                Image result for pattern of magnetic reversals on the ocean floor

 

It means that if you go back in time, the ocean was smaller and we were closer to Africa and Europe.

magnetic-striping.gif 240×180 pixels | Cuadros

It also seems to mean that the magnetic north pole and south pole have swapped places over the years.

So, does this mean that the Earth is growing?  

Hypotheses abounded.  Some said the Earth was expanding.  Some said that Earth was "breathing" (growing and then shrinking).  It was clear that at least in the Atlantic ocean, the Earth was spreading.

Some scientists traveled to other places to search for similar spreading.  Some used lasers to measure the rate of growth by seeing how quickly New York and Paris are moving apart from each other.  Much data was recieved.  Here is what they found:

There were some parts of the world that were moving apart as measured by the dated sea floor and lasers.

Some were moving closer together as measured by lasers.  But where was the land going?

Some moved all over the place.  By using the magnetic minerals in rocks pointing to the north pole, we could see where the magnetic north pole was reletive to that land.  And it appeared that the north pole wandered.  But really telling is that the north pole seemed to wander differently for different lands!  That would be impossible!  The lands must have most differently from one another rather than having multiple north poles.

Paleomagnetism and plate tectonics - YouTube

10.3 Geological Renaissance of the Mid-20th Century | Physical Geology

 

To make them line up, the continents must have moved and if you line them up, they recreate pangea!  This is called "apparent polar wander path".

 

But where is the land going again? 

In the 1950s, a geologist studying earthquakes discovered the last piece of the puzzle...where the land disappears to.

He was researching the power and depth of earthquakes in the South Pacific and found this:

Image result for earthquake, depth

From where he was (the star), the earthquakes made a slope descending down into the Earth.  This turned out to be the plate sliding under the other plate:

Image result for earthquake, depth

In other words, he discovered where the plates went.

As you can see, the land is sinking back into the Earth at these places and the force of that causes earthquakes and volcanoes.  The earthquakes get weaker as the land slides past more magmafied rock further underground until some point where all earthquakes seem to stop.  He concluded that this is the point where the rocks are too magmafied to resist the other rocks sliding (everything melts).

Subduction Zone Earthquake GIF - Find & Share on GIPHYBest Subduction GIFs | Gfycat

In some places, land collides with land and you get mountains:

Himalayas Forming GIF | Gfycat

 

 

So there is tons of evidence that plates of Earth's crust are moving.  But what are the sections of Earth's crust?

We call them plates and they can be traced out by looking at the pattern of earthquakes and volcanoes:

Image result for earthquakes and volcanoes

The pattern of earthquakes and volcanoes seem to mark out chunks of Earth...

 


The evidence shows that all the plates except the African plate are moving.  The fastest, largest, and oldest plate is the Pacific plate which is moving at about 9 cm / year (that is the rate at which your fingernails grow!).


 

 

 

 

So, plates are moving!

There are three ways they can move:

So, the three types of plate bounradies:

Related image

 

Or:

Evolution of Continents and Oceans

 

 

Looking closer at the boundaries:

When magma from the core wells up and splits the crust, you get two plates moving away from each other:

Image result for divergent plate boundaries

Divergent Boundary GIF | Gfycat

These will have hot magma from the core (mafic and friendly) as well as weak, shallow earthquakes

 

 

Where two plates come together, they will either crash into each other or one will sink under the other:

Convergent plate boundaries:

Image result for convergent plate boundaries

Plate Boundaries GIF | Gfycat

These make powerful earthquakes and either tall mountains or dangerous (felsic) volcanoes.

 

 

When plates slide past each other, we get the last of the boundaries:

Transform plate boundaries:

Image result for transform plate boundariesPlate Boundaries: Transform Fault GIF | Gfycat

These cause powerful earthquakes!  But no volcanoes usually.

 

These are the agreed upon plates:

Plate Tectonics Gif & 168What is plate tectonics, and how does it work?

 

Our next unit will be the effects of plate tectonics:  Earthquakes, volcanoes, and mountains!