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This is geology, B. 
I'm all of us, trampled, unless 

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you live in a place like Japan 
or California, most of us have 

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never experienced an earthquake,
but we certainly hear about them

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regularly, especially when the 
damage they reek is newsworthy 

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this podcast. 
Focuses on earthquakes, the 

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geological faults on which they 
occur, and their impact on 

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humans. 
James Jackson is Professor of 

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active tectonics at Cambridge 
University and an expert on the 

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geological processes including 
earthquakes that are shaping our

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continents today. 
James Jackson, welcome to 

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geology B, what's going on 
geological speaking. 

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When an earthquake strikes, this
week happens when rocks break 

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and slide past each other on 
surfaces called, folks. 

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They could think of a knife cut 
in the earth and the rocks are 

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sliding past each other on. 
At knife, cut. 

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Now normally it's held together 
by friction and you have to 

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overcome that friction. 
So imagine you have a brick on a

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table and you push the brick. 
You have to push a certain 

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amount before it actually jumps 
forward and that's what's 

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happening in. 
The earthquake is friction which

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is an overcome and it's the 
shaking as the Rocks grind past 

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each other, doing that movement,
which causes the damage, the 

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earthquake people feel and is 
the shaking. 

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But the cause of it, is this 
breaking of rocks on false So do

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we know where all these Faults 
Are what we look like cotton 

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under that, because what happens
is that, they move again and 

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again, in earthquakes, the same 
fault, will move again and again

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it only moves a few meters even 
in the biggest earthquakes, but 

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given the huge time we have on 
Earth, after thousands of these 

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earthquakes, you actually make 
the landscape. 

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So the landscape is often a clue
to where The Faults Are and so 

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reading the landscape is a bit 
like learning to read at new 

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alphabet when you book once you 
speak, The language, you have a 

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head start and where these 
things are. 

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Does that mean that if there are
faults away from landscape 

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features? 
We don't know where they are. 

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Well, most of the folks have 
some effect in the landscape. 

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So the folks can either move up 
and down or sideways moving up 

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and down, makes mountains, or it
makes basins and lakes, 

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depending, which side of the 
fault you are. 

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And so that's a help and places 
where this is going on the other

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folks move sideways. 
As they do an example, the San 

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Andreas Fault in California, 
They still end up as features in

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the landscape because as the 
Rocks grind past each other and 

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folks who get broken up and they
get the easily eroded by streams

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and rivers and so on. 
So, they quite often make linear

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values, or Scott's or features 
in the landscape, which are 

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quite often visible from the 
air, for example, in are 

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photographs or Satellite 
photographs and they're often 

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followed by roads and rail 
hissing. 

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So, people exploit these things 
also So when an earthquake 

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strikes, how much movement might
occur across a fault? 

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Well, that is basically what 
determines the size of the 

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earthquake, or the magnitude or 
the Richter magnitude has been 

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straight As refer to it. 
But even in the really ready, 

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biggest earthquakes, the 
movement is 1020 meters of 

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biggest. 
We know, of, in modern times was

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the one in Japan in 2011, which 
moved 50 meters which was 

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extraordinary, but that really 
was unusual. 

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Most the small earthquakes will 
move just a few millimeters or 

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so. 
Two meters. 

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So that's really what determines
the size of the earthquake. 

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So thank you Nate earthquake. 
You're talking about maybe 10 

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meters or more slip a magnitude 
5 earthquake. 

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You're talking about a 
centimeter or a few centimeters.

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That's really what determines 
the size of the earthquake. 

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And how could we measure this 
slip? 

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Well, there are various ways of 
doing it. 

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Sometimes it breaks the surface,
and you can just see it because 

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actually, the magnitude also 
determines how long the 

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faulting. 
So the great earthquake in 

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smarter in 2004 which produce 
sucks Me for example, was 1,200 

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kilometers long. 
That's from here, where I'm 

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speaking Cambridge London to 
Rome, right? 

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That's a great length and it, 
moved 20 meters or so huge 

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amount. 
So, that kind of thing is easy 

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to spot. 
The smaller ones are often 

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underground. 
A don't have any motion visible 

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at the surface at all, but we 
have very sophisticated ways of 

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seeing what's going on. 
We can tell from the sound or 

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shaking that the earthquakes, 
generate how much that there's 

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been. 
That's the science of 

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seismology. 
We can see How much the ground 

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surface roundabout moves by 
looking from space with radar 

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images, or Optical images? 
And we also now use GPS to do 

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the same thing, GPS is the 
technology that is used for your

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sat-nav, a, from the car, for 
example, which if you process it

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carefully enough, will show you 
how things move to within a few 

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millimeters. 
You don't need that accuracy for

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your car, but we can do it when 
we use it for our purposes. 

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So did we do that? 
For example, for the big T 11 

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earthquake in Japan? 
Yes, you do. 

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Because actually and this is 
quite interesting, the analogy I

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gave you a pushing a brick 
across the surface of the table 

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isn't quite right. 
Imagine you had a sponge and you

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push the sponge across the 
surface. 

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The sponge will actually 
compress quite a bit before it 

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suddenly jerked forward. 
And that's what happens to the 

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Rocks. 
So you can see the Rocks 

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actually bending and bulging 
before earthquakes and you can 

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see after earthquakes how they 
relax again and they change 

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shape. 
So after The great Japan 

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earthquake in 2011, the whole of
Japan on that and stretched, it 

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relaxed about 3 meters. 
So Japan was 3 meters wider 

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after the earthquake and it was 
before and do we measure that by

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having GPS sensors on each 
Coast? 

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Well changing. 
So, in fact, there are hundreds 

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or thousands of GPS sites 
measuring all the time because 

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ditions in places like Japan and
that's increasingly throughout 

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the world. 
And part of the reason is to 

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monitor earthquakes. 
And so on these sites will tell 

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Where they are relative to each 
other through within a few 

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millimeters. 
So they move several meters, 

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that's very, very easy to spot. 
But actually, to be honest, the 

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main reason they're being 
installed everywhere around the 

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world is this is now how you 
define property boundaries on 

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maps, you no longer say the 
boundary of my house is where 

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that tree is or where this river
is, you just give it a latitude 

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and longitude from the GPS and 
that's the basis now of modern 

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surveying. 
So that's why that is now 

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rapidly expanding as a resource.
The other thing you can do, this

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is another Modern trick, which 
is very interesting. 

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You can do this with radar 
images, from space or Optical 

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images from space. 
Is you take a photograph of a 

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large area and you divide it up 
into little pixels, little 

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patches on the ground, maybe 50 
centimeters across and then you 

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take another picture after the 
earthquake. 

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And in the region where the 
fault is. 

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These pixels have moved around 
on the edges of your picture. 

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If they haven't moved around. 
So, you simply superimpose one 

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on the other and round, the 
edges of your picture. 

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The pixels have moved, they all 
overlap. 

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Perfectly. 
And we're the folks is they've 

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all moved slightly and you can 
measure how much they've moved 

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in this will again give you the 
movement of the ground within a 

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few centimeters. 
It's not as accurate as GPS, but

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you cover a much wider area, 
instead of just a single point 

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and these things are very 
powerful when they're all used 

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together. 
So if you use seismology and the

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space Imaging and the GPS all at
the same time, you really can 

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nail what happens in 
extraordinary detail which we 

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could only have dreamt about 20 
years ago. 

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That's amazing. 
So So, with these satellite 

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image Maps, can we but of 
actually see this building 

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moved. 
So many meters over that way and

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river move that way. 
Yes, indeed. 

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You can easily and actually, 
this is a bit of a pain in the 

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neck for land, surveys in 
countries like New Zealand. 

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Their National Grid is moving 
around all the time, it has to, 

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it has to change with time 
because because this is 

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happening throughout the country
and the same is true in Japan. 

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The downside of measuring things
to Within A millimeter is that 

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they are moving within a few 
millimeters a year. 

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Most of these, are they Any of 
you. 

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So although most of the 
earthquakes we hear about happen

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in areas that we know high risk,
like, you mentioned Sumatra in 

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Japan and I suppose that apply 
to the whole Western rim of the 

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Pacific, as well as places, 
like, California earthquakes 

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actually, do also happen 
elsewhere, but much less often. 

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Why is that? 
Yes, this is an interesting 

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feature of our modern Earth 
today is that the really, really

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big earthquakes happen around 
the rim of the oceans and the 

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Pacific and in place. 
Is like Indonesia, but that is 

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not actually where most people 
die. 

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In earthquakes, many more people
die in earthquakes in the middle

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of continents and particularly 
in Asia. 

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So the Great Earthquake felt for
Trans all the way through the 

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Mediterranean, the Middle East 
and into Asia, all the way to 

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China through places like North 
India, Tibet and Central Asia 

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that area which is a huge, huge 
area as small earthquakes, but 

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they kill many more people. 
And there are multiple reasons 

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for that but the reason why it's
so different is Because the 

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continents behave in a different
way, from the oceans, the oceans

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are really the story of plate 
tectonics which everybody learns

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about now even in primary school
that the Earth is split up into 

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these spherical caps which move 
around relative to each other 

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and the earthquakes happen, 
where these caps interact with 

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each other and round, the edges 
of the oceans places like Japan,

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South America, Central America, 
or Alaska. 

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For example. 
What happens is the ocean slides

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underneath the adjacent 
continent? 

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Rather like a conveyor belt. 
Imagine the conveyor belt or 

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escalator on the staircase, 
going back into the ground. 

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That's what's happening to the 
ocean as it slides on the 

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continent and that interface 
where we ocean slides under the 

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continent, that's where the 
earthquakes happen. 

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So there's essentially one 
fault, which is doing the job 

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and it has to move pretty often 
because it's moving quite fast. 

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Typically a few centimeters per 
year. 

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Now, the continents are all the 
different because the continents

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are not really part of that 
story. 

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The continents are like, 
Floating on these plates. 

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They like passengers. 
And they don't cause any 

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trouble. 
If they're just an island in the

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middle of the Pacific or 
something, you get a problem 

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where one continent bashes into 
another continent. 

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And this is the problem with 
India, for example, which 

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belongs adjacent to Madagascar 
and Antarctica and Australia in 

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the Southern Ocean, it broke 
away and crossed as an island in

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the Indian Ocean until it bashed
into Asia. 

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And when you have a situation 
because the continents are made 

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of different material from the 
ocean, it's much less dense the 

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confidence that I life jacket. 
So they simply won't go down 

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there. 
I go down the hole like the 

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escalator or the conveyor belt 
and they just bash into the next

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continent and the whole thing 
crunches up. 

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And so what's happened in the 
case of India is India, has 

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smashed up Asia all the way from
the edge of the Himalayas to 

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Mongolia which is 3,000 
kilometers further. 

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North, the whole place is 
smashed up. 

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So there are many, many 
earthquakes are of a much wider 

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region instead of essentially 
being a single big fault on big 

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earthquake, Do you have around 
the edges of the oceans? 

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So what happens over millions 
and millions of years? 

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As movement happens repeatedly 
over either a single fault as 

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you mentioned at the plate 
boundaries or this massive 

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network of faults that you may 
have in the interior of a 

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continent. 
Well, what happened to India, 

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collided with a sure about 50 
million years ago and it's going

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at about 4 centimeters per year.
It's not like a car crash, it's 

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not stopped, it's still plowing 
into Asia that rate for He's 

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here about the rate, your 
fingernails grow and over 50 

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million years, then India has 
plowed 2000 km into Asian crush 

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it up. 
And that's why there are 

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hundreds and thousands even of 
faults in that part of Central 

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Asia. 
And because each of them is 

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contributing to that job of 
allowing India to move north, 

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eat particular, one doesn't have
to move very often whereas The 

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Faults offshore Japan or South 
America. 

230
00:11:50,500 --> 00:11:54,200
For example, they have to do all
the work, they're moving 

231
00:11:54,200 --> 00:11:56,200
frequently because they have to 
do all the work. 

232
00:11:56,300 --> 00:11:59,600
Does anybody want V to do it? 
So words earthquake to repeat 

233
00:11:59,600 --> 00:12:04,000
every few tens or maybe a 
hundred years or so in Japan and

234
00:12:04,000 --> 00:12:07,000
South America, in Central Asia, 
where there thousands of faults,

235
00:12:07,200 --> 00:12:09,400
each fault, may only repeat its 
movements. 

236
00:12:09,400 --> 00:12:13,500
Every few thousand years often 
Way Beyond human memory or 

237
00:12:13,500 --> 00:12:15,500
recorded history. 
And so they tend to catch 

238
00:12:15,500 --> 00:12:16,500
people. 
Unawares. 

239
00:12:16,700 --> 00:12:19,200
People are unaware that they're 
living in a dangerous place 

240
00:12:19,600 --> 00:12:21,400
because there are earthquakes 
all over the place. 

241
00:12:21,400 --> 00:12:23,600
There's nothing particularly 
distinguishes where they are. 

242
00:12:24,600 --> 00:12:28,300
Let's come down to the Fatal 
Attraction between cities and 

243
00:12:28,300 --> 00:12:31,900
earthquakes. 
Why do we build cities in areas 

244
00:12:31,900 --> 00:12:35,500
that are prone to earthquakes? 
Yeah, this is an interesting 

245
00:12:35,500 --> 00:12:37,500
feature again of Central Asia, 
really? 

246
00:12:37,500 --> 00:12:40,500
Or this great Alpine Himalayan 
earthquake belt from the 

247
00:12:40,500 --> 00:12:44,700
Mediterranean to China is that 
earthquakes occur and seemed 

248
00:12:44,700 --> 00:12:48,700
quite often to Target places 
where people live and you think 

249
00:12:48,700 --> 00:12:52,100
it's just as bad luck or is this
the kind of being vindictive? 

250
00:12:52,300 --> 00:12:55,900
And the reason for that is that 
the earthquakes and the faults. 

251
00:12:56,300 --> 00:13:00,600
Responsible for making the 
mountains and the particular 

252
00:13:00,600 --> 00:13:03,300
responsible for the edges of the
mountains where the mountains 

253
00:13:03,300 --> 00:13:06,200
meet deserts or high plateaus 
like to bed. 

254
00:13:06,800 --> 00:13:09,200
And that's where people live. 
If you like living on the edges 

255
00:13:09,200 --> 00:13:12,200
of mountains, because that's 
where the water supply is, its, 

256
00:13:12,200 --> 00:13:15,200
where agriculture is possible. 
It's usually where the trade 

257
00:13:15,200 --> 00:13:17,900
route runs on the edge of the 
mountains and of course it's 

258
00:13:17,900 --> 00:13:21,500
strategically important for 
access to those trade routes as 

259
00:13:21,500 --> 00:13:22,900
well. 
So what happens is that 

260
00:13:22,900 --> 00:13:26,100
settlements grow up along those 
trade routes on the edges of 

261
00:13:26,200 --> 00:13:28,800
Mountains and then they develop,
and they become bigger and 

262
00:13:28,800 --> 00:13:30,100
bigger. 
And so, the populations 

263
00:13:30,100 --> 00:13:33,400
concentrate in these dangerous 
places, it would be fine to live

264
00:13:33,400 --> 00:13:36,600
in the middle of the flat desert
in Iran or Central Asia, but 

265
00:13:36,600 --> 00:13:38,700
there is no likelihood there. 
There's no Waters and 

266
00:13:38,700 --> 00:13:41,000
agriculture possible. 
You can't live there. 

267
00:13:41,100 --> 00:13:44,600
And so you live with where life 
is possible in these desert 

268
00:13:44,600 --> 00:13:48,300
countries and that is almost 
inevitably places where life is 

269
00:13:48,300 --> 00:13:51,900
possible because the faulting 
has created the circumstances 

270
00:13:51,900 --> 00:13:54,100
that make agriculture and water 
supply possible. 

271
00:13:55,400 --> 00:13:59,200
So, You've described how that 
can happen at the edge of 

272
00:13:59,200 --> 00:14:01,900
mountain ranges such as the 
Himalayas or the Alps where you 

273
00:14:01,908 --> 00:14:05,400
have well in the Himalayan case 
India plowing into Asia. 

274
00:14:06,000 --> 00:14:09,000
Does that also apply on 
coastlines? 

275
00:14:09,000 --> 00:14:12,800
Because we love to build cities 
on coastlines in places where 

276
00:14:12,800 --> 00:14:14,900
the earthquakes. 
Yes, is tectonic plates that 

277
00:14:14,900 --> 00:14:17,900
just crunched together. 
They can also pull apart and 

278
00:14:17,900 --> 00:14:22,200
drift apart, and that's for 
example, why the coastline is 

279
00:14:22,200 --> 00:14:25,400
where it is between Greece and 
Turkey or between Norway and 

280
00:14:25,400 --> 00:14:27,500
Scotland. 
Although Annoying Scotland is no

281
00:14:27,500 --> 00:14:29,500
longer active. 
It did it all about 100 million 

282
00:14:29,500 --> 00:14:33,300
years ago, but now it's active 
in places like Greece, Central 

283
00:14:33,300 --> 00:14:36,300
Central Aegean, Sea of Japan, 
Greece, and Turkey, and indeed, 

284
00:14:36,300 --> 00:14:38,000
that is why the coastline is 
where it is. 

285
00:14:38,000 --> 00:14:40,800
That's where most of the action 
is, that's where the earthquakes

286
00:14:40,800 --> 00:14:42,800
are. 
And so, if you live in countries

287
00:14:42,800 --> 00:14:46,300
where there are earthquakes, 
it's a good idea to ask why is 

288
00:14:46,300 --> 00:14:48,000
landscape? 
Like it does. 

289
00:14:48,000 --> 00:14:52,200
And that's nearly always because
of faulting associated with 

290
00:14:52,200 --> 00:14:55,000
earthquakes in places like 
California or the Mediterranean 

291
00:14:55,000 --> 00:14:58,400
Middle, East Central Asia. 
Zeeland East Africa, the 

292
00:14:58,400 --> 00:15:01,200
mountains are there because of 
the activity and faults in 

293
00:15:01,200 --> 00:15:05,500
earthquake. 
So what impact have earthquakes 

294
00:15:05,500 --> 00:15:08,700
had over history on these cities
that have succumbed to this 

295
00:15:08,700 --> 00:15:13,900
attraction to earthquakes well. 
So this is very interesting that

296
00:15:13,900 --> 00:15:17,600
the number of modern cities 
which have grown into a huge 

297
00:15:17,600 --> 00:15:21,700
population, centers along, for 
example, the old Silk routes, 

298
00:15:21,800 --> 00:15:24,700
which connected China, to the 
Mediterranean, a lot of cities, 

299
00:15:24,700 --> 00:15:27,000
along those routes have been 
destroyed, Multiple times in the

300
00:15:27,000 --> 00:15:30,100
past, but in the past, they were
intended to be rather small, 

301
00:15:30,500 --> 00:15:34,400
they tended to be stopovers on 
trade routes but now there are 

302
00:15:34,400 --> 00:15:37,700
any of them even capital cities 
of countries in Central Asia and

303
00:15:37,700 --> 00:15:40,100
they've been destroyed in the 
past, but whereas, in the past 

304
00:15:40,100 --> 00:15:44,300
say, they're unlucky, they lost 
10,000 people or so now they 

305
00:15:44,300 --> 00:15:48,100
have cities of million or more 
and they're very much more 

306
00:15:48,100 --> 00:15:49,800
vulnerable. 
It's still in the dangerous 

307
00:15:49,800 --> 00:15:53,400
place but they've increased the 
population dramatically without 

308
00:15:53,500 --> 00:15:57,600
I'm sorry to say in most cases. 
Their resilience to the 

309
00:15:57,600 --> 00:15:59,300
earthquakes that are bound to 
happen again. 

310
00:16:00,200 --> 00:16:03,500
Can we help people in these 
cities, prepare for the next 

311
00:16:03,500 --> 00:16:06,700
earthquake, by predicting when 
it'll happen or roughly when 

312
00:16:06,700 --> 00:16:10,200
it'll happen, for example, I 
know that we can detect bulging 

313
00:16:10,200 --> 00:16:14,300
movement on volcanoes that for 
warn us of eruptions on 

314
00:16:14,300 --> 00:16:16,500
volcanoes. 
Does that also apply on the 

315
00:16:16,500 --> 00:16:18,300
tectonic scale? 
Two continents. 

316
00:16:18,900 --> 00:16:23,100
Well, now you've touched a very 
interesting question and we have

317
00:16:23,100 --> 00:16:25,400
to be careful how we use words 
in this area. 

318
00:16:26,200 --> 00:16:29,000
Short term prediction means 
saying, there's going to be an 

319
00:16:29,000 --> 00:16:32,300
earthquake sometime within. 
You know, say let's say next 

320
00:16:32,300 --> 00:16:36,700
Wednesday, plus or minus of a 
and in some particular place 

321
00:16:37,000 --> 00:16:40,200
such and such a size and we 
can't do that the science isn't 

322
00:16:40,200 --> 00:16:43,800
there, people have looked very 
hard for precursors. 

323
00:16:43,800 --> 00:16:46,400
They're called with some sort of
Warning Sign beforehand. 

324
00:16:46,900 --> 00:16:50,000
There's nothing which has been 
found to be reliable and it's 

325
00:16:50,000 --> 00:16:53,600
not something which has been 
successful. 

326
00:16:54,200 --> 00:16:57,600
We contrast that with 
Forecasting, long-term 

327
00:16:57,600 --> 00:16:59,800
forecasting is fine. 
Long-term forecast is simply 

328
00:16:59,800 --> 00:17:02,100
saying where there's been an 
earthquake in the past few days 

329
00:17:02,100 --> 00:17:04,200
about it will happen again in 
the future sometime. 

330
00:17:04,200 --> 00:17:07,200
You can't say when but we can 
say quite a lot with a bit of 

331
00:17:07,200 --> 00:17:10,099
work, about how big that 
earthquake will be, what its 

332
00:17:10,099 --> 00:17:13,099
characteristics will be, how 
much the likely shaking will be 

333
00:17:13,300 --> 00:17:16,500
along last, how big it will be, 
how much the default might move.

334
00:17:16,500 --> 00:17:18,700
But all these things are of 
interest to Architects and 

335
00:17:18,700 --> 00:17:22,800
engineers and planners because 
if they know what the threat is,

336
00:17:22,800 --> 00:17:25,700
what they're up against, they 
can actually design things for 

337
00:17:25,700 --> 00:17:28,900
it and that's It's been very 
successful again in countries 

338
00:17:28,900 --> 00:17:32,100
around the Pacific Rim. 
For example, it's much harder to

339
00:17:32,100 --> 00:17:36,000
do in Central Asia because there
are more faults most that we 

340
00:17:36,000 --> 00:17:39,800
don't know about and there are 
generally other priorities and 

341
00:17:39,800 --> 00:17:43,600
this is the problem is that in 
many cities in places where 

342
00:17:43,600 --> 00:17:47,300
earthquakes are less frequent, 
but more dangerous in those 

343
00:17:47,300 --> 00:17:48,900
places people have other 
priorities. 

344
00:17:48,900 --> 00:17:51,300
So if I was to say to you that 
the last earthquake was 500 

345
00:17:51,300 --> 00:17:53,300
years ago in your city, you 
would say. 

346
00:17:53,300 --> 00:17:56,000
Well everyday, I takes me two 
hours to get to work. 

347
00:17:56,200 --> 00:17:58,100
As congestion, the air quality 
is rubbish. 

348
00:17:58,100 --> 00:18:02,200
Our problems of water supply 
traffic Thomas on this 

349
00:18:02,200 --> 00:18:05,000
earthquake, 500 years ago, 
that's not my problem, but 

350
00:18:05,000 --> 00:18:08,500
actually, it is your problem 
eventually, but it's not highly 

351
00:18:08,500 --> 00:18:11,800
prioritized by contrast. 
If you lived in, in Chile, for 

352
00:18:11,800 --> 00:18:15,000
example, you feel earthquakes 
all the time, and, you know, 

353
00:18:15,000 --> 00:18:17,900
that you'll feel 95. 
Earthquake every year. 

354
00:18:17,900 --> 00:18:20,800
You'll feel 97 probably every 
ten years and they'll probably 

355
00:18:20,800 --> 00:18:22,600
be a magnitude 8 earthquake in 
your lifetime. 

356
00:18:22,800 --> 00:18:25,200
You know, this is not a 
theoretical threat, it will 

357
00:18:25,200 --> 00:18:28,100
affect you, your Children and 
your grandchildren and people 

358
00:18:28,100 --> 00:18:30,200
are quite happy to prioritize 
it. 

359
00:18:30,600 --> 00:18:34,900
And so in fact they're helped 
around the Pacific Rim by having

360
00:18:34,900 --> 00:18:38,400
many many more earthquakes in 
the same place repeating as it 

361
00:18:38,400 --> 00:18:41,700
were and in Central Asia where 
they're more distributed and 

362
00:18:41,800 --> 00:18:45,100
less frequent in any one 
particular place and so we can 

363
00:18:45,100 --> 00:18:47,900
help them. 
They need to do the work to put 

364
00:18:47,900 --> 00:18:51,300
in the work to know what the 
hazard is that they're actually 

365
00:18:51,300 --> 00:18:54,200
facing. 
There's no real shortcut to that

366
00:18:54,700 --> 00:18:58,200
but it's just on the whole not. 
Sighs places like Japan, New 

367
00:18:58,200 --> 00:19:02,500
Zealand, California and Chile 
have put in decades of really 

368
00:19:02,600 --> 00:19:06,100
hard, scientific effort to find 
out what they're up against so 

369
00:19:06,100 --> 00:19:09,900
they can plan and prepare and 
they've been super be successful

370
00:19:09,900 --> 00:19:12,000
at it. 
When you say what they're up 

371
00:19:12,000 --> 00:19:16,100
against, does that mean mapping 
the faults in detail? 

372
00:19:16,100 --> 00:19:20,200
So we have a better idea to east
of where the next one might be 

373
00:19:20,200 --> 00:19:24,300
that's going to rupture the. 
Yes certainly that's part of it.

374
00:19:24,500 --> 00:19:26,700
But there are two things which 
could send a few or an engineer 

375
00:19:26,700 --> 00:19:29,300
building a dam. 
For example, in a River Gorge, 

376
00:19:29,300 --> 00:19:32,200
you want to know why that Gorge 
is there and if the gorge is 

377
00:19:32,200 --> 00:19:35,000
there because there's a fault, 
the rivers flowing down it that 

378
00:19:35,000 --> 00:19:37,500
affect how you build your down, 
which I get physically ripped 

379
00:19:37,500 --> 00:19:39,600
apart. 
So there's an interest in 

380
00:19:39,600 --> 00:19:42,700
knowing where the fault itself 
is for sure, for particular 

381
00:19:42,700 --> 00:19:46,900
facilities and threats. 
But also, in many places for 

382
00:19:46,900 --> 00:19:49,000
planning purposes, statistics 
are good enough. 

383
00:19:49,000 --> 00:19:52,500
You just want to know in this 
particular area, what is the 

384
00:19:52,500 --> 00:19:56,500
largest likely ground shaking 
the duration, one of the First, 

385
00:19:56,500 --> 00:19:59,500
you select shaking in order to 
allow people to plan how to 

386
00:19:59,500 --> 00:20:01,700
build buildings and so on. 
So there's a difference between 

387
00:20:02,000 --> 00:20:05,200
being physically ripped apart by
being astride the fault and 

388
00:20:05,200 --> 00:20:07,200
being shaken. 
Because your next to the fold, 

389
00:20:08,000 --> 00:20:09,700
how good are the historical 
records? 

390
00:20:10,000 --> 00:20:12,800
Speaking of knowing what the 
impact is being in history in 

391
00:20:12,800 --> 00:20:17,200
these high-risk areas and 
ironically, the risk areas which

392
00:20:17,200 --> 00:20:19,100
are certainly in Central Asia 
and the Alpine. 

393
00:20:19,100 --> 00:20:22,500
Himalayan Central Asia region 
their historical record is much 

394
00:20:22,500 --> 00:20:25,300
better than around the Pacific 
Rim so that the historical 

395
00:20:25,300 --> 00:20:28,000
record in the right places at 
least between the Mediterranean 

396
00:20:28,000 --> 00:20:30,300
and China go back 2,000 years or
so. 

397
00:20:30,700 --> 00:20:34,200
Whereas around the Pacific Rim, 
they've been inhabited by people

398
00:20:34,200 --> 00:20:37,800
writing records or keeping 
records for not very long, a few

399
00:20:37,800 --> 00:20:42,100
hundred years except for Japan 
but in Asia there's an enormous 

400
00:20:42,100 --> 00:20:45,600
amount of information in the 
records of Empires. 

401
00:20:45,600 --> 00:20:48,400
So the Byzantine Empire, the 
Ottoman Empire, the various 

402
00:20:48,400 --> 00:20:52,600
Persian Empires and of course 
China were quite bureaucratic. 

403
00:20:52,600 --> 00:20:56,700
They kept very good records of 
these things which Be an 

404
00:20:56,700 --> 00:21:00,200
enormous goal by now. 
People go back and look at these

405
00:21:00,500 --> 00:21:03,600
counts kept by the bureaucracies
of those time. 

406
00:21:04,300 --> 00:21:06,400
It's a very, very scholarly 
activity. 

407
00:21:06,400 --> 00:21:09,200
You have to be a fantastic 
linguist and historian just to 

408
00:21:09,208 --> 00:21:12,200
get to first base, might be able
to look at in this stuff and 

409
00:21:12,200 --> 00:21:14,400
then you have to know we talked 
about in terms of the geology. 

410
00:21:14,400 --> 00:21:17,000
The seismology engineering to 
know how to interpret. 

411
00:21:17,000 --> 00:21:19,100
These records are very often 
exaggerated. 

412
00:21:19,300 --> 00:21:23,500
They have particular styles of 
describing these calamities and 

413
00:21:23,500 --> 00:21:25,600
they're not interested in things
like ground motion, their 

414
00:21:25,600 --> 00:21:29,000
interests Add in disruption to 
life and property and trade and 

415
00:21:29,000 --> 00:21:31,000
so on. 
But you can interpret these 

416
00:21:31,000 --> 00:21:33,300
things and they are extremely 
helpful. 

417
00:21:33,500 --> 00:21:35,800
You have to get at that sort of 
information in these other 

418
00:21:35,800 --> 00:21:39,600
countries should be settled this
or for less Long in a more 

419
00:21:39,600 --> 00:21:41,600
forensic. 
Detective kind of way by looking

420
00:21:41,600 --> 00:21:44,400
at the geological evidence, 
which is also possible that hard

421
00:21:44,400 --> 00:21:48,700
work, that's fascinating that 
work that needs to be done is 

422
00:21:48,700 --> 00:21:53,500
both very much historical and 
sociological and really human in

423
00:21:53,500 --> 00:21:55,500
nature. 
Going back these thousands of 

424
00:21:55,500 --> 00:21:59,600
years as I was on the other end 
very cutting-edge measuring 

425
00:21:59,700 --> 00:22:03,200
precisely where Faults Are and 
using all the battery of 

426
00:22:03,200 --> 00:22:06,500
techniques that we have today to
figure out the present 

427
00:22:06,500 --> 00:22:08,700
situation. 
It's very interesting it and 

428
00:22:08,700 --> 00:22:10,800
there's a very good relationship
between these routes. 

429
00:22:11,000 --> 00:22:13,400
The historical work. 
Is an immense. 

430
00:22:13,900 --> 00:22:16,300
Long-term work of scholarship is
not the sort of thing. 

431
00:22:16,300 --> 00:22:18,800
You achieve in a three-year 
research around it. 

432
00:22:18,800 --> 00:22:21,500
Something we know people spend 
their life time, researching the

433
00:22:21,500 --> 00:22:24,100
history of earthquakes in Clash 
or something like that, and they

434
00:22:24,100 --> 00:22:26,200
come up with these historical 
earthquakes and then it It's the

435
00:22:26,208 --> 00:22:29,500
job of the modern scientists to 
then figure out. 

436
00:22:29,500 --> 00:22:31,500
Okay, where was The Fault? 
Which was responsible for that 

437
00:22:31,500 --> 00:22:33,200
earthquake? 
Can we actually find on the 

438
00:22:33,200 --> 00:22:35,100
ground? 
What did it and the evidence 

439
00:22:35,100 --> 00:22:38,000
that it really did do it for the
whole thing together. 

440
00:22:38,000 --> 00:22:40,800
So, there's a very close working
relationship between these 

441
00:22:40,800 --> 00:22:44,300
different groups. 
So, you live in Cambridge near 

442
00:22:44,300 --> 00:22:49,500
London and I live in Boston. 
Are we in a safe area for my 

443
00:22:49,500 --> 00:22:53,700
historical earthquake point of 
view in the sense that most of 

444
00:22:53,700 --> 00:22:55,700
the earthquakes in the United 
States on the West Coast? 

445
00:22:56,100 --> 00:22:58,900
And most of the earthquakes in 
Europe, by the Mediterranean 

446
00:22:59,300 --> 00:23:02,100
heading Eastward, through Italy,
Italy, Greece, and Turkey and so

447
00:23:02,100 --> 00:23:05,400
on, it doesn't mean we don't 
have any, we have some and lost 

448
00:23:05,400 --> 00:23:07,200
of confidence have smaller 
earthquakes. 

449
00:23:07,200 --> 00:23:09,400
We have any from in Cambridge. 
I remember from the last ten 

450
00:23:09,400 --> 00:23:11,300
years, the couple of 
earthquakes, which are working 

451
00:23:11,300 --> 00:23:13,900
people up there. 
It's very, very small by the 

452
00:23:13,900 --> 00:23:16,300
standards of these proper 
earthquake countries. 

453
00:23:16,300 --> 00:23:18,700
Could something people wouldn't 
get out of bed for, but they're 

454
00:23:18,700 --> 00:23:20,700
not negligible, you have to 
watch out slightly. 

455
00:23:20,700 --> 00:23:23,300
So for example, if you're 
building something which is very

456
00:23:23,300 --> 00:23:26,800
sensitive, like a nuclear power 
station, you really need to know

457
00:23:26,800 --> 00:23:30,500
what's going on. 
So you will have some assessment

458
00:23:30,500 --> 00:23:32,800
of what you think. 
The likely largest historical if

459
00:23:32,800 --> 00:23:36,500
B was or might be in the future 
and you will over designed to be

460
00:23:36,500 --> 00:23:40,000
safe in that. 
And so although people in 

461
00:23:40,000 --> 00:23:42,800
England really don't think about
it, breaks the electricity 

462
00:23:42,800 --> 00:23:45,400
generating board who run the new
capacitation, certainly do. 

463
00:23:45,400 --> 00:23:49,400
And they've designed to in order
to be conservative for what they

464
00:23:49,400 --> 00:23:51,200
think is the largest historical 
earthquakes. 

465
00:23:51,500 --> 00:23:53,600
And the same is true, for 
example, needs Coast United 

466
00:23:53,600 --> 00:23:55,900
States. 
And that's more interesting. 

467
00:23:56,100 --> 00:24:00,200
Because actually you probably 
know that the Atlantic opens in 

468
00:24:00,200 --> 00:24:04,100
the Jurassic 150 million years 
ago something and of course, the

469
00:24:04,100 --> 00:24:06,900
Appalachians is part of 
Scotland, essentially belonged 

470
00:24:06,900 --> 00:24:09,800
up against Ireland and Scotland 
and you think it's just the 

471
00:24:09,800 --> 00:24:11,900
other half of that situation in 
the North Sea. 

472
00:24:12,200 --> 00:24:15,300
Now, in the UK and Northern 
Europe, we have of a long 

473
00:24:15,300 --> 00:24:19,300
historical record mainly based 
on monastic record monastic 

474
00:24:19,300 --> 00:24:21,900
Chronicles, which go back. 
Nearly two thousand years and 

475
00:24:21,900 --> 00:24:25,500
there really has never been a 
really big earthquake in the UK 

476
00:24:25,500 --> 00:24:28,400
and the We'll see in those last 
two thousand years, nothing 

477
00:24:28,400 --> 00:24:31,500
awesome about Matthew 5 and a 
half which is really not going 

478
00:24:31,500 --> 00:24:34,200
to cause trouble and you go to 
United States. 

479
00:24:34,200 --> 00:24:36,600
The same is not true. 
It's been settled for a few 

480
00:24:36,600 --> 00:24:39,200
hundred years at least a good 
historical record for the last 

481
00:24:39,200 --> 00:24:42,300
few hundred years. 
And in that time, they've been 

482
00:24:43,000 --> 00:24:45,900
several earthquakes quite a lot,
bigger than anything in Europe 

483
00:24:45,900 --> 00:24:48,600
in the last 2,000 years, and 
most famous was in Charleston. 

484
00:24:48,600 --> 00:24:52,500
South Carolina in 1886, there's 
one in caveman, which is where 

485
00:24:52,500 --> 00:24:55,900
you never be in Massachusetts. 
I think that was about 1750 

486
00:24:56,100 --> 00:25:00,500
Five, but these were Manchu 6, 
Plus, and certainly bigger than 

487
00:25:00,800 --> 00:25:03,100
anywhere in Northwest Europe, 
know why there should be that 

488
00:25:03,100 --> 00:25:06,800
contrast between geologically. 
What if you like two halves of 

489
00:25:06,800 --> 00:25:10,000
the same mirror, like the lad. 
You just broke split. 

490
00:25:10,000 --> 00:25:12,900
The two in part. 
Why the American side should 

491
00:25:12,900 --> 00:25:15,100
behave? 
So differently from the European

492
00:25:15,100 --> 00:25:17,500
side. 
No one really understands, but 

493
00:25:17,800 --> 00:25:20,600
they do. 
And so you have to design for 

494
00:25:20,600 --> 00:25:24,500
certainly big earthquakes and 
people are contemplating in 

495
00:25:24,500 --> 00:25:27,100
Northwest Europe. 
Charleston earthquake did a lot 

496
00:25:27,100 --> 00:25:29,300
of damage in South Carolina in 
1880. 

497
00:25:29,300 --> 00:25:32,900
See, it was a big deal and I 
just very well investigated and 

498
00:25:32,900 --> 00:25:35,300
they were written up and there's
a lot of detail about it. 

499
00:25:35,900 --> 00:25:38,800
Didn't do too much because of 
course in those days in South 

500
00:25:38,800 --> 00:25:42,300
Carolina, people mostly lived in
wooden houses which were quite 

501
00:25:42,300 --> 00:25:43,700
well built, they behave very 
well. 

502
00:25:43,700 --> 00:25:46,300
Where does the best building 
material can happen in office? 

503
00:25:46,300 --> 00:25:48,900
Europe would is an expensive 
building material so it's not 

504
00:25:48,900 --> 00:25:52,100
that common. 
I'm going to ask you for my last

505
00:25:52,100 --> 00:25:55,900
question to be a little bit of 
forecaster, I know you do. 

506
00:25:56,000 --> 00:25:59,300
Like to do that. 
But what I'm wondering is that 

507
00:25:59,300 --> 00:26:02,800
even though the earthquakes that
have happened in these dangerous

508
00:26:03,000 --> 00:26:07,400
belts in Central Asia and 
elsewhere are on time scales 

509
00:26:07,400 --> 00:26:09,200
longer than an individual human 
life. 

510
00:26:09,200 --> 00:26:12,500
So, there isn't a personal 
memory that perhaps makes people

511
00:26:12,700 --> 00:26:16,300
aware and attuned to the risk. 
One thing that has happened on a

512
00:26:16,300 --> 00:26:18,900
shorter time scale is this 
enormous growth in our 

513
00:26:18,900 --> 00:26:20,900
scientific knowledge 
understanding which you've 

514
00:26:20,900 --> 00:26:24,100
alluded to, in this talk? 
Do you have a sense as to 

515
00:26:24,108 --> 00:26:27,700
whether this knowledge can be 
brought to bear to make this 

516
00:26:27,900 --> 00:26:31,600
connection between cities and 
false, a little less fatal in 

517
00:26:31,600 --> 00:26:35,000
the next few years, and decades 
while development proceeds in 

518
00:26:35,008 --> 00:26:38,900
these countries, I hope so. 
That is an excellent question 

519
00:26:38,900 --> 00:26:42,300
and that has occupied me the 
last 10 years. 

520
00:26:43,000 --> 00:26:45,900
How do you actually turn the 
scientific knowledge into some 

521
00:26:46,200 --> 00:26:49,400
increased Public Safety, and 
it's presumptuous to think the 

522
00:26:49,400 --> 00:26:51,700
problem is just scientific. 
Of course, it's not it's to do 

523
00:26:51,700 --> 00:26:53,700
with well. 
Health and Social logical 

524
00:26:53,700 --> 00:26:56,200
conditions, cultural conditions,
economics. 

525
00:26:56,200 --> 00:26:59,400
All those kinds of things as 
well in the long run. 

526
00:26:59,400 --> 00:27:02,200
You know, the only thing which 
works is education. 

527
00:27:02,900 --> 00:27:06,100
People need to know what they're
up against a need to know, it's 

528
00:27:06,100 --> 00:27:09,800
not hopeless, right? 
That the great iniquity, I think

529
00:27:09,800 --> 00:27:11,900
is short-term earthquake 
prediction, which is like 

530
00:27:11,900 --> 00:27:15,300
promise of a Panacea, a silver 
bullet if you allow the public 

531
00:27:15,300 --> 00:27:17,900
to believe in it, it also allows
them to think it's not their 

532
00:27:17,900 --> 00:27:20,700
problem, a scientist will sort 
it out one day, they'll say the 

533
00:27:20,700 --> 00:27:22,300
earthquakes can be Wednesday at 
9:30. 

534
00:27:22,300 --> 00:27:25,700
We I didn't have to do anything.
That is faithful that kills lots

535
00:27:25,700 --> 00:27:29,200
of people that attitude and 
that's one of the roles of the 

536
00:27:29,200 --> 00:27:31,800
scientists is to say, actually, 
that isn't going to happen. 

537
00:27:32,300 --> 00:27:35,800
On the other hand, there are 
things you can do to make life 

538
00:27:35,800 --> 00:27:38,600
safer big a on. 
There are lots of very switched 

539
00:27:38,600 --> 00:27:42,900
on good people in those areas 
governments and ngos and Civic 

540
00:27:42,900 --> 00:27:46,500
leaders who want to do the right
thing and who care about this 

541
00:27:46,800 --> 00:27:49,100
and they need help but the 
scientists can help them by 

542
00:27:49,500 --> 00:27:52,500
helping them be realistic about 
what the public. 

543
00:27:52,700 --> 00:27:55,000
He's going to face and they're 
in the number of such studies in

544
00:27:55,000 --> 00:27:58,900
countries like China and Nepal 
where you do a detailed study. 

545
00:27:58,900 --> 00:28:01,900
You know this was our son 
incidentally in Kathmandu which 

546
00:28:01,900 --> 00:28:05,500
had the big earthquake in 2015 
before that earthquake and NGO 

547
00:28:05,500 --> 00:28:08,500
had put together a study of what
would happen if the previous 

548
00:28:08,500 --> 00:28:12,800
earthquake which was 1934 in 
Katmandu repeated, right? 

549
00:28:12,800 --> 00:28:16,200
And what would happen if that 
1934 earthquake repeated today, 

550
00:28:16,500 --> 00:28:18,900
given the so change in 
circumstances in terms of 

551
00:28:19,200 --> 00:28:22,000
Greater population population 
density, the quality of 

552
00:28:22,000 --> 00:28:24,700
buildings. 
The lifelines by which they mean

553
00:28:24,700 --> 00:28:28,400
things like roads and water 
supply and power Appliance on 

554
00:28:28,900 --> 00:28:32,200
what would happen today and they
did that study and it wasn't 

555
00:28:32,200 --> 00:28:36,100
some arm wavy publicity stunt. 
It was two years of really hard,

556
00:28:36,200 --> 00:28:39,900
scientific evaluation of what 
that earthquake was in, 1934, 

557
00:28:39,900 --> 00:28:42,400
what caused it, where the fault 
was that moved? 

558
00:28:42,400 --> 00:28:44,600
What was the ground shaking? 
What would that ground-shaking 

559
00:28:44,600 --> 00:28:47,400
do today? 
And they publish it as a story, 

560
00:28:47,400 --> 00:28:51,500
almost as a cartoon picture book
illustrating the consequences of

561
00:28:51,500 --> 00:28:53,900
such an earthquake for a Family 
in Katmandu. 

562
00:28:54,000 --> 00:28:56,600
So the father would be working 
the other side of the city, the 

563
00:28:56,600 --> 00:28:59,200
bridges over the river, would 
have been collapsed so he would 

564
00:28:59,200 --> 00:29:00,900
take him two days to get home in
Wild. 

565
00:29:00,900 --> 00:29:03,000
What do people do? 
They're going to camp on the 

566
00:29:03,000 --> 00:29:05,200
football field. 
They have 23 Days In and Out of 

567
00:29:05,200 --> 00:29:09,200
Water and so on and so on time. 
And this was a story to get 

568
00:29:09,200 --> 00:29:11,000
people to concentrate their 
minds and what would actually 

569
00:29:11,000 --> 00:29:13,200
happen. 
And then in 2015, the earthquake

570
00:29:13,200 --> 00:29:16,400
did happen and you could read 
this story book and more. 

571
00:29:16,400 --> 00:29:19,000
Let's turn over the page and say
this is what's gonna happen 

572
00:29:19,000 --> 00:29:22,000
tomorrow and it more or less. 
Did they had a lucky Escape? 

573
00:29:22,000 --> 00:29:24,800
Because you're okay. 
Wasn't quite as big as 1934. 

574
00:29:25,100 --> 00:29:29,400
So instead of getting 100,000 
people about 10,000 people James

575
00:29:29,400 --> 00:29:31,100
Jackson, thank you very much.
