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This is geology B with Oliver 
stimple. 

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Since the first geological 
surveys of Southern Greenland in

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the 19th and early 20th 
centuries, it has been 

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recognized that the region 
contains some remarkable igneous

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rocks these include 
extraordinarily thick Dykes up 

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to 800 meters, thick and 
elliptical intrusions several 

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kilometers in size containing a 
profusion of exotic minerals in 

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the 1930s, this period of 
igneous. 

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Activity was christened the Gada
period after the north are 

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Bishopric of God are established
in the area in the 12th century.

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In the 1970s, the rocks of the 
Garda period would dated using 

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uranium lead, radiometric dating
and found to be between 1.1 and 

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1.3 billion years old. 
The dating also revealed that 

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most of the Rocks surrounding 
the thick Dykes and elliptical 

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intrusions of the Garda period 
is a giant. 

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Granite batholith, that is 1.8 
to 1.9 billion years old. 

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The baffle if was in placed 
during a mountain building a And

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accompanying the Assembly of the
Palio proterozoic supercontinent

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called Noona about 700 million 
years before the Garda rocks 

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were formed for a refresher on 
Noona and supercontinents. 

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In general. 
You can listen to David Evans in

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an early episode of geology B. 
It was not until the 1950s that 

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geological studies of the area 
revealed just how exceptional 

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the god are rocks. 
Are one of the leading 

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researchers who brought this to 
light is Brian Upton. 

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Who was studied the Region's 
geology intensively, and spent 

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over 20 seasons in the field 
between 1957 and 2005. 

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In what follows Brian? 
Upton? 

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Discusses both types of God are 
intrusions the giant Dykes, and 

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the elliptical intrusions that 
Scott them. 

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He refers to the latter 
variously as alkaline complexes 

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and Central complexes. 
Brian Upton is Emeritus 

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professor of geology at the 
University of Edinburgh. 

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Brian Upton. 
Welcome to geology, B. 

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Thank you very much. 
I'm very happy to be with you. 

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What led you to the guard? 
Our region. 

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When you first arrived on the 
scene, in 1955 principal 

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motivation for this was partly 
for looking for more uranium, 

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but also Also looking for more 
crowl, light, for the aluminium 

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industry, in the course of this.
We would also mapping 

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everything. 
Okay, went along. 

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What structural features did you
find? 

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I was put on to some fascinating
ground that had recently been 

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discovered by helicopter, 
reconnaissance work, which 

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included some very large, dikes.
And some new Alpha line 

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complexes. 
I was delighted by that and it 

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was only in the fullness of time
that I will. 

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It was possible whole system, 
the whole evolutionary process 

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that led to the extraordinary 
rocks. 

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So you found these enormously 
thick Dykes. 

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What do you think might have 
caused the dikes to be so very 

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thick. 
Well during the Precambrian, the

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heat flow to the upper mantle 
and into the crust was 

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considerably greater than it 
was. 

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Subsequently were talking over a
thousand million years ago. 

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And I think the energy was 
sufficient that when they 

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actually go and shoot Food 
around the world, goes some 

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other big ones being used. 
We see these in Canada, we've 

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seen Ethan Sweden extreme 
Southwest Australia and the 

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biggest of the laughs is the 
exam, Bob, we great dike which 

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is about 13 kilometers across 
and hundreds of kilometers long 

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but I didn't know how he said I 
was looking at it, we were might

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relate to the elbows. 
And in fact it is chemically 

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rather different. 
It's unusual in this high 

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content of So called 
incompatible elements is an 

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alpha Li to break. 
Dyke was all of the others are, 

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by no means how Kelly, what can 
we infer by the tectonic context

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that led to the formation of 
these huge? 

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Dikes in the guard, our 
Province, really nothing major 

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happened in that area for 
several hundred million years, 

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but there was a large Granite 
basileus that have been formed 

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after the last ocean closure 
there. 

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I'm the new activity ligado, 
activity. 

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Tended to be concentrated along 
the axis of this granite 

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basileus, and it looks with the 
center of the Basilisk. 

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Mechanically weak and had. 
Given way to allow Magnus to 

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come up to fractures a whole 
bunch of Dykes, which in places 

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Amalgamated to form one, which 
was as big as 800 meters, you 

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found Dykes. 
But you also found some large. 

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Mountain scale intrusions. 
Can we talk about those a bit? 

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We started getting these 
elliptical things which I will, 

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most certainly are feeding 
volcanoes comparable to those of

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the East African Rift. 
But with a top two or three 

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kilometers missing because this 
whole region of the Guard, our 

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Province on the Rocks around it 
had been uplifted very, very 

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gently during the course of the 
thousand million years or so it 

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has never been folded. 
We'll be in badly altered in any

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way. 
It'll be lifted up and in so 

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doing it. 
And being exposed to erosion 

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which had taken the skin off 
either. 

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Taken the top seal four 
kilometers off. 

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So we were looking modestly deep
in the crust but not very deep, 

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but we're losing, the stuff is 
parts. 

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So these elliptical intrusive 
complexes are cyanides what our 

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sign i'ts. 
And what minerals do they 

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principally contain? 
Well, I have to say that the 

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most widespread and the 
important mineral on the whole 

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surface of our planet, are those
of the group called feldspars, 

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which are aluminium silicate, 
but the aluminium silicate, 

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sheets are held together by 
other elements in particular by 

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calcium or by potassium or by 
sodium and those with potassium 

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and sodium are called Alkali 
feldspars. 

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And if you've got a rock, which 
is dominantly L4, I fell sparse 

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is called a siren, right? 
So, how did the rocks of these 

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Central complex has compared 
with those of the giant Dykes 

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once I was mostly interested in 
will sell one makeup right 

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across both of the sets of John,
dikes and was a very much more 

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granitic type of rock, be 
emptied. 

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Dikes are all made of gabbros 
very much richer, and magnesium 

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and calcium, and iron and the 
essential. 

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Lex is so much richer and 
potassium and sodium, and 

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aluminium and silicone. 
So I think they were probably 

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products of crossed all melting 
it with probably remelting of 

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the old batholith, they g x, 
which were the source of these 

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things. 
But we've never really been able

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to get a definitive answer on 
that. 

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You went back to study these 
rocks over 20 times over the 

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course of many decades. 
What made these rocks. 

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So special, They while 
remarkable for minerals 

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containing a whole variety of 
rare, metals are mentioned, 

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uranium zirconium under the 
elements that go with that like 

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niobium and hitch him. 
But also Elements which we know 

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now are extremely important in 
21st century technology whether 

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we're talking about mobile 
phones or wind generators but 

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quite a lot of PSI nights around
the world. 

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Do contain some exotic minerals 
containing rare elements. 

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Don't they Nothing nearly like 
some of those when we got our 

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problems and the one we were 
talking about specifically was 

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the Illinois outside complex, 
which again, cross Cuts these 

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John Dykes, I'm talking about, 
it's on the same Rift system, 

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the same linear system, but my 
feet are from the dikes and the 

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Illinois. 
Psyche itself is culminating all

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of that activity. 
It's finished about 1104 million

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years ago. 
And since then there's been 

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virtually never activity. 
Okay, so the intrusion that most

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attracted your attention was 
called the Illinois, music, 

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intrusion. 
How did it get all that's 

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exotic? 
Minerals and rare elements. 

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Is it basically a result of 
extreme magma fractionation in a

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magma chamber? 
Yes, I'm fractionation was 

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taking place. 
With unusual. 

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He's and Readiness because these
dark rocks. 

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Have quite High floor, you 
contents to them. 

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And fluorine is an element. 
That makes a huge amount of 

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difference to The Melting of 
igneous rocks. 

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First of all, if it's sad, the 
melting points are lower than if

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it's not. 
Secondly Glory moreover its I am

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fluoride is extremely 
efficacious in, breaking down, 

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complicated silicate structures 
and in so doing it. 

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Makes the mag mostly liquid, the
molten material very, very much 

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more fluid. 
It can flow very much more 

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greatly, not down to water or 
paraffin fluidity, but very much

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more than most natural long-term
Magma's because it was easy for 

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the English to move in. 
It, it means that again not 

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atoms, but ions can move quite 
long distances, unimpeded to 

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join up and form large crystals 
and Crystal fractionation 

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depends. 
Being able to remove crystals 

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are two ways of doing that. 
I've of the pistols are so dense

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that when they form that, they 
sink to the bottom of the magma.

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Chamber of that, they're in and 
leave of liquid above it 

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impoverished and that type. 
But the liquid above, it would 

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then be also enriched in those 
other materials that didn't make

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it into the crystals that sank. 
Yes, for alternatively. 

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On this applies particularly to 
Illinois. 

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Exact sum Elementals are of low 
density, can actually float. 

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So, they go to the top of the 
pot, I used to like them. 

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This still talking to students 
having a bucket or water and 

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putting sound of fragments of 
cork into it. 

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And of course, all the sound 
settles on the bottom, 10 

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o'clock. 
Floats to the top obviously, 

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depleted the water in between, 
of both the lights and the 

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heaviest. 
So, a process, very simply like 

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that is involved in Crystal 
Cove. 

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Formation. 
And with the fluoride ions, as I

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say, the molten rocks for 
Magma's are very, very much more

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fluid through the crystals can't
float, or see much more readily 

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than they can in most like most.
So, does that mean that? 

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Because of this extreme 
Mobility, that's conferred by 

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the presence of the fluorine and
the chlorine paps that you 

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essentially get much more 
extreme fractionation going on 

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crystal fractionation. 
Okay, Was all over the world, 

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all the time. 
But is simply is able to proceed

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more effectively, more, readily 
faster and better in these 

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foreign Rich rocks and those 
that are deficient in Florian. 

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So, part of the fractionation 
process, you've just described 

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involves some elements. 
Forming crystals, readily, While

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others do not and remain behind 
and become progressively. 

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More enriched, what determines 
whether an element remains 

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behind or is So called 
incompatible element 

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incompatible elements of those 
that just do not fit easily into

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Crystal structures. 
So they tend to get left out. 

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But again, left of the wall 
flowers, around the dance hall. 

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If they pay small elements or 
atoms, lithium and beryllium are

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very small and it's difficult 
for them to get taken into in 

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destructively tend to get 
leftover and concentrated them 

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late. 
Residuals of crystal. 

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Fractionation or if you're a 
very big fat around, you can't 

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get into any of these 
structures. 

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Your bust, so things like 
potassium barium, particularly 

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huge ones like uranium and 
thorium exclusion concentrated 

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in late stuff, and then some of 
them just have a pretty weird 

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bonding habits to put it that 
way and they get left out. 

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Gold will be one of those. 
Nobody wants it. 

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Sits on his head which is why 
you can go find native golden, 

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the rivers. 
You can't find most elements of 

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native elements that most of 
them combined. 

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00:13:02,900 --> 00:13:08,400
But some like gold Platinum 
Mercury just get left out this 

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Friday all called incompatible 
with I still want to do. 

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This is a big like human 
relationships. 

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You're too fat. 
You're too small or your just 

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awkward, you get left on. 
And so, the last rocks to form, 

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then the ones that are most 
enriched in Developments. 

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Do we have any idea as to what 
percent of the original magma? 

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Body that might have represented
a very, very, very small 

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percentage. 
You start off with a huge volume

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of slightly enriched material. 
You take away all of the other 

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minerals, which are not, those 
of the enrichment, and the more 

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you take out the more you 
concentrate. 

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And so, we must be talking about
a really large volume of 

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material. 
Would that originally have come 

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from the mantle, or from the 
deep crust, No, The Mantel 

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cross-boundary this comes from 
the mantle and we're talking 

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about processing of huge magma 
volumes which must be very many 

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cubic kilometers of magma down 
below. 

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Which are busy undergoing, 
Crystal fractionation, and then 

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the batches of the melts 
produced by just rise to the 

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surface and form. 
The things that we can see and 

228
00:14:18,100 --> 00:14:20,200
get out and collect from their 
lies. 

229
00:14:21,000 --> 00:14:25,800
So do you think that this mantle
source of an enriched magma that

230
00:14:25,800 --> 00:14:30,000
then wound up being fractionated
to less than 1% to form the 

231
00:14:30,000 --> 00:14:33,200
final rocks that we see in these
intrusive complexes doing. 

232
00:14:33,200 --> 00:14:38,000
That was already, then enriched 
in fluoride is And chlorine 

233
00:14:38,000 --> 00:14:43,000
ions, it was relatively 
impoverished in the mantle rocks

234
00:14:43,200 --> 00:14:47,800
depth and then it gets more and 
more concentrated as Crystal. 

235
00:14:47,800 --> 00:14:50,600
Fractionation process has 
proceeded. 

236
00:14:51,300 --> 00:14:54,200
Are there any theories as to why
some matter rocks? 

237
00:14:54,200 --> 00:14:58,100
Might at that time in the 
neoproterozoic 1.12? 

238
00:14:58,100 --> 00:15:01,500
1.2 billion years ago, have 
already been enriched in these 

239
00:15:01,500 --> 00:15:04,900
halogens. 
Why we got our problems in 

240
00:15:04,900 --> 00:15:10,300
particular was enriched. 
Is unknown, it's not just 

241
00:15:10,300 --> 00:15:13,100
fluorine. 
It's also Claudine and to a 

242
00:15:13,100 --> 00:15:18,300
lesser extent, its fellow 
elements bromine and iodine, but

243
00:15:18,300 --> 00:15:20,600
the ones are particular interest
of fluorine. 

244
00:15:20,800 --> 00:15:25,100
And then the next heaviest is 
for you in the other Malta as 

245
00:15:25,400 --> 00:15:29,200
crystallization of the sun. 
I just took place chlorine or 

246
00:15:29,200 --> 00:15:33,100
chloride ions became more and 
more concentrated and then 

247
00:15:33,100 --> 00:15:37,300
linked up with sodium and sodium
silicate perform a minute. 

248
00:15:37,600 --> 00:15:41,400
Which was a low density three 
could float and it was not 

249
00:15:41,400 --> 00:15:45,100
acting the cell fragments of 
cork in the sand and cork 

250
00:15:45,100 --> 00:15:47,800
experiment. 
And instead of going down is so 

251
00:15:47,800 --> 00:15:51,300
teed up to the roof of whatever 
chamber there was there. 

252
00:15:52,000 --> 00:15:56,000
And in the when I was a kid, got
one unit which is about 17 

253
00:15:56,000 --> 00:16:00,800
kilometers across, it's about 10
kilometers broad. 

254
00:16:00,800 --> 00:16:06,700
So that's 170 square kilometers.
And then the thing is about five

255
00:16:06,700 --> 00:16:10,000
or six. 
Five kilometers thick, so finish

256
00:16:10,000 --> 00:16:13,700
up with an extraordinary 
concentration of fluorine or 

257
00:16:13,700 --> 00:16:19,100
sodium chloride Etc which is 
totally unique across the globe.

258
00:16:19,100 --> 00:16:22,100
You mentioned that the God our 
Province contains several of 

259
00:16:22,100 --> 00:16:26,200
these elliptical intrusive 
complexes in addition to all the

260
00:16:26,200 --> 00:16:29,700
Exotic minerals that we're going
to talk a bit more about is ill,

261
00:16:29,700 --> 00:16:31,700
Emmaus, a call. 
So the place with the greatest 

262
00:16:31,700 --> 00:16:34,400
concentration of fluorine, 
another extraordinary 

263
00:16:34,400 --> 00:16:37,300
concentration, not very far away
for the place. 

264
00:16:37,400 --> 00:16:41,200
Hold it back towards, where the 
influence of my own Eleazar, 

265
00:16:41,200 --> 00:16:44,300
remarkable white mineral there 
and they used it. 

266
00:16:44,300 --> 00:16:48,300
I think for washing soda and 
various other things before it 

267
00:16:48,300 --> 00:16:51,500
was the sculpted. 
It was extremely useful in 

268
00:16:51,500 --> 00:16:55,500
extracting aluminium from 
aluminium or the rockhold 

269
00:16:55,500 --> 00:16:58,700
bauxite. 
And it's primarily, because 

270
00:16:59,000 --> 00:17:03,800
addition of fluoride to walks, I
lowers the melting temperature 

271
00:17:03,800 --> 00:17:07,300
greatly, so it's a hugely 
cheaper extraction. 

272
00:17:07,400 --> 00:17:10,200
Assess the amount of energy 
requires, much less. 

273
00:17:11,099 --> 00:17:14,700
And in that particular case, it 
also turns the Melt into an 

274
00:17:14,700 --> 00:17:18,800
electrolytic solution you can 
post an electrical circuit and 

275
00:17:18,800 --> 00:17:23,400
you can separate the aluminium 
at one of the electrodes and 

276
00:17:23,400 --> 00:17:27,700
that is still the worldwide 
method of separating of oxide 

277
00:17:28,500 --> 00:17:32,800
giving throat was known from 
suddenly the 19th century in the

278
00:17:32,808 --> 00:17:37,300
waves were using it and European
explorers found this stuff. 

279
00:17:37,400 --> 00:17:40,800
From the also felt aluminium 
process important. 

280
00:17:41,500 --> 00:17:46,500
It was mined for the best part 
of a hundred years, but during 

281
00:17:46,500 --> 00:17:50,600
World War 2, when aluminium was 
critically needed particularly 

282
00:17:50,700 --> 00:17:54,700
for aircraft production, 
something like 12 million tons 

283
00:17:54,900 --> 00:17:58,100
of Corona. 
Light was wind, from ich, totems

284
00:17:58,100 --> 00:18:00,900
sent to the United States for 
the war effort. 

285
00:18:01,800 --> 00:18:04,400
So, we've got this place called 
in ductility, which is 

286
00:18:04,400 --> 00:18:07,200
extraordinarily rich in 
fluorine. 

287
00:18:07,600 --> 00:18:11,000
The whole goddamn problems have 
got high Florian but it was 

288
00:18:11,000 --> 00:18:13,400
quite ridiculously highly 
concentrated. 

289
00:18:13,400 --> 00:18:17,800
Not just one fluoride mineral 
I've spoken of a highlight but 

290
00:18:18,100 --> 00:18:21,500
16 others. 
So got our problems have been 

291
00:18:21,500 --> 00:18:23,200
famous. 
If it was fighting each other 

292
00:18:23,200 --> 00:18:26,300
alone, but then we've got this 
other one I'm talking about him 

293
00:18:26,300 --> 00:18:29,200
outside and he comes back to the
question, why? 

294
00:18:29,200 --> 00:18:33,300
You get these super high 
concentrations of the simple, 

295
00:18:33,300 --> 00:18:37,300
haylage of elements, fluorine 
chlorine bromine and iodine. 

296
00:18:37,400 --> 00:18:41,800
You, okay, well, concentrated 
why we still don't have an 

297
00:18:41,800 --> 00:18:45,300
answer. 
So in those two regions in the 

298
00:18:45,300 --> 00:18:49,600
mouse Arc and evicted are there.
Lots of other exotic minerals 

299
00:18:49,600 --> 00:18:52,600
and other minerals that are only
known there or which it is that 

300
00:18:52,600 --> 00:18:56,400
type location where they were 
first discovered it a church 

301
00:18:56,400 --> 00:18:59,500
quite a lot of the floor eyes. 
There will be tossed about 

302
00:18:59,500 --> 00:19:03,800
globally unique. 
Both igneous rocks and son. 

303
00:19:03,800 --> 00:19:07,600
I sung, granite's. 
You would be lucky to find the 

304
00:19:07,600 --> 00:19:10,700
perhaps a dozen different 
minerals and Iraq. 

305
00:19:10,700 --> 00:19:15,800
In the uml Zack, you've got 220 
known different minerals. 

306
00:19:15,800 --> 00:19:18,400
So it's order of magnitude 
bigger. 

307
00:19:18,400 --> 00:19:23,900
It is a ridiculous. 
High concentration of extremely 

308
00:19:23,900 --> 00:19:28,000
exciting goodies. 
So, which is, why is a mouse 

309
00:19:28,000 --> 00:19:31,400
icon has become such a focus of 
international? 

310
00:19:31,900 --> 00:19:35,000
Interest. 
You could imagine every country 

311
00:19:35,000 --> 00:19:38,600
in the world with our 
technological basis is desperate

312
00:19:38,600 --> 00:19:43,200
to get at it. 
I'm would suspect very strongly,

313
00:19:43,200 --> 00:19:48,200
but Mr. Tongues Bid to Buy 
Greenland from Denmark was first

314
00:19:48,200 --> 00:19:50,500
and foremost concentrated on 
Illinois. 

315
00:19:50,500 --> 00:19:52,100
Mouse icon. 
One or two others. 

316
00:19:52,100 --> 00:19:55,300
In the got our problems. 
That's extraordinary though. 

317
00:19:55,300 --> 00:19:59,100
So the variety of minerals stay 
in a piece of cyanide that 

318
00:19:59,100 --> 00:20:01,700
you'll find in this complex and 
their mouths. 

319
00:20:01,800 --> 00:20:04,800
Complex is literally over about 
10 times. 

320
00:20:04,800 --> 00:20:08,600
The number that you would find 
in the next closest alkaline 

321
00:20:08,600 --> 00:20:11,300
intrusion or similar kind of 
plutonic Rock. 

322
00:20:11,800 --> 00:20:15,200
Yes, many of them were. 
Absolutely totally unique to 

323
00:20:15,200 --> 00:20:18,700
allows the mineral that they 
were most interested in before 

324
00:20:18,700 --> 00:20:21,300
uranium is, are an extraordinary
mineral? 

325
00:20:21,300 --> 00:20:25,600
Because it's basically a 
silicate is God silicon and 

326
00:20:25,600 --> 00:20:30,200
oxygen but it also doubles up by
being a phosphate and also it's 

327
00:20:30,200 --> 00:20:33,900
a silicone phosphate. 
Well, I've never ever heard of 

328
00:20:33,900 --> 00:20:38,000
any comparable mineral anywhere 
else from the steam stupid. 

329
00:20:38,400 --> 00:20:40,600
And it is, the students should 
be in the contains the 

330
00:20:40,600 --> 00:20:43,900
relatively High. 
Uranium, I want to come back to 

331
00:20:43,900 --> 00:20:47,300
the tectonics of the region and 
the history that we think must 

332
00:20:47,300 --> 00:20:49,600
have happened. 
So because you've got dikes and 

333
00:20:49,600 --> 00:20:52,800
you've got these intrusions, are
we talking about an inferred 

334
00:20:52,800 --> 00:20:57,600
region of Continental rifting. 
It was an area of Continental 

335
00:20:57,600 --> 00:21:00,700
rifting about eleven hundred 
million years ago. 

336
00:21:01,200 --> 00:21:02,000
It's right now. 
Arrow. 

337
00:21:02,000 --> 00:21:04,300
It's only about 15 kilometers 
across. 

338
00:21:04,400 --> 00:21:09,100
So, we're talking about rifting 
that was going on about 1.1, 1.2

339
00:21:09,100 --> 00:21:10,900
billion years ago. 
We're talking about a quarter of

340
00:21:10,900 --> 00:21:14,000
the age of the Earth. 
Can we use this extraordinary 

341
00:21:14,000 --> 00:21:18,100
glimpse into an ancient Rift 
Zone 2 and 50 anything about how

342
00:21:18,100 --> 00:21:20,200
the planet might have been 
different than or whether plate 

343
00:21:20,200 --> 00:21:24,500
tectonics was different. 
The plants are for about four 

344
00:21:24,500 --> 00:21:26,100
and a half thousand million 
years ago. 

345
00:21:26,100 --> 00:21:28,000
And there must have been 
extremely hot. 

346
00:21:29,200 --> 00:21:32,500
It's been using heat other since
its floozy, he At the present 

347
00:21:32,500 --> 00:21:36,200
time but very, very, very slowly
for the last few hundred million

348
00:21:36,200 --> 00:21:40,900
years, but a thousand million 
years, it was still really quite

349
00:21:40,900 --> 00:21:44,100
warm. 
And as I used to tell students 

350
00:21:44,100 --> 00:21:47,200
from the Precambrian, they just 
did things bigger and better 

351
00:21:47,300 --> 00:21:50,400
because they have more energy to
drive things around. 

352
00:21:50,800 --> 00:21:53,700
So we're back when the Earth was
not hot. 

353
00:21:53,700 --> 00:21:59,000
But a lot more Mount the thermal
loss through the crust was a lot

354
00:21:59,000 --> 00:22:03,600
more than it is the person time.
And did that contribute to the 

355
00:22:03,600 --> 00:22:08,000
extraordinary thickness of these
giant dikes and perhaps to the 

356
00:22:08,000 --> 00:22:10,800
extreme Mobility. 
Then of this magma body that led

357
00:22:10,800 --> 00:22:13,300
to this extreme fractionation 
and illa ma sack. 

358
00:22:14,200 --> 00:22:16,300
Definitely. 
If you start looking at modern 

359
00:22:16,300 --> 00:22:20,700
geology real say from about 700 
800 million years ago doesn't 

360
00:22:20,700 --> 00:22:22,300
sound very modern. 
But it is. 

361
00:22:22,700 --> 00:22:27,700
You're getting dikes formed all 
over the place, but I died like 

362
00:22:27,800 --> 00:22:30,700
20 meters across will be quite 
unusual. 

363
00:22:30,900 --> 00:22:35,400
Get dykes Approaching a 
kilometer on one is really very,

364
00:22:35,400 --> 00:22:38,300
very rare. 
Indeed, it was just more energy 

365
00:22:38,300 --> 00:22:42,700
available to pull things apart 
and do cause damage from the has

366
00:22:42,700 --> 00:22:45,000
been subsequently. 
One of the things you mentioned 

367
00:22:45,000 --> 00:22:48,100
when we spoke Ali was that these
igneous rocks of the Guard, our 

368
00:22:48,100 --> 00:22:52,500
period appear to be in quite 
pristine condition. 

369
00:22:53,100 --> 00:22:57,300
So, before reliable radiometric,
dating results became available,

370
00:22:57,600 --> 00:23:00,500
did you conclude therefore that 
the Rocks were relatively young 

371
00:23:00,500 --> 00:23:04,000
geologically speaking? 
And we are in such beautiful 

372
00:23:04,000 --> 00:23:07,400
pristine condition. 
First of all these must be 

373
00:23:07,600 --> 00:23:10,900
perhaps about has always the 
organic rocks from the west of 

374
00:23:10,900 --> 00:23:12,600
Scotland. 
And they have Aegean region 

375
00:23:12,600 --> 00:23:15,700
which are about 20 million years
or so old. 

376
00:23:15,700 --> 00:23:20,600
But certainly not Precambrian to
say it's a bit of continental 

377
00:23:20,600 --> 00:23:24,000
crust that the gods forgot 
about, they don't lift it alone.

378
00:23:24,000 --> 00:23:28,000
After the god or period. 
Some things did happen because 

379
00:23:28,000 --> 00:23:31,400
cream and split apart from 
Canada from Labrador. 

380
00:23:31,800 --> 00:23:35,300
Continental region. 
Containing the Gaga rocks was 

381
00:23:35,300 --> 00:23:38,200
elevated. 
Just very very, very gently and 

382
00:23:38,200 --> 00:23:42,100
slowly it was lifted up by 
magical hands from a few 

383
00:23:42,100 --> 00:23:45,700
kilometers down towards the 
surface and of course everything

384
00:23:45,700 --> 00:23:49,600
on the surface, continually 
being rubbed away continually 

385
00:23:49,600 --> 00:23:53,500
name, sandpaper by wind and 
Raymond ratio period has been 

386
00:23:53,500 --> 00:23:56,900
rubbed away. 
Very effectively by ice but even

387
00:23:56,900 --> 00:24:02,300
so we're talking about an area 
all over about 20000. 80's where

388
00:24:02,300 --> 00:24:06,100
these god-awful knocks outcrop 
and it's all been recently. 

389
00:24:06,100 --> 00:24:09,600
Scoured hangover laughs, a 
million meals were served in the

390
00:24:09,600 --> 00:24:13,300
ice ages, but it's been 
extremely gently treated. 

391
00:24:13,300 --> 00:24:17,400
It hasn't been folded, watery, 
fluid, so Pastor actually of 

392
00:24:17,400 --> 00:24:22,400
alteration and your minerals. 
So it is a very, very remarkable

393
00:24:22,500 --> 00:24:27,500
example of apostle continent and
I find that quite wonderful. 

394
00:24:27,800 --> 00:24:31,600
I want to end by asking you what
it was like to do feel. 

395
00:24:31,800 --> 00:24:34,400
Work in Greenland starting in 
the 1950s. 

396
00:24:34,400 --> 00:24:38,000
Well, before any of today's 
tourist infrastructure and 

397
00:24:38,000 --> 00:24:39,800
mobile phone service was in 
place. 

398
00:24:40,400 --> 00:24:42,600
Well, first of all green was a 
very big place. 

399
00:24:42,600 --> 00:24:45,700
It's about 2,000 kilometers from
top to bottom. 

400
00:24:45,700 --> 00:24:49,900
So if you cut it out on your own
Globe, tastier, say the North 

401
00:24:49,900 --> 00:24:53,600
End over Scotland or the tail 
end and probably somewhere over 

402
00:24:53,900 --> 00:24:57,900
Iraq or Persia to lot of it. 
It has some enormous Coastline 

403
00:24:58,000 --> 00:25:01,600
thousands and thousands of 
kilometers of co-lead coast. 

404
00:25:01,700 --> 00:25:03,600
This is not going to get 
overcrowded. 

405
00:25:04,200 --> 00:25:06,000
What was it? 
Like, Well, there must be 

406
00:25:06,000 --> 00:25:09,800
something wrong with me but I 
love empty places, unspoiled 

407
00:25:09,800 --> 00:25:13,200
battling places and those are 
still working there. 

408
00:25:13,200 --> 00:25:16,000
Your form very, very close 
friendships will break loose 

409
00:25:16,000 --> 00:25:19,500
bonding all sorts of mates which
last for decades. 

410
00:25:20,100 --> 00:25:23,400
I've worked all over the world 
but times I've spent in the 

411
00:25:23,400 --> 00:25:27,500
Arctic everywhere from Siberia 
to Canadian object. 

412
00:25:27,600 --> 00:25:30,100
I love the people. 
I meet are extremely interesting

413
00:25:30,100 --> 00:25:32,900
people very resilient They would
be living now. 

414
00:25:33,400 --> 00:25:36,200
People that don't know about 
hardships and can live very 

415
00:25:36,200 --> 00:25:38,600
simply. 
We had my radio in the 

416
00:25:38,600 --> 00:25:40,900
beginning. 
My mail I would be dumped by 

417
00:25:40,900 --> 00:25:45,500
those on the coast with a load 
of supplies and attend and we 

418
00:25:45,500 --> 00:25:48,100
would be told they'll be back in
the 70 weeks time. 

419
00:25:48,500 --> 00:25:51,900
You look after him and he looks 
after you. 

420
00:25:52,300 --> 00:25:56,400
So the buddy system is critical.
You need your mate on your mate,

421
00:25:56,400 --> 00:26:00,500
knees, you so things don't fall 
you don't fall off. 

422
00:26:01,700 --> 00:26:03,900
After yourselves the best years 
of my life. 

423
00:26:05,200 --> 00:26:07,100
Brian Upton. 
Thank you very much. 

424
00:26:07,300 --> 00:26:09,400
Enjoy talking to you Oliver 
many. 

425
00:26:09,400 --> 00:26:21,800
Thanks. 
For more about geology b, as 

426
00:26:21,800 --> 00:26:24,900
well as pictures and 
illustrations, that support this

427
00:26:24,900 --> 00:26:28,000
podcast, go to geology B.com.
