The first 200 lines.
Today, we are in the midst of a scientific revolution
in our understanding of the Earth
and our relationship to it.
Recently, scientists have begun to
think of the Earth in a new way -
almost as a living organism.
Like a living thing it is forever on the move,
driven by the restless energy
locked up in its interior.
And as the planet has evolved,
so has life,
shaped by the same forces
that move continents and change climates.
In Earth Story we shall explore this new vision
of a living planet
and the essence of this vision
is an understanding of time.
The most profound question
any scientist can ask about the earth
is also a simple one -
how old is it?
It's a question geologists have been striving
to answer for 200 years.
At the turn of the century
one such geologist came to a remote corner
of Southern Africa
called the Barberton Mountain Land.
His name was Alan Hall
and he had a commission from the South African government
to map this area looking for gold.
The Barberton Mountain Land
is several thousand square kilometers of rugged terrain,
cut through by rivers.
Rocky outcrops dot the hills,
signs of the bedrock hidden beneath the landscape.
Hall's aim was to criss-cross the region,
recording these outcrops,
and so build up a picture
of the rocks below the surface.
It was an immense task.
But as he worked his way across the landscape
Hall slowly realized that something was missing.
However hard he looked,
he could find in the rocks
none of the usual signs of fossilized life.
Could Barberton be a fragment of the Earth
from a time before life began?
Just how old was this place?
Hall's question came at a critical moment.
For a hundred years scientists had been arguing
about the age of the Earth
They were struggling to overcome ideas
which had held sway for centuries.
Ideas sanctioned by the full authority
of religious doctrine.
The book of Genesis relates how God created the earth
and everything in it, including ourselves,
in just 6 days.
The implication was that earth history and human history
had begun at the same moment
and this provided 17th century scholars
with a way to determine the age of the earth.
By simply adding up the ages
of Adam's descendants as listed in the Bible,
they concluded that the planet
must have been created in 4004 BC,
which meant it was less than 6,000 years old.
But it didn't look that way to geologists.
when they studied places like Barberton
they saw evidence that the landscape
had changed over time -
that it had a long history.
Hall's modern-day successor is Maarten de wit.
He too is fascinated
by the question of Barberton's antiquity.
I really got interested in this part
of the world many years ago,
but the opportunity to come here didn't arise
until much later.
At the end of the 70s
I came down here to Barberton
and it turned out to be one of the best moves of my life.
It's one of these areas
that has something extremely special
to tell about the story of the earth.
Maarten, like Hall before him,
has mapped the rocks of Barberton in detail.
when you do this,
a striking pattern quickly emerges.
well once you start mapping the hills here,
you'll notice that the landscape
is dominated by stripes -
stripes of rocks -
like that one there.
And if you get your eye in,
after a while you'll see, in fact, all these rock layers,
all are visible.
In this case this huge mass here
has finer vertical rock layers.
Everywhere in Barberton
the landscape seems to be made of layers.
By the nineteenth century,
geologists had begun to realize
that the process that created these layers
was still at work all around them.
Hall and his contemporaries knew that water
can be a powerful agent of change,
eroding rock, but also creating it... over time.
well take this river, for example,
like many rivers,
cutting through the rocks,
moving material downstream -
sand and silt -
and as it moves down
that material will deposit somewhere
in a quiet spot layer upon layer,
and as these layers get deposited on top of one another
they turn into rock slowly.
well here you have a slab of rock.
Now this slab represents a river bed.
There you can even see the sand grains.
These would have been the sand grains in the river.
These ridges that you see here,
they are ripples.
I can tell that it would have flowed
from my hand here downwards in that direction.
Now you can see if you look downwards
that in fact there are several of these
slabs stacked on top of one another.
Here's one,
there you see another one over here,
and another one,
and another one still, and more.
These are dozens of slabs
and they're all tilted right now,
but originally they would have been horizontal
and they represent all history of rivers.
A long history of deposition.
To nineteenth-century scientists
a world made up of layers
didn't look as if it had been created
all in one go as the Bible says.
It must have been built up overtime.
But how much time?
The first person to realise
the profound importance of this question
was a Scotsman, James Mutton.
At Siccar Point on the east coast of Scotland
exposed in the cliff side
there's a small patch of rock
which made a deep impression on Hunt.
Chris Nicholas is a geologist
who has made a special study of his work.
So here we are at one of the most
famous geological localities in the world.
This is Hutton's Unconformity
and what Hutton noticed here
in this cliff
is that at the bottom of the cliff you have these
vertical strata,
overlain by horizontal strata
and between the two
there was an undulating erosional surface.
And what Hutton recognised
was that well if all rocks
were deposited horizontally on the sea-bed,
what on earth was this grey rock doing being vertical
at the base of the cliff there was something wrong here.
And he started to look at rocks in more detail
and he came up with this idea
that what must have happened
is that the grey rock must have been twisted and turned
so that it was vertical,
uplifted out of the sea,
eroded off and then drowned again,
so that the red rock could be deposited on top.
And more than that, it was then uplifted again
to form the cliff we now see.
So there were at least 2 cycles of deposition,
uplift and then erosion
that he could see in this cliff.
And he went on to say "well, these cycles must have taken
an immense amount of time to complete"
because when he looked around him and saw rivers
and the sea eroding today
it doesn't really erode very quickly.
And also he said "well how many cycles
could have taken place before these
and how many will come after this,
we just don't know".
And it led him on to this idea
of the immensity
of geological time
and he came out with a very famous quote of,
well, he could see no vestige
of a beginning and no prospect of an end.
For Hutton the earth was infinitely old.
Siccar Point represents the discovery of geological time
and it's shaped the way
that geologists think and work ever since.
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