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If he had been standing on this very spot in 1969, this is what you | :00:15. | :00:19. | |
would have seen, great fiery Fountains of lock-up reaching up | :00:19. | :00:25. | |
into the sky. Today, we discovered the incredible power of volcanoes | :00:25. | :00:29. | |
and the influence they have over our planet. This is volcano Live | :00:29. | :00:39. | |
:00:39. | :01:11. | ||
Look at this incredible landscape. Good morning from Hawaii. Where | :01:11. | :01:18. | |
broadcasting live from the Big Island. It is a place simply here | :01:18. | :01:23. | |
because although the volcanoes that created it. Yesterday, we came to | :01:23. | :01:28. | |
you live from the summit of this volcano, Kilauea, and it is the | :01:28. | :01:34. | |
most active volcano in the world. Look at this crater, known as | :01:34. | :01:38. | |
Halem'uma'u. You can see a great plume of gas coming from that | :01:38. | :01:43. | |
greater. Beneath it is a lake of lava. You cannot appreciate its | :01:43. | :01:47. | |
power or its beauty in daylight but at night, it is completely | :01:47. | :01:52. | |
different. This is a time-lapse photographs taken from Albeniz | :01:52. | :01:59. | |
crabbed researcher, Tom, showing not just the glory of the lake, but | :01:59. | :02:02. | |
look at the Milky Way. You can see the pulses of magma | :02:02. | :02:07. | |
coming out, fantastic. This landscape is so apocalyptic but it | :02:07. | :02:12. | |
used to be lush rainforest until May 1969 when that eruption | :02:12. | :02:16. | |
happened. The magma that fed that started beneath the lake of lava, | :02:16. | :02:21. | |
and some of it came along tunnels underground, along the rift zone, | :02:21. | :02:28. | |
and burst out there, producing that crater. It covered this area in 17 | :02:28. | :02:35. | |
cubic miles of lava. It is enough to cover Oxford. Or Cambridge, and | :02:35. | :02:38. | |
we like to be democratic. Tonight we will be looking at the | :02:38. | :02:42. | |
destructive power of volcanoes, but also the surprising role that they | :02:42. | :02:47. | |
have to play in creating new land and your life. Here is what is | :02:47. | :02:54. | |
coming up. -- new life. Tonight at visit an Icelandic town which | :02:54. | :02:59. | |
fought back against a volcano and one. | :02:59. | :03:04. | |
In Chile, a group of volcanologists hike through the landscape, turned | :03:04. | :03:07. | |
white and closely by an extraordinary ongoing eruption. | :03:07. | :03:12. | |
Ed Byrne gets his rocks off in the lab. | :03:12. | :03:15. | |
And in or why's rainforest, I discovered a unique ecosystem that | :03:15. | :03:25. | |
:03:25. | :03:27. | ||
could not exist without the volcano. -- and here in Hawaii's rainforest. | :03:27. | :03:35. | |
We are standing in an area of the Kilauea volcano, and it is not an | :03:35. | :03:43. | |
easy landscape to navigate. I will do my best to meet Don Swanson, in | :03:43. | :03:46. | |
research -- researcher from the Hawaiian volcano observatory on the | :03:46. | :03:53. | |
Big Island. You had the privilege, I think, of being here in 1969 when | :03:53. | :03:56. | |
the eruption went off, but before you tell us about that, can you | :03:56. | :04:02. | |
give us an idea of what this landscape was like before? This | :04:02. | :04:06. | |
landscape was smooth and forested with only a few bare areas from | :04:06. | :04:13. | |
previous eruptions. It was vastly different from this. And in 1969, | :04:13. | :04:17. | |
what happened? What did the scientists notice was going on? | :04:17. | :04:21. | |
noticed that earthquakes were beginning so we rushed down here | :04:21. | :04:27. | |
just after the eruption had started. There were fountains in the air, 20 | :04:27. | :04:34. | |
of 30 metres high. We have some dramatic pictures. Later on, the | :04:34. | :04:39. | |
Fountains of higher than that, as the summer progressed. -- Fountains | :04:39. | :04:45. | |
got higher. By the end of the year, it was completely mature. I think | :04:45. | :04:49. | |
that is the thing that we do not appreciate. You think of an | :04:49. | :04:52. | |
eruption being something that happens and then ends quite quickly. | :04:52. | :04:57. | |
You're saying it went on for months. It lasted for four years with a | :04:57. | :05:04. | |
little recess in between. The most exciting time was during the first | :05:04. | :05:12. | |
nine months when it had the highest Fountains. Four geologists -- for a | :05:12. | :05:14. | |
geologist to witness something like this must be incredibly important | :05:14. | :05:23. | |
and exciting. It is, both exciting and important. We have a chance to | :05:23. | :05:29. | |
see repeatedly fountains being erupted and various things that we | :05:29. | :05:32. | |
do not normally get a chance to see. This was a very stimulating | :05:32. | :05:37. | |
eruption frost. I cannot believe that not only did you have the | :05:37. | :05:40. | |
presence of mind to rush down and study what was going on but you | :05:40. | :05:45. | |
brought your camera. We have some lovely photographs taken. This one | :05:45. | :05:53. | |
gives us a sense of the scale of those fountains. That is about as | :05:53. | :05:59. | |
tall as the Empire State Building. We had Fountains even taller. They | :05:59. | :06:03. | |
start slowly, build up and play for several hours and then they just go | :06:03. | :06:10. | |
off. It is like someone has just turned the tap off. I love this one | :06:10. | :06:17. | |
because it shows you again the tremendous scale, and puts us in a | :06:17. | :06:23. | |
period of time, with the '60s cars. That was the observatory's car. A | :06:23. | :06:27. | |
few minutes after right at that photograph, it was the only car | :06:27. | :06:31. | |
left. And then there was a high fountain, continuing, and the | :06:31. | :06:38. | |
fountain material was blown to the car. The car needed a new paint job. | :06:38. | :06:42. | |
The more spectacular sight from that time, if I could call it a | :06:42. | :06:50. | |
waterfall, a lava fall, is perhaps a better description. I think that | :06:50. | :06:56. | |
is the most spectacular sight I have ever seen. It is bigger than | :06:56. | :07:01. | |
Niagara Falls, would you believe it? It fell into the crater for | :07:01. | :07:07. | |
several hours before the crater was almost full. Absolutely beautiful. | :07:07. | :07:12. | |
I'm going to take advantage of unify May, because we have been | :07:12. | :07:17. | |
having questions sent in by our viewers. One was sent in from mini- | :07:17. | :07:21. | |
me, and she wanted to know how close you get to love but because | :07:22. | :07:31. | |
your face melts. -- close to lava. Another viewer wants to know what | :07:31. | :07:36. | |
would happen to your hand if you touched Malton lava. Well, you can | :07:36. | :07:40. | |
get pretty close if there is only a little bit. You can use your arm or | :07:40. | :07:44. | |
your jacket as a shield, and you can touch it if you're wearing | :07:44. | :07:49. | |
gloves but not for very long. With a big fountain, there is so much | :07:49. | :07:54. | |
heat coming off that you have to stand back quite a long way. Or you | :07:54. | :08:00. | |
would get burned. We went out to the lava field just out there which | :08:00. | :08:02. | |
you will see it in tomorrow's programme and the heat is just | :08:02. | :08:07. | |
extraordinary. I felt like my face might melt if I got closer. When it | :08:07. | :08:12. | |
gets that hot, you want to get out. Thank you very much for your time. | :08:12. | :08:16. | |
We will be joining Don later in the programme. We have been in Hawaii | :08:16. | :08:22. | |
for about a week, preparing for the series. One of the first things we | :08:22. | :08:28. | |
wanted to do was go out and explore these extraordinary surroundings. | :08:28. | :08:35. | |
We set off down the chain of craters road. On all sides, it was | :08:35. | :08:39. | |
lush, green rainforest, but then the vegetation started thinning out, | :08:39. | :08:46. | |
and it was like being on a completely different planet. It is | :08:46. | :08:54. | |
like an ocean of lava. That is extraordinary. It almost looks like, | :08:54. | :08:57. | |
and he will make me feel like I am from the great British a cough, it | :08:58. | :09:07. | |
:09:08. | :09:12. | ||
looks like a well-cooked a Brownie. -- Bake-off. That is as far as the | :09:12. | :09:21. | |
eye can see. I have never seen anything on this scale. And then | :09:21. | :09:30. | |
there was a final surprise. Does it go right across the road? I just on | :09:30. | :09:36. | |
the road would bend around but it has completely stopped. Shelvey get | :09:36. | :09:44. | |
out? Yes. -- shall we get out. That is great, that is the end of the | :09:44. | :09:51. | |
road absolutely. Quite literally. One of the things we're doing this | :09:51. | :09:55. | |
week in our volcanic control hobbit is keeping a track on the eruptive | :09:55. | :09:58. | |
activity around the world. The Smithsonian are sending us daily | :09:58. | :10:02. | |
updates on what has been happening and we had a map showing those | :10:02. | :10:09. | |
volcanoes that have an alert going on. These are active volcanoes, | :10:09. | :10:14. | |
typically to between 20 and 30 a day. They are spread around the | :10:14. | :10:21. | |
whole planet. Yesterday we told you about a volcano in Guatemala a, | :10:21. | :10:27. | |
called Fuego, that was erupting, but we have had the latest news | :10:27. | :10:32. | |
from the Smithsonian, that this volcano, Santa Maria, has also been | :10:32. | :10:37. | |
showing signs of erupting, and apparently triggering avalanches. I | :10:37. | :10:43. | |
think we have some footage. It is one of these special satellite | :10:43. | :10:49. | |
images. It is his saddle a light that travels around the planet and | :10:49. | :10:54. | |
images at night time, picking out hot spots, fires or volcanoes. This | :10:54. | :10:59. | |
is Santa Maria, and here is the volcano. This is a thermal hot spot, | :10:59. | :11:03. | |
where magma is getting close enough to the surface to be seen from | :11:03. | :11:09. | |
space. I expect that as it comes up, the volcano was becoming unstable. | :11:09. | :11:16. | |
There is a small town near that volcano, and I have actually been | :11:16. | :11:20. | |
there, it is rather beautiful. Quite a small population, just | :11:20. | :11:25. | |
200,000 people. Do we know what sort of alert has been put on the | :11:25. | :11:29. | |
volcano? There is no evacuation. These things happen all the time | :11:30. | :11:34. | |
and sometimes they go to nothing. There is another one causing | :11:34. | :11:39. | |
concern in Japan. You know this volcano quite well. I went there | :11:39. | :11:42. | |
are few years ago and it is a volcano on an island with | :11:43. | :11:48. | |
communities immediately below it. Across the bay, there is a big town. | :11:48. | :11:57. | |
If we go to the webcam, the other day the plumes were a 1000 feet. -- | :11:57. | :12:00. | |
8000 feet. It is still active but it has not accelerated or | :12:00. | :12:07. | |
intensified. With an eruption like that, can it go in ate and flows? | :12:07. | :12:14. | |
Can you get huge plumes and then it comes down? -- ebbs and flows. | :12:14. | :12:18. | |
will see this repeated over the next few days. They are really | :12:18. | :12:22. | |
unpredictable, volcanoes. It could go to nothing or it could become a | :12:22. | :12:27. | |
big eruption. You can keep an eye on all of the active volcanoes on | :12:27. | :12:37. | |
:12:37. | :12:39. | ||
our map, many of them have webcams. Access them on our website: Also, | :12:39. | :12:44. | |
send your questions in. We will be asking a few more of | :12:44. | :12:50. | |
those later. Now, we have seen how lava can transform the landscape. | :12:50. | :12:56. | |
But so can volcanic ash. In June of last year, a volcano called Puyehue | :12:56. | :13:02. | |
started erupting. Earlier this year, with that eruption still ongoing, | :13:02. | :13:06. | |
Hugh Tuffen from Lancaster University joined an expedition to | :13:06. | :13:16. | |
:13:16. | :13:33. | ||
go and see the eruption for himself. I wanted to be a vulcanologist | :13:34. | :13:37. | |
because I love mountains and a love the idea that mountains can be | :13:37. | :13:40. | |
alive, they are not just static and in the background, they are | :13:40. | :13:45. | |
actually almost living things, changing the scenery in front of us. | :13:45. | :13:54. | |
My specialism is rile lytic magma. It is this kiss and rich in cellar | :13:54. | :13:58. | |
Cup. We almost never watch eruptions like this taking place. | :13:58. | :14:01. | |
They are very rare and there have only ever been two worldwide in my | :14:01. | :14:09. | |
lifetime. In June of last year, a volcano called Puyehue erupted for | :14:09. | :14:14. | |
the first time in 50 years. The plume was 40 kilometres in altitude, | :14:14. | :14:18. | |
disrupting flights in the southern hemisphere for some time. By the | :14:18. | :14:25. | |
following January, it had calmed down. I had to get out there. It | :14:25. | :14:29. | |
was an epic journey to get there, as the volcano is in a remote | :14:29. | :14:39. | |
:14:39. | :14:42. | ||
location. Five -- 500 miles south of the capital. | :14:42. | :14:49. | |
The rainforest are normally green and lush, and full hummingbirds, it | :14:49. | :14:54. | |
is beautiful. But we found it to be desolate and quiet, stifled and | :14:54. | :15:02. | |
covered in ash. Do what up was tough, continuous | :15:02. | :15:09. | |
uphill, carrying 25 kilograms. -- the walk up. John Castro and Ian | :15:09. | :15:15. | |
Skipper joined me. John is an expert in this type of volcano. | :15:15. | :15:22. | |
to Sheikh! Tell me about it. Ian is an expert on vent processes. We are | :15:22. | :15:30. | |
two-thirds of the way up. We are hearing persistent rumblings. | :15:30. | :15:34. | |
booming sound got louder and louder but we still could not see anything | :15:34. | :15:38. | |
through the trees. But there was one point when there was a clearing | :15:38. | :15:41. | |
and suddenly we could see this billowing ash rising up from the | :15:41. | :15:51. | |
:15:51. | :15:56. | ||
My hairs stood on end. I was look, Duff, Duff, Duff. It's fantastic. | :15:57. | :16:00. | |
We had to find somewhere to camp. We needed water and far enough from | :16:00. | :16:05. | |
the vents that we were out of range of any of the large blocks of lava | :16:05. | :16:13. | |
that were being blasted out. Being so close to the vent felt | :16:13. | :16:17. | |
exhilarating. It's just incredibly exciting to see the vent on one of | :16:17. | :16:20. | |
the volcanoes that we've been studying for so many years. It's | :16:20. | :16:30. | |
:16:30. | :16:30. | ||
live right in front of us. Wow. Textbook. One of the unsolved | :16:31. | :16:36. | |
mysteries of rhyolites is how the gas escapes. There has to be some | :16:36. | :16:41. | |
way of how the gas gets out. It seems as though they were valves | :16:41. | :16:45. | |
through which gas and ash was able to escape very rapidly, but then | :16:45. | :16:48. | |
these were blocking up and then a new valve was opening up right next | :16:49. | :16:55. | |
to it. Wow, look. It's just cleared itself there. This really helped us | :16:55. | :17:02. | |
to think about the way that gas is able to escape from this very thick | :17:02. | :17:08. | |
rhyolitic magma. It gradually got darker and darker and as it did so, | :17:08. | :17:18. | |
:17:18. | :17:18. | ||
the vents came to life. I then realised that I had a switch on the | :17:18. | :17:23. | |
camera, which meant we could go to watch in infrared light and we | :17:23. | :17:27. | |
could suddenly see bombs of lava that were being ejected on the long, | :17:27. | :17:32. | |
lazy paths before they landed on the ground. It was a beautiful | :17:32. | :17:36. | |
thing to watch, but also very useful as we can then work out how | :17:36. | :17:42. | |
fast the bombs are moving and this all links in to how the gas is able | :17:42. | :17:47. | |
to escape from the magma at the vent. It's very exciting for us | :17:47. | :17:52. | |
indeed, because we are rhyolite experts and we've been studying it | :17:52. | :18:00. | |
for years. To actually see all the secrets being revealed by Puyehue | :18:00. | :18:10. | |
:18:10. | :18:12. | ||
was quite something. Great tough from hue. We'll be joining him | :18:12. | :18:16. | |
again for the other part of his expedition later in the programme. | :18:16. | :18:20. | |
What struck me about that eruption, was it was turning a landscape | :18:20. | :18:25. | |
white and yet, you think of col vanic eruptions turning land black, | :18:25. | :18:31. | |
so why was that? -- volcanic ejupgss turning the land black, so | :18:31. | :18:41. | |
:18:41. | :18:42. | ||
where -- eruptions turning the land black, so why is that? There is | :18:42. | :18:46. | |
hardly any silicone, so that's why they are grey and black, but | :18:46. | :18:55. | |
although there is no change in chemistry, threw -- there is a | :18:55. | :19:05. | |
:19:05. | :19:06. | ||
change in texture. This is a smooth, polished. Pahoehoe is very runy and | :19:07. | :19:10. | |
it flows and then it kind of freezes and cools quickly, so it | :19:10. | :19:16. | |
has the glaze on top of it. Often, the other magma, you can see, it | :19:16. | :19:18. | |
flows underneath, but on the surface you get a feeling of the | :19:18. | :19:22. | |
motion and flow that goes on. This would have been seeping up out of | :19:22. | :19:27. | |
the ground as we saw in some of the footage yesterday? That's the red | :19:27. | :19:32. | |
rivers of lava. It would run quite quickly and almost be like a sort | :19:32. | :19:37. | |
of treacle or something? Yeah. Creeping across. Look just next | :19:37. | :19:41. | |
door to this. Same chemistry and similarly erupted from just over | :19:42. | :19:48. | |
there and look at it. It is rubble here. This stuff is from a much | :19:48. | :19:52. | |
more slow-moving lava. It's stickier and so when it cools it | :19:52. | :19:57. | |
starts to cool and slow down. does it get sticky, why from the | :19:57. | :20:01. | |
same col vain know? Temperature. When it's lower it get stickier and | :20:01. | :20:05. | |
it's harder to move. Think of oil. The point is, this is horrible to | :20:05. | :20:13. | |
walk on and you'll lacerate yourself and the people called this | :20:13. | :20:18. | |
A'a, and they tell me this is because it hurts when you stand on | :20:18. | :20:24. | |
it. As we have seen, volcanoes can cause devastation not just on land, | :20:24. | :20:28. | |
but unfortunately on human populations as well. Since records | :20:28. | :20:32. | |
began, it's believed that about 250,000 people have lost their | :20:32. | :20:36. | |
lives as a result of volcanoes. In disaster movies, it's often this | :20:36. | :20:42. | |
stuff, the lava, that is seen as the culprit, but how accurate is | :20:42. | :20:52. | |
:20:52. | :20:56. | ||
that? Ed Byrne discovers. classic 1997 disaster movie, | :20:56. | :21:06. | |
:21:06. | :21:07. | ||
volcano. It's got Tommy Lee Jones in it. A volcano has gone off in LA | :21:07. | :21:12. | |
and lava is incinerating all in its path. How much of this is science | :21:13. | :21:19. | |
fact and how much Hollywood fiction? Dr Alison is one of the | :21:20. | :21:24. | |
country's leading experts. She wants to explode some lava myths. | :21:24. | :21:29. | |
Alison, this was once lava and presumably if you heat it up hot | :21:29. | :21:33. | |
enough it can be lava again? Probably have to heat it to 1100 | :21:33. | :21:41. | |
degrees or so. I see a torch here. Can we do that? Yes, we can. Don't | :21:41. | :21:49. | |
try this at home, kids. Wow. It's pretty quick. You can see the gas | :21:49. | :21:53. | |
bubbles are growing. Yes. It melted really quickly, but it flows very, | :21:53. | :22:00. | |
very slowly, doesn't it? Yeah. have to be pretty low-moving to get | :22:00. | :22:06. | |
killed by a lava flow? You can generally outrun one. That's quite | :22:06. | :22:13. | |
cool. I just made lava. You did. Pretty sweet! What about these | :22:13. | :22:19. | |
things? Lava bombs? How dangerous are they in the real world? Lava | :22:19. | :22:26. | |
bombs form in explosive eruptions. Lava flows are when the advice kus | :22:26. | :22:34. | |
fluid comes out and pours out the top and -- viscous fluid comes out | :22:34. | :22:37. | |
and pours out and bombs are relatively big pieces. The bombs, | :22:37. | :22:42. | |
when they come out of the vent, often they go on a trajectory like | :22:42. | :22:48. | |
a Canon ball. This one is like one and surprisingly light for a rock. | :22:48. | :22:52. | |
There are a lot of bubbles in there, so they are gases that are driving | :22:52. | :23:00. | |
the eruptions. This is what they look like in real life. How far | :23:00. | :23:05. | |
from a volcano do they generally fly? It depends on how explosive | :23:05. | :23:09. | |
the eruption is, but generally, no more than a kilometre or something | :23:09. | :23:15. | |
like that. What is the major killer then from a volcano? The main | :23:15. | :23:24. | |
killers during eruptions and shortly after are pyroclastic flows. | :23:24. | :23:29. | |
They go further away from the volcano than a bomb would go. | :23:29. | :23:34. | |
an explosive volcano erupts it throws enormous columns of hot ash | :23:34. | :23:38. | |
particles and gases into the atmosphere. Gravity can cause an | :23:38. | :23:43. | |
ash column to collapse and when it does it can turn into what is known | :23:43. | :23:47. | |
as a pyroclastic flow. These can travel dozens of miles, moving at | :23:47. | :23:52. | |
hundreds of miles an hour, at temperatures of up to 1,000 C and | :23:52. | :23:56. | |
they destroy everything in their path and since 1600 more than | :23:56. | :24:02. | |
40,000 people have been killed by such flows. More than any other | :24:02. | :24:08. | |
immediate volcanic hazard. Alison, explain to me how this tank can be | :24:08. | :24:13. | |
used to recreate the flow? As you can probably tell, there is water | :24:13. | :24:16. | |
in here. We are going to pretend this water is actually the | :24:16. | :24:21. | |
atmosphere. This will be gas and we'll make our pyroclastic flow in | :24:21. | :24:26. | |
here. This will be the volcanic ash and we'll be simulating an ash | :24:26. | :24:33. | |
column above a volcano that becomes unstable and collapses. Then when I | :24:33. | :24:41. | |
open this gate that's the volcano collapsing. Exactly. Here it goes. | :24:41. | :24:46. | |
Typically in a volcano it's going downhill and it might hit a flat | :24:46. | :24:50. | |
area, but because it's gravity driving it, it wants to go down, so | :24:50. | :24:56. | |
it tends to stay in valleys and goes downhill. The flows can travel | :24:56. | :25:06. | |
:25:06. | :25:09. | ||
over land, over hills and even over water. When crack toia erupted, the | :25:09. | :25:14. | |
flows killed throws of people across the sea. How could this have | :25:14. | :25:18. | |
happened? Not even the scientists are sure, but Alison has a theory. | :25:18. | :25:26. | |
We have got some ash heated to 600 degrees Celsius. We are going to | :25:26. | :25:33. | |
pour it into the water and you can see the ash bouncing off. That's | :25:33. | :25:37. | |
because we are having a little steam explosion. This all becomes | :25:37. | :25:42. | |
clear when filmed with a high-speed camera. As the superhot ash hits | :25:42. | :25:47. | |
the water the steam throws the ash back up into the air. Could this be | :25:47. | :25:53. | |
what happened in Indonesia? steam explosions are adding energy | :25:53. | :25:57. | |
and pressure and it's like a bit of a cushion and reduces the friction | :25:57. | :26:03. | |
at the base and also keeping that ash in the pyroclastic flows that | :26:03. | :26:06. | |
are sinking. That's why it just goes so much further over water | :26:06. | :26:14. | |
then? That's part of the reason. There's another idea and that is | :26:14. | :26:19. | |
that pummice has a lot of bubbles and it floats and you often get | :26:19. | :26:23. | |
rafts on the sea and it might be that the flows are also making use | :26:23. | :26:26. | |
of that raft to help them travel. Skimming on the rafts as well? | :26:26. | :26:36. | |
:26:36. | :26:38. | ||
Right. The fit many brings home it's not the flows, but the | :26:38. | :26:43. | |
pyroclastic flows that kill. Later this week I'll really investigate | :26:43. | :26:49. | |
those more carefully when I go to Vesuvius in Italy. We have looked | :26:49. | :26:54. | |
at flows and lava and ash, but something that you may not think is | :26:54. | :26:58. | |
a volcanic distructive force is mud. But, believe me, it can be. If you | :26:58. | :27:03. | |
have an ash eruption, followed by heavy rainfall or the ash mixes | :27:03. | :27:09. | |
with melted ice, you can get mud and that can often change into | :27:09. | :27:17. | |
mudflows known as lahas. That happened in 1985 in Colombia. It's | :27:17. | :27:24. | |
a volcano called Nevado Del Ruiz. These scenes are shocking to this | :27:24. | :27:32. | |
day. It caused the death of 23,000 people. It was the deadliest | :27:32. | :27:36. | |
volcanic eruption in south American history. Why was it, Iain, or why | :27:36. | :27:41. | |
did it, I suppose, cause such a great loss of life? I think there | :27:41. | :27:48. | |
was no monitoring. This mudflow started way up the valley. People | :27:48. | :27:51. | |
could have had 30 minutes' warning if there had been an instrument | :27:51. | :27:54. | |
telling them there was a flow on the way and people could have found | :27:54. | :28:00. | |
high ground or something. One of the ironies of these disasters is | :28:00. | :28:04. | |
they kickstart changes in technology and practice that make | :28:04. | :28:07. | |
us forecast and study them much better. It's a sad testiment, but | :28:07. | :28:13. | |
it's true. What is interesting is just it week, though, Nevado Del | :28:13. | :28:18. | |
Ruiz has restarted again and if we can go to see where it is. It's | :28:18. | :28:21. | |
just over here. If we have a look at the footage that has just come | :28:21. | :28:27. | |
back in the last week from the webcams there, you can see plume | :28:27. | :28:32. | |
activity and ash cloud coming out of the crater. Here it is in the | :28:32. | :28:36. | |
background. This is the modern town there. What is really interesting - | :28:37. | :28:40. | |
there, it's a much more active scene. That's one that we will be | :28:40. | :28:46. | |
keeping an eye open on. Do we think that - are they starting an | :28:46. | :28:51. | |
evacuation? Is there a class of warnings as far as they are | :28:51. | :28:56. | |
concerned? They've raised the warn to 11-2, which means it's likely in | :28:56. | :29:02. | |
days or weeks and evacuation has started. Even if it's as bad as | :29:03. | :29:06. | |
1985 the death toll won't be as near. That is a testiment as to how | :29:06. | :29:11. | |
far we have come in 30 years. can keep an eye on the webcams of | :29:11. | :29:21. | |
:29:21. | :29:22. | ||
that and all the activity ones by going to the website: It seems they | :29:22. | :29:27. | |
are our ultimate adversities and there's nothing we can do to stop | :29:27. | :29:30. | |
them erupting, but there's an amazing story, which I discovered | :29:30. | :29:34. | |
in Iceland of a community that fought against a volcano to stop | :29:34. | :29:44. | |
:29:44. | :29:44. | ||
what seemed to be an inevitable Five miles off the southern coast | :29:44. | :29:52. | |
of Iceland lies a small volcanic island. This is Heimaey and the | :29:52. | :29:55. | |
approach to the harbour is protected by looming cliffs of | :29:55. | :29:59. | |
black rock, a clue to events which rocked this place to its | :29:59. | :30:09. | |
:30:09. | :30:28. | ||
At 2am on the morning of January 23rd, 1973, a fissure in my long | :30:28. | :30:34. | |
opened up and split this part of the island in two. -- a mile long. | :30:34. | :30:41. | |
Today, the evidence of the eruption is easy to find. This was the stuff | :30:41. | :30:46. | |
that was coming out of that volcano. It is actually a sort of ash, but | :30:46. | :30:53. | |
it is more like gravel. It was literally raining down. Of course, | :30:53. | :30:58. | |
it was not in her stuff like this, it was that about 1000 degrees | :30:58. | :31:05. | |
Celsius. -- inert. So to be here when that happened | :31:05. | :31:14. | |
must have felt like being in a living hell. To the 5000 | :31:14. | :31:20. | |
inhabitants of this tiny island, it felt like the end. The volcano | :31:20. | :31:24. | |
threatens to engulf everything, and although it was a heart-wrenching | :31:24. | :31:31. | |
decision, they knew immediately that they had to leave. It was pure | :31:31. | :31:36. | |
luck that the night the volcano erupted, the harbour was full of | :31:36. | :31:40. | |
fishing boats. On a normal night, all of the men and all of the boats | :31:40. | :31:43. | |
would have been out to sea. But there had been a huge storm the | :31:43. | :31:50. | |
night before or, that had kept men and boats at home. When the volcano | :31:50. | :31:54. | |
erupted, suddenly there was a means of escape from what must have | :31:54. | :32:02. | |
seemed at the time an inescapable fate. | :32:02. | :32:05. | |
During the first night of the eruption, almost the entire | :32:05. | :32:14. | |
population was evacuated by boat to the mainland. 100 or so people, | :32:14. | :32:19. | |
mostly young men, stayed behind to try and save as many homes as they | :32:19. | :32:28. | |
could. At first, they concentrated on Clearing ash, hoping to stop | :32:28. | :32:35. | |
roofs collapsing. But the ash kept falling and many houses were soon | :32:35. | :32:45. | |
:32:45. | :32:46. | ||
completely buried. Just this single chimney now emerges where a whole | :32:46. | :32:51. | |
community once thrived. Worse was to come, as a huge laugh off low | :32:51. | :32:56. | |
advance towards the town, consuming everything in its path. -- lava | :32:56. | :33:03. | |
flow. And when the lava finally reached the coast, but began to | :33:03. | :33:12. | |
threaten the most valuable part of the island. -- it began to threaten. | :33:12. | :33:18. | |
The harbour entrance was just a few hundred metres wide. As lava added | :33:18. | :33:21. | |
new vans to the coast, there was the chance that the gap might be | :33:22. | :33:29. | |
closed forever. For those who had stayed behind, | :33:29. | :33:33. | |
like this local welder, that was the moment when the real fightback | :33:33. | :33:40. | |
began. TRANSLATION: We knew we had to save the harbour because our | :33:40. | :33:44. | |
livelihood depends on our ability to be able to sail out to sea. If | :33:44. | :33:48. | |
we're going to live here, we have to be able to fish. Our way of life | :33:48. | :33:53. | |
would not last long without the fishing industry, that is how it is. | :33:53. | :33:58. | |
It seemed unthinkable that anything could be done, but one | :33:58. | :34:05. | |
volcanologists have an idea. -- one a vulcanologist had an idea. | :34:05. | :34:10. | |
Several years earlier, he had seen how a lava flow near the coast had | :34:10. | :34:14. | |
changed direction when it came into contact with sea water. He wondered | :34:14. | :34:19. | |
if the same thing can be achieved deliberately this time in Nevado | :34:19. | :34:24. | |
Del Ruiz. -- in Heimaey. whispered to work welding pipes. As | :34:24. | :34:29. | |
soon as we began spraying sea water on the lava, it starts and to | :34:29. | :34:34. | |
harden. We noticed that the laughter was losing ground and | :34:34. | :34:38. | |
actually being diverted. -- the lava. Everyone was saying, it is | :34:38. | :34:48. | |
:34:48. | :34:49. | ||
working, spray more, spray more! The team worked around the clock. A | :34:49. | :34:53. | |
huge network of pipes was put together, and extra pumps were | :34:53. | :35:03. | |
:35:03. | :35:03. | ||
shipped in to get water right into the heart of the lava flow. | :35:03. | :35:11. | |
TRANSLATION: An unbelievable amount of sea water was sprayed onto the | :35:11. | :35:21. | |
:35:21. | :35:22. | ||
lava to stop the advance. Huge amounts. Constantly. I had a no | :35:22. | :35:27. | |
idea how much, but it would be fun to know. | :35:27. | :35:34. | |
Incredibly, cooled by the water, a huge barrier of solidified lava was | :35:34. | :35:39. | |
built up alongside the harbour. This new wall of rock stopped the | :35:39. | :35:46. | |
lava flow 200 metre short of the cliffs on the far side. Today, the | :35:46. | :35:52. | |
gap remains and access to the harbour has been preserved. | :35:52. | :35:57. | |
By standing up to the volcano, the people of Heimaey had maintained | :35:57. | :36:01. | |
their livelihood and to this day, they continued to harvest the rich | :36:01. | :36:07. | |
fishing grounds of the northern Atlantic. | :36:07. | :36:14. | |
It must have been a really fantastic feeling, that somehow, | :36:14. | :36:19. | |
against all odds, you were doing it. TRANSLATION: A volcano was not | :36:19. | :36:22. | |
exactly an ordinary type of adversity, not a tall, so it was | :36:22. | :36:26. | |
amazing to see the plan actually working. It is incredible that we | :36:26. | :36:31. | |
were able to stop the lava and save our town and are -- and a harbour. | :36:31. | :36:38. | |
It was miraculous. It just worked. In 1973, the people of Heimaey had | :36:38. | :36:42. | |
the audacity to stand up to the worst that nature could throw at | :36:42. | :36:47. | |
them. It was an amazing display of resilience. For Iceland, it was a | :36:47. | :36:51. | |
rare victory for the people in their long battle against the | :36:51. | :36:57. | |
volcanoes in their midst. Iceland's Prime Minister told me that it was | :36:57. | :37:00. | |
5000 years since the last volcano here and perhaps it will be another | :37:00. | :37:05. | |
5000 years until the next. As he put it, the people of Iceland live | :37:05. | :37:15. | |
:37:15. | :37:18. | ||
with fire beneath their feet. An incredible story. Perhaps just | :37:18. | :37:22. | |
as incredible is the fact that 20% of the world's population live | :37:22. | :37:30. | |
within 100 kilometres of a volcano. This is bigger island, and we are | :37:30. | :37:35. | |
just down chain of craters road. That is the greater were we were | :37:35. | :37:41. | |
last night, the Halem'uma'u crater. And this is the volcano that | :37:41. | :37:49. | |
everyone has turned their attention to, the biggest volcano and the | :37:49. | :37:58. | |
world. The lava flows, in 1984, flowed down the side here towards | :37:58. | :38:04. | |
the main town on Big Island, Hilo. When this blows, it throws out an | :38:05. | :38:11. | |
enormous amount of lava. It pours down the mountainside, as you can | :38:11. | :38:20. | |
see. In that last eruption, the lava. Within four miles off Hilo. | :38:20. | :38:25. | |
It is a fairly terrifying fact. It could happen and it is already | :38:25. | :38:28. | |
happening down here. There are lava flowers that have taken over a | :38:28. | :38:35. | |
Little Town that Ian and I will visit tomorrow. It is called | :38:35. | :38:39. | |
Kalapana. The population here have got their eyes on that. I believe | :38:39. | :38:47. | |
Ian is out on the lava and we will be interviewing gone Swanson again. | :38:47. | :38:52. | |
-- Don Swanson. Water was the safe here in Iceland, but here, it is | :38:52. | :39:02. | |
different? -- was the saviour. Water can cause expose of eruptions. | :39:02. | :39:06. | |
It heats up and forms steam and the steam power as the explosions. | :39:06. | :39:11. | |
Talking of explosions, this is the fissure that erupted in. 1969. This | :39:11. | :39:21. | |
is. The fountain here was not very large but during the course of the | :39:21. | :39:27. | |
summer, it became very high. Extraordinary. Why is it that | :39:27. | :39:31. | |
volcanoes switch from a gentle, if you sit tight, too explosive? | :39:31. | :39:40. | |
seems as if the summit region has to come maps -- has to collapse so | :39:40. | :39:43. | |
water can get into the plumbing system. Once that happens, you | :39:43. | :39:50. | |
generate steam explosions. Kilauea has a Dr Jekyll And Mr Hyde | :39:50. | :39:57. | |
personality. It is by Bola! It can switch from lava flows to expose of | :39:57. | :40:07. | |
:40:07. | :40:11. | ||
eruptions. -- by Polar. explosive cannot get? -- can it get. | :40:11. | :40:16. | |
We have had six eruptions in the last 1200 years sending ash well up | :40:16. | :40:22. | |
into the jet stream, 10, 15 kilometres high. And in the tropics, | :40:22. | :40:26. | |
that allows it to move around. is the problem with aircraft | :40:26. | :40:32. | |
Catholic. -- aircraft traffic. It can be really dangerous. This | :40:32. | :40:38. | |
landscape is incredible. These are trees! These are trees. The lava | :40:38. | :40:42. | |
flowed around the tree and it was cooled by the tree. Then the level | :40:42. | :40:47. | |
of the lava dropped, and this became an island. It shows you the | :40:47. | :40:54. | |
personality of what we're looking at. We are exploring that in Chile | :40:54. | :41:02. | |
a different way. The first day was all about | :41:02. | :41:09. | |
watching events and the plumes. The second day, we wanted to get in and | :41:09. | :41:14. | |
watch the lava flow itself. This was an obsidian lava flow. It is | :41:14. | :41:21. | |
volcanic glass. This is solidified magma, which has not formed any | :41:21. | :41:29. | |
crystals. It was quite a slog to get there, | :41:29. | :41:36. | |
going up a bridge and downer Bridge, and eventually we came over a slope. | :41:36. | :41:46. | |
:41:46. | :41:46. | ||
-- down a ridge. Eventually we saw a spectacular lava flow. | :41:46. | :41:49. | |
But was the first time in our lives that we had ever seen and obsidian | :41:49. | :41:59. | |
:41:59. | :42:00. | ||
flow, a rhyolitic lover flow in action. -- a lava flow. That is the | :42:01. | :42:04. | |
lava float there, the material flowing out from the base of the | :42:04. | :42:08. | |
volcano. This was as far from a river of red lava as you can get, | :42:09. | :42:14. | |
it was like a glacier of creaking lava, groaning, almost | :42:14. | :42:24. | |
:42:24. | :42:25. | ||
imperceptibly moving. One to his unique is that we are | :42:25. | :42:29. | |
seeing the explosive phase and the effusive phase, which is still | :42:29. | :42:34. | |
evidence -- which is still active. Rhyolitic eruptions have always | :42:34. | :42:39. | |
been couched in terms of a full serve -- explosive or effusive, so | :42:39. | :42:44. | |
easily -- either it is producing pumice or lava. Both are happening | :42:44. | :42:47. | |
at the same time so what we're watching here is new evidence that | :42:47. | :42:51. | |
is telling us something detail about how these volcanoes work. | :42:51. | :42:58. | |
John went down to the edge of the lava flow. John is collecting some | :42:58. | :43:02. | |
samples of obsidian. I hope to see him running away from their pretty | :43:02. | :43:12. | |
:43:12. | :43:28. | ||
fast. Move! Definitely some hard one samples. | :43:28. | :43:34. | |
The that samples is a nice resource for us, that we can use to study in | :43:34. | :43:41. | |
more detail how the love for deforms and how it loses gas. -- | :43:41. | :43:45. | |
how the lava reforms. We are running out of food and water. We | :43:45. | :43:52. | |
decided to go back down to the ballet. As we walked down through | :43:52. | :44:00. | |
the forest, it was so quiet again. Eventually, when we got down to the | :44:00. | :44:04. | |
valley itself, everything seemed brilliantly colourful after the | :44:04. | :44:13. | |
black and white landscape that we had come from. | :44:13. | :44:18. | |
We went down to a beautiful lake at the foot of the volcano. Many of | :44:18. | :44:24. | |
the lakes around the volcano have floating rafts of pumice. It is | :44:24. | :44:29. | |
such a light rock as it is full of bubbles. There are huge slicks of | :44:29. | :44:37. | |
pumice floating on the surface. It is a beautiful thing to witness. | :44:37. | :44:40. | |
When you come down from the summit, there is no better way to get | :44:40. | :44:47. | |
cleaned up than to go for a little swim in the exfoliating pumice raft. | :44:47. | :44:51. | |
It was one of the most exciting trips I have ever been on. It was a | :44:51. | :44:55. | |
practical challenge, tyrant, and really exciting as well. We felt a | :44:55. | :45:00. | |
little bit on the edge sometimes, just through being so close to the | :45:00. | :45:06. | |
events. For me, being able to watch these processes that I had been | :45:06. | :45:10. | |
studying for years, that was really a special thing that I will | :45:10. | :45:20. | |
:45:20. | :45:24. | ||
You can see why he thinks that. This is obsidian. Beautiful. This | :45:24. | :45:33. | |
is glass. Absolutely. Have a look at this. That is the pumice. You | :45:33. | :45:37. | |
can see all the gas bubbles. things from the same col vain know | :45:37. | :45:42. | |
and totally different formations. There's a lot of silicone and that | :45:42. | :45:46. | |
blasts out. You are taking glass into your lungs. Good for your feet | :45:46. | :45:50. | |
though. Time for our viewers' questions. We have this crackers. | :45:50. | :45:54. | |
One of the topics that has come up tomb and again is yellowstone, when | :45:54. | :46:00. | |
is it going to blow? Big question. This is the supervolcano in America | :46:00. | :46:05. | |
and we are going to be dealing with that on Thursday, so we'll hold off | :46:05. | :46:09. | |
there. Tune in then. The other thing, our favourite fact of | :46:09. | :46:13. | |
yesterday's programme was to tell you that the volcano was not only | :46:14. | :46:18. | |
the biggest in the world, but the second biggest in the Solar System, | :46:18. | :46:28. | |
but everyone wants to know what is the biggest? It's the one on Mars. | :46:28. | :46:34. | |
Mr Judd and her year-nines in Malden in Essex, they want to know | :46:34. | :46:41. | |
will there be an eruption in England? An interesting one. No. | :46:41. | :46:45. | |
There was activity in Britain about 50 million years ago, but we have | :46:45. | :46:55. | |
shifted our position. The source is under Iceland now. I'm pretty sure. | :46:55. | :46:59. | |
John Hunter in Workington in Cumbria, he wants to know, does | :46:59. | :47:04. | |
lava contain precious metals? does. The hot fluid has lots of | :47:04. | :47:08. | |
precious metals that gets blown out in the plumes. There is a lot of | :47:08. | :47:12. | |
metals coming out. On Mount Etna, this is my favourite fact, every | :47:12. | :47:18. | |
year 700 grammes of gold gets ejected. You will be out there with | :47:18. | :47:23. | |
your little bag. It's not that much, given how much stuff comes out, | :47:23. | :47:27. | |
it's not worth going out with your panning basket. Paul Hill in Ealing, | :47:27. | :47:33. | |
he wants to know, how far down is the deepest magma chamber? That's | :47:33. | :47:38. | |
quite hard to tell, because often they have different chambers, | :47:38. | :47:43. | |
there's a lower and they climb up to shallows, but tens of miles down. | :47:43. | :47:53. | |
:47:53. | :47:53. | ||
Did you not say it's about a mile under this Halem'uma'u one here? | :47:53. | :48:02. | |
Typically. Keep your questions coming. It may surprise you that | :48:03. | :48:07. | |
volcanoes can be created as well as distructive. They build new land | :48:07. | :48:12. | |
and with that comes new life and the national park here, where we | :48:12. | :48:17. | |
are, is a World Heritage Site not for the volcanoes, but | :48:17. | :48:20. | |
extraordinary biodiversity. A lot of you have been in touch saying | :48:20. | :48:26. | |
you want to see the flora and fauna, and you are in luck and so were we, | :48:26. | :48:32. | |
because last week an ejock gist, who works here found and -- ecol | :48:32. | :48:36. | |
gist who works here phoned and said there is a plant that flowers once | :48:36. | :48:43. | |
in the 25-year lifespan and then it dies. And there's one, in fact more | :48:43. | :48:53. | |
:48:53. | :48:54. | ||
than one, in bloom right this minute and we had to go and see it. | :48:54. | :49:00. | |
It's beautiful. You are on the volcano at 6600 feet elevation and | :49:00. | :49:03. | |
where I'm taking you is a really special place and I think you'll | :49:03. | :49:13. | |
:49:13. | :49:18. | ||
enjoy it. Look. These are the flowers. They are the silver shards. | :49:18. | :49:21. | |
I don't think I've ever seen anything like it. You don't always | :49:21. | :49:26. | |
see them flowering. If you had come last year there would have been no | :49:26. | :49:31. | |
flowering plants. It's the most beautiful thing. I agree. And the | :49:31. | :49:41. | |
:49:41. | :49:41. | ||
scent. Yes. There's a very heavy smell of honey. They live to be | :49:41. | :49:48. | |
maybe 20 or 30 years. How rare is it? Very rare. We only know of | :49:48. | :49:51. | |
three natural populations remaining in the world. All are on this | :49:51. | :49:59. | |
mountain and the largest population is only 700 individuals. This | :49:59. | :50:09. | |
:50:09. | :50:10. | ||
amazing plant is totally indemic to this volcano? Yes Yes. There are | :50:10. | :50:13. | |
others found on other mountains on the different islands. This is | :50:13. | :50:21. | |
specific to here. That's extraordinary. It was so unusual, | :50:21. | :50:24. | |
but we as a crew were actually in the right spot at the right time. | :50:24. | :50:29. | |
How many times have you said, "You should have been here last week."? | :50:29. | :50:34. | |
Spot on. What a great surprise and treat it was seeing that. It's | :50:34. | :50:39. | |
lovely. That sentiment that volcanoes are places where life can | :50:39. | :50:44. | |
flourish to such exotic things is really important. It's easy to | :50:44. | :50:48. | |
forget through all the images of spewing lava. I went out to see the | :50:48. | :50:58. | |
good side of volcanoes the other day. Walking through the black lava | :50:58. | :51:01. | |
fields it's hard to imagine that volcanoes are capable of anything | :51:01. | :51:06. | |
other than total destruction. Around 150 years ago this beautiful | :51:06. | :51:09. | |
bay used to stretch all the way around here. Those trees over there, | :51:09. | :51:15. | |
they were on the shoreline and beside it was a thriving little | :51:15. | :51:20. | |
fishing village. In 1859 this happened. A huge lava flow flowed | :51:20. | :51:25. | |
from the biggest volcano and it for through the trees and destroyed the | :51:25. | :51:28. | |
fishing village and filled in half the bay as it spilled out into the | :51:28. | :51:37. | |
sea. Although the eruption was devastating, the lava created new | :51:37. | :51:41. | |
land and added almost two square miles to the shoreline, providing a | :51:41. | :51:46. | |
new habitat for life. And it's not just here. All over the island, | :51:46. | :51:55. | |
volcanoes are building land. They built the wol island and every | :51:55. | :52:00. | |
other island in the entire chain. - - whole island and every other | :52:00. | :52:04. | |
island in the entire chain. Now there's a whole string of island | :52:04. | :52:08. | |
paradises. All of them built by volcanoes. Blanketed in forest and | :52:08. | :52:13. | |
bathed in sunlight, the islands have become a haven for life, | :52:13. | :52:22. | |
teaming with -- teeming with unineat species. -- unique species. | :52:22. | :52:26. | |
This looks really rich. It is. The amazing thing about this forest is | :52:26. | :52:30. | |
virtually everything we are seeing is found nowhere else in the world, | :52:30. | :52:38. | |
only in Hawaii. This is a healthy forest, so in terms of plants, | :52:38. | :52:45. | |
there's over 2,000 species found only here. I can hear some birds. | :52:45. | :52:52. | |
The chattering is the Nectar- feeding bird and it has a curved | :52:52. | :52:57. | |
bill to fit into the flowers, so there's an incredible pairing of | :52:57. | :53:06. | |
the plants and birds here. important is volume cannism here? | :53:06. | :53:11. | |
It's fundamental. It's founded by the volcano. They create the | :53:11. | :53:21. | |
islands and they are in the ocean. It's the arena for all the | :53:21. | :53:25. | |
evolution and adaptation to happen. Even the rain, because obviously it | :53:25. | :53:30. | |
falls on this speck of land. Without that we wouldn't have the | :53:30. | :53:40. | |
amazing rain forests, that's for sure. Even in this forest, you are | :53:40. | :53:47. | |
never far from the devastation. The sun's out. It comes and goes. | :53:47. | :53:51. | |
that's it. The forest is there and now this. We are into the lava. | :53:51. | :53:57. | |
These flows come from an eruption in 1974. The cracks ripped open | :53:57. | :54:01. | |
through the earth. It's incredible, that abrupt line between lush | :54:01. | :54:09. | |
forest and suddenly, wham, black lava. It may look desolate, but | :54:09. | :54:15. | |
life has found a way to thrive again. This is the native tree, | :54:15. | :54:20. | |
found nowhere else in the world. They are adapted to grow out of | :54:20. | :54:25. | |
here. What is it rooting into then? There's no soil and in many cases | :54:25. | :54:28. | |
they don't even need to be in a crack, as you would expect. They | :54:28. | :54:33. | |
can be just stuck to the side of a rock, with the roots goes over the | :54:33. | :54:41. | |
top. Many think volcanoes are fertile, but it's hard for plants | :54:41. | :54:45. | |
to get at the nutrients? Yes. Lava has all the minerals a plant could | :54:45. | :54:50. | |
ever want, but they are locked into the lava. As near as we can figure, | :54:50. | :54:53. | |
this tree is surviving completely off of what little nutrients there | :54:53. | :55:00. | |
is in rainwater. It's a symbol of resilience? Absolutely. As the | :55:00. | :55:04. | |
volcanoes age and become inactive the raw materials we are seeing | :55:04. | :55:08. | |
here will begin to erode and be weathered away and it will | :55:08. | :55:12. | |
contribute to the rich col vainic soils we always here about. -- hear | :55:12. | :55:17. | |
about. In a few decades, the trees will have transformed the land back | :55:17. | :55:25. | |
into lush forest. In a few thousand years the mineral-rich lava will be | :55:25. | :55:29. | |
broken down into soil that will support countless more plant | :55:29. | :55:34. | |
species. They do a lot more than provide new trepbts for plants to | :55:34. | :55:40. | |
grow, because without -- new Trents for plants to grow, because without | :55:40. | :55:48. | |
them there wouldn't be any plants at all. Here at the summit there's | :55:49. | :55:54. | |
barely a plant to be seen, but it's what's in the air that's important. | :55:54. | :56:04. | |
:56:04. | :56:04. | ||
That huge cloud is mostly water vapour. Also sulphur dioxide and | :56:04. | :56:10. | |
Co2, which is crucial for plants because it allows them to process | :56:10. | :56:17. | |
the sun and store it as energy. When our planet first formed 4.5 | :56:17. | :56:23. | |
billion years ago it was volcanic activity that put Co2 into the | :56:23. | :56:28. | |
atmosphere, so without it plants would never have evolved. We tend | :56:28. | :56:34. | |
to think of Co2 as a greenhouse gas, keeping the planet warm. Too much | :56:35. | :56:38. | |
and it can make the planet dangerously warm, but too little is | :56:38. | :56:43. | |
also dangerous too. If there was none in the atmosphere then heat | :56:43. | :56:49. | |
would just leak out into space. If there was no greenhouse gases at | :56:49. | :56:54. |