Investigates the hidden forces that drive the planet's largest and most…
Geologic Journey II - The Collision Zone: Asia
- Description
- Reviews
- Citation
- Cataloging
- Transcript
Welcome to the Collision Zone -- the fiery unpredictability of Indonesia's volcanoes at one end, the massive Himalayas at the other and millions of years of tectonic tension in between.
The collision zone of the old world is about to be the hub of the new. India, the Himalayas and the island arc of Indonesia will form the centre of the world's next supercontinent.
As the story unfolds we discover a tale of where the Earth has been and what the Earth shall be: a whole new world that we'll barely recognize.
96-page Teacher Resource Guide, written by practicing educators, provides a wealth of activities, lesson plans and curriculum outcomes to assist in integrating the video into the classroom.
'Watching [The Collision Zone: Asia] is like going on a field trip with a group of experts to the Himalaya and other areas, but doing so in less than an hour, rather than the weeks it would take to do so in person. The film nicely connects the evolution of the geology over many millions of years to the here and now of natural hazards and the environment. The emphasis on the relationship between the geology and people living there makes this a more special journey.' Dr. Roland Burgmann, Chair and Professor, Department of Earth and Planetary Science, University of California-Berkeley
'The photography is breathtaking and the science content is accurate...get ready to be amazed.' Coralee Smith, NSTA Recommends
'The science is excellent and current, the storyline is engaging, and the cinematography is nothing short of breathtaking. Although I have taught this material for years, there was information in the video new to me and archive footage that I had never seen before. [Along the African Rift] vividly illustrates the dramatic processes of continental rifting and the birth of new oceans...[The Pacific Rim: Americas] explores in spectacular fashion the destructive forces of plate tectonics.' Dr. Damian Nance, Professor of Geological Sciences, Ohio University, Editor, GSA Today
'The Western Pacific Rim and The Pacific Rim: Americas are excellent for civics and history classes. Throughout history, individuals and society have lived with natural hazards to garner natural resources. The modern construct of plate tectonics rationally explains the occurrence of earthquakes, tsunamis, and volcanoes on the Pacific Rim along with mineral and agricultural bounty, access to the ocean, and picturesque scenery. The interviews in the series clearly illustrate how informed people address this trade-off. Both titles in the series can spark excellent discussion about the hazards and benefits of living along active plate boundaries.' Dr. Norman Sleep, Professor of Geophysics, Stanford University, Author, Principles of Geophysics
'Blends the latest geologic findings with captivating cinematography, bringing the viewer on a worldwide tour of the tectonic forces that mold the surface of our planet...A heart-stopping adventure especially ideal for classroom viewing, or high school and public library DVD collections. Highly recommended.' The Midwest Book Review
'Exceptional...What makes this series especially compelling and of interdisciplinary interests are the discussions of the local cultures and mythologies that have developed based on historic and recent geologic activities, along with the adaptations the local peoples have made to changes in their environment. This stunning series is a valuable addition to any college, high school or public library.' Barbara Gage, Prince George's Community College, Science Books and Films
Citation
Main credits
Suzuki, David T. (narrator)
Gregg, Andrew (film director)
Gregg, Andrew (film producer)
Gregg, Andrew (screenwriter)
Other credits
Director of photography, Ed Middleton; editor, Geoff Matheson; original music, Ken Myhr.
Distributor subjects
Anthropology; Asian Studies; Earth Science; Environment; Geography; Geology; History; Oceans and Coasts; Plate Tectonics; Science, Technology, Society; SociologyKeywords
00:00:08.840 --> 00:00:15.760
A high altitude world of great
and fragile mountains, where
00:00:15.760 --> 00:00:19.830
people live on the edge of
change in awe and fear of a
00:00:19.830 --> 00:00:22.255
landscape that could
come crashing down.
00:00:26.910 --> 00:00:30.300
For centuries, cultures have
lived and worshiped with the
00:00:30.300 --> 00:00:36.860
tremors beneath their feet,
tremors that tear apart the
00:00:36.860 --> 00:00:42.000
Himalayas, while rivers wash
the debris away across a
00:00:42.000 --> 00:00:45.970
plate, through the densest
population in the world, into
00:00:45.970 --> 00:00:48.130
an ocean and out of the
mouths of volcanoes.
00:00:56.450 --> 00:00:59.430
While cities grow and scientists
try to predict the
00:00:59.430 --> 00:01:09.050
timing of the next big event
in the collision zone.
00:01:36.240 --> 00:01:38.070
I've always wanted to
see the Himalayas.
00:01:38.070 --> 00:01:39.850
I've always wanted to
see the geology.
00:01:39.850 --> 00:01:41.660
I've lectured about it.
00:01:41.660 --> 00:01:44.690
I've written textbooks that
include sections on the
00:01:44.690 --> 00:01:46.980
Himalayan geology.
00:01:46.980 --> 00:01:49.820
But by coming here to the
Himalayas, you just
00:01:49.820 --> 00:01:51.165
have to say, wow.
00:01:56.690 --> 00:02:01.000
Canadian geologist Nick Eyles is
getting in a little R&R in
00:02:01.000 --> 00:02:03.185
the middle of his tectonic
tour of the planet.
00:02:06.850 --> 00:02:10.639
As he cruises along outside of
Kathmandu in Nepal, he's
00:02:10.639 --> 00:02:14.070
considering what he's going to
see up there in the mountains
00:02:14.070 --> 00:02:15.870
where the earth works
as a machine.
00:02:20.670 --> 00:02:24.700
A machine kickstarted by a
continental collision after
00:02:24.700 --> 00:02:26.900
the last supercontinent
broke apart.
00:02:29.410 --> 00:02:32.770
It's one of the greatest
stories in our history.
00:02:32.770 --> 00:02:35.720
55 million years ago is an
important marker in Earth's
00:02:35.720 --> 00:02:39.590
history because that marks the
end of the Tethys Ocean.
00:02:39.590 --> 00:02:42.350
India began its long migration
northwards,
00:02:42.350 --> 00:02:44.860
collides with Asia finally.
00:02:44.860 --> 00:02:47.530
And that's the extinction
of an ocean.
00:02:47.530 --> 00:02:50.000
And those oceanic sediments,
with all their included
00:02:50.000 --> 00:02:56.250
fossils, became caught
in a huge vice.
00:02:56.250 --> 00:02:59.230
And they've been uplifted 2
millimeters a year over 55
00:02:59.230 --> 00:03:00.820
million years.
00:03:00.820 --> 00:03:04.580
And they're now eight kilometers
above sea level.
00:03:04.580 --> 00:03:07.480
It's hard to imagine that
something as formidable as the
00:03:07.480 --> 00:03:11.550
Himalayan mountain range
could be so delicate.
00:03:11.550 --> 00:03:13.840
They are coming down as
fast as they went up.
00:03:13.840 --> 00:03:17.950
They're impermanent features
of the planet.
00:03:17.950 --> 00:03:20.640
So for all the size of the
Himalayas, they're the biggest
00:03:20.640 --> 00:03:24.070
features on the planet, they
are still ephemeral.
00:03:24.070 --> 00:03:26.950
They're being torn
down by gravity.
00:03:26.950 --> 00:03:30.260
And enormous fluxes of sediment
are being driven out
00:03:30.260 --> 00:03:31.710
into the oceans.
00:03:31.710 --> 00:03:35.440
Nick is going to investigate
that and what eroding
00:03:35.440 --> 00:03:38.150
mountains mean to the people
who live among them.
00:03:44.060 --> 00:03:46.850
Then he's going to follow the
sediment stream as it gets
00:03:46.850 --> 00:03:50.220
flushed out of the mountains and
down throughout India, out
00:03:50.220 --> 00:03:53.510
to the Indian Ocean and down
to Indonesia, where it gets
00:03:53.510 --> 00:03:56.800
recycled into new land
by volcanoes.
00:03:56.800 --> 00:03:59.770
New lands that will turn
into the world's next
00:03:59.770 --> 00:04:01.020
supercontinent.
00:04:08.730 --> 00:04:12.920
Nick is joining a donkey train
in the Nepali territory of
00:04:12.920 --> 00:04:16.490
Mustang, where the evidence of
the collision is everywhere.
00:04:16.490 --> 00:04:18.120
It's a wonderful thing to see.
00:04:18.120 --> 00:04:21.092
So we're going to lots of
fossils which were flourishing
00:04:21.092 --> 00:04:22.610
in this long-dead ocean.
00:04:22.610 --> 00:04:27.120
Nick's companion is Professor
B.P. Upreti Professor Upreti
00:04:27.120 --> 00:04:30.170
knows how to see this land
as a place in constant
00:04:30.170 --> 00:04:31.290
transition.
00:04:31.290 --> 00:04:35.196
What are now mountains
was once ocean floor.
00:04:35.196 --> 00:04:37.800
So to build these high
mountains, we've had to
00:04:37.800 --> 00:04:39.200
destroy an ocean.
00:04:39.200 --> 00:04:43.280
And rocks that were once below
sea level are now up to 8,000
00:04:43.280 --> 00:04:44.330
meters above sea level.
00:04:44.330 --> 00:04:47.590
And that's true that in all
these sediments that were
00:04:47.590 --> 00:04:50.350
deposited in the ocean bottom,
they have been uplifted.
00:04:50.350 --> 00:04:53.160
They're squeezed up
and then they have
00:04:53.160 --> 00:04:54.850
come up to this height.
00:04:59.700 --> 00:05:02.410
The root to the heart
of Mustang is the
00:05:02.410 --> 00:05:03.660
Kali Gandaki Gorge.
00:05:10.070 --> 00:05:13.510
For a thousand years, traders
and nomads have traveled
00:05:13.510 --> 00:05:15.790
through here, past
the twisted rock
00:05:15.790 --> 00:05:17.715
faces, gnarled by tectonics.
00:05:26.220 --> 00:05:29.570
It's a land of serene beauty,
but it's also prone to
00:05:29.570 --> 00:05:30.820
earthquakes and landslides.
00:05:35.740 --> 00:05:38.930
At one time, these were
flat-lying sediments sitting
00:05:38.930 --> 00:05:42.050
quietly underwater.
00:05:42.050 --> 00:05:43.030
Now look at them.
00:05:43.030 --> 00:05:45.680
It's a great example of crustal
shortening, isn't it,
00:05:45.680 --> 00:05:48.700
where you take rain rocks and
you fold them and you create
00:05:48.700 --> 00:05:50.380
this high topography?
00:05:50.380 --> 00:05:51.640
Yeah.
00:05:51.640 --> 00:05:53.010
It's the same way.
00:05:53.010 --> 00:05:55.830
These rocks were deposited in
the bottom of the ocean when
00:05:55.830 --> 00:05:57.860
they were laid horizontally.
00:05:57.860 --> 00:06:01.890
And then when they collided,
the rocks at the base here,
00:06:01.890 --> 00:06:05.020
then they started buckling
up and then they folded.
00:06:05.020 --> 00:06:09.320
And now we have these
mountains formed.
00:06:09.320 --> 00:06:12.350
From here you can see the trails
of the glaciers carving
00:06:12.350 --> 00:06:13.600
out the Himalayas.
00:06:17.210 --> 00:06:19.990
Down closer, you can see
how glaciers work as
00:06:19.990 --> 00:06:21.240
massive earth movers.
00:06:33.660 --> 00:06:36.240
That is the Khumbu Icefall
down there.
00:06:36.240 --> 00:06:39.650
As the glaciers have receded,
they have carried boulders and
00:06:39.650 --> 00:06:43.640
gravels and dumped them here,
onto a field of ice that works
00:06:43.640 --> 00:06:45.320
as a giant conveyor belt.
00:06:53.230 --> 00:06:57.870
That is a glacial lake, dammed
up by ice, ready to burst, a
00:06:57.870 --> 00:07:00.270
flood of water and sediment
that will rush downstream.
00:07:06.570 --> 00:07:10.400
It's an entire system of
erosion, a machine that
00:07:10.400 --> 00:07:12.260
continually works
toward change.
00:07:16.710 --> 00:07:19.545
Up here, impermanence
is everywhere.
00:07:24.440 --> 00:07:27.660
This is a huge landscape,
isn't it?
00:07:27.660 --> 00:07:29.770
You've been working up here
more than 30 years.
00:07:29.770 --> 00:07:33.550
So why don't you take me through
what we're seeing.
00:07:33.550 --> 00:07:36.410
The place is called Khadburi
down there in that village.
00:07:36.410 --> 00:07:41.690
You can see that this is a
boundary like area between the
00:07:41.690 --> 00:07:46.510
upper Mustang and the
lower Mustang area.
00:07:46.510 --> 00:07:51.460
And here, interestingly,
you have the old
00:07:51.460 --> 00:07:54.470
sediments of the ocean.
00:07:54.470 --> 00:07:58.900
The oceanic sediments, these are
now converted into rocks.
00:07:58.900 --> 00:08:02.810
These rivers were flowing south
from Tibet side even
00:08:02.810 --> 00:08:04.460
before the rise of
the Himalayas.
00:08:04.460 --> 00:08:10.050
So this river has cut through
the Himalaya as the Himalaya
00:08:10.050 --> 00:08:11.300
was rising.
00:08:19.230 --> 00:08:22.530
So in a way, the rivers
are older than
00:08:22.530 --> 00:08:23.750
the Himalayan rising.
00:08:23.750 --> 00:08:27.130
And these rivers have been
carrying sediments from all
00:08:27.130 --> 00:08:30.950
these areas throughout its
history and bringing them to
00:08:30.950 --> 00:08:34.825
the Ganges River and then
finally to the Bay of Bengal.
00:08:40.370 --> 00:08:42.270
These valleys were all filled
with these sediments.
00:08:42.270 --> 00:08:45.230
And now, very little has
remained and that means the
00:08:45.230 --> 00:08:48.940
power of these rivers carrying
down these sediments.
00:08:48.940 --> 00:08:50.770
And one day, all these
sediments will be
00:08:50.770 --> 00:08:52.055
all gone from here.
00:08:52.055 --> 00:08:54.315
So despite their thickness,
they're very transitory,
00:08:54.315 --> 00:08:55.170
aren't they?
00:08:55.170 --> 00:08:56.010
They won't be there very long.
00:08:56.010 --> 00:08:57.520
Yes, definitely.
00:08:57.520 --> 00:09:00.390
In the due course of time
everything that you see, these
00:09:00.390 --> 00:09:02.320
deposits will be all gone.
00:09:02.320 --> 00:09:04.830
And only the bedrocks
will be left there.
00:09:07.850 --> 00:09:10.110
Throughout the Himalayas, one of
the most impressive things
00:09:10.110 --> 00:09:14.880
you see are huge landslides and
debris flows tearing down
00:09:14.880 --> 00:09:16.210
the mountains.
00:09:16.210 --> 00:09:19.950
And as soon as the uplift stops,
as soon as India and
00:09:19.950 --> 00:09:23.450
Asia become locked, then
gravity will win.
00:09:23.450 --> 00:09:25.910
We know that in about 200
million years time, the
00:09:25.910 --> 00:09:29.405
Himalayas will we beveled
to a low relief surface.
00:09:32.340 --> 00:09:34.800
People have lived and farmed
in Mustang for
00:09:34.800 --> 00:09:36.780
more than 1,000 years.
00:09:36.780 --> 00:09:41.170
The sediments make for fertile
fields and the landscape forms
00:09:41.170 --> 00:09:43.030
the very core of
their beliefs.
00:09:43.030 --> 00:09:57.170
[SPEAKING NEPALI]
00:09:57.170 --> 00:09:58.960
These are people of the
Bhote tradition.
00:10:03.970 --> 00:10:07.480
Bhote monks mediate in caves
carved into the walls of the
00:10:07.480 --> 00:10:09.660
Kali Gandaki.
00:10:09.660 --> 00:10:12.135
They crawl into the embrace
of the rock itself.
00:10:26.340 --> 00:10:30.680
This village's name, Lubrak,
means crag of the snake skin.
00:10:30.680 --> 00:10:35.420
It's named after this relief
on the canyon wall.
00:10:35.420 --> 00:10:38.450
People here believe that there
are nasty snake spirits in the
00:10:38.450 --> 00:10:41.020
rock that will cause
trouble unless they
00:10:41.020 --> 00:10:42.270
pray to them daily.
00:10:45.740 --> 00:10:47.990
Lubrak rests on a shoulder
of a stream
00:10:47.990 --> 00:10:49.750
that feeds the Gandaki.
00:10:49.750 --> 00:10:53.010
But it is in the shadow of a
massive boulder that will
00:10:53.010 --> 00:10:57.502
demolish the town if or
when it's dislodged.
00:10:57.502 --> 00:10:58.300
Yeah.
00:10:58.300 --> 00:11:02.350
Unfortunately, the village is
not in a very good place in
00:11:02.350 --> 00:11:05.810
the sense that when you have
very large earthquakes, a lot
00:11:05.810 --> 00:11:08.550
of these buildings will collapse
and also a lot of
00:11:08.550 --> 00:11:12.015
these boulders will come down
and damage the building and
00:11:12.015 --> 00:11:14.010
kill people.
00:11:14.010 --> 00:11:15.730
I can very large blocks
up there--
00:11:15.730 --> 00:11:16.530
Yeah.
00:11:16.530 --> 00:11:17.310
--scattered around.
00:11:17.310 --> 00:11:19.030
And I can see a wide area where
there's obviously been a
00:11:19.030 --> 00:11:19.810
recent landslide.
00:11:19.810 --> 00:11:22.820
So the next major earthquake
for this area will begin to
00:11:22.820 --> 00:11:25.090
send all this coming
down the slope.
00:11:25.090 --> 00:11:28.410
You may ask why these people
are living in these areas?
00:11:28.410 --> 00:11:31.540
Whenever you have these kind of
land slides, you have more
00:11:31.540 --> 00:11:35.780
flat radius formed and more
gentle slopes are formed.
00:11:35.780 --> 00:11:39.160
And naturally, that is a good
place for farming agriculture.
00:11:39.160 --> 00:11:42.790
So therefore, many of these
areas where you have these
00:11:42.790 --> 00:11:47.480
villages, settled somewhere
in the landslide areas.
00:11:47.480 --> 00:11:50.640
These landslides only occur once
every few hundred years.
00:11:50.640 --> 00:11:54.050
So there's major opportunities
there for communities to
00:11:54.050 --> 00:11:58.260
occupy those areas safely until
the next landslide.
00:11:58.260 --> 00:11:59.960
But it's a dangerous
landscape.
00:11:59.960 --> 00:12:07.260
[SPEAKING NEPALI]
00:12:07.260 --> 00:12:10.480
So it's really no wonder that
the monks of Lubrak pray for
00:12:10.480 --> 00:12:12.740
the serenity of the landscape.
00:12:12.740 --> 00:12:16.090
Everyone here is conversant on
the tectonic history of the
00:12:16.090 --> 00:12:17.540
Kali Gandaki.
00:12:17.540 --> 00:12:20.730
They speak of an earthquake
in 1505 as
00:12:20.730 --> 00:12:22.530
if it happened recently.
00:12:22.530 --> 00:12:25.404
Of course, in geologic
terms it did.
00:12:32.500 --> 00:12:35.820
Religions have always attempted
to explain why the
00:12:35.820 --> 00:12:37.500
Earth does what it does.
00:12:37.500 --> 00:12:40.240
And geologists have always tried
to apply their science
00:12:40.240 --> 00:12:43.070
to the landscape to
do the same thing.
00:12:43.070 --> 00:12:45.840
It's a question of
perspective.
00:12:45.840 --> 00:12:48.750
145, 150 million years
or a little older.
00:12:48.750 --> 00:12:51.910
The study of geology isn't
really very old.
00:12:51.910 --> 00:12:54.520
But the cultures of
the Himalayas are.
00:12:54.520 --> 00:12:57.080
So for centuries, whenever
they found the fossil of
00:12:57.080 --> 00:13:01.490
Jurassic era sea shell, they had
no choice but to regard it
00:13:01.490 --> 00:13:04.220
with a degree of mysticism.
00:13:04.220 --> 00:13:06.760
We'll see if we can excavate one
of kings of the Jurassic.
00:13:06.760 --> 00:13:09.612
These are called
ammonite, yeah.
00:13:09.612 --> 00:13:14.137
Now, the age of these rocks
are Upper Jurassic, 150
00:13:14.137 --> 00:13:19.240
million to 145 million
or a little older.
00:13:19.240 --> 00:13:23.580
And during this time,
the sea was ruled
00:13:23.580 --> 00:13:26.830
by these have ammonites.
00:13:26.830 --> 00:13:28.860
The continents, particularly
the northern--
00:13:28.860 --> 00:13:29.700
Found one.
00:13:29.700 --> 00:13:32.260
Yeah, it's beautiful.
00:13:32.260 --> 00:13:33.530
It's perfect.
00:13:33.530 --> 00:13:34.970
Yeah, it came out.
00:13:34.970 --> 00:13:36.220
It's wonderful.
00:13:38.820 --> 00:13:41.246
So these are kings of the
Jurassic Ocean, which are now
00:13:41.246 --> 00:13:44.040
more than 3,000 meters
above sea level.
00:13:44.040 --> 00:13:45.570
Yeah, that's very interesting.
00:13:45.570 --> 00:13:50.740
And these ammonites were
living in the ocean.
00:13:50.740 --> 00:13:53.655
Now, they are at the top
of the mountain.
00:13:56.800 --> 00:13:59.380
This is the proof that this
part of the mountain was
00:13:59.380 --> 00:14:03.370
undersea at some time about 150
million years before here.
00:14:03.370 --> 00:14:05.410
They dominated those oceans,
didn't they?
00:14:05.410 --> 00:14:05.890
Yeah.
00:14:05.890 --> 00:14:07.655
In a way that the dinosaurs
dominated life on
00:14:07.655 --> 00:14:07.910
land at the same time.
00:14:07.910 --> 00:14:08.180
Yes, exactly.
00:14:08.180 --> 00:14:11.206
This is very interesting.
00:14:11.206 --> 00:14:13.540
Is there a local
name for these?
00:14:13.540 --> 00:14:14.460
Saligram is the name.
00:14:14.460 --> 00:14:14.750
Saligram.
00:14:14.750 --> 00:14:15.850
Saligram.
00:14:15.850 --> 00:14:17.100
Ammonite is the scientific
name.
00:14:23.550 --> 00:14:26.240
[NEPALESE], Namaste.
00:14:26.240 --> 00:14:29.560
Nick and Professor Upreti are
joined by anthropologist Carol
00:14:29.560 --> 00:14:32.810
Dunham, who's been studying the
cultures of these valleys
00:14:32.810 --> 00:14:34.400
for 30 years.
00:14:34.400 --> 00:14:36.700
She's going to lead them
to a sacred site
00:14:36.700 --> 00:14:38.296
over the next ridge.
00:14:38.296 --> 00:14:43.230
[SPEAKING NEPALI]
00:14:43.230 --> 00:14:46.290
One of the most important
Mustang traditions is to make
00:14:46.290 --> 00:14:49.850
sure visitors leave happy and
that prayers are said to keep
00:14:49.850 --> 00:14:51.333
the earth's rumblings at bay.
00:15:05.190 --> 00:15:06.990
The mules trudge
up steep cliffs
00:15:06.990 --> 00:15:08.240
of compressed sediments.
00:15:11.820 --> 00:15:13.400
This is a land of trails
00:15:13.400 --> 00:15:15.560
connecting valleys and cultures.
00:15:15.560 --> 00:15:18.780
Suspension bridges have helped
shorten some routes.
00:15:18.780 --> 00:15:22.090
But it's still best when
travelling in Mustang to give
00:15:22.090 --> 00:15:23.340
yourself time.
00:15:27.000 --> 00:15:30.740
Pilgrims have passed by this
shrine of stones, this stupa,
00:15:30.740 --> 00:15:33.390
for centuries.
00:15:33.390 --> 00:15:37.030
Each little rock left behind is
like a coin thrown into a
00:15:37.030 --> 00:15:39.290
wishing well.
00:15:39.290 --> 00:15:41.883
I can really feel the
elevation right now.
00:15:41.883 --> 00:15:42.346
Yeah.
00:15:42.346 --> 00:15:45.124
Each breathe is precious, huh.
00:15:45.124 --> 00:15:48.730
At his time of year, the temple
at Muktinath becomes a
00:15:48.730 --> 00:15:51.045
pilgrimage site for Hindus
from Kathmandu
00:15:51.045 --> 00:15:52.744
and Southern Nepal.
00:15:57.010 --> 00:15:57.740
Ah, saligrams.
00:15:57.740 --> 00:15:58.440
Yeah.
00:15:58.440 --> 00:16:01.330
We've seen these in every
community we've visited.
00:16:01.330 --> 00:16:05.030
Now, how does a fossil
become revered?
00:16:05.030 --> 00:16:07.330
These ammonites are found
here in these areas.
00:16:07.330 --> 00:16:13.450
Traditionally, these ammonites
are worshiped by the Hindus.
00:16:13.450 --> 00:16:18.160
They represent life itself,
the very life itself.
00:16:18.160 --> 00:16:23.360
So would they carry these as
good luck symbols with them?
00:16:23.360 --> 00:16:25.120
It's about a god actually.
00:16:25.120 --> 00:16:30.350
So they actually worship
it every day at home.
00:16:30.350 --> 00:16:35.475
I have these saligrams at my
home, where my ancestors were
00:16:35.475 --> 00:16:36.725
for many generations.
00:16:43.220 --> 00:16:46.130
Some of these Hindus have walked
for two weeks to get
00:16:46.130 --> 00:16:49.150
here, up the side of a mountain,
near the foot of a
00:16:49.150 --> 00:16:51.986
landslide where a crystal
clear spring emerges.
00:16:55.540 --> 00:16:59.310
For these worshipers, there is
a sacredness to this place,
00:16:59.310 --> 00:17:01.830
tied to the drama of the
landscape and the
00:17:01.830 --> 00:17:03.900
presence of the water.
00:17:03.900 --> 00:17:06.480
The 108 spouts symbolize
all of the water
00:17:06.480 --> 00:17:07.730
actually on this planet.
00:17:10.900 --> 00:17:14.890
So today, they're purifying
and they're bathing as a
00:17:14.890 --> 00:17:18.819
symbol also of representing
the whole world itself.
00:17:27.819 --> 00:17:32.210
Today, actually they're
worshiping the goddess Durga,
00:17:32.210 --> 00:17:33.685
for the Hindus here.
00:17:33.685 --> 00:17:35.390
But before they do that,
they have to bathe.
00:17:35.390 --> 00:17:38.350
They have to purify themselves
so they can see clearly.
00:17:38.350 --> 00:17:40.390
And that's really where the
importance of water is, which
00:17:40.390 --> 00:17:41.915
is essential.
00:17:41.915 --> 00:17:44.970
To purify the mind and the body,
they believe you have to
00:17:44.970 --> 00:17:46.220
do that water.
00:17:50.740 --> 00:17:53.160
As a geologist, I've noticed
that this area a giant
00:17:53.160 --> 00:17:55.612
landslide and this spring
is emerging at
00:17:55.612 --> 00:17:57.250
the back of the landslide.
00:17:57.250 --> 00:17:59.552
Do they know that, that that
landslide could happen again
00:17:59.552 --> 00:18:00.900
in the future?
00:18:00.900 --> 00:18:04.050
I think that there is a great
awareness that they live in a
00:18:04.050 --> 00:18:05.450
very volatile place.
00:18:05.450 --> 00:18:07.680
And they see that in
a sacred sense.
00:18:07.680 --> 00:18:10.655
Their world view is one that
they need to propitiate the
00:18:10.655 --> 00:18:13.340
Earth's spirits that
they coexist with.
00:18:13.340 --> 00:18:15.270
So their response is
a religious or
00:18:15.270 --> 00:18:16.820
ritual one to that.
00:18:16.820 --> 00:18:19.570
And they believe that these
landslides are caused when
00:18:19.570 --> 00:18:21.575
there is disharmony and when
they're unhappy with the
00:18:21.575 --> 00:18:22.825
Earth's spirits.
00:18:25.170 --> 00:18:28.470
What I really love, as I said,
the stories, where you will
00:18:28.470 --> 00:18:31.716
look at it and as a geologist,
will tell one story in the
00:18:31.716 --> 00:18:34.870
striations, in the folds, in the
crumples of the mountain.
00:18:34.870 --> 00:18:39.690
For them, they will see a very
dramatic interplay of spirits
00:18:39.690 --> 00:18:43.240
at play, that is frozen there,
demons and spirits that live
00:18:43.240 --> 00:18:44.730
within the rock itself.
00:18:44.730 --> 00:18:46.180
So I come up here
as a geologist.
00:18:46.180 --> 00:18:48.490
And I would map this area to
try and understand how the
00:18:48.490 --> 00:18:50.310
Himalayas were built.
00:18:50.310 --> 00:18:53.420
But I'm sort of missing the
big picture, aren't I?
00:18:53.420 --> 00:18:56.780
Well, I think that while you
look at that incredible, rich
00:18:56.780 --> 00:18:59.680
story, there is a very
profound story that's
00:18:59.680 --> 00:19:03.140
invisible, that they see
as well within there.
00:19:03.140 --> 00:19:06.630
And when that is lost, we lose
a very profound link to the
00:19:06.630 --> 00:19:07.880
Earth Itself.
00:19:19.150 --> 00:19:22.480
Over the years, pilgrims have
carved prayers into rock.
00:19:22.480 --> 00:19:24.100
These are Mani stones.
00:19:24.100 --> 00:19:26.780
And they ask the land for
peaceful passage along these
00:19:26.780 --> 00:19:28.030
mountain paths.
00:19:34.220 --> 00:19:36.060
But there are no guarantees.
00:19:36.060 --> 00:19:38.205
This path cuts through the
Muktinath landslide.
00:19:42.960 --> 00:19:44.220
We've talked about
these as hazards.
00:19:44.220 --> 00:19:46.190
We've got the community
down there.
00:19:46.190 --> 00:19:48.650
But basically, this is how
mountains are pulled down,
00:19:48.650 --> 00:19:49.770
aren't they?
00:19:49.770 --> 00:19:50.510
Yeah.
00:19:50.510 --> 00:19:54.250
This is the mountain's fate.
00:19:54.250 --> 00:19:57.960
They rise and then finally
they are brought down.
00:19:57.960 --> 00:20:02.216
And one day, they become
flat and almost
00:20:02.216 --> 00:20:04.015
there is mountain left.
00:20:04.015 --> 00:20:05.760
And this is the process
that happens.
00:20:05.760 --> 00:20:08.510
Erosions goes on and on.
00:20:08.510 --> 00:20:11.910
And this is how the mountains
have to come down and finally
00:20:11.910 --> 00:20:13.160
become the plains.
00:20:21.270 --> 00:20:24.740
Flattening the Himalayas means
an immense amount of material
00:20:24.740 --> 00:20:28.350
will be carried down through
the Kali Gandaki Gorge.
00:20:28.350 --> 00:20:30.980
The problem is that the glaciers
is in the Himalayas
00:20:30.980 --> 00:20:35.020
are melting faster these days,
expelling more sediments and
00:20:35.020 --> 00:20:37.220
dumping a gigantic load
into the river
00:20:37.220 --> 00:20:38.470
systems to the south.
00:20:49.446 --> 00:20:51.332
It's amazing the amount
of sediment in this
00:20:51.332 --> 00:20:52.890
river, isn't it?
00:20:52.890 --> 00:20:55.350
One of the heavies silt
loads of any river
00:20:55.350 --> 00:20:55.842
system in the world.
00:20:55.842 --> 00:20:56.826
It might be the heaviest.
00:20:56.826 --> 00:20:59.912
That's because of the Himalayan
mountains, the size
00:20:59.912 --> 00:21:02.864
of them, and the fact there are
glaciers eroding down into
00:21:02.864 --> 00:21:03.848
their slopes.
00:21:03.848 --> 00:21:05.324
They're so young and moving.
00:21:05.324 --> 00:21:07.784
They let off a tremendous
amount of soil.
00:21:10.740 --> 00:21:13.710
Claudia Sadoof is
a hydroeconomist
00:21:13.710 --> 00:21:15.140
with the World Bank.
00:21:15.140 --> 00:21:17.460
She's studying how the countries
that feed off the
00:21:17.460 --> 00:21:21.240
Himalaya runoff can deal with
all the muck that's now
00:21:21.240 --> 00:21:23.040
carried by rivers.
00:21:23.040 --> 00:21:27.168
Well, this caused amazing
problems in all the barriages
00:21:27.168 --> 00:21:28.659
and dams downstream.
00:21:28.659 --> 00:21:29.653
Absolutely.
00:21:29.653 --> 00:21:34.140
Any infrastructure built on the
river for hydropower or
00:21:34.140 --> 00:21:38.874
for irrigation is clogged up
with all this sediment levels.
00:21:38.874 --> 00:21:41.670
And in order to control for
the amazing flooding and
00:21:41.670 --> 00:21:44.631
movement of this river, large
embankments are built
00:21:44.631 --> 00:21:46.322
throughout the system as well.
00:21:46.322 --> 00:21:49.710
When the sediment builds
up-- whoo, whoo, whew--
00:21:49.710 --> 00:21:50.320
Cold?
00:21:50.320 --> 00:21:51.991
--between the barriers
and the enbankment.
00:21:51.991 --> 00:21:53.241
It's insulation water.
00:21:56.284 --> 00:21:59.540
So that must reduce the lifetime
of these dams, if you
00:21:59.540 --> 00:22:01.261
got huge amounts of sediments
coming in,
00:22:01.261 --> 00:22:02.480
Quite significantly.
00:22:02.480 --> 00:22:05.380
Not only the dams themselves,
which begin to have their
00:22:05.380 --> 00:22:07.655
reservoirs expelled very
quickly, but even the
00:22:07.655 --> 00:22:12.280
hydropower turbines are eaten up
by all the soils that goes
00:22:12.280 --> 00:22:14.937
through the turbines because
there's so much soil and silt
00:22:14.937 --> 00:22:18.070
in these waters.
00:22:18.070 --> 00:22:20.540
Now, as a geologist, I see this
river carrying enormous
00:22:20.540 --> 00:22:22.530
volumes of sediment
down to the ocean.
00:22:22.530 --> 00:22:23.615
It's a natural system.
00:22:23.615 --> 00:22:26.140
But you need to manage that
system, don't you?
00:22:26.140 --> 00:22:28.430
What are the main challenges
that arise from all the
00:22:28.430 --> 00:22:30.772
sediment that's going
down river?
00:22:30.772 --> 00:22:34.660
Well, the sediment is so heavy
that it affects all of the
00:22:34.660 --> 00:22:37.280
infrastructure that are
built on the river.
00:22:37.280 --> 00:22:39.260
The river moves and
it meanders.
00:22:39.260 --> 00:22:43.400
And as the river washes the
sediment down, the sediment
00:22:43.400 --> 00:22:45.250
builds up and it creates
little eddies and
00:22:45.250 --> 00:22:46.240
it turns the river.
00:22:46.240 --> 00:22:48.250
And the river flows and is
braided throughout its system.
00:22:48.250 --> 00:22:51.240
So it becomes a very
unpredictable river, that can
00:22:51.240 --> 00:22:54.070
be extremely disruptive
at times of flood.
00:23:03.170 --> 00:23:06.510
Eight tributaries flow through
the Kathmandu Valley, fed by
00:23:06.510 --> 00:23:08.730
waters from the Himalayas.
00:23:08.730 --> 00:23:11.910
This temple on the banks of the
Bagmati River is the place
00:23:11.910 --> 00:23:15.000
where Hindus cremate their dead
and commit the ashes to
00:23:15.000 --> 00:23:17.410
the sacred waters, which
eventually joined
00:23:17.410 --> 00:23:20.470
the Ganges in India.
00:23:20.470 --> 00:23:23.700
There are over 3 million people
around Kathmandu.
00:23:23.700 --> 00:23:26.660
30 years ago, there were only
a few hundred thousand.
00:23:32.105 --> 00:23:35.390
There are few checks against
growth here, even less
00:23:35.390 --> 00:23:38.390
oversight for how buildings
are built and where.
00:23:40.970 --> 00:23:43.830
At times, it feels like
Kathmandu is a city out of
00:23:43.830 --> 00:23:46.690
control and that's what gives
it much of its charm.
00:23:50.190 --> 00:23:54.270
But it's also a disaster
waiting to happen.
00:23:54.270 --> 00:23:58.000
Kathmandu is built on an old
lake bed made of sediments
00:23:58.000 --> 00:24:00.210
that poured in here from
the mountains.
00:24:00.210 --> 00:24:02.750
And the lake bed is on
an earthquake zone.
00:24:18.320 --> 00:24:20.900
These schoolchildren take
their earthquake drills
00:24:20.900 --> 00:24:23.395
seriously, right down
to the fake injuries
00:24:23.395 --> 00:24:26.428
and the gory make-up.
00:24:26.428 --> 00:24:30.170
[SPEAKING NEPALI]
00:24:30.170 --> 00:24:33.460
But when a major earthquake does
hit here, covering their
00:24:33.460 --> 00:24:36.350
heads and running out the front
door of the school might
00:24:36.350 --> 00:24:38.670
not be enough for these
kids to survive.
00:24:38.670 --> 00:24:43.370
[SPEAKING NEPALI]
00:24:43.370 --> 00:24:46.710
As the city has grown very
rapidly, and poorly planned it
00:24:46.710 --> 00:24:49.620
must be said, we've now got
buildings on top of very
00:24:49.620 --> 00:24:51.520
steep, very unstable slopes.
00:24:51.520 --> 00:24:54.710
So the school we just visited
is right on the top there.
00:24:54.710 --> 00:24:57.090
And part of the school has
collapsed down slope.
00:24:57.090 --> 00:24:59.690
So if there's a major
earthquake, you can imagine
00:24:59.690 --> 00:25:01.190
the results there'll
be to the building.
00:25:05.700 --> 00:25:08.910
One of the other caps Professor
B.P. Uphreti wears
00:25:08.910 --> 00:25:12.200
is that of an earthquake
preparedness expert.
00:25:12.200 --> 00:25:15.540
Nepal is overdue for another
large earthquake, isn't it?
00:25:15.540 --> 00:25:15.990
Yes.
00:25:15.990 --> 00:25:16.140
Yes.
00:25:16.140 --> 00:25:19.270
This wouldn't be the place
to be, would it?
00:25:19.270 --> 00:25:23.616
In fact, this core part of the
city, Kathmandu Valley's core
00:25:23.616 --> 00:25:26.245
part, and particularly the
capital of the city's core
00:25:26.245 --> 00:25:28.990
part, is this area.
00:25:28.990 --> 00:25:34.180
And this is going to be really
a ready difficult place when
00:25:34.180 --> 00:25:35.170
you have big earthquakes.
00:25:35.170 --> 00:25:37.680
A lot of houses have
collapsed here.
00:25:37.680 --> 00:25:40.577
And there is a study that
we did one square
00:25:40.577 --> 00:25:42.320
kilometer of the area.
00:25:42.320 --> 00:25:46.510
There were over 2,000
deaths in this area.
00:25:46.510 --> 00:25:50.200
These streets are very narrow
and people have very little
00:25:50.200 --> 00:25:51.520
chance to escape out.
00:25:56.130 --> 00:25:57.980
Kathmandu is very old city.
00:25:57.980 --> 00:25:59.940
They have many such
earthquakes.
00:25:59.940 --> 00:26:04.290
So they also have developed some
indigenous technology for
00:26:04.290 --> 00:26:06.740
artifacts and features to
put in the buildings and
00:26:06.740 --> 00:26:08.660
particularly the temples.
00:26:08.660 --> 00:26:12.270
For example, they have very good
foundations, very wide
00:26:12.270 --> 00:26:12.950
foundations.
00:26:12.950 --> 00:26:16.180
Even if the temples are
torn, but their
00:26:16.180 --> 00:26:17.830
foundation is very wide.
00:26:17.830 --> 00:26:21.280
It's a pyramidal structure
in a way.
00:26:21.280 --> 00:26:23.760
Many of these temples have
survived in the last
00:26:23.760 --> 00:26:27.610
earthquake of 1934 of
8.3 Richter scale.
00:26:27.610 --> 00:26:30.880
I presume modern day Kathmandu,
which is growing so
00:26:30.880 --> 00:26:33.730
quickly with urban sprawl, the
buildings are put up cheaply,
00:26:33.730 --> 00:26:34.650
aren't they?
00:26:34.650 --> 00:26:38.660
That's exactly the scariest
thing that is happening today
00:26:38.660 --> 00:26:43.260
in Nepal, in Kathmandu, is that
the buildings are coming
00:26:43.260 --> 00:26:46.240
up so quickly and the structures
are not safe.
00:26:46.240 --> 00:26:50.230
And if you are not going to make
good structures, they are
00:26:50.230 --> 00:26:52.500
more vulnerable and more
dangerous than
00:26:52.500 --> 00:26:55.070
the traditional buildings.
00:26:55.070 --> 00:26:57.950
Normally we say it's not the
question whether there will be
00:26:57.950 --> 00:27:00.475
an earthquake in Kathmandu
or not, in it is when.
00:27:08.410 --> 00:27:10.920
So we know by looking at the
geology of the continents,
00:27:10.920 --> 00:27:14.910
going back 4 billion years, even
more, that Himalayan type
00:27:14.910 --> 00:27:16.160
mountains are ephemeral.
00:27:22.840 --> 00:27:25.990
So you're converting
massive, impressive
00:27:25.990 --> 00:27:28.226
mountains into sediment.
00:27:31.780 --> 00:27:34.240
These rivers feed
into the Ganges.
00:27:34.240 --> 00:27:37.220
If we remember the analogy that
the Earth here works like
00:27:37.220 --> 00:27:40.880
a machine, then the Ganges is
the transport link that
00:27:40.880 --> 00:27:42.845
delivers raw materials
to the factory.
00:27:46.610 --> 00:27:50.500
But the Ganges is also the
source of life for a sixth of
00:27:50.500 --> 00:27:53.720
the planet's population.
00:27:53.720 --> 00:27:56.830
As the Himalayan sediments flow
through, some are left
00:27:56.830 --> 00:28:01.580
behind to make incredibly
fertile farmland.
00:28:01.580 --> 00:28:04.890
But now, there are more people
relying on the Ganges and what
00:28:04.890 --> 00:28:08.360
it provides than ever before.
00:28:08.360 --> 00:28:11.020
The strain on the system
has become enormous.
00:28:28.010 --> 00:28:31.190
Here are some facts about
the Ganges River.
00:28:31.190 --> 00:28:34.770
It's over 2,500 kilometers
long, snaking from the
00:28:34.770 --> 00:28:36.525
Himalayas to the
Bay of Bengal.
00:28:48.560 --> 00:28:50.680
Along its route, the
Ganges sustains
00:28:50.680 --> 00:28:53.570
over a billion people.
00:28:53.570 --> 00:28:56.780
In Calcutta alone, near the
river's mouth, there are over
00:28:56.780 --> 00:29:00.370
5 million people, and for each
of them, the river is the
00:29:00.370 --> 00:29:01.620
center of life.
00:29:03.904 --> 00:29:08.440
The sheer volume of people that
are using this water is
00:29:08.440 --> 00:29:11.390
just amazing to anyone who
tries to understand the
00:29:11.390 --> 00:29:13.840
different river systems
of the world.
00:29:13.840 --> 00:29:17.270
Dr. Saugata Datta teaches at
Kansas State University in
00:29:17.270 --> 00:29:18.550
America now.
00:29:18.550 --> 00:29:21.390
But he grew up here in Calcutta,
studying both the
00:29:21.390 --> 00:29:25.110
water and everything that gets
poured into the Ganges,
00:29:25.110 --> 00:29:29.000
industrial waste, garbage,
sewage, even the ashes from
00:29:29.000 --> 00:29:30.250
Hindu funerals.
00:29:37.430 --> 00:29:40.980
At the same time, babies are
baptized in the river and
00:29:40.980 --> 00:29:43.660
people perform their ablutions,
even though the
00:29:43.660 --> 00:29:47.660
river water itself is
far from hygienic.
00:29:47.660 --> 00:29:50.630
The water causes skin
rashes, infections,
00:29:50.630 --> 00:29:52.810
and intestinal problems.
00:29:52.810 --> 00:29:56.260
Getting the water uncontaminated
is out of the
00:29:56.260 --> 00:29:58.360
question right now,
as it stands.
00:29:58.360 --> 00:30:00.900
I don't suppose the central
problem is it's a holy river
00:30:00.900 --> 00:30:01.800
for many people.
00:30:01.800 --> 00:30:04.870
So how do you slowly
ween them off that?
00:30:04.870 --> 00:30:10.360
People still have this belief
that the river water, the
00:30:10.360 --> 00:30:12.400
Ganges River water, is actually
coming from the
00:30:12.400 --> 00:30:16.330
Himalayas and it is untainted
throughout its journey or
00:30:16.330 --> 00:30:19.002
course until it gets
into the delta.
00:30:22.270 --> 00:30:24.960
How do you tell a billion people
that something they
00:30:24.960 --> 00:30:28.840
believe is so sacred is filled
with impurities?
00:30:28.840 --> 00:30:32.060
How does a scientist separate
his work from his beliefs?
00:30:35.090 --> 00:30:38.180
I was born and brought
up in this culture.
00:30:38.180 --> 00:30:43.900
I understood the presence of the
river in our society, in
00:30:43.900 --> 00:30:45.340
our religion.
00:30:45.340 --> 00:30:51.350
And it is inborn or ingrained
in my family too.
00:30:51.350 --> 00:30:54.080
We still know the science behind
it We exactly know how
00:30:54.080 --> 00:30:55.970
the pollution is happening.
00:30:55.970 --> 00:31:01.770
We know that it is one most
polluted waters of the water.
00:31:01.770 --> 00:31:06.450
But still to us, it remains as
holy water which we can use
00:31:06.450 --> 00:31:11.690
for the entire time to
come for the future.
00:31:16.050 --> 00:31:18.950
Calcutta, like India, is growing
at a stunning rate.
00:31:26.130 --> 00:31:29.320
The demand for water has drawn
people into the streets, where
00:31:29.320 --> 00:31:31.395
they pump it up from an
underground aquifer.
00:31:38.570 --> 00:31:41.980
He's pumping groundwater from
a shallow aquifer that runs
00:31:41.980 --> 00:31:43.350
beneath this massive city.
00:31:43.350 --> 00:31:45.430
Isn't there some pollution
into this?
00:31:45.430 --> 00:31:45.780
Yes.
00:31:45.780 --> 00:31:47.600
There should be some pollution
into this.
00:31:47.600 --> 00:31:51.800
But more as we're closer to the
city, to the river Ganges
00:31:51.800 --> 00:31:54.960
in this case, about three
to four kilometers, the
00:31:54.960 --> 00:31:56.545
contamination is much lower.
00:31:56.545 --> 00:31:59.010
So this is pretty much clear
water right now.
00:31:59.010 --> 00:32:02.246
They're using the water for
drinking purpose for all the
00:32:02.246 --> 00:32:04.070
hotels and restaurants nearby.
00:32:04.070 --> 00:32:05.980
And the deep water must be
coming from hundreds of
00:32:05.980 --> 00:32:08.840
kilometers away, up in the
Himalayas and driven down
00:32:08.840 --> 00:32:10.808
pretty deep in the basin.
00:32:10.808 --> 00:32:12.058
That's true.
00:32:15.740 --> 00:32:18.495
Himalayan water providing
for all of these people.
00:32:22.690 --> 00:32:25.840
The problem is that no one is
really sure how much longer
00:32:25.840 --> 00:32:29.220
the tap from the Himalayas
will remain open.
00:32:29.220 --> 00:32:32.410
The glaciers are melting and
presumably one day will be
00:32:32.410 --> 00:32:33.660
gone entirely.
00:32:37.500 --> 00:32:39.550
That would be catastrophic.
00:32:39.550 --> 00:32:43.500
Meanwhile as the glaciers in
Nepal melt faster, the Ganges
00:32:43.500 --> 00:32:46.840
carries more of the sediments
downstream than the watershed
00:32:46.840 --> 00:32:48.090
can handle.
00:32:50.165 --> 00:32:53.870
As freighters head towards
Calcutta, they churn up water
00:32:53.870 --> 00:32:57.690
turbid with Himalayan mud.
00:32:57.690 --> 00:32:59.195
And it's increasing
day by day.
00:33:02.810 --> 00:33:07.230
Right now, it's about 530
million tons of sediment
00:33:07.230 --> 00:33:10.445
throughout the Ganges
River per year.
00:33:10.445 --> 00:33:14.950
And in my 20, 25 years of
growing up in the city myself,
00:33:14.950 --> 00:33:18.740
I have seen more and more
population is encroaching and
00:33:18.740 --> 00:33:21.310
making the channel of the river
smaller and smaller.
00:33:26.910 --> 00:33:30.580
For centuries, Calcutta has
been a gateway to the sea.
00:33:30.580 --> 00:33:33.080
But now, the port
is in jeopardy,
00:33:33.080 --> 00:33:34.800
clogged with sediments.
00:33:34.800 --> 00:33:36.320
The ships hit bottom.
00:33:36.320 --> 00:33:40.210
And in some parts, it's
impossible to navigate at all.
00:33:40.210 --> 00:33:43.560
Meanwhile out here, south of the
city where the river meets
00:33:43.560 --> 00:33:47.040
the sea, life is spent on
fishing boats hauling nets
00:33:47.040 --> 00:33:50.050
through the pull of the mud or
by farming on one of the
00:33:50.050 --> 00:33:53.710
myriad bars of silt that make
up the fingers of the Ganges
00:33:53.710 --> 00:33:56.570
delta, the world's largest
river delta.
00:34:02.060 --> 00:34:05.810
The sediments in the delta
coalesce as small islands and
00:34:05.810 --> 00:34:08.909
then grow as even more
sediments gather.
00:34:08.909 --> 00:34:12.969
But the land they form is low
lying and typhoons can come
00:34:12.969 --> 00:34:16.120
screaming in here and obliterate
everything, the
00:34:16.120 --> 00:34:18.739
farms, the channels,
the livestock,
00:34:18.739 --> 00:34:19.989
and the people here.
00:34:25.790 --> 00:34:29.199
Through it all, that stream
of sediment never stops.
00:34:29.199 --> 00:34:33.080
Some stays, but the bulk
is carried out to sea.
00:34:33.080 --> 00:34:35.810
The sediments fan into
the Bay of Bengal and
00:34:35.810 --> 00:34:37.280
are swept away south.
00:34:37.280 --> 00:34:38.510
You can see them.
00:34:38.510 --> 00:34:40.800
They look like wisps of sand.
00:34:40.800 --> 00:34:44.150
What was once seabed and then
was once the tops of
00:34:44.150 --> 00:34:47.380
mountains, is again at the
bottom of the ocean.
00:34:47.380 --> 00:34:51.210
And as they arrive in Indonesia,
the sediments reach
00:34:51.210 --> 00:34:52.719
the end of the production
line.
00:34:52.719 --> 00:34:56.790
They are about to be fed into
the fiery furnace of the
00:34:56.790 --> 00:34:58.040
collision zone.
00:35:12.820 --> 00:35:16.570
Yogyakarta, is the cultural
capital of Java, Indonesia.
00:35:21.230 --> 00:35:25.190
The downtown is built around a
400-year-old sultan's palace
00:35:25.190 --> 00:35:35.980
that was knocked down by a
vicious earthquake in 2006.
00:35:35.980 --> 00:35:39.140
The earthquake, which registered
7.8 on the Richter
00:35:39.140 --> 00:35:42.260
scale, leveled much of
the rest of the city.
00:35:42.260 --> 00:35:44.680
Almost 6,000 people
died and 1 and 1/2
00:35:44.680 --> 00:35:46.545
million were left homeless.
00:35:51.090 --> 00:35:55.350
Yogyakarta is in a precarious
spot, atop the meeting place
00:35:55.350 --> 00:35:57.920
of two violent tectonic
plates.
00:35:57.920 --> 00:36:01.830
And it's not very far from
Marapi, the volcano that
00:36:01.830 --> 00:36:05.870
created so much havoc
in the fall of 2010.
00:36:05.870 --> 00:36:10.880
Marapi is fed by the tectonics
beneath Indonesia.
00:36:10.880 --> 00:36:14.100
The Indo-Australian plate grinds
against the Pacific
00:36:14.100 --> 00:36:16.360
plate along these Indonesian
islands,
00:36:16.360 --> 00:36:18.590
Sumatra, Java, and Bali.
00:36:18.590 --> 00:36:21.380
That's why Indonesian
looks like it does.
00:36:21.380 --> 00:36:25.000
Geologically, it's known as
an island arc, the surface
00:36:25.000 --> 00:36:28.320
expression of subsurface
machinery right along the
00:36:28.320 --> 00:36:30.990
fault line.
00:36:30.990 --> 00:36:33.260
This is one of the most
dangerous places in the world.
00:36:33.260 --> 00:36:35.880
This is a subduction zone which
runs along the whole
00:36:35.880 --> 00:36:37.880
south coast of Indonesia.
00:36:37.880 --> 00:36:41.380
And the dangerous part is when
the two plates are locked,
00:36:41.380 --> 00:36:44.680
strain builds up and eventually
the Asian plate
00:36:44.680 --> 00:36:47.780
finally releases all that energy
and pops up over the
00:36:47.780 --> 00:36:53.070
Indian plate, and that produces
a large earthquake.
00:36:53.070 --> 00:36:55.840
And of course at about 100
kilometers depth, the edge of
00:36:55.840 --> 00:36:59.470
that plate is melting and that
produces the volcanoes, which
00:36:59.470 --> 00:37:03.290
lie just inland and form this
spine no along the hole of the
00:37:03.290 --> 00:37:05.580
Indonesian plate.
00:37:13.340 --> 00:37:19.410
In 2004, more than 230,000 were
killed by a tsunami that
00:37:19.410 --> 00:37:21.030
hit the west coast of Sumatra.
00:37:27.205 --> 00:37:31.620
In 2009, the Sumatran city of
Padang was shaken by an
00:37:31.620 --> 00:37:34.015
earthquake that killed
an estimated 1,300.
00:37:40.960 --> 00:37:44.940
In the fall of 2010, there were
actually twin tragedies
00:37:44.940 --> 00:37:46.590
for Indonesians.
00:37:46.590 --> 00:37:49.530
First, a tsunami swamped
some remote
00:37:49.530 --> 00:37:52.160
islands, killing hundreds.
00:37:52.160 --> 00:37:54.800
Then central Java was
covered with ash.
00:37:54.800 --> 00:37:58.194
Marapi erupted with much
more force than it
00:37:58.194 --> 00:38:00.465
has shown in a century.
00:38:00.465 --> 00:38:02.700
Temperature around 700.
00:38:02.700 --> 00:38:06.400
Christian Auwe is a ranger who
patrols the landscape around
00:38:06.400 --> 00:38:09.310
the base of Marapi and
has seen every
00:38:09.310 --> 00:38:11.280
one of its many moods.
00:38:11.280 --> 00:38:13.405
He was here in 2006.
00:38:13.405 --> 00:38:17.670
Mount Marapi sometimes they call
it Good Guy and Bad Guy.
00:38:17.670 --> 00:38:23.860
Good Guy because it bring good
things like those boulders,
00:38:23.860 --> 00:38:26.890
stones, sands for buildings.
00:38:26.890 --> 00:38:28.810
Also for the soil is good.
00:38:28.810 --> 00:38:33.590
And you can throw peanuts and
it will grow quickly.
00:38:33.590 --> 00:38:37.230
But in the same time,
destroy everything,
00:38:37.230 --> 00:38:39.825
like houses, people.
00:38:44.230 --> 00:38:47.470
When it's quiet, Marapi can
yield everything from rocks
00:38:47.470 --> 00:38:50.810
for construction to grains
harvested from the volcanic
00:38:50.810 --> 00:38:54.220
earth, which is super fertile
and is the basis for some
00:38:54.220 --> 00:38:55.470
valuable agriculture.
00:39:02.030 --> 00:39:05.270
But when Marapi starts to
thunder, all of the people who
00:39:05.270 --> 00:39:08.540
live around the giant volcano
are evacuated.
00:39:08.540 --> 00:39:11.880
It's a cycle that repeats itself
once every five years
00:39:11.880 --> 00:39:14.750
and makes for a very volatile
place to live.
00:39:17.320 --> 00:39:21.130
The real dangers here are the
pyroclastic flows and they are
00:39:21.130 --> 00:39:23.030
intensely deadly.
00:39:23.030 --> 00:39:26.830
Pyroclastic flows are clouds of
hot gas and rock that can
00:39:26.830 --> 00:39:30.510
whip down the side of a volcano
at terrifying speeds,
00:39:30.510 --> 00:39:33.070
at temperatures of 1,000
degrees Celsius.
00:39:39.050 --> 00:39:41.620
You've seen a lot of
pyroclastic flows.
00:39:41.620 --> 00:39:44.350
If we were standing here when
one came around that corner,
00:39:44.350 --> 00:39:47.770
down the gorge, what would
it looks like?
00:39:47.770 --> 00:39:49.620
I cannot think about it--
00:39:49.620 --> 00:39:53.422
I'd die immediately because the
speed of the lava is 100
00:39:53.422 --> 00:39:54.790
kilometers per hour.
00:39:54.790 --> 00:39:57.440
We only three kilometers
away from up there.
00:39:57.440 --> 00:39:59.610
So you said no, I'm
standing here.
00:39:59.610 --> 00:40:01.710
I cannot tell anything--
00:40:01.710 --> 00:40:02.960
die.
00:40:04.980 --> 00:40:08.780
During the 2006 eruption, two
journalists thought they were
00:40:08.780 --> 00:40:10.340
at a safe distance.
00:40:10.340 --> 00:40:14.260
They had no idea how fast the
pyroclastic flow would pounce
00:40:14.260 --> 00:40:15.300
on top of them.
00:40:15.300 --> 00:40:26.620
[SPEAKING INDONESIAN]
00:40:26.620 --> 00:40:30.560
We got news that they were in
the bunker and they died.
00:40:30.560 --> 00:40:33.740
The day after we come back here
to look for them, but
00:40:33.740 --> 00:40:37.840
because of the thick material,
the pyroclasts is too thick,
00:40:37.840 --> 00:40:41.460
and then we have some
time, two days
00:40:41.460 --> 00:40:44.160
digging we found them.
00:40:44.160 --> 00:40:50.700
[SPEAKING INDONESIAN]
00:40:50.700 --> 00:40:55.490
One guy we found next to the
gate over there, the doors.
00:40:55.490 --> 00:40:56.740
He was--
00:40:59.170 --> 00:41:00.790
what do you call it--
00:41:00.790 --> 00:41:03.750
burned like a barbecue.
00:41:03.750 --> 00:41:05.965
And the other guy was
in the bathroom.
00:41:05.965 --> 00:41:08.940
It was boiling, die.
00:41:08.940 --> 00:41:09.970
They both--
00:41:09.970 --> 00:41:10.670
death--
00:41:10.670 --> 00:41:11.730
yeah.
00:41:11.730 --> 00:41:14.410
Two days after the eruption,
we found them.
00:41:14.410 --> 00:41:29.140
[SPEAKING INDONESIAN]
00:41:29.140 --> 00:41:32.236
Marapi has done nasty things
to a lot of people.
00:41:35.370 --> 00:41:39.050
In 1830, 1,400 died.
00:41:39.050 --> 00:41:42.450
In 1994, another
64 were killed.
00:41:45.840 --> 00:41:49.430
All is quiet on this day though,
barely a burp on the
00:41:49.430 --> 00:41:50.680
seismograph.
00:41:54.300 --> 00:41:59.145
But on May 27, 2006, the
seismograph looked like this.
00:42:03.150 --> 00:42:05.200
Marapi misbehaves often.
00:42:05.200 --> 00:42:08.350
So to keep tabs on things
in the quiet times, the
00:42:08.350 --> 00:42:10.880
caretakers make a monthly
trek to the summit.
00:42:17.190 --> 00:42:20.420
Just before sunrise, their
headlights catch blooms of
00:42:20.420 --> 00:42:23.810
volcanic rock, particulates
swirl in the air with the
00:42:23.810 --> 00:42:25.060
sulphur gases.
00:42:29.350 --> 00:42:32.890
This place here is the death
zone of one of the subduction
00:42:32.890 --> 00:42:36.630
related volcanoes, all because
of the magmatite which is
00:42:36.630 --> 00:42:37.965
pushing up from underneath
the volcano.
00:42:37.965 --> 00:42:39.600
It's pretty stiff.
00:42:39.600 --> 00:42:42.620
And most people have an image of
volcanoes with red-hot lava
00:42:42.620 --> 00:42:43.620
running down the slope.
00:42:43.620 --> 00:42:46.490
It's not the case in this
type of volcano.
00:42:46.490 --> 00:42:50.840
Where it's very stiff, magma has
pushed up from the magma
00:42:50.840 --> 00:42:52.890
chamber and forms
this lava dome.
00:42:52.890 --> 00:42:54.950
And we've been spending the last
couple hours wandering
00:42:54.950 --> 00:42:56.260
around this lava dome.
00:42:56.260 --> 00:42:59.130
And it gets pushed
up, pushed up.
00:42:59.130 --> 00:43:00.380
And it eventually collapses.
00:43:02.910 --> 00:43:05.900
And one can safely predict that
in the next few months,
00:43:05.900 --> 00:43:08.850
the next few years, the whole
side of the mountain will give
00:43:08.850 --> 00:43:11.365
way and there will be an
enormous pyroclastic flow.
00:43:17.060 --> 00:43:21.050
The rising sun reveals the
steaming dome of Marapi.
00:43:21.050 --> 00:43:23.580
There is no looking over
the lip here, to
00:43:23.580 --> 00:43:25.640
peer down into a crater.
00:43:25.640 --> 00:43:29.200
After Marapi explodes, the lava
congeals and covers the
00:43:29.200 --> 00:43:34.440
volcano with a cap, a
form-fitting lid.
00:43:34.440 --> 00:43:37.320
And you can see cracks
around here.
00:43:37.320 --> 00:43:40.650
We've already had two small
earthquakes this morning.
00:43:40.650 --> 00:43:46.790
And the whole side of the lava
dome will very soon collapse.
00:43:46.790 --> 00:43:49.340
All the signs are here,
the tremors, the
00:43:49.340 --> 00:43:51.630
steam, and the heat.
00:43:51.630 --> 00:43:52.850
This area is cracking.
00:43:52.850 --> 00:43:55.210
This area is literally
falling apart.
00:43:55.210 --> 00:44:00.320
And the cracks provide conduits
for sulfur dioxide
00:44:00.320 --> 00:44:02.640
and other sulfur gases and
also a lot of water
00:44:02.640 --> 00:44:04.330
vapor to come up.
00:44:04.330 --> 00:44:05.180
So these are called
00:44:05.180 --> 00:44:07.690
"fumaroles," which means smoking.
00:44:07.690 --> 00:44:10.068
And he's measuring the
temperature of
00:44:10.068 --> 00:44:11.550
one of these fumaroles.
00:44:17.972 --> 00:44:19.470
Now, these are scalding
temperatures.
00:44:19.470 --> 00:44:21.440
These are just a little
bit below boiling.
00:44:21.440 --> 00:44:23.070
So this is quite a
dangerous area.
00:44:23.070 --> 00:44:27.980
And the rocks too are being
rotted by gas moving up
00:44:27.980 --> 00:44:29.180
through them.
00:44:29.180 --> 00:44:32.870
So this area is completely
disintegrating.
00:44:32.870 --> 00:44:34.870
By walking around, looking at
what's happening to these
00:44:34.870 --> 00:44:39.530
slopes, taking temperatures,
we're in for a big one.
00:44:39.530 --> 00:44:43.760
This is not a place where
you want to hang around.
00:44:43.760 --> 00:44:46.720
It makes me nervous because
I've seen these things in
00:44:46.720 --> 00:44:49.900
action and they're extremely
dangerous.
00:44:49.900 --> 00:44:52.820
But as a geologist, I am
absolutely fascinated by the
00:44:52.820 --> 00:44:56.590
opportunity to come here and
look and see what happens
00:44:56.590 --> 00:44:59.020
before a pyroclastic
flow takes off.
00:45:02.324 --> 00:45:07.280
The pyroclastic flows burst
forth from Marapi only a year
00:45:07.280 --> 00:45:11.250
after Nick visited the
volcano summit.
00:45:11.250 --> 00:45:14.660
Hundreds of thousands of
Javanese were forced to flee
00:45:14.660 --> 00:45:19.500
as Marapi's devastation spread
out farther and farther.
00:45:19.500 --> 00:45:24.010
In the grand tectonics sense,
Marapi is part of the same
00:45:24.010 --> 00:45:26.930
machine that began
in the Himalayas.
00:45:26.930 --> 00:45:31.030
And one day, the end product
will roll out on the tectonic
00:45:31.030 --> 00:45:33.615
assembly line, a whole
new supercontinent.
00:45:46.740 --> 00:45:49.520
This is the debris that
was left behind by
00:45:49.520 --> 00:45:54.820
Marapi's 2006 eruption.
00:45:54.820 --> 00:45:55.940
There were a few unlucky
00:45:55.940 --> 00:45:59.420
homeowners who had to relocate.
00:45:59.420 --> 00:46:02.580
Tourists come up here now, while
they can, to tramp up
00:46:02.580 --> 00:46:06.040
and down the path, next to the
farmers laden with harvest
00:46:06.040 --> 00:46:07.290
from their volcanic fields.
00:46:11.360 --> 00:46:14.120
Some people buy flowers
to make offerings to
00:46:14.120 --> 00:46:15.370
the goddess of Marapi.
00:46:19.670 --> 00:46:24.210
But Marapi is dangerous even
after the eruptions calm down
00:46:24.210 --> 00:46:26.900
because there is always
the risk of lahars.
00:46:40.330 --> 00:46:44.430
A lahar is a massive mudslide
rolling with the weight and
00:46:44.430 --> 00:46:47.020
consistency of concrete.
00:46:47.020 --> 00:46:50.540
When heavy rains soak the
volcanic debris left behind by
00:46:50.540 --> 00:46:54.684
the pyroclastic flows, the
whole mass is dislodged.
00:46:58.180 --> 00:47:01.050
Lahars have been clocked at over
100 kilometers an hour.
00:47:08.230 --> 00:47:11.560
The government has build some
retaining walls here to try to
00:47:11.560 --> 00:47:14.970
control the flow for when
a lahar happens again.
00:47:14.970 --> 00:47:17.210
It's just another hazard
of living along the
00:47:17.210 --> 00:47:18.790
Indo-Australian plate margin.
00:47:21.380 --> 00:47:25.040
All this debris is the final
byproduct of the mechanisms
00:47:25.040 --> 00:47:28.040
that raised the Himalayas,
caused them to share their
00:47:28.040 --> 00:47:31.300
sediments, and then carried
those sediment all the way
00:47:31.300 --> 00:47:35.620
here to be shot out
of a volcano.
00:47:35.620 --> 00:47:37.040
Well, it's a grand cycle.
00:47:37.040 --> 00:47:40.600
You have plates colliding,
huge mountains
00:47:40.600 --> 00:47:42.120
being thrown up.
00:47:42.120 --> 00:47:44.440
Those mountains are
defying gravity.
00:47:44.440 --> 00:47:45.790
Gravity doesn't like
mountains.
00:47:45.790 --> 00:47:47.610
It wants to pull them down.
00:47:47.610 --> 00:47:49.870
Huge amounts of sediments
are being released.
00:47:49.870 --> 00:47:51.980
They are flushed down
into the oceans.
00:47:51.980 --> 00:47:54.630
And then they're recycled
in subduction
00:47:54.630 --> 00:47:56.290
zones to form new lands.
00:47:56.290 --> 00:48:00.040
So it's a great epic of mountain
building, plate
00:48:00.040 --> 00:48:00.930
collisions.
00:48:00.930 --> 00:48:04.320
And sediments are the thread
that connects that to the
00:48:04.320 --> 00:48:08.990
future chapters of new land
and new supercontinents.
00:48:08.990 --> 00:48:11.780
And that's the point,
why all of this huge
00:48:11.780 --> 00:48:14.350
tectonic activity continues.
00:48:14.350 --> 00:48:18.110
It's all about building the
plates, building the land, and
00:48:18.110 --> 00:48:20.465
ultimately constructing
a new supercontinent.
00:48:24.370 --> 00:48:27.120
Supercontinents form
with a frequency of
00:48:27.120 --> 00:48:29.620
about 400 million years.
00:48:29.620 --> 00:48:33.090
The last supercontinent broke up
about 200 million years ago
00:48:33.090 --> 00:48:35.090
to form the modern oceans.
00:48:35.090 --> 00:48:39.460
And slowly, those modern oceans
are being consumed.
00:48:39.460 --> 00:48:42.650
The ocean crust is being lost
down subduction zones.
00:48:42.650 --> 00:48:45.610
And we're just starting to get
into the next phase of
00:48:45.610 --> 00:48:48.820
building another
supercontinent.
00:48:48.820 --> 00:48:51.115
And we can predict the position
of future continents
00:48:51.115 --> 00:48:55.550
with a lot more accuracy than
we can next week's weather.
00:48:55.550 --> 00:48:58.470
So as a geologist if look built
into the future, we can
00:48:58.470 --> 00:49:01.840
say with accuracy that in 200
million years' time there will
00:49:01.840 --> 00:49:05.860
be another supercontinent and
it will be centered around
00:49:05.860 --> 00:49:07.110
Indonesian.
00:49:08.610 --> 00:49:10.600
And then the process
will start again.
00:49:13.520 --> 00:49:16.090
But that is 200 million
years away.
00:49:16.090 --> 00:49:19.410
And for many of us, that amount
of change in that vast
00:49:19.410 --> 00:49:21.060
time frame is unimaginable.
00:49:24.590 --> 00:49:28.740
But change, at least in the
short term, is familiar to the
00:49:28.740 --> 00:49:29.990
people who live here.
00:49:33.620 --> 00:49:35.980
Just come visit and
stay awhile.
00:49:35.980 --> 00:49:39.050
Before long, you'll feel
the earth move too.
Distributor: Bullfrog Films
Length: 50 minutes
Date: 2012
Genre: Expository
Language: English
Grade: 8-12, College, Adult
Color/BW:
Closed Captioning: Available
Interactive Transcript: Available
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