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(explosion)
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00:00:04,404 --> 00:00:07,973
NARRATOR:
Mount St. Helens-- the biggest
volcanic eruption
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00:00:08,041 --> 00:00:11,677
in North America
in nearly a century.
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00:00:13,446 --> 00:00:20,085
Virtually all life for 200
square miles is wiped out.
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00:00:26,693 --> 00:00:29,895
It seems impossible that life
could ever return
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00:00:29,963 --> 00:00:32,865
to this barren wasteland.
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00:00:32,932 --> 00:00:34,767
We found a lot of our
conventional wisdom
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00:00:34,834 --> 00:00:36,602
was just flat wrong.
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00:00:36,669 --> 00:00:39,405
NARRATOR:
In recent years
there are ominous signs
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00:00:39,472 --> 00:00:42,141
the volcano is awakening.
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00:00:42,208 --> 00:00:44,143
MAN:
These things were like
skyscrapers that were being
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00:00:44,210 --> 00:00:45,778
shoved out of the ground.
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00:00:45,845 --> 00:00:47,212
They were literally that big.
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00:00:51,584 --> 00:00:53,819
NARRATOR:
A 30-year quest to understand
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00:00:53,887 --> 00:00:57,256
one of the most complicated
volcanoes in the world
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00:00:57,323 --> 00:01:02,728
is revealing new mysteries
deep inside the mountain.
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MAN:
We don't know whether it's going
to erupt explosively again
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00:01:06,466 --> 00:01:14,706
in two years or in 20 years
or in 200 years.
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00:01:14,774 --> 00:01:18,343
NARRATOR:
Is Mount St. Helens preparing
to erupt again?
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Right now, on NOVA--
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"Mount St. Helens:
Back from the Dead."
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Major funding for NOVA
is provided by the following...
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00:01:48,475 --> 00:01:51,743
Supporting NOVA and promotingg
public understanding of science.
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00:01:54,781 --> 00:01:57,483
And the Corporation
for Public Broadcasting,
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00:01:57,550 --> 00:01:59,251
and by PBS viewers like you.
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00:02:07,060 --> 00:02:10,062
NARRATOR:
October 2004.
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00:02:10,130 --> 00:02:13,565
Mount St. Helens
comes back to life.
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Steam and ash spew from the
crater on the mountain's summit.
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We saw the boiling material
come out of the ground,
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00:02:29,516 --> 00:02:31,517
we saw that it was blasting up,
it was dark
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and it was light
at the same time.
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It made a plume that rose up
over the rim of the caldera.
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00:02:36,489 --> 00:02:38,390
It came up to above
our altitude,
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to 10,000 or 12,000 feet.
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00:02:43,029 --> 00:02:45,397
NARRATOR:
It's a frightening development.
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00:02:45,465 --> 00:02:48,400
(explosion)
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00:02:48,468 --> 00:02:51,570
For years, Mount St. Helens
has been quiet.
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00:02:51,638 --> 00:02:53,739
The volcano went from quiet
to unrest to eruption
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very, very rapidly.
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00:03:00,180 --> 00:03:03,615
NARRATOR:
It could be headed
for a massive explosion.
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00:03:03,683 --> 00:03:05,417
DZURISIN:
It seemed possible
that we were headed
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toward an explosive eruption.
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00:03:07,820 --> 00:03:09,188
We didn't know.
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00:03:09,255 --> 00:03:11,690
That was a key question.
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00:03:11,758 --> 00:03:13,492
NARRATOR:
The effort to understand
what is happening
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00:03:13,560 --> 00:03:16,995
inside the mountain couldn't be
more urgent.
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00:03:17,063 --> 00:03:18,997
Is the volcano about
to repeat the events
48
00:03:19,065 --> 00:03:22,434
of three decades earlier, when
it shattered the tranquility
49
00:03:22,502 --> 00:03:24,436
of its peaceful surroundings?
50
00:03:30,510 --> 00:03:32,778
(bird screeches)
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00:03:32,845 --> 00:03:36,381
NARRATOR:
Spring 1980.
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Mount St. Helens is one
of the major peaks
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in the Cascade Mountains.
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00:03:45,892 --> 00:03:50,095
It's an area of outstanding
beauty, rich in wildlife.
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00:03:53,800 --> 00:03:58,604
For over 120 years,
the volcano has been quiet.
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00:03:58,671 --> 00:04:02,074
But in recent weeks
it's been rumbling.
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00:04:02,141 --> 00:04:06,345
Nobody is sure what to expect.
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00:04:06,412 --> 00:04:09,715
Then, on May 18, 1980,
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00:04:09,782 --> 00:04:14,853
a 5.1 magnitude earthquake
rocks the mountain.
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00:04:26,966 --> 00:04:29,334
Within ten seconds,
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00:04:29,402 --> 00:04:31,870
the volcano's northern flank
collapses
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00:04:31,938 --> 00:04:34,906
in the largest landslide
in recorded history.
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00:04:37,443 --> 00:04:41,913
It releases millions of tons of
magma in a colossal explosion.
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00:04:47,387 --> 00:04:52,057
A cloud of searing gas and rock,
known as a pyroclastic flow,
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00:04:52,125 --> 00:04:54,993
races over the surrounding
countryside.
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00:05:00,300 --> 00:05:02,334
Forests are flattened.
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00:05:10,810 --> 00:05:13,111
Four miles below the summit,
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00:05:13,179 --> 00:05:17,115
an enormous lake is choked
with debris.
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The eruption continues to shoot
poisonous steam and ash
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00:05:28,261 --> 00:05:30,662
miles into the air.
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00:05:40,640 --> 00:05:43,208
It was just, again,
astounding is the best word
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00:05:43,276 --> 00:05:45,644
to describe what happened in
1980 here in Mount St. Helens.
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00:05:51,851 --> 00:05:53,752
NARRATOR:
The northern slope of
the mountain is buried
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in several feet of ash.
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00:06:05,498 --> 00:06:08,633
Virtually all life
is extinguished.
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00:06:13,272 --> 00:06:16,241
57 people are dead.
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00:06:16,309 --> 00:06:22,314
They include loggers, campers,
scientists and a reporter.
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Some are up to 13 miles away
in areas considered safe.
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The plume of steam and ash rises
miles into the sky
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00:06:36,529 --> 00:06:38,296
for the rest of the day.
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00:06:38,364 --> 00:06:41,066
The drifting ash cloud
disrupts air traffic
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00:06:41,134 --> 00:06:44,336
for hundreds of miles.
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00:06:44,404 --> 00:06:49,074
The scale of the destruction
is enormous.
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00:06:55,448 --> 00:06:57,716
NARRATOR:
Across more than
200 square miles,
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the surge of ash and rock
incinerates trees.
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00:07:07,794 --> 00:07:09,194
Thousands of birds
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from more than a hundred species
disappear.
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00:07:16,602 --> 00:07:20,439
Billions of insects are gone.
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00:07:23,743 --> 00:07:27,012
Deer and elk are wiped out.
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00:07:34,987 --> 00:07:38,723
This vast area of devastation
becomes known as the blast
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00:07:38,791 --> 00:07:40,592
or blow-down zone.
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00:07:45,064 --> 00:07:48,633
Nearer the crater, ash and rocks
from the landslide
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00:07:48,701 --> 00:07:50,802
litter the northern slope
of the mountain.
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00:07:55,508 --> 00:07:57,943
It looks like the moon.
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00:08:00,580 --> 00:08:02,681
It's called the pumice plain.
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00:08:04,817 --> 00:08:06,852
It's directly below the crater.
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00:08:10,089 --> 00:08:13,625
Four miles from the volcano,
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00:08:13,693 --> 00:08:16,394
the enormous Spirit Lake
is scarcely recognizable.
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00:08:20,066 --> 00:08:24,402
The avalanche has lifted its bed
more than 200 feet.
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00:08:27,340 --> 00:08:30,675
The surface is smothered
in dead trees.
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00:08:30,743 --> 00:08:34,412
Hundreds of species of aquatic
life, including insects,
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amphibians and fish, are killed.
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00:08:38,851 --> 00:08:40,385
CHARLIE CRISAFULLI:
It was black water.
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00:08:40,453 --> 00:08:42,420
And it de-gassed and bubbled,
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00:08:42,488 --> 00:08:44,689
and there were hot springs
that were coming up.
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00:08:44,757 --> 00:08:46,324
If you were to put your fingers
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00:08:46,392 --> 00:08:49,160
in to your wrist and wiggle
them, you wouldn't even be able
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00:08:49,228 --> 00:08:50,395
to see your fingertips.
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00:08:50,463 --> 00:08:53,365
That's how grossly modified
the water was.
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00:08:56,903 --> 00:08:58,637
NARRATOR:
Mount St. Helens is now
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a lifeless jumble of shattered
forest, rock and ash.
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00:09:03,476 --> 00:09:07,379
It's hard to imagine life
will ever return.
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00:09:15,421 --> 00:09:17,255
The eruption was so powerful,
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00:09:17,323 --> 00:09:19,925
it altered the shape
of the mountain.
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00:09:26,399 --> 00:09:30,135
Mount St. Helens was a typical
cone-shaped volcano
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known as a stratovolcano.
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00:09:37,677 --> 00:09:41,379
But the landslide has torn
1,300 feet off the summit,
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00:09:41,447 --> 00:09:47,352
leaving a gaping crater
a mile wide and 2,000 feet deep.
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00:09:47,420 --> 00:09:50,822
It's the largest volcanic
eruption in North America
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00:09:50,890 --> 00:09:53,592
in nearly a century.
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00:09:59,131 --> 00:10:02,567
(helicopter blades whirring)
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00:10:02,635 --> 00:10:07,739
Weeks after the eruption,
scientists arrive at the crater.
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00:10:09,475 --> 00:10:12,477
The volcano is still steaming
and rumbling.
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00:10:12,545 --> 00:10:14,813
It's a new and unfamiliar world.
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00:10:18,117 --> 00:10:21,553
One of the first to arrive
is Dan Dzurisin.
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DZURISIN:
There was a tremendous amount
of steam
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00:10:23,422 --> 00:10:26,124
and you could see
that it was very hot.
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00:10:26,192 --> 00:10:28,326
You didn't see red lava oozing
out of the ground.
129
00:10:28,394 --> 00:10:31,196
You didn't see fantastic
fire fountains.
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00:10:31,263 --> 00:10:36,668
There was this constant
background roar of rocks
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00:10:36,736 --> 00:10:39,604
cascading down the crater walls.
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00:10:39,672 --> 00:10:42,040
Occasionally a very large rock
the size of the helicopter
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00:10:42,108 --> 00:10:44,142
would come bouncing down
and you could watch it
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00:10:44,210 --> 00:10:47,812
and it was almost slow motion
because the crater was so large.
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00:10:47,880 --> 00:10:51,383
NARRATOR:
Mount St. Helens has a long
history of eruptions.
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00:10:51,450 --> 00:10:56,054
More than 500 years ago, two
massive explosions took place
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00:10:56,122 --> 00:10:57,922
within two years of each other.
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00:10:57,990 --> 00:11:00,825
They were nearly four times
larger than May 1980.
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00:11:02,895 --> 00:11:07,132
The mountain sits on one of
the most active seismic zones
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00:11:07,199 --> 00:11:11,336
in the world,
the Pacific Ring of Fire--
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00:11:11,404 --> 00:11:15,740
a vast arc of volcanoes running
for thousands of miles.
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00:11:15,808 --> 00:11:18,910
It's home to some of the biggest
and most dangerous volcanoes
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00:11:18,978 --> 00:11:21,312
active today.
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00:11:34,260 --> 00:11:37,462
Here, the enormous plates
making up the earth's crust
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00:11:37,530 --> 00:11:42,133
are being squeezed together.
146
00:11:43,035 --> 00:11:45,990
Along the coast, the
plate below the Pacific
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00:11:46,016 --> 00:11:48,559
is sliding un the
North American plate.
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00:11:48,659 --> 00:11:54,172
60 miles down
pressure and friction melt the rock.
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00:11:55,437 --> 00:11:57,938
Magma wells up.
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00:11:58,006 --> 00:12:01,008
When it reaches the surface,
it bursts out.
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00:12:01,076 --> 00:12:03,611
(explosion)
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00:12:10,585 --> 00:12:13,954
But there are still many
unanswered questions.
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00:12:16,891 --> 00:12:20,027
Scientists' understanding
of what triggers an eruption
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00:12:20,095 --> 00:12:22,696
this massive is incomplete.
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00:12:22,764 --> 00:12:24,431
And given the scale
of destruction,
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00:12:24,499 --> 00:12:26,734
they need to find a way
to predict
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00:12:26,801 --> 00:12:30,738
when it might happen again
before it's too late.
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00:12:30,805 --> 00:12:33,140
Mount St. Helens is
about to become
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00:12:33,208 --> 00:12:37,811
one of the most intensely
studied volcanoes in the world.
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00:12:45,553 --> 00:12:49,523
The mysteries are not
just geological.
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00:12:49,591 --> 00:12:52,693
Biologists want to know
if any life has survived
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00:12:52,761 --> 00:12:54,395
and what its future will be.
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00:13:00,001 --> 00:13:02,169
Charlie Crisafulli,
one of the leading experts
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00:13:02,237 --> 00:13:06,840
on the mountain's ecology,
arrives soon after the eruption.
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00:13:06,908 --> 00:13:09,443
CRISAFULLI:
Nothing could have prepared me
for the sights and sounds
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00:13:09,511 --> 00:13:11,512
that I saw when I got here.
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00:13:11,579 --> 00:13:17,484
It was complete
and utter barrenness
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00:13:17,552 --> 00:13:20,154
and there was no sign of life
whatsoever.
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00:13:20,221 --> 00:13:23,123
NARRATOR:
His job is to survey
the mountain,
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00:13:23,191 --> 00:13:26,060
looking for any living things.
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00:13:26,127 --> 00:13:29,730
CRISAFULLI:
It was just intriguing to think
about how would life come back
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00:13:29,798 --> 00:13:30,798
to this landscape.
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00:13:30,865 --> 00:13:32,032
What would the pattern be?
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00:13:32,100 --> 00:13:33,867
How would the rate be?
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00:13:37,172 --> 00:13:40,574
NARRATOR:
Much of the mountain is
still inaccessible.
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00:13:40,642 --> 00:13:43,377
So he starts work
in the blow-down zone
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00:13:43,445 --> 00:13:46,980
in an area some eight miles
downhill from the crater.
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00:13:47,048 --> 00:13:52,519
CRISAFULLI:
We flew over in a helicopter
very close to the ground.
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00:13:52,587 --> 00:13:54,888
We would have these bumping,
twisting flights
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00:13:54,956 --> 00:13:56,924
across the landscape
following a contour.
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00:14:01,296 --> 00:14:02,863
NARRATOR:
In the first three months,
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00:14:02,931 --> 00:14:05,866
there's nothing but
dead and uprooted trees.
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00:14:09,270 --> 00:14:11,438
Then he notices something...
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00:14:14,509 --> 00:14:17,244
Signs of freshly
disturbed earth.
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00:14:21,950 --> 00:14:23,917
CRISAFULLI:
Lo and behold,
in many locations,
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00:14:23,985 --> 00:14:26,754
brown earth on top
of the gray volcanic ash.
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00:14:28,490 --> 00:14:31,158
NARRATOR:
Is there something down there?
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00:14:31,226 --> 00:14:34,394
Crisafulli returns on foot
to investigate.
189
00:14:42,270 --> 00:14:48,909
There, emerging from the ash,
is a tiny burrowing animal.
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00:14:48,977 --> 00:14:53,814
It's a northern pocket gopher.
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00:14:53,882 --> 00:14:55,115
CRISAFULLI:
It was very thrilling.
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00:14:58,386 --> 00:15:02,589
NARRATOR:
How can it possibly have
survived when nothing else has?
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00:15:06,461 --> 00:15:08,562
CRISAFULLI:
This tiny animal lives entirely
beneath the ground.
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00:15:08,630 --> 00:15:10,731
And so when the blast occurred,
195
00:15:10,799 --> 00:15:12,766
it would have been
safely protected
196
00:15:12,834 --> 00:15:14,568
beneath a mantle of soil
197
00:15:14,636 --> 00:15:17,738
and may very well have survived
in many locations.
198
00:15:17,806 --> 00:15:22,075
NARRATOR:
Over the following months,
he finds more gophers.
199
00:15:24,212 --> 00:15:28,282
It appears that life is
returning to the mountain
200
00:15:28,349 --> 00:15:30,784
just three months
after the eruption.
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00:15:37,525 --> 00:15:40,794
NARRATOR:
By fall, the volcano
is still active.
202
00:15:43,398 --> 00:15:45,265
Plumes of steam and ash
203
00:15:45,333 --> 00:15:48,035
continue to shoot thousands
of feet into the air.
204
00:15:51,272 --> 00:15:54,341
But something else
is happening, too.
205
00:15:54,409 --> 00:15:57,044
The crater floor
appears to be moving.
206
00:15:58,980 --> 00:16:02,749
Is the mountain preparing
for another major eruption?
207
00:16:02,817 --> 00:16:06,153
DZURISIN:
We would sometimes
notice a crack
208
00:16:06,221 --> 00:16:08,288
that hadn't been there
the day before.
209
00:16:08,356 --> 00:16:11,024
And by the end of the day
the crack was larger.
210
00:16:11,092 --> 00:16:13,794
And you realized that the ground
was moving beneath your feet.
211
00:16:16,698 --> 00:16:19,032
NARRATOR:
It's an unsettling experience
212
00:16:19,100 --> 00:16:23,270
to stand on the floor of a
volcano that's visibly moving.
213
00:16:26,541 --> 00:16:30,110
If you stood and looked very,
very, very carefully,
214
00:16:30,178 --> 00:16:31,645
with a reference point
in the background,
215
00:16:31,713 --> 00:16:34,982
sometimes you could see it move,
but just barely.
216
00:16:35,049 --> 00:16:40,888
NARRATOR:
The scientists set up a time-
lapse camera on a nearby ridge.
217
00:16:49,030 --> 00:16:52,499
Over several days,
the pictures show a dome
218
00:16:52,567 --> 00:16:55,569
rising in the middle
of the crater floor.
219
00:16:55,637 --> 00:17:00,374
The volcano is oozing
a sticky gray lava,
220
00:17:00,441 --> 00:17:03,744
cooling as it reaches
the surface.
221
00:17:10,451 --> 00:17:14,288
Over several months,
the dome grows larger.
222
00:17:21,129 --> 00:17:23,297
The geologists are puzzled.
223
00:17:23,364 --> 00:17:25,966
What is going on
inside the mountain?
224
00:17:26,034 --> 00:17:28,802
Is Mount St. Helens simply
rebuilding its summit
225
00:17:28,870 --> 00:17:31,238
or is it about to blow up?
226
00:17:31,306 --> 00:17:34,675
DZURISIN:
We didn't know
what might come next,
227
00:17:34,742 --> 00:17:36,944
whether the lava might continue
to grow for many years--
228
00:17:37,011 --> 00:17:38,712
or even decades or centuries--
229
00:17:38,780 --> 00:17:40,280
and we didn't know
if there might be
230
00:17:40,348 --> 00:17:42,649
explosive eruptions in store.
231
00:17:44,719 --> 00:17:47,287
NARRATOR:
Then winter closes in,
232
00:17:47,355 --> 00:17:49,623
restricting access
to the mountain.
233
00:17:51,893 --> 00:17:54,995
The scientists' work is limited.
234
00:17:55,063 --> 00:17:58,098
Answers will have to wait
until spring.
235
00:18:11,312 --> 00:18:13,547
(bird singing)
236
00:18:13,614 --> 00:18:19,519
Spring 1981, nearly a year
after the initial eruption.
237
00:18:19,587 --> 00:18:22,723
Life returns to the hills and
valleys of the Cascade Range.
238
00:18:23,925 --> 00:18:25,792
But on Mount St. Helens,
239
00:18:25,860 --> 00:18:29,329
the devastation of the previous
year is still obvious.
240
00:18:32,367 --> 00:18:33,867
Despite the danger,
241
00:18:33,935 --> 00:18:37,337
Crisafulli moves closer
to the active volcano's core.
242
00:18:40,808 --> 00:18:45,312
The pumice plain is buried
in several feet of coarse ash.
243
00:18:47,015 --> 00:18:50,150
It's a dusty, barren wilderness.
244
00:18:50,218 --> 00:18:54,454
Life seems impossible.
245
00:18:54,522 --> 00:18:57,624
CRISAFULLI:
This is an area where super-hot
incandescent flows came down
246
00:18:57,692 --> 00:18:59,326
and killed all life
that was here.
247
00:19:04,399 --> 00:19:08,235
NARRATOR:
Helicopter is the only way in.
248
00:19:08,302 --> 00:19:10,337
CRISAFULLI:
We were flying back and forth,
very low,
249
00:19:10,405 --> 00:19:13,206
just above the ground surface,
looking for any form of life.
250
00:19:16,077 --> 00:19:21,048
NARRATOR:
He crisscrosses the area
but there's nothing to see.
251
00:19:21,115 --> 00:19:27,954
Then suddenly,
amidst the acres of barren rock,
252
00:19:28,022 --> 00:19:32,325
there's an unexpected flash
of color.
253
00:19:32,393 --> 00:19:36,096
CRISAFULLI:
So we set the helicopter down
and we walked up.
254
00:19:36,164 --> 00:19:40,400
Right out in the center of
the pumice plain we saw a plant.
255
00:19:42,070 --> 00:19:45,872
NARRATOR:
At first, Crisafulli can hardly
believe his eyes.
256
00:19:45,940 --> 00:19:48,608
It was a prairie lupine, a
species that typically grows
257
00:19:48,676 --> 00:19:52,112
high in the slopes
of Mount St. Helens.
258
00:19:52,180 --> 00:19:56,750
NARRATOR:
It's not only growing,
it's flourishing.
259
00:19:56,818 --> 00:19:59,219
CRISAFULLI:
Not only had the plant
established,
260
00:19:59,287 --> 00:20:02,122
but at that point
was in full flower.
261
00:20:02,190 --> 00:20:04,024
And it was quite remarkable.
262
00:20:04,092 --> 00:20:06,460
When we saw the first one
we were very surprised.
263
00:20:08,429 --> 00:20:11,331
NARRATOR:
It's only four miles
from the volcano's crater.
264
00:20:11,399 --> 00:20:14,067
It's the first sign of life
265
00:20:14,135 --> 00:20:17,170
in an area where everything has
been extinguished.
266
00:20:21,309 --> 00:20:24,744
But how has the plant managed
to grow in such a barren area?
267
00:20:24,812 --> 00:20:27,948
The answer is a special
root structure
268
00:20:28,015 --> 00:20:30,817
that provides its own
fertilizer.
269
00:20:30,885 --> 00:20:35,489
These are little factories where
a bacterium works with the plant
270
00:20:35,556 --> 00:20:39,192
and provides nitrogen
to the plant.
271
00:20:39,260 --> 00:20:45,665
In return the plant provides
the bacterium with simple sugars
272
00:20:45,733 --> 00:20:48,368
that it fixes through
photosynthesis.
273
00:20:48,436 --> 00:20:50,370
And so this is a great
relationship
274
00:20:50,438 --> 00:20:52,606
where you scratch my back,
I'll scratch yours.
275
00:20:56,811 --> 00:20:59,513
NARRATOR:
This special process means
lupines can grow
276
00:20:59,580 --> 00:21:03,016
in even the most
inhospitable terrain.
277
00:21:03,084 --> 00:21:05,819
The lupine, like the gopher
Charlie found earlier,
278
00:21:05,887 --> 00:21:08,622
is a pioneering species.
279
00:21:08,689 --> 00:21:10,257
CRISAFULLI:
It's really important
280
00:21:10,324 --> 00:21:12,025
in landscapes
like Mount St. Helens,
281
00:21:12,093 --> 00:21:14,294
because the volcanic material
that fell on the ground
282
00:21:14,362 --> 00:21:16,730
tends to be really
nutrient poor.
283
00:21:21,202 --> 00:21:22,869
NARRATOR:
The conditions are difficult,
284
00:21:22,937 --> 00:21:26,940
but can the lupine pave the way
for other life to follow?
285
00:21:35,650 --> 00:21:39,452
NARRATOR:
In the spring, geologists also
return to the mountain.
286
00:21:39,520 --> 00:21:42,222
During the winter months,
287
00:21:42,290 --> 00:21:45,158
lava has continued to ooze out
of the crater floor.
288
00:21:49,197 --> 00:21:52,065
The lava dome has grown several
hundred feet taller
289
00:21:52,133 --> 00:21:55,535
and doubled in diameter.
290
00:21:58,472 --> 00:22:01,341
It's still a hazardous place.
291
00:22:01,409 --> 00:22:03,410
DZURISIN:
When I stepped out of
the helicopter in 1981
292
00:22:03,477 --> 00:22:05,278
on the crater floor,
293
00:22:05,346 --> 00:22:08,215
steam was actively rising
off the growing lava dome.
294
00:22:13,321 --> 00:22:15,388
There was still a tremendous
amount of noise.
295
00:22:18,826 --> 00:22:20,260
Rock falls were constant...
296
00:22:20,328 --> 00:22:24,464
and 2,000 feet above your head
297
00:22:24,532 --> 00:22:26,700
used to be where the summit
of the volcano was.
298
00:22:31,405 --> 00:22:33,740
You were now standing
in a crater with a lava dome
299
00:22:33,808 --> 00:22:35,709
that had not been there a few
months previously
300
00:22:35,776 --> 00:22:37,644
or a year previously.
301
00:22:37,712 --> 00:22:40,213
It was actively steaming.
302
00:22:40,281 --> 00:22:44,884
That was a very...
very exciting thought.
303
00:22:47,054 --> 00:22:50,390
NARRATOR:
It's a rare opportunity to watch
the process of dome building
304
00:22:50,458 --> 00:22:52,525
unfold in front of their eyes.
305
00:22:56,530 --> 00:22:59,065
The geologists set up
instruments to monitor
306
00:22:59,133 --> 00:23:01,434
what's going on,
307
00:23:01,502 --> 00:23:05,772
including seismometers that can
detect tremors set off by lava
308
00:23:05,840 --> 00:23:09,409
as it forces its way
through the rocks.
309
00:23:09,477 --> 00:23:13,480
They place a series of these
as close to the lava dome
310
00:23:13,547 --> 00:23:15,782
as possible.
311
00:23:19,520 --> 00:23:21,688
(birds chirping)
312
00:23:21,756 --> 00:23:24,090
At the Cascades Volcano
Observatory
313
00:23:24,158 --> 00:23:28,495
in southern Washington,
the seismic data pours in.
314
00:23:31,332 --> 00:23:34,668
DZURISIN:
The seismic record like this
315
00:23:34,735 --> 00:23:36,803
records any vibration
of the ground...
316
00:23:39,373 --> 00:23:42,742
so we can see real
rock-breaking earthquakes,
317
00:23:42,810 --> 00:23:44,010
we can see rock falls.
318
00:23:44,078 --> 00:23:45,745
(rumbling)
319
00:23:48,382 --> 00:23:49,749
It's our job to try
to understand
320
00:23:49,817 --> 00:23:51,084
what all those signals mean
321
00:23:51,152 --> 00:23:54,287
in terms of what
the volcano might do.
322
00:23:54,355 --> 00:23:57,590
NARRATOR:
The first traces reflect
extreme activity.
323
00:23:59,794 --> 00:24:01,828
DZURISIN:
Here you see the record
is almost continuous--
324
00:24:01,896 --> 00:24:04,497
one earthquake after the other--
bang, bang, bang.
325
00:24:07,101 --> 00:24:08,968
The seismic signal is
essentially continuous.
326
00:24:14,275 --> 00:24:16,710
NARRATOR:
The lava is breaking
through rocks
327
00:24:16,777 --> 00:24:18,912
and flowing across
the crater floor.
328
00:24:22,616 --> 00:24:27,220
Then, the seismic record reveals
a cyclical pattern.
329
00:24:33,661 --> 00:24:35,795
For periods of weeks to months,
330
00:24:35,863 --> 00:24:39,399
earthquake activity in the
crater would be pretty quiet.
331
00:24:39,467 --> 00:24:43,136
NARRATOR:
The lava is no longer flowing.
332
00:24:43,204 --> 00:24:45,972
DZURISIN:
And then a few days later, we
might see a pattern like this,
333
00:24:46,040 --> 00:24:48,742
more and more of these
very sharp earthquakes.
334
00:24:50,411 --> 00:24:53,513
NARRATOR:
It's the sign of lava
on the move again,
335
00:24:53,581 --> 00:24:55,782
forcing its way
through the round.
336
00:25:01,889 --> 00:25:04,858
DZURISIN:
Eventually lava would make it
on to the surface,
337
00:25:04,925 --> 00:25:06,726
maybe in just a couple of days,
338
00:25:06,794 --> 00:25:09,462
and we're seeing a continuous
record of ground shaking,
339
00:25:09,530 --> 00:25:10,697
both earthquakes and rock falls.
340
00:25:20,608 --> 00:25:24,010
Then, after a period
of dome growth
341
00:25:24,078 --> 00:25:31,384
that might last a few days or a
few weeks, it goes quiet again.
342
00:25:31,452 --> 00:25:35,588
That episode has ended and
the pattern begins itself over.
343
00:25:38,926 --> 00:25:41,694
NARRATOR:
This cycle of dome building
continues
344
00:25:41,762 --> 00:25:43,463
for the next five years.
345
00:25:46,667 --> 00:25:49,869
The pattern is so regular
that when the cycle begins,
346
00:25:49,937 --> 00:25:52,205
the scientists can accurately
predict
347
00:25:52,273 --> 00:25:54,674
what the volcano will do next.
348
00:25:57,278 --> 00:25:59,646
When the first rock-breaking
earthquakes occur,
349
00:25:59,713 --> 00:26:02,482
they know it's only a matter
of days or weeks
350
00:26:02,550 --> 00:26:06,119
before the lava starts
to flow again.
351
00:26:06,187 --> 00:26:10,857
At one point the dome reaches
nearly 1,000 feet--
352
00:26:10,925 --> 00:26:13,660
almost as high as
the Empire State Building.
353
00:26:16,163 --> 00:26:23,570
Then, in late 1986,
the seismographs go quiet.
354
00:26:32,546 --> 00:26:33,780
DZURISIN:
It was pretty clear
355
00:26:33,848 --> 00:26:36,749
that that period of dome
building had ended.
356
00:26:36,817 --> 00:26:39,686
NARRATOR:
But for how long?
357
00:26:39,753 --> 00:26:42,288
Has the mountain gone
back to sleep?
358
00:26:42,356 --> 00:26:45,558
JON MAJOR:
It wasn't clear whether the
mountain had gone back to sleep
359
00:26:45,626 --> 00:26:47,060
now for centuries
360
00:26:47,127 --> 00:26:50,029
or whether it was going
to just go back to sleep
361
00:26:50,097 --> 00:26:51,331
for a couple of years.
362
00:26:53,267 --> 00:26:55,735
NARRATOR:
It seems the pattern
has changed.
363
00:26:58,339 --> 00:27:00,907
For six years the scientists
have been able to predict
364
00:27:00,975 --> 00:27:02,976
what the mountain will do next.
365
00:27:05,513 --> 00:27:12,452
Now they are back to guessing
if and when it will erupt again.
366
00:27:18,959 --> 00:27:22,495
But even if the volcano
has gone to sleep,
367
00:27:22,563 --> 00:27:25,465
the wildlife continues
to bounce back.
368
00:27:30,905 --> 00:27:33,973
More and more gophers
are spreading across
369
00:27:34,041 --> 00:27:36,142
the blow-down zone.
370
00:27:38,779 --> 00:27:41,814
Lupines are colonizing
the pumice plain.
371
00:27:44,451 --> 00:27:48,922
And what's happening
at Spirit Lake is remarkable.
372
00:27:52,927 --> 00:27:56,596
The May 1980 eruption
obliterated all visible life
373
00:27:56,664 --> 00:27:57,830
in the lake.
374
00:27:57,898 --> 00:28:01,868
The surface was smothered
in a blanket of debris.
375
00:28:03,671 --> 00:28:07,574
In the murky water there was
an explosion of bacteria.
376
00:28:10,277 --> 00:28:12,245
CRISAFULLI:
There were a couple of species
of pneumonia
377
00:28:12,313 --> 00:28:13,513
that were described,
378
00:28:13,581 --> 00:28:15,181
and also the disease...
379
00:28:15,249 --> 00:28:17,383
the bacteria that causes
Legionnaires Disease,
380
00:28:17,451 --> 00:28:19,018
legionella.
381
00:28:19,086 --> 00:28:21,654
And so, many of us working
in the lakes in the early days
382
00:28:21,722 --> 00:28:22,855
came down with a fever.
383
00:28:24,858 --> 00:28:28,328
NARRATOR:
The bacteria rapidly consumed
the oxygen,
384
00:28:28,395 --> 00:28:31,831
making life impossible for
any air-breathing organisms,
385
00:28:31,899 --> 00:28:35,602
including fish, amphibians
and insects.
386
00:28:41,375 --> 00:28:43,209
We said it's going to be
decades and decades
387
00:28:43,277 --> 00:28:45,979
before this resembles anything
like a typical lake
388
00:28:46,046 --> 00:28:48,715
in the Cascade Mountain Range.
389
00:28:48,782 --> 00:28:50,516
Well, we were surprised,
390
00:28:50,584 --> 00:28:52,085
because that's not exactly
what happened.
391
00:28:56,857 --> 00:29:00,493
NARRATOR:
Scientists begin
routine water sampling.
392
00:29:05,432 --> 00:29:09,502
It's a unique opportunity to see
if and when life will return
393
00:29:09,570 --> 00:29:11,437
from the dead.
394
00:29:15,075 --> 00:29:18,044
At first there's nothing.
395
00:29:18,112 --> 00:29:24,350
But as the debris settles,
the water clears.
396
00:29:24,418 --> 00:29:27,220
Light levels improve.
397
00:29:27,287 --> 00:29:31,391
Then, three years
after the eruption,
398
00:29:31,458 --> 00:29:35,061
there's a crucial discovery...
399
00:29:35,129 --> 00:29:38,798
microscopic plants.
400
00:29:40,734 --> 00:29:46,572
They're phytoplankton-- plants
that turn sunlight into oxygen.
401
00:29:50,077 --> 00:29:54,213
They've been brought in by birds
or blown in by the wind.
402
00:29:54,281 --> 00:29:58,885
They are the basic building
block of aquatic life.
403
00:30:01,588 --> 00:30:03,656
Over the following months,
404
00:30:03,724 --> 00:30:05,625
as light levels continue
to improve,
405
00:30:05,693 --> 00:30:08,695
the plankton population grows.
406
00:30:08,762 --> 00:30:12,065
CRISAFULLI:
In fact, between 1983 and 1986,
407
00:30:12,132 --> 00:30:15,702
135 different species
of these tiny plants
408
00:30:15,769 --> 00:30:18,371
had colonized the lake.
409
00:30:18,439 --> 00:30:23,976
They provide the oxygen and
also the prey for the food web.
410
00:30:24,044 --> 00:30:27,780
NARRATOR:
Sunlight, oxygen and food.
411
00:30:27,848 --> 00:30:31,150
Several years after
its complete destruction,
412
00:30:31,218 --> 00:30:35,421
Spirit Lake is coming
back to life.
413
00:30:41,328 --> 00:30:45,131
Four miles away,
the volcano remains quiet.
414
00:30:45,199 --> 00:30:49,368
The lava dome has stopped
growing.
415
00:30:49,436 --> 00:30:53,239
Many geologists think
the show is over,
416
00:30:53,307 --> 00:30:56,142
at least in their lifetime.
417
00:30:56,210 --> 00:30:59,579
We had the feeling that we had
probably seen our last eruption
418
00:30:59,646 --> 00:31:01,214
of Mount St. Helens.
419
00:31:01,281 --> 00:31:03,850
We knew there was a chance
it would erupt again.
420
00:31:03,917 --> 00:31:06,919
But none of us were
betting on it.
421
00:31:06,987 --> 00:31:11,724
NARRATOR:
As the mountain sleeps,
wildlife bounces back...
422
00:31:14,728 --> 00:31:17,697
even in the most
unexpected places.
423
00:31:17,765 --> 00:31:20,066
In one of the most devastated
areas of the mountain--
424
00:31:20,134 --> 00:31:24,170
the pumice plain--
a gopher is seen.
425
00:31:28,075 --> 00:31:29,909
It's surviving by eating lupine.
426
00:31:36,350 --> 00:31:38,184
Lupines provide the food.
427
00:31:38,252 --> 00:31:40,052
Gophers enrich the pumice
428
00:31:40,120 --> 00:31:42,655
by burrowing their way
through the ash.
429
00:31:42,723 --> 00:31:48,561
They mix in fresh soil and
help new plants to spread.
430
00:31:58,105 --> 00:32:01,207
CRISAFULLI:
When you walked around the
landscape, it was those islands
431
00:32:01,275 --> 00:32:03,743
created by gopher-turned soils
that were very green
432
00:32:03,811 --> 00:32:05,645
and full of flower and seeds.
433
00:32:07,714 --> 00:32:13,085
NARRATOR:
The gophers also play another
role in helping wildlife spread.
434
00:32:13,153 --> 00:32:17,657
Crisafulli finds a salamander
in a gopher's tunnel.
435
00:32:17,724 --> 00:32:20,626
CRISAFULLI:
What's interesting about
the gopher is they create
436
00:32:20,694 --> 00:32:22,862
kilometers of underground
tunnel systems.
437
00:32:25,332 --> 00:32:27,667
NARRATOR:
Elk are returning
to the area,
438
00:32:27,734 --> 00:32:32,438
helping to expand this amazing
web of life.
439
00:32:38,979 --> 00:32:41,147
CRISAFULLI:
When elk move across
the landscape,
440
00:32:41,215 --> 00:32:45,251
they collapse the tunnels,
creating entranceways
441
00:32:45,319 --> 00:32:48,421
that salamanders and other
amphibians can get access to.
442
00:32:48,488 --> 00:32:50,923
And once they get beneath
the ground,
443
00:32:50,991 --> 00:32:53,092
these are very cool and moist
sites that enable them
444
00:32:53,160 --> 00:32:55,494
to survive in an otherwise
inhospitable area.
445
00:32:58,432 --> 00:33:01,100
And the importance of that
is that it allows them to use
446
00:33:01,168 --> 00:33:04,303
these underground burrows
as stepping stones
447
00:33:04,371 --> 00:33:06,873
during hot, dry weather and
eventually to colonize
448
00:33:06,940 --> 00:33:09,475
new patches of terrestrial
habitat
449
00:33:09,543 --> 00:33:11,711
as well as ponds and lakes.
450
00:33:13,847 --> 00:33:15,181
(frog croaking)
451
00:33:21,288 --> 00:33:25,458
NARRATOR:
Spirit Lake now teems
with amphibians.
452
00:33:28,929 --> 00:33:33,633
Fish, brought to the lake
by fishermen, are thriving,
453
00:33:33,700 --> 00:33:35,801
a clear indication
that the water quality
454
00:33:35,869 --> 00:33:38,037
is returning to normal.
455
00:33:38,105 --> 00:33:41,340
CRISAFULLI:
What's happened with the fish
was actually remarkable.
456
00:33:41,408 --> 00:33:42,909
While we don't have
a good handle
457
00:33:42,976 --> 00:33:45,711
on the total number of fish,
we know from our snorkeling
458
00:33:45,779 --> 00:33:49,415
and surveys that
the population is enormous.
459
00:33:55,689 --> 00:33:57,690
NARRATOR:
Spirit Lake is beginning
to resemble
460
00:33:57,758 --> 00:34:00,726
a typical mountain lake.
461
00:34:00,794 --> 00:34:04,697
Just over a decade
after the eruption,
462
00:34:04,765 --> 00:34:09,735
life is flooding back to
the slopes of Mount St. Helens.
463
00:34:09,803 --> 00:34:11,704
The rate of recovery
is far faster
464
00:34:11,772 --> 00:34:14,307
than anybody had expected.
465
00:34:14,374 --> 00:34:19,078
CRISAFULLI:
Clearly our understanding of
the ability of these organisms
466
00:34:19,146 --> 00:34:23,582
to disperse was greatly
underappreciated.
467
00:34:23,650 --> 00:34:25,618
We found a lot of our
conventional wisdom
468
00:34:25,686 --> 00:34:27,353
was just flat wrong.
469
00:34:27,421 --> 00:34:29,522
(birds chirping)
470
00:34:33,060 --> 00:34:37,430
NARRATOR:
Then, as life recovers,
new threats emerge.
471
00:34:40,367 --> 00:34:42,668
In September 2004,
472
00:34:42,736 --> 00:34:45,237
the seismographs at the Cascades
Volcano Observatory
473
00:34:45,305 --> 00:34:48,307
pick up a new series
of tremors
474
00:34:48,375 --> 00:34:50,910
deep below Mount St. Helens.
475
00:34:50,978 --> 00:34:53,846
The volcano has woken up.
476
00:34:55,949 --> 00:34:59,785
John Pallister takes a
helicopter to investigate.
477
00:34:59,853 --> 00:35:02,855
PALLISTER:
You could see the absolute
beginning of the eruptions,
478
00:35:02,923 --> 00:35:05,424
unusual-- really unusual--
to just happen to be there,
479
00:35:05,492 --> 00:35:06,592
in a helicopter,
480
00:35:06,660 --> 00:35:09,328
the crater rim,
on the upwind side,
481
00:35:09,396 --> 00:35:11,931
so the plume was going away
from us.
482
00:35:11,999 --> 00:35:17,036
NARRATOR:
Pallister has no idea how big
this eruption will be.
483
00:35:17,104 --> 00:35:20,406
PALLISTER:
We saw the boiling material
come out of the ground.
484
00:35:20,474 --> 00:35:22,842
We saw that it was blasting up.
485
00:35:22,909 --> 00:35:25,411
It was dark ash coming out
and light steam coming out
486
00:35:25,479 --> 00:35:26,912
at the same time.
487
00:35:30,584 --> 00:35:33,753
It made a plume that rose up
over the rim of the caldera
488
00:35:33,820 --> 00:35:36,155
and drifted downwind.
489
00:35:36,223 --> 00:35:38,357
NARRATOR:
The speed and suddenness
of the eruption
490
00:35:38,425 --> 00:35:41,327
catches everybody by surprise.
491
00:35:41,395 --> 00:35:44,163
The volcano went from quiet
to unrest to eruption
492
00:35:44,231 --> 00:35:45,765
very, very rapidly.
493
00:35:45,832 --> 00:35:48,567
(explosions)
494
00:35:56,009 --> 00:35:58,544
NARRATOR:
During the next two weeks,
there are three more eruptions
495
00:35:58,612 --> 00:36:01,313
of steam and ash.
496
00:36:01,381 --> 00:36:04,417
No one knows what will
happen next.
497
00:36:04,484 --> 00:36:05,918
DZURISIN:
It seemed possible
498
00:36:05,986 --> 00:36:09,221
that we were headed toward
an explosive eruption.
499
00:36:09,289 --> 00:36:10,623
We didn't know.
500
00:36:10,690 --> 00:36:12,324
That was a key question.
501
00:36:14,261 --> 00:36:18,364
NARRATOR:
Then, after 14 days,
the seismographs quiet down.
502
00:36:22,702 --> 00:36:27,339
Almost as quickly as it started,
the eruption stops.
503
00:36:32,746 --> 00:36:34,580
But then something strange
happens.
504
00:36:38,018 --> 00:36:40,286
Over the next few weeks,
the seismographs pick up
505
00:36:40,353 --> 00:36:42,154
a new pattern of tremors
506
00:36:42,222 --> 00:36:44,557
the geologists have never
seen before.
507
00:36:52,365 --> 00:36:55,134
Could they be linked
to a gigantic lump of lava
508
00:36:55,202 --> 00:36:56,802
growing out of the crater floor?
509
00:36:59,840 --> 00:37:04,477
PALLISTER:
It was a huge kind
of recumbent spine,
510
00:37:04,544 --> 00:37:07,546
this big mass lying
in the crater floor
511
00:37:07,614 --> 00:37:09,648
some 300 meters or so high.
512
00:37:09,716 --> 00:37:14,887
NARRATOR:
The spine of lava is as long
as the Eiffel Tower.
513
00:37:14,955 --> 00:37:18,090
MAJOR:
Everybody was just awestruck.
514
00:37:18,158 --> 00:37:20,960
To have this large spine just
shoving up out of the ground
515
00:37:21,027 --> 00:37:23,295
was completely different
and outside the experience
516
00:37:23,363 --> 00:37:25,131
of any of us here in the staff.
517
00:37:28,235 --> 00:37:34,273
NARRATOR:
Despite the risk, John Pallister
goes in to take samples.
518
00:37:34,341 --> 00:37:36,342
PALLISTER:
We landed right next to it.
519
00:37:39,746 --> 00:37:42,281
And I was able to get out,
helicopter helmet on,
520
00:37:42,349 --> 00:37:45,184
rapidly run up to the edge
of the spine.
521
00:37:45,252 --> 00:37:48,687
NARRATOR:
It's an unbelievable sight.
522
00:37:51,391 --> 00:37:56,695
DZURISIN:
Had someone suggested to me
that we make a movie
523
00:37:56,763 --> 00:38:00,132
of a lava dome growing that way,
I think I would have said
524
00:38:00,200 --> 00:38:02,301
it's a little too fantastic,
let's make it more realistic.
525
00:38:07,641 --> 00:38:09,341
NARRATOR:
At the observatory,
526
00:38:09,409 --> 00:38:11,377
where geologists
have been puzzling over
527
00:38:11,444 --> 00:38:18,784
the strange seismic traces,
they now realize what they are.
528
00:38:18,852 --> 00:38:22,054
They're the unique autograph
of the giant spines
529
00:38:22,122 --> 00:38:24,990
as they push their way
out of the ground.
530
00:38:30,297 --> 00:38:34,300
DZURISIN:
This is the seismic signature
of solid blocks of rock
531
00:38:34,367 --> 00:38:36,502
grinding their way
through the volcano,
532
00:38:36,570 --> 00:38:40,206
coming out onto the surface.
533
00:38:40,273 --> 00:38:44,410
As they do, they make these
small seismic signals,
534
00:38:44,477 --> 00:38:48,514
one just like the other, just
like the other, very repetitive.
535
00:38:48,582 --> 00:38:51,984
We came to call them
"drumbeats."
536
00:38:52,052 --> 00:38:55,521
NARRATOR:
The drumbeats continue
for several years.
537
00:38:55,589 --> 00:39:01,594
Spine after spine of solid lava
emerges from the crater floor.
538
00:39:01,661 --> 00:39:06,165
It's unlike anything geologists
have seen on Mount St. Helens.
539
00:39:06,233 --> 00:39:08,500
PALLISTER:
Now, spine doesn't do justice
to these things.
540
00:39:08,568 --> 00:39:10,135
These things were
like skyscrapers
541
00:39:10,203 --> 00:39:11,737
that were being shoved out
of the ground.
542
00:39:11,805 --> 00:39:12,871
They were literally that big.
543
00:39:15,041 --> 00:39:19,178
NARRATOR:
Sometimes the blocks grow
at a rate of 16 feet a day.
544
00:39:22,148 --> 00:39:24,550
Then they collapse.
545
00:39:28,154 --> 00:39:31,190
Seen through a time-lapse
camera,
546
00:39:31,258 --> 00:39:34,059
one solid lump of lava
after another
547
00:39:34,127 --> 00:39:36,495
pushes up through
the crater floor.
548
00:39:40,333 --> 00:39:42,534
The process is mystifying.
549
00:39:42,602 --> 00:39:45,904
What do the spines mean?
550
00:39:45,972 --> 00:39:49,041
Why was the eruption in 2004
so different
551
00:39:49,109 --> 00:39:51,076
than the style of eruption
in the 1980s?
552
00:39:53,480 --> 00:39:57,149
Why in the 1980s did you have
this more fluid lava
553
00:39:57,217 --> 00:40:00,653
that created the sort of short,
stubby lava flows
554
00:40:00,720 --> 00:40:02,388
that came out and built
the lava dome?
555
00:40:05,659 --> 00:40:08,427
Whereas in 2004, you basically
had solid rock being pushed up
556
00:40:08,495 --> 00:40:10,029
in the ground.
557
00:40:10,096 --> 00:40:12,865
NARRATOR:
There's one urgent question.
558
00:40:12,932 --> 00:40:16,969
Is the volcano building up
to another major eruption?
559
00:40:17,037 --> 00:40:20,472
MAJOR:
Trying to make sense of what was
going on was a challenge.
560
00:40:20,540 --> 00:40:23,275
Trying to understand how the
eruption was going to progress
561
00:40:23,343 --> 00:40:25,511
was a challenge.
562
00:40:25,578 --> 00:40:27,579
We had lots of discussions
about whether or not
563
00:40:27,647 --> 00:40:29,581
it was going to be
an explosive eruption,
564
00:40:29,649 --> 00:40:31,550
whether it was going to be
another dome building eruption.
565
00:40:36,156 --> 00:40:39,625
NARRATOR:
There is one way to find out.
566
00:40:39,693 --> 00:40:43,362
Analyzing samples of the lava
might explain
567
00:40:43,430 --> 00:40:48,867
the mysterious solid blocks and
what they mean for the future.
568
00:40:54,341 --> 00:40:58,544
At the volcano observatory,
John Pallister compares lava
569
00:40:58,611 --> 00:41:02,648
from the spines with samples
taken from previous eruptions.
570
00:41:05,051 --> 00:41:07,152
Could there be something
in their composition
571
00:41:07,220 --> 00:41:11,590
that explains why the mountain
sometimes pushes up spines...
572
00:41:13,827 --> 00:41:17,262
sometimes oozes lava...
573
00:41:19,933 --> 00:41:23,369
and sometimes explodes?
574
00:41:23,436 --> 00:41:25,404
(rumbling)
575
00:41:29,542 --> 00:41:32,144
Pallister begins with
a sample of the lava
576
00:41:32,212 --> 00:41:35,748
that erupted so explosively
in May 1980.
577
00:41:35,815 --> 00:41:40,386
He's immediately struck
by the large areas of blue.
578
00:41:40,453 --> 00:41:44,223
PALLISTER:
Okay, so what's important
about this 1980 rock
579
00:41:44,290 --> 00:41:49,094
is the abundance
of this blue area, which...
580
00:41:49,162 --> 00:41:51,330
and that's basically bubbles.
581
00:41:51,398 --> 00:41:53,732
Now, that's not a mineral;
582
00:41:53,800 --> 00:41:55,768
that's just open space
in the thin section.
583
00:41:55,835 --> 00:41:57,369
That's where gas bubbles were.
584
00:41:57,437 --> 00:42:00,406
This sample would float in
water, it had so much gas in it.
585
00:42:02,409 --> 00:42:07,112
NARRATOR:
The gas comes from water,
a component of the magma.
586
00:42:07,180 --> 00:42:08,947
As magma rises,
587
00:42:09,015 --> 00:42:12,618
changes in pressure turn
the water into gas.
588
00:42:12,685 --> 00:42:15,554
The gas pressurizes the magma.
589
00:42:15,622 --> 00:42:19,591
It's what gives volcanoes
their explosive force.
590
00:42:19,659 --> 00:42:22,027
(explosions)
591
00:42:22,228 --> 00:42:25,130
PALLISTER:
1980 had a lot of gas in it.
592
00:42:25,198 --> 00:42:27,032
So it exploded,
tore itself apart
593
00:42:27,100 --> 00:42:29,368
in a tremendous explosive
eruption.
594
00:42:36,776 --> 00:42:40,679
NARRATOR:
But when he looks at lava taken
from the 1983 period
595
00:42:40,747 --> 00:42:43,916
of dome building,
it's different.
596
00:42:46,753 --> 00:42:50,322
PALLISTER: There is much less
of this open space,
597
00:42:50,390 --> 00:42:54,059
of the gas filling space
in the rock.
598
00:42:54,127 --> 00:42:59,998
NARRATOR:
The 1983 lava behaves like
a bottle of soda going flat.
599
00:43:02,936 --> 00:43:05,204
Finally he looks at
a sample of lava
600
00:43:05,271 --> 00:43:08,407
from one of the spines in 2005.
601
00:43:08,475 --> 00:43:10,509
PALLISTER:
I don't see any blue space,
602
00:43:10,577 --> 00:43:12,344
any of that--
oh, there's just a little bit--
603
00:43:12,412 --> 00:43:16,615
but dominantly it is...
it is lacking in space.
604
00:43:16,683 --> 00:43:21,286
It's a gas-poor magma...
in fact almost none.
605
00:43:24,190 --> 00:43:27,893
NARRATOR:
There's just enough gas
to push it to the surface.
606
00:43:27,961 --> 00:43:31,096
But by the time it gets there,
there's nothing left.
607
00:43:31,164 --> 00:43:32,865
PALLISTER:
So this one came up slow
608
00:43:32,932 --> 00:43:37,936
and it made sticky, solidified
spines instead of making
609
00:43:38,004 --> 00:43:39,938
either lava flows or
an explosive eruption.
610
00:43:43,076 --> 00:43:45,043
NARRATOR:
It's a crucial insight.
611
00:43:45,111 --> 00:43:47,679
The amount of gas determines
the nature of the lava
612
00:43:47,747 --> 00:43:50,549
and the force of the eruption.
613
00:43:50,617 --> 00:43:56,021
PALLISTER:
It all comes down to the gas
budget for the eruption.
614
00:43:56,089 --> 00:44:00,893
Is it going to fizzle
or is it going to explode?
615
00:44:02,695 --> 00:44:06,832
NARRATOR:
Suddenly the mountain's behavior
makes sense.
616
00:44:06,900 --> 00:44:10,068
The spines are a sign the magma
under Mount St. Helens
617
00:44:10,136 --> 00:44:13,572
is running low on gas.
618
00:44:13,640 --> 00:44:19,945
Then, in 2007, as if to confirm
this new insight,
619
00:44:20,013 --> 00:44:26,018
the familiar drumbeat
seismic traces...
620
00:44:26,085 --> 00:44:27,819
vanish completely.
621
00:44:30,757 --> 00:44:34,159
No more spines appear.
622
00:44:34,227 --> 00:44:39,565
The lava below the mountain
has finally run out of gas.
623
00:44:45,004 --> 00:44:47,239
How long will it take
the mountain to build up
624
00:44:47,307 --> 00:44:50,208
enough gas pressure
for another eruption?
625
00:44:54,681 --> 00:44:56,048
I think that's the most
important question
626
00:44:56,115 --> 00:44:57,616
we have to answer.
627
00:44:57,684 --> 00:45:00,719
How long does it take to build
up the gas necessary
628
00:45:00,787 --> 00:45:02,821
to drive an explosive eruption?
629
00:45:02,889 --> 00:45:07,159
NARRATOR:
That's now the question
they need to answer.
630
00:45:16,703 --> 00:45:20,405
Geologists go back to the
mountain to look for clues.
631
00:45:25,178 --> 00:45:30,048
The eruption in 1980 took
the top off Mount St. Helens,
632
00:45:30,116 --> 00:45:34,019
leaving its history exposed in
the rock walls of the crater.
633
00:45:41,394 --> 00:45:43,929
Most of the important previous
eruptions are marked
634
00:45:43,997 --> 00:45:47,032
by different colored bands.
635
00:45:47,100 --> 00:45:49,568
The lower part of the walls
where you see gray
636
00:45:49,636 --> 00:45:53,738
and some yellows and some pinks
637
00:45:53,740 --> 00:45:56,942
are all part of the older
edifice of Mount St. Helens.
638
00:45:59,779 --> 00:46:03,782
NARRATOR:
These rocks, which make up the
bottom half of the rock face,
639
00:46:03,850 --> 00:46:06,952
are around 16,000 years old.
640
00:46:07,020 --> 00:46:10,656
MAJOR:
Then, if you look higher
on the wall, near the top,
641
00:46:10,723 --> 00:46:14,426
you see darker colors.
642
00:46:14,494 --> 00:46:16,261
And those are rocks
that began erupting
643
00:46:16,329 --> 00:46:20,065
about 3,000 to 2,500 years ago.
644
00:46:25,038 --> 00:46:27,239
So, by looking at what we call
the stratigraphy
645
00:46:27,241 --> 00:46:29,941
in this magnificent exposure
of the rock types
646
00:46:30,009 --> 00:46:33,812
in the crater walls, we can
piece back the puzzle
647
00:46:33,880 --> 00:46:36,648
and understand the history
as far as eruptive activity
648
00:46:36,716 --> 00:46:39,217
of Mount St. Helens.
649
00:46:39,285 --> 00:46:43,722
NARRATOR:
Do the rocks give any indication
how long it takes to build up
650
00:46:43,790 --> 00:46:46,358
enough gas between eruptions
651
00:46:46,426 --> 00:46:48,860
for the sleepy mountain
to awake again?
652
00:46:55,802 --> 00:46:58,437
John Pallister sorts
and categorizes rocks
653
00:46:58,504 --> 00:47:02,274
from earlier eruptions.
654
00:47:02,341 --> 00:47:06,244
He checks notes and photos
to try and determine
655
00:47:06,312 --> 00:47:10,582
how often the mountain has
erupted violently.
656
00:47:10,650 --> 00:47:12,517
Drawing on previous records,
657
00:47:12,585 --> 00:47:16,621
he builds up a picture
of Mount St. Helens' past.
658
00:47:16,689 --> 00:47:19,357
For much of the last
4,000 years,
659
00:47:19,425 --> 00:47:22,928
there seems to be
a fairly clear pattern.
660
00:47:22,995 --> 00:47:24,963
If we look at the number
of big eruptions
661
00:47:25,031 --> 00:47:27,566
over the length of time
the volcano's been active,
662
00:47:27,633 --> 00:47:29,868
you might say that there's one
roughly every thousand years,
663
00:47:29,936 --> 00:47:31,436
a big eruption.
664
00:47:31,504 --> 00:47:34,306
So from our context here
we could say
665
00:47:34,373 --> 00:47:36,508
that it takes on the order
of a thousand years
666
00:47:36,576 --> 00:47:39,177
to build up enough gas
to get a really large eruption.
667
00:47:43,149 --> 00:47:48,386
NARRATOR:
The record suggests some of
these eruptions have been huge,
668
00:47:48,454 --> 00:47:53,558
more than ten times
larger than 1980,
669
00:47:53,626 --> 00:47:59,765
potentially enveloping vast
areas of Washington and Oregon.
670
00:47:59,832 --> 00:48:02,968
But that would imply that the
next really big one isn't due
671
00:48:03,035 --> 00:48:04,936
for about another century.
672
00:48:08,040 --> 00:48:12,210
Except for one little detail
around 500 years ago.
673
00:48:14,347 --> 00:48:17,215
PALLISTER:
In 1479 A.D. and 1482
674
00:48:17,283 --> 00:48:18,517
there were two very large
eruptions.
675
00:48:18,584 --> 00:48:20,986
(explosions)
676
00:48:25,391 --> 00:48:28,960
So the volcano is capable
of surprising us and producing
677
00:48:29,028 --> 00:48:30,362
two highly explosive eruptions
678
00:48:30,429 --> 00:48:32,130
in a span of less than
three years.
679
00:48:32,198 --> 00:48:37,736
NARRATOR:
Both these eruptions were
much bigger than May 1980.
680
00:48:37,804 --> 00:48:40,338
There is no straightforward
pattern.
681
00:48:42,608 --> 00:48:45,343
Mount St. Helens can pause
for a thousand years
682
00:48:45,411 --> 00:48:50,615
between big explosive eruptions,
or it can pause for three.
683
00:48:53,319 --> 00:48:56,521
These results have left
geologists with one certainty
684
00:48:56,589 --> 00:48:58,657
and a number of questions.
685
00:49:00,359 --> 00:49:02,994
First of all, we expect
this volcano to erupt again
686
00:49:03,062 --> 00:49:04,629
as repeatedly in the past;
687
00:49:04,697 --> 00:49:07,065
there's no reason to think
it's gone to sleep forever now.
688
00:49:09,869 --> 00:49:12,370
NARRATOR:
There will be another eruption,
689
00:49:12,438 --> 00:49:18,944
but nobody can determine when
or just how big it will be.
690
00:49:19,011 --> 00:49:22,614
PALLISTER:
We don't know whether it's going
to erupt explosively again
691
00:49:22,682 --> 00:49:26,885
n two years or in 20 years
or in 200 years.
692
00:49:26,953 --> 00:49:30,655
That's an area that needs
a lot more work,
693
00:49:30,723 --> 00:49:32,357
a lot more research
to understand
694
00:49:32,425 --> 00:49:35,794
and it is of fundamental
importance to being able
695
00:49:35,862 --> 00:49:38,063
to forecast and to save lives
and to save property.
696
00:49:47,473 --> 00:49:49,708
(bird screeches)
697
00:49:53,880 --> 00:49:57,282
NARRATOR:
For 30 years, Mount St. Helens
has led scientists
698
00:49:57,350 --> 00:50:01,519
on an extraordinary journey
of surprise and discovery.
699
00:50:01,587 --> 00:50:06,591
When they surveyed the
destruction in the early 1980s,
700
00:50:06,659 --> 00:50:09,261
nobody could have predicted
the speed with which
701
00:50:09,328 --> 00:50:11,730
life has returned.
702
00:50:11,797 --> 00:50:13,665
CRISAFULLI:
It was another form
of an eruption,
703
00:50:13,733 --> 00:50:16,468
it was an eruption of nature.
704
00:50:16,535 --> 00:50:18,370
Nature marched back
with a vengeance.
705
00:50:21,540 --> 00:50:25,844
NARRATOR:
Mount St. Helens has revealed
a rich and complex web of life
706
00:50:25,912 --> 00:50:29,281
that has never been
documented before.
707
00:50:29,348 --> 00:50:32,384
Today the slopes of the mountain
are a living testimony
708
00:50:32,451 --> 00:50:38,623
to the miraculous ability of
nature to return from the dead.
709
00:50:38,691 --> 00:50:40,992
CRISAFULLI:
Each time you would
come out here
710
00:50:41,060 --> 00:50:43,728
and there would be a surprise,
something would be unveiled,
711
00:50:43,796 --> 00:50:45,897
something that you hadn't
seen before.
712
00:50:45,965 --> 00:50:47,966
Perhaps it would be
a new species of spider
713
00:50:48,034 --> 00:50:49,267
or a new species of beetle.
714
00:50:54,540 --> 00:50:56,741
Nature is very resilient,
715
00:50:56,809 --> 00:50:58,610
and that is the take-home
message from 30 years
716
00:50:58,678 --> 00:51:01,813
of ecological work on
the Mount St. Helens volcano.
717
00:51:07,219 --> 00:51:12,991
NARRATOR:
But as nature bounces back, the
mountain still broods overhead.
718
00:51:15,127 --> 00:51:18,430
It's like a ticking time bomb
waiting to destroy life
719
00:51:18,497 --> 00:51:22,267
all over again.
720
00:51:22,335 --> 00:51:24,536
MAJOR:
Based on the history
of this volcano,
721
00:51:24,603 --> 00:51:26,538
we know it's been
extremely active
722
00:51:26,605 --> 00:51:29,341
and it's not a matter of
whether, if it will erupt again,
723
00:51:29,408 --> 00:51:31,242
it's a matter of when
it will erupt again,
724
00:51:31,310 --> 00:51:35,146
when will it reactivate,
when will it reawaken.
725
00:51:35,214 --> 00:51:39,851
NARRATOR:
These are questions scientists
are still wrestling with.
726
00:51:39,919 --> 00:51:42,620
DZURISIN:
We have yet to find
a silver bullet,
727
00:51:42,688 --> 00:51:47,225
a magic thing that we can
measure that tells us
728
00:51:47,293 --> 00:51:49,227
when the volcano is going
to turn on.
729
00:51:50,529 --> 00:51:55,000
NARRATOR:
Mount St. Helens
will erupt again.
730
00:51:55,067 --> 00:52:00,905
The only questions are when and
how big that eruption will be.
731
00:52:28,234 --> 00:52:30,001
On NOVA's "Mount St. Helens"
Web site,
732
00:52:30,069 --> 00:52:32,904
go behind the scenes
with director Daniel Hissen.
733
00:52:32,972 --> 00:52:34,506
See stunning images
734
00:52:34,573 --> 00:52:37,509
of the landscape's remarkable
return to life, and more.
735
00:52:37,576 --> 00:52:39,110
Find it on pbs.org.
736
00:52:40,746 --> 00:52:43,515
Captioned by
Media Access Group at WGBH
access.wgbh.org
737
00:52:57,897 --> 00:53:02,567
This NOVA program is available
on DVD at shopPBS.org,
738
00:53:02,635 --> 00:53:05,870
or call 1-800-play-PBS.
67559
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