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(explosion)

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           NARRATOR:
 Mount St. Helens-- the biggest
       volcanic eruption

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        in North America
      in nearly a century.

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   Virtually all life for 200
   square miles is wiped out.

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 It seems impossible that life
       could ever return

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   to this barren wasteland.

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     We found a lot of our
      conventional wisdom

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     was just flat wrong.

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           NARRATOR:
        In recent years
    there are ominous signs

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   the volcano is awakening.

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MAN:
     These things were like
  skyscrapers that were being

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   shoved out of the ground.

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 They were literally that big.

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           NARRATOR:
 A 30-year quest to understand

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  one of the most complicated
     volcanoes in the world

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   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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  in two years or in 20 years
        or in 200 years.

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           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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Supporting NOVA and promotingg
public understanding of science.

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      And the Corporation
    for Public Broadcasting,

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  and by PBS viewers like you.

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           NARRATOR:
         October 2004.

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        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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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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      It came up to above
         our altitude,

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   to 10,000 or 12,000 feet.

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           NARRATOR:
It's a frightening development.

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          (explosion)

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  For years, Mount St. Helens
        has been quiet.

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The volcano went from quiet
     to unrest to eruption

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      very, very rapidly.

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           NARRATOR:
       It could be headed
    for a massive explosion.

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           DZURISIN:
       It seemed possible
      that we were headed

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 toward an explosive eruption.

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        We didn't know.

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    That was a key question.

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           NARRATOR:
    The effort to understand
       what is happening

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inside the mountain couldn't be
          more urgent.

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      Is the volcano about
to repeat the events

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 of three decades earlier, when
  it shattered the tranquility

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 of its peaceful surroundings?

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        (bird screeches)

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           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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  It's an area of outstanding
   beauty, rich in wildlife.

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      For over 120 years,
  the volcano has been quiet.

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      But in recent weeks
      it's been rumbling.

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 Nobody is sure what to expect.

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Then, on May 18, 1980,

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   a 5.1 magnitude earthquake
      rocks the mountain.

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      Within ten seconds,

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  the volcano's northern flank
           collapses

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    in the largest landslide
      in recorded history.

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It releases millions of tons of
 magma in a colossal explosion.

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A cloud of searing gas and rock,
  known as a pyroclastic flow,

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   races over the surrounding
          countryside.

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     Forests are flattened.

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  Four miles below the summit,

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an enormous lake is choked
          with debris.

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The eruption continues to shoot
    poisonous steam and ash

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      miles into the air.

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      It was just, again,
  astounding is the best word

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  to describe what happened in
 1980 here in Mount St. Helens.

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           NARRATOR:
     The northern slope of
     the mountain is buried

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    in several feet of ash.

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       Virtually all life
        is extinguished.

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      57 people are dead.

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 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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    for the rest of the day.

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     The drifting ash cloud
      disrupts air traffic

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     for hundreds of miles.

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  The scale of the destruction
          is enormous.

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           NARRATOR:
        Across more than
       200 square miles,

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   the surge of ash and rock
       incinerates trees.

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       Thousands of birds

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from more than a hundred species
           disappear.

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 Billions of insects are gone.

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  Deer and elk are wiped out.

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 This vast area of devastation
   becomes known as the blast

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       or blow-down zone.

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Nearer the crater, ash and rocks
       from the landslide

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   litter the northern slope
        of the mountain.

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    It looks like the moon.

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 It's called the pumice plain.

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It's directly below the crater.

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  Four miles from the volcano,

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    the enormous Spirit Lake
is scarcely recognizable.

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The avalanche has lifted its bed
      more than 200 feet.

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    The surface is smothered
         in dead trees.

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 Hundreds of species of aquatic
    life, including insects,

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amphibians and fish, are killed.

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      CHARLIE CRISAFULLI:
      It was black water.

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 And it de-gassed and bubbled,

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   and there were hot springs
      that were coming up.

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If you were to put your fingers

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  in to your wrist and wiggle
them, you wouldn't even be able

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to see your fingertips.

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  That's how grossly modified
         the water was.

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           NARRATOR:
    Mount St. Helens is now

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 a lifeless jumble of shattered
     forest, rock and ash.

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   It's hard to imagine life
       will ever return.

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 The eruption was so powerful,

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      it altered the shape
        of the mountain.

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 Mount St. Helens was a typical
      cone-shaped volcano

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   known as a stratovolcano.

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   But the landslide has torn
   1,300 feet off the summit,

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leaving a gaping crater
a mile wide and 2,000 feet deep.

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   It's the largest volcanic
   eruption in North America

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      in nearly a century.

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  (helicopter blades whirring)

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   Weeks after the eruption,
scientists arrive at the crater.

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 The volcano is still steaming
         and rumbling.

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It's a new and unfamiliar world.

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   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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       and you could see
that it was very hot.

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 You didn't see red lava oozing
       out of the ground.

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    You didn't see fantastic
        fire fountains.

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    There was this constant
    background roar of rocks

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cascading down the crater walls.

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 Occasionally a very large rock
   the size of the helicopter

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    would come bouncing down
     and you could watch it

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 and it was almost slow motion
because the crater was so large.

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           NARRATOR:
  Mount St. Helens has a long
history of eruptions.

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  More than 500 years ago, two
 massive explosions took place

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within two years of each other.

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  They were nearly four times
     larger than May 1980.

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  The mountain sits on one of
 the most active seismic zones

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         in the world,
   the Pacific Ring of Fire--

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a vast arc of volcanoes running
    for thousands of miles.

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It's home to some of the biggest
  and most dangerous volcanoes

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         active today.

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   Here, the enormous plates
making up the earth's crust

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  are being squeezed together.

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 Along the coast, the
plate below the Pacific

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is sliding un the
North American plate.

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 60 miles down
pressure and friction melt the rock.

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        Magma wells up.

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  When it reaches the surface,
         it bursts out.

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          (explosion)

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    But there are still many
     unanswered questions.

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   Scientists' understanding
  of what triggers an eruption

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  this massive is incomplete.

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      And given the scale
of destruction,

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    they need to find a way
           to predict

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   when it might happen again
     before it's too late.

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      Mount St. Helens is
        about to become

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   one of the most intensely
studied volcanoes in the world.

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     The mysteries are not
        just geological.

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    Biologists want to know
    if any life has survived

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  and what its future will be.

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      Charlie Crisafulli,
   one of the leading experts

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   on the mountain's ecology,
arrives soon after the eruption.

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          CRISAFULLI:
 Nothing could have prepared me
   for the sights and sounds

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  that I saw when I got here.

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        It was complete
      and utter barrenness

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 and there was no sign of life
          whatsoever.

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           NARRATOR:
      His job is to survey
         the mountain,

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 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

172
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       to this landscape.

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What would the pattern be?

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     How would the rate be?

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           NARRATOR:
    Much of the mountain is
      still inaccessible.

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       So he starts work
     in the blow-down zone

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  in an area some eight miles
   downhill from the crater.

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          CRISAFULLI:
  We flew over in a helicopter
   very close to the ground.

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  We would have these bumping,
        twisting flights

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      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.

183
00:14:09,270 --> 00:14:11,438
  Then he notices something...

184
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.

187
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.

190
00:14:48,977 --> 00:14:53,814
It's a northern pocket gopher.

191
00:14:53,882 --> 00:14:55,115
          CRISAFULLI:
     It was very thrilling.

192
00:14:58,386 --> 00:15:02,589
           NARRATOR:
    How can it possibly have
survived when nothing else has?

193
00:15:06,461 --> 00:15:08,562
          CRISAFULLI:
This tiny animal lives entirely
      beneath the ground.

194
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.

201
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.


