From Seattle, WA to Portland, OR
via Mount Saint Helens National
Volcanic Monument
ON THIS PAGE:
JUST THE
FACTS
RIDE
REPORT
ELSEWHERE AT my80days.com:

JUST THE FACTS
Ending Mileage: 



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Actual
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As Planned
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Day of Travel
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Monday June 25, 2001
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Monday June 25, 2001
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Departing From
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Seattle, WA
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Seattle, WA
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Destination
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Portland, OR
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Portland, OR
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Distance (in miles)
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276
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274
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Distance (in kilometers)
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444
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442
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Departure Time
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10:15 AM
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Arrival Time
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8:10 PM
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Total Travel Time
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9 hours 55 minutes
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5 hours 47 minutes
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Average Speed (in mph)
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28 mph average
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47 mph average
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Average Speed (in kph)
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45 kph average
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76 kph average
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RIDE REPORT
Waking up this morning, I feel a little melancholy. The visit with
Ron and Carole was really nice and I miss them. In fact, for the
first time in this trip, I really feel a little homesick. Ever since
entering Washington, I have the feeling that I'm 'close to home'.
Washington has a distinctively 'western' feel to it. Not cowboys and
horses kind of western but more like the big metropolitan west coast
attitude kind of feeling. It doesn't look like Los Angeles or San
Francisco but the feel is there. So I feel like I'm home but of
course I'm not in my own bed.
I spend an hour or so watching the local news and getting an
update on the weather situation. What a big surprise, I am about to
run into ANOTHER unseasonable weather event. Seems that there is some
tropical moisture coming from the south so I can expect rain in a day
or two as I head into Oregon and northern California. Not as bad as
the unseasonable snowfall, hail, wind and rain in Montana and North
Dakota, but at least my streak is continuing.
So I weigh my various options. I can be home in a two days, three
days if I take it easy. But if I do that I'll miss seeing some
friends in San Francisco that are always a pleasure to visit. I'll
also miss seeing my sister and her husband, their crazy cat and
friendly dogs not to mention the new furniture. I finally decide to
stick to my original plan and just ride it as planned and have a good
time.
The hotel is surprised to find out that I'm leaving a day early. I
thought about sticking around but Seattle is a bit of a pain in the
ass on a motorcycle. While I like the hotel and the location, it is
much more expensive than my budget allows. I'm staggered that the car
valet has a motorcycle license, as already checked out my bike in the
garage and is very happy to bring the bike around. He's just started
riding and has a much smaller bike and was a little excited to get a
chance to ride (albeit a very short ride) on a big cruiser.
Out into Seattle traffic, it seems that getting to Interstate 5
should be a really simple operation. Unfortunately some road work has
the direct paths cut off so I follow street signs down past the new
baseball field and out into an industrial area. It is several miles
to the on ramp but at least I don't need to disclose any missed turns
or retell any getting lost stories. The weather this morning is
beautiful. Not quite as clear as Saturday but sunny and warm. Traffic
is the usual urban playground. Everyone is jostling for a slightly
better spot. Ten lane changes later and you're still only a few car
lengths ahead of where you started. Truck traffic is pretty heavy.
Once past Tacoma, the road opens up a bit and things are pretty
smooth.
One of my objectives for this trip was to get a better sense of
where my family came from. In some ways, I feel like I'm doing very
poorly in meeting this objective for a number of reasons. Weather in
the Midwest kept me from visiting my mother's birthplace in Dubois,
Indiana. I had a good visit at my father's hometown in Underwood, ND
but again bad weather kept me from nosing around the general area as
much as I would have liked. Finally, my dysfunctional attitude
towards relatives has limited my contact to my father's family in
particular.
Just south of Tacoma is the US Army base at Fort Lewis,
Washington. This is one of the places where my mom lived during her
childhood. There is a museum and I think it would be interesting to
spend some time on the base. The federal government is now on a high
alert (Republican paranoia) and so every visitor to the base must
either be active duty military with ID card and proper stickers for
their car or stop at the gate and present license, registration and
insurance. There is a lot of grumbling from regular visitors without
tags in the line ahead of me. The soldier issuing my pass is friendly
as he goes through the process. Just as he is about to hand me the
pass he remembers that the museum is closed on Mondays. Oh well, good
intentions and all.
I get back onto I-5 heading south. The museum building faces the
freeway only a couple of miles south of the main gate. Its a
wonderful old wooden building covered with gingerbread decoration.
Clearly this is a building that dates back to the earliest days of
this army post. It is attractive but incongruous in its setting.
Soon,
I'm at Washington's state capital of Olympia. The building is a very
traditional one: light colored stone, pillared grand entrances and a
large dome. Olympia has been the capital of Washington since
territorial days. The capitol buildings, there have been two, were
deliberately built away from the rest of the city. In the earliest
days, it was necessary to cross a swampy area to get to the building
itself. The first wooden building was abandoned when the current
building was constructed after statehood. The capitol building is
part of a large collection of formal buildings housing the state's
administrative and judicial functions.
Both the motorcycle and I are hungry. I haven't eaten since last
night and now I can feel it. I make a stop at a Hardee's of all
places for some chicken. I am conscious that it is now early
afternoon and I want to spend some time at Mount Saint Helen's
Volcanic Monument. The turn off for the monument is about fifty miles
south of Olympia off Interstate 5. The route partially retraces my
route to Aberdeen from Yakima only this time I'm headed south rather
than north. South of Olympia the interstate becomes a two lane
highway again and so it feels like there is more traffic than there
probably really is. I finally get to the exit for Washington 504,
Spirit Lake Highway.
From this view, Mt St. Helens looks peaceful almost
normal with few indications of events of May 1980.
From this view, the mud flow is just visible along the
floor of the Toutle River Valley.
Same vantage point but with some zoom, the mud flow is
very clear.
Coldwater Lake from the Coldwater Ridge Visitor Center.
The explosion destroyed the forest once it crossed the ridge
to the right of this photo. Debris (near to the camera and
off frame) dammed the Coldwater Creek forming this lake in
the moments following the eruption.
This is Johnston Ridge. We are less than ten miles to Mt.
St. Helens. This ridge bore the full brunt of the avalanche
and subsequent lateral eruption. It will be a long time
before a forest returns to this ridge. Smaller plants, for
example, the wildflowers in the foreground are trailblazing.
This is the view from Johnston Ridge. All the land in
this picture was moved by some part of the eruption that
morning. There is a dense pumice field at the foot of the
mountain. The impact of erosion can be clearly seen.
A closer view of the lower left of the photo
above.
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There are three visitor's centers operated by the
National Forest Service along with a county-operated
educational center between I-5 and Mt St. Helens itself. The
first visitor center is only a few miles of I-5 and provides
an overview of the mountain's explosive eruption on May 18,
1980. I'm surprised by the amount of observation that was
ongoing when the eruption occurred. I'm also amazed by the
relatively small size of this eruption at least as measured
by volume of material discharged during the event. As I
recall, the eruption of Krakatoa in the late 1800s
discharged approximately 150 times the volume of material.
The explosion of Mt Mazama that created Crater Lake in
Oregon was on the order of 1,000 times the size.
From this first visitor center, Mount St. Helens appears
peaceful. A snow capped peak not quite as symmetrical as
Rainier but clearly volcanic in form. The appearance is so
deceiving that I come close to skipping the trip to the
second and third centers. What a huge mistake that might
have been.
Washington 504 is a great ride. To the west, I pass
through a number of small communities, stopping in Toutle
for gas. The trip is about 90 miles out and back and I don't
want to get stranded. The first clue that something is out
of the ordinary is a directional sign for the mud flow
containment structure.
A few miles further and a large sign announces that you
are entering the blast zone. At first things seem pretty
normal -- the forest has been replanted. And then almost
suddenly you pass a point where the trees are just all gone.
For miles and miles, you only see stumps and blown down tree
trunks. Sometimes that is all you can see. As you continue
to the second USFS visitor's center at Coldwater Ridge,
Mount St. Helens continues to grow. Finally there is turn
out where you can look down onto the area covered by the
avalanche and subsequent landslides. The devastation is so
awesome and nature's restoration so tentative, that the
eruption could have been yesterday and not more than twenty
years ago.
The visitor's center at Coldwater Ridge focuses on the
aftermath and natural activities that are working to restore
the landscape. The visitor center offers a highly
picturesque view down onto Lake Coldwater. Lake Coldwater
was formed by the debris carried by the avalanche and
subsequent eruption as well as the lateral eruption. Spirit
Lake is larger than Coldwater but can not be accessed by
vehicle from the western approach. Spirit Lake is the famous
view of water covered by downed trees in the days after the
eruption.
From Coldwater Ridge, WA 504 heads down into an area that
is covered with hummocks. Hummocks are the pyramid-shaped
hills resulting when the side of Mt. St. Helens was blown
over Johnston Ridge and landed in the valley. Then the road
begins a long climb up to Johnston Ridge. For the last hour
I have wondered why I as so cold. When I get to Johnston
Ridge and realize that I'm at 4200 feet, I realize why I am
so chilly despite the sunny day. Without trees, I lost my
best visual cue that I have gained altitude.
The view from Johnston Ridge is amazing. This is one time
where seeing is believing. The magnitude of the geologic
changes is sweeping and the scale can not be imagined. This
has already proven to be an amazing day.
Inside the observatory, the programs focus on the
eruption and the immediate aftermath. What I did not realize
is that a series of related events were triggered that
morning.
For many weeks, scientists and lay people had been
watching the mountain. The scientists documented a huge
bulge on the side of the mountain. Subterranean pressure had
forced the ground to rise dramatically. Destabilized the
mountainside collapsed and formed an avalanche of earth, ice
and water that raced down the side of the mountain into
Spirit Lake. It is estimated that this wall of material was
moving at 100 miles per hour.
Within seconds, the release of the overburden allowed the
explosion to begin. For the first time, a volcano erupts
from its side in a lateral explosion. The explosion
literally blows the top and more of the side of the mountain
directly at Johnston Ridge at more than three hundred miles
per hour. The blast is deflected over the ridge and into the
valley behind as well as to the west into the Toutle River
Valley. Observers here, thinking they were safe from a
normal vertical eruptions, die immediately.
This explosion is caught in outrageous photographs taken
by hikers at Mt Hood. A family is celebrating a child's 16th
birthday by hiking to the summit. They take their pictures
near the summit with Mt St. Helens in the background. The
timing is uncanny. The first jets of the eruption are
shooting from the mountainside. The father recounts that
they braced themselves for a shock wave that never came but
that the temperature rose by 15-20 degrees (F). As the
eruption continues, they noticed the huge amount of
lightening in the sky above the volcano. They decided to
abandon their trip when metal objects, including his son's
braces, began to vibrate from the electrical charge.
The explosion did knock down all threes in area of more
than two hundred square miles. The logs are not burned as
there was so little oxygen in the air that combustion could
not occur. A family survives near Spirit Lake by
accidentally being in the shadow of a ridge. They begin to
make their way out and are stopped by the fallen trees. They
will spend the next thirty hours picking their way across
the fields of giant fallen trees try to escape the volcanic
dust.
With the eruption now in progress, a third part of the
mountain is in motion. Water trapped below the avalanche and
displaced mountainside is now making its way to the surface
and creating a hug mud flow. That is joined by melting snow
and glaciers on top of the mountain. This flow moves down
several streams and rivers chiefly the Toutle River.
A man and woman recount awakening that morning. They know
that something is happening on the mountain but like other
observers and campers are sure they are safe due to their
distance from the peak. They are making breakfast near the
side of the Toutle River. They are both roused by the sound
of logs being carried down the river on the mud flow. The
air is filled with the smell of pine logs. They look upriver
to see a railroad bridge being carried toward them on the
mud flow. They try to make it to their car but are carried
away by the river. His leg is crushed by the logs banging
against each other. They both manage to mostly stay on top
of the logs and survive. A Christmas tree lot provides such
a strong cue to him that each year he relives those
frightening hours.
The next onslaught is airborne rocks and debris thrown up
by volcano's eruption. The dust is so dense that it is dark
on the ground. Pumice is falling as rocks the size of eggs.
Two observers try to outrun the advancing cloud, having
continued to take photos of the unfolding avalanche for too
long, but eventually can not move safely. They wait for
several hours before joining a convoy led by a logging
truck. Men sit at both ends of the front bumper feeling for
the road with sticks and giving the driver direction as to
when to stop and turn.
Ash fall would begin within the hour in cities such as
Yakima and Spokane in western Washington. In Yakima, nearly
two inches of ass would fall in the days following the
eruption. Those cities, attempting to clean up the ash using
water sprayers would deplete both cities' water supplies and
require water use restrictions until the following springs.
Helicopter pilots, dispatched within fifteen minutes to
rescue people stranded by the eruption are at a loss. Their
maps and memory of the area is antiquated in minutes by the
changes to the landscape. The forest, lakes, roads, rivers
-- all gone.
My visit to Mt. St. Helens turned out to be truly awe
inspiring. I can not recommend this visit highly enough.
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The ride down from Johnston Ridge to Interstate 5 allows for some
real contemplation of this event. Thank goodness it did not occur
more closely to a major population center. While fifty-seven people
were killed that morning, the toll is very small compared to what
could have happened without adequate warning.
The rest of the day's ride is nearly anticlimactic. The ride down
the Columbia River Valley is beautiful. The bridge crossing is very
dramatic. I finally duck into a small mom and pop motel for the
night. Tomorrow, I'm off to Grants Pass.
Route Summary
Depart Seattle on Interstate 5 heading south.
Exit I-5 onto Washington 504 Spirit Lake Highway heading east.
At Johnston Ridge Visitor Center (end of WA504), turn around and
head west on WA504.
At intersection with I-5, enter I-5 heading south.
Cross state line into Oregon
Arrive Portland
(c) 2001 Thomas N. Engler Revision Date: 07/16/2001