This is Interstate 90 crossing Lake Washington
on a floating bridge. A legacy of the Ice Age, this lake is far
too deep and the lake bottom too soft for a normal bridge. But Glacial Lake Washington was bigger. Three major Ice Age troughs sit between Seattle
and the Cascade foothills. And an intricate network of spillways got
established with freshwater being transferred from one glacial lake to the next as the Puget
Lobe was leaving Seattle almost 17,000 years ago. Let’s head east on I-90 out of Seattle on
Interstate 90. Driving from Seattle to North Bend hasn’t
always been so easy. Back in the 1920’s, east-bound travelers
heading for the Cascade Range took the Sunset Highway,
a narrow, two-lane road around the south end of Lake Washington, through Renton and the
coal mines, and then on to Issaquah. But in the late 1930’s, a major step forward. Two new tunnels were dug through the sands
and clays of Seattle's Mount Baker Ridge. The largest-diameter, soft-earth tunnels in
the world at the time. And the world’s first floating bridge built
of reinforced concrete. The opening of the Lake Washington Bridge
in 1940 meant an efficient escape from downtown Seattle due east out over Lake Washington
and Mercer Island. Drivers were now cutting directly across the
lay of the land. North-South-trending hills sculpted by the
Puget Lobe Ice Sheet during the last gasp of the Ice Age. And between those drumlins, equally impressive
glacial troughs. Long ditches carved by rivers of rushing meltwater
underneath an ice sheet 3,000 feet thick. The deepest troughs still have water in them. Puget Sound, Lake Washington and Lake Sammamish. 16,900 years ago, when the Puget Lobe was
at maximum size the weight of the ice pushed the land down
by more than 250 feet. The ice sheet plugged the drainage of the
entire Puget Lowland. Rivers from the surrounding mountains, freshwater,
were backed up at the ice front. The water was trapped, nowhere to go, unable
to drain to the Pacific Ocean. At times, the lake was so large it spilled
south into the Chehalis River and got to the Pacific that way. But as the ice began its retreat to the north,
the glacial lake scene started to change. Spillways got established. Floods of freshwater being transferred from
one trough to the next. Seattle lies at the edge of the deepest trough,
but between Seattle and North Bend, 3 separate tongues of ice sat in 3 significant troughs. The ice retreat caused glacial lakes to form
where the ice tongues had been. And then the freshwater transfer game from
one trough to the next began. Eventally, the ice sheet retreated to Canada,
the Strait of Juan de Fuca was reopened, and the waters of the Puget Sound were connected
once again with the salty Pacific Ocean. The only fresh water remains of the massive
Glacial Lakes of the Ice Age? Today’s Lake Washington and Lake Sammamish. Well that’s a cool story, but this is 'I-90
Rocks'. How much of the story can you see from the
freeway? Well for starters,
Surely you’ve noticed a huge gravel pit in Issaquah at Exit 17. This is the Lakeside Gravel Pit. Right next to Interstate 90 at Issaquah. It’s an active mine. They’re pulling sand and gravel out of this
huge deposit. Much of the sand and gravel was already used
to build Interstate 90 a few decades ago. Why is there so much sand and gravel here? It’s an Ice Age deposit. It’s not a moraine though. This is an Ice Age River Delta. Where an Ice Age River flowed into Glacial
Lake Sammamish. River deltas form when rivers enter quiet
bodies of water. The famous Mississippi River Delta in Louisiana
is made of silt. But here in Issaquah, the delta is made of
sorted sand and even gravel. A fast-moving Ice Age river. One of those spillways between glacial lakes. In this case, Glacial Lake Snoqualmie overtopping
its rim and spilling southwest through surrounding uplands toward Glacial Lake Sammamish. So how can we be sure this a river delta? Couldn’t it be a moraine or something else
during the Ice Age? It’s the bedding here. These are inclined beds of sand and gravel. Foreset beds in the guts of this river delta. Here’s how it works. Ice Age river coming into Glacial Lake Sammamish. The river is bringing sand and gravel. But the sand and gravel is being dumped as
the river is going into the lake. The speed of the river is dropping to nothing. Each new batch of sand and gravel is getting
dumped down the face of this delta underwater. Big avalanches of sand and gravel. And therefore, the delta continues to grow. Continues to build out into the lake. And the height of the delta is the height
of Glacial Lake Sammamish long ago. Up on top of the delta, there’s a nice flat
bench. That’s the old shoreline of Glacial Lake
Sammamish. That’s Lake Sammamish today. During the Ice Age, Lake Sammamish was up
to here. This was the lake level. Beachfront property at that lake during the
Ice Age right here. Wood fragments from the bottom of the delta
have been dated at 15,500 years old. In 1991, a 14,600 year old log was found near
the top of the delta. So this gravel deposit took about 1,000 years
to build, when Ice Age lakes ruled here. These guys won’t be running out of gravel
anytime soon. The entire Tradition Plateau is one big Ice
Age River Delta. One of many Ice Age River Deltas that rim
the Puget Lowland. The elevation of the delta tops are consistently
120 feet above today’s lakes. At the crest of Eastgate, look east across
the Lake Sammamish basin to see the high water mark of Glacial Lake Sammamish. I-90 climbs up two major Ice Age spillways. Heading east at Exit 11, you know the climb. That’s a spillway. Water spilling west from Glacial Lake Sammamish
down into Glacial Lake Washington. And the freeway climb after passing the gravel
pit and leaving Issaquah? Another spillway. This one from Glacial Lake Snoqualmie down
into Glacial Lake Sammamish. Approaching the base of the Cascade Range,
bedrock outcrops begin appearing along I-90, and we arrive in the North Bend area. From the top of Rattlesnake Ridge, terrific
views of Mt Si and the three forks of the Snoqualmie River converge here. Snoqualmie Valley flooding is still a problem
at times. And where the river cascades over ancient
volcanic bedrock, gorgeous Snoqualmie Falls is just a few miles from I-90. At the foot of Mount Si, one more significant
Ice Age landmark of the Puget Lowland. This ridge that looms over I-90 is important. It’s a glacial moraine, composed of poorly-sorted
loose rocks that formed at the edge of a glacier. But which glacier? Ice that flowed down I-90 from Snoqualmie
Pass? Or the ice sheet that pushed over Seattle
from British Columbia? Dig into the moraine and you'll find rocks
from Canada. Not rocks from the Cascades. The Puget Lobe, the same ice sheet that filled
much of the Puget Lowland, crept way over here to North Bend. Pushed its way up this valley. And the Grouse Ridge Moraine marks the eastern
edge of the ice sheet. But there’s more here than just a moraine. This is another pit. Another active mine using Ice Age rock. But how is this pit different than back in
Issaquah? Remember, in the pit in Issaquah we had bedded
deposits. Layered foreset beds. An Ice Age river going into a Glacial Lake. This is different. Here at North Bend, we’re at the edge of
the Puget Lobe. Along the ice margin. We don’t have those sloping beds. The beds are horizontal. They’re sorted. And there’s also huge glacial erratics all
through this deposit. It’s kind of a pain in the neck for the
miners to get this sediment out. To work around these huge boulders. Specifically, this is a moraine and outwash
complex. And the surface of the outwash is beautifully
flat. So coming away from this morainal ridge, we
have this beautiful, flat bench. The outwash of Grouse Ridge. Within, all of these rocks from Canada. Not from the Cascades. The Puget Lobe, many times during the Ice
Age, blocked Cascade rivers draining the mountains. So we had glacial lakes ponded against the
outwash. Rivers bringing sorted rocks from both directions,
off of the ice, and also down from the Cascades. The glacial deposits here clearly state that
at the end of the Ice Age, the Puget Lobe and the Cascade mountain glaciers were not
in snyc. During the last ice sheet advance, alpine
glaciers in the Cascades were already retreating back into the mountains. So the I-90 drive from Seattle to North Bend
has tons of Ice Age geology. But there’s another story here that goes
back even further into our past, and is likely part of our future. The Seattle Fault, a significant east-west
crack in the bedrock, runs right beneath the freeway here. The bedrock layers have been vertically offset
by thousands of feet. The Seattle Fault has generated hundreds of
earthquakes. The fault is responsible for at least 4 magnitude
7 earthquakes in the past 2,500 years. And there is concern for the future. Plate tectonic forces responsible for past
Seattle Fault earthquakes continue to squeeze the crust. The most recent quake caused the bedrock south
of the fault to jump up suddenly 21 feet about 1,100 years ago. Between Bellevue and Issaquah, have you ever
noticed how the freeway runs along a boundary with ridges on the right and lowlands on the
left? Earthquakes on the Seattle Fault created this. Each quake on the fault lifted the Issaquah
Alps a little higher and dropped the basin a little lower. The hard bedrock on display south of I-90
includes 30 million-year-old volcanic rocks and siltstones of the Blakely Formation. North of I-90, the bedrock is buried by thousands
of feet of soft sediment that is prone to seismic shaking. In Bellevue, I-90 crosses Mercer Slough. 1000 feet of very soft peat soils. Earthquake ground-shaking is expected here. In response, the Washington State Department
of Transportation has been seismically retrofitting this stretch of I-90. Overpass columns have been reinforced with
steel jackets. And cross beams under the freeway have been
secured with fixed blocks of concrete. Engineers and geologists working together
to help prepare us for the future. How can we be sure there was an earthquake
900 AD on the Seattle Fault? All sorts of different kinds of evidence point
to the same conclusion. In the bottom of Lake Washington, there’s
a dense forest that’s in the lake. Landslides went into the lake. Brought the tress with them. The trees have been dated. 900 AD. A buried log has been found at West Point,
north of Seattle. Discovery Park. The log sits in sand. The sand’s been interpreted as a tsunami
generated by the 900 AD earthquake. Charcoal from bogs on Bainbridge Island. Tree rings from trees that were killed by
rock avalanches on the Olympic Peninsula. Plus, it’s not just the Seattle Fault. The Tacoma Fault and the Saddle Mountain Fault
over by Hood Canal all talk about a 900 AD earthquake
Shallow levels in the crust in the Puget Sound. Also at the bottom of Lake Washington, old
wooden coal cars sitting upright on the lake bottom. Still loaded with coal. What happened here? In January of 1875, a barge containing 18
coal cars was rounding the northern tip of Mercer Island when strong winds tipped the
barge and sent the cars plunging to the bottom of the lake. The coal came from 40 to 50 million-year-old
sedimentary rock layers below the Blakely Formation in the Issaquah Alps. The bedrock in the uplifted side of the Seattle
Fault. Newcastle, once the second largest city in
King County, produced more than 200,000 tons of coal annually at its peak in the 1880’s. To bring the coal from the Newcastle mines
to Seattle, the coal was loaded into wooden cars, and sent on rails to the eastern shore
of Lake Washington. The cars were barged across the lake to the
western shore near present-day Husky Stadium. Unload the barges, more rails and then another
barge across Lake Union and through Seattle to the docks. By then, the coal had been handled 11 different
times. The coal was regularly shipped as far south
as San Francisco, California. Seattle provided 22 percent of the coal produced
on the Pacific Coast at the time. With coal, Seattle was able to stand out from
the other Puget Sound towns that relied mostly on lumber. Today’s Issaquah Alps are very popular areas
for Seattle hikers and bikers. But there’s a geologic reason these uplands
have very few condos, malls, and housing developments. Cougar, Squak, and Tiger Mountains are riddled
with old coal mines. More than 50 mines, many multi-storied, are
now sealed underground for safety reasons. The mine shafts, now filled with groundwater,
have rotting timber supports. Development has not been allowed above many
of the old mines because of the danger. Coal mining in the Seattle area. An important, often forgotten, chapter between
Seattle and North Bend. Well we made it to North Bend. Seattle to North Bend. Through all of that Ice Age geology and the
Seattle Fault. Let’s head up into the Cascades for our
next episode. Up this glacial valley. Up and over Snoqualmie Pass. And look at the Cascade geology. That’s next up. Thanks for watching this one. Onward to the east we go.
Wow this is done by Nick Zentner, I know him from CWU, heck he tried to make a geology major! Fantastic guy and a great video!
Never knew there were coal mines in the Puget Sound. Very cool.
You did not tell me that there was going to be school.
This was really interesting. I know Puget sound was created by glaciers but has no idea how!
That was way more interesting than it had any right to be.
I hope he does Mima Mounds at some point. Both fun to say, and fun to climb on. Silver Creek Falls and in Oregon the Petrified forest in Oregon are also really cool. The dry lake deserts of the alavord / steens mountains are also interesting. There are so many interesting things here, very busy geologically speaking.
I feel like if you know a little more about the history of a place it means so much more than just climbing to the top of Mount Si because it's there.
That was good, but it was way more than 2 minutes.