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Welcome to Seattle Washington it's an amazing place for geology what's beneath that noisy Stadium it's a long way down to bedrock the bedrock here has been buried by more than a thousand feet of mud sands gravels that were dumped here by ancient ice sheets distant volcanoes old lakes and rivers even by early residents of Seattle and there's an earthquake fault here a big one it's all right here there's lots to learn you're ready it's game time dig into most of Seattle's Hills, and you'll find complicated sets of poorly sorted rocks and beds of sand and gravel that were dumped here by an ice sheet that came from Canada the Puget lobe advanced and retreated over Seattle at least seven times in the last two million years each ice advanced laid down a different generation of glacial till Canadian rocks strewn all over the Puget lowland stretching from the Olympic Peninsula clear over to the Cascade Range deposits that were first mapped in detail by Jay Harlem Brett back in 1913 kind of hard not to notice a boulder like this right glacial erratics carried in ice from the north the most recent advance began 25,000 years ago in British Columbia ice crossed the border 19,000 years ago and made it as far south as Tonight Washington by sixteen thousand nine hundred years ago that was just yesterday geologically the glacier was 3,000 feet thick over Seattle yep I said 3,000 feet thick I that was three Columbia centers hi the weight of the ice caused the crust to sag by as much as 300 feet since 16,000 years ago Seattle has been ice-free and the crust is rebounded, but the blanket of glacial deposits remain almost 75 percent of Seattle surface deposits were laid down by the most recent ice advanced bedrock here is hard to find only 3% of the Seattle area has exposed bedrock at the surface steeply dipping sandstones in a sea of loose glacial rocks Bluffs throughout the Puget Sound reveal complex LY interbedded glacial and interglacial deposits and Seattle's famous rain makes these deposits especially prone to landslides sometimes with tragic results as it flowed south the Puget lobe acted like a comb running over the landscape sculpting graceful elongated north-south oriented hills called drumlins Beacon Hill first Hill Capitol Hill Queen Anne Hill Mercer Island they're all drumlins one of the very few drumlin fields in all North America have you driven here in Seattle the traveling is easy going north and south along drumlin tops are through Valley bottoms but driving east or west here means you're going against the lay of the land when east-west streets are necessary steep climbs are in order interstate 90 cuts across the grain one of the most expensive stretches of our country's interstate system the freeway tunnels through drumlins and uses bridges to span ice age troughs between the drumlins as you leave Seattle on i-90 you skirt around the north end of one drumlin and then drive through the next one then a floating bridge over a trough then crossing...
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