I'll be utterly honest: I liked him, and not just because he said flattering things about this humble cyber-cantina. He spent time getting a good feel for what I wanted, and aimed me in appropriate directions. This is precisely what dealers should do, and it's appreciated. Either Seattle's different or things have changed since I last trailed my father around to different dealerships, doing awful things like test-driving cars in snowstorms because my dad knew he'd get a better bargain on yucky days, because I haven't yet run into dealers oozing oil. My dear dealer-reader stands out even among the comfortable salesmen I've spent the last few days with. Even if I don't end up buying a car from him, I'll have no problem steering business his way.
His identity shall be revealed at the end of my searches, as long as he consents. Otherwise, you can contact me for the info, should you be in the Seattle area and wanting to see a man about a car.
Tomorrow, it's off to my stalkers at Nissan for a discussion about the price of new cars and how my bank account can't deal with same. Look, I have books to buy and field trips to finance - not going to spend all of my monthly cash on a car, m'kay? Today's dealer seems to understand that. Will they?
So yes, car shopping continues fine, and I'm now spoiled for choice. My intrepid companion's agreed to allow me to drag him along tomorrow to help me narrow down the final contenders - since he's always with me on these trips, he should have some input regarding the car I stuff him in to.
I see you squirming. You're tired of this car-shopping talk and want your geology, don't you? Well, you shall have it.
You see, my dealer has been perusing some posts here, and we discussed a bit o' this and that whilst tooling around in various autos. At one point, he asked me if there were volcanoes near Seattle. Meaning, other than Mounts Rainier and Baker (if you ever get to meet him in person, ask about Baker - you'll marvel).
That would be a huge yes. There's Glacier Peak, in fact, which was recently highlighted by my favorite Northwest geoblogger, Dan McShane. Mount Rainier's closer, but not by much, and if you're living in the North Sound sneering at all those idiots in the South Sound who might get buried in the next big eruption, well, between Baker and Glacier Peak, you're probably covered. In lahars, that is.
Courtesy of USGS |
Courtesy of USGS |
The biggest danger from Mount Rainier is to the South Sound area, and we're not so much worried about it going boom as going splat:
Courtesy of USGS |
Rainier's not very noisy as far as stratovolcanoes go, not likely to put on a big pyrotechnic show, but it's rotting from the inside. It's one tiny eruption, one heavy warm rainfall, or one earthquake away from releasing a mudflow that will seriously inconvenience a good number of Puget Lowland residents. It's not considered the most dangerous volcano in America for nothing.
So, neither of the easily-visible volcanoes are likely to present Seattle with an impressive show (unless you count being buried under volcanic mudflows as a great afternoon's entertainment). But Glacier Peak's been known to go boom in a big way (pdf).
Courtesy of USGS |
So, why do we have mountains created by uplift and folding, and mountains created by booms big and small, all looming on Seattle's skyline? Let's have a look at a couple of illustrations.
First, the Cascade volcanoes:
Courtesy of USGS |
Now the Cascade Range as a whole:
Courtesy of Wikipedia |
Courtesy of PNSN |
That's the quick-and-dirty explanation of what's going on round the Seattle area. It's what gives us spectacular scenery that could very well kill us one day. And to think I haven't even mentioned the faults, the subduction zone quakes, and the tsunamis! Or the three thousand feet of ice we'll be enjoying if the Ice Age decides to mount a comeback.
Just look at it this way: we've got a front-row seat to some of the most spectacular shows geology can put on. As I told my dear dealer, our geology's young, but it's had a busy youth. And it ain't half done yet.
great post dana.
ReplyDeleteJust a couple of more pointers - then I'll shut up. Used car prices are high these days on account of slumping new car sales, which results in fewer trade-ins and a subsequent diminshment of supply relative to demand. Under most circumstances, I always advised my friends never to buy a used car if it was a Nissan, Honda, or Toyota, since these brands command the highest re-sale value relative to new - which means the savings by buying used are usually marginal considering what you are giving up. So - if your budget can stand it and you like these brands - spend a little time online estimating payments on the "new" models. You might be surprised.
ReplyDeleteIn any case, if you are looking at used - go to Kelly (KBB.com) and print out the "private party" and the "wholesale - average condition" price sheets. The wholesale is going to be very close to what the dealer actually has in the car and the "private party" is the most you should expect to pay.
Good luck and post a pic of yourself "pimpin on yer twenty-fo's" when you get your new ride...
*blush* Thanks, Suzanne!
ReplyDeleteChris, your pointers are fantastic! When we finally meet IRL, I won't be able to buy you all the drinks I owe you in one session, because you'd die of alcohol poisoning. ;-)
Between the two of you, I feel empowered to go make a deal. It's like I've got a posse with me when I walk onto the lot. I hope someday I can return all the favors!
Nice write up and good luck with the car quest.
ReplyDeleteI won't comment on car buying -- I'm not that good at it myself, and I've avoided it by keeping my car for 12 years now -- but I'll pick on your quick and dirty subduction zone explanation.
ReplyDeleteYou get your coastal mountain building because things get smooshed, as you put it, but those gorgeous cascades are volcanic through and through. What happens is that the downgoing plate is really, really wet. As it's subducted, the water percolates up through the mantle and into the crust beneath the volcanoes, and soaks the rock. It turns out that wet rocks melt at a lower temperature than dry rocks, so these wet rocks melt and make magma chambers. Then, where there's weakness in the crust, the magma pushes it's way up... and presto, you have a volcano!
That's also a quick and dirty explanation, but it's a little more accurate.