Dana came into town on Monday, so I got little reading done on the 8th, 9th and 10th. Then Thursday, Interzone WiFi was down, and OSU visitor was exceptionally weak and difficult to access... I was awfully frustrated. So yesterday morning, I was effectively four days behind in my reading. With this rebuilt machine, though, skimming, skipping and reading is much quicker. I also decided to simply delete all news items older than two days, which means maybe 1500 items skipped- I'm sure I missed some MSM science news I'd like to have read, and I've been pleased at how often (and generally, well) OregonLive covers geology-related news in Oregon and the PNW broadly, so I probably missed 2 or 3 of those as well. Well worth it though, to save myself six or seven hours of browsing time. So I spent eleven hours yesterday, and better than four today, plowing my way back to the beginning of the week. And now I'm caught up. Whew!
In other news, I can say with some degree of excitement and pleasure that our rain has returned with a vengeance. The prediction yesterday was for about 0.1 to 0.25 inches; we got 0.37, and it looks like some serious accumulation tomorrow night through Tuesday morning. Various sites are predicting 2-4 inches in this area. To which I say "Bring it on, baby!" A report that I read this morning, from Cliff Mass Weather Blog, commented, "In the Olympics, north Cascades, and southwest BC terrain (particularly Vancouver Is) amounts reach 5-10 inches, with a few higher values on the windward slopes. Wow." So 2-4 inches sounds about right to me.
On with the show. My goal today is to summarize the geotripping Dana and I did on Monday, Tuesday and Wednesday, along with a few photos. Our original intent was to either hit NW California and the Josephine Ophiolite along route 199, or central/eastern Oregon doing day trips out of Bend- in particular, Dana wants to hit up John Day National Monument, and I've never been to the Painted Hills unit near Mitchel, so I'd like to do that. For various reasons, though, we decided to simply do day trips out of Corvallis. Due to a number of other factors, we did an awful lot of last-minute plan changes, too. But it all worked out well- I don't think there's anything we missed on this trip due to time shortages. Dana and I are both getting better at budgeting our time. And on the plus side, there were a number of things neither of us had anticipated seeing, but did. So overall: good trip!
Monday, we decided to just hang out around town, take in some local parks, and do the architectural walk around the OSU campus that I've done with Ryan and Emily. First stop, Chip Ross Park, north of town. The geology is kind of subtle here, but the views are good, and the interesting component is broadly interpreting the geomorphology visible from the park.
Saprolite (which I learned as 'saprolith,' but I gather is the preferred English geo-usage now) at the base of the hill, as we headed back to the car. The word comes from roots meaning dead or rotten rock.
Avery Park. I was thinking maybe a box elder, but followup says not. So no real clue what kind of tree this is- it has compound leaves that remind me of walnut or pecan, but not quite right for those.
We also did my tour of the OSU campus with a focus on the rocks used in construction, but I took no photos, and ones I've taken previously are not on this computer right now, so I'll just leave that dangle. To make up for it, I'll just let you know that between the two of us, we found complimentary men's and women's rooms that have good examples of fossiliferous stylolitic limestone. The one I've stopped at before is in the Memorial Union, and only the men's room has that rock. It's okay during the summer, when there's no one around, but not good during the regular school year. We also ran into Peter Clarke, Aaron's advisor. I introduced myself to him with, "Hi! My name's Lockwood DeWitt, and there's no reason on earth you should remember me."
Day 2: Up to McKenzie Junction, down the Upper McKenzie River, with stops at Clear Lake, Sahalie Falls, and Koosah Falls, then up over McKenzie Pass to Sisters, dinner, then back to Corvallis, with just enough light to get twilight silhouette of Mt. Washington.
Cascadia State Park. Hydrology/hydrogeology emerged as the unexpected theme of this trip- that is, I was certainly aware water would be an aspect of what we would see, but I wasn't expecting the way it came to dominate my attention and thinking. Not in a bad way, of course, but in an interesting way.
Pretty sure this is the location, in FlashEarth) I'd always assumed the underlying material, with the sort of badlands topography, was an ash tuff. It's not. It shows only modest (if any) rounding, but it's more coarsely lithic and mixed in terms of fragment types than you can see in a drive by. I'm thinking maybe explosive debris, but I'll need to flesh out my reasoning another time.
McKenzie Juction, fall foliage, a fairly fresh lava flow, and Dana's car. This was beautiful spot to stop, as the viney maple was fiery red, and symbolically very pleasing on flows that cooled quite recently.
This shows a down log underwater, extending under the "Clear Lake" label.
Sahalie Falls. Compare the flow rate here to that of the Santiam at Cascadia: much, much greater. Turns out, there's a very interesting set of reasons for that, which I'll get back to someday.
It's getting late, so I'll cover day 3 tomorrow, after I get the Funnies up. Stay tuned... there's more awesome yet to come!
Followup: forgot to drop this in... I was just a little bit into this when Dana posted her summary of her vacation, of which this was about half. And Part 2 of my summary is here.
Is This Your Hat?
2 years ago