Sunday, July 18, 2010

I'm Lichen It

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South Idaho

IMG_0021Home on the range cows, wandering around the sagebrush, munching on cheat grass. Pretty happy cows, who like to stare down your truck in an endearingly benign fashion. Ranching is a large industry here, with herds of cows dotting the landscape.

(Sometimes, the cattle trucks park for a rest outside my open window. That particular scent is less than endearing.)

P1200887This is where milk comes from. Or some variety of dairy product, at least. Dairy is another large industry here, responsible for other herds of cows.

IMG_9826Native bunch grass, which grows abundantly in Laidlaw Park. Laidlaw Park is a very large area completely surrounded by lava flows, so it’s had some natural protection from invasive species.

IMG_9830Virga, a kind of rain that falls, but evaporates before hitting the ground.

IMG_9834In the middle ground, those dark areas are lava flows from the Great Rift, and some small cinder cones dotting the horizon.

IMG_9883The Snake River canyon, at sunset (obviously.)

P1200880This is the Snake River, farther upstream, cutting through basalt flows.

P1200922Cheat grass is a non-native species found all over. Before it dries out for the summer, it turns this nice purple color. Then it dries out, the seeds get caught in the undercarriage of your car, lights on fire, and torches the desert. (I hear that’s not appreciated.)

P1200938I know some people don’t like it, but I rather enjoy the desert, mainly because you can see the sky. Though I do wish it would cool off a little – it’s getting well over 90 degrees, and there's really only so much water one can drink!

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Saturday, July 10, 2010

Craters of the Moon NM: A Quick Trip

A couple weekends ago, I drove up to Craters of the Moon National Monument. It was a nice trip, though a vague out-of-sorts feeling and a late departure led to a fairly short trip.

I’m not too worried about scheduling a return trip, however, since it’s closer than the grocery store. For serious.

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On the drive up, I was really impressed by the erosion of the nearby hills, and the really nice alluvial fan beneath them.

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On the other side of the road was this really nice tumulus.

When I first arrived, I took a short, quarter-mile walk along the North Crater Flow Trail.

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These large blocks are pieces of the North Crater that broke apart, and were rafted along in the lava flow. This may look like a really flat expanse of lava, but it’s much more textured in other areas.

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This is some ropy pahoehoe lava from that same area. This forms when the lava has a very low resistance to flow and is also flowing relatively quickly, usually near the beginning of the flow. The skin that forms on top the flow gets pushed forward by the onset of more lava, much like when you stir cold hot chocolate. (My advice: pull that off. Nasty.)

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Do you see the extrustion of lava flowing towards you here, across the top of a flatter section of lava? This is called a squeeze up, and occurs when the pressure inside a flow forces lava through the thick crust above it. In this case, it occurred at a pressure ridge – a section where the pressure inside a flow built up, and created a ridge.

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After that, it was time for the ranger-led tour of Indian Tunnel, a lava tube. My first experience with lava tubes was here, so I was intrigued to see if it measured up to my remembrances. When I was 13, it was the coolest thing ever – I took notes the whole way, complete with sketches. (For serious.)

I’ll be honest, since I have more lava cave experience now, it wasn’t overly impressive – there are much cooler caves elsewhere on the Monument/Preserve, including some of the best lava caving I’ve done.

However, Indian Tunnel definitely is a good one for kids – the cave segments aren’t long enough for natural light to disappear, and it’s an easy walk. The children on my tour seemed totally excited, especially two boys who made Good Photo-Ops For Mommy a goal. (“Get a picture of me up here, Mom!” “Come take it from over there!”)

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The cave is in a part of the Blue Dragon flow, named because it has this crazy blue sheen to it – it’s much brighter in person. It’s rather strange looking, and apparently scientists don’t know why it occurs.

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This is about the longest section of darkness, and the end of the tour. You travel along the flat floor of the tube up to this point, where crossing some breakdown is necessary at a skylight.

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This is a small example of a bench at the skylight. This occurs as the tube curves, and the inside edge slows down enough to cool somewhat. They can be much more dramatic than this, but this also showcases some nice lichen formation – that green stuff on the wall.

(The white sections are either secondary mineral deposits – probably calcite – or pigeon poop. Here’s something I learned on this tour: pigeons aren’t native to Idaho – they were brought in by the US Calvary, as carrier pigeons. If I ever meet a US Calvary man from that era, there are a few choice words I’d like to say to him.)

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This is an example of the ceiling in Indian Tunnel. You can see the white calcite deposits on the ceiling here, which made the ceiling look like meringue to me as a child. The floor was much more brownie-like. (I might have been hungry…)

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This is looking back at the skylight, after crossing the small pile of breakdown. Skylights are places where the tube’s roof has collapsed, which can occur in a variety of ways. If it occurs after the roof has cooled, but while the lava is still flowing, the breakdown can be rafted away from the entrance. If it occurs after the roof has cooled and the lava has stopped flowing, it creates this pile of breakdown, which is a joy and a pleasure to clamber over.

After you cross beneath the skylight, you enter another short period of cave, and then climb out another skylight. Viola! The cave is over.

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Your reward for making it to the end is a short hike across a barren lava field, where you can admire some more flow features.

All in all, it was an enjoyable trip. Next time, I’m planning on leaving earlier, so I can hike some of the longer trails, check out some other caves, and get a better look at the spatter cones and tree molds.




Note: I'm trying Windows Live Writer out. I'm hoping it will enable me to draft posts off-line, and then quickly post them when I can get on-line. That's why the pictures are small in this post.

Saturday, July 3, 2010

When to Tattle on Professors: An Example

I’ve had my share of awesome professors, and more than my share of hateful professors. Only occasionally, when it was warranted, did I complain. Recently, I discovered that, if you complain like a mature adult with dignity, you garner more respect from the administrator. (Funny, that.) I’m actually really proud of the way I handled the situation – it’s given me a standard to live up to the next time I need to complain about a superior.
The situation was this: I made an honest scheduling mistake, not realizing that this professor required special treatment for this procedure. When this issue became apparent, they got very angry, and said some harsh words. I chalked it up to finals week stress, and made alternate scheduling arrangements. I then sent an email to said professor, apologizing for the problem, accepting responsibility for it, and purposing the alternate solution. Professional, calm, apologetic, and proof-read by someone other than myself.
In a nutshell, the email I received back was less than professional, and basically demonstrated some egomaniacal shit-flipping of the highest order. A highly inconvenient solution – but my only one – was laid forth: take the final three hours from when I read the email, two days earlier than anticipated.
When I went in, I was honestly scared I was going to be slapped. Instead, the professor was calm, collected, and explanatory – though not apologetic in the slightest, of course.
After the final, I went to the Dean. I brought our email exchange, and explained that the problem was resolved, but someone needed to speak to this professor about his attitude toward students – preferably after grades were finalized. He said he would, and I moved on, despite knowing that my final was a disaster due to this issue.
If this had been the first time he’d been a jerk, I would have let it slide – we’re all human, right? But I’ve seen enough of his behavior to know that this isn’t the first, or last, time he treats a student like a lesser being.
And that right there is the line of appropriate behavior between students and professors – how you treat not just another human, but someone who is trying to learn from and look up to you, and someone who has put their time, effort, and future into your hands. It’s a mutual bond of respect that requires compassion on both sides, and occasionally some self-control.
When that line is crossed, I think it’s acceptable to rat out the professor to an administrator. Respect may be earned, but there’s a basic level we all deserve – even we lowly students.

A caveat: complaining about professors is unwarranted when you really did screw up. I’ve heard stories from professors about students who go to the president of the college because they didn’t pass a class, despite flunking all the tests. As an easily distracted under-acheiver, I’ll just say: put on your big boy/girl britches and deal. If you didn’t read the syllabus correctly, didn’t study hard enough, or didn’t withdraw in time, you made your own grave. Learn from your mistakes, but don’t put the burden of your failure on the professor.
The same goes for students who approach the professor after every test, trying to explain why they deserve those two points they missed on question four. Seriously? Get some dignity