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The solar and electrical engineering REU students went on a group trip to Yellowstone on Saturday, June 3. We went to a lot of different places, all beautiful!
A bison we saw walking along a river. There were some that walked in the road ahead of our car. The park service was trying to get them off of the road. | |
The Grand Prismatic Pool. The browns, reds, yellows, and greens are caused by bacterial mats, caused by bacteria and other small organisms called "extremophiles." The kind that grow there is a function of temperature. The blue parts are caused by the scattering of blue-wavelength light in the water, and the shade is a function of pool depth. | |
Another geothermal pool. This one is too hot to have bacterial mats, so it's at least 75 celsius. It still has the aforementioned scattering effect. | |
Old Faithful. It sputtered for about 15 minutes before the actual eruption. | |
A lake in the park. We pulled over because it was such a great view - you can see the actual Yellowstone Lake behind it. | |
Me in front of Yellowstone Lake! There was a pretty steep cliff down to the shore. | |
Artist Point: an overlook of a canyon with a waterfall at the end. It looks like someone dribbled watercolors over the cliffs. The whole scene looked like a dream and not quite real. (My companions agreed that it also looks like the waterfall that Bilbo and the dwarves go over in The Hobbit.) | |
The paint pots! All of the colors are caused by bacterial mats like the ones at the geothermal pools. We spent a lot of time guessing the mechanism for forming the round shapes of the terraces. |
Allison Bartz, (c) 2017