I don’t normally post about food, but this was too good to pass up.
The food they serve at the cafeteria on the summit can sometimes be very interesting. For my breakfast (dinner for people that are awake during the day) today, I had rice with the little alphabet letters you find in alphabet soup commonly.
Naturally, the thing to do when served this is to spell GPI. The ‘P’ was particularily hard to find in my dinner.
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Time for my second GPI observing run! And this one is especially exciting as this run will officially start the GPI Exoplanet Survey. Flying down to observe on GPI can be its own adventure though. The closest city to the Gemini South Telescope is La Serena. Coming from the Bay Area, it takes about a full day to get to La Serena, involving at least two layovers (e.g. Dallas and Santiago), and often it doesn’t go exactly at planned.
This time, our flight from Dallas to Santiago encountered a mechanical error and was delayed. Unfortunately, since this happened around midnight, this meant we would not fly out until the next morning. The airline had to book everyone in hotels for the night, and I’m not sure if it is because they were running low on hotel rooms, but we were booked into an extremely interesting hotel. It was a Andy Warhol themed hotel, filled with Warhol artwork and Warhol-esque furniture. The toiletries even had Warhol inspired designs (I kept one as a souvenir). Here’s a picture of the lobby, although this picture doesn’t quite do it justice.
Here’s another shot of the lobby with some of our fellow stranded passengers waiting to check in.
This certainly was a memorable forced layover in Dallas. But now I’ve made it to the summit, it’s time to focus on finding some exoplanets!
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A piece of Mars: This 600×450 m (1969×1476 ft) polar scene shows sinuous channels 2-8 m (7-26 ft) wide carved out of ice-filled and ice-covered terrain. They’re not formed by flowing water, but instead by flowing gas that gets trapped under thick winter ice. The pressure of the underground gas builds until it explodes, forcing its way out, and carrying brown soil with it. Local winds blow the soil downwind (to the upper right), forming distinctive streaks. This happens every year on Mars. Awesome. (HiRISE ESP_038399_0945, NASA/JPL/Univ. of Arizona)
A piece of Mars: Wind ha blown the dark, rippled sand between jagged hills, from top to bottom in this frame (663 m or 2175 ft across). Regardless of the terrain, sand finds a way to get through — just like at the beach, it manages to get everywhere. (HiRISE ESP_037494_1685, NASA/JPL/Univ. of Arizona)
A piece of Mars: Topography in color is draped over an image of a windblown cliff. The entire shape of the landscape here was formed by wind, from the large 400 m (1312 ft) tall zigzag cliff, to the small streamlined shapes in the valley. Even the deep gorge that looks like a stream channel was formed by winds, all blowing toward the upper left. (HiRISE PSP_006694_1895 NASA/JPL/Univ. of Arizona, HRSC ESA/DLR/FU Berlin)
A piece of Mars: This looks like a pair of eyes looking at us. It’s really some small brown hills, two of which (the “eyes”) are surrounded by dark gray sand that has blown into scours as the wind interacts with the topography of the hills. It’s a great way to tell what direction the strongest winds blow here: from the bottom to the top of the frame (the frame is 509×382 m or 1670×1253 ft). (HiRISE ESP_037995_1755, NASA/JPL/Univ. of Arizona)
A Piece of Mars: This field of 2 m wide sand ripples has a dark splotch in the middle (the scene is 300×225 m or 984×738 ft). The splotch is the peak of a low hill that straddles the classification gap between proper dunes and simple drifts of sand. Maybe it was a dune that has been modified down to this bump, or maybe it’s a drift that could grow into a dune, if enough sand blew in and accumulated on it. (HiRISE ESP_038117_1385, NASA/JPL/Univ. of Arizona).
A piece of Mars: These funny shaped dunes were formed by winds blowing from two directions – one from the top of the frame and one from the upper right. Both winds make steep slopes (slip faces) on the downwind (lee) sides of the dunes. With enough sand supply, the “point” between the slip faces will continue to extend toward the lower left as the two winds take turns driving the sand back and forth. (HiRISE ESP_037203_2555, NASA/JPL/Univ. of Arizona)
A piece of Mars: There are two sets of ripples here: tan ones and gray ones, each oriented to a different wind (scene is 300×225 m, or 984×738 ft). The gray ones sit on top of the tan ones, so the gray ones are younger. Now come the fun questions: why the different colors? Are they made out of different material (and if so, why), or are the older tan ones different because the gray sediment has weathered to tan over time? (HiRISE PSP_002387_1985, NASA/JPL/Univ. of Arizona)
A piece of Mars: Wind flow on Mars can be quite dramatic. Here, a single wind-sculpted hill stands 1.5 km (0.93 mi) wide and 600 m (1970 ft) high (color shows elevation). That sounds big, but vastly larger is the volume of material that has been removed to form it. A sandy ridge forming a “bow shock” indicates present-day winds still blow in the same direction. (HiRISE ESP_017173_1715, NASA/JPL/Univ. of Arizona)