WEBVTT FILE 1 00:00:01.159 --> 00:00:07.379 hi everyone um so this video is gonna Center on a really cool data set that 2 00:00:07.379 --> 00:00:12.900 was collected at lone star geyser in Yellowstone in years 2010 and 2014 and 3 00:00:12.900 --> 00:00:19.470 so this right here is the geyser cone and what I am overlaying here is a 4 00:00:19.470 --> 00:00:33.170 representation of what the subsurface can you pause this for a second 5 00:00:40.940 --> 00:00:46.920 alright thanks pause thanks okay so this is a representation of what the 6 00:00:46.920 --> 00:00:51.210 subsurface plumbing system looks like beneath the geyser or what we think it 7 00:00:51.210 --> 00:00:55.410 looks like and the main thing to take away is that there is this cavity that's 8 00:00:55.410 --> 00:00:59.969 offset from the vent and that's we think that's important because it allows for 9 00:00:59.969 --> 00:01:03.149 gas and pressure to build up in the system which then leads to these 10 00:01:03.149 --> 00:01:09.030 episodic eruptions you're good so guy lone star geyser is like many other 11 00:01:09.030 --> 00:01:14.010 geysers and that it erupts with remarkable regularity so this is what 12 00:01:14.010 --> 00:01:19.170 the cycles look like it's showing 10 hours of data and three eruption cycles 13 00:01:19.170 --> 00:01:23.159 so at the top here this is the temperature at the vent which is a proxy 14 00:01:23.159 --> 00:01:27.930 for the amount of water discharged so an eruption you can tell that there's an 15 00:01:27.930 --> 00:01:31.710 eruption by this broad peak up here and so you can see that there are these 16 00:01:31.710 --> 00:01:36.509 three eruptions in the middle I'm showing the location of the hydrothermal 17 00:01:36.509 --> 00:01:43.350 tremor, so tremor in geyser systems is thought to reflect bubble nucleation or 18 00:01:43.350 --> 00:01:48.180 collapse and so we see that there's this sort of persistent location of tremor 19 00:01:48.180 --> 00:01:53.970 during the cycle and then just before an eruption the tremor will migrate towards 20 00:01:53.970 --> 00:01:58.560 the guys event and this persistent location corresponds to that bubble 21 00:01:58.560 --> 00:02:03.869 cavity that I showed earlier and then on the bottom we have tilt data so this is 22 00:02:03.869 --> 00:02:09.479 showing you how the ground is deforming and that's maybe reflecting the motion 23 00:02:09.479 --> 00:02:17.740 of subsurface fluids during the eruption great so these time series graphs are 24 00:02:17.740 --> 00:02:26.370 kind of hard to always to figure out the relationship between different hang-up 25 00:02:27.900 --> 00:02:32.350 okay so sometimes it can be difficult to understand the relationships between 26 00:02:32.350 --> 00:02:36.820 different data types when you're just looking at these time series graphs and 27 00:02:36.820 --> 00:02:41.050 so we're gonna look at a different way of understanding that data using data 28 00:02:41.050 --> 00:02:45.310 movies that make use of sound as well as visuals to try and understand the 29 00:02:45.310 --> 00:02:49.360 relationships between different data types thank you so this is the key 30 00:02:49.360 --> 00:02:55.760 that's going to show us what the movie is looks like 31 00:03:00.060 --> 00:03:03.580 so that's the water discharge or the temperature at the vent 32 00:03:23.260 --> 00:03:27.700 no just turn it down a bit that sound 33 00:03:37.380 --> 00:03:43.510 okay great so so now that you guys know what the different sounds and visuals 34 00:03:43.510 --> 00:03:46.360 are corresponding to now we're going to put it all together and listen to three 35 00:03:46.360 --> 00:03:51.140 eruption cycles in 2010 and then three eruption cycles in 2014 36 00:05:56.660 --> 00:06:02.250 okay so we wanted to look at how stable this kind of system is over the course 37 00:06:02.250 --> 00:06:07.319 of from 2010 to 2014 so now I'm going to play those two videos side by side so 38 00:06:07.319 --> 00:06:11.250 that you can sort of directly compare how the eruptions line up between the 39 00:06:11.250 --> 00:06:12.920 different years 40 00:07:18.080 --> 00:07:25.720 all right um so it's really remarkable that I don't know if you guys could pick 41 00:07:25.720 --> 00:07:28.750 out the eruptions when they were happening but between both of the years 42 00:07:28.750 --> 00:07:33.760 the second eruption happens at exactly the same time between the years but then 43 00:07:33.760 --> 00:07:42.130 it's it's also interesting that the last eruption of 2010 seems delayed relative 44 00:07:42.130 --> 00:07:46.360 to the eruption in 2014 so there is something that's making these eruptions 45 00:07:46.360 --> 00:07:50.770 extremely regular but then there is also the ability to modulate that regularity 46 00:07:50.770 --> 00:07:56.680 and delay some eruptions so now one other question that comes out of these 47 00:07:56.680 --> 00:08:02.080 movies is that even though the eruptions happen very regularly the pre-play so 48 00:08:02.080 --> 00:08:06.550 there's sort of surges in activity just before the eruptions those were really 49 00:08:06.550 --> 00:08:10.120 irregular and they seemed to happen at completely random times in the different 50 00:08:10.120 --> 00:08:13.840 years and the different eruption cycles so that's another question is what's 51 00:08:13.840 --> 00:08:18.580 what's causing the eruptions to be so regular even though the sort of lead-up 52 00:08:18.580 --> 00:08:23.230 activity seems to be very irregular so I'm for the final movie we're gonna zoom 53 00:08:23.230 --> 00:08:28.660 in on just one eruption cycles so that we can listen to the details of the 54 00:08:28.660 --> 00:08:30.940 eruption cycle yeah 55 00:09:15.760 --> 00:09:20.080 this is that pre-play that I was talking about 56 00:09:25.860 --> 00:09:28.540 and this is the eruption 57 00:09:41.740 --> 00:09:46.920 thanks very much everyone if anyone has any