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Originally posted by Robin Marks
reply to post by shikori
You're watching the YMR webicorder. It's really sensitive. You need to cross reference. If you see something on one webicorder and it's a quake, it will show up on other stations. These stations also pick up earthquakes from other parts of the world. So if you see one, then you need to check the worldwide quakes to find location.
Trust me, you'll know when something is really happening on the webicoders when someone posts a notice or is alerting the others to something happening.
The best thing you can do is research siesmographs and learn how to read them. Local quakes have a very pronounce begining. If you go through many of the pages on this thread you will find lots of quakes posted and you may be able to figure it out from them.
Yellowstone has been quiet. Real quiet. So relax and watch to see when someone posts quakes.
Originally posted by Anmarie96
reply to post by Robin Marks
That was something I was pondering earlier today --- Yellowstone has be toooo quiet. We had the uplift over the past years - now - flatline. in all directions. Since last years swarm, very minor swarms (which, is really, not normal) There are always quakes in the park, mini swarms, larger swarms, ups and down, -, -, but --- it has been almost eerrillllyyy quiet - shhh. But who had said it over at YVO I think it was that I remember, - When We don't see activity is when we worry?? Am I remembering that correctly? -- I feel that way anyway. She seems in a soot of hover state, her preasure was about to pop, she's maintained her blood preasure at a high rate - but, something has got to give soon
As indicated earlier, the problem is ice and snow build up at the main telemetry node where all the data are gathered and put on a microwave tower for transport from the Henrys Fork area (outside the park) down to Salt Lake City.
Moreover, since the data problems differ slightly for each station, that results in a very "locatable" phenomenon for the computer. It would be possible to filter out this "bad behavior", but would result in slower response time (a no-no for seismic networks) and possibly some missed earthquakes.
Eventually, when the park receives another T1 line at Mount Washburn, we will get everything on the internet directly, and the system will improve (and be more redundant to problems).