Geology 101 with Willsey, Episode #29: Earthquake Location and Size

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  • Опубліковано 16 січ 2025

КОМЕНТАРІ • 66

  • @shawnwillsey
    @shawnwillsey  19 днів тому +5

    Please LIKE and SUBSCRIBE. I also appreciate your continual support of these geology education videos. To do so, click on the "Thanks" button just above (right of Download button) or by going here: www.paypal.com/donate/?hosted_button_id=EWUSLG3GBS5W8 Or: www.buymeacoffee.com/shawnwillsey

    • @RWBHere
      @RWBHere 10 днів тому

      Shawn, at 26:24, that's a mistake on the diagram. That energy level was for the Soviet Union's ,Tsar Bomba' (King Bomb), which was a thermonuclear (Hydrogen) bomb, and equated to about 56 megatons of TNT. Hiroshima and Nagasaki nuclear fission bombs (one Uranium bomb and one Plutonium bomb) were very much smaller than that; the energy equivalent of around 16 and 25 kilotons of TNT.

  • @clydebennish2106
    @clydebennish2106 14 днів тому +3

    In the early 90s i worked as an electronics intern for the geophysical institute at the university of Alaska in Fairbanks. I and another guy were sent out to install seismic and telemetry equipment in remote locations to include the mouth of st augustine volcano. Funny story is years after i left i went back to visit the guys where they took out a map and said they sent a crew to update a certain site i helped build between Fairbanks and Anchorage, but they couldnt find it. It was a site initially chosen by them that looked good but our helicopter couldnt land there. On the fly we picked a similar ledge about a mile away, installed the tower, radios, antenna, batteries, burried the sensor, then tested... we reported the new location upon return. I took one look at their map and immediately noticed their problem... they were looking in the wrong place... they failed to document our new site. Boy, were they ever red in the face. That expensive gear would have been lost for eternity if i hadnt paused my trip to visit the GI and say hello. Apparently the guy with whom i did the field work had left the department a year after i did and he would have been the only other reference. I loved that work.

  • @pacco5728
    @pacco5728 15 днів тому +1

    Pleaseeeee keep these coming, I am in introductory geoscience right now and your videos make it so much easier to absorb the information.

  • @timpointing
    @timpointing 17 днів тому +3

    Final note: thanks for the simple and clear explanation of the problems with the Richter scale and the need for the Moment Magnitude scale. 👍🏻

  • @maruillescas6608
    @maruillescas6608 18 днів тому +5

    ¡Gracias! Greetings from Mexico. Happy New Year Profesor Shawn

  • @ykennedy4473
    @ykennedy4473 18 днів тому +3

    Thanks!

  • @oscarmedina1303
    @oscarmedina1303 18 днів тому +3

    Thank you Shawn.

  • @StevenStyczinski-sy8cj
    @StevenStyczinski-sy8cj 19 днів тому +2

    You are doing such an awesome explanation of how thees things happen that I as a 66 year old remember being taught the magnitude scale when I was in grade school. Please continue teaching us!

  • @jacquie-h4530
    @jacquie-h4530 18 днів тому +2

    Thank you, again, Shawn, for making a complex subject easy to understand. I knew my way around the Modified Mercalli Scale but had found the change from the Richter Scale to the Moment Magnitude Scale hard to fathom, but you made the difference easy to grasp. I hope you have a great New Year.

  • @JanClancey
    @JanClancey 18 днів тому +1

    Ahh mind blown those numbers are massive.. thanks for a little seasonal grounding. Cheers Shawn

  • @YOICHIHAGIWARA
    @YOICHIHAGIWARA 14 днів тому

    ありがとうございます!

  • @kevenbennett8827
    @kevenbennett8827 19 днів тому +3

    Earthquake study and coffee. The best mix. A real earthquake would spill my coffee, #!@p*! Thanks, Shawn!

  • @codyedwards6922
    @codyedwards6922 18 днів тому

    Thank you for the classroom time, you are an amazing teacher and person. Giving back the way you do inspires me to do the same, give back.

  • @muzikhed
    @muzikhed 9 днів тому

    Very good, very interesting. Thanks, really enjoyable learning series.

  • @sueellens
    @sueellens 18 днів тому +1

    Fascinating. Thank you so much Shawn! Happy New Year to you and your family! ❤

  • @Bed-rx1
    @Bed-rx1 18 днів тому +1

    You continue to date my overall knowledge Doc, lol. The Intensity Scale was not around when I was in school. Good stuff, thanks.

  • @marymachunis3778
    @marymachunis3778 18 днів тому

    Thanks for another fascinating lesson, Shawn. I didn't know about the second scale for measuring earthquakes. Happy New Year!

  • @codyedwards6922
    @codyedwards6922 18 днів тому +1

    Great job!!👏

  • @zyadabdulrahman989
    @zyadabdulrahman989 15 днів тому +1

    Good morning,sir!
    Will you explain in physical geology only, or in other branches like geophysics?
    thanks for your videos they are so benificial for me.

  • @cyndikarp3368
    @cyndikarp3368 18 днів тому +1

    Thanks

  • @runninonempty820
    @runninonempty820 19 днів тому +5

    I knew that a magnitude 6 was much bigger than a 4, but I didn't realize HOW much. The scale is crazy!

    • @pmm1044
      @pmm1044 18 днів тому

      Cuz magnitudes use exponential functions. 😳

  • @hamidrezasepahian7608
    @hamidrezasepahian7608 10 днів тому

    excellent

  • @jrepka01
    @jrepka01 18 днів тому

    The ~32x energy difference makes quick-and-dirty comparisons of energy differences fairly easy: 2 tenths of a point in magnitude is equivalent to a doubling in energy, So the rough energy difference between Mw 8.8 and Mw 7.0 is 500x (2^9). The difference in depth of 22 miles to 8 miles reduces the total energy difference by a factor of ~7.5 (using the inverse square law). This brings the total surface energy relative to the two sites to a difference of 60x to 70x, before even considering other factors. One of the big secondary factors is that the epicenter of Haiti EQ was directly beneath Port-Au-Prince, where more than half of the population lived -- maximum shaking was concentrated in this area. In Chile the shaking lasted much longer but the energy was distributed over a much larger area.

  • @timpointing
    @timpointing 17 днів тому

    One question that i've had since watching the Icelandic eruptions and the EQs associated with magmatic movement: How accurate are the calculated focus positions. Are we talking +/- 10m, 100m, 1000m? Or maybe a percentage of the distance from the various seismometers?

  • @homkh4258
    @homkh4258 16 днів тому

    Thanks for video. I don't understand how did you calculate the epicenter distance by P and S wave difference time? And how did you the focus of earthquake within the earth?

  • @timpointing
    @timpointing 17 днів тому

    In actual fact, in the final quiz, it is the "32" that is the rounded number. A Moment Magnitude difference of 2, as in the example, is a factor of exactly 1000 in the energy released. (The "32" is just a handy, easy to remember approximation. It should really be 10 times the square root of 10, or the square root of 1000: 31.6227766...)

  • @timpointing
    @timpointing 17 днів тому +1

    Yet another final comment 😂:
    The Moment Magnitude scale uses a subscript of "W" to denote "work". To quote Wikipedia:
    Caltech seismologist Hiroo Kanamori [...] took the simple but important step of defining a magnitude based on estimates of radiated energy, Mw , where the "w" stood for work (energy)

  • @StellaVinum
    @StellaVinum 18 днів тому +2

    About ten minutes in I’m wondering are you going to mention negative depth earthquakes? That’s probably not a 101 topic though. The first time I ran across one of those lead me down a long reading rabbit hole about how sea level affects the zero depth in the model.

  • @timpointing
    @timpointing 17 днів тому

    Quick question: why is the graph of S/P wave times vs distance not a couple of straight lines? Is it because of the waves travelling through the Earth, not across a plane, and also possibly them encountering different material in the Earth's interior with different propagation speeds?

  • @geomodelrailroader
    @geomodelrailroader 17 днів тому

    Earthquakes this one subject we should know about. One the main things that we have to worry about here in Idaho right on the canyon rim is earthquakes. Mount Borah is very much alive if there's any movement there we will feel it, if the Wasatches move we will feel it, if something happens in the Ruby Range or in the Silver Zones we will only feel small tremors. Here is a big difference between the different types of earthquakes that you will feel: p-waves come from the Earth's core you will feel them when they hit. S-waves also called aftershocks are closer to the surface. S-waves cannot go through volcanic rock and when you look at a seismograph you can barely see them. You know when an earthquake is coming when you see the big p-wave on the seismograph. If you are in an earthquake zone get on the ground and squat and cover your head. Look for anything solid a door, edge of a bed a desk anything. Stay away from windows and never go outside. All earthquakes must be reported to the USGS the moment they hit or to the Rock Doctor himself and Wilsey will report it to the USGS. Remember an earthquake can strike anytime anywhere and we will not notice it until it's too late. Be prepared for anything.

  • @jeffbrooks8024
    @jeffbrooks8024 18 днів тому

    How do they work out the total amount of energy released

  • @squadman3376
    @squadman3376 10 днів тому

    My sister lives in Santiago, Chile. in that 2010 EQ, They were sleeping on the 16th floor of their modern, anti seismic apartment. Little damage to the building but furniture , pictures dishes, all bouncing and breaking. It was horrific and loooooong !!.....they were OK otherwise. Rocks Rule !

  • @mch8172
    @mch8172 18 днів тому

    What kind of energy is released in an earthquake? Is it the strain energy density integrated over some region of rock surrounding the focus that is released after the fault shifts?

  • @professorsogol5824
    @professorsogol5824 19 днів тому +2

    30:33. "An 8.1 is worse than a 7.6". Ok, please tell me if got the math right 8.1 - 7.6 = 0.5 or 1/2. 32 to the 1/2 power is the same as the square root of 32 or 5.66 (rounded off). So a 8.1 earthquake releases 5.66 times as much energy as a 7.6 earthquake.

  • @almeisam
    @almeisam 18 днів тому

    Well do I remember the Nisqually earthquake, being 4 miles from the epicenter. I saw lamp posts waving side to side, and my car doing the same.

  • @debranelson1987
    @debranelson1987 18 днів тому

    Science rules....end of story...mic drop...keep it coming!

  • @helenskene2849
    @helenskene2849 18 днів тому

    Kia Ora from New Zealand
    Eq1 = christchurch earthquakes (but many)
    Eq2 = kaikoura earthquake (from 180km away felt like a wave form)

  • @jdst1042
    @jdst1042 18 днів тому

    Good Content, you need to link up with thegeomodel guy Phillip Prince.

  • @jfmezei
    @jfmezei 18 днів тому

    Another question (you'd hate me if I were a real student). In the Vanuatu earthquake footage of "CCTV video: People flee cafe as magnitude 7.3 earthquake hits Vanuatu" from Associated Press, which I assume you have seen, we can see people running out (and 2 falling), but then, something very violent happens with the fridges suddently moving a large distance (probably about 1m).
    If I had had a very precise GPS attached to one of the building's columns, would it have recorded the whole building moving while the fridges stayed put and would the building's position have returned to normal at the end, of would there have been a permanent shift in position of similar magnitute as we saw the fridges move?
    Or did the fridges get "thrown" by the ground with some vertical movement which amplified their horizontal travel and the ground didn't move horizontally that much?
    Since the building retained power, is it safe to state whatever this building experienced was experienced equally over a much larger area otherwise power cables would have snapped somewhere?
    Would this video properly represent the different phases P, S and Surface waves)? People fleeing as part of P wave and fridges vuiolelntly moving as part of S or later Surface waves?

    • @ingridcc1-123
      @ingridcc1-123 18 днів тому

      A GPS units attached to objects that can move or be thrown around by the earthquake wouldn't record information that would be very useful to anyone, because there are too many factors involved, like how the building the object is in was constructed as well as how tall it is (if the height of the building matches the 'period' / timing of the earthquake waves, and they last a while, then the building will experience 'resonance' - like giving a swing a little push at just the right point can make it swing higher and higher - and can fail catastrophically whereas buildings much taller or shorter will do better). Also tons more factors like the size, shape, weight of the fridge, which way it was facing compared to the direction of the waves, how top-heavy it was, etc. Too much of a mishmash of irrelevant data. Seismometers are attached to solid ground. They just measure the shaking of the ground not the shaking of a particular building or refrigerator.

    • @jfmezei
      @jfmezei 17 днів тому

      @@ingridcc1-123 But attaching GPS to the building's columns that are anchored into ground would show if the building moved 1m and the fridges didn't move, or whether the building barely moved by vibration caused fridges to move.

  • @candui-7
    @candui-7 19 днів тому

    Over 100 years ago Edgar Cayce prophesied California will fall into the ocean. (Actually the quote is that California will become an archipelago.) On a road trip through the San Joaquin Valley it dawned on me what he meant. (Hint: Sacramento is 10 m above current sea level.) No earthquakes required.

    • @oscarmedina1303
      @oscarmedina1303 18 днів тому +1

      100 years ago, plate tectonics was unknown. Edgar Cayce didn't understand basic geology and the fact that California, west of the San Andreas fault, is attached to and sitting on top of the Pacific plate.

    • @candui-7
      @candui-7 18 днів тому +1

      @@oscarmedina1303 I don't think Edgar was thinking much about sea level rise either.

  • @BillRicker
    @BillRicker 10 днів тому

    Nomogram calculation!

  • @CoreyCoffell
    @CoreyCoffell 17 днів тому

    Why can earth sciences conceive of a centric view while our solar system is constantly portrayed as a membrane rather than centric?

  • @residentpotato6023
    @residentpotato6023 19 днів тому +1

    Instead of bowls wouldn’t it be a cylinder? The epicenter would be where the cylinders touch each other at the depth of the epicenter?

    • @gerardacronin334
      @gerardacronin334 19 днів тому

      I think you’re right! If they were bowls, there would be no point of intersection other than at the surface.

    • @oscarmedina1303
      @oscarmedina1303 18 днів тому +1

      Technically they are spheres. It's just that above the ground there is no transfer of energy. They are spheres because the shockwaves travel in all directions as the same speed. This creates a sphere. Where the spheres intersect, you draw a line directly vertical to the surface to determine the epicenter.

    • @gerardacronin334
      @gerardacronin334 18 днів тому

      @ The spheres interact at the surface. But it seems to me the circumference of the circles at a given distance from the seismometer on the surface of the earth indicates the latitude and longitude at which one should “dig down” or “drop a plumb line”. But what do I know, I’m just a regular human, albeit one with STEM training,

    • @jrepka01
      @jrepka01 18 днів тому

      Hemispheres match the parameters of the distance. An EQ 1000 km away from you could mean 1000 km to the north, to the south-east, etc. It could also (in theory) be 1000 km below you. Points on the surface of a cylinder would be progressively further from the seismograph as you go deeper.
      For an EQ at depth, the circles won't intersect at the surface, they'll overlap leaving a gap in the shape of a pseudo-triangle. But the spheres will all intersect at a single point beneath the surface, giving you the depth

    • @jfmezei
      @jfmezei 18 днів тому

      If you beleive in the conspiracy theory that the Earth is a obloid sphere instead of established fact it is flat, the half sphere vs cylinder model works better when distances are great. The Earth's (alleged) curvature means that the intersection between 2 spheres sufficiently apart may happen below ground level. And the distance calculated at a seismograph is accurately reflected by the sphere model since the radius = distance and remains accurante everywhere along surface of sphere below ground. In a cylinder, the distance between surface of cylinder and the seismograph increases as you go deeper so you exceed the calculated distance.

  • @utubewatcher806
    @utubewatcher806 18 днів тому

    Triangulation..

  • @jfmezei
    @jfmezei 18 днів тому

    How dare you force us to study between Christmas and News Years 🙂
    Your presentation treated the focus as a "point" (with one very very brief mention it ot could be longer). Wouldn't a movement typically involve one side of a fault moving against the other side over a certain distance? Wouldn't the lenght of fault involved in the movement be a major part of the energy released? Surrely, 2 10cm diameter rocks moving agaist each other can't cause a calamity with high rises topplng over, bridges falling into San Francisco bay, or Los Angeles losing its bouyancy and sinking into the Pacific to create new beach front properties in San Bernadino?
    Are they able to calculate the length of a fault involved in an earthquake?
    If you have 2 alternate universes where in one, you gave a 8.0 magnitude earthquake with movement over 1km of San andreas fault, while in the other universe it is an 8.0 over the same area, but 5km of San Adreas fault moves (and both at same depth). Would both generate the same damage intensity but the second one have wider area of damage? or would it release far more energy due to 5 times the mass of rocks moving?

  • @hansschleichert7852
    @hansschleichert7852 16 днів тому

    Thanks!

  • @jonride6836
    @jonride6836 16 днів тому

    Thanks!

  • @scottsheppard532
    @scottsheppard532 16 днів тому

    Thanks!

  • @victorrichenstein1646
    @victorrichenstein1646 19 годин тому

    Thanks!