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(NASA SCIENCE FILES

THE CASE OF THE SHAKY QUAKE

AIRS: November 20,2002

 

Video Audio
Focus Questions In this segment of the Case of the Shaky Quake, you will be asked the following questions.
What is a seismologist?
Describe the layers of the Earth.
What are two types of clues that help us learn about the Earth’s history? And when you see this icon you know the answer is near.
Tree House Seg #1
In this segment of the Case of the Shaky Quake, you will be asked the following questions.
What is a seismologist?
Describe the layers of the Earth.
What are two types of clues that help us learn about the Earth’s history? And when you see this icon you know the answer is near.


(R.J.) “I think this bone goes right here. It looks like it’s part of the tail.”
(Bianca)Wrong it’s actually part of the head.
(R.J.)O.k. This is the closest we’re going to get to a dinosaur dig.
(Bianca) Jacob is going to have so much fun looking for dino bones.
(Anthony) Excuse me, they’re called fossils.
( Starts to feel the shake)
(Bianca) Did you feel that?

(Anthony) Huh?
(R.J.) I did. What could it be?
(Second Shake)

(Anthony) I felt that one.
(Bianca) Now that you’re with us, what do you think it is?

(Anthony) It’s an earthquake!
(R.J.)Don’t jump to conclusions. Go to the NASA SCI Files web site and see if they have any information on earthquakes.
(turn to camera) Visit the research rack on the NASA SCI Files web site for resources on earthquakes. I found two places in Virginia where seismologists record earthquakes.
( Bianca) A size what?
(R.J.) A seismologist is somebody who studies and measures earthquakes.

(Tony) Look , a seismogram is located near us at the Tidewater Community College. ( Reading from screen) Let’s call
Seismologist, Michael Lyle.

Split screen with
Anthony and Mr. Lyle
(Lyle) Michael Lyle. Tidewater Community College, Seismology Lab.
( Anthony , trying to be formal and grownup) Hello, Mr. Lyle. Tony De Angelo, Tree House Detective. I would like to inquire if your instrument picked up a tremor a few minutes ago.
( Mr. Lyle) Yes. Our seismograph did detect something.
(Anthony) Was it an earthquake?!
(Mr. Lyle) Maybe. But, it’s not clear from my reading here.
(Anthony) Okay, we’ll check back with you.
  (Turning to the group) Mr. Lyle says there’s a very good possibility there’s been an earthquake. (Turn to camera) Okay I exaggerated a little bit.
(Bianca) We all know it’s going to take alot more research to solve this problem Look, here’s an update from KSNN.
  KSNN Newsroom
TUNE I’m Ted Tune with this Kids Science News Network Special Report. Strange vibrations in the area have local residents concerned. We’ve sent our reporter, the usually unshakable IM Lissning, outside to look around. IM?
LISSNING Well, Ted, I’m outside. I don’t see anything. (Giant pig flies up through the sky like a rocket behind IM.)
TUNE Well, IM, don’t get “shaken up.” Why don’t you look around a little?
LISSNING Mostly because it’s starting to rain, Ted. I’m coming back in.
TUNE IM? IM? And she calls herself an investigative journalist. Anyway, that was IM Lissning with a live repo-OWW (Lissning’s microphone hits Tune in head)
  (R.J.) I’m glad we weren’t the only ones who felt the vibrations.
(Anthony) I think there’s sufficient evidence to show we need to launch an official investigation.
(Bianca) In simple words, let’s go to the problem board.
At the problem board ((R.J.) We know we felt the shake. TCC recorded something and KSNN reported a mysterious vibration.
Anthony (Tony) Since we’re pretty sure it’s an earthquake, I think we need to……..
(Bianca) Wait a minute. We need to do a lot more research before we come to that conclusion.
(Tony) Okay we need to do more research on earthquakes (Turn to Camera) They’ll see I’m correct. (goes off and picks up math book and does calculations in his journal)
(R.J.) I think we need to know what else can cause vibrations.

(Anthony) I’m sorry what did you say. I was just calculating the cost of remodeling our tree house to make it earthquake proof.
(Bianca) Anthony, we don’t even know if it was an earthquake and we sure don’t have enough information to know how to make a tree house earthquake proof.
(Anthony) Well, I estimate that it would take about $20,000 and if we took out a loan with an interest rate of 6.5% for 30 years, then our payment would be only $128 a month. For the principal and interest.
Kids look at him like he is crazy and laugh.
(Anthony) OK, OK. We need to get back to the problem. Dr. D is from California. I’m sure he’s been in a few earthquakes.
Dr. D’s Segment #1 (Anthony) Hi Dr. D.
Dr. D: Hi Guys. What’s up?
(Bianca) We felt our tree house shake this morning, and we want to know what happened.
Dr D: Yeah. I felt something too.
(Anthony)We think that it might have been an earthquake, but we can’t prove it yet.
(Catherine) Have you ever been in an earthquake?
Dr. D: Yes I have, but it didn’t feel the same as what I felt this morning.
(Bianca) See, I told you it wasn’t an earthquake.
Dr. D: Wait a minute. All earthquakes don’t feel the same. To begin understanding earthquakes, you have to know something about the structure of the Earth.
(Catherine)That makes sense. What can you tell us?
Dr. D: Let me cut this peach in half.
(Bianca) Careful
Dr. D I will thanks. This will be our earth.
(Anthony)Only it’s a lot smaller.
Dr. D: It’s called a scale model. This pit is like the core of the Earth. The Earth’s core is about half its diameter.
( Catherine)What’s it made of?


Dr. D: We’ve never been there, but we think that it’s made of iron and nickel. The inner part of the core is solid and the outer part is liquid. It is so dense that if you had a gallon (showing gallon) jug full of the Earth’s core material, it would weigh over a hundred pounds!
(Anthony)Wait a minute Dr. D. You lost me. How do we know how big the core is and what it’s made of? How do we know when we’ve never been there!?
Dr. D: Well, it’s just a guess.
(Anthony)You’re kidding
Dr. D: Actually it’s a pretty good guess based upon a lot of evidence. One of the biggest clues to the Earth’s structure comes from the study of earthquakes.
(Bianca)So we’re using earthquakes to help understand earthquakes?
Dr. D: That’s right. The part of the peach that you eat is what we call the mantle of the earth. It’s not as dense as the core, but it’s denser than what is on the outside.
(Catherine)What’s the outside called?
Dr. D: It’s called the crust.
(Bianca)Just like a crust of bread.
Dr D: Very good. The Earth’s crust is very thin. The crust under the oceans is typically between 5 and 10 km thick and is made of dark dense rock called basalt. The continental crust is about 30 to 70 km thick and is made of a lighter, less dense rock like this granite.
(Anthony)Is there a reason why the Earth is layered like this?(Dr. D) It’s because of density. Watch this experiment. I’m going to put some green tinted water and some salad oil into this graduated cylinder and shake them up. Let’s see what happens.
(Anthony) Thee salad oil is on top, and then the water.
Dr. D: Now let’s add some motor oil. It turns out that the least dense, the motor oil, is on top, and the densest, water is on the bottom. That’s just what happened in the early history of the earth when it was all liquid.
(Catherine) Earth liquid? Strange, but what’s this have to do with earthquakes?
Dr. D: The crust on the outside of the earth is rigid and brittle. It is broken into about 12 segments that we call plates- like this cracked boiled egg. These plates float on the more dense but flexible mantle below- kind of like this egg white. They are in continual movement.
(Anthony) Wow, this is too weird. Why don’t we feel them moving?
Dr. D: They move about as fast as your fingernails grow, which is only a few centimeters a year. But, we have fossil evidence of that movement that we call Plate Tectonics.
Anthony: Are fossils also a clue to understanding earthquakes?
Dr. D: Well, …, yes!

(Catherine) But, Dr. D, are there other things that can cause vibrations?
(Dr. D) That’s a good question. Anything that makes a very loud sound can make things shake a little.
(Bianca) I watched fireworks on the Fourth and some were so big, I did feel a vibration.
Dr. D: Oh no! I’m late for an appointment. Why don’t you stay here awhile and discuss this some more.
(Bianca) Ok. Bye Dr. D. What about a sonic boom? We learned from the Case of the Barking dogs that sonic booms create a noise because the plane travels faster than the speed of sound.
(Catherine) That’s it! We have our hypothesis. If Airplanes were flying faster than the speed of sound, then it would cause the ground to vibrate.
(Bianca) I don’t think a sonic boom is our hypothesis because I forgot that my dad says the military never flies faster than the speed of sound over land anymore.
(Catherine) Oh, I thought we had it.
(Anthony) I’m glad R.J. and Jacob are going to California for the Science Fair. Maybe they can research earthquakes for us.
(Bianca) Wait a minute. Jacob is in Utah looking for fossils. Dr. D said that there was fossil evidence of plate tectonics.
(Anthony). I wonder if that’s the same thing as the Continental Drift Theory my teacher talked about.
(Catherine) Maybe, but, I don’t understand what fossils and Plate Tectonics have to do with earthquakes?
(Bianca) Let’s E- mail Jacob and ask him to find the answers.
(Catherine) Okay. I’ll do it.
(Anthony) We need to do some investigating on our own. Let’s go back to the tree house and find out if anyone else has felt the vibration.

Location: Utah Fossil Trip
Jacob: (Turn to camera) Wow, look at this place. It is so cool. I can’t believe I’m touching a dinosaur bone. Is this real? ( doubting)
D. Whitman : Yes of course! These dinosaur bones here at Dinosaur National Monument are about a 150 million years old. . Do you want to see something really neat?
Jacob: Yes!
D. Whitman: Follow me.
( Enter dinosaur quarry)
Jacob : Amazing. I’ve never seen anything like this! Did you just put these bones on the wall?
D.Whitman: No. This is a dinosaur quarry where our paleontologists continue to dig up new bones. There are over 15-hundred bones on this wall.
Jacob: Why did they all end up here?
D.Whitman: Well, a river collected the bones and buried then in sand and gravel. Over the years more layers of sand and mud covered the bones and then hardened into rock. The bones also became hard as rock as water seeping through the ground filled them with dissolved minerals. They became fossils.
Jacob: Oh, I almost forget, my friends want to find out if fossils are clues to Plate Tectonics and earthquakes?
D.Whitman : I can probably help you out.
Jacob: What was the environment like?
D.Whitman: The area was flat and arid and that was where all the dinosaurs ended up.
Jacob: What was the climate like?
D.Whitman: It was hot year around and the reason for that is that this area was a lot closer to the equator 150 million years ago. So because of plate tectonics or continental drift. As a matter of fact, where we are standing right now was about 400 miles closer to the equator at the time the dinosaurs lived here.
Jacob: It’s hard to believe that land can actually move that far.
Alfred Wegener in the early 1900’s when he first proposed the idea that he called Continental Drift.
Jacob: What is continental drift?
D.Whitman: It was a theory that stated that the continents were once all one large land mass called Pangaea. Clues indicate that in the last 200 million years, the continents have moved or “drifted” horizontally to their current locations.
. The revised theory, called Plate Tectonics, said that the earth’s crust and outer mantle, which is called the Lithosphere, is split into segments called plates. The movement of these plates, called Plate Tectonics, causes rocks to bend and break. Jacob: You mean fossil clues?D.Whitman: Fossils can be clues to cont. drift. For example, fossils of the reptile Mesosaurus have been found in South America and Africa. These reptiles lived in fresh water and on land, so how could they be found on different continents, unless the continents had at one time been together? Another clue can be found in rocks
Jacob: Strange. How do you know a rock found here can be the same as another rock found in the Colorado Plateau?
D. Whitman: Let’s take a walk and find out.
Jacob: Great.
D. Whitman: Jacob , you’re looking at the Green River.
Jacob: I know I’ve never seen anything like this before. How can you tell that two rock structures are the same?
D. Whitman: It’s like being a detective. Look over at the sandstone over here. It looks like six other sandstone. You have to look at at the rocks that are associated with it. If you look at the sandstone that’s directly below it. It’s the chin lee formation. The sandstone above it is the Glenn Canyon formation.
Jacob: Do you have Earthquakes here?
D. Whitman. Here earthquakes are caused by mountain building. 65 million years ago, the rocks were being pushed up. Have you ever seen a cake in the oven? What happens when it rises too much?
Jacob: It will collapse.
D. Whitman. The same thing happens with the rock . They bend. But, they only can bend so far and they break.
Jacob And when the rocks break, does that cause an earthquake? D. Whitman: That’s correct When the rocks move along the fault line , they cause an earthquake So did I answer your questions?
Jacob: Yes, I can’t wait to e-mail the tree house detectives
Utah: Do you have time to go fossil hunting?
Jacob : Sure!
Utah : Let’s go! What’s Up?
Will fossils help the tree house detectives solve the mystery?

Do you think the tree house detectives experienced an earthquake?
What else could have caused the vibration? Stay tuned for the case of the Shaky quake.
Focus Questions:
Segment #2
In this segment of the Case of the Shaky Quake you will be asked these questions.
What are three types of faults?
What are three types of plate boundaries? How does a seismograph measure the shaking of the Earth?
( Just getting off phone)
(Kali)That was my last call. A lot of people on my list said they felt a vibration.
( looking at computer)
(Bianca) Look at all the E-mails. Some say it felt like an explosion.

(Anthony) Let’s E–mail KSNN and ask if there were any reports of an explosion in the area.

(Kali) Okay, I’ll do that. I love writing to KSNN.
(Bianca)Maybe this is our new hypothesis. If there was an explosion, then it would cause the ground to vibrate.

(Kali) I was talking to one person who said it felt like a big heavy truck driving by.
(Anthony) This E mail describes it like a sonic boom. But, we know it’s not a sonic boom.

(Bianca) Here’s an update from KSNN. I wonder if they received our E mail.
KSNN KSNN Newsroom. Tune is handed a note
TUNE This just in… Ah! The Tree house Detectives have raised the question: Were there any explosions that could account for the vibrations detected yesterday around Noon? For the answer we go to IM Lissning, on the scene.
LISSNING (at construction site) Ted we’re here at the site of the new Mega-Bulk-Mart. Yesterday at exactly 12 noon, the original “This Little Piggy” Bar-B-Que restaurant was demolished to make way for construction. We have this exclusive video tape, sent to us by Mr. Flange Lugnut.
Video shows restaurant and giant pig sculpture being blown up. First the building goes, then the Pig is launched into the sky by the second blast.
LISSNING There you have it folks. The tremors felt yesterday were simply gigantic explosions. Nothing to worry about. Back to you, Ted.
Tree house (Anthony) I.M. is obviously not a Scientist. Doesn’t she know you can’t jump to conclusions? You must do research.
(Bianca) Cool! That confirms my hypothesis. Look at our clock; it stopped at noon, so they must be the same explosions.
Turn to camera (Bianca) That’s what I call using my observation skills. Observing is an important part of the scientific process.
(Anthony) You’re like I.M., jumping to conclusions! I still think it could be an earthquake and I don’t want to take any chances.
(Kali) Maybe Tony is right. Jacob said in his email from the Dinosaur National Monument, that the movement of the Earth’s crust and upper mantle, called Plate Tectonics causes earthquakes.
(Anthony) I’m reading more about plate tectonics in my earth science book. It says that crustal movement occurs along fault lines. Maybe we need to learn about faults.

(Bianca) Let’s do an Internet search.
I’ll go to a search engine and type in the words earthquakes, faults, and VA.
(Tony) Finding Anything?

(Bianca)The search shows several web sites listed for United States Geological Survey or USGS. Let’s go to their home page and find out who they are.
(Tony) (reading screen) They monitor earthquakes all over the US.
It sounds like they would be able to help us.
Graphics (Bianca) I clicked California on their map and they have an office in San Francisco. Let’s send Jacob and R.J. an email and ask them to talk to the USGS.
USGS
Jacob: Okay guys. We are standing in front of the trench for the San Andreas Fault in Olema California. This was the epicenter of the 1906 earthquake.
Stenner: Hi, you must be the tree house detectives. I got your the e-mail. How can I help you?
R.J.: Our friends in VA. felt a vibration the other day and they want to find out if it was an earthquake.
Jacob: They said we need to learn more about faults.
Stenner: A fault is a weak point in the Earth’s lithosphere where the rock layers have broken apart and slipped.
Would you like to see the San Andreas Fault?
Jacob : Sure.
Jacob: Are there different kinds of faults?
Stenner: Yes, there are three types of faults. There is the normal fault in which the block above the fault, called the hanging wall, moves down the block below called the footwall (graphic). These occur where the crust is pulling apart.
R.J.: Is there an abnormal fault?
Stenner: (laughs) Well, I wouldn’t call it abnormal but there is a thrust or reverse fault which is opposite of the normal fault. Its hanging wall moves up the footwall and these faults occur where the crust is being pushed together. (graphic)Jacob: What’s the last type of fault?Stenner: It’s a strike-slip fault. This fault is vertical and the blocks slide past each other.Jacob: We learned that the earth’s lithosphere was broken into pieces called plates and the plate movement cause earthquakes. But, I don’t get it. Are plates and faults the same?
Stenner: Moving plates grind and scrape against each other at their edges, which we call plate boundaries. Plate boundaries are made up of many faults.
R.J: Are there different types of plate boundaries like there are different kinds of faults.
Stenner: Yes, there are also three
Divergent boundaries are where the Earth’s crust is pulled apart. This can form new crust, cause rift valleys, and even volcanoes to form.
This divergence causes the Atlantic to widen about 2 cm per year
Jacob: That’s not very much, it must move really slowly.
Stenner: Yes it does. A convergent boundary is where plates crash head-on or crunch together.
R.J.: I hope those boundaries move slowly too!
Stenner: They only move a few cm a year, so the collisions can last over millions of years. When two continental plates collide, they fold into huge mountains like the Himalayas. (Chris did a graphic of subduction)
Jacob.: (turn to camera) Wow, now I am beginning to understand why the Earth is shaped the way it is.
Stenner: The last plate boundary is the one you are probably most familiar with. It is called a transform boundary, like the San Andreas Fault, where the plates slide past each other. The area west of that fault is moving north.
Jacob: So does that mean that California is not going to break off and fall into the ocean?
Stenner: (laughs) No. That is a common misconception. Actually, Los Angeles will someday be side by side with San Francisco? In about 10 million years!
R.J.: That’s a long time.
Jacob: I don’t think we have any boundaries in VA. Do earthquakes occur anywhere else?
Stenner: Yes. Earthquakes in the interior of plates are called intraplate earthquakes. In 1886, there was also a large intraplate earthquake in Charleston, South Carolina.
R.J.: (turn to camera) South Carolina is near VA; maybe they did have an earthquake. USGS
Stenner: Do you want to make your own earthquake?
Jacob: Yah! But will it knock houses down?
Stenner: No, it won’t actually be a real earthquake, just a simulation of a very small one. I have a set-up here that we can pretend is like the earth’s plates moving. You will turn this crank and be the forces driving the plates of the earth to move, called stress. And this brick will be like one of the earth’s plates that is being drug along the board, another plate. So turn this slowly and watch as you add more and more stress to the plate…
Kid turns slowly.
Brick suddenly slides forward.
Jacob: Ahh! Was that the earthquake?
Stenner: Yep,
Jacob: Turn to camera- That’s my kind of earthquake.
Jacob: This has really been helpful Ms
Stenner: You’re welcome. Email if you have any other questions or visit the USGS web site.
 


(Anthony) Done. Do you know what kind of dinosaur this is?
(Kali) Yes a ------.
(Anthony) Not bad. (Another tremor, dinosaur breaks)
(Bianca) What’s going on?
(Kali) I don’t know. But, I don’t like it!
(Anthony) Now, that was an earthquake!

(Bianca) How do you know?

(Anthony) It just felt like one.

(Kali) Maybe this is another construction blast. I’ll call KSNN again. ( Actor goes to make call)
(Anthony) Look. The dinosaur is destroyed. This will never get built.
(Bianca) Listen. We have bigger problems right now.

(Kali) KSNN just confirmed there were no reports of a construction blast. What could it be?
(Anthony) I don’t know. But, we really need to organize our thoughts. Let’s go to the problem board.

Problem Board (Bianca) We know we’ve had two tremors.

(Kali) We know that KSNN says the first tremor was from a construction blast and the second was not.
(Anthony)We know the structure of the earth is divided into layers.
(Kali) We also know the Earth’s crust is broken into plates and these plates move and can cause earthquakes.

(Bianca) Oh yeah ,and remember that E mail from Jacob and R.J.? They talked to the USGS, who confirmed there are a lot of faults in the Earth’s crust.
(Anthony) Now, we need to know if there are any faults in our area that can be causing tremors.
(Bianca) I think we need to visit the seismologist at TCC to find out if there are any faults in our area. We can also see if they recorded another tremor this time.
Let’s get up and go.
(Turn to camera) (Kali) We might be closer to finding out if this vibration was an earthquake!
Seismologist
Bianca: That must be a seismograph; I recognize it from television. Let’s go over there and see if we can find Mr. Lyle.
Catherine; Hi, Mr. Lyle. We are the tree house detectives. We called you about an earlier tremor. Now we need to know if you recorded any tremors on your seismograph today.
Lyle: As a matter of fact, we did. Here it is right here.
Bianca: Wow! Was it an earthquake? Can you really tell from that reading?
Lyle: We're not sure at this time. We have to first analyze the data because not all detected tremors are related to earthquakes.
Bianca : turn to camera. Analyzing your data is very important in the scientific process.
Lyle: In our area, most tremors that we record are relatively small, travel a short distance, and seem to occur mostly between 8 AM and 5 PM. This suggests that they are caused by human conditions.
Catherine: We learned that earthquakes occur because the Earth's crust is broken and moving along fault lines. Are there faults in VA?
Lyle: Yes, there are numerous faults in Virginia, but all of them are not active faults.
Bianca: Wow, does VA get a lot of Earthquakes?
Lyle: Not really, in the last 30 years there have been more than 150 earthquakes in VA, but most are low intensity events that are seldom felt by people.
Bianca : Where do most of the VA earthquakes occur?Lyle: Most seem to occur in the central and western part of the state.
Catherine: We don’t live near that part of the state. Hmmm. What other things can cause a reading on your seismometer?
Lyle: Anything that shakes the ground can be recorded. Here is a reading of that construction blast the other day.
Bianca : It looks so small, but it created such a big boom.
Lyle: Well, our seismometer or measuring instrument is very sensitive. This is what automobile traffic and even storm waves from the beach look like.
Bianca: That is pretty neat.
Lyle: And the seismometer is buried 230 feet below us. It’s so sensitive, we had to put it in a very quiet place.
Catherine: That's way down there Lyle: Do you want to see the seismogram of a real earthquake?
Bianca: Yes!
(Walk over to another area)
Bianca : What are those little square marks?Catherine: How can you figure anything out?
Lyle: You guys have lots of questions( laughing)
Well, every square ticks off a minute.Bianca: Oh so you can tell when the earthquakes happen and how long they last. Lyle: That’s correct. To most people, these looks like a bunch of squiggly lines. But, when I look at them I see S and P waves. ( showing S and P waves)
Catherine: Like sound waves.Lyle: They are somewhat like sound waves. These are vibrations in the earth.Catherine: That doesn’t look at all like the tremor we felt. Does that mean it wasn’t an earthquake?

Lyle: Not necessarily. A local earthquake could look different from this.
Catherine: We need one of these in our tree house, and then we could measure the next tremor.

Lyle: I think Dr. D is down the hall building a seismograph.
Bianca: Dr. D. A seismograph! We’re there!

Dr. D’s Lab at TCC Bianca Hi, Dr. D. Is this the seismograph you’re building?

Dr. D: That’s right. I’m almost finished. This seismograph is not very sensitive, but it should work to measure the horizontal movement.
Catherine You actually use a plain old brick from a house?Dr D: Yeah sure. Let me start from the beginning. A seismograph measures the shaking of the Earth. To measure this shaking, we take advantage of Isaac Newton’s first law.
Catherine: I think I remember . Isn’t it also called inertia?
Dr. D: I’m impressed. So what is inertia?Catherine: It means that objects at rest stay at rest, and objects in motion remain in motion.
Dr. D: That’s right. The more mass that an object has the more inertia it has, and the more resistant it is to changes in its motion. This brick has a lot of inertia. When the Earth shakes, the base of the seismograph will shake, but the brick ,which is not tied to the seismograph will not shake. This pen over here marks the shaking.
Bianca: Can we try it?
Dr. D: Let’s make an earthquake by shaking the table.
Catherine: It really works. Look at the waves. Did we do that?
Dr. D: You sure did! Here’s a different kind of seismometer. It measures vertical motion, and uses electricity to record the shaking.
Bianca: It looks really different.
Dr. D: Because it has inertia, this magnet hanging on the spring tends to stay still when the frame moves up and down. A magnet moving through a coil of wire produces electricity, which this meter over here records.Catherine :Can we try this one too?
Dr. D: Tell you what, here is a more sensitive seismometer that I bought and have hooked up to this computer.
Bianca. That graph looks a lot like the seismogram that Mr. Lyle showed us.

Catherine: The harder I hit the table, the larger the signal. This is really cool
Bianca: And look at how it vibrates up and down.

Dr. D: Because it gives an electrical signal, it is easy to amplify the signal so that even a small shaking can show up on the computer. Why don’t you take this seismograph back to the tree house and see if you can record another tremor.
Bianca: That’s great Dr. D. We’ll be prepared now.
Dr. D: I have a friend at NASA’s Jet Propulsion Lab in Pasadena, California who uses satellites to measure the movement of the earth’s crust from space. You might want to talk to her in your quest to be earthquake experts.


What’s Up?
What is GPS and how is it used?
What are P and S waves and how do they differ?
What are two types of scales used to measure earthquakes? We’ll find out next in the Case of the Shaky Quake

Segment #3 – Focus Questions In this segment of the Shaky Quake you will be asked these questions.
Will the seismograph help the tree house detectives solve the mystery?

And will the satellites provide the answer?
Tree house
Segment #3
(Catherine) Ummm? I’m not so bad.
(Kali) What?
(Catherine) I’m looking at my field soccer journal and so far in my career I have made 282 field goals and I attempted 670. That means that my shooting percentage is 42.1 percent. That means that I make a goal about half the time. (turn to camera) See you even use math in sports.
(Bianca) Ok… Getting back to business. This is a homemade seismograph on loan from Dr. D. Now we’ll be prepared if there’s another tremor.
(Catherine)(Turn to camera) I don’t know if I would depend on this machine to help us out, it looks rather weak.

(Kali) But maybe this instrument isn’t the only way to detect earthquakes.
(Bianca) Remember, Dr. D told us about JPL and how it monitors crustal movements using satellites. He gave us the name of his friend. I wrote it down. Andrea Donnellan Let’s dial her up
CU See Me with
JPL
Catherine: Hi, we’re the tree house detectives. Dr. D said that you might be able to help us learn more about how crustal movement is monitored.
Donnellan: Sure can. I work with a program that uses GPS to watch the movement of the crust.
Kali: I’ve heard of GPS, but I’m not sure what it is or how it works.
Donnellan: GPS stands for Global Positioning System. It’s a satellite navigation system consisting of 24 satellites. Pilots and boaters use it to plot their course. Geologists use it to accurately measure the position of monitoring stations. Here in Southern California we have a network of 250 stations, similar to this one.
Bianca: How does knowing the position of these stations help you understand earthquakes?
Donnellan: . It shows us the stretching, warping and movement of the crust that is not readily noticeable. (Kali): How accurate is it?
Donnellan: We can measure the positions of points on the Earth to 3 mm horizontally and 7 mm vertically.
(Catherine): That’s small! How does this differ from what a seismograph does?
Donnellan: A seismograph measures earthquakes when they happen. With GPS, we can actually measure the quiet motions of the Earth. That means we can measure the strain buildup as well as the earthquakes themselves.
It is particularly useful in identifying active blind faults.
(Kali): What’s a blind fault?
Donnellan: A blind fault is a break in the crust that doesn’t break through the surface anywhere. Naturally, these faults are not easy to locate or study, and might go unnoticed without the GPS technology?
(Bianca): That’s pretty impressive.
(Turn to camera) I’m glad we have the ability to “see” these faults. Will this technology help to predict earthquakes?
Donnellan: We are integrating data from a lot of different sources into computer simulations. These simulations should help us understand the earthquake process. . We hope to eventually be able to do short term forecasting.
(Catherine): Can you give us an example?
Donnellan: By monitoring all the stations, we can find which faults have the greatest slip rate. The slip rate, typically measured in mm/year, is how fast the two sides of a fault are moving past each other. These faults that have the greatest slip rate may be the locations of future earthquakes.
Bianca: Wish you were able to make a prediction now. Can GPS help us know if we experienced an earthquake in Virginia?
Donnellan: Although GPS uses station displacement to determine the size of an earthquake, it does not measure the actual shaking of the ground like a seismograph does. A seismograph is pretty sensitive and should help you find the answer to your question.
Bianca: Thank you very much Dr. Donnellan.


(Catherine) Cool! I can’t believe the GPS can detect 3 millimeters of movement from space!
(Catherine) Check this out. Come closer.
3 milimeters is only this big.
(Anthony walks in)

(Bianca) Hi Tony. We’re talking about GPS In the future, it might help us predict earthquakes.
(Anthony) Yeah that’s great, BUT, what about problem right now!
(Kali) Dr. Donnellan told us if there was an earthquake in Virginia seismographs would pick it up.
(Bianca) But, we looked at seismograms and we still don’t have a definite answer.
Let’s do some problem solving.
(Tony) I have an idea. Let’s call R.J. and Jacob.
(Catherine) Tell them Hi , I’ve got to go.
I have soccer practice today.
( All) Bye


(Tony) Hi guys! How’s California?

(R.J.) It’s great! Nice, Sunny and we’re also learning a lot at the science fair.
(Jacob) So you’re still trying to solve the tremor problem?
(Bianca) Yes, but, we need your help with the problem board.
(Jacob) Okay, let’s go to it.
(Kali) We know the second set of tremors was not related to the first set.
(R.J.) We know the plate’s movements can cause earthquakes and there are a lot of faults.
(Tony) We know there are faults in Virginia.
(Bianca) We also know other things can cause movement on the seismograph.
(Jacob) Like what?
(Bianca) The seismologist told us that quarry blasts, sonic booms, and thunderstorms can be mistaken for earthquakes.
(Jacob) Thunderstorms? Did you guys have storms that day?
(Anthony) It was cloudy and stormy that day. But, I don’t remember seeing any lightning.
(Kali) But, it did sound like a clap of thunder.
(Bianca) And that would register on the seismograms.
(Kali) Earthquakes don’t make noise so it must have been thunder. Maybe this is our new hypothesis? If there was thunder, then it would cause vibrations on earth.
(R.J.) Don’t throw away the earthquake hypothesis too fast. During my vacation, I’ve been researching earthquakes, and look I just happened to find these accounts of an earthquake in Oklahoma.
( reading accounts)
“I heard something like a loud clap of thunder or something exploding.
Here’s another one. “It sounded like a big truck and it rattled things in my house. .
(Anthony) Great job, Bud. Our competing earthquake hypothesis still survives.
(Jacob) I still think that we need to know if there was lightning and thunder that day
I’ll check with the Weather Service.
(Anthony) We never checked out what the seismologist told us about the p and s waves. I think we should; it might be a clue.
(R.J.) We can help you. We’re supposed to meet Dr. D and his friend, Dr. Tang at the California Academy of Science Museum to see the earthquake room. We can ask him.
(Jacob) Neat. I hope it’s not as real as the hurricane room.
(R.J) I’m sure that we can find out more about earthquake waves at the Museum.
(R.J.) Well. Let’s not just sit here. Let’s get to work.

Dr. D at CA Academy
Jacob:This place is great. Look there’s Dr D.R.J.: Hi Dr D.
Dr. D:Hi guys. Good to see you in San Francisco, California. I understand from the E mail you want to know more about earthquake waves?
R.J and Jacob :Yes.
Dr. D:So I put together some demonstrations for you.
Jacob:Great.
Dr. D: Let’s talk about three different types of waves. The first two are P and S waves. They are body waves because they travel through the body of the Earth.
R.J.: Mr. Lyle showed the other tree house detectives those on his seismogram.Dr. D: P stands for primary or compressional, and S is for secondary or sheer waves. P waves make the Earth vibrate back and forth along the direction of motion. Let me show you with this slinky. (Illustrates P waves with a slinky)
Jacob:That doesn’t look like the kind of wave that I’m used to seeing.( Turning to camera) Like the ocean waves.
Dr. D: The wave you’re used to seeing has an up and down motion or side to side. That would probably be the S, or sheer wave. It looks like this.
R.J.Can we try this?
Dr. D: An important difference between P and S waves is that P waves travel faster than S waves, almost twice as fast.
R.J.: I guess that means that P waves will always arrive first.
Dr. D: That’s right. And this difference in time between the arrival of P and S waves can help us tell find the the epicenter of an earthquake.
Jacob:What’s an epicenter?
Dr. D: It’s the point on the earth directly above the focus, or point where earthquake originates. (NOTE: Could also say place where rocks break, point of rupture, point of fracture, slippage along the fault)
Have you ever heard about counting the seconds between seeing the lightning and hearing the thunderR.J.I have, but I didn’t believe it.
Dr. D: Well, it works because light and sound travel at different speeds. For example, When you see the lightning start counting (Snap) Lightning Appears. Jacob: One thousand one, one thousand two, One thousand three (thunder sound) kids jump back Whoa.
Dr. D The sound arrived 3 seconds after the lightning that means that the lightning is 1 km away. You can do the same kind of thing with P and S waves to find the distance to the epicenter of an earthquake. First you’ll feel the P wave, then seconds later you’ll feel a more powerful “s” wave. Every second you count, means you’re another10 km away from the epicenter.
Jacob: I don’t think I would be counting the seconds if I was in an earthquake!Dr D: The third and slowest of the waves, the surface wave, is the most destructive of them all. Here in California, they have to build buildings to withstand these destructive waves.
R.J.:How do they know how to do that?
Dr. D: One way is for engineers to use shaky tables like this to test their designs. Lets try it out
Jacob:I’ll bet my structure will withstand the greatest earthquake.
R.J.We will see who is the best engineer .
(boys design lego structures and then destroy them with the shaky table)
Jacob I guess that we have a bit more to learn about the power of earthquakes
R.J. Didn’t you tell us that we could experience an earthquake here at the museum?

Jacob: I hope that it’s not like the hurricane room that Bianca and Catherine went through. That must be Dr. Tang over there.

R.J. Dr Tang?
Tang : Tree house detectives?
Jacob: That’s us. Nice to meet you Dr. Tang
Tang: I understand you are interested in experiencing an earthquake.
Jacob; Well, I’m not sure about that. But, we do need to learn more about how experts measure the power of an earthquake.
Tang : One scale that scientists use is called a Richter Scale. It tells us the strength of an earthquake.
R.J. Are there other scales that scientists use?
Tang : Yes, scientists now prefer a more precise scale that’s called the moment magnitude scale. It gives a number to an Earthquake that tells us its total energy released. Jacob: What’s the number of “our earthquake”?
Tang Well, if it was an earthquake, people could feel , it would have to be at least a 2, A moderate earthquake would be about a “5”.
Jacob Wasn’t there a major earthquake here in San Francisco in 1906? What was its number?
Tang: Well, it was a 7.7, but to see what that means, you really ought to experience the earthquake.
R.J. I’m not sure I want to do that.
Tang :Don’t worry, it’s quite safe. We’re going to do it in our earthquake room here at the California Academy of Sciences.
Experience Quake Montage
R.J. Cool! It seemed so real. How do scientists know so much about it?
Tang:Well, we studied people’s diaries and looked at how different houses and churches were damaged and where the earthquake ruptured the ground around San Francisco during this time period.
Jacob I guess observations are important?
( Turn to camera) Your science journal might be valuable evidence one day.
Tang : Yes. Even today, with sophisticated instruments, scientists still want to hear what people experienced. Here take a look at this earthquake questionnaire.
Jacob: Wow! Look at this . They want to know was it difficult to stand or walk?
R.J And did objects rattle or fall off the shelf.
Jacob: Here’s a simple question. What’s your zip code?
R.J. Does it make a difference where you live?
Tang: The effects of an earthquake depend greatly on how far away you are from the source.
Jacob: You mean, the farther away, the less shaking you feel during a quake?
Tang : Yes, but it also depends on what the ground is like.
R.J.: What does the ground have to do with it?
Tang: Let’s look at this gelatin. If I push it even a little bit, it jiggles a lot. Now look at this rock. I can push it, but it doesn’t jiggle at all.
Jacob: I know where I would want to stand during an earthquake—on solid rock!
Tang: Yes, a house built on sand or mud would not do well in an earthquake. Jacob: Thanks so much Dr. Tang. You’ve given us a lot of good information.
(Tang) You’re welcome. Good luck solving your mysterious quake.
What’s Up?
Could a thunderstorm have caused the tremor?
Will P and S waves help solve the mystery?
What should the tree house detectives investigate next?
Don’t miss the conclusion of the case of the Shaky Quake!

Segment 4 /Focus
Questions

In The final episode of the Case of the Shaky Quake, you will be asked these questions.How many earthquakes occur each year?How many seismic stations are necessary to pinpoint the epicenter of an earthquake?What are the differences between meteors, meteorites, and meteoroids?(Kali) Why are you so down?
(Bianca) I called the weather Service and they said that there were no lightning strikes recorded in our area on the day that we felt that last tremor
(Anthony) Maybe I shouldn’t mention that I called another seismologist at Virginia Tech which is about 300 Kilometers away and their seismograph also detected something about the same time we felt the tremor.
(Kali) So, that information doesn’t mean my thunder hypothesis is wrong!
(Anthony) It might. Think about it. The seismologist said the weather was clear that day, no thunderstorms in sight.

(Bianca) Mr. Lyle said his seismographs only detect local thunder.
Well, maybe you’re right.

(Anthony) The seismologist also said eyewitnesses reported seeing a fire ball in the sky and they heard a loud noise.
(Bianca) I don’t remember seeing a fireball that day.

(Kali) Here comes Dr. Textbook
wide shot looking and
waiting
ECU
( Dr. Textbook)
Hello! Dr. Textbook here with some “earth shattering facts.” (Tremor occurs and he looks around.)
You’ll never guess how many detectable earthquakes there are in the world each year. Try 500-thousand. That’s a half million earthquakes a year!

Californians listen up! Every year the Southern Part of California has 10-thousand earthquakes. But, most of them are not felt.

Whew!
Which state is the most earth quake prone? Not California! Alaska! It has a magnitude 7 earthquake every year.

And here’s a trick question? Is there such thing as earthquake weather? NO! Earthquakes happen in the cold, the rain and in the heat! .
Now, let’s see if we can feel one of those 500 thousand earthquakes.
( Pause) Probably not a very good idea!

(Kali) Earthquakes are like hurricanes.
They’re so powerful and can be so deadly.

(Bianca) Look, we have an e -mail from Jacob and R.J. They say Dr. D told them about how P and S waves can help you find the center of the earthquake.

(Anthony) Back to the e -mail, Dr. D says you must have three seismic stations to locate the epicenter.
(Kali) We’ve have two seismic stations; maybe that’s enough?

(Bianca) I doubt it. But, I have an idea. Let’s write the SCI Files Kids club and ask them if they know how to use S and P waves to map an epicenter.

(Kali) We have a response from Roberts Parks Elementary School in Norfolk Va.
(Student) Hi .We’re from Mr. Daryl Ransom’s Third grade class at Roberts Parks Elementary school in Norfolk, Virginia.
Classroom Activity Anthony: Hi, we are the tree house detectives and we see that you are doing an activity to find where an earthquake occurred. Can you tell us about it?
Student: Sure. Our mentors from the Society of Women Engineers helped us with the activity called triangulation.
Kali : It must have something to do with threes.
Student: Yes, we learned that in order to find the origin or epicenter of an earthquake, we needed to have data from three different seismic stations.
Bianca: Did you need any special materials?
Student: No, just a world map, a seismogram, a graph, and a drawing compass.
Anthony: What did you do next?
Student: First, we looked at the seismic recordings and determine when the S and P waves each arrived at the seismic stations.
Kali: How could you tell which one was which?
Student: We know that the P waves travel faster and arrive first. (show graphically) We then found the difference between the two times in seconds. For example, at the Denver, Colorado station, the P waves arrived at 10 hours and 16 minutes and the S waves arrived at 10 hours 18 minutes and 30 seconds.
Anthony: I know. The difference was 2 minutes and 30 seconds.
Student That’s correct. We then used the graph to mark off 2 minutes and 30 seconds along the edge of a piece of paper. We slid the paper along the graph between the S waves and the P waves to find the distance in Kilometers that the waves had traveled.
Kali: How far did the waves travel?
Student: About 1600 kilometers. After finding the distance the waves traveled, we located the city on the map. We used the map scale and our drawing compass to measure that distance. (show students doing this) We placed the point of our compass on the city and drew a circle.
Bianca: Why a circle?
Student: We know that the earthquake occurred 1600 km from Denver, but that could be 1600 km in any direction. So we used the 1600 km as our radius and the earthquake occurred some where along the circle.
Kali: How did you pinpoint the location?
Student: We repeated the steps with the next seismic recording for Terre Haute, IN. (show them doing this)
Bianca: But the two circles intersect at two different points. How can you tell which one is the epicenter?
Student: That’s why you need a third seismic station. Once all three stations are plotted on the map, you find where the three circles intersect. The intersection is the approximate epicenter of the earthquake.
Anthony: I wonder if there is a third seismic stations that recorded our tremor.
Student: If there is, then you can triangulate the data and find the epicenter.
Bianca: Thanks, we really appreciate this. You have been a big help.
( On Camera Line already shot): You're welcome. Goodbye from the NASA SCI Files Kids club at Robert Parks Elementary School in Norfolk, VA.
Tree house
Anthony: They answered one question for us. We really do need three seismic stations, not two to map the epicenter.

Bianca: Is the earthquake our only hypothesis?
( Anthony) It is for me. Just kidding. We need more conclusive evidence that this was an earthquake.
R.J. walks in
R.J: Will this help?
Anthony: R.J. Your back!
R.J. I have this tape of Jacob and me in an earthquake. Bianca: You were in an earthquake?

R.J. No, this is the earthquake room at the Academy. Anthony: That does look like what we saw in our tree house.
Kali This case isn’t as easy to solve as the others.


Bianca No one will confirm that it’s an earthquake. Not even the seismologist.
.

Anthony: Let’s call another seismic station to see if their instruments picked up a tremor. That might help confirm it.

Bianca: I don’t know why but I think it could be something else.

Kali Here comes KSNN. Maybe, they have more information.
KSNN
KSNN Newsroom
TUNE Ladies and gentlemen, we are continuing to investigate the recent tremors. It seems that the quakes felt by our viewers may have had different sources. For more we go live to IM Lissning.
LISSNING (With a lizard who is wearing a lab coat) Ted I’m here with esteemed scientist, Doctor Liz Ard. Doctor Ard, what can you tell us about the events of yesterday?
ARD Well, IM, we have received vibration reports from cities all along the east coast. Many people also saw a fireball, which we now believe was a meteor, entering Earth’s atmosphere. Our tracking cameras were able to record this image (giant pig from restaurant on fire flying through the sky) before the meteor flew out of sight.
LISSNING Amazing! Thank you Doctor. Back to you Ted.
TUNE (Tune is hiding behind his desk) Well, folks, those vibrations were merely giant explosions and huge meteors falling from space. Nothing to worry about. (Ted looks up, gets nervous, and starts to sweat.) Nothing at all… mommy?
(Ted) A meteor? Okay We’ll keep you updated.
Tree house Kali: What is a meteor?

R.J. I can tell you. I have my “M’
Encyclopedia.
Anthony: Of course
R.J. Let’s see a meteor is a small piece of rock that enters the earth’s atmosphere and burns up as it falls.

Bianca: Could this meteor be our new hypothesis?
Anthony:No I don’t think so. We had a tremor, but no fireball.
Maybe we just didn’t see it.
Kali:
Anthony: My notes say it was a cloudy day here. That’s right. VA Tech reported seeing a fireball. But, they also said it was a clear day.
R.J.: I wonder if a meteor could travel faster than the speed of sound.
Bianca: If it did, it could cause a sonic boom, just like an airplane.
R.J. And we learned that sonic booms can cause tremors.
Anthony: That might work. Let’s word the hypothesis like this: if there was a fireball or a meteor and it traveled faster than sound, then it could form a sonic boom and cause the tremor.
Bianca: I don’t think it could make the windows rattle.
Anthony: That’s a pretty far fetched idea. This isn’t SCI Fi.
Turn to camera Kali: No its’ the SCI Files!
Bianca I think we really need to look into the meteor as the possible cause.
We just talked to JPL. Let’s call them again.
SEE U SEE ME

JPL Interview


Anthony:Yeah! We are a little confused on what a meteor actually is. Isn’t it the same thing as a meteoroid and a meteorite?
Baalke:
I’m glad to help you. I’m Ron Ballke. I’m known as a meteorite enthusiast. It’s easy to get the three of them confused. Meteoroids are small pieces of rock, usually from a comet or the collision of asteroids that are moving through space. If a meteoroid enters into Earth’s atmosphere and it burns up, it is called a meteor. People often see these and call them “shooting stars.”
Bianca: People near us reported seeing a fireball. Is a fireball like a shooting star?
Baalke: Yes, a fireball is just the name given to a very bright meteor. They are sometimes so bright that they can even be seen in the daytime.
Kali: So what’s a meteorite?
Baalke: Most meteoroids that enter the earth’s atmosphere burn up completely, but if a meteoroid is large enough, part of it may survive. When it strikes the Earth, it is called a meteorite. These can cause craters such as Meteor Crater in Arizona.
Kali: We understand that a fireball was sighted near our town, and that it might have caused a sonic boom. It this possible?
Baalke: Yes, if it is large enough. The larger size allows meteors to last longer and to penetrate deeper into the atmosphere. Once it gets into the atmosphere, if it is traveling at a speed greater than the speed of sound, then it will cause a sonic boom.
Bianca: I remember from our barking dog’s mystery that sound travels at 340 m/sec so that means it is moving fast!
Anthony: Would a sonic boom from a meteor be powerful enough to cause a seismic reading?
Baalke: Yes, a seismometer can detect a sonic boom from a meteor if it is large enough. However, to hear the sonic boom, you have to be relatively close, typically within 50 miles, but you can see the fireball from about 500 miles away!
R.J: I would love to see one.
Baalke: Most fireballs are not observed because 75% of the Earth is ocean and there aren’t too many people in the middle of the ocean. In July of 2001, there was a fireball that was seen from Virginia to Ontario Canada. And sonic booms were reported by people stretched over more than a 100 miles.
Kali: Wow. This is so cool.
Does JPL track meteors?
Baalke: We don’t formally deal with meteors, but JPL manages NASA’s Near-Earth Object Program. We estimate that 1,000 asteroids and comets, larger than 1 km that approach the earth. Our goal is to locate at least 90% of these objects within a decade and to closely monitor them and analyze their orbits for future potential impacts with earth.
Anthony: This has been a lot of help Mr. Baalke. I think we have found the answer to our mystery.
Baalke: Dr. Peter Brown at the University of Western Ontario is an expert on fireballs. You might want to send him an e-mail an ask him some more questions.
Bianca: Thanks so much
Baalke: Any time.
Tree house Kali: I’ll send Dr. Brown an E mail.

R.J. Wow, I didn’t know there really could be sonic booms from meteors.

Bianca: We talked about sonic booms being the answer.
Anthony: But, not sonic booms from a meteor

Kali: We got an e-mail back from Dr. Peter Brown. He says that it probably would take a meteoroid of at least several hundred kilograms, which is the size of a small chair, to produce a sonic boom strong enough to be recorded by a seismograph.
Bianca: Look at this. He also says that if large meteoroid has enough energy and gets deep enough into the atmosphere, it can produce a very substantial shaking of the ground or windows.
Bianca: This must be it (Turn to camera) I think we have the answer!
R.J. I wonder what Dr. D would think about this.
Let’s go see him.

DR D’S LAB Tree house

DR D’S LAB Kali: I’ll send Dr. Brown an E mail.

R.J. Wow, I didn’t know there really could be sonic booms from meteors.

Bianca: We talked about sonic booms being the answer.
Anthony: But, not sonic booms from a meteor

Kali: We got an e-mail back from Dr. Peter Brown. He says that it probably would take a meteoroid of at least several hundred kilograms, which is the size of a small chair, to produce a sonic boom strong enough to be recorded by a seismograph.
Bianca: Look at this. He also says that if large meteoroid has enough energy and gets deep enough into the atmosphere, it can produce a very substantial shaking of the ground or windows.
Bianca: This must be it (Turn to camera) I think we have the answer!
R.J. I wonder what Dr. D would think about this.
Let’s go see him

(R.J.): Hi, Dr. D. We think we have solved our problem.
DR D: Great. Was it an earthquake?

R.J.: We’re pretty sure that it wasn’t an earthquake. We think that we have proof it was a sonic boom produced by a meteor.
Dr D: A meteor? How did you come to that conclusion?

(Catherine looking at Anthony): It wasn’t easy. Anthony kept insisting it was an earthquake.
I knew it was a sonic boom all along.



Jacob: Not really. We dismissed the sonic boom hypothesis in the beginning because planes don’t generally fly that fast any more over land.

Anthony: Eventually, we came back to the idea of a sonic boom when KSNN reported that a fireball had been seen at the same time the vibrations were felt.

Catherine: When we heard that the people at Virginia Tech saw a fireball, heard a sonic boom, and recorded a seismic reading just a few minutes before we did, it still didn’t register with us that a meteor could be the answer.
Anthony: That’s because it was overcast that day and we didn’t see a fireball.
Jacob: Who would have thought that it would be a fast moving chunk of rock? (Turn to camera) Would you think?Catherine: Then we checked with some experts who told us that meteors can cause sonic booms.
Dr. D: Well, it sounds like you have learned several important things. You’ve learned not to dismiss a hypothesis too quickly as you did with the sonic boom hypothesis.Anthony: Yes, and VA Tech practically gave us the answer, but we didn’t even consider it.
Dr. D: Sometimes the answer is right in front of you, but you can’t always see it. The problem is that you have not completely solved your mystery.
R.J.: We haven’t? What do you mean? We have lots of evidence.
Jacob: We know that it wasn’t a construction blast.
Anthony: We even ruled out an earthquake for a number of reasons.
Catherine: We also eliminated thunder since there weren’t any lightning strikes that day.
Jacob: So Dr. D isn’t the fireball explanation the best one?
Dr. D: Well, to quote the greatest detective of all time, Sherlock Holmes, “Eliminate all other factors, and the one which remains must be the truth."

R.J.: Isn’t that what we did?
Anthony: Well, I guess we also didn’t completely rule out earthquakes..
Dr. D: You have shown that a fireball can cause a sonic boom and that a fireball was seen elsewhere, but you don’t yet have enough evidence to prove that the fireball caused the vibrations that you felt.
Dr. D: In science, you quite often go with the best explanation, even though it is not proven beyond question. Anthony: All who agree that this is the best explanation that we can find say aye.
AYE
Dr. D: Even though you had a lot of dead ends, Along the way, you’ve learned a lot about earthquakes. Sometimes the journey is just as important as the destination.
R.J.: You mean, what we learn along the way is as important as reaching a conclusion.
DR. D: Something like that. Congratulations
Vibration
Jacob: Oh no! It’s happening again!
Anthony: Yes!
(Credit Roll)

 

 
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