Craters and Meteorites
|Areas of Science||
|Time Required||Very Short (≤ 1 day)|
|Material Availability||Readily available|
|Cost||Very Low (under $20)|
AbstractHave you ever heard someone say that the moon is made of cheese? Even though the craters on the surface of the moon resemble holes in Swiss cheese, we know that this common myth is not true. Find out how craters are formed and why they are different sizes by doing this simple science project.
ObjectiveInvestigate how the size of a meteorite is related to the size of the crater it makes upon impact.
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Last edit date: 2020-06-23
Craters are round, bowl-shaped depressions surrounded by a ring, like the one shown in Figure 1. They are made when a meteorite collides with a planet or a moon. The craters are what make our moon look like Swiss cheese. Each round hole is the place where a meteorite impacted, or hit, the surface of the moon, so craters are often called impact craters. Often, the meteorite that creates a crater explodes on impact, so the crater is an empty reminder of the collision.
Figure 1. This is a picture of the Barringer Crater in the desert of Arizona. (David Roddy, USGS)
There are meteoroids traveling around throughout space, and all of the moons and planets have been impacted by meteorites since the formation of our solar system. (Note: they are called meteoroids when they're still in space, and meteorites when they land on a planet or moon). On Earth, we only see a few impact craters because of a couple of different reasons. First, most meteoroids never reach the Earth's surface because they burn up in the atmosphere. This is what we are seeing when we watch a shooting star during a meteor shower (meteor refers to the visible streak of light). Second, impact craters from meteorites can be changed by geological forces (like earthquakes and continental movements), or eroded away by atmospheric forces (like wind or rain). There is no atmosphere on the moon, which means that falling meteoroids do not burn up and there is no weather to erode away the craters. In fact, the footprints of the astronauts who landed on the moon over 30 years ago are still there, perfectly preserved!
Where can you find the few impact craters on the Earth? There are only about 170 scientifically-confirmed impact craters on the Earth. Not all of them are obvious because most are eroded, covered by sediment, or under water. Each crater has to be identified using several different kinds of clues. First, geological clues are found by looking for pieces of the exploded iron-rich meteorite, or for glass that formed during the impact. Satellite imaging can be used to visualize crater formations that are beneath the Earth's surface or a body of water. Finally, chemical evidence is used to date the crater and find traces of elements that are more common in space than on our planet.
By piecing together this evidence, scientists can study craters on Earth and link them to different periods of Earth's history. This involves many different types of scientists, including astronomers, geologists, chemists, paleontologists, and meteorologists (who actually study weather, and not meteorites). This has led to an interesting hypothesis being proposed about the formation of a sea, the extinction of the dinosaurs, and even the origins of life!
The craters on both the Moon and Earth come in many sizes. And some are very deep, while others are shallow. Have you ever wondered why? Vanessa and Chris from DragonflyTV did, so they conducted a science project to figure out how meteorite impacts can create so many different-looking craters. They hypothesized that if meteorites hit with different speeds, they would create craters with different depths and sizes. Do you think they were right? Vanessa and Chris really used their marbles for this project—watch the video and find out!
Speed is not the only meteorite variable that could change the look of an impact crater. In this science project you will investigate whether or not the size of a crater depends upon the size of the meteorite. To test this, you will use different sized, nearly spherical objects as your "meteorites," like the objects shown in Figure 2. What types of clues will you look for in your investigation? How will studying an impact crater give you information about the collision, even if the meteorite is no longer there? Are there other clues of a meteorite impact that are important?
Figure 2. In this astronomy science project, you will use different sized, nearly spherical objects, like the ones shown here, to act as your "meteorites." How will the size of the meteorite affect what kind of crater it makes?
Terms and Concepts
- Impact crater
- How do you think the size of a crater is related to the size of the meteorite?
- What is the difference between a meteor and a meteorite?
- What is a shooting star?
- How is an impact crater formed?
- Twin Cities Public Television. (2006). Moon Craters by Vanessa and Chris. PBS Kids Go! DragonflyTV. Retrieved May 14, 2008.
- Harvey, Samantha, et al. (2013, July 2). Meteors & Meteorites: Overview. National Aeronautics and Space Administration (NASA). Retrieved July 11, 2013.
- Line, Brett. (2013, February 14). Asteroid Impacts: 10 Biggest Known Hits. National Geographic. Retrieved July 11, 2013.
- Lunar and Planetary Institute. (n.d.). Explore! Shaping the Planets: Impact Cratering. Retrieved July 11, 2013.
- Assimov, Isaac. 1990. Library of the Universe: Projects in Astronomy. Milwaukee, WI: Gareth Steven's Inc.
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Materials and Equipment
- Different-sized objects that are nearly spherical (at least 3 total), such a rubber ball, a baseball, and a piece of roundish fruit.
- Tip: Solid objects may work better than hollow ones.
- Note: Smaller objects, such as marbles and beads, will not work well for this science project unless you use metal or magnetic balls and a magnet to carefully remove them, as was shown in the DragonflyTV video in the Background.
- Ruler, metric
- Cardboard box; it should be larger than a shoebox and fairly deep. Something like a small moving box would be perfect.
- Flour (10-lb bag)
- Cocoa powder
- Flour sifter or sieve
- Optional: Graph paper
- Lab notebook
- In your lab notebook, make a data table like Table 1.
- Be sure to include the types of objects that you will be testing.
- Using a ruler, measure the diameter of each of your nearly spherical objects (in centimeters [cm]). The diameter is the distance across the middle of the sphere, from one side to the other. Write your measurements in the data table in your lab notebook. Each object will serve as a "meteorite" in this science project.
|Object||Diameter of Object
|Diameter of Craters|
|Average Crater Diameter
- Prepare your meteorite landing area.
- Slowly pour a 10-lb bag of flour into the cardboard box. Shift the box from side to side to evenly distribute the flour. The flour should be a depth of at least 5 cm in your box. If there is not enough flour, you can either transfer the flour to a smaller box, or add another bag of flour.
- Use a sifter or sieve to add a thin layer of cocoa powder.
- When you are done preparing it, your box should look similar to the one in Figure 3.
Figure 3. Your prepared box should look similar to this one.
- Now drop one of your "meteorites" into the box by holding the object out at arm's length over the box and letting go. Use the ruler to make sure you drop the meteorite from a height of 50 cm above the flour.
- After the "meteorite" impacts the flour, carefully remove the object without disturbing the "crater" left behind.
- Repeat steps 4 to 5 two more times using the same object, each time in a different spot in the box. Remember to drop the meteorite the same way and from the same height each time for accurate results. You should now have three craters made by the first object.
- Measure the diameter of the first crater by measuring the distance across the center of the depression in the flour, as shown in Figure 4. Be very careful not to disturb the flour and cocoa with your ruler, by breathing too hard, or by shaking the box. Write the diameter of the first crater in the data table in your lab notebook.
Figure 4. Measure the diameter of the impact crater by measuring the distance across the center of the depression, as indicated here with the black lines.
- Repeat step 7 for the other two craters, writing each measurement in the data table.
- Calculate the average crater diameter by adding up the three measurements and then dividing your answer by three. Write the answer in your data table.
- Prepare your box for the next "meteorite".
- Mix the cocoa into the flour.
- Shake the box from side to side to even out the flour until it is smooth and level.
- Add a new thin layer of cocoa.
- Repeat steps 4-10 for all of your objects, each time recording the diameter of the three craters and the averages in the data table in your lab notebook.
- Be sure to always drop the meteorites the same way and from the same height so that your results are accurate.
- Now make a graph of your data.
- You can make a graph by hand using graph paper or use a website like Create a Graph to make a graph on the computer and print it.
- On the left axis (y-axis), plot the average diameter of the crater (in cm), and on the bottom axis (x-axis), plot the diameter of the meteorite (in cm).
- What size craters did the smallest objects make? What size craters did the biggest objects make? Do you notice any pattern between the size of the crater and the size of the meteorite? What do you think your results tell you about how the diameter of a meteorite is related to the diameter of the crater it makes upon impact?
If you like this project, you might enjoy exploring these related careers:
- Meteorites are very dense, iron-rich materials. Even slight changes in size can result in large changes in overall weight of a meteorite. Do small meteorites and large meteorites make the same-sized craters? How is the impact of a crater affected by the weight of the meteorite? You can do an experiment by weighing the different objects to see if the weights of the objects are correlated to the size of craters they produce. The trick to this experiment is to find similarly sized, but differently weighted objects to use as meteorites.
- How does the impact of a crater change in different types of surface material? You can do an experiment using different types of material, like sand, cornmeal, clay, dirt, ash, salt, etc. How do impact craters form in different types of surface materials? What can this tell us about the geology of a crater? Can this information be used to predict the surface properties of other planets?
- Meteorites move at different speeds through space, depending upon many factors, like the origin, size, or composition of the meteorite. This means that meteorites impact the planet at different speeds. Can this change the way an impact crater is formed? How is the size of a crater related to the speed of a meteorite? You can do an experiment to investigate this by using a ladder to drop a "meteorite" from different heights above the landing pad. As you drop an object from a higher distance, the object will be moving faster when it hits the surface. Will the size of the crater change as you drop the object from a higher distance?
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