Little Things on Planets
May 20th, 2010 by christine
Earth has a very strong atmosphere.
Q&A with Tom Overton of Gems and Gemology Magazine and Wendy Van Norden of National Earth Sciences Teacher Assn.
BY JOSEPHINE
Earth is the only planet that has life, because it is in the perfect spot. Any closer to the sun, and it would be too hot and things would die. Any farther away from the sun, and the oceans would freeze. Tom and Wendy answered my questions about planets and the atmospheres of different planets.
Q: Can you tell how old a planet is?
Tom: It’s not possible to determine exactly how old something like a planet is. However, scientists can get a good estimate by measuring the age of the planet’s rocks and applying that to what they know about how planets form. One the most useful methods is a technique called radiometric dating or radioisotope dating. A radioisotope is an element that, over time, can turn into another element. Because scientists have extensively studied all the elements in nature, they know how long it takes for one radioisotope to turn into something else. So, if a geologist finds a rock that is composed of a mixture of one radioisotope and the element that it turns into, by measuring the amounts of each, they can determine how long it has been since the radioisotope was pure. Some radioisotopes turn into other elements very quickly; others take many, many years. When working with very old rocks, geologists look for an element called uranium, which slowly turns into lead over billions of years. By measuring the uranium and lead in these rocks, geologists know that the oldest rocks on earth are about 4.4 billion years old.
Wendy: We assume that all of the planets formed at the same time that the solar system formed. (Pluto is a possible exception.) We base the age of the earth on the age of meteors and the moon that formed at the same time as the solar system and upon our oldest rocks on earth. We can date the rocks and meteorites by radiometric dating. Some of the minerals in the rocks contain radioactive elements, and over time, those radioactive elements decompose into different elements. By seeing how much has decomposed and knowing the rate of decomposition, we can figure out that the moon rocks and meteorites are 4.55 billion years old. The oldest rock that we found on earth is 4.4 billion years old. So we assume that all the planets of our solar system are 4.55 billion years old. However, now we know that there are planets around other suns, and we have no way of knowing their age (yet)!
Q: Are we the only planet with gravity? If we are, why?
Tom: All objects have gravity—even you. Gravity is a force of attraction exerted between two objects. If you have only one object, there would be no detectable gravity. However, any two objects that are close enough together will exert a gravitational force on each other. The strength of the force depends on how big the two objects are and how close together they are. However, gravity is a fairly weak force compared to other forces scientists are aware of, so it takes a very large object like a moon, planet, or star to generate a gravitational force strong enough for you to feel. It is gravity that keeps the moon in orbit around the earth, and the earth in orbit around the sun.
Wendy: Every planet has gravity. In fact, everything with mass has gravity, even you! The more mass a planet has (like Jupiter), the more gravity it has.
Q: How hot is lava on earth?
Tom: Lava is melted rock, and rock has to get very hot in order to melt. However, there are different types of lava, each of which can exist at different temperatures. Bright red liquid lava that you might see spurting out of a volcano is the hottest, over 1,200 degrees Celsius. Other types of lava are darker and thicker, and might be around 700 to 900 degrees. The behavior and melting temperature of lava is determined by its chemical composition. Hot, runny lava is high in iron and magnesium, while thicker, chunkier lava is high in silica and aluminum.
Wendy: The temperature of lava can depend on the kind of lava. The lava of Hawaii that creates the black rock called basalt, can be over 1,000 degrees Celsius, while the kind of magma that creates granite, an important rock of the earth’s crust can be about 800 degrees Celsius. You don’t get to see that kind of magma very often, because instead of just flowing down the side of a volcano, it tends to erupt violently, like at Yellowstone.
Q: Is the moon really just a part of the earth, or is it separate?
Tom: The moon is not physically part of the earth. However, some scientists think it might once have been. There are several theories about how the moon formed. Some scientists think it was a very small planet that was captured by the earth’s gravity long ago. Others think it formed at the same time as the earth, from the same cloud of gas and dust. However, the most popular theory today is that the early earth was struck by another planet soon after it formed, and from that, a large mass of rock was thrown into orbit around the earth. That mass of rock eventually formed into the moon. So in a way, the moon may be a part of the earth that got knocked loose.
Wendy: The most accepted theory about the formation of the moon states that early earth was hit by a planet the size of Mars. This ripped a big chunk of the earth, which formed the moon.






