Formation of the Solar System (Ch. 8)_ Guided Reading Questions

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Apr 3, 2024

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Mackenzie Jackson 1. What happened to the shape and to the temperature of the solar nebula as it started spinning faster? When the nebula started to spin faster, it flattened out and created a disk but it also started to become more dense and increased in temperature in the middle which causes it eventually to turn into a star which later became the Sun. 2. What explains the orderly motions of our solar system today? The orderly motions of the solar system can be explained by the fact that the solar system began in a flattened spinning cloud of dust and gas. 3. (p. 221) What sort of radiation do we detect from nebulae that are forming new star systems? We expect infrared radiation from the gas emitting thermal radiation. 4. Figure 8.4 (p221) What do we call such a disk? What are the concentric gaps in the disk (not the bright parts of the disk)? We call the areas or concentric gaps around the the disks the probable planet forming location. 5. Why are there two major types of planets? Your explanation should include the “frost line”. The two major types of planets are terrestrial and jovian planets. The main difference between these two types is that terrestrial planets were formed in the warmer inner part of the disk while jovian planets were formed in the colder outer regions. The frost line indicates where the warmer region ends and where the colder outer regions begin. 6. (p. 222) What is condensation and how is this related to forming planets? Condensation is the process by which a solid or liquid forms from a gas. This only matters when talking about the formation of planets because the closer or more inner a planet was forming explains the gas concentration while planets that were formed outside of the frost line due to cooler temperatures, were able to condense and rocks and hydrogen compounds were formed forming planets 7. (Table 8.1) Look at the four categories that the ingredients of the solar nebula fall into. Which category is dominant and why do you think that is?
The category that is dominant is hydrogen and helium gas and this is because stars need hydrogen and helium to burn to emit light and thermal radiation so it required the atmosphere around nebulae to be very abundant in hydrogen and helium. 8. (p. 223) Why did terrestrial planets end up being so small? These planets tend to be much smaller because the amount of metal and rock make up such a small portion of the original nebula. 9. (p. 223 and Fig. 8.6) What is accretion? The process of smaller items coming together to make larger objects while explains the formation of terrestrial planets 10. (p. 224) Why are Jovian planets so large? This is because Jovian planets contain large parts of hydrogen and helium gasses which are very abundant in the original nebula. 11. (p. 225) What happened to the material in the Solar nebula that was not incorporated into planets, asteroids or comets? It was cleared away by high energy radiation from the Sun and a solar wind that blew outwards in all directions. 12. (p. 226) Where are most asteroids found? Where are most comets found? Most asteroids are found grouped in the asteroid belt while comets end up in the Kuiper belt or the Oort cloud. 13. (p. 226) Why do we see craters on the Moon? We see craters on the Moon because they’re proof of the heavy bombardment and this was when many leftover planetesimals collided with other planets and left scars. 14. (p. 226) How did our Moon form? What size was the object that collided with Earth? How do we know this? A Mar sized object collided with the Earth and this blasted Earth’s outer layers into space. Some debris rains back down on Earth while some other debris accrete and become the Moon. 15. (p. 231) What does radiometric dating tell us? It is the method on how we measure the age of a rock and it's based on the number of atoms and isotopes a rock has. 16. (p. 232) How old is the solar system and what is this number based on?
The solar system is said to be approximately 4.5 billion years old and this is due to the dating of the oldest isotopes.
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