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Things That Fall From the Sky

Things That Fall From the Sky. Comets & Meteors. Questions from Before. What is Jupiter made of? Gas (hydrogen-rich gasses and helium), but in a liquid form. Can rocks fall from the sky? Yup. Questions for Today. What is a meteor? How old is the Earth?

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Things That Fall From the Sky

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  1. Things That Fall From the Sky Comets & Meteors

  2. Questions from Before • What is Jupiter made of? • Gas (hydrogen-rich gasses and helium), but in a liquid form. • Can rocks fall from the sky? • Yup.

  3. Questions for Today • What is a meteor? • How old is the Earth? • Will we all be killed by a giant asteroid?

  4. Meteors: Things That Fall From the Sky

  5. Meteors • There are many small chunks of matter orbiting the Sun. • A piece that is in space is a meteoroid. • A piece that burns up in the Earth’s atmosphere is a meteor (a bright streak of light). • A piece that lands on Earth is a meteorite.

  6. Meteors • Many “meteor showers” are associated with comets.

  7. Dust from Comets • The dust tail contains small particles evaporated from the comet. • These particles remain in orbit about the Sun. • If the Earth passes through the “dust cloud”, then several meteors may be seen.

  8. Meteor Showers • During periods of high meteor activity, most of the events appear to come from one spot on the sky.

  9. Meteor Showers • During periods of high meteor activity, most of the events appear to come from one spot on the sky. • This point is roughly where the comet’s tail was.

  10. Meteor Showers • During periods of high meteor activity, most of the events appear to come from one spot on the sky. • This point is roughly where the comet’s tail was. Dust particles enter the atmosphere and burn up, causing a streak of light.

  11. Rocks from Space • Some early cultures were aware that rocks sometimes fell from the sky. These items had great religious value, e.g. the Black Stone of Ka’aba.

  12. Rocks from Space • Some early cultures were aware that rocks sometimes fell from the sky. These items had great religious value, e.g. the Black Stone of Ka’aba. • “Enlightened” scientists in the 18th and 19th centuries declared that stones cannot possibly fall from space. It was all primitive superstition.

  13. Rocks from Space • Thomas Jefferson said: “It is easier to believe that two Yankee professors [Profs. Silliman and Kingsley of Yale] would lie than that stones would fall from the sky.”

  14. Rocks from Space • Thomas Jefferson said: “It is easier to believe that two Yankee professors [Profs. Silliman and Kingsley of Yale] would lie than that stones would fall from the sky.” • Jefferson was wrong: stones do fall from the sky.

  15. Rocks from Space • Evidence that rocks fall from space:

  16. Rocks from Space • Evidence that rocks fall from space: • There have been eyewitness accounts of impacts.

  17. Rocks from Space • Evidence that rocks fall from space: • There have been eyewitness accounts of impacts. • In many cases, the mineral composition of samples indicates the material cannot be native to Earth.

  18. Rocks from Space • Evidence that rocks fall from space: • There have been eyewitness accounts of impacts. • In many cases, the mineral composition of samples indicates the material cannot be native to Earth. • Most older samples are iron, most “fresh” samples are stony material.

  19. Rocks from Space

  20. Where to Find Meteorites • Antarctica is one of the best places to find meteorites on Earth, owing to the high contrast (black rocks on white snow). http://www-curator.jsc.nasa.gov/curator/antmet/program.htm

  21. Where to Find Meteorites • Over time, meteorites tend to get concentrated in certain areas because of large-scale ice flows. http://www-curator.jsc.nasa.gov/curator/antmet/program.htm

  22. Meteorites • Most older samples are iron.

  23. Meteorites • Most older samples are iron. • Iron is dense and not easily weathered.

  24. Meteorites • Most older samples are iron. • Iron is dense and not easily weathered. • Most “fresh” samples are composed of stony materials.

  25. Meteorites • Most older samples are iron. • Iron is dense and not easily weathered. • Most “fresh” samples are composed of stony materials. • This material is easily weathered and does not last long on the Earth’s surface.

  26. Rocks from Space • Why is are meteorites useful?

  27. Rocks from Space • Why is are meteorites useful? • They are material samples from outside the Earth that can be analyzed in the laboratory.

  28. Rocks from Space • Why is are meteorites useful? • They are material samples from outside the Earth that can be analyzed in the laboratory. • We can measure the age of the solar system by studying meteorites.

  29. Radioactive Decay • A chemical element is uniquely determined by the number of protons its nucleus has. For example, hydrogen has 1 proton, carbon has 6 protons, etc.

  30. Radioactive Decay • A chemical element is uniquely determined by the number of protons its nucleus has. For example, hydrogen has 1 proton, carbon has 6 protons, etc. • Different isotopes of the same element differ only in their number of neutrons. For example 12C has 6 protons and 6 neutrons and 14C has 8 neutrons and 6 protons.

  31. Radioactive Decay • Different isotopes of the same element differ only in their number of neutrons. For example 12C has 6 protons and 6 neutrons and 14C has 8 neutrons and 6 protons. • A radioactive isotope is an isotope prone to spontaneous change.

  32. Radioactive Decay • Different isotopes of the same element differ only in their number of neutrons. For example 12C has 6 protons and 6 neutrons and 14C has 8 neutrons and 6 protons. • A radioactive isotope is an isotope prone to spontaneous change. • 14C changes into 14N • 40K changes into 40Ar

  33. Radioactive Decay • A radioactive isotope is an isotope prone to spontaneous change. • 14C changes into 14N • 40K changes into 40Ar • The decay rate for a given isotope is fixed and can be measured in the laboratory. The rate is usually given as a “half life”, which is the amount of time required for half of a given sample to decay.

  34. Radioactive Decay • The decay rate for a given isotope is fixed and can be measured in the laboratory. The rate is usually given as a “half life”, which is the amount of time required for half of a given sample to decay. • The half life can be as short as a fraction of a second or as long as billions of years.

  35. Radioactive Decay • For a given atom, there is a certain probability that it will decay.

  36. Radioactive Decay • For a given atom, there is a certain probability that it will decay. • For a large collection of atoms, a well-determined half life emerges from the statistics of a large number of events. Image from Nick Strobel (http://www.astronomynotes.com)

  37. Radioactive Decay • Example: the half life of 40K is 1.25 billion years. Suppose we start with 1 kg. • In 1.25 billion years, we have 1/2 kg of 40K and 1/2 kg of 40Ar.

  38. Radioactive Decay • Example: the half life of 40K is 1.25 billion years. Suppose we start with 1 kg. • In 1.25 billion years, we have 1/2 kg of 40K and 1/2 kg of 40Ar. • In 2.50 billion years, we have 1/4 kg of 40K and 3/4 kg of 40Ar.

  39. Radioactive Decay • Example: the half life of 40K is 1.25 billion years. Suppose we start with 1 kg. • In 1.25 billion years, we have 1/2 kg of 40K and 1/2 kg of 40Ar. • In 2.50 billion years, we have 1/4 kg of 40K and 3/4 kg of 40Ar. • In 3.75 billion years, we have 1/8 kg of 40K and 7/8 kg of 40Ar.

  40. Radioactive Decay • My measuring the relative amounts of the radioactive “parent” isotope to the resulting “daughter” isotope in a rock, one can measure the amount of time since the rock sample solidified.

  41. Radioactive Decay • My measuring the relative amounts of the radioactive “parent” isotope to the resulting “daughter” isotope in a rock, one can measure the amount of time since the rock sample solidified. • In practice one looks at many parent/daughter combinations, and also looks at stable isotopes of the parent and/or daughter.

  42. Radioactive Decay • The oldest rocks on the Earth were solidified about 4 billion years ago.

  43. Radioactive Decay • The oldest rocks on the Earth were solidified about 4 billion years ago. • The oldest rocks from the Moon were solidified 4.4 billion years ago.

  44. Radioactive Decay • The oldest rocks on the Earth were solidified about 4 billion years ago. • The oldest rocks from the Moon were solidified 4.4 billion years ago. • The oldest meteorites solidified 4.55 billion years ago.

  45. Radioactive Decay • The oldest rocks on the Earth were solidified about 4 billion years ago. • The oldest rocks from the Moon were solidified 4.4 billion years ago. • The oldest meteorites solidified 4.55 billion years ago. The Sun and the solar system are about 4.6 billion years old.

  46. Rocks from Space • Why is are meteorites useful? • They are material samples from outside the Earth that can be analyzed in the laboratory. • We can measure the age of the solar system by studying meteorites.

  47. Next:Minor Planets or Asteroids

  48. Minor Planets or Asteroids • The region between between Mars and Jupiter is populated by thousands of small rocky bodies called minor planets or asteroids.

  49. Minor Planets or Asteroids • The region between between Mars and Jupiter is populated by thousands of small rocky bodies called minor planets or asteroids. • Ceres, the largest one with a diameter of 1000 km, was discovered in 1801.

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