Description
Transcript: Radioactive carbon dating is the way we measure the age of formerly living things. Every living thing takes in carbon either in the food that it eats or absorbing it from the carbon dioxide in the atmosphere. Most of the carbon from the atmosphere is in the stable form carbon-12, but one in a million molecules of carbon in the atmosphere involve carbon-14, the radioactive form. The radioactive form of carbon, carbon-14, decays with a half-life of 5700 years to nitrogen-14. When any living thing dies it stops ingesting carbon, and so the amount of carbon-14 is fixed at a particular value. The rate at which it changes to nitrogen-14 therefore gives the age of the object. Carbon dating has been used to date the age of the oldest trees on Earth and has been used, for example, to show that the Shroud of Turin was a fake. It's routinely used to measure the age of formerly living things.
Transcript: Earth’s atmosphere is unique within the solar system mostly because of the nitrogen and oxygen that form the bulk of the Earth’s atmosphere: 75 percent nitrogen, 20 percent oxygen, plus carbon dioxide, argon, water vapor and other trace gasses. The weather on the Earth is generated...
Published 07/20/11
Transcript: The ancient Greeks knew about loadstones. These were curtain rocks which, when suspended in a fluid, would appear to line themselves in response to a mysterious force. That mysterious force was magnetism, first understood through the experimentation of the physicist Michael Faraday....
Published 07/20/11
Transcript: Cratering affects the evolution of planets. The cratering history of the Earth has varied over its history. Cratering was much stronger in the first half billion years when there was plenty of debris left over from the formation of the solar system. When you look at the Moon we are...
Published 07/20/11