Description
Transcript: Radioactivity is the process by which we've estimated the age of the Earth. It's also crucial in understanding how the Earth works and the source of geological activity. The interior rocks of the Earth contain small concentrations of radioactive elements or compounds. The radioactive decay process releases energy in the forms of particles and radiation. This energy suffuses through the rock and melts the rock driving geological activity. In any sufficiently massive planet, radioactive decay of the interior rocks causes geological activity. Thus leads to a situation were the surface of a planet can be solid while parts of the interior are liquid. In a sense radioactivity is the engine that drives geological activity.
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