Description
Transcript: There are three basic types of rocks found on the Earth. The first are called igneous rocks. These form from molten material that is cooled and solidified. They are very common in the rocks of the Earth's surface. Granite and basalt are two examples. Earth is a restless place, and the second major type is called sedimentary rocks. You might think that wind, sun, and rain can have little effect on something as hard as a rock, but acting over millions of years, erosion can take an enormous toll on a surface of a rock. Wind and rain cause erosion, and erosion acting over millions of years breaks down rocks and turns it into small particulate matter that is washed by rain and rivers down to the ocean and into stream beds. These layers, as they're deposited and compressed, create sedimentary rocks. Two examples are sandstone and limestone. The third major type of rocks are metamorphic rocks. Earth is a restless place in its interior as well, and very few of Earth's rocks have remained unchanged for the history of the Earth. Metamorphic processes occur when igneous or sedimentary rocks are modified by extreme heat or pressure or sometimes hot water in the presence of acidic solvents. These materials fundamentally change the structure of the rock. Marble is an example.
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