When rocks are formed, usually from lava flows, the magnetic orientation of them is set as they solidify. As these rocks are affected by continental drift and other factors such as earthquakes, the original magnetic orientation remains.
Using the known strengths of the earth's magnetic field over time, it is possible to then tell where these rocks originally emerged.
•The magnetic orientation of rocks of different ages can be compared to get an idea of how the position of a continent has changed over time. This is the exact answer out of the book.
There is nothing -_-
Earths magnetic orientation is locked into the rock when the rock cools
The Earth's magnetic field. This is proven by measuring the magnetic orientation of the rocks as you move away from the Mid ocean Ridge.
Although Lodestone is a naturally occurring magnetic rock, not all magnetic rocks are known as lodestone, and it is only magnetized because of the magnetite mineral in it.
•The magnetic orientation of rocks of different ages can be compared to get an idea of how the position of a continent has changed over time. This is the exact answer out of the book.
The orientation of a rocks magnetic field can tell you it's relative age.
There is nothing -_-
The orientation of a rocks magnetic field can tell you it's relative age.
There is nothing -_-
There is nothing -_-
There is nothing -_-
There is nothing -_-
Earth's magnetic orientation is locked into the rock when the rock cools
Earths magnetic orientation is locked into the rock when the rock cools
Earths magnetic orientation is locked into the rock when the rock cools
The seafloor spreads apart, creating new rocks that record magnetic orientation. Small grains of magnetite on the volcanic basalt (ocean floor) have magnetic properties.