We All Have Our Faults Earthquakes are powerful movements
of the earth. They can be small, only a quiver or shudder. Or they can be
quite large and harmful. What exactly is an earthquake and why in the world
does the earth move so much?
The earth's crust is separated into enormous plates that are constantly
moving. All of our continents and oceans ride on these thick plates as they
crash together, move apart or slide by each other. The area where the plates
meet is called a fault line. Because the earth is constantly expanding,
the currents of molten rock underneath the plates build up pressure which
is released through slight shifts.
Plates rubbing together
on fault lines cause earthquakes. The biggest earthquakes occur at the plates'
edges. An instrument called a seismograph records the earth's movements.
Right this minute, there's probably an earthquake happening somewhere in the world. The good news is that most are very small, so small we don't notice them. But a few are so violent that they can collapse buildings, break gas and plumbing pipes, and trigger events that start fires and landslides. Earthquakes in the ocean can cause giant waves called tsunamis to roll inland and destroy coastal property. ROCK & ROLL ZONES The areas in the world that are on or near fault lines have more earthquakes. The people that live in earthquake zones need to know what to do in case of an earthquake. Do you live in an area that has earthquakes? If you do, it's important that you and your family are prepared. Here's some things that you should know:
Books: James, Ian. Planet Earth, (Great Britain, Dempsey Parr, 1998). Steele, Philip. Rocking and Rolling, (Massachusetts: Candlewick Press, 1997). Websites: Visit the Cal Tech Seismological Lab at: http://www.gps.caltech.edu/~polet/recofd.html Check out the earth's plates on This Dynamic Earth at: http://pubs.usgs.gov/publications/text/dynamic.html |