Download Using Seismographs, Then and Now The Modern Seismograph

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project

Document related concepts
no text concepts found
Transcript
Using Seismographs, Then and Now
Using Seismographs, Then and Now
The Modern Seismograph
A modern seismograph, also called a seismometer, records the shaking of Earth's surface caused by
seismic waves. A seismogram is the record a seismograph makes. A seismogram shows seismic waves
as jagged up-and- down lines. Scientists compare multiple seismograms in order to pinpoint an
earthquake's epicenter.
Modern seismograph
The First Seismograph
Zhang Heng, a Chinese scientist, invented the first-known seismograph around 132 CE. It didn't look
anything like a modern seismograph. It was shaped like a large vase. The vase had eight dragons around
the outside, each looking downward and holding a ball loosely in its mouth. Below the eight dragons
were open-mouthed frogs. When an earthquake struck, the balls fell into the frogs' mouths below.
ReadWorks.org · © 2016 ReadWorks®, Inc. All rights reserved. This article is based on an original work of the Core Knowledge® Foundation made available through licensing under a Creative Commons
Attribution-NonCommercial-ShareAlike 3.0 Unported License. This does not in any way imply that the Core Knowledge Foundation endorses this work. This article is licensed under a Creative Commons
Attribution-NonCommercial-ShareAlike 3.0 Unported License. https://creativecommons.org/licenses/by-nc-sa/3.0/
Using Seismographs, Then and Now
Depending on which balls fell, it was possible to estimate the distance and direction to the earthquake's
source.
First-known seismograph
Learning About Our Earth from Seismographs
Scientists can learn a lot from seismographs, beyond just where an earthquake's epicenter. Take the
Danish scientist Inge Lehmann, for example. In her time, around 1900, scientists thought the earth had
just three layers: an outer crust, a solid mantle, and a liquid core. Lehmann studied seismograph records
of earthquakes. She analyzed how seismic waves changed as they traveled through Earth's interior.
Lehmann collected thousands of records organized in boxes-there were no computers back then! She
saw patterns in how seismic waves behaved as they moved through Earth. Lehmann concluded that
Earth's core has two parts: a liquid outer core and a solid inner core. In 1936, she announced her findings
and changed our view of Earth!
ReadWorks.org · © 2016 ReadWorks®, Inc. All rights reserved. This article is based on an original work of the Core Knowledge® Foundation made available through licensing under a Creative Commons
Attribution-NonCommercial-ShareAlike 3.0 Unported License. This does not in any way imply that the Core Knowledge Foundation endorses this work. This article is licensed under a Creative Commons
Attribution-NonCommercial-ShareAlike 3.0 Unported License. https://creativecommons.org/licenses/by-nc-sa/3.0/
Using Seismographs, Then and Now
ReadWorks.org · © 2016 ReadWorks®, Inc. All rights reserved. This article is based on an original work of the Core Knowledge® Foundation made available through licensing under a Creative Commons
Attribution-NonCommercial-ShareAlike 3.0 Unported License. This does not in any way imply that the Core Knowledge Foundation endorses this work. This article is licensed under a Creative Commons
Attribution-NonCommercial-ShareAlike 3.0 Unported License. https://creativecommons.org/licenses/by-nc-sa/3.0/