Chapter 10 Notes

Geological processes

The earth’s interior is separated into three concentric zones

• Core
• Mantle
• Crust

What we know about the interior comes from indirect evidence

• Density measurements
• Seismic (earthquake) wave studies

 
an integral in which the range of integration is specified: its value equals the area on a graph bounded by a curve, the x-axis, and two given ordinates

The numbers at the top and bottom of the S-curve are called the upper and lower limits of integration respectively. Any integral that has such limits of integration is called a definite integral.

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