Email Print Share
December 12, 2007

Map showing how Pompeii's buildings caused changes in direction and temperature of flows.

This map shows how the city of Pompeii and its buildings caused changes in the direction and temperature of the pyroclastic flows that entered Pompeii during the A.D. 79 eruption. Our results show that the presence of the city caused the flow to move in different directions, such as moving along roads and around city walls. The presence of the city also influenced the flow temperature. The flows were cooled in places, although not to temperatures that would be comfortable for humans sheltering in the remains of the city. Imagine being in front of a ground-hugging cloud that is moving toward you at a hundred miles an hour or more, and it contains sand, rocks and bits of building, and (if that's not enough already) has a temperature of more than 100 degrees Celsius (212 degrees Fahrenheit).

Credit: Gurioli et al., 2005


Images credited to the National Science Foundation, a federal agency, are in the public domain. The images were created by employees of the United States Government as part of their official duties or prepared by contractors as "works for hire" for NSF. You may freely use NSF-credited images and, at your discretion, credit NSF with a "Courtesy: National Science Foundation" notation.

Additional information about general usage can be found in Conditions.

Also Available:
Download the high-resolution JPG version of the image. (37 KB)

Use your mouse to right-click (Mac users may need to Ctrl-click) the link above and choose the option that will save the file or target to your computer.

Related story: Feverish Effort Under Way to Understand Mt. Vesuvius