| |
| | [No title] |
 | | In this end-member, also called Airy isostasy, the load rides just high enough in the fluid that the pressure directly beneath the load, at some arbitrary depth, is equal to that beyond the edge of the load, measured at the same depth. |
 | | This is what is implied by the name isostasy, which means equal pressure (iso- for equal, -stasia for standing or static). |
 | | If the pressures were not equal, the fluid would flow from high pressure to low, meaning that the elevations of the load would change, and the problem would not be static. |
| www.es.ucsc.edu /~rcoe/eart110c/Lab7_text.doc (864 words) |
|