10 December, 1999
Fumaroles Part 1 of 2
The fumaroles around Mt Erebus are magnificent. One part of the science being done on the volcano is the study of the many and fantastic ice towers created by fumaroles around the crater. In many places around the mountain the rock is either broken or the soil is porous which allows the volcano to degas. This means that the steam and gases under pressure inside the volcano have a place to escape besides from inside the crater When this steam reaches the cold air of Antarctica it freezes and forms ice towers. Each tower is different, in shape, size and structure. Some are tall and thin and appear very fragile, others look to be study and solid ice. A few can be climbed down inside, all have steam coming out of them
Jean Wardell, graduate student at New Mexico Tech is currently mapping and measuring these fumaroles for their gas emission. She climbs up into the steam vent (sometimes several feet high) and uses her instruments to measure the speed of the gas as it escapes, the relative humidity( RH), the CO2 content., the temperature and the presence of any other gases. The gases coming from the fumaroles are largely water vapor, and CO2.
Contact the TEA in the field at .
If you cannot connect through your browser, copy the TEA's e-mail address in the "To:" line of your favorite e-mail package.