|
Heat and volcanic gases from slowly cooling magma rise and warm the dense salty water that occupies fractured rocks above the Yellowstone magma chamber. That brine, in turn, transfers its heat to overlying fresh groundwater, which is recharged by rainfall and snowmelt from the surface. Water boiling at depth below the surface is hotter than the temperature of boiling at the surface. If it rises quickly, this superheated water can flash to steam, propelling both steam and hot water to the surface as a geyser. More commonly, hot water rises and loses its heat at a steady rate, flowing to the surface as a hot spring. Refer to Figure 4.
Steamboat, located in Norris Geyser Basin, is one of Yellowstone's most famous geysers. Eruptions occur sporadically, but are well worth the wait. Columns of hot water reach heights up to 100 meters. This is followed by a raucus steam phase that can last for over a day, loudly discharging steam nearly 200 meters into the atmosphere.
Steamboat has proven more active during the early 21st Century than any time since the early 1980s. Between late 1991 and 2000, there were no eruptions. However, since May 2000, Steamboat has erupted 5 times... most recently on April 27, 2003.
|
