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Old Faithful

Old Faithful

Nathaniel P. Langford and Gustavus C. Doane, of the 1870 Washburn Expedition, coined the name Old Faithful to testify to this geyser’s punctual regularity. Old Faithful is one of thousands of thermal features in Yellowstone National Park that result from a subterranean magma spike— where magma rises to within 40 miles of the earth’s surface, compared to an average distance of 90 miles. This unique feature accounts for the park’s Upper Geyser Basin, which contains nearly one quarter of Earth’s geysers.

Predicting Eruption Time

Yellowstone boasts six grand geysers, each eject­ing water spouts exceeding 100 feet. One of these giants, Old Faithful, ranges in height from 105 to 185 feet. It is a popular attraction; crowds flock to see it year round. For visitors to better under­stand the geyser, general rules have been devised to help predict eruption times.

Joseph Le Conte’s claim that Old Faithful erupted hourly became replaced by a generaliza­tion saying eruptions lasting under 4 minutes are followed by another in 40 to 60 minutes, and eruptions over 4 minutes are followed in 75 to 100 minutes. Over time, more detailed studies yielded more specific rules. In general, an erup­tion of 1.5 minutes will be followed in 45 min­utes. Approximately 65 minutes of rest follow a 3-minute eruption, and it takes 86 minutes to rebuild after a 5-minute eruption. Old Faithful’s eruptions, on average, last 4 minutes.

Many factors upset the balance of geysers over time. People can cause immense damage. Even within two years, from the 1870 expedition to a formal survey in 1872, noticeable damage had been done to Old Faithful’s cone by speci­men collectors. More damage has ensued as the geyser sees 3 million visitors yearly. A 1980s cleanup project removed debris from the geyser itself, as visitors sometimes throw coins and other objects in. These activities all affect a gey­ser’s stability.

Earthquakes serve as an additional factor that could contribute to lessening the reliability of Old Faithful. Seismographs record up to 215 tremors on the Yellowstone Plateau each year. Large earthquakes noticeably affect the balance of gey­sers. Before a 1959 quake, eruptions occurred at an average 65-minute interval. This quake and another in 1975 lengthened intervals, and a 1983 quake increased the average to 78 minutes.

Although geysers come and go, one should not prematurely conclude Old Faithful has yet become less predictable. Correlations and frequent obser­vation continue to yield reliable estimates even as rest intervals increase. Though Old Faithful now erupts less often, it still maintains an uncannily consistent schedule.

Jared Nathaniel Peer

See also Geology; Plate Tectonics; Wegener, Alfred

Further Readings.

Bryan, T. S. (1995). The geysers of Yellowstone. Niwot:

University Press of Colorado.

Bryan, T. S. (2005). Geysers: What they are and how they work. Missoula, MT: Mountain Press.

Schreier, C. (1992). A field guide to Yellowstone’s geysers, hot springs and fumaroles. Moose, WY: Homestead.

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