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Norris Geyser Basin
THERMAL DISTURBANCES
Periodically, Norris Geyser Basin experiences large-scale changes
that last a few weeks. This phenomenon is so common that it is known
as a thermal disturbance. The water levels in hydrothermal features
change, temperatures and pH levels fluctuate, and eruptive patterns
become different.
The thermal disturbances at Norris are not fully understood. Some
scientists think they result from a subterranean eruption within
the underground reservoir that supplies water to the area's hydrothermal
features. Other researchers speculate thermal disturbances may be
due to fluctuations in the geyser basin's water supply.
In late summer, when there is less cool surface water, changes in
temperature and pressure might occur in the groundwater system feeding
the hydrothermal vents, with the result that the deeper reservoir
becomes overheated.
Other scientists theorize that thermal disturbances may be related
to earthquakes or due to fluctuations within the underlying magma
chamber.
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