It is highly likely that Old Faithful will eventually stop erupting, as geysers are temporary geological features. While it has been remarkably consistent for over 150 years, the Upper Geyser Basin in Yellowstone is a dynamic volcanic system. Past research into silica deposits shows that during severe, multi-decade droughts in the 13th and 14th centuries, Old Faithful actually ceased erupting entirely because there wasn't enough groundwater to fuel the system. Today, minor earthquakes and changes in the local water table already cause the intervals between its eruptions to fluctuate; for instance, the average wait time has increased from 60 minutes in the 1960s to about 94 minutes today. A significant earthquake or a shift in the underlying hydrothermal "plumbing" could easily choke off its water supply or divert the heat source, turning the world's most famous geyser into a dormant hot spring.