White Dome Geyser, Geyser in Yellowstone National Park, United States.
White Dome Geyser is a geyser in Yellowstone's Lower Geyser Basin featuring a distinctive cone-shaped mineral deposit that rises above the ground. Water shoots upward to approximately 30 feet (9 m) during eruptions lasting about 2 minutes, with steam and spray mixing together in the spray.
The geyser formed gradually through mineral deposition from hot water and has shaped the landscape of the Lower Geyser Basin for centuries. Its consistent activity has made it a recognizable feature that drew the attention of early park visitors and scientists exploring geothermal systems.
Scientists discovered Thermus aquaticus bacteria near White Dome Geyser, leading to advances in DNA research through polymerase chain reaction procedures.
The geyser can be reached from Firehole Lake Drive and erupts at unpredictable intervals ranging from minutes to hours. Visitors should be prepared to wait and remain flexible with their time, as eruption timing is not guaranteed and patience is essential.
The geyser exhibits a distinctive pattern where water first spurts upward in preliminary bursts before a full eruption takes place. This warm-up phase sometimes allows visitors to anticipate when the main event will occur and position themselves accordingly.
Location: Teton County
GPS coordinates: 44.53930,-110.80300
Latest update: December 6, 2025 17:43
Geysers represent some of the most visible expressions of hydrothermal activity, occurring where underground water reservoirs are heated by magmatic sources. Yellowstone National Park in Wyoming holds more than half of the world's known geysers, including Old Faithful with its reliable eruptions every 90 minutes and Steamboat, the tallest active geyser on Earth. Iceland offers the Haukadalur Valley, home to the namesake Geysir and Strokkur, which erupts every few minutes. The high plateau of El Tatio in Chile sits at 14,100 feet (4,300 meters) and forms the highest elevation geyser field in the world. Other notable locations include the Whakarewarewa thermal area in Rotorua on New Zealand's North Island, where the Pohutu geyser performs regularly, and the Valley of Geysers in Russia's Kamchatka Peninsula. These sites demonstrate the ongoing volcanic activity beneath the Earth's surface and attract visitors interested in observing natural thermal phenomena. Eruption patterns vary in frequency and intensity, with some geysers following predictable schedules while others remain irregular.
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