In today's article we are going to delve into the topic of Doublet Pool, a topic that has aroused great interest in recent years. Doublet Pool is an area of study that has captured the attention of academics, experts and enthusiasts alike, and has generated debate and research in various fields. From its impact on society to its implications in everyday life, Doublet Pool has proven to be a relevant and constantly evolving topic. In this article, we will explore different aspects and perspectives of Doublet Pool, in order to shed light on this fascinating topic and provide a more complete view of its importance in today's world.
Doublet Pool | |
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Location | Yellowstone National Park, Teton County, Wyoming, USA |
Coordinates | 44°27′52″N 110°49′47″W / 44.4643188°N 110.8296237°W |
Elevation | 7,356 feet (2,242 m) |
Type | Hot spring |
Temperature | 194.4 °F (90.2 °C) |
Depth | 8 feet (2.4 m) |
Doublet Pool is a hot spring in the Upper Geyser Basin of Yellowstone National Park, Wyoming.
Doublet Pool is 8 feet (2.4 m) deep and its temperature is approximately 194.4 °F (90.2 °C). Its scalloped edge is made of geyserite. Eruptions can occur in Doublet Pool, but only last up to 8 minutes. The pool on the right pulses over the vents about every two hours. Occasionally there will be vibrations, surface wave motion, and thumping; these effects are caused by collapsing gas and steam bubbles deep underground.