Beauty and Chromatic Pools - Yellowstone N.P., Wyoming
Posted by: Volcanoguy
N 44° 28.099 W 110° 50.334
12T E 512814 N 4923902
Beauty and Chromatic Pools are located in the Upper Geyser Basin of Yellowstone National Park.
Waymark Code: WMDQG2
Location: Wyoming, United States
Date Posted: 02/14/2012
Views: 20
Beauty and Chromatic Pools are two colorful pools in the Upper Geyser Basin. The two pools are interconnected at depth. One pool overflows while the other drops in level and cools. This state will continue for a few years and then the water will shift to the other pool and it begins to overflow. When this waymark was established Chromatic Pool was the active one. The photos on the sign show Beauty Pool active. Please indicate which pool was active on your visit.
Information sources from The Geyser Observation and Study Association (
visit link) and Yellowstone National Park.com (
visit link)
Text of sign at Beauty Pool:
Beauty and Chromatic Pools
Living Color
The vivid colors of Beauty Pool’s basin and runoff channels are created by microscopic lifeforms. Incredibly, these organisms survive and thrive in an environment that would be lethal to us and most other living creatures. Scientists are just beginning to understand these lifeforms; amazingly, hot spring environments may sustain a diversity of organisms rivaling that of terrestrial rain forests.
Thermal Feature Color Gradient
In the geyser basins with alkaline or neutral pH (Upper, Midway, Lower, West Thumb, and Mammoth Hot Springs), color is primarily a function of what lives and grows in a feature. The graph to the right represents the upper environmental temperature limits for life and the corresponding colors (which vary over the course of a year as a consequence of seasonal changes) in the features or runoff channels.
Hidden Connections
Beauty Pool shares an underground link with Chromatic Pool (to your immediate left). When Beauty Pool is full, Chromatic Pool’s water level is much lower; sometimes the reverse may be observed. Many other features in the Upper Geyser Basin have demonstrated similar behavior. The factors affecting such exchanges of function are many and may include phenomena such as earthquakes and continuing mineral accumulations in each features’s underground “plumbing.”