Show Navigation
back to search results

Colorful Bacterial Mats, Grand Prismatic Spring, Yellowstone National Park, Wyoming

A variety of thermophiles, which are microorganisms that thrive in heat, are responsible for the colors in the Grand Prismatic Spring, located in the Midway Geyser Basin area of Yellowstone National Park, Wyoming. The yellow-green color comes from the thermophilic cyanobacteria Synechococcus, which is found in the hottest water of the spring (up to 161°F or 72°C). Phormidium, which is orange, is found in the spring's middle temperatures (113-140°F or 45-60°C). Calothrix, which is brown or black, is found in the coolest temperatures, although not lower than 86°F or 30°C. The terraces are the result of minerals that solidify in water that spills out of the spring.

Add to Cart Add to Lightbox Download
Filename
Yellowstone_Grand-Prismatic-Spring_Bacterial-Mats_5470.jpg
Copyright
Copyright 2019 Kevin Ebi/LivingWilderness.com. All rights reserved.
Image Size
8688x5792 / 13.9MB
https://www.livingwilderness.com/licensing-prints-terms.htm
https://www.livingwilderness.com/licensing-prints.htm
Grand Prismatic Spring hot spring spring geothermal thermophile thermophiles cyanobacteria Phormidium Synechococcus Calothrix colorful thermophilic water mineral minerals Yellowstone Yellowstone National Park Midway Geyser Basin nature pattern patterns Wyoming WY United States United States of America bacteria bacterial bacterial mat bacterial mats
Contained in galleries
A variety of thermophiles, which are microorganisms that thrive in heat, are responsible for the colors in the Grand Prismatic Spring, located in the Midway Geyser Basin area of Yellowstone National Park, Wyoming. The yellow-green color comes from the thermophilic cyanobacteria Synechococcus, which is found in the hottest water of the spring (up to 161°F or 72°C). Phormidium, which is orange, is found in the spring's middle temperatures (113-140°F or 45-60°C). Calothrix, which is brown or black, is found in the coolest temperatures, although not lower than 86°F or 30°C. The terraces are the result of minerals that solidify in water that spills out of the spring.
Prev Next
Info
  • Facebook
  • Twitter
x

Living Wilderness Nature Photography

  • Nature Photography Galleries
    • All Galleries
    • Search
    • Cart
    • Lightbox
    • Client Area
  • Portfolio
  • Search Nature Photography
  • Books
  • Blog
  • About
  • Contact