The information for this guide was taken from the Norris Geyser Basin Trail Guide, which is available at the trailhead.
Norris is outside the Yellowstone Caldera, but inside the first and largest caldera.
Norris is one of the most active earthquake areas in the park.
This is one of the most acidic hydrothermal areas in Yellowstone.
Many acidic geysers, which are rare in the rest of the world, are here.
Steamboat Geyser is the tallest active geyser in the world.
Norris Geyser Basin is one of the hottest and most dynamic of Yellowstone's hydrothermal areas. Many hot springs and fumaroles have temperatures above the boiling point (200°F) here. Water fluctuations and seismic activity often change features.
It's hard to imagine a setting more volatile than Norris. It is part of one of the world's largest active volcanoes. And it sits on the intersection of three major faults. One runs from the north; another runs from the west. These two faults intersect with a ring fracture from the Yellowstone Caldera eruption 640,000 years ago. These conditions helped to create this dynamic geyser basin.
Each year at Norris new hot springs and geysers appear; others become dormant. Geologic events cause many of these changes. Even small earthquakes can trigger changes in hydrothermal behavior. Some changes are brief; others last longer.
Geysers and hot springs may also create changes in themselves. Some Norris hot springs, like Cistern, rapidly dissolve underground rock. As hot water moves toward the surface, the dissolved minerals deposit along subterranean passages and around the surface vents. Eventually, these deposits can choke off the flow of water. New features may be born as hot, pressurized water seeks a route to the surface.
Some features in Norris Geyser Basin can undergo dramatic behavioral changes simultaneously. Clear pools become muddy and boil violently, and some temporarily become geysers. Geysers cease erupting or have altered cycles. New features appear. This sudden activity is known as a "thermal disturbance" and can last a few days or more than a week. Gradually, most features return to "normal."
Why this happens is not fully understood. Norris has the greatest water chemistry diversity among Yellowstone's hydrothermal areas. Multiple underground hot water reservoirs exist here and as their water levels fluctuate, concentrations of chloride, sulfate, iron, and arsenic change. Although Norris is known for its acid features, it also has alkaline hot springs and geysers. As underground waters and chemistry shift, they could contribute to sudden dramatic changes in minerals and pH. Further study will help unravel the mystery of this phenomenon.
The Colors of Norris
Many of the colors you see here are evidence of thermophiles (heat-loving microorganisms) and their activity.
Yellow deposits here typically contain sulfur. They form when hydrogen sulfide gas (the rotten egg odor you may have noticed) is converted to sulfur. Some thermophiles live in these areas because they use chemicals like sulfur for energy. They form communities of mats and streamers (formations that look like waving clumps of hair) in the hottest acidic runoff, which measure between 140°F and 181°F.
Dark brown, rust, and red colors abound in Norris and contain varying amounts of iron. Red-brown mats may also contain bacteria and archaea that help build the mats by metabolizing and depositing iron. These iron-oxide deposits often contain high levels of arsenic. These communities form in water below 140°F.
Emerald-green mats color many of the runoff channels of hot springs and geysers here. Algae are the dominant life forms in these mats and contain chlorophyll, a green pigment that helps convert sunlight to energy. Some bacteria and archaea grow in these mats, which form below 133°F.
Dark blackish-green mats form in even cooler water. An alga called Zygogonium forms these communities of mats and streamers.
Color placement within thermal water changes, in part, because temperatures and chemistry change. In a hot spring, for example, the hottest water is closest to a hot spring's vent. As the water flows outward, it gradually cools. This range of water temperature, called a thermal gradient, supports various thermophilic habitats. Chemical composition also changes as water flows from thermal features, mixes with other water sources, and is diluted or concentrated. As temperatures or chemical compositions change, microbial populations—and the colors they create—shift to a location they favor.
Some Like It Hot!
Norris Geyser Basin supports an astounding diversity of life. The majority of species here are microscopic thermophiles—heat-loving microorganisms. They survive in conditions of high heat and acidity or alkalinity that would instantly kill most other life forms.
Thermophiles are included in all three domains of life:
Bacteria This domain includes bacteria that can cause disease, fertilize soil, recycle material, and renew supplies of oxygen, nitrogen, and water. At Norris, some bacteria metabolize iron and other minerals.
Archaea The organisms in this domain were once considered bacteria, but their genes show they are as different from bacteria as they are from animals and plants. Scientists think they evolved long ago when earth's environment was much hotter. Many of the microbes in Norris are archaea.
Eukarya Within this domain are plants, animals, and fungi. Some of Norris's thermophiles—algae—also belong in this domain.
Viruses, which are not included in the three domains, also thrive in Yellowstone's hydrothermal features. The viruses here are different from other known viruses because they survive such extreme conditions.
Due to Norris Geyser Basin's rough terrain and highly changeable conditions, please expect uneven ground and steep grades that exceed 8 percent. Rocks and roots protrude into sections of dirt trail. Most of these sections are marked on the map, but may change. Proceed with extreme caution.
Geyser Basins: Windows to Earth's Interior
All of Yellowstone's hydrothermal areas are fueled by magma (molten rock) beneath the park. This magma heats water percolating down from the surface along fractures and faults. This superheated water rises back toward the surface, collecting into larger channels that serve as the "plumbing" for each hydrothermal feature.
Geysers form if the plumbing channel contains a constriction. Between eruptions, temperatures in the superheated, pressurized water beneath the constriction build up, creating increasing amounts of steam. Eventually the steam pushes water out of the constriction, water pressure deep in the system drops instantaneously, and the geyser erupts.
Hot springs are features with no plumbing constriction. Superheated water cools slightly as it reaches the surface, and is replaced by hotter water from deeper sources. This sets up a pattern of water circulation, which helps prevent the chain reaction leading to an eruption.
Fumaroles (steam vents) are Yellowstone's hottest surface features. Their underground channel systems penetrate the hot rock masses, but are generally dry. What little water does drain into the fumarole's plumbing converts instantly to steam.
Mudpots form when acid decomposes surrounding rock into clay. This clay mixes with water to form mud of varying consistency and color. Gases bubble and burst through the mud and create the playful plopping so characteristic of these features.
Animals at Norris
Like other hydrothermal areas in Yellowstone, Norris provides a warm respite from winter for bison and elk. They can also find plants growing here year-round and water to drink.
Watch for bison in the spring; they can seem to suddenly appear as they walk about the basin.
Elk give birth to their calves in May. Do not approach calves; adults fiercely defend their young. Bull elk in the fall are also dangerous.
Look and listen for killdeer. They nest on bare ground and will call in alarm if visitors are close by. Also look for swallows, which fly over the basin catching insects to eat.
Norris Geyser Basin is home to many insects associated with thermophiles. It also provides habitat for colorful dragonflies. Look for them in grassy areas near Crackling Lake in Porcelain Basin and Puff 'n Stuff Geyser in Back Basin.
Hydrothermal features are fragile rarities of nature. Yellowstone preserves the largest collection of hydrothermal features on the planet. You have an unparalleled opportunity to view hot springs, geysers, mudpots, and fumaroles in a natural setting.
Change takes place naturally in a hydrothermal area, but people can disrupt these processes and cause irreparable damage. Rocks, sticks, and other objects thrown into a hydrothermal feature may be permanently cemented in place, choking off water circulation and ending all activity.
For the sake of all who follow, never throw objects into any feature. Stay on established walkways for your safety and to protect fragile formations that have formed over thousands of years.
It is illegal to collect any natural or cultural objects or to remove, deface, or destroy any plant, animal, or mineral in Yellowstone's hydrothermal areas. Bring drinking water; take out all trash.
While viewing or photographing the area, protect your camera, glasses, and binocular lenses from hydrothermal heat and stray.
Toxic gases exist in Yellowstone. Dangerous levels of hydrogen sulfide and carbon dioxide have been measured in some hydrothermal areas. If you feel sick, leave the location immediately.
Help preserve Yellowstone for the future.