Yellowstone Virtual Junior Ranger

A graphic of a junior ranger badge on a computer screen.
 

Now, there are two ways to become a Yellowstone National Park Junior Ranger! If you are coming to the park you can pick up a booklet and earn a Junior Ranger badge in person. If you can't make it to the park, however, you can still earn a Virtual Junior Ranger badge right here on our website! To get your virtual badge, explore the following sections and complete each of the activities below. Then, a park ranger will swear you in and you can download your Virtual Junior Ranger badge to show off to your family and friends. Have fun!

 
Purple badge with silhouette mountain and word "Geology" over image of a rock mountaintop overlooking other mountains.
 

About 631,000 years ago, Yellowstone exploded in a massive volcanic eruption. It blew volcanic ash and gas into the air. As the underground magma reservoir emptied, a giant crater, or caldera, formed. Take a look at what is beneath Yellowstone:

 

Cross-section of earth showing the crust (A), mantle (B), core (C), and a hotspot (D)

 

  • Crust (A) is the layer of rock that we walk on, is very thin, and made of solid rock.
  • Mantle (B) is very hot, often consisting of rocks in molten form. Sometimes hot melted rocks called lava come out to the surface of the earth.
  • Core (C) is divided into two parts: the liquid inner core and the solid outer core. Rapidly circulating liquid metal releases heat through the outer core and into the overlying mantle.
  • Hotspot (D) is a relatively small, very hot region of magma (molten rock from the mantle) that is close to earth's surface.

 

Water heated by magma escapes from the ground through geysers, hot springs, and other hydrothermal features in the park.

A blue hot spring pool steams, surrounded by a scaly white landscape.


The last highly explosive Yellowstone eruption was approximately 174,000 years ago. It created what is now the West Thumb of Yellowstone Lake.

►Check it out!

Look at the map of ash fallout from the previous three major eruptions. If you live in the US, does your state have ash from the Yellowstone super volcano?

Map of Lower 48 of US showing three different ash-falls in gray shades.

Graphic showing locations of three major eruptionsAs earth's plates drift, the North American plate slowly moves over the Yellowstone hotspot.

Check out these three major eruptions. Can you guess where the next eruption might happen?







 


Purple map overlain by three shades of gray the cover the majority of the US with text that asks,

Yes. The heat undeneath the park fuels many of the hydrothermal features. Earthquakes (1,000 to 3,000 per year) reveal activity below ground. The University of Utah Seismograph Stations track this activity closely. Visit the university's seismograph web page to see real-time monitoring data.

A caldera is a large depression in the earth that is formed after a volcano erupts and collapses. One of the largest volcanic eruptions known to have occurred in the world created one of the largest known calderas, the Yellowstone Caldera, which is 30 x 45 miles (48 x 72 km) wide. Simulate for yourself how the Yellowstone Caldera was formed.

What You'll Need

  • Large shoebox
  • Newspaper or craft paper
  • Balloon
  • Plastic straw
  • Binder clip
  • Tape
  • Flour

Series of three photographs showing the 3 steps in the activity.

What To Do

  1. Line your box with paper and punch a hole in one end. Insert the straw into the balloon and tape it tightly so no air leaks out. Feed the straw through the box hole.
  2. Blow up the balloon with just enough air to fill the box. Fold over the end of the straw and seal with the binder clip. Place the box on paper and sprinkle flour over the balloon until it is completely covered.
  3. Slowly take the binder clip off and allow the balloon to deflate. Can you see the edges of your caldera?
 
Blue badge with white silhouette of an eruption geyser over an image of a steaming pool of water.
 

Deep blue pool of hot water surrounded by a barren, gray ground.

Hot Springs

  • The most common hydrothermal feature in Yellowstone.
  • Plumbing has no constrictions.
  • Superheated water cools as it reaches the surface, sinks, and is replaced by hotter water from below.
  • This process, known as convection, prevents water from reaching the temperature needed to set off an eruption.













An eruption of water and steam rises from a crater on the bank of a small river.

Geysers

  • Hot springs with a constriction in their plumbing system.
  • This allows pressure to build to the point where an eruption occurs to release the built up pressure.
  • Over half of the world's geysers are found in Yellowstone.















Thick, whitish mud-like substance bubbles and pops.

Mudpots

  • Acidic hydrothermal features with limited water supply.
  • Some thermophiles use hydrogen sulfide as an energy source.
  • This helps convert gas into sulfuric acid, which breaks down rock into clay minerals.
  • Various gases escape through the wet clay, causing it to bubble.















Steam rises up from a barren, rocky hillside.

Fumaroles

  • The hottest hydrothermal features in the park.
  • Limited amount of water in these features causes water to flash into steam before reaching the surface.
  • Also known as steam vents.

Cross-section of the earth showing some of the paths water takes to make hydrothermal features on the surface.
  • A - Snow melt and rain water move down through rock layers.
  • B - Magma below the surface heats the water.
  • C - Weight of water above causes pressure and heat to build below.
  • D - Constrictions in the plumbing system cause water and steam to explode with force.

In the 1990s, researchers lowered a video camera into Old Faithful's vent. Here's what they found!
  • At 22 feet (6 m) underground, Old Faithful's plumbing system shrinks to a few inches wide.
  • At 24 feet (7 m), a small waterfall of relatively cool groundwater flows into the conduit.
  • At 35–45 feet (10–13 m), a large cavern—about the size of a small car—lies inside Old Faithful.
  • A "liquid tornado" of wildly boiling, churning water at the lower end of the cavern stopped the camera from seeing any further.

Though most geysers are not predictable, Old Faithful is famous for its regularity. Use the rangers' formula below to predict its next eruption. You will need a place to record your work and answers.

Step 1

Open the Old Faithful Geyser Live-stream Webcam. Wait for Old Faithful to erupt and time its eruption from when water begins splashing continuously out of the cone until only steam is coming out.

A. Start Time: _______
B. End Time: _______
C. Length of Eruption (to nearest 1/2-minute): _______

Step 2

Using the table below, find the length of the eruption (C) in the first column. Read directly across to the second column in the same row and note the interval or number of minutes (D) until the next eruption.

Table of Old Faithful eruption lengths and intervals between eruptions.
C. Length of Eruption D. Interval Until Next Eruption
< 3 minutes 68 minutes
> 3 minutes 94 minutes

Step 3

Add the start time for the first eruption (A) with the interval number of minutes until the next eruption (D). This is the prediction for the next eruption!

_________(A) + _________(D) = ____________ (Your Prediction!)

Step 4

Return to the Old Faithful Geyser Live-stream Webcam to find the rangers’ prediction for the next eruption: __________ How close is your prediction to theirs? ________________________

Step 5

Watch the next Old Faithful Geyser eruption. When did it start? ________ How did the actual start time compare to your prediction? To the rangers’ prediction? Remember, Old Faithful is a natural feature and changes often, so any prediction may not prove to be exactly right.

 
The yellow circular image with a bison silhouette is superimposed over an image of a family of red foxes.
 

Four images of wildlife: pika eating leaves, bighorn sheep on rocks, fox crossing snowy field, and beaver sitting in water.

Every animal has a habitat—a place that provides the food, shelter, space, and water it needs to stay alive. Learning about animals and how they live is important to understanding their role in Yellowstone's environment.

  • Food (A) is essential. An animal must look for food or eat most of the time it's awake.
  • Shelter (B) protects an animal from predators and allows it to rest.
  • Space (C) is the room an animal needs to find food, water, and attract a mate.
  • Water (D) is needed for drinking, finding food, or just for fun.

A grizzly bear standing on some downed trees.

Grizzly Bears

  • They can run up to 45 miles per hour (72 kph).
  • They eat nuts, berries, plant roots, and other animals—making these top predators omnivores.
  • They scratch their backs on "rub trees," leaving behind hair that scientists use to learn about bears.





A black bear looks out from a tree.

Black Bears

  • They are more common than grizzly bears, and are found across North America.
  • While they are called black bears, their fur can be brown, blond, or cinnamon in color.
  • They have shorter, more curved claws that allow them to climb trees. However, this makes them less capable diggers compared to grizzly bears.




Bison grazing through an open woodland.

Bison

Yellowstone National Park is the only place in the United States of America where bison have lived continuously since prehistoric times. Yellowstone is also home to the nation's largest bison population on public land.

  • Males can weigh 2,000 pounds (907 kg).
  • They roam great distances as they continuously eat.
  • Their thick winter coats are so well insulated snow can stay on their backs without melting.


Elk resting on the ground.

Elk

An estimated 10,000 to 20,000 elk live in Yellowstone during the summer season. During the winter, most leave the park.

  • They are the most abundant large mammal in Yellowstone.
  • Male antlers can weight about 30 pounds (14 kg) per pair and are shed every year.
  • Calves are born with white spots to help them hide from predators.


Female alpha wolf walking across snow.

Northern Rocky Mountain Wolves

Wolves are highly social animals and live in packs. Although wolf packs once roamed from the Arctic tundra to Mexico, loss of habitat and extermination programs led to their demise throughout most of the United States of America by early in the 1900s. Today, nearly 100 wolves call Yellowstone home.

  • They live and travel in packs of ten animals (on average).
  • They communicate through barks, whines, growls, and howls.
  • The pack cares for new pups until they can hunt on their own, at about ten months.

Yellowstone cutthroat trout swimming in a shallow stream.

Yellowstone Cutthroat Trout

Yellowstone cutthroat trout are the most wide-spread native trout in the park, and are an important food for at least 16 species of birds and mammals. However, their population has declined substantially since the mid-1980s due to the invasion of lake trout into Yellowstone Lake.

  • They have a red-orange mark under their jaw.
  • They require cool, clean water in streams or lakes.
  • They spawn, or lay eggs, in spring and early summer.
 
Green preservation badge with a silhouette ranger hat over a scene of NPS employees fixing a boardwalk in winter.
 

As the world's first national park, Yellowstone did not come with a rule book or a manual on how national parks should be run. Things didn't always go well, but we continue to learn and improve the ways we preserve this amazing place.

  • In the early days of the park, bears could be fed along roadsides and at garbage dumps. Today, bears in the park find natural food and are wild.
  • Opened in 1914, the Geyser Baths Bathhouse was a swimming pool at Old Faithful. Today, we understand how easily hydrothermal systems can be damaged and destroyed.
  • Until the early 1900s, all predators were routinely killed in Yellowstone. Today, predators are valued as an important part of Yellowstone's ecosystem.

To preserve Yellowstone, we must all be good stewards. Stewardship means making a difference in our world and trying to make it a better place. Yellowstone's park rangers were once kids, just like you, and have dedicated their lives to protecting special places like Yellowstone.

The arrowhead is the symbol of the National Park Service and what it protects. It is a reminder of the nature and culture national parks protect. Take a look at the arrowhead, then take a look at what each part of the arrowhead represents.

Brown arrowhead pointing down with a green sequoia growing in front of a snow-capped mountain and a white bison grazing.

The mountain represents: geology such as mountains, volcanoes, glaciers, arches, dunes, geologic processes, fossils, and so forth.
The sequoia tree represents: vegetation such as trees, cactuses, grasses, wildflowers, aquatic plants, lichen, and so forth.
The bison represents: wildlife such as mammals, birds, reptiles, insects, fish, coral, amphibians, mollusks, and so forth.
The lake represents: water resources such as rivers, lakes, oceans, and shorelines.
The arrowhead shape represents: cultural resources and heritage such as Native Americans, explorers, inventors, artists, American history, and technological advancements.

 

 
A graphic of the word Congratulations in front of a blue background.
 
 

Virtual Junior Ranger Pledge

As a Virtual Junior Ranger, I _______________ promise to learn all I can about Yellowstone National Park, and its plants, animals, history, and natural features. I will continue to learn and teach others about how to protect the natural world.

 
A graphic of a badge with the words: Junior Ranger Yellowstone NP Virtual Visit
 

Right click the image above and select "Save As" to save and print your Virtual Junior Ranger badge. After printing it, cut it out and glue it to cardboard or tape it into your passport book!

Last updated: February 23, 2024

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Contact Info

Mailing Address:

PO Box 168
Yellowstone National Park, WY 82190-0168

Phone:

307-344-7381

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