Bryce Point to Peekaboo Connector Trail Closure
Due to a large rockslide, the connecting trail from Bryce Point to Peekaboo Loop is closed. Trail will be reopened once repairs are made. The Peekaboo Loop is open, but must be accessed from Sunset or Sunrise Point.
Backcountry Campsite Closures
Due to bear activity at select campsites in Bryce Canyon's backcountry, multiple backcountry campsites have been closed until further notice: Sheep Creek, Swamp Canyon, Natural Bridge, Iron Spring, Corral Hollow, Riggs Spring and Yovimpa Pass.
Activity 5: Earthquake Waves
SURFING ROCK WAVES
Earthquakes happen all over the world. On the surface we do not always feel them. The movement we do feel can be described in two motions: P waves and S waves. Students will use slinkies to imitate and better understand the two types of waves.
Instructional Method: Experiment
Goal: Explain wave motions associated with earthquakes.
Objectives: Students will be able to:
Activity time: 30 minutes
When movement occurs between two pieces of crust, called fault blocks, we feel an earthquake. To create a mini-earthquake, slide two blocks of rock against each other. Can you feel the roughness of the two rocks as they pass by each other? The friction between the two rocks is what creates the vibrations in an earthquake except on a much greater scale. These vibrations in nature are called seismic waves.
Most earthquakes are too small to be felt by people. Larger earthquakes are not only felt by people, but can severely damage structures. The motion from an earthquake travels through rock in the form of waves. There are two types of waves associated with earthquakes: P waves and S waves.
The fastest of the waves is a primary wave, or P wave. These waves feel like a push-and-pull movement on the crust as it is stretched and compressed. P waves are also called compressional waves. The slower of the two waves is called a secondary wave, or S wave. These waves travel in a side to side motion and produce more shaking than P waves. The side-to-side motion of S-waves causes the most damage to structures during an earthquake.
In large earthquakes it is possible to feel the difference between P and S waves. P waves feel like someone has run a semi-truck into your house and S waves feel more like you are riding waves at a lake or ocean. The following schematic shows how these waves travel through rock.
It is possible to simulate the motion of both P and S waves by using a Slinky. The push-pull motion of a P wave can be seen by stretching and compressing a slinky. The shaking motion of an S wave can be seen by moving a stretched Slinky side to side.
Have you ever experienced an earthquake? What did it feel like to you? Could you distinguish between the P waves and the S waves? Which do you think is more destructive to houses, P waves or S waves? Why? What do you think you should do to protect yourself during an earthquake?
Instead of using slinkies you can create P and S waves in a box of sand. Fill a rectangular box with 2-3 inches of sand. Be sure the sand is very dry. On the sand place small sticks or Lego houses. Shake the box or hit the side of it and observe what happens to the house and sand. It may help to place toothpick markers throughout the sand standing on end. Watch what happens to the toothpicks when the box is shaken. Does this work? Can you distinguish between P and S waves? How? Do you have to shake the box differently to create both types of waves?
Included National Parks and other sites:
Aniakchak National Monument and Preserve
Utah Science Core:
5th Grade Standard 2 Objective 1,2,3
Did You Know?
The Bryce Canyon Paintbrush was discovered June 24, 1965 at Inspiration Point in Bryce Canyon National Park. This rare wildflower is only found in southwestern Utah. More...