U.S. Highway 89 Bryce Canyon to Grand Canyon
Road damage south of Page, Arizona will impact travel between Bryce Canyon and Grand Canyon National Parks. Click for a travel advisory and link to a map with suggested alternate routes: More »
Sunset Campground Construction
From April-July 2014, three new restroom facilities will be constructed in Sunset Campground. Visitors may experience construction noise and dust, as well as some campsite and restroom closures. 'Sunset Campground' webpage has additional information. More »
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.
Wall Street Section of Navajo Loop Closed
Due to dangerous conditions (falling rock and treacherous, icy switchbacks), the Wall Street section of the Navajo Loop Trail is CLOSED. It will reopen in Spring once freezing temperatures have subsided.
Backcountry Campsite Closures
Due to bear activity at select campsites in Bryce Canyon's backcountry, two backcountry campsites have been closed until further notice: Sheep Creek and Iron Spring.
Activity 7: Plateaus
CREATING FLAT-TOPPED MOUNTAINS
Have you ever seen a flat-topped mountain? How are they created? In this activity, students see how broad uplifted areas breakup, forming plateaus such as those on the Colorado Plateau.
Instructional Method: Experiment
Goal: To present an example of a landform that resulted from plate tectonics.
Objectives: Students will be able to:
Preparation: 15 min.
Plateaus are broad flat-topped mountains with steep sides. They form due to a number of tectonic forces. This activity will discuss four different ways plateaus form.
As upwelling magma pushes its way toward the surface but does not break through, it can push up large flat areas. This magma plume can be created from a melting subducted plate. Scientists believe that this is one process that helped to formed the Colorado Plateau. (Plate Tectonics concepts can be further examined by connecting to the Plate Tectonics Unit page.)
Colliding crustal plates can form mountains and plateaus. The compressed crust buckles like the hood of a car in a collision. Mountains form nearby the collision, while planar uplifted areas form farther away from the collision source. An example of this is found on the Mongolian Plateau in Asia. As India collided with Asia, the Himalayan Mountains were buckled and uplifted like the hood of a crashed car but the area behind the collision zone is undeformed, creating the Mongolian Plateau.
Alleviating overburden or lightening of the crust by erosion allows large planar surfaces to uplift. If a large amount of heavy sediment is removed from a region, that area of the crust becomes lighter and rises as a result. This same process occurs to melting glaciers. As the glacier mass diminishes it becomes lighter and sticks higher into the air. For plateaus to uplift, the entire area must erode continuously.
As a plateau region elevates, stresses cause breaks in the crust known as faults. A fault often separates smaller plateaus from one another on the Colorado Plateau. As a result of faulting, some of the uplifted regions are pushed higher than the surrounding area.
Erosion helps to define one plateau from another. Rivers follow the path of least resistance, where rocks are weakest. Rock near faults tend to be weak and broken. Flowing water easily cuts into broken rock along a fault and over time forms a broad river valley. Separation by the new valley allows us to easily differentiate between plateaus.
A large concentration of plateaus is found within the Colorado Plateau. It is an uplifted region broken into many smaller plateaus. It comprises portions of four states: Utah, Arizona, New Mexico and Colorado. All of the Colorado River drainage basin is located on the Plateau, and thus its name.
Smaller structures resembling plateaus are known as mesas and buttes. Mesas are like plateaus, only smaller. Buttes are even smaller than mesas. On the side bar there is a list of National Parks found on the Colorado Plateau. Each National Park protects a unique feature created by the Plateau uplift. The following activity allows students to create plateaus in a few different ways.
I. Sand plateaus (represents upwelling forces)
II. Wood block plateaus (represent compressional and extensional forces)
III. Ice uplift (represents removal of overburden)
Explain to students that their action in uplifting the sand cake is taking the place of magma rising to the surface of Earth. The irregular uplifting caused by the students resulted in small breaks in the sand. In nature these would be called faults. Ask students how erosion may separate the broken sand cake into plateaus. How can the Colorado Plateau be more than one plateau? Why is the entire region uplifted? What can happen to land that is uplifted? Do plateaus always have flat tops? Why? Ask students to draw sketches of the blocks and label plateaus with sides and top.
Instead of using your hand to show how the plateau formed, you can use the sand to allow students to make a plateau. Have students draw a plateau on paper and then sculpt a plateau out of sand. Have them imagine that their hands are erosional forces carving the sand away. On their picture write what forces their hands represent, i.e. rivers, ice, gravity, etc.
Included National Parks and other sites:
Arches National Park
Utah Science Core:
4th Grade Standard 4 Objective 1,2
Did You Know?
The geologic term, hoodoo, lives on at Bryce Canyon National Park as perpetuated by early geologists who thought the rock formations could cast a spell on you with their magical spires and towering arches. More...