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 9: Earth Layers
PIT OF THE EARTH
Earth's layers are like a chocolate covered cherry. To introduce the concept of Earth layers, students will diagram and label the candy and describe how each layer of candy relates to an Earth layer.
To visualize the properties of the different Earth layers
Students will be able to:
Activity: 30 min.
Earth is composed of five main divisions or layers:
The layer we are most familiar with is the crust. Surprisingly, it is the thinnest layer of the four, despite how massive it seems to us. It is approximately 5 to 40 kilometers thick. There are two types of crust: continental crust and oceanic crust. The continental crust is the layer on which we live. The thicker portion of the crust is the continental portion, and likewise, the thinnest part is oceanic crust. The crust is ridged and brittle, but seemingly solid. This layer corresponds with the chocolate cover of the candy.
The continental crust is much lighter, or less dense, than the oceanic crust. Because the oceanic crust is more dense, it submerges below the lighter continental crust when the two collide. (Both types of crust ride on top of the solid lithosphere, which is considered part of the crust. The lithosphere then rides on top of the weaker, partially molten asthenosphere, which is part of the mantle).
The mantle is the layer second most familiar to us. The mantle in portions is solid and rocky, but also fluid and molten towards its outer edge in places. Because it is partially solid and partially molten, it can be compared to a plastic, solid but flexible like a Pink Pearl Eraser. It is believed to contain convection currents that drive the movement of crustal plates (refer to Floating Continents). As heat rises to the surface, pieces of crust float around like rafts on a pool, taking thousands of years to move. Mantle thickness ranges from 40 to 2900 kilometers. In our chocolate covered cherry analogy, it is the cream or fluid surrounding the cherry under the chocolate.
Below the mantle is the outer core. Scientists believe that the outer core is composed of a molten, metallic layer 2270 kilometers thick. This layer is believed to contain large amounts of nickel. Scientists have been able to determine that it is a liquid by monitoring earthquake waves as they pass through the Earth's core. The waves dissipate as they pass through this layer in a way that indicates it is liquid and not solid. This is the cherry.
If a chocolate covered cherry had a pit, it would be the inner core, a solid iron-rich mass with a radius of 1216 kilometers. At center of the Earth, the pressure from gravity is thought to be so high, that any material in this location would have to be a solid. Scientists believe that the Earth's magnetic fields are related to the orientations of the outer and inner core.
The following activity allows students to slice through the layers of Earth discovering the different properties of those layers.
If we pretend that we are standing on the surface of this candy, what would we be standing on? How does that chocolate shell correspond with the Earth, and what layer are we standing on? What is below the crust? What do we think it is like? What part of the candy did we say it was like? What about the outer core, where is that found? What about in the cherry candy? What do we think we know about the inner core? Why did we not see it in the candy today? How is the Earth like this chocolate covered cherry? How is it not like this candy? Why do you think we used this candy to illustrate what we think the inside of the Earth is like? Can we see the inside of the Earth? What part can we see (crust)? What else do we know about the crust? Is it completely solid? Is it broken like some of our chocolates?
This activity can also be done with a hard-boiled egg. The shell is the crust, cracked and broken. The egg white, solid but flexible is the mantle. The yolk can be correlated with the outer core, though it is not fluid, and there is no inner core correlation. This variation is less messy.
Included National Parks and other sites:
Utah Science Core:
2nd Grade Standard 6 Objective 1,2,3
Did You Know?
Pronghorn, once roaming the plains of North America in numbers second only to Bison, can be found at Bryce Canyon National Park. They are the fastest land mammal on the continent and only the second fastest mammalian runner in the whole world, reaching speeds of up to 60 mph! More...