The layers inside the Earth
Grade 6 Science Worksheet

Circle the best answer.
Bo compares two layers. Which is hotter: the mantle or the inner core?
- The mantle, since it is closer to the Sun
- The mantle, since it is made of lava
- Both the same, since deep rock heats up evenly everywhere
- The inner core, since heat rises with depth
USGS says the core is nearly twice as dense as the mantle. Which reason does Esme give?
Cutaway, not to scale, with the core shaded dark and labeled metal, and the mantle labeled rock. Cutaway, not to scale, with the core shaded dark and labeled metal, and the mantle labeled rock. Cutaway, not to scale rock metal - It is iron and nickel metal under great pressure
- A drill sample from the core was weighed
- It is a liquid ocean of heavy lava
- It is cooler down there, so it packs together tighter
Temperature, pressure, density. Temperature, pressure and density all change as you go deeper. Which pattern does Jun find in the USGS notes?
- They peak in the mantle, then fall
- Only temperature increases with depth
- All three increase with depth
- All three decrease with depth
The crust is about 5 km thick under oceans and about 30 km under continents. Where is it thickest, by Kira's reading?
Cross-section, not to scale: the crust under an ocean (thin), under flat land (thicker) and under a mountain range (thickest), with blank depth labels. Cross-section, not to scale: the crust under an ocean (thin), under flat land (thicker) and under a mountain range (thickest), with blank depth labels. not to scale ocean flat land mountain range crust - Under the oceans, since water adds weight
- The same everywhere, about 30 km
- Under flat farmland
- Under big mountain ranges, up to about 100 km
“Cross-section, not to scale:” Luz reads that the crust under the open Pacific Ocean floor, far from any island, is only about 5 km thick. What does that show?
Cross-section, not to scale: thin crust under the Pacific Ocean floor beside thicker crust under a continent. Cross-section, not to scale: thin crust under the Pacific Ocean floor beside thicker crust under a continent. Pacific Ocean floor thin crust continent thicker crust - Ocean crust is thicker than the crust under continents
- The crust is the thickest layer anyway
- Ocean crust is much thinner than continental crust
- The Pacific floor sits right on top of the core
USGS compares the Earth to a boiled egg. In that model, which part of the egg stands for the crust, by Noah's matching?
Drawing of a boiled egg cut in half: shell, white and yolk. Drawing of a boiled egg cut in half: shell, white and yolk. boiled egg cut in half shell white yolk - The yolk
- The whole egg, since the crust is thick
- The white
- The thin shell
Drawing of a boiled egg cut in half beside a cutaway of the Earth, not to scale. USGS says the core is unlike an egg yolk in one way. Which difference does Pia find?
- The core is the thinnest layer
- The core is made of stone, just like the mantle is
- The core is cooler than the mantle
- The core has two parts, one liquid and one solid
In the egg model, the egg white stands for the mantle. In which way is the white a good match, says Ren?
Drawing of a boiled egg cut in half: shell, white and yolk. Drawing of a boiled egg cut in half: shell, white and yolk. boiled egg cut in half shell white yolk - It is runny and liquid, the way a lava ocean would be
- It is a thick layer between the shell and the yolk
- It is the thinnest part
- It is the hottest part
Drawing of a ball about 13 cm across, labeled "1 cm stands for about 1,000 km". Drawing of a ball about 13 cm across, labeled "1 cm stands for about 1,000 km". ball about 13 cm across 1 cm stands for about 1,000 km Tala makes a ball model of Earth about 13 cm wide, so 1 cm stands for about 1,000 km. About how thick is the 30 km continental crust on it?
- About 3 mm
- About 30 cm
- About 3 cm
- About 0.3 mm
The deepest hole ever drilled is about 12 km (USGS). On the ball model, where 1 cm stands for about 1,000 km, how deep does Ari draw it?
Use the picture in question 9.
- About 1.2 cm, well into the mantle
- About 0.12 mm, not even through the crust
- About 12 cm, nearly across the whole ball
- Down to the core