How Earth formed and separated into layers
Grade 9 Science Worksheet

Circle the best answer.
A mixture of oil, water and sand is shaken and left to settle. How is this like early Earth, by Esme's reading?
- Densest sinks, lightest floats, as iron sank and rock rose
- Layers appear without any settling
- The lightest part sinks, as the crust did
- Shaking makes the layers, as earthquakes did
Cutaway with blobs of iron in molten rock. Molten iron is denser than molten rock. In a partly molten young Earth, which way would it move, by Jun's reading?
- It sinks toward the center
- It escapes into space through the crust
- It stays where it is
- It rises to the surface
Read this first
Table, Earth's layers (USGS), with columns Layer, Thickness, State
Crust, about 5 km (oceans) to 30 km (continents), solid, brittle; mantle, about 2,900 km, hot, semi-solid rock; outer core, about 2,200 km, liquid iron-nickel; inner core, about 1,250 km, solid iron-nickel.
Using the USGS table, about how far is it from the surface to the top of the core under a continent, by Kira's math?
- About 30 km
- About 2,930 km
- About 5,100 km
- About 2,200 km
Using the table, about how thick is the whole core (outer plus inner), by Luz's math?
- About 6,350 km
- About 950 km
- About 1,250 km
- About 3,450 km
Earth is about 12,750 km wide (USGS). A 30 km continental crust is what fraction of that, by Milo's math?
- About 2.4%
- About 24%
- About 50%
- About 0.24%
Scientists find the outer core is liquid and the inner core solid. Which evidence shows this, by Pia's reading (USGS)?
Cutaway with earthquake wave paths bending and stopping. Cutaway with earthquake wave paths bending and stopping. - Lava from volcanoes is pure core metal brought up from below
- How earthquake waves travel through the layers
- The magnetic field is a solid bar
- Drilling down to the core
Cutaway of the inner core labeled 5,400 °C. NASA gives the inner core a radius of about 1,221 km and a temperature as high as 5,400 °C (9,800 °F). Why is it solid, by Ren's reading?
- It is liquid, like the outer core
- Huge pressure keeps it solid despite the heat
- It is made of light rock
- It is cold, below freezing
Earth is about 4.54 billion years old. On a 4.54 m timeline (1 m per billion years), how far from the start is a mark for 4.0 billion years ago, by Tala's math?
Timeline ruler: 4.54 m long, 1 m per billion years. Timeline ruler: 4.54 m long, 1 m per billion years. 1 m per billion years 4.54 m long start - About 0.54 m
- About 54 m
- About 4.0 m
- About 0.54 mm
Table, Earth's layers (USGS), with columns Layer, Thickness, State
Crust, about 5 km (oceans) to 30 km (continents), solid, brittle; mantle, about 2,900 km, hot, semi-solid rock; outer core, about 2,200 km, liquid iron-nickel; inner core, about 1,250 km, solid iron-nickel.
The mantle has more iron and magnesium than the crust (USGS). How does that fit the sorting story, by Zee's reading?
- The crust should hold the most iron
- The mantle should be the lightest layer, floating above the crust
- Denser, iron-richer rock settled below the lighter crust
- The layers have no differences
Which statement about the lithosphere is right, by Ari's reading (USGS)?
- It is the crust alone, 2,900 km thick
- It is the inner core's surface
- It is the rigid crust plus the upper mantle, at least 80 km thick
- It is the liquid outer core