Structure & Composition
Temperature & Density
Thickness & Layers
Plate Boundaries & Movement
Geologic Events
100

This is the thin, solid outermost layer of Earth where we live; it is made mostly of rock and is composed of continental and oceanic types

Crust (continental and oceanic crust).

100

Compared to the crust, the mantle is generally this: hotter or colder?

 Hotter.

100

Which Earth layer is the thickest by depth?

 Mantle.

100

 The theory that explains the movement of Earth's plates is called what?

 Plate tectonics.

100

A sudden release of energy in Earth that causes shaking is called a what?

An earthquake.

200

The mantle is made of this type of material that is solid but can flow slowly over long times; name it (two words)

 Solid rock that can slowly flow (mantle rock / solid rock that behaves plastically / peridotite)

200

Density typically increases or decreases as you go from the crust to the core? Choose one.

Increases.

200

About how thick (in kilometers) is the Earth's crust on average (give a rounded range for continental crust)?

Continental crust: about 25–70 km (commonly cited ~30–50 km); oceanic crust is much thinner (~5–10 km).

200

Name the three main types of plate boundaries.

Divergent, convergent, transform

200

 Name one geologic event that commonly occurs at convergent plate boundaries. 

Volcanic eruptions, mountain building, deep ocean trenches (any one).

300

The inner core is composed mainly of this metal, which makes it very dense and solid

 Iron (mostly iron, with some nickel).

300

 Approximate relative temperature: is the inner core hotter, cooler, or about the same as the mantle?  

Hotter.

300

What is the lithosphere and which layers does it include?

 The lithosphere is the rigid outer layer composed of the crust and the uppermost solid mantle.

300

 At what type of plate boundary do plates move toward each other and often form mountains or cause subduction?

Convergent boundary (especially oceanic-continental or oceanic-oceanic leading to subduction).

300

Explain how subduction can lead to volcanic eruptions (2–3 sentences).

When one plate subducts beneath another, the subducted plate melts as it sinks into the hotter mantle; magma forms and can rise through the overriding plate to feed volcanic eruptions.

400

Give two compositional differences between the continental crust and the oceanic crust.

Continental crust: thicker (~30–70 km), less dense, composed largely of granitic rocks; Oceanic crust: thinner (~5–10 km), denser, composed mainly of basaltic rocks

400

Explain briefly how temperature and pressure together explain why the inner core is solid despite being extremely hot

Very high pressure in the inner core forces atoms into a solid lattice despite very high temperatures; pressure raises the melting point.

400

 Explain the difference between the lithosphere and the asthenosphere in one or two sentences.

 The lithosphere is rigid and brittle; the asthenosphere lies below it, is hotter, weaker, and can flow, allowing plates to move

400

Describe what happens at a transform boundary in one sentence and give one real-world example.

Transform boundary: plates slide past each other horizontally, causing earthquakes (example: San Andreas Fault

400

Describe two differences between earthquakes and volcanic eruptions in terms of causes and effects.

Earthquakes are sudden releases of energy along faults and mainly cause ground shaking; volcanic eruptions involve magma, lava, ash, and gases and can build cones or cause widespread ashfall. Earthquakes are usually instantaneous events (seconds to minutes) while volcanic activity can be prolonged.

500

Describe, in one sentence, the primary composition of the outer core and explain why it is liquid while the inner core is solid.

Outer core is mostly molten iron and nickel (liquid) because temperatures are high enough to melt it and pressure is lower than in the inner core; inner core is solid iron-nickel due to extremely high pressure.

500

Rank these layers from least dense to most dense: mantle, crust, inner core, outer core.

 Least dense → crust, mantle, outer core, inner core → Most dense.

500

 Provide approximate thickness ranges (in km) for: crust, mantle, and core  

Crust: ~5–70 km; 

Mantle: ~2,900 km; 

Core (inner + outer): ~3,480 km

 (outer ~2,260 km + inner ~1,220 km).

500

 Explain how convection in the mantle helps drive plate movement (2–3 sentences)

Mantle convection involves heating near the core and cooling near the surface; warm mantle rock rises and cooler rock sinks, creating convection currents that exert drag and push on the base of tectonic plates, helping drive their movement

500

Construct a short explanation (3–4 sentences) that connects plate tectonic movement to both earthquakes and volcanic eruptions, using correct scientific terms.

The motion of lithospheric plates is driven by mantle convection, slab pull, and ridge push. Where plates interact, stress builds up along plate boundaries; sudden release of that stress causes earthquakes. At convergent boundaries or hotspots, subduction or melting of mantle material produces magma that rises and causes volcanic eruptions. Both processes are direct results of plate tectonic movement.