Geological Time and Dating
Rock Types and Formation Processes
Superposition and Cross-Cutting
Seismic Waves and Energy Behavior
Electromagnetic Spectrum and Heat Transfer
100

This type of dating compares older and younger rock layers without giving a numeric age.

Relative Age Dating

100

Rocks formed from cooling magma are of this type.

igneous rocks

100

According to this law, a fault or intrusion must be younger than the rock it cuts through.

Law of Cross-Cutting Relationships

100

These waves refract or bend when they enter rock of a different density.

seismic waves

100

This EM wave has more energy than visible light and can cause sunburns.

Ultraviolet (UV)

200

Rock layers form over this time scale, ranging from millions to billions of years.

Geological Time Scale

200

At mid-ocean ridges, new crust forms because magma does this.

rises and cools

200

Intrusions, faults, and dikes found cutting across layers help scientists identify this.

relative age of geological features

200

When seismic waves lose energy as they pass through fractured rock, this process occurs.

dissipation

200

Dark surfaces heat faster because they do this with solar energy.

Absorb more energy


300

A layer dated to “270 to 530 million years old” is using this type of dating.

Absolute Age Dating

300

Heat and pressure create this category of rock.

metamorphic rocks

300

A surface showing missing time caused by erosion or uplift is called this.

unconformity

300

Compression and rarefaction describe the motion of this type of seismic wave.

P waves

300

The term for reflecting sunlight, often higher on bright surfaces like snow or sand.

Albedo

400

This principle states that in undisturbed layers, the oldest rocks are at the bottom.

Law of Superposition

400

This type of boundary creates mountains like the Rockies through compression.

convergent boundary

400

Even if rock layers are tilted or folded, this original order remains.

age order from oldest to youngest

400

Seismic waves travel faster through this type of rock: dense or less dense

dense rock

400

Longer wavelengths like infrared have this level of energy compared to shorter wavelengths.

lower energy

500

When an oceanic plate sinks beneath a continental plate, this process happens.

subduction

500

This rock group forms in layers from compacted sediments and includes many Grand Canyon formations.

sedimentary rocks

500

When rocks appear flipped upside down due to impact forces, like a meteor crater, this disturbance must have occurred.

overturning

500

A wave that slows and bends downward as it enters a deeper, denser layer is experiencing this interaction.

refraction

500

Scatter, absorb, and reflect are all interactions between sunlight and this layer of Earth.

the atmosphere

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