Volcano Patterns
Hotspots & Hawaii
Earthquakes
Hazard Maps
Seismic Waves
100

This is where most volcanoes are found on Earth

What are plate boundaries

100

This is a stationary source of magma beneath a moving tectonic plate

what is a hotspot

100

This is where most earthquakes occur.

Plate boundaries


100

These maps show the probability of earthquakes or volcanoes in an area.

hazard map

100

This tool measures ground motion during an earthquake.

seismograph

200

This famous region around the Pacific Ocean has many active volcanoes

what is the Ring of Fire

200

in a hotspot chain, this island is most likely to be volcanically active

What is the island of Hawaii

200

This type of plate boundary is known for earthquakes but not volcanoes.

what is a transform boundary
200

These maps are used instead of predicting the exact time of earthquakes.

Risk Map

200

This type of data does a seismograph collect.

Ground motion over time

300

This type of boundary forms volcanoes when plates collide

Convergent Boundary

300

This process explains how the Hawaiian Islands formed over time

what is plate movement over a hotspot

300

This is the MOST important evidence scientists use to predict earthquake risk.

what is past earthquake locations

300

This is what areas with many past earthquakes are likely to have in the future.

More earthquakes

300

This improves when scientists add more seismographs to a network.

Accuracy / detection ability

400

This type of plate boundary forms volcanoes where plates pull apart

Divergent Boundary

400

This happens to older islands as they move away from the hotspot

What is they become inactive

400

This pattern of earthquakes helped scientists understand plate tectonics.

They occur in narrow zones

400

This is one way cities use hazard maps to stay safe.

building codes / city planning

400

Scientists use long-term seismograph data to identify this.

High-Risk areas

500

This is why volcanoes appear in clusters instead of randomly

What is plate movement / interactions

500

This evidence from island age proves tectonic plates are doing this

What is moving

500

This is what aftershocks tell scientists about stress in Earth’s crust.

Stress is still adjusting along faults

500

This is why scientists cannot predict the exact time of earthquakes.

Unpredictable

500

This incorrect idea is something seismographs CANNOT do.

Predict exact earthquakes