Volcanoes – Answer Key

Sheet 3. Rows and columns are numbered from the top left, starting at 1.

Answers

  • summit row 11, col 6, right
  • pumice row 3, col 1, right
  • tephra row 2, col 6, right
  • cinder cone row 4, col 13, down
  • molten rock row 5, col 2, right
  • hotspot row 3, col 16, left
  • mudflow row 7, col 14, down
  • tremor row 6, col 2, right
  • shield volcano row 14, col 16, left
  • basalt row 12, col 3, right
  • extinct row 15, col 15, left
  • fumarole row 10, col 9, up
  • dormant row 7, col 16, down
  • pyroclastic row 1, col 13, left
  • plume row 10, col 2, down
  • island arc row 15, col 1, up

A vent in the crust, not just a mountain

A volcano is an opening in a planet’s crust that lets molten rock, gas and ash escape from below the surface. This puzzle’s sixteen words cover the shapes volcanoes take, what actually comes out of them, and the geology that decides where they form in the first place.

What the words mean

Magma versus lava

Magma is molten rock while it is still underground. The moment it reaches the surface and erupts, it gets a new name: lava. The distinction is not just terminology, since magma underground behaves very differently from lava exposed to air, cooling and losing gas far more slowly below the surface. Ash and pyroclastic material are different again, made of shattered rock and glass fragments thrown out during an explosive eruption rather than flowing out as a liquid.

The three main volcano shapes

Not all volcanoes look alike, and the shape usually tells you how the lava behaved when it erupted. A shield volcano forms from thin, runny lava that spreads out over a wide area before hardening, producing a broad, gently sloped shape, and a look at real shield volcano examples shows why they can be enormous in width but relatively low in height. A composite volcano, also called a stratovolcano, builds up from alternating layers of lava and ash into a steep, cone-shaped peak, and an explanation of how composite volcanoes form covers why their eruptions tend to be more explosive than a shield volcano’s. A broader guide to the main types of volcanoes puts shield, composite and cinder cone volcanoes side by side.

Why volcanoes form where they do

Most volcanoes sit along the edges of tectonic plates, the massive slabs of crust that make up Earth’s surface and slowly shift over geologic time. Where two plates collide or pull apart, magma finds a path to the surface, which is why volcanoes tend to cluster in long chains rather than appearing at random. A summary of tectonic plates explains why the Pacific Ocean’s edge, often called the Ring of Fire, hosts such a large share of the world’s active volcanoes.

Eruptions and what they release

An eruption is the release of magma, gas and rock from a volcano, and it can be slow and effusive or fast and explosive depending on how much gas is trapped in the magma and how thick that magma is. A caldera forms afterward in some cases, a large depression left behind when a magma chamber empties and the ground above it collapses. Volcanic gas, mostly water vapor along with carbon dioxide and sulfur compounds, escapes during an eruption and can affect air quality and climate far beyond the immediate area.

Using this in a classroom

The three sheets share the same grid and the same sixteen words, so a class can move between formats without switching vocabulary. The plain grid works well for a review day. The definitions sheet gives a short clue per word, suited to a first introduction to volcano terminology. The word bank sheet lists a brief description next to each word, a middle option for students who need some support but not a full answer.

This puzzle fits grades 4 through 8, when plate tectonics and volcanic activity typically enter the earth science curriculum. Given how much regional volcano content exists on this site, a strong classroom project is to assign students a country or region to research, such as Italy, Japan, New Zealand, or Iceland, and have them report back on the volcano types and eruption history specific to that place. The puzzle and its answer key print as separate pages, which makes it easy to hand out the puzzle in one session and the key in the next without any overlap.

A useful add-on: after the puzzle, have students sort found words into “what happens underground” and “what happens at the surface,” which reinforces the magma-versus-lava distinction that trips up so many students on a test.

What volcanoes and earthquakes do not share

Volcanoes and earthquakes both come from the same underlying cause, plate tectonics, which leads a lot of students to assume they always happen together. They do not. The difference between a volcano and an earthquake comes down to what is actually moving: an earthquake is a sudden release of built-up stress along a fault, while a volcano is an ongoing pathway for magma to reach the surface. A region can have frequent earthquakes with no active volcanoes nearby, and the reverse is also true. Not every volcano even involves magma in the way people expect, either; a look at mud volcanoes shows a very different process, where pressurized mud and gas erupt rather than molten rock. Scientists who study these systems work in volcanology, a field that spends as much time on monitoring and eruption forecasting as it does on the eruptions themselves. For a different puzzle tomorrow, the daily science word search covers new terms every day.