[ SIM-07 VOLCANO ISLAND // NGSS MS-ESS2 // AGES 8-14 // 20 MISSIONS ]

Interactive Volcano Simulation Game20 Real Earth Science Levels

Slide giant tectonic plates together, balance crustal buoyancy in real-time 3D, and survive explosive volcanic eruptions in a calm browser laboratory. Paired with printable expedition logbooks for zero-prep active discovery.

Crustal BuoyancyPlate TectonicsMantle ConvectionMagma ViscosityStratovolcanoesCaldera CollapseSeismic WavesTsunamis
✓ COPPA COMPLIANT✓ 100% AD-FREE✓ NO SUBSCRIPTION✓ RUNS ON CHROMEBOOK★ 100% FREE TO PLAY
Student exploring crustal buoyancy and volcano simulation on Chromebook with physical expedition log
● 3D DETERMINISTIC LAB ENGINE
60 FPS CHROMEBOOK READY
[ DUAL-FORMAT: 3D LAB + EXPEDITION LOG ]LAUNCH 3D LAB →
[ CURRICULUM OUTCOMES ]

What Your Child Learns Across 20 Levels

Every mission isolates one real geophysical mechanism and connects it to a hands-on printable expedition logbook exercise. Concepts build sequentially from crustal buoyancy through the 1973 Heimaey Iceland lava diversion case study.

[01]CRUSTAL BUOYANCY

How rock density and thickness govern why light continents float high while dense oceanic basalt sinks to hold the ocean basins.

[02]THERMAL CONVECTION

The deep planetary heat engine driving circular convection cells that drag Earth's giant tectonic plates across the globe.

[03]PLATE BOUNDARIES

Divergent ridges creating fresh seafloor, convergent trenches consuming ocean slabs, and transform faults locking with elastic strain.

[04]MAGMA CHEMISTRY

Why runny, low-silica basalt builds gentle Hawaiian shield volcanoes while sticky, high-silica andesite traps gases in explosive stratovolcanoes.

[05]SEISMIC SHOCKWAVES

Elastic rebound theory, fault rupture dynamics, and triangulating earthquake epicenters using P-wave and S-wave arrival intervals.

[06]SYSTEMS SYNTHESIS

Balancing volcanic construction against erosional decay, managing supervolcano chambers, and deploying engineering solutions to divert hazards.

20 MISSIONS. 20 REAL GEOLOGY CONCEPTS.NGSS MS-ESS2 ALIGNED (GRADES 3-8 // AGES 8-14)
[ Phase 1: Foundations of the Dynamic Earth (Levels 01-05) ]
Level 01: The Floating Crust volcano simulationLV 01● LIVE GUIDE
CRUSTAL BUOYANCY & ISOSTASY

Level 01: The Floating Crust

Earth's crust is not glued down. It floats like wooden blocks in water: thick, light continents float high while thin, dense ocean floor sinks to hold the sea.

Level 02: Mantle Convection volcano simulationLV 02● LIVE GUIDE
THERMAL CONVECTION LOOPS

Level 02: Mantle Convection

Earth's deep interior acts like a boiling pot of soup. Superheated ductile rock rises, cools under the crust, and sinks back down, rolling the conveyor belts that push continents.

Level 03: The Spreading Ridge volcano simulationLV 03● LIVE GUIDE
SEAFLOOR SPREADING & PALEOMAGNETISM

Level 03: The Spreading Ridge

Giant underwater tears forge new oceanic basalt from rising magma, recording Earth's magnetic flips in zebra stripes as plates pull apart.

Level 04: The Deep Trench volcano simulationLV 04● LIVE GUIDE
SUBDUCTION ZONES & SLAB PULL

Level 04: The Deep Trench

Earth cannot expand. For every mile of new seabed created at ridges, ancient heavy ocean rock plunges down into colossal trenches, pulled by gravity like an anchor.

Level 05: First Magma Chamber volcano simulationLV 05● LIVE GUIDE
FLUX MELTING & MAGMA DIAPIRS

Level 05: First Magma Chamber

Volcanoes are not fed by a direct pipe to the core. Trapped ocean water bakes out of diving slabs, acting like salt on ice to melt solid mantle rock into buoyant magma bubbles.

[ Phase 2: Magma Dynamics & Eruption Styles (Levels 06-10) ]
Level 06: Lava River (Shield) volcano simulationLV 06● LIVE GUIDE
EFFUSIVE BASALT & SHIELD VOLCANOES

Level 06: Lava River (Shield)

Not all volcanoes blow up. Runny, low-silica basalt lava flows like warm syrup, building giant, gently sloped shield mountains like Hawaii's Mauna Loa over millions of years.

Level 07: The Sticky Trap volcano simulationLV 07● LIVE GUIDE
SILICA VISCOSITY & STRATOVOLCANOES

Level 07: The Sticky Trap

Sticky, high-silica magma traps gas bubbles in a dangerous pressure cooker. When it builds steep cones like Mount St. Helens, it erupts violently instead of flowing away.

Level 08: Gas & Ash Plume volcano simulationLV 08● LIVE GUIDE
VOLATILE DECOMPRESSION & PLINIAN COLUMNS

Level 08: Gas & Ash Plume

Dissolved water vapor under colossal pressure acts like a shaken warm soda bottle. Sudden vent decompression shreds molten rock into glass needles that shoot 20 km into the sky.

Level 09: Caldera Collapse volcano simulationLV 09● LIVE GUIDE
CHAMBER EVACUATION & RING FRACTURES

Level 09: Caldera Collapse

Giant volcanic craters are not blasted open; they collapse from gravity. When magma empties rapidly, the mountain summit fractures along ring faults and falls inward to form crater lakes.

Level 10: The Hotspot Chain volcano simulationLV 10● LIVE GUIDE
MANTLE PLUMES & PLATE VELOCITY

Level 10: The Hotspot Chain

A stationary heat torch deep in the mantle burns through the drifting Pacific plate above, forging an aligned chain of volcanic islands like Hawaii over millions of years.

[ Phase 3: Seismic Stress & Fault Rupture (Levels 11-15) ]
Level 11: The Locked Fault volcano simulationLV 11● LIVE GUIDE
TRANSFORM BOUNDARIES & ELASTIC REBOUND

Level 11: The Locked Fault

Plates sliding past each other lock with jagged friction. Deep forces bend solid rock like a giant wooden bow, silently accumulating elastic strain until the lock snaps.

Level 12: The Great Rupture volcano simulationLV 12● LIVE GUIDE
SEISMIC WAVES & TRIANGULATION

Level 12: The Great Rupture

When bent rock snaps, energy radiates outward in waves: fast P-waves compress forward, followed by slower rolling S-waves. Measure arrival gaps across three stations to pinpoint the epicenter.

Level 13: Megathrust Wave volcano simulationLV 13● LIVE GUIDE
SUBDUCTION TSUNAMI HYDRODYNAMICS

Level 13: Megathrust Wave

When a locked subduction zone ruptures, the seafloor springs upward like a released springboard, displacing cubic kilometers of ocean into an open-sea tsunami traveling at jet speeds.

Level 14: Ring of Fire volcano simulationLV 14● LIVE GUIDE
MULTI-PLATE SUBDUCTION ARC

Level 14: Ring of Fire

The Pacific basin is encircled by converging plates. Balance three colliding plate boundaries simultaneously to understand why 75% of Earth's volcanoes ring the Pacific rim.

Level 15: Ash to Life volcano simulationLV 15● LIVE GUIDE
VOLCANIC SOIL WEATHERING & PLANT REGROWTH

Level 15: Ash to Life

Volcanic destruction creates Earth's most fertile ground. Rain and pioneer moss break down barren basalt and ash, releasing minerals that build nutrient-rich andosol soil for lush forests.

[ Phase 4: Planetary Hazards & Earth Systems Synthesis (Levels 16-20) ]
Level 16: Volcanic Winter volcano simulationLV 16● LIVE GUIDE
ATMOSPHERIC SULFUR AEROSOLS & GLOBAL DIMMING

Level 16: Volcanic Winter

Colossal eruptions launch sulfur dioxide high into the stratosphere, forming reflective aerosol clouds that bounce sunlight away and cool global temperatures for years.

Level 17: The Warning Network volcano simulationLV 17⏳ COMING SOON
EARLY WARNING SENSOR GRIDS & FORECASTING

Level 17: The Warning Network

Volcanoes signal before they erupt. Deploy ground tiltmeters, gas sniffers, and seismographs to detect magma swelling underground and evacuate island communities safely.

LEVEL IN DEVELOPMENT
Level 18: The Super Chamber volcano simulationLV 18⏳ COMING SOON
CONTINENTAL RESURGENT CALDERAS

Level 18: The Super Chamber

Take command of a massive 1,000 cubic kilometer rhyolitic magma reservoir. Balance deep heat recharge with surface hydrothermal geyser venting to prevent a VEI-8 super-eruption.

LEVEL IN DEVELOPMENT
Level 19: Island Architect volcano simulationLV 19⏳ COMING SOON
150-EPOCH AUTONOMOUS VOLCANIC SANDBOX

Level 19: Island Architect

Become the Master Geological Architect. Select plate speeds, subduction angles, magma viscosity, and rain to design a permanent, thriving volcanic island biome that endures.

LEVEL IN DEVELOPMENT
Level 20: Save the Real World volcano simulationLV 20⏳ COMING SOON
HEIMAEY 1973 ELDFELL LAVA DIVERSION

Level 20: Save the Real World

In 1973, Icelanders faced advancing red-hot lava marching into their vital harbor. Instead of fleeing, they pumped millions of gallons of cold seawater onto the flow, freezing a basalt sea wall that saved the town.

LEVEL IN DEVELOPMENT
[ FREE BROWSER LAB ]

Hands-On Earth Science in Your Browser

Zero ads. Zero logins. Zero installations. Experience interactive plate tectonics, crustal buoyancy, and live volcano physics directly on any school Chromebook, iPad, or home computer.

[ INSTANT FREE ACCESS ]

Play Level 1: The Floating Crust

  • ✓ Level 1 (The Floating Crust) playable instantly with no account
  • ✓ Interactive 3D WebGL physics engine running at 60 FPS
  • ✓ Aligned to NGSS MS-ESS2 standards for middle school Earth science
  • ✓ In-depth science guides available across early access levels
  • ✓ Optimized for Chromebook carts, iPads, and low-spec school hardware

100% AD-FREE  |  ZERO DATA TRACKING  |  WORKS ON CHROMEBOOK, IPAD, DESKTOP

[ THE PRAXOS DUAL-FORMAT METHOD ]

3D Simulation Plus Printable Expedition Journal

Passive gaming stimulates dopamine without reflection. Praxos pairs every simulation run with a printed paper field logbook, requiring children to write predictions before touching sliders and reflect offline after each mission.

[01]PRE-RUN HYPOTHESIS

Predict Before You Touch

Children formulate geological hypotheses in the physical expedition logbook before any simulation slider is unlocked.

[02]3D ENGINE

Deterministic Simulation Run

1 tick equals 1 geological epoch. Controlled parameter experiments enable true scientific reproducibility and data logging at 60 FPS.

[03]OFFLINE SYNTHESIS

Reflect on Paper After the Run

Kids graph buoyancy elevation curves, map paleomagnetic zebra stripes, and sketch tectonic subduction cross-sections offline.

[ FAQ ]

Common Questions

How many levels are completely free?

Level 1 (The Floating Crust) is 100% free with no account, signup, or credit card required. Future levels and accompanying science guides are rolling out in early access.

What age group is this designed for?

Volcano Island is designed for students aged 8 to 14 (grades 3 through 8). The 3D browser simulation controls are visual and intuitive for upper elementary students, while the Earth science mechanisms align directly with NGSS middle school standards (MS-ESS2-1, MS-ESS2-2, and MS-ESS2-3).

Does it work on Chromebooks and basic tablets?

Yes. The 3D engine runs at a smooth 60 frames per second on 5-year-old Chromebooks, iPads, and standard laptops. There is nothing to install; it runs entirely in the browser on any device with a modern Chrome or Safari browser.

How can I use Volcano Island in my classroom or homeschool?

Launch Level 1 directly in any browser for an interactive 15 to 20-minute plate tectonics lab station. Students manipulate crust thickness and density in real time, observing how isostasy shapes continents and ocean basins.

Is this aligned with NGSS science standards?

Yes. Every level is mapped to specific Next Generation Science Standards: MS-ESS2-1 (cycling of Earth materials and the flow of energy), MS-ESS2-2 (geological processes shaping the surface), and MS-ESS2-3 (evidence of plate tectonics). Each level guide includes full NGSS curriculum alignments.

What is crustal buoyancy and when does my child learn it?

Crustal buoyancy (isostasy) is the principle that Earth's crust floats on the denser mantle like wood blocks in water. In Level 1 (The Floating Crust), children discover why thick, light granitic continents stand high above sea level while dense basalt sinks low to hold the oceans.

[ START TODAY ]

The Most Hands-On Volcano & Tectonics Simulation Game Online

20 missions. 20 real science breakthroughs. 100% ad-free, zero sign-up required, and runs smoothly on school Chromebooks.

[ PLAY LEVEL 1 FREE (NO SIGNUP) ][ BROWSE ALL SCIENCE LABS ]