Google Gravity Lava Mr Doob |top| Page

"Google Gravity Lava" is a classic browser-based physics experiment created by

While the standard Google Gravity remains a landmark in browser-based creativity, the lava version adds a sensory layer of heat, fluidity, and chaos — turning a search page into a molten playground.

Whether you are using the Standard Gravity or the Lava variant, the interactivity is what sets Mr.doob’s work apart from a static video. Google Gravity Lava Mr Doob

Google Gravity is an interactive web experiment created by Ricardo Cabello, a developer widely known as . It is a physics-based simulation that breaks the standard layout of the Google homepage, causing all interface elements—such as the logo, search bar, and buttons—to fall to the bottom of the browser window as if affected by gravity. ☄️ Key Experiments by Mr.doob

Google Gravity (and its lava remix) helped inspire a wave of “break the internet” experiments: Google Sphere, Google Space, Google Underwater. More importantly, it – showing that a single developer with three.js could turn the world’s most visited webpage into a lava lamp. "Google Gravity Lava" is a classic browser-based physics

Here’s a creative write-up for — a playful, interactive web experiment.

When you load the page, the familiar Google interface suddenly loses its foundation. The logo, search bar, and buttons all crash to the bottom of the screen. It is a physics-based simulation that breaks the

In versions explicitly featuring the "lava" effect, the interaction becomes more visceral. The viscosity of the "lava" often creates additional drag on the objects. Elements may sink slower or appear to be "sizzling" as they rest on the bottom of the page. The particle effects involved mimic the flow of liquid, making the destruction of the Google homepage feel more organic and chaotic than the rigid block drop of the standard version.

Rather than just falling like blocks, web elements could be melted down. Web GL (Web Graphics Library) allowed the browser to render thousands of independent particles simultaneously. These particles interacted with one another, mimicking the viscosity, surface tension, and flow of real lava or liquid mercury.