History

Each row is 15 minutes of ground motion, oldest at the top — read it like lines on a page. Height means how hard the ground moved, so an earthquake is a sudden fat burst that tapers away, while ordinary noise is an even fuzz.

The four colours carry no meaning. They cycle red, green, blue, black purely so your eye can follow one row without sliding into the next. This is a single sensor recording a single channel — not four feeds at once.

Faded stretches are things happening nearby — footsteps, a door, a car. They are identified by pitch: only something within a few metres arrives with energy above 15 Hz, because distance strips the high frequencies out of a real earthquake. The solid core drawn inside a faded burst is the 1–8 Hz part, the band a quake would occupy.

Coloured triangles mark where an earthquake from the USGS catalogue should have arrived — where to look, not a claim that this station caught it. Full guide to reading the drum →

See what a real earthquake looks like on this drum → the M4.2 Cloverdale quake of 29 July 2026, 45 km away

a saved image of that night’s drum, shown at half size — not live

Nothing like the little bursts. At 02:40 UTC the trace swings three rows up and three rows down — the drum clips there on purpose, so a big event reads as a big event without wrecking its neighbours — and takes about 80 seconds to die away, tapering the whole time. Everything else on these four hours is the ordinary fuzz of a summer night: cars on the highway, the air conditioner, a door. People in Santa Rosa felt this one as a single jolt.

The small blip on the 03:45 row, about 3½ minutes in, is a M2.2 aftershock from the same spot — what a quake nobody feels looks like: a burst that still starts sharp and tapers, just a hundred times smaller.