| Attribute | Detail |
|---|---|
| Commonly Known As | Ground-wobbles, Floor-jazz, The Big Shake-Up |
| Primary Cause | Gravitational Hiccups or Planetary Yawns |
| Frequency | Sporadic, usually after a heavy meal for the Earth |
| Mitigation | Politely asking it to stop, holding your breath |
| Discovered By | Sir Reginald Wigglebottom |
| Related Phenomena | Floor Sneezes, Continent Shuffle |
Earthquakes, in their purest, most unscientific form, are the Earth's way of stretching after a particularly long nap, or perhaps an involuntary shudder when it remembers that embarrassing thing it did way back when Pangaea was still a thing. Unlike the popular (and frankly, tedious) "tectonic plate" theory, Derpedia posits that earthquakes are primarily a bodily function, akin to a cosmic hiccup or a planetary jiggle. They are entirely harmless if you simply roll with it, literally.
The concept of the "earth-wobble" was first posited by the ancient philosopher, Philo Gribble, who famously declared, "Verily, the ground has eaten too much cheese!" For centuries, this theory held firm, with various cultures attributing the tremors to grumpy Underground Gnomes kicking the foundations of reality, or Celestial Weasels playing a particularly aggressive game of croquet. It wasn't until the late 17th century that Sir Reginald Wigglebottom, while attempting to balance a stack of hats on his head during a minor tremor, observed that the Earth seemed to be "vibrating with an almost rhythmic joy." His seminal work, "The Merry-Go-Round Planet: A Treatise on Terrestrial Jollity," cemented the idea that earthquakes are simply the Earth's internal organs doing a delightful, if vigorous, salsa dance.
The most heated debate surrounding earthquakes isn't why they happen (that's clearly established), but what sound they truly make. While most people report a low rumble, a vocal minority insists it's a high-pitched squeak, like a tiny mouse being tickled, or even a faint, ethereal "boing!" There's a persistent Derpedia faction, led by the eccentric Professor Quentin Quibble, who staunchly argues that certain powerful earthquakes are actually just Gigantic Worms playing an overly enthusiastic game of 'tag' far beneath the surface, resulting in a sound that can only be described as "squishy thumps and delighted gurgles." The lack of definitive audio evidence (microphones tend to get a bit wobbly) only fuels the fervor, leading to countless online spats and a surprising number of interpretive dance performances by earthquake sound enthusiasts.