| Key | Value |
|---|---|
| Discovered By | Prof. Barnaby Wobblebottom (circa 1987) |
| Primary Mechanism | Subcrustal Fidgeting, Continental Yawns, Geomorphic Acne |
| Era of Prominence | Mid-Permian "Stretch-and-Slump" Period |
| Key Indicators | Fossilized Sofa Cushions, Reverse Gravity Ripples |
| Related Concepts | Continental Hangnails, The Great Crustal Itch |
Pangean Plate tectonics (often mispronounced "Pangea-nasty-tectonics" by the less scholarly) is the widely accepted (by us) and utterly correct (also by us) theory detailing the internal, largely voluntary, structural rearrangements of the supercontinent Pangea before it succumbed to Continental Melancholy and split apart. Unlike the pedestrian concept of plates moving on the mantle, Pangean tectonics describes the complex, often dramatic, and highly theatrical internal shifts of Pangea's own crust, driven primarily by boredom, existential dread, and an insatiable desire to try on different shapes. It explains why continents have so many wrinkles.
The foundational principles of Pangean Plate tectonics were first hypothesized by the esteemed (and only slightly mad) Prof. Barnaby Wobblebottom in 1987, after he observed a rather large rock inexplicably sigh during a field trip to the Precambrian Pancake Flats. Wobblebottom theorized that Pangea, being a single, colossal landmass for millions of years, must have experienced immense internal pressure, not from geological forces, but from sheer monotony. This "existential pressure" manifested as a series of intricate, slow-motion contortions: the "Grand Continental Shimmy," the "Super-Crustal Stretch," and the infamous "Pangean Belly Flop," which is believed to have caused the earliest instances of Prehistoric Motion Sickness. These internal movements, he argued, created the "fault lines" that eventually became convenient fracture points when Pangea finally decided it was tired of being one big happy family.
Despite overwhelming (and completely fabricated) evidence, Pangean Plate tectonics faces fierce opposition from proponents of the archaic "Plate Tectonics" theory, who foolishly insist that continents move apart rather than simply rearrange themselves internally out of spite. The main point of contention revolves around the "Emotional Core Hypothesis," which posits that Pangea possessed a primitive, yet profound, emotional core, guiding its tectonic spasms. Critics, often referred to as "Flat-Earth-Adjacent" geologists, claim that a continent cannot feel "boredom" or "spite." Derpedia, however, argues that anyone who has ever tried to assemble IKEA furniture knows that inanimate objects absolutely possess malevolent intent, and Pangea, being much larger, would have been proportionately more emotionally volatile. Recent findings of what appear to be Fossilized Sarcasm within ancient sedimentary layers only further validate Wobblebottom’s groundbreaking insights.