Introduction
The Plateau is the last stable surface on a planet that no longer supports balance. Formed by crustal rebound after the hydrosphere retracted, it is a region of uplifted terrain—broad shelves of fractured rock, continental shelf boundary, and sedimentary buildup that both offers relief from the silt and heat of lower elevations and holds the remaining freshwater aquifers of Earth, deep below its surface.
Elevations range from 500 to 1,200 meters, above the exposed lowlands, formerly the oceanic abyssal plains. Sharp ridges formed were fault zones fractured, and half-submerged rusted monoliths dot the terrain where oceanic vessels became moored, and then stripped by wind, sand, and salvage gangs.
The terrain carries the memory of continental drainage: dried rivers, long-dead ocean species now trapped in clay deposits, and water reservoirs driven deep by shifting sand and tectonic pressure.
Weather
Temperatures swing harshly, with daytime heat reaching up to 60°C. Evening temperatures hover between 15-20°C, providing some relief, with optimum travel hours being at early and mid-morning. This is when most caravans travel, content to trade the heat for a chance encounter with raiders, hostile city-state militias, or wild animals that use the cover of darkness to spring a surprise attack.
Key Effects
- Wind dominates the surface, bringing with it sand, ash, and fine dust from the alkali plains and the silt-choked valleys below.
- Static discharges occur regularly near exposed steel or glass, a result of layered atmospheric friction.
- Rain falls rarely. When it does fall the results can be unpredictable—the sand and dust no longer capable of quickly absorbing runoff.
- Sandstorms and Scirocco are common. Haboob clouds can cause entire cities to close their gates and take shelter inside the walls.
- Lightning storms are common, especially during sandstorms. Caravans take note of this and equip themselves with electrostatic attractors.
Everyone works around the weather. Nothing is immune from its effects. Aside from the beasts that prowl the sands, only the Dryrunner Wahka move during the hottest portions of the day.
Terrain Features
The Plateau does not resemble a single biome. It is an amalgam of post-collapse features: badlands that were once agricultural plains, reed-choked dust basins that formed in drainage hollows, and artificial verdant pockets tied to remaining water systems.
Patches of Bygone Era infrastructure still exist, often half-buried or fused into the landscape—visible as concrete ridges, steel building frames, open mine shafts, or corroded tower bases.
The dust here isn’t just sand. It’s the pollutants and byproducts of 3,000 years of failed industry. This is the true footprint the Anthropocene has left behind: new materials not created by nature, baked into the rock and forming layers of sediment.
The environment is unforgiving but consistent. This consistency—more than fertility, moisture, or biodiversity—is why the Plateau remains central to life in Errata.
It is high enough to avoid total atmospheric breakdown, flat enough to support movement and construction, and stable enough to permit the storage and transmission of power. At its highest elevations the former great cities of the world cling to life, or at least those that survive do.
In Errata, that alone is rare enough to define the region’s importance. Survival here is not a gift of nature, but the outcome of environmental coincidence and strategic retention.
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