This article is written from the post-Advent War perspective, about 1500 years before the modern Reclamation Era.
The Great Basin of Deseret encompasses the arid, mountainous highlands of what was once eastern Nevada and western Utah. Dominated by towering escarpments, desiccated playas, and geothermal springs, the region’s inhospitable geography is deeply symbolic to its inhabitants, who correlate elevation to purity.
Blessed with (struggle), chosen to endure.
When the seas recede and the rains return;
It is our children who will till the land and rebuild
Something about being forged in the heat of standing so close to god.
Climate
Inhospitably hot overall, with amplified extremes. Summers are brutal, with temperatures ranging from 110–130°F (43–54°C) in the valleys. High elevations become frigid easily, though there is no snowpack to encourage the cold to linger. Rainfall is inconsistent, and arrives with enough force to wipe towns from the map.
Hydrology
Deep aquifers (e.g., Snake Valley or Pahranagat Valley).
Highland oases and surviving deep aquifers (such as Snake Valley or Pahranagat Valley) support a network of semi-autonomous valleys owned by regional patriarchs. The dried remains of ancient lakebeds such as Bonneville and Lahontan are deeply pitted from salt and mineral extraction
The Great Basin is at too high of an elevation to be flooded by sea level rise, but without yearly melt from glaciers or the Sierra Nevada snowpack, once-critical rivers such as the Truckee, Humboldt, and Sevier now exist more as roads than as water sources.
Salt flats and playas (like Bonneville Salt Flats or the Black Rock Desert) may fill into shallow seasonal lakes after rare rainstorms. Ancient lakebeds (e.g., Lake Lahontan or Lake Bonneville) might see temporary reflooding, but not sustained water.
Ecology
Desertification dominates and dust storms are common. Existing flora like sagebrush, creosote, and saltbush persist in stressed forms, while invasive species such as brome choke out native life and fuel seasons of wildfire.
The treeline has retreated to the refugia of the isolated highlands, where cooler climate and occasional precipitation supports native piñon pine and juniper trees, as well as sacred groves of imported cedar of Lebanon.
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