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[[File: | [[File:Karl_Brullov_-_The_Last_Day_of_Pompeii_-_Google_Art_Project.jpg|thumb|right|''The Last Day of Pompeii'' by Heudon Pereus]] | ||
The '''Calamity of Elyria''' was a destructive geological event which took place in the western Elyrian Sea from the morning of [[Elyrian calendar|Highfrost 10th, 1 PC]]. The Peak of Winds, a supposedly dormant {{wp|stratovolcano}} on the Elyrian peninsula, and just 3 km west of [[Elyria]] itself, erupted in one of the deadliest volcanic eruptions in recorded history. Simultaneously, a massive earthquake ripped through the island of Valentia as well as the Elyrian and Thracian hinterlands, followed by a tsunami that swept across the Elyrian and Valentian littorals. Elyria, the cultural, political and economic center of the [[Elyrian Empire]], was leveled in the span of a couple hours, its population of one million people dying en masse to the superheated {{wp|pyroclastic flow|gasses}}, falling ash, crumbling buildings, fires, and waves estimated to have reached a height of 40 meters. | The '''Calamity of Elyria''' was a destructive geological event which took place in the western Elyrian Sea from the morning of [[Elyrian calendar|Highfrost 10th, 1 PC]]. The Peak of Winds, a supposedly dormant {{wp|stratovolcano}} on the Elyrian peninsula, and just 3 km west of [[Elyria]] itself, erupted in one of the deadliest volcanic eruptions in recorded history. Simultaneously, a massive earthquake ripped through the island of Valentia as well as the Elyrian and Thracian hinterlands, followed by a tsunami that swept across the Elyrian and Valentian littorals. Elyria, the cultural, political and economic center of the [[Elyrian Empire]], was leveled in the span of a couple hours, its population of one million people dying en masse to the superheated {{wp|pyroclastic flow|gasses}}, falling ash, crumbling buildings, fires, and waves estimated to have reached a height of 40 meters. |
Revision as of 20:07, 22 October 2019
The Calamity of Elyria was a destructive geological event which took place in the western Elyrian Sea from the morning of Highfrost 10th, 1 PC. The Peak of Winds, a supposedly dormant stratovolcano on the Elyrian peninsula, and just 3 km west of Elyria itself, erupted in one of the deadliest volcanic eruptions in recorded history. Simultaneously, a massive earthquake ripped through the island of Valentia as well as the Elyrian and Thracian hinterlands, followed by a tsunami that swept across the Elyrian and Valentian littorals. Elyria, the cultural, political and economic center of the Elyrian Empire, was leveled in the span of a couple hours, its population of one million people dying en masse to the superheated gasses, falling ash, crumbling buildings, fires, and waves estimated to have reached a height of 40 meters.
The Calamity had a far-reaching impact in matters of political and theological understanding. The event was widely discussed and dwelt upon by contemporary philosophers and inspired major developments in theodicy, kickstarting the religious reforms that would bring about the birth of modern Vayonism. The eruption caused a volcanic winter that lowered global temperatures for at least the following decade, bringing about crop failures which directly caused the Grothic Migration of the following century.
Nature of the event
Reconstructions of the eruption and earthquake and their effects vary considerably in the details but have the same overall features. The eruption lasted for two days. The morning of the first day saw early, smaller fissures and releases of ash and smoke on the mountain, though how much alarm this may have caused varies depending on the source.
Around 2:00 a.m. of the second day, the Peak of Winds violently erupted, spewing forth a deadly column of super-heated tephra and gases to an estimated height of 40 km and ejecting molten rock, pumice and volcanic ash at 2 million tons per second. This was also the start of intense seismic activity throughout the entire eastern Elyrian basin.
Elyria, as well as several adjoining areas, was quickly obliterated and buried underneath massive pyroclastic surges and ashfall deposits. The soft, marshy ground of the city opened up in great fissures and sunk into itself. Sources place the receding of the sea just moments after, exposing coastal sandbanks littered with lost cargo and shipwrecks that crowds quickly flocked to. Half an hour later, a wall of water an estimated 40 meters tall swept through the sandbanks and coastal areas, penetrating over 1 km inward in some places.
Estimates place the earthquake's magnitude in the range of 9.0–10.0 and the volcanic eruption with a VEI of 7.