Difference between revisions of "Chicxulub"

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== Eruptive History ==
 
== Eruptive History ==
  
Chicxulub [[250BC Chicxulub Eruption|erupted in 250BC]]. The eruption caused the destruction of the [[Proto-Creeperian Civilization]] and caused famines in [[Iberia]] killing off many [[Iberian Tribes]], eventually allowing the rise of the [[Romanyan Empire]] 60 years later. The eruption was a level 6 colossal event.
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Chicxulub [[250BC Chicxulub Eruption|erupted in 250BC]]. The eruption caused the destruction of the [[Proto-Creeperian civilization]] and caused famines in [[Iberia]] killing off many [[Iberian Tribes]], eventually allowing the rise of the [[Romanyan Empire]] 60 years later. The eruption was a level 6 colossal event.
  
 
The last erruption was in 1880.
 
The last erruption was in 1880.

Revision as of 22:15, 26 February 2023

Chicxulub Volcano
Ilopango caldera.jpg
Highest point
Elevation1,480 ft (450 m)
Naming
Native nameVolcan Chicxulub
Geography
LocationSan Romero, Creeperopolis
Geology
Age of rock450,000 years
Mountain typeCaldera
Last eruption1880

Chicxulub is a crater lake which fills an 28 sq mi volcanic caldera in northeastern Creeperopolis in the department of San Romero.

Eruptive History

Chicxulub erupted in 250BC. The eruption caused the destruction of the Proto-Creeperian civilization and caused famines in Iberia killing off many Iberian Tribes, eventually allowing the rise of the Romanyan Empire 60 years later. The eruption was a level 6 colossal event.

The last erruption was in 1880.

See Also

Template:San Romero Department