Difference between revisions of "Chicxulub"
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(Created page with "{{Infobox mountain | name = Chicxulub Volcano | other_name = | etymology = | native_name = Volcan Chicxulub | native_name_lang = | transl...") |
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== Eruptive History == | == Eruptive History == | ||
− | Chicxulub [[250BC Chicxulub Eruption|erupted in 250BC]]. The eruption caused the destruction of the [[Proto-Creeperian | + | 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 | |
---|---|
Highest point | |
Elevation | 1,480 ft (450 m) |
Naming | |
Native name | Volcan Chicxulub |
Geography | |
Location | San Romero, Creeperopolis |
Geology | |
Age of rock | 450,000 years |
Mountain type | Caldera |
Last eruption | 1880 |
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.