Difference between revisions of "Balürtö Typë"
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;Other Names:Balürö Typë; ''Blue Peak'' | ;Other Names:Balürö Typë; ''Blue Peak'' | ||
;Type:Strato Volcano | ;Type:Strato Volcano | ||
:Balürö Typë is a large strato volcano The original peak had collapsed many thousands of years in the past, but a secondary cinder cone has since developed into a central island of a great caldera lake. This central cone last erupted in | :Balürö Typë is a large strato volcano The original peak had collapsed many thousands of years in the past, but a secondary cinder cone has since developed into a central island of a great caldera lake. This central cone last erupted in 382 YG, for a period of 17 months. | ||
:The local region is riddled with ancient lava vents, domes, and tubes forming a vast subterranean network of rivers and caves, | :The local region is riddled with ancient lava vents, domes, and tubes forming a vast subterranean network of rivers and caves, | ||
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==History== | ==History== | ||
:The lake is warmed from the volcano and supports a variety of aquatic life, and flora which is atypical for the otherwise chilly climate in this part of the mountains. | :The lake is warmed from the volcano and supports a variety of aquatic life, and flora which is atypical for the otherwise chilly climate in this part of the mountains. | ||
:Several colonies of [[Etausi (people)#Etausi-Daut|Etausi Daut]] | :Several colonies of [[Etausi (people)#Etausi-Daut|Etausi Daut]] have settled in the interior of the ancient caldera, and the surrounding caves. They compete with several large warrens of [[Pëlöryk (people)|Pëlöryk]] for food and other resources. | ||
==Stories== | ==Stories== | ||
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[[Category:Geographic Feature]] | [[Category:Geographic Feature]] | ||
[[Category:Lake]] | |||
[[Category:Mountain]] | |||
[[Category:Volcano]] | [[Category:Volcano]] |
Latest revision as of 16:54, 17 August 2022
About
- Name
- Other Names
- Balürö Typë; Blue Peak
- Type
- Strato Volcano
- Balürö Typë is a large strato volcano The original peak had collapsed many thousands of years in the past, but a secondary cinder cone has since developed into a central island of a great caldera lake. This central cone last erupted in 382 YG, for a period of 17 months.
- The local region is riddled with ancient lava vents, domes, and tubes forming a vast subterranean network of rivers and caves,
Location
- Kythus
- This volcano is located in the Darlom Mountains in Northern Kythus.
History
- The lake is warmed from the volcano and supports a variety of aquatic life, and flora which is atypical for the otherwise chilly climate in this part of the mountains.
- Several colonies of Etausi Daut have settled in the interior of the ancient caldera, and the surrounding caves. They compete with several large warrens of Pëlöryk for food and other resources.