Difference between revisions of "Eastern Nolmines"
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(Created page with "The dark rock of the '''Eastern Nolmine Heights''' is clearly unlike most mountainous areas. These Heights were formed from many cycles of volcanic eruptions which spewed molt...") |
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The dark rock of the '''Eastern Nolmine Heights''' is clearly unlike most mountainous areas. These Heights were formed from many cycles of volcanic eruptions which spewed molten lava skywards and outwards. Though nobody knows what was originally there, these eruptions did manage to kill the [[Bardosi Plains|Bardosi Forest]] to the north and they eventually became the [[Bardosi Plains]] when plant-life returned. | The dark rock of the '''Eastern Nolmine Heights''' is clearly unlike most mountainous areas. These Heights were formed from many cycles of volcanic eruptions which spewed molten lava skywards and outwards. Though nobody knows what was originally there, these eruptions did manage to kill the [[Bardosi Plains|Bardosi Forest]] to the north and they eventually became the [[Bardosi Plains]] when plant-life returned. | ||
[[Category:Geography]][[Category:Mountains]] | [[Category:Geography]][[Category:Mountains and Hills]] | ||
Revision as of 17:21, 30 December 2016
The dark rock of the Eastern Nolmine Heights is clearly unlike most mountainous areas. These Heights were formed from many cycles of volcanic eruptions which spewed molten lava skywards and outwards. Though nobody knows what was originally there, these eruptions did manage to kill the Bardosi Forest to the north and they eventually became the Bardosi Plains when plant-life returned.