The Capulin
Volcano was formed in the period of the Raton-Clayton Volcanic field, where the
cone rose to over a thousand feet about the plain, which was aver 8000 feet
about sea level. It is in located in New Mexico, the lava flowed from a single
vent that was created from small fragments that was flung into the air, it
solidified as cinders around the vent. This formed the oval cone that is there
today.
What evidence do
you see regarding the nature of past eruptions?
Evidence of the
other episodes of activity can be seen in nearly 100 nearby volcanic peaks and
lava capped mesas. There Is a series of the extinct volcanic peaks such as the
Sierra Grande and the Johnson Mesa that is west of Capulin.
Was it explosive
or quiescent? Why?
It is stated that
it was a blast that created the Capulin, which form the conical mountain that
cover the vent were the eruption occurred. It is said that the cinder was
ejected during a successive eruption and fell back upon the vent. It also
indicated that Capulin was an ear-shattering explosion.
What kinds of
hazards would be associated with this particular volcano?
The hazards that
was document was wildfires and wildlife that would have inhabited the land at
the time of the eruption. In most recent documentation it speaks of wildfire
and control burn to help the natural fire cycle.
Will it be likely
to erupt again?
It does not seem
that it would erupt in the future as the lava has seemingly move away from the
Capulin as the many other approximately 100 additional peaks that were created
nearby, indicate in my view the movement of the lava keep moving further away.
Note details of
particular interest to you.
Volcanic fields
stretch across New Mexico, yet their cause is not completely understood. Most
volcanic activity in the world occurs at plate boundaries below the earth's
surface, along the Pacific Ring (NPS, 2015).
Reference:
National Parks Service. (2015). Capulin
Volcano, National Monument of New Mexico. Retrieved from: https://www.nps.gov/cavo/learn/nature/volcano-formation.htm
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