An Interview with Kilauea Volcano
2018 marked the largest volcanic eruption Kilauea volcano has seen this century. Two lava lakes suddenly drained, explosions rocked the summit crater, earthquakes rattled Hawaii island, and a massive fissure eruption took place in Puna. Rivers of lava flooded the landscape and poured into the ocean in a 2 mile wide ocean entry. The fissure eruption finally ended in August, closing out a 35 year eruption on Kilauea volcano.
On the one year anniversary of the fissure eruptions, I thought it would be interesting to sit down with Kilauea volcano herself and get her perspective on life as a volcano, the eruption, and what she has up her sleeve next.
Happy International Day of Volcanoes!
Happy International Day of Volcanoes!
So, if we’re getting “technical,” April 10 is the UNOFFICIAL International Day of Volcanoes. But that’s not stopping thousands of people around the world from celebrating the wild and wonderful volcanoes that rock our world.
What’s the big deal about volcanoes anyway?
Volcanoes are freaking awesome! And for more reasons than one:
The Moon is Lava!
VITAL STATS
Name: Earth’s Moon
Eruption Status: Dormant?
Last Eruption: Less than 100,000 years ago
Location: 238,900 miles out in space
Do you remember playing “The Floor is Lava” when you were a kid? If not, you should definitely start a game right now. Wherever you are. It’s a blast! But let’s play a different game today…
The Moon is Lava!
It certainly looked as though this might be the case last Sunday evening during the lunar eclipse. The usual pearly glow of the full moon (a super moon in this case) was replaced by a deep red glow as the Earth blocked the sun’s light. Lunar eclipses like this only happen when the Sun, Earth, and Moon are in a straight line. Earth completely blocks the sunlight from the moon, and what light does refract around the Earth’s atmosphere gives the moon a bloody red appearance. Phew! So that’sall it was? Good. But let me tell you a little secret, my friend. The moon IS lava.
Capulin: The Boca Trail
VITAL STATS
Name: Capulin
Type: Cinder Cone
Eruption Status: Extinct
Last Eruption: Approximately 60,000 years ago
Location: 36.7811° N, 103.9695° W
Northeastern New Mexico; Raton-Clayton Volcanic Field
We coasted down the volcano road, enjoying our descent from Capulin’s summit. The clouds had finally lifted and myriad volcanoes now popped up from the dusty New Mexican landscape. My partner in crime and I headed in to the Visitor Center for a quick break and a chat with the friendly and knowledgable park rangers. They offered us great information about how Capulin became a national monument in 1916 and how summit road was covertly created in 1925 so that the first Model T’s could putter to the top. Our ranger friends even were able to answer questions about the volcanism of the area. They confirmed that what we spotted on the lava flow trail earlier in the day was indeed andesite – which gave this volcano its explosive past.
Itching to get back outside and explore the Boca Trail, we drove back to the same parking lot where the Lava Flow trail started. Instead of heading South and sweeping through the volcano’s second lava flow, this trail heads north and winds between the cinder cone and the third lava flow. But here, we found something special. We found the vent from which each of these lava flows emerged.
Capulin: The Summit
VITAL STATS
Name: Capulin
Type: Cinder Cone
Eruption Status: Extinct
Last Eruption: Approximately 60,000 years ago
Location: 36.7811° N, 103.9695° W
Northeastern New Mexico; Raton-Clayton Volcanic Field
The clouds that enshrouded Capulin’s cone finally began to break around mid-morning. We raced to the summit to see what had been hidden behind the thick mist all morning. What we found was breathtaking.
Capulin’s summit crater is perched over 1,300 feet above the surrounding plains, and the drive to reach it is nothing short of intimidating. If you’re not driving, take a peek out the passenger side window. There are no guardrails and the view is straight down. This cone has virtually no slope. Not intimidating…not at all…
Capulin: The Lava Flow Trail
Vital Stats
Name: Capulin
Type: Cinder Cone
Eruption Status: Extinct
Last Eruption: Approximately 60,000 years ago
Location: 36.7811° N, 103.9695° W
Northeastern New Mexico; Raton-Clayton Volcanic Field
Capulin volcano has 4 lava flows – three of which are absolutely massive. They each started from a vent at the base of the volcano, which has left the stunning cone shape intact. As we waited for the clouds at the summit to lift, we decided to take a hop down the Lava Flow Trail.
This trail is a 1 mile loop through the second lava flow. It only scratches the surface; this flow extends over 2 miles down toward Highway 87! We were anxious to get our boots on the ground and go exploring. So off into the silent, misty morning we went.
Capulin Volcano
Vital Stats
Name: Capulin
Type: Cinder Cone
Eruption Status: Extinct
Last Eruption: Approximately 60,000 years ago
Location: 36.7811° N, 103.9695° W
Northeastern New Mexico; Raton-Clayton Volcanic Field
The drive east through Northern New Mexico can be a pretty boring one. The landscape is flat and brown, minus a few hills popping up here and there. Major yawn factor – until you see the unmistakable cone of a volcano standing majestically next to the highway. And then you realize exactly what you’re driving through.
The Raton-Clayton Volcanic Field stretches from southern Colorado to the western border of Oklahoma and Texas, near the town of Clayton, NM. This volcanic field is a bit of an anomoly in the volcano world. Most volcanoes form on hot spots (like Hawaii) or along plate boundaries (Cascade Range). New Mexico doesn’t sit on either one. However, a continental rift does run though the area where the land is pulling apart and much thinner than the surrounding crust. This is what allowed magma to rise to the surface, creating some spectacular volcanic activity.