Smith Volcano

Smith Volcano, also known as Mount Babuyan, is a cinder cone on Babuyan Island, the northernmost of the Babuyan group of islands on Luzon Strait, north of the main island of Luzon in the Philippines. The mountain is one of the active volcanoes in the Philippines, which last erupted in 1924.

Smith Volcano
Mount Babuyan
Aerial view of Smith Volcano (foreground) on the western part of Babuyan Island with Babuyan Claro in the background
Highest point
Elevation688 m (2,257 ft)[1]
Coordinates19°32′11.84″N 121°54′46.24″E
Geography
Smith Volcano
Location within the Philippines
LocationBabuyan Islands
CountryPhilippines
RegionCagayan Valley
ProvinceCagayan
MunicipalityCalayan
Geology
Mountain typeStratovolcano
Volcanic arcBabuyan (Bashi) Segment of Luzon-Taiwan Arc
Last eruption1924

The volcano is politically located in the Municipality of Calayan, Cagayan province, the town that has jurisdiction over the Babuyan Islands except Fuga Island.

Physical features

The sparsely-vegetated cinder cone is 688 meters (2,257 ft) high with a base diameter of 4.5 kilometers (2.8 mi).[1] Layers of basaltic lava flows are evident south of the volcano.[1][2]

Smith Volcano is one of the probably five Pleistocene-to-Holocene volcanic centers on Babuyan Island (also known as Babuyan de Claro Island) with Smith, the youngest volcano on the island. The largest on the island is Babuyan Claro (also known as Mt. Pangasun), an active stratovolcano with two well-preserved summit craters 300 and 400 m (980 and 1,310 ft) in diameter, located in the center of the island.[2] Babuyan Claro is about 4.3 kilometers (2.7 mi) peak-to-peak southeast of Smith Volcano, which is the north-westernmost summit on the triangular-shaped island.[3]

Eruptions

Smith Volcano has erupted six times, the last of which was in 1924.[3]

Emergency investigation of 1993

A team of volcanologists from the Philippine Institute of Volcanology and Seismology (PHIVOLCS) Quick Response Team conducted an investigation on July 8, 1993 following reports of unusual volcanic activity at Babuyan Island. Results of the survey showed that Smith Volcano was quiet with no volcanic earthquakes recorded during the survey.

gollark: So basically, the "god must exist because the universe is complex" thing ignores the fact that it... isn't really... and that gods would be pretty complex too, and does not answer any questions usefully because it just pushes off the question of why things exist to why *god* exists.
gollark: To randomly interject very late, I don't agree with your reasoning here. As far as physicists can tell, while pretty complex and hard for humans to understand, relative to some other things the universe runs on simple rules - you can probably describe the way it works in maybe a book's worth of material assuming quite a lot of mathematical background. Which is less than you might need for, say, a particularly complex modern computer system. You know what else is quite complex? Gods. They are generally portrayed as acting fairly similarly to humans (humans like modelling other things as basically-humans and writing human-centric stories), and even apart from that are clearly meant to be intelligent agents of some kind. Both of those are complicated - the human genome is something like 6GB, a good deal of which probably codes for brain things. As for other intelligent things, despite having tons of data once trained, modern machine learning things are admittedly not very complex to *describe*, but nobody knows what an architecture for general intelligence would look like.
gollark: https://media.discordapp.net/attachments/348702212110680064/896356765267025940/FB_IMG_1633757163544.jpg
gollark: https://isotropic.org/papers/chicken.pdf
gollark: Frankly, go emit muon neutrinos.

See also

References

  1. "Smith Volcano". Philippine Institute of Volcanology and Seismology (PHIVOLCS). Retrieved on December 26, 2013.
  2. "Smith Volcano, Cagayan, Cagayan Valley, Philippines". Google Map. Retrieved on December 26, 2013.
  3. "Babuyan Claro – Background". Global Volcanism Program. Smithsonian Institution. Retrieved December 26, 2013.
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