What Is the Pacific Ring of Fire? - podcast episode cover

What Is the Pacific Ring of Fire?

Sep 05, 20248 min
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Episode description

The Ring of Fire is a loop around the Pacific Ocean that's a literal hotbed of volcanoes, earthquakes, hydrothermal vents, and other geologic activity. Learn how the interactions among tectonic plates cause all this mayhem in today's episode of BrainStuff, based on this article: https://science.howstuffworks.com/environmental/earth/geology/ring-of-fire.htm

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Speaker 1

Welcome to Brainstuff, a production of iHeartRadio. Hey Brainstuff, Lauren Vogelbaum. Here. When the explorer Ferdinand Magellan visited Earth's biggest ocean in fifteen twenty, he found the waters pleasantly calm, and that's why to this day we call it the Pacific Ocean, a pacific meaning peaceful, which is ironic considering that there's a vast loop of volcanoes and seismic activity running through

and around the Pacific Ocean. This is the infamous Ring of Fire, a perimeter some twenty five thousand miles long. That's forty thousand kilometers where most of the world's earthquakes and volcanic vents take place. Today, let's talk about how it works. Spoiler alert, it's got nothing to do with

the love song made popular by Johnny Cash. Unfortunately. The Ring of Fire hugs the western coast of South, Central and North America, spans Alaska's Aleutian Island Arc through Rushes cam Chocup Peninsula, then shoots down through Japan, the Philippines, Indonesia, pap New Guinea, and New Zealand. The ring completes itself by going through northwestern Antarctica, which has a number of volcanoes. All of these areas touch on the Pacific tectonic Plate

and a few smaller plates that brush up against it. Okay, you and I live on top of the Earth's lithosphere, our home world's rocky exterior crust. But this layer isn't some rigid, single piece shell. Instead, it's made up of about fifteen to twenty tectonic plates depending on who you ask, that fit together pretty snugly and slowly drift over the molten materials that lay deeper inside our planet. A heat from the Earth's core causes them to move against one another.

Boundaries between these plates come in three major categories, convergent, divergent, and transform, and the Ring of Fire includes examples of each one. Let's start with divergent boundaries. These occur when two neighboring plates move away from one another. In those areas, molten magma rises up from beneath the plates and eventually hardens to create new crust. Under the Pacific Ocean, the huge Pacific Plate is being pushed away from four of

its smaller counterparts by the powerful East Pacific Rise. This is a strip of heavy activity that parallels the coast of South America a couple thousand miles out, stretching from the Gulf of California down through Easter Island, approaching Antarctica and New Zealand. Around Easter Island, which is offshore of Chile, we see the fastest expansion of the Earth's crust in the world, over six inches a year, or about one

hundred and fifty millimeters. Divergent boundaries also create hydrothermal vents deep in the ocean that spew material and heat into the water, and researchers have found fascinating ecosystems there that, unlike any other ecosystem on Earth, doesn't have photosynthesis as its base. These creatures live off the vents independent of the Sun's energy. Next, let's talk about transform boundaries, areas where two plates sideswipe each other up. In California proper,

we have the San Andreas Fault. That's a classic transform boundary. The state of California is straddled across the Pacific Plate and the North American Plate. The North American Plate is headed south, the Pacific is moving north. A friction between them causes the earthquakes that California is infamous for. But what happens when plates collide head on. That's a convergent boundary wherein one plate will be driven underneath the other.

This point of contact is called a subduction zone. The Pacific Plate has a subduct zone at its northwestern rim, along its boundary with the Philippine Sea Plate, which is riding up over the Pacific Plate. This interaction caused part of the Philippine Plate to break off millions of years ago, forming a tiny plate in between called the Mariana which

is also riding over the Pacific Plate. These interactions forged the Mariana Islands, one thousand miles east of the Philippine Archipelago and created the yawning underwater chasm called the Mariana Trench, which contains the deepest point of any ocean on Earth. Its floor, named the Challenger Deep, lies some thirty six thousand feet below sea level. That's around eleven thousand meters.

For contrast, the peak of Mount Everest is only twenty nine thousand feet above sea level or nine thousand meters, which means the Mariana Trench is significantly deeper than Everest is tall. Around this and other subduction zones, researchers are investigating reservoirs of hot water moving up from the ocean floor as a potential source of geothermal energy. Solar and wind power grab more headlines, but engineers are also working

on harnessing these underwater geothermal sources of cleaner energy. Meanwhile, across the ocean, between the southeast part of the Pacific Plate and the South American Continental Plate, there's a smaller oceanic plate called the Nasca. At this very moment, the Nasca Plate is being driven underneath the South American Plate. The convergence process sets off a lot of earthquakes in western South America. It's also uplifting mountains and sending up

magma to feed volcanoes. There are some four hundred and fifty two volcanoes, both active and dormant, spread out across throwing a fire, including plenty of vents and fissures that arept underwater. As far as we know, these account for seventy five percent of all volcanic activity in the world. The area also accounts for around ninety percent of the

planet's earthquakes. Some of the worst natural disasters in recorded history, like the eighteen eighty three Krakatoa eruption, the nineteen sixty Chile earthquake and the two thousand and four Indian Ocean tsunami had their origins along the Ring of Fires tectonic boundaries. However, there are so many small plates and different interaction zones involved in the Ring that any disasters that happen on

opposite sides of it are just coincidence. A case in point, a series of earthquakes rocked Japan's Kshu Island in April of twenty sixteen. That same month, Chile suffered a quake with a Richter scale magnitude of seven point two. The epicenters were almost ten thousand miles apart for sixteen thousand kilometers. Although a strong earthquake can trigger weaker ones in nearby places, the gap between Chile and Japan is far too big

for the ethquakes to be linked. After all, the Pacific is the world's largest ocean, though it may not always retain that title do in no small part to all the subduction zones on its flanks. The Pacific might close within the next two hundred and fifty million years. As Asia, Australia, and the Americas converge. Planet Earth may wind up with a new super continent not too dissimilar from the giant land mass called Pangaea that started breaking apart around two

hundred million years ago. But that's just one hypothesis. Some geologists think that the Atlantic or the Arctic oceans are more likely to disappear than the Pacific. We'll all just have to wait and find out. Today's episode is based on the article seven hot facts about the Pacific Ring of Fire on HowStuffWorks dot com, written by Mark Mancini.

Brain Stuff is production by Heart Radio in partnership with hostiff works dot Com and is produced by Tyler Klang and Ramsey young A. Four more podcasts from my heart Radio. Visit the iHeartRadio app, Apple Podcasts, or wherever you listen to your favorite shows. M

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