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SciShow, "The Deep Sea Sub Built By a Cereal Company.", November 13, 2026, YouTube, 12:11, https://youtube.com/watch?v=S7ELHbvqaeA. |
The Alvin submersible revolutionized deep-sea exploration in 1964, and it's still being used today. But it wasn't made by a traditional submarine builder or defense contractor. It was built by General Mills.
Hosted by: Denali Kincaid (they/them)
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Sources: https://docs.google.com/document/u/1/d/e/2PACX-1vTjNl5Jpd_uFsM_0NAGwZwdgRZ7xeuMLBbW7lex1oIneDDC9b2m5OgvAuytMUU5kmgI2olyhOn43A21/pub
Hosted by: Denali Kincaid (they/them)
This premiere is part of Learn-a-Thon, an annual celebration of Complexly's mission to create trustworthy stuff that inspires curiosity and lowers barriers to knowledge-building. Check out our other events happening Nov 9th-20th here: https://youtube.com/playlist?list=PLaiLa8UfepUw&si=7U7VZmeFmRnfqn2Q
Every donation of every size supercharges our impact. Visit https://Complexly.org/Learnathon to make a tax-deductible donation now!
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Support us for $8/month on Patreon and keep SciShow going!
https://www.patreon.com/scishow
Or support us directly: https://complexly.com/support
Join our SciShow email list to get the latest news and highlights:
https://mailchi.mp/scishow/email
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Huge thanks go to the following Patreon supporters for helping us keep SciShow free for everyone forever: ., Adam Brainard, Alex Hackman, Bethany Matthews, Blood Doctor Kelly, Cye Stoner, Anita, Anne Herrington, Friso, Jeremy Mattern, Garrett Galloway, Chris Curry, Chris Mackey, Chris Peters, David Johnston, Eric Jensen, J.V. Rosenbalm, Jaap Westera, Jacob Puthoff, Jason A Saslow, Jon Coffman, Joseph Ruf, Jp Lynch, Kevin Bealer, Kevin Knupp, Lyndsay Brown, Matt Curls, Piya Shedden, Shaji John, Steve Gums, Timos Gies, Toyas Dhake, yeyette
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Looking for SciShow elsewhere on the internet?
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Sources: https://docs.google.com/document/u/1/d/e/2PACX-1vTjNl5Jpd_uFsM_0NAGwZwdgRZ7xeuMLBbW7lex1oIneDDC9b2m5OgvAuytMUU5kmgI2olyhOn43A21/pub
This is Alvin.
Alvin is a quirky deep-sea submersible that changed marine science forever. Alvin was the first sub that allowed scientists to both see AND sample the ocean floor.
Alvin is so iconic that even today, more than 60 years later, it’s STILL being used to explore the bottom of the ocean. The way Alvin came to be, though, isn’t what you’d expect. It wasn’t built by a traditional submarine producer like General Dynamics Corporation.
And it wasn’t built by some massive aerospace company like Boeing, either. It also wasn’t built by a defense contractor like Lockheed Martin. Instead, Alvin was built by General Mills.
That’s right. The Wheaties company. [♪ INTRO] Humans have been on Earth for at least 300,000 years. And for pretty much that entire time, we’ve been trying to explore one of the greatest wonders of our planet: the ocean.
But exploring the deep-sea has proven to be a lot more complicated than we thought. Most of our historic exploration has been limited to the ocean’s surface. But we’re a pretty stubborn species, so we invented diving bells … basically open bottomed, bell-shaped contraptions that trap an air pocket inside it for people to breathe.
Diving bells allowed humans to get deeper than they ever could on their own, but they couldn’t get THAT deep still. So, we invented submarines and submersibles. Submarines can operate independently, while submersibles usually rely on another vessel to shuttle them around and act as a home base essentially.
Modern subs came around in the 1920s, with better materials for handling deep ocean pressures. These could get us to the seafloor independently, but they had a major limitation, which is they usually had no windows, and they couldn’t collect or sample anything. So starting in the 40s and 50s, we put windows in something called the bathyscape.
It could survive the pressures of the deep ocean, and you could actually see the ocean while you were down there. But again, it had one major flaw: We could only look, we couldn’t really sample much from it. That’s because sampling arms would have created a weak point in the hull.
A geophysicist named Allyn Vine was working at Woods Hole Oceanographic Institution or WHOI at the time. And he thought there had to be a way to do both. He wanted to build the world's first deep-diving submersible that could see AND sample the seafloor.
So in 1962, he convinced the leaders at WHOI to call for bids to do that. Any company that believed it was capable of designing and building a deep sea sub could apply. And there were two final contenders … one was aerospace manufacturer North American Aviation, and the other was none other than General Mills.
Today, we know General Mills as a cereal company. They make Cheerios, Wheaties, and most importantly, Lucky Charms. But they’ve been around since 1866, and they’ve actually dabbled in a lot of different products during that time.
They’ve made clothing, toys, and boardgames. They even helped create early versions of the recording black boxes that are used in airplanes. So it actually wasn’t THAT crazy for them to show interest in a side project like building a deep sea submersible.
When the bid from General Mills came in at almost $100,000 lower than its rival, they were given the contract. A cereal company was about to build the first ever manned submersible for scientific research. They decided to name it Alvin, in honor of Allyn Vine.
Work on the submersible began in the same room as the equipment that made the cereal. The original design looked something like this. And you can see that compared to the sleek military subs people were used to seeing, Alvin is a bit… tubby.
But there were very good reasons for its shape. Inside the sub’s frame, there was a set of batteries, a buoyancy sphere and variable ballast that enabled the sub’s vertical movement in the water column. Outside the frame, there was a rear propeller and rudder for steering, the lift propeller, light and sonar equipment, and a robotic arm for sampling.
But the most important design element was a new feature to address the crushing pressure of the ocean. The best demonstration I can give for exactly how much pressure we're talking about is this. This is a styrofoam cup, or at least it was before the ocean shrunk it.
It’s a tradition in deep sea science to decorate styrofoam cups and tie them to the outside of a sub before an adventure to the ocean floor. So the pressure of the deep sea inevitably shrinks the cup. It’s kind of like an ocean shrinky-dink!
To deal with all that pressure and still give scientists a view of the ocean floor, Alvin designers added a personnel sphere made of titanium. The reason a sphere works so well is that it’s one of the most pressure-resistant shapes. The compression is evenly distributed across its entire surface, which prevents weak points in the sub.
Titanium is also considered the best material to withstand deep-sea pressures. Its high strength-to-weight ratio is better than steel’s, and it has equal strength in every direction. This makes it even more resistant to compressive forces than materials like carbon fiber.
When Alvin was completed in 1964, it was an engineering marvel. And it wasn’t long before it was being used to make all kinds of amazing deep sea discoveries. Arguably the biggest discovery was in 1977, when a group of geologists were studying a location called the Galapagos Rift.
They towed a camera behind their ship and caught a glimpse of something shimmering in the water. Previous research had suggested that there might be hydrothermal vents here. Those are places where circulating seawater water is superheated by magma in the Earth's crust before returning up to the seafloor through deep sea vents.
They sent Alvin down to investigate whether this was true, and what they found had never been seen anywhere else on Earth. Huge. Colonies.
Of life. More than 2500m deep in the ocean. Giant Mussels.
Species of crabs and deep sea octopus completely unknown to science at the time. And huge stalk-like tube worms that were bigger than anything known to marine biologists before. There were small spherical animals they called “dandelions" that used web-like fibers to sit above the ocean floor and feed.
And all these images are the original photos taken from that first dive to the vents. It was an incredible discovery. But there was one problem.
They were geologists, so they hadn’t brought any equipment to store biological specimens in! In fact, there wasn’t a single biologist on board. One of the greatest discoveries in modern history, and it was a bunch of rock people who found it.
Since they didn’t have any formaldehyde to preserve the biological specimens, they did exactly what you’d expect a bunch of geologists in the 70s to do. They stored the specimens in the Vodka that they had brought with them. The smell of the water they brought up from the vents provided a clue as to how these creatures could survive in the darkness of the deep ocean.
It didn’t smell like normal seawater. It smelled like rotten eggs. That smell was hydrogen sulfide coming out of the vents.
It had been feeding bacteria, and an entire ecosystem had developed around it. An ecosystem almost completely dependent on life without any photosynthesis. Alvin played a huge role in revealing how these vents form from volcanism at mid-ocean ridges.
Mid-ocean ridges are a place on the earth's surface where two tectonic plates are moving away from each other. Magma, which becomes lava at the surface, comes up between these two plates. It's a 65,000 km long chain of underwater volcanoes running across the entire planet. 70% of Earth’s surface, almost our entire ocean floor, is formed by volcanism at mid ocean ridges.
And when eruptions happen underwater, the lava hardens into all kinds of weird shapes. You get lava flows that look like pillows, folded curtains, and lavas that look essentially like its been hacked into pieces. Being a very creative bunch, marine geologists have named them pillow flows, curtain folded flows, and hackly flows.
You can even get whirlpool-shaped rock on the ocean floor made by tiny lava whirlpools. If you’re wondering why everything in these photos has a faint shine to it, that’s because the top layer of the lava crust is a kind of volcanic glass called mid ocean ridge basalt, or MORB. That’s right: A lot of the ocean floor is covered in glass.
Even though MORB glass is incredibly common, few people have heard of it because it’s all at the bottom of the ocean. Some of my favorite features that Alvin has explored along mid-ocean ridges are lava drips and lava pillars. Lava drips form when water gets trapped in the molten rock and is vaporized by the heat.
This hot steam in the now solid lava crust actually re-melts the underside of that crust and causes it to drop through the vapor. And then these are Lava Pillars. From a distance they almost look like ancient ruins, but these aren’t man made … they’re volcano made.
They form when the trapped seawater can't vaporize. It wants to escape from the lava, but the lava heats it up and causes the water to geyser up and out of the lava itself. As it does, it rapidly cools the lava all around it into what looks like a straw made of volcanic rock.
As the lava slowly drains out of this area and leaves a hollowed out lava crust behind, it leaves rings like water might leave on your bath tub. These rings are prized by scientists who use them to study how the chemical makeup of the lava changes throughout an eruption. Countless other discoveries have also been made from Alvin.
In 1986, it dove to the site of the Titanic shipwreck to investigate the debris field. In 2010, it explored the site of the Deepwater Horizon Oil spill to study the impacts that had on marine life. Alvin even worked with the US Navy to recover a lost Hydrogen bomb at the bottom of the sea.
Since its launch, Alvin has taken more than 14,000 scientists and pilots to the ocean floor. I got to be one of them during the first year of my PhD! In fact, this shrunken cup I showed you earlier is the one I made to commemorate my first Alvin dive.
I dove on Alvin Dive 5245 to a depth of 2,565 m at my favorite mid ocean ridge, the East Pacific Rise. I traveled with an incredible research team in 2024 for what we called the lava watch cruise. We were looking for signs of a new volcanic eruption on the ocean floor.
We didn’t find any, but we did discover five new hydrothermal vents and the cooled remains of a giant underwater lava lake I’m currently attempting to write a paper on. The eruption we were looking for did eventually happen a year later, though. And it was captured on camera by, you guessed it, the Alvin submersible.
Alvin has had a lot of upgrades over the years, but ultimately, it’s still the same quirky sub from all those years ago. It has bigger windows, and it can now go down to 6,500 m deep, reaching 99% of the ocean floor. It probably won't happen in my lifetime, but with vehicles like Alvin, I can’t help but believe it’s only a matter of time before we’ve finally seen all of it. [♪ OUTRO]
Alvin is a quirky deep-sea submersible that changed marine science forever. Alvin was the first sub that allowed scientists to both see AND sample the ocean floor.
Alvin is so iconic that even today, more than 60 years later, it’s STILL being used to explore the bottom of the ocean. The way Alvin came to be, though, isn’t what you’d expect. It wasn’t built by a traditional submarine producer like General Dynamics Corporation.
And it wasn’t built by some massive aerospace company like Boeing, either. It also wasn’t built by a defense contractor like Lockheed Martin. Instead, Alvin was built by General Mills.
That’s right. The Wheaties company. [♪ INTRO] Humans have been on Earth for at least 300,000 years. And for pretty much that entire time, we’ve been trying to explore one of the greatest wonders of our planet: the ocean.
But exploring the deep-sea has proven to be a lot more complicated than we thought. Most of our historic exploration has been limited to the ocean’s surface. But we’re a pretty stubborn species, so we invented diving bells … basically open bottomed, bell-shaped contraptions that trap an air pocket inside it for people to breathe.
Diving bells allowed humans to get deeper than they ever could on their own, but they couldn’t get THAT deep still. So, we invented submarines and submersibles. Submarines can operate independently, while submersibles usually rely on another vessel to shuttle them around and act as a home base essentially.
Modern subs came around in the 1920s, with better materials for handling deep ocean pressures. These could get us to the seafloor independently, but they had a major limitation, which is they usually had no windows, and they couldn’t collect or sample anything. So starting in the 40s and 50s, we put windows in something called the bathyscape.
It could survive the pressures of the deep ocean, and you could actually see the ocean while you were down there. But again, it had one major flaw: We could only look, we couldn’t really sample much from it. That’s because sampling arms would have created a weak point in the hull.
A geophysicist named Allyn Vine was working at Woods Hole Oceanographic Institution or WHOI at the time. And he thought there had to be a way to do both. He wanted to build the world's first deep-diving submersible that could see AND sample the seafloor.
So in 1962, he convinced the leaders at WHOI to call for bids to do that. Any company that believed it was capable of designing and building a deep sea sub could apply. And there were two final contenders … one was aerospace manufacturer North American Aviation, and the other was none other than General Mills.
Today, we know General Mills as a cereal company. They make Cheerios, Wheaties, and most importantly, Lucky Charms. But they’ve been around since 1866, and they’ve actually dabbled in a lot of different products during that time.
They’ve made clothing, toys, and boardgames. They even helped create early versions of the recording black boxes that are used in airplanes. So it actually wasn’t THAT crazy for them to show interest in a side project like building a deep sea submersible.
When the bid from General Mills came in at almost $100,000 lower than its rival, they were given the contract. A cereal company was about to build the first ever manned submersible for scientific research. They decided to name it Alvin, in honor of Allyn Vine.
Work on the submersible began in the same room as the equipment that made the cereal. The original design looked something like this. And you can see that compared to the sleek military subs people were used to seeing, Alvin is a bit… tubby.
But there were very good reasons for its shape. Inside the sub’s frame, there was a set of batteries, a buoyancy sphere and variable ballast that enabled the sub’s vertical movement in the water column. Outside the frame, there was a rear propeller and rudder for steering, the lift propeller, light and sonar equipment, and a robotic arm for sampling.
But the most important design element was a new feature to address the crushing pressure of the ocean. The best demonstration I can give for exactly how much pressure we're talking about is this. This is a styrofoam cup, or at least it was before the ocean shrunk it.
It’s a tradition in deep sea science to decorate styrofoam cups and tie them to the outside of a sub before an adventure to the ocean floor. So the pressure of the deep sea inevitably shrinks the cup. It’s kind of like an ocean shrinky-dink!
To deal with all that pressure and still give scientists a view of the ocean floor, Alvin designers added a personnel sphere made of titanium. The reason a sphere works so well is that it’s one of the most pressure-resistant shapes. The compression is evenly distributed across its entire surface, which prevents weak points in the sub.
Titanium is also considered the best material to withstand deep-sea pressures. Its high strength-to-weight ratio is better than steel’s, and it has equal strength in every direction. This makes it even more resistant to compressive forces than materials like carbon fiber.
When Alvin was completed in 1964, it was an engineering marvel. And it wasn’t long before it was being used to make all kinds of amazing deep sea discoveries. Arguably the biggest discovery was in 1977, when a group of geologists were studying a location called the Galapagos Rift.
They towed a camera behind their ship and caught a glimpse of something shimmering in the water. Previous research had suggested that there might be hydrothermal vents here. Those are places where circulating seawater water is superheated by magma in the Earth's crust before returning up to the seafloor through deep sea vents.
They sent Alvin down to investigate whether this was true, and what they found had never been seen anywhere else on Earth. Huge. Colonies.
Of life. More than 2500m deep in the ocean. Giant Mussels.
Species of crabs and deep sea octopus completely unknown to science at the time. And huge stalk-like tube worms that were bigger than anything known to marine biologists before. There were small spherical animals they called “dandelions" that used web-like fibers to sit above the ocean floor and feed.
And all these images are the original photos taken from that first dive to the vents. It was an incredible discovery. But there was one problem.
They were geologists, so they hadn’t brought any equipment to store biological specimens in! In fact, there wasn’t a single biologist on board. One of the greatest discoveries in modern history, and it was a bunch of rock people who found it.
Since they didn’t have any formaldehyde to preserve the biological specimens, they did exactly what you’d expect a bunch of geologists in the 70s to do. They stored the specimens in the Vodka that they had brought with them. The smell of the water they brought up from the vents provided a clue as to how these creatures could survive in the darkness of the deep ocean.
It didn’t smell like normal seawater. It smelled like rotten eggs. That smell was hydrogen sulfide coming out of the vents.
It had been feeding bacteria, and an entire ecosystem had developed around it. An ecosystem almost completely dependent on life without any photosynthesis. Alvin played a huge role in revealing how these vents form from volcanism at mid-ocean ridges.
Mid-ocean ridges are a place on the earth's surface where two tectonic plates are moving away from each other. Magma, which becomes lava at the surface, comes up between these two plates. It's a 65,000 km long chain of underwater volcanoes running across the entire planet. 70% of Earth’s surface, almost our entire ocean floor, is formed by volcanism at mid ocean ridges.
And when eruptions happen underwater, the lava hardens into all kinds of weird shapes. You get lava flows that look like pillows, folded curtains, and lavas that look essentially like its been hacked into pieces. Being a very creative bunch, marine geologists have named them pillow flows, curtain folded flows, and hackly flows.
You can even get whirlpool-shaped rock on the ocean floor made by tiny lava whirlpools. If you’re wondering why everything in these photos has a faint shine to it, that’s because the top layer of the lava crust is a kind of volcanic glass called mid ocean ridge basalt, or MORB. That’s right: A lot of the ocean floor is covered in glass.
Even though MORB glass is incredibly common, few people have heard of it because it’s all at the bottom of the ocean. Some of my favorite features that Alvin has explored along mid-ocean ridges are lava drips and lava pillars. Lava drips form when water gets trapped in the molten rock and is vaporized by the heat.
This hot steam in the now solid lava crust actually re-melts the underside of that crust and causes it to drop through the vapor. And then these are Lava Pillars. From a distance they almost look like ancient ruins, but these aren’t man made … they’re volcano made.
They form when the trapped seawater can't vaporize. It wants to escape from the lava, but the lava heats it up and causes the water to geyser up and out of the lava itself. As it does, it rapidly cools the lava all around it into what looks like a straw made of volcanic rock.
As the lava slowly drains out of this area and leaves a hollowed out lava crust behind, it leaves rings like water might leave on your bath tub. These rings are prized by scientists who use them to study how the chemical makeup of the lava changes throughout an eruption. Countless other discoveries have also been made from Alvin.
In 1986, it dove to the site of the Titanic shipwreck to investigate the debris field. In 2010, it explored the site of the Deepwater Horizon Oil spill to study the impacts that had on marine life. Alvin even worked with the US Navy to recover a lost Hydrogen bomb at the bottom of the sea.
Since its launch, Alvin has taken more than 14,000 scientists and pilots to the ocean floor. I got to be one of them during the first year of my PhD! In fact, this shrunken cup I showed you earlier is the one I made to commemorate my first Alvin dive.
I dove on Alvin Dive 5245 to a depth of 2,565 m at my favorite mid ocean ridge, the East Pacific Rise. I traveled with an incredible research team in 2024 for what we called the lava watch cruise. We were looking for signs of a new volcanic eruption on the ocean floor.
We didn’t find any, but we did discover five new hydrothermal vents and the cooled remains of a giant underwater lava lake I’m currently attempting to write a paper on. The eruption we were looking for did eventually happen a year later, though. And it was captured on camera by, you guessed it, the Alvin submersible.
Alvin has had a lot of upgrades over the years, but ultimately, it’s still the same quirky sub from all those years ago. It has bigger windows, and it can now go down to 6,500 m deep, reaching 99% of the ocean floor. It probably won't happen in my lifetime, but with vehicles like Alvin, I can’t help but believe it’s only a matter of time before we’ve finally seen all of it. [♪ OUTRO]







