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UPDATE: Jul. 31, 2025, 2:20 p.m. EDT This article has been updated to include the streaming details of “Alien: Earth.”
The best streaming deals to watch the ‘Alien’ franchise:


BEST FOR STUDENTS
Hulu Student
$1.99 per month
(save $8 per month)

BEST FOR T-MOBILE CUSTOMERS
Hulu with ads
Free for one year for T-Mobile users on Go5G Next plan
(save $79.99)

There’s a new addition to the Alien universe and for the first time, it’s in the form of a TV series. Alien: Earth premieres Aug. 8, nearly a year to the day after Alien: Romulus, the latest film in the Alien franchise, hit theaters.
Created by Noah Hawley, the Emmy-winning creator of Fargo and Legion, Alien: Earth is set in 2120, two years before the events of the 1979 original Alien movie. And this time it doesn’t drag us to the deepest reaches of space — it brings extraterrestrial horror to our home planet.
Unlike many other film franchises, all of the Alien films currently live inside one streaming app — from the original to 2024’s Alien: Romulus. As of Aug. 8, that will also include the Alien: Earth series. It’s a modern-day streaming miracle, truly. Here are all the juicy details on how to watch the entire Alien franchise online (and in order).
How many Alien movies are there?
There are seven films in the classic Alien franchise, including the newest release, Alien: Romulus. Prior films include Alien (1979), Aliens (1986), Alien 3 (1992), Alien: Resurrection (1997), Prometheus (2012), and Alien: Covenant (2017). There are also two crossover films to add to your binge if you really want to complete the saga, although no one will blame you if you skip AVP: Alien vs. Predator (2004) and Aliens vs. Predator: Requiem (2007). Then, of course, the new FX series Alien: Earth adds a new layer of lore into the mix.
How to watch the Alien films in order
Like any good franchise, the official release order of the films and new series differs from the actual narrative. The order you watch them is completely up to you. If you want to simply watch the whole franchise in release order, it would go like this:
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Alien (1979)
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Aliens (1986)
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Alien 3 (1992)
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Alien Resurrection (1997)
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AVP: Alien vs. Predator (2004)
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Aliens vs. Predator: Requiem (2007)
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Prometheus (2012)
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Alien: Covenant (2017)
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Alien: Romulus (2024)
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Alien: Earth (2025)
If you’re more into the timeline jumps and lore of it all, you’ll probably want to watch in chronological order. Though it’s the newest film in the franchise, Romulus takes place somewhere in the 57-year gap between Alien and Aliens. And the new series is basically a prequel to the original Alien, set two years before. So story-wise, your marathon would go something like this:
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How to watch the entire Alien franchise online
Thanks to Hulu, you can watch every single Alien movie in one place — including the latest film Alien: Romulus, which made its streaming debut last fall. And while Alien: Earth is an FX series, it will stream simultaneously on Hulu — the official streaming home of FX.
It’s becoming rare for an entire franchise to live on a single streamer, so you should definitely take advantage of your chance to enjoy an Alien marathon. Hulu subscriptions start at just $9.99 per month. Plus, there are plenty of ways to save on a subscription. We’ve rounded up all the best Hulu streaming deals below.
Is there a Hulu free trial?
New to Hulu or returning after a while? You can kick off your streaming with a free 30-day trial. That’s the most generous of any streamer. Just remember that if you want to avoid charges, you’ll have to cancel your subscription before the 30 days are up. If you choose to keep it going, it’ll cost you $9.99 per month with ads or $18.99 without.
The best Hulu streaming deals
Best Hulu deal for most people: Hulu annual subscription
If you just want to save some money after your trial ends, you can sign up for an annual Hulu subscription instead of monthly and save about 16%. Hulu with ads now costs $9.99 per month, but if you pay annually, that monthly fee drops down to just $8.33 per month. Sure, you’ll have to pay more upfront, but in the long run, it’ll save you about $19.89 total.
Best bundle deal: Get Hulu and Disney+ for 45% off
Want more bang for your buck? You can bundle Hulu with Disney+ (with ads) for just $10.99 per month. That’s just $1 more per month and about 45% in savings for access to another entire streaming library. Even better, if you’re a sports fan, you can add ESPN+ into the mix for just $16.99 per month and save 47% on all three streaming services.
Best for students: Hulu Student
As long as you’re a college student, you can sign up for Hulu for just $1.99 per month instead of the usual $9.99 per month. That’s 80% in savings for the ad-supported plan. You’ll just have to verify your student status using SheerID in order to secure the deal.
Best for T-Mobile users: Hulu (with ads)
T-Mobile customers on the Go5G Next or any Experience Beyond plans now get Hulu with ads included with their plan for no extra cost. And that’s on top of the already stacked streaming lineup of Netflix and Apple TV+. Just head over to the T-Mobile promo page and click on “redeem now” to claim your offer if you haven’t already. You’ll just have to enter your T-Mobile number and account details in order to sign up.
Note: After your initial 12-month promotional period, you’ll have to take action to keep your subscription alive.
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![Scientists Found a Continent-Sized Geological Structure Hiding Beneath Antarctica
The East Antarctic Ice Sheet is almost unfathomably huge. Covering about 75% of the entire frigid continent (nearly everything on its side of the Transantarctic Mountains), the sheet covers about 3.9 million square miles (10.2 million square kilometers) and extends down 1.4 miles (2.2 km), on average, before coming into contact with Earth’s surface. At its deepest, the ice plunges down over 3 miles (4.9 km). For decades, scientists assumed that this literally continent-sized block of ice rested on an expansive and stable chunk of Earth’s crust known as a craton. A team of researchers has now complicated that picture—mapping a vast, interconnected geological structure that fans out from a troubling “tectonic deformation.” Beneath this ice sheet, thinner and more geologically recent slices of crusty lithosphere fan out into hidden valleys called “pull-apart basins.” These basins—30 elongated wedge-shaped valleys in total—constitute an entirely new, continental-scale geological region underneath Antarctica, in fact, one which the researchers have named the East Antarctic Fan-Shaped Basin Province (EAFBP). But it’s how they likely formed that has now caught researchers’ attention.
To put it bluntly, it turns out that about 90% of the planet’s fresh water ice may not be on solid ground. Geologist John Goodge called the team’s findings “provocative” in an independent commentary on the new study, published Thursday in the journal Nature Geoscience.
“East Antarctica is typically considered from seismic tomography and geodetics to be ancient and generally stable,” according to Goodge, who studies continental tectonics with the nonprofit Planetary Science Institute. “[But] something else is going on at depth.” Continental divides Goodge speculates that this seemingly “coherent pull-apart system,” as presented in the new study, might help explain a variety of mysterious heat and water flows beneath this ice sheet’s surface, like that enormous subglacial lake identified in 2016 or some of the hundreds more like it.
The study’s authors, led by geophysicist Egidio Armadillo at the University of Genoa in Italy, agreed: “Because these basins underlie about half of the East Antarctic Ice Sheet, they are likely to heavily influence both ice-flow and landscape evolution,” the researchers wrote in their study, also published Thursday in Nature Geoscience. Armadillo’s team, coordinating across Europe and the U.K., developed their new understanding of Antarctica’s hidden bedrock via an exhaustive set of sensory data. Gravitational and magnetic anomalies were mapped via low-altitude airborne surveys. Ground surface features were mapped with seismic tools, using sound waves that vibrate through the ice and ping back information about subglacial landscapes in 3D. The grey, magenta, and cyan lines represent the apparent new fault lines discovered. Credit: Nature Geoscience All of this data—the fruits of “multi-national efforts to image within and below the ice sheet,” as Goodge put it—had already revealed that regions of the continent were “undergoing more rapid movement and ice-mass loss than previously recognized.” Armadillo’s team merely helped to explain why.
The mechanism Armadillo and his colleagues proposed for the formation of these fan-shaped basins is called “distributed rotational extension.” It involves points called Euler poles around which tectonic plates pivot or rotate rather than smash into each other or pull apart. The result is a bit like decks of cards being spread out on a table, thinning out the stack of Earth’s crust as it moves. An icy situation Goodge took pains to spell out the basins’ implications for melting Antarctic ice due to climate change and the risk of rising global sea levels.
The mere existence of these basins, he wrote, “could introduce widespread, systemic instability to the East Antarctic Ice Sheet” via thinner layers of Earth’s crust and more heat flow from below. On top of that, a series of fault-line “troughs” documented between the basins appear “tailor-made to promote outward flow of ice streams from the interior” into the world’s oceans, he said. That said, the team’s findings are unlikely to end this debate. As Goodge noted, Antarctica is “the last continental frontier of scientific exploration.” It’s still a very mysterious place, one that’s challenging to study given its inhospitable temperatures and extreme geography. Its “cryptic subglacial geology” might stay that way for a while. #Scientists #ContinentSized #Geological #Structure #Hiding #Beneath #AntarcticaAntarctica,Geology,mapping,Plate tectonics Scientists Found a Continent-Sized Geological Structure Hiding Beneath Antarctica
The East Antarctic Ice Sheet is almost unfathomably huge. Covering about 75% of the entire frigid continent (nearly everything on its side of the Transantarctic Mountains), the sheet covers about 3.9 million square miles (10.2 million square kilometers) and extends down 1.4 miles (2.2 km), on average, before coming into contact with Earth’s surface. At its deepest, the ice plunges down over 3 miles (4.9 km). For decades, scientists assumed that this literally continent-sized block of ice rested on an expansive and stable chunk of Earth’s crust known as a craton. A team of researchers has now complicated that picture—mapping a vast, interconnected geological structure that fans out from a troubling “tectonic deformation.” Beneath this ice sheet, thinner and more geologically recent slices of crusty lithosphere fan out into hidden valleys called “pull-apart basins.” These basins—30 elongated wedge-shaped valleys in total—constitute an entirely new, continental-scale geological region underneath Antarctica, in fact, one which the researchers have named the East Antarctic Fan-Shaped Basin Province (EAFBP). But it’s how they likely formed that has now caught researchers’ attention.
To put it bluntly, it turns out that about 90% of the planet’s fresh water ice may not be on solid ground. Geologist John Goodge called the team’s findings “provocative” in an independent commentary on the new study, published Thursday in the journal Nature Geoscience.
“East Antarctica is typically considered from seismic tomography and geodetics to be ancient and generally stable,” according to Goodge, who studies continental tectonics with the nonprofit Planetary Science Institute. “[But] something else is going on at depth.” Continental divides Goodge speculates that this seemingly “coherent pull-apart system,” as presented in the new study, might help explain a variety of mysterious heat and water flows beneath this ice sheet’s surface, like that enormous subglacial lake identified in 2016 or some of the hundreds more like it.
The study’s authors, led by geophysicist Egidio Armadillo at the University of Genoa in Italy, agreed: “Because these basins underlie about half of the East Antarctic Ice Sheet, they are likely to heavily influence both ice-flow and landscape evolution,” the researchers wrote in their study, also published Thursday in Nature Geoscience. Armadillo’s team, coordinating across Europe and the U.K., developed their new understanding of Antarctica’s hidden bedrock via an exhaustive set of sensory data. Gravitational and magnetic anomalies were mapped via low-altitude airborne surveys. Ground surface features were mapped with seismic tools, using sound waves that vibrate through the ice and ping back information about subglacial landscapes in 3D. The grey, magenta, and cyan lines represent the apparent new fault lines discovered. Credit: Nature Geoscience All of this data—the fruits of “multi-national efforts to image within and below the ice sheet,” as Goodge put it—had already revealed that regions of the continent were “undergoing more rapid movement and ice-mass loss than previously recognized.” Armadillo’s team merely helped to explain why.
The mechanism Armadillo and his colleagues proposed for the formation of these fan-shaped basins is called “distributed rotational extension.” It involves points called Euler poles around which tectonic plates pivot or rotate rather than smash into each other or pull apart. The result is a bit like decks of cards being spread out on a table, thinning out the stack of Earth’s crust as it moves. An icy situation Goodge took pains to spell out the basins’ implications for melting Antarctic ice due to climate change and the risk of rising global sea levels.
The mere existence of these basins, he wrote, “could introduce widespread, systemic instability to the East Antarctic Ice Sheet” via thinner layers of Earth’s crust and more heat flow from below. On top of that, a series of fault-line “troughs” documented between the basins appear “tailor-made to promote outward flow of ice streams from the interior” into the world’s oceans, he said. That said, the team’s findings are unlikely to end this debate. As Goodge noted, Antarctica is “the last continental frontier of scientific exploration.” It’s still a very mysterious place, one that’s challenging to study given its inhospitable temperatures and extreme geography. Its “cryptic subglacial geology” might stay that way for a while. #Scientists #ContinentSized #Geological #Structure #Hiding #Beneath #AntarcticaAntarctica,Geology,mapping,Plate tectonics](https://gizmodo.com/app/uploads/2026/06/East-Antarctic-Fan-shaped-Basin-Province.jpeg)
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