Before heading on a trip to Tahoe last weekend, GM offered me the use of the company’s 9,000-pound monument to excess – the new 2026 electric Escalade IQL (starting at $130,405) – for a week to test-drive. Before you continue, note that I’m not a professional car reviewer. TechCrunch has excellent transportation writers; I am not one of them. I do, however, drive an electric car.
I was immediately game. I’d first glimpsed one last summer at a car show, where some regional car dealers had stationed themselves at the end of a long field dotted with exquisite vintage automobiles. My immediate reaction was “Jesus, that’s enormous,” followed by a surprising admiration for its design, which, despite its enormous scale, shows restraint. For lack of a better word, I’m going to say it’s “strapping.” Its proportions just work.
My excitement waned pretty quickly when the car was dropped off at my house a day before our departure time. This thing is a monstrosity — at 228.5 inches long and 94.1 inches wide, it made our own cars look like toys. My first apartment in San Francisco was smaller. Trying to drive it up my driveway was a little harrowing, too; it’s so big, and its hood is so high, that if you’re ascending a road at a certain slope – we live midway down a hill; our mailbox is at the top of it – you can’t see whatever is directly in front of the car.
I thought about just leaving it in the driveway for the duration of the trip. The other alternative was doing what I could to grow more comfortable with the prospect of driving it 200 miles to Tahoe City, so I tooled around in it that night and the next day, picking up dinner, heading to an exercise class — just basic stuff around town. When I ran into a friend on the street, I volunteered as quickly as possible that this was not my new car, that I was going to possibly review it, and wasn’t its size ridiculous? It felt like a tank. I thought: other than hotels that use SUVs like the Escalade to ferry guests around, what kind of monster chooses a car like this?
Five days later, it turns out that I am that kind of monster.
Look, I don’t know how or when I fell for this car. If I’d written this review after two days, it would read very differently. Even now, I’m not so blind that I don’t see its shortcomings.
It was the Escalade’s performance in a terrible snowstorm that really won my heart, but let me walk you through the steps between “Ugh, this car is a tank” and “Yes! This car is a tank.”
Techcrunch event
Boston, MA
|
June 9, 2026
Just getting into it requires a little more exertion than would seem to make sense. I’m fairly athletic and I still found myself wondering if this thing shouldn’t come with an automated step stool.
Inside is where digital maximalism does its work. The dashboard opens with a 55-inch curved LED screen with 8K resolution that reads less like a car display and more like a situation room. Front passengers get their own screens. Second-row passengers also get 12.6-inch personal screens along with stowable tray tables, dual wireless chargers, and — with the most lavish version of the car — massage seats that will make them forget they’re in a vehicle at all. Google Maps handles navigation. And the polarized screen technology deserves its own praise: while one of my kids binge-watched Hulu in the front seat, not a frame of it leaked into my sightline from behind the wheel.
The cabin itself is built around the premise that no one inside should feel crowded, and it delivers. Front legroom stretches to 45.2 inches; the second row offers 41.3; even the third row manages 32.3 inches. Seven adults could share this machine for a long while without fraying each other’s nerves. Heated and ventilated leather seats with 14-way power adjustment come standard in the first two rows, and the whole operation runs on 5G Wi-Fi.
The car also comes standard with Super Cruise, GM’s hands-free driving system, which I’m not sure I quite figured out. True car reviewers seem to love it; when I tried it, the car felt like it was drifting to an alarming degree between the outer boundaries of the highway lane, and when that happens, it unleashes an escalating sequence of warnings. First, a red steering wheel icon materializes on-screen. Then your seat pulses haptic warnings against your rump. Ignore those and a chime — both reminder and reproach — fills the cabin. GM calls this impolite series a “driver takeover request.”
Did I mention the 38-speaker AKG Studio sound system? So good.
As for the exterior — this is a handsome giant, but it takes some getting used to. At first, I found the grille, which is just for show, almost comically imposing. This is definitely a car for people who are the boss, or want to be the boss, or want to look like the boss while privately dealing with existential crises. Pulling up to a glass-lined restaurant one night, I’m pretty sure I blinded half the patrons as I swung into a parking spot perpendicular to the building, the Escalade’s headlights flooding through the windows.
Then there is the light show the car launches whenever it detects you approaching via the key or the MyCadillac app. It’s as if it’s saying, “Hey, chief, where we headed?” before you’ve so much as touched a door handle. (In the vernacular of Cadillac, this is thanks to its “advanced, all-LED exterior lighting system,” highlighted by a “crystal shield” illuminated grille and crest, along with vertical LED headlamps and “choreography-capable tail lamps.”)
It is, objectively, a bit much. I loved it immediately.
Despite its size, the Escalade IQL is unexpectedly nimble. Not “sports car darting through traffic” nimble, but “I can’t quite believe something this colossal doesn’t handle like a battleship” nimble.
Now we arrive at the frustrations. The front trunk — or “frunk” in the lexicon of EV devotees — operates in mysterious and frustrating ways. Opening requires holding the button until completion. Release prematurely and it halts mid-ascent, frozen in automotive purgatory, forcing you to restart the entire sequence. Closing demands the same sustained pressure. The rear trunk, conversely, requires two distinct taps followed by immediate button abandonment. Hold too long and nothing happens.
Relatedly, twice, the vehicle refused to power down after I’d finished driving. The car simply sat there, running, even when shifted to park and opened the door (which tells the car to turn off). One clunky solution: open the frunk, close the frunk, shift into drive, then park, then exit entirely.
As for the software, it’s absolutely fine unless you’ve owned a Tesla, in which case, prepare for disappointment. This seems to be true across the board — everyone I know who owns both a Tesla and another EV, no matter how high end, says the same thing. Once you’ve internalized how effortlessly Tesla’s software dissolves barriers between intention and execution, every other automaker’s software feels like a compromise.
Which brings us to the nadir of the trip: charging in Tahoe during winter. For all its virtues, the Escalade IQL is, by any measure, a thirsty machine. The battery is a 205 kWh pack — enormous, and it needs to be, because the car burns through roughly 45 kWh per 100 miles, which is considerably more than comparable electric SUVs. Cadillac estimates 460 miles of range on a full charge, and in ideal conditions that holds up. Tahoe in winter, however, is not ideal conditions. We’d also arrived with less charge than we should have. A series of side trips on the way up, including an emergency detour to find shirts for a family member who had packed none, had eaten into the battery more than expected. By the time we needed to charge, we genuinely needed to charge.
We approached a Tesla Supercharger in Tahoe City that appeared on the MyCadillac app, but when we plugged in to the designated stall, nothing happened. We searched for answers, discovering that even Tesla stations that accept non-Tesla vehicles throttle energy to 6 kilowatts per hour anyway, but it was a frustrating experience. A nearby EVGo had shuttered a month prior. ChargePoint’s two units at the Tahoe City Public Utility lot were, respectively, broken and willing to connect but not to actually charge anything. We briefly contemplated a 35-mile drive to Incline Village, did the math on what stranded would actually look like, and decided against it. Then I discovered an Electrify America station 12 miles away. We drove through gathering snow, arrived shortly before 11 p.m., and it worked. We sat there for an hour fighting exhaustion before driving home.
The following morning revealed another issue via an app alert: tire pressure had dropped to 53 and 56 PSI in the front (recommended: 61) and 62 PSI in the rear (recommended: 68). I have no idea whether the car had been delivered that way or whether something else was going on — either way, it meant someone standing at a gas station filling tires while being pelted directly in the face with ice. (That someone was my husband.) The tires held steady after that, even as the week kept doing its worst. For a family trip, it was going great.
At this point, in fact, I would have told you that the Escalade IQL is unquestionably luxurious and ideal for families of four or more who value space and technology. I would tell you it came burdened by real tradeoffs: forward visibility obstructed by its commanding hood, parking challenges inherent to its dimensions, limited charging infrastructure for a machine this ravenous, and tires tasked with supporting 9,000 pounds. It’s a beautiful car, I would have said, but it’s not for me.
But the snow that had started to fall kept falling. Within two days, eight feet had accumulated, making it impossible to ski — the entire point of the trip — and terrifying to drive. Except I found that I wasn’t terrified because we had the Escalade, which, because of its weight, felt like driving a tank through the snow. What could have been harrowing felt serene. It was quiet, it was strong, it was taking charge in a bad situation.
I also adjusted to the size. By the end of this past week I had stopped mouthing “I’m sorry” to whoever who was waiting for me to figure out where to park it. I had stopped caring what it said about me that I was driving a car whose entire design philosophy is: the owner of this vehicle is not waiting in line. Eight feet of snow had fallen, we needed groceries, and I was the one with the tank, suckers! I could sense my husband falling for the car, too.
Then, as tends to happen in Tahoe, the snow stopped all at once and the sun came out, and the Escalade was just a very dirty car sitting in the driveway (sorry, GM!). It was in this moment that I realized: I still like it, and it’s not because of the emergency alone. I love riding high, with the speaker system flooding the car with a favorite soundtrack. That light show still gets me. The car’s long, curved LED screen is a marvel, among other features.
The frunk is still unhinged. I won’t soon forget the panic of not being able to charge the car where I thought I could. Parking this thing is truly an exercise in patience. I have strong opinions about unnecessary consumption. None of that has changed.
I just also, somehow, want this car, so when the GM middleman comes to collect it, I may hide it under a tarp — a very large tarp — and tell him he has the wrong address.
Source link
#9000pound #monster #dont #give #TechCrunch
![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 "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://i0.wp.com/gizmodo.com/app/uploads/2026/06/East-Antarctic-Fan-shaped-Basin-Province.jpeg?ssl=1 "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")
Post Comment