Table of Contents (click to expand)
- What Is Water Pressure, And Why Does It Push From Every Side?
- How Much Pressure Is At The Titanic, And At The Bottom Of The Ocean?
- Why Does Water Barely Squeeze, Even Under 16,000 psi?
- What Would 6,000 psi Do To A Human?
- Is There An Upper Limit To Water Pressure?
- Can Water Pressure Cut Through Steel?
- At What psi Does Steel Break, And Why Doesn't The Ocean Break It?
- So, Is There An Upper Limit To Water Pressure, And Could It Punch Through Steel?
There is no known upper limit to water pressure, but there is a limit to how long water stays liquid: squeeze it to about 10,000 times the air pressure at sea level and it freezes solid at room temperature, into a dense form of ice called ice VI, then into ice VII at roughly twice that pressure. Water itself barely shrinks along the way, losing only about 5 percent of its volume at the bottom of the Challenger Deep, where the pressure is about 1,080 atmospheres or 16,000 psi. Pressure alone never cuts steel: the ocean floor squeezes a steel hull evenly from every side and leaves it whole, while a 60,000 psi waterjet cuts steel because the water leaves the nozzle at over twice the speed of sound carrying garnet grit, which sandblasts a hairline groove through the metal.
Dive to the bottom of a swimming pool and hold still. Your ears ache. That is the weight of three meters of water pressing on your eardrums, and it already hurts.
Now watch a waterjet cutter at work, like the one in the video below. A pencil-thin stream of water slices a steel plate like cheese. The obvious conclusion is that water pressure, turned up far enough, beats anything. Which raises two questions. How far can you turn it up before something gives? And is there a point where water refuses to be squeezed any further?
The answers are stranger than the questions. Water never runs out of ways to be squeezed. It runs out of ways to stay water. And the thing cutting the steel was never the pressure at all.
What Is Water Pressure, And Why Does It Push From Every Side?
Press your palm flat on a table. You are applying a force over the area of your hand. That is pressure: force spread over an area. NOAA defines water pressure as “the force per unit area exerted by a liquid on an object.”
Air is already doing this to you. At sea level it presses on every square inch of you with about 14.7 pounds of force, an amount called one atmosphere, or 1 atm. You do not notice because, as NOAA puts it, “the fluids in your body are pushing outward with the same force.” Hold on to that baseline. Every big number in this article is a multiple of the air pressing on you right now.
Underwater, the weight of the water above you adds to that. The formula:
P = ρgh
P is the pressure. ρ (the Greek letter rho) is the density of the water, g is the pull of gravity, and h is the depth. For seawater the numbers work out to a tidy rule: every 10 meters (33 feet) of depth adds about one more atmosphere. We used the same formula to explain why a bathtub drains faster while you are still in it.
One more thing about liquids, and it matters most later. Water does not push down. It pushes in, from every direction at once, with the same strength. That is Pascal’s principle. A submarine at depth is not being sat on. It is being hugged, hard, from all sides.

How Much Pressure Is At The Titanic, And At The Bottom Of The Ocean?
The wreck of the Titanic sits about 3,800 meters (12,500 feet) down, per NOAA. A University of Florida engineering note gets 378 atmospheres of water pressure at that depth. Add the air on top and you have about 380 atm. That is roughly 5,500 psi, or 38 MPa. Search results often round it to 6,000 psi.
In the terms we set up: every square inch of a submersible’s hull at the Titanic carries about 5,500 pounds. That is a large SUV, parked on a postage stamp, on every postage stamp.
The bottom of the ocean is worse. The Challenger Deep in the Mariana Trench is about 10,935 meters (35,876 feet) down. NOAA’s JetStream puts the pressure there at “about 1080 atmospheres or 16,000 pounds per square inch.” In metric, about 110 MPa. Nearly three Titanics, stacked.
So the ocean tops out around a thousand atmospheres. That sounds like a ceiling. It is not. It is only the deepest hole we happen to have.

Why Does Water Barely Squeeze, Even Under 16,000 psi?
Take a liter of water to the bottom of the Challenger Deep, under 16,000 psi. How much smaller is it? About 5 percent. Not half. Not a tenth. A shot glass, poured off the top of a liter bottle.
Every material has a stiffness against squeezing. Physicists call it the bulk modulus, and the bigger the number, the harder the stuff is to shrink. MIT’s Classical Mechanics course tabulates it. Water sits at 2.2 billion pascals, which is 2,200 MPa. Air is around 0.1 MPa. Steel is 160,000 MPa. The rule connecting them is short:
ΔV / V = P / K
The fraction of volume you lose (ΔV / V) equals the pressure you apply (P) divided by the bulk modulus (K). Three steps to the ocean floor:
- Pressure at the Challenger Deep: about 110 MPa.
- Bulk modulus of water: 2,200 MPa.
- Divide: 110 ÷ 2,200 = 0.05, or 5 percent.
At the Titanic, the shrink is under 2 percent. Even the 5 percent is an overestimate, because water stiffens as you squeeze it; MIT notes its value “increases at higher pressure.”
Now flip the sum around. To shrink water by 1 percent you need about 22 MPa, or 217 atmospheres, more than two kilometers of ocean. To shrink air by 1 percent you need one hundredth of an atmosphere, because a gas’s stiffness equals its own pressure. Think of a bag of sponges and a bag of marbles. Squeeze the sponges and they collapse. Squeeze the marbles and the bag stays the same size, no matter how red your face gets.
This is why the deep ocean is not a giant compressor, and why the bottom of the ocean stays cold. You cannot heat something by squeezing it if it refuses to be squeezed.

What Would 6,000 psi Do To A Human?
This question sits under the Titanic one for a grim reason. On June 18, 2023, the submersible Titan imploded on its way to the wreck. The NTSB’s investigation found that its hull failed at a depth of about 3,363 meters (11,032 feet). Five people died.
What pressure does to a body follows from the last section. Your body is mostly water, and water barely squeezes. The tissue is not the problem. The problem is every pocket of gas: lungs, sinuses, the middle ear, the gut. Gas collapses to a fraction of its volume under a few extra atmospheres. A rigid, air-filled hull collapses all at once when it gives way. Our article on what makes a submarine implode covers that failure in detail.
Could you survive 25,000 feet underwater? No. That is 7,620 meters, about 760 atmospheres. The deepest scuba dive on record, Ahmed Gabr’s 2014 descent to 332 meters, is a shade over 1 percent of that depth. People reach the deep ocean only inside a rigid hull that keeps one atmosphere around them. The Navy bathyscaphe Trieste did it first, on 23 January 1960. Don Walsh and Jacques Piccard rode a steel sphere to the floor of the Challenger Deep.
Are there fish at Titanic depth? Yes, comfortably. The deepest confirmed fish, a snailfish, was filmed at 8,336 meters (27,000 feet), more than twice as deep. Fish have no air-filled lungs to crush, which is how deep-sea fish avoid being crushed.

Is There An Upper Limit To Water Pressure?
Strictly, no. Nothing in physics says you must stop adding force. Inside the Earth, the rock above does the adding for you. Pressures in the core reach about 360 GPa. That is 3.6 million atmospheres, or more than 3,000 Challenger Deeps. In the lab, Princeton geoscientist Thomas Duffy notes that diamond-anvil presses “rarely reach more than 300 GPa.” His team’s laser experiments hit 1,314 GPa. Nobody has found a ceiling. They have found only bigger hammers.
Water, though, changes its mind long before that. Keep squeezing liquid water at room temperature and, at about 1 GPa, it freezes. No cooling required. A 2014 study in Scientific Reports lays out the sequence. Under compression at room temperature, liquid water freezes into ice VI at about 1 GPa. It then “transforms into ice VII at pressures over 2 GPa.” A 2025 paper in Nature Materials pins the freezing pressure of ice VI at 0.96 GPa.
One GPa is about 10,000 atmospheres, or 145,000 psi. Stack nine Challenger Deeps and the water in your glass turns into a solid you could knock on, at 20 °C (68 °F). These are not the ice in your freezer. Their molecules pack far tighter, the only way to take up less room when the pressure demands it.
This is not a chalkboard curiosity. Gemologists have found ice VII trapped inside natural diamonds that formed hundreds of kilometers down. The trapped pockets still hold 7 to 28 GPa. Somewhere in the Earth, water sits at room temperature as a solid, because it has nowhere to go.

Can Water Pressure Cut Through Steel?
Yes, water cuts steel every day in machine shops, and we have a whole article on waterjet cutters. The short version: a pump squeezes water to between 20,000 and 60,000 psi and fires it through a jewel nozzle a few hundredths of an inch across. That is 4,100 atmospheres, nearly four Challenger Deeps, from a box in a workshop.
But look at what the pressure is for. It is not applied to the steel. It is applied to the water, inside the pump, and when that water escapes through a tiny hole its pressure turns into speed. Bernoulli’s equation gives the exchange rate:
v = √(2P / ρ)
Here v is the speed of the jet, P is the pump pressure and ρ is the density of water. Plug in 414 MPa (60,000 psi) and 1,000 kg per cubic meter:
- 2 × 414,000,000 ÷ 1,000 = 828,000
- The square root of 828,000 is about 910
- So the jet leaves at roughly 910 meters per second, about 2,000 mph, well over twice the speed of sound
The University of Florida’s manufacturing lab notes put it at “approaching Mach 3.” A waterjet is not a press. It is a gun that fires water.
And even that gun does not cut steel on its own. The same notes list what a pure water jet is used for: “foam, rubber, cloth, paper, food products.” For metal, shops feed a fine, hard grit into the stream past the nozzle, almost always garnet. MIT’s workshop guide says the water and garnet cut “by eroding the material.” The water is a delivery truck for millions of tiny sharp stones. The stones do the cutting, one microscopic chip at a time, along a groove about 0.025 inches wide. MIT’s guide puts the workable thickness at “1/16” through 4”” even for hard materials.

At What psi Does Steel Break, And Why Doesn't The Ocean Break It?
Here is a number that looks like it settles the argument. Ordinary structural steel, the grade called A36, starts to bend for good at a pull of 36,000 psi. It tears apart between 58,000 and 80,000 psi. A waterjet pump runs at 60,000 psi. Case closed?
Not even close, and the reason is the whole point of this article. Those steel figures are for pulling: a bar stretched from both ends until it snaps. The ocean does not pull. It squeezes, from every side at once. Squeezing a solid block of steel from all sides does not tear it. It shrinks it, by a hair. Steel’s bulk modulus is 160,000 MPa, so the 110 MPa at the Challenger Deep shrinks a solid block by about 0.07 percent. Steel does not break under water pressure. It gets slightly smaller.
What breaks is a hollow. A hull with one atmosphere inside and 380 outside has a difference across its wall, and that difference bends the wall inward. That is a shape problem, not a steel problem. It is why the Trieste’s steel sphere sat on the floor of the Challenger Deep in 1960 and came back up.
Now compare the waterjet. Its 60,000 psi does not press on the steel from all sides. It has become a stream of grit at 900 meters per second, aimed at one spot the width of a pencil lead. Each garnet grain lands on a patch of metal so small that the local stress spikes past the steel’s breaking point, and a chip comes away. Then the next grain, and a few million more. Cutting is concentrated, one-directional force plus abrasion. Ocean pressure is spread-out, all-directional force with nothing to abrade. Same unit on the gauge, different job.
Which also answers a question that travels with these: is 100 psi too high for water pressure? For your house, yes. Most plumbing codes call for a pressure-reducing valve above 80 psi. Higher pressures, the guidance says, “can rupture pipes and damage fixtures.” The ocean floor is 200 times that. The waterjet is 750 times that. Your kitchen tap lives on the bottom rung of a tall ladder.

So, Is There An Upper Limit To Water Pressure, And Could It Punch Through Steel?
There is no ceiling on water pressure. You can keep squeezing all the way to the Earth’s core, and physics will not stop you. What ends is water’s career as a liquid. At around 10,000 atmospheres it freezes into ice VI, at around 20,000 into ice VII, both at room temperature. Water does not have a maximum pressure. It has a resignation letter.
And pressure alone never punched through anything. The 16,000 psi at the bottom of the Challenger Deep squeezes a steel sphere from every side and leaves it a hair smaller. The 60,000 psi in a waterjet pump never touches the steel. It becomes speed, the speed becomes a stream of garnet, and the garnet does the cutting, grain by grain. Take the grit out and the same jet is trimming foam and slicing cake.
So the next time a video shows water slicing steel, you will know what you are looking at. Not water winning a shoving match. Water, at twice the speed of sound, carrying a small and furious sandstorm. And if someone asks how hard you can squeeze water, the answer is: as hard as you like. It will stop being water before it stops being squeezed.

References (click to expand)
- How does pressure change with ocean depth? — NOAA National Ocean Service
- Water Pressure At 12500 Feet — University of Florida, Mechanical & Aerospace Engineering (PDF)
- Pressure: Pascal’s Principle — HyperPhysics, Georgia State University
- R.M.S. Titanic: Frequently Asked Questions — NOAA Office of General Counsel
- How deep is the ocean? — NOAA National Ocean Service
- Learning Lesson: A Pressing Engagement — NOAA JetStream
- Chapter 27: Static Fluids — MIT OpenCourseWare, 8.01SC Classical Mechanics (PDF)
- Fundamental Properties of Fluids — Introduction to Aerospace Flight Vehicles, Embry-Riddle Aeronautical University
- Hull Failure and Implosion of Submersible Titan, MIR-25-36 — National Transportation Safety Board (PDF)
- Ahmed Gabr breaks record for deepest SCUBA dive — Guinness World Records
- What is the deepest-living fish? — NOAA Ocean Exploration
- Ultrahigh-pressure laser experiments shed light on cores of ‘super-Earth’ exoplanets — Princeton University
- Anomalous behaviour of proton conduction in ice VII — Scientific Reports 4, 5778 (2014)
- Multiple freezing–melting pathways of high-density ice through ice XXI phase at room temperature — Nature Materials (2025), via PubMed Central
- Diamonds Help Solve the Enigma of Earth’s Deep Water — Gems & Gemology, Gemological Institute of America
- Abrasive Water Jet Processes, EML2322L — University of Florida, Mechanical & Aerospace Engineering (PDF)
- Pressure: Bernoulli Equation — HyperPhysics, Georgia State University
- A Gentle Introduction to Abrasive (Waterjet) Machining, Part I — MIT FabLab (PDF)
- Structural steels and minimum tensile properties — MIT Department of Civil and Environmental Engineering, 1.51 (PDF)
- Service Water Pressure — Building America Solution Center, Pacific Northwest National Laboratory
- Trieste (Bathyscaphe) — Dictionary of American Naval Fighting Ships, Naval History and Heritage Command
How this article was made. It was researched from the sources cited above and drafted with the help of AI, then fact-checked, edited and approved by Abhishek Jain before publication. Illustrations that are not credited to a photographer are generated diagrams or illustrations, not photographs.







