The Geographical Challenges of Mexico City - Why We're Sinking
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Mexico City

The Geographical Challenges of Mexico City - Why We're Sinking

Sarah Mitchell
Sarah Mitchell
February 11, 2026 9 min read 67

Yes, Mexico City is sinking at an alarming rate of approximately 20 inches per year due to excessive aquifer extraction beneath the ancient Lake Texcoco clay bed. In some areas, subsidence reaches 1.5 feet annually, and projections show parts of the city could drop 65-100 feet by 2100. This geological crisis affects infrastructure, buildings, and water systems across the metropolitan area.

Living in Mexico City means living in one of the world's most geographically challenging metropolitan areas. The city faces an ecological crisis that most residents don't fully understand: we're literally sinking. After a decade here, I've come to appreciate just how profound this problem is and what it means for the city's future.

The Sinking City

Mexico City is sinking at an average rate of 20 inches per year. In some areas, the subsidence is even more dramatic, up to 1.5 feet annually. This isn't a gradual, barely perceptible process. It's fast enough that you can see the effects over just a few years.

What This Means Long-Term

The projections are staggering. By the end of this century, some areas of Mexico City could drop by 65 to 100 feet. That's not a typo, we're talking about sections of the city potentially sinking the equivalent of a 10-story building over the course of a lifetime.

The Historical Context: Tenochtitlan

To understand why Mexico City is sinking, you need to understand its history. The Aztecs built their capital, Tenochtitlan, on a swampy island in the middle of Lake Texcoco around 1325 CE.

Aztec Engineering

The Aztecs were sophisticated engineers. They created an innovative system of floating gardens (chinampas), built causeways connecting the island to the mainland, and constructed elaborate dams and canals to manage water levels and prevent flooding.

The system worked remarkably well. Tenochtitlan was one of the largest cities in the world at its peak, with a population estimated between 200,000-400,000 people, all living on what was essentially a managed wetland.

The Spanish Destruction

When the Spanish conquered Tenochtitlan in 1521, they made a catastrophic decision: instead of preserving the sophisticated Aztec water management systems, they destroyed them.

The Spanish filled in canals, destroyed dams, and gradually began draining the lake to create more "buildable" land. They wanted to build a European-style city, and the Aztec hydraulic infrastructure didn't fit that vision.

This was an ecological disaster whose consequences we're still experiencing 500 years later.

The Water Paradox

Here's what makes the situation particularly frustrating: Mexico City receives substantial rainfall, about 30 inches per year, comparable to many U.S. cities. Yet the city faces severe water scarcity.

Why the Paradox Exists

When the Spanish filled in Lake Texcoco and destroyed the natural water management systems, they eliminated the city's ability to capture and store rainwater. Instead of being absorbed and stored, rainwater runs off the impermeable urban surface, creating flooding during rainy season while contributing nothing to the water supply.

It's an absurd situation: a city that floods during rainy season while simultaneously experiencing water shortages.

Population Growth and Aquifer Extraction

As Mexico City's population exploded to over 9 million in the city proper (and over 20 million in the greater metropolitan area), water demand increased dramatically.

Pumping from Below

To meet this demand, the city extracts enormous amounts of water from the aquifers beneath it. We're essentially mining water from underground, water that took thousands of years to accumulate.

But here's the problem: Mexico City is built on soft clay deposits left behind by the ancient lake. When you extract water from the aquifers beneath this clay, the clay compacts. And when clay compacts, the city above it sinks.

The Vicious Cycle

More people need more water. More water extraction causes more sinking. More sinking damages infrastructure, making it harder to manage water effectively. The cycle compounds on itself.

The Compounding Infrastructure Problems

The sinking isn't uniform across the city, which creates additional challenges.

Uneven Subsidence

Different parts of the city are sinking at different rates depending on the local geology and the intensity of water extraction in that area. This uneven sinking causes serious infrastructure problems.

Damaged Buildings

Historic buildings throughout the city lean at precarious angles because their foundations have settled unevenly. Walking through Centro Histórico, you can see colonial-era buildings that are visibly tilted.

Some buildings have their original first floor now at or below current ground level because the street around them has sunk while the building itself, built on deeper foundation, has sunk less (or sometimes not at all).

Buckled Streets and Sidewalks

Uneven subsidence creates waves and buckling in streets and sidewalks. What was once a level street now has pronounced ups and downs as different sections settle at different rates.

The Angel of Independence

One of the most visible examples of subsidence is the Angel of Independence, one of Mexico City's most iconic monuments. When it was built in 1910, you could walk directly from street level to the monument's base. Over the decades, as the ground around it sank, the monument appeared to grow taller.

Eventually, 14 additional steps had to be added to reach the monument from the new, lower street level. The monument didn't grow, the ground around it dropped.

Earthquakes: Making a Bad Situation Worse

Mexico City sits in an active seismic zone, and the soft clay lake bed amplifies earthquake effects.

The Lake Bed Effect

When earthquakes occur, the soft clay beneath Mexico City acts like jello, amplifying and extending the shaking. Earthquakes that might cause minor damage elsewhere create devastating effects here because the ground itself magnifies the seismic waves.

Subsidence and Seismic Risk

As the city continues to sink and infrastructure becomes stressed, the vulnerability to earthquake damage increases. Buildings that are already stressed from uneven settlement are more vulnerable to seismic damage.

Water Infrastructure Challenges

The sinking has created serious problems for water and sewage infrastructure.

Gravity-Based Systems Don't Work

Sewage systems typically rely on gravity to move waste downhill and out of the city. But when the city is sinking unevenly, the "downhill" keeps changing. Areas that used to drain now flood. Pipes that used to work now back up.

Leaking Water Mains

As the ground shifts and settles, water mains crack and leak. Mexico City loses an estimated 40% of its water to leaks in the distribution system. We're pumping water from depleting aquifers, causing the city to sink, and then losing nearly half of that water to broken pipes caused by the sinking.

It's a perfect example of a self-reinforcing negative feedback loop.

What's Being Done?

The city is aware of these problems and has implemented some measures, though they're far from sufficient.

Reduced Extraction

There have been efforts to reduce aquifer extraction by importing more water from outside the valley. The Cutzamala System, for example, pumps water from over 100 miles away, though this is expensive and energy-intensive.

Water Treatment and Reuse

Expanding water treatment and reuse could reduce demand on the aquifers, though implementation has been slow.

Rainwater Capture

There have been pilot programs for rainwater capture and infiltration, trying to replenish the aquifers rather than letting rainwater simply run off. But the scale of implementation is tiny relative to the need.

The Long-Term Question

Here's the uncomfortable question nobody wants to answer: is Mexico City's current location sustainable long-term?

You have a city of 20+ million people built on soft clay, sinking at an accelerating rate, depleting its water supply, vulnerable to earthquakes, with infrastructure increasingly stressed by uneven settlement.

At what point does this become untenable? What happens when key infrastructure simply can't function anymore because of the subsidence? What happens when the aquifers are depleted?

These aren't hypothetical questions. They're challenges the city will face within the lifetimes of people living here now.

Living with the Reality

As someone who's lived here for over a decade, I've developed a sort of fatalistic acceptance of the situation. You learn to handle the buckled sidewalks, you notice the buildings that lean a bit more each year, you deal with the periodic water shortages.

But I've also developed deep respect for the resilience and ingenuity of Mexico City residents. This is a population that's been solving impossible problems for centuries, from the Aztecs building a thriving city on a lake to modern residents navigating the challenges of subsidence and water scarcity.

Related Mexico City Guides

Frequently Asked Questions

How fast is Mexico City sinking?
Mexico City sinks at an average rate of 20 inches (50 cm) per year, with some areas experiencing subsidence up to 1.5 feet (45 cm) annually. The rate varies across different neighborhoods depending on local geology and aquifer extraction intensity.
Why is Mexico City built on a lake bed?
The Aztecs founded Tenochtitlan on Lake Texcoco in 1325 CE based on a prophecy. They built sophisticated water management systems that made living on the lake viable. After the Spanish conquest in 1521, colonizers drained the lake rather than maintaining the Aztec hydraulic infrastructure.
Can Mexico City's sinking be stopped?
Stopping the subsidence completely is nearly impossible. The best approach is slowing it through reduced aquifer extraction, increased water importation from outside the valley, improved water treatment and reuse, and rainwater capture systems. However, implementation remains limited relative to the scale of the problem.
What happens to buildings as the city sinks?
Buildings experience uneven settlement, causing them to tilt and crack. Historic structures in Centro Histórico visibly lean. Some buildings have their original first floors now at or below street level. Infrastructure like water mains and sewage pipes crack from the shifting ground, contributing to the city's 40% water loss rate.
Written by
Sarah Mitchell
Sarah Mitchell
United States From Austin, United States | Mexico Living in Mexico City, Mexico

Austin tech refugee. Mexico City resident since 2014. Decade in CDMX. Working toward citizenship. UX consultant. I write about food, culture, and the invisible rules nobody tells you about.

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