IBOV 171,031.73 ▲ 1.85% IPSA 11,338.38 ▲ 0.89% IPC MEX 65,729.18 ▲ 2.14% MERVAL 2,913,184 ▲ 1.35% COLCAP 2,459.23 ▲ 0.61% BVL PERÚ 58,698.13 ▲ 2.60% USD/BRL5.14▼ 0.14% USD/MXN16.90▼ 0.36% USD/CLP914.28— 0.00% USD/COP3,038▼ 1.18% USD/PEN3.35▼ 0.06% USD/ARS1,499▲ 0.12% USD/UYU40.20▲ 1.58% USD/PYG5,996▲ 1.55% USD/BOB11.43▲ 0.41% USD/DOP58.82▲ 0.20% USD/CRC450.05▲ 3.34% USD/GTQ7.62▲ 2.21% USD/HNL26.81▲ 0.31% USD/NIO36.62▲ 0.61% USD/VES778.00▼ 0.13% USD/PAB1.00— 0.00% USD/BZD2.00— 0.00% USD/JMD 157.28 — 0.00% USD/TTD6.71▲ 0.79% EUR/BRL6.00▼ 0.64% BRENT 88.88 ▼ 0.03% WTI 83.11 ▼ 0.11% IRON ORE 161.91 — — COPPER 6.61 ▲ 0.03% GOLD 4,461 ▲ 1.78% SILVER 65.59 ▲ 1.26% SOY 1,184 ▲ 3.20% CORN 480.50 ▲ 10.02% WHEAT 655.00 ▲ 3.93% COFFEE 317.25 ▼ 5.51% SUGAR 16.43 ▼ 1.79% ORANGE JUICE 138.55 ▼ 0.47% COTTON 85.03 ▲ 2.33% COCOA 5,719 ▲ 3.18% BEEF 223.60 ▼ 3.93% CATTLE 339.10 ▼ 3.16% LITHIUM 75.20 ▲ 1.47% PETR4 41.64 ▼ 0.05% VALE3 72.97 ▲ 0.83% ITUB4 38.60 ▼ 1.03% BBDC4 16.85 ▲ 0.36% ABEV3 14.89 ▼ 0.80% BBAS3 19.37 ▲ 0.47% B3SA3 14.26 ▼ 0.21% WEGE3 47.59 ▲ 0.49% PRIO3 59.14 ▼ 0.19% SUZB3 41.33 ▲ 2.35% RENT3 34.68 ▼ 0.09% AZZA3 15.89 ▼ 2.63% CSAN3 3.22 ▼ 1.83% RAIZ4 0.25 — 0.00% PCAR3 2.75 ▼ 0.36% GMAT3 3.65 ▼ 1.08% PSSA3 48.13 ▼ 0.54% CVCB3 1.33 ▼ 2.92% POSI3 3.36 ▲ 2.44% SLCE3 13.34 ▲ 0.30% NATU3 8.14 ▼ 0.73% IBOV 171,031.73 ▲ 1.85% IPSA 11,338.38 ▲ 0.89% IPC MEX 65,729.18 ▲ 2.14% MERVAL 2,913,184 ▲ 1.35% COLCAP 2,459.23 ▲ 0.61% BVL PERÚ 58,698.13 ▲ 2.60% USD/BRL 5.16 ▲ 0.01% USD/MXN 17.06 ▼ 0.24% USD/CLP 913.98 ▲ 0.04% USD/COP 3,140 ▲ 0.03% USD/PEN 3.36 ▼ 0.66% USD/ARS 1,493 ▲ 0.10% USD/UYU 40.27 ▲ 1.24% USD/PYG 5,939 ▲ 1.68% USD/BOB 11.64 ▼ 0.76% USD/DOP 58.34 ▲ 1.25% USD/CRC 445.92 ▲ 0.89% USD/GTQ 7.62 ▲ 2.21% USD/HNL 26.79 ▲ 1.57% USD/NIO 36.62 ▲ 0.69% USD/VES 762.44 ▼ 0.13% USD/PAB 1.00 — 0.00% USD/BZD 2.00 — 0.00% USD/JMD 157.28 — 0.00% USD/TTD 6.70 ▲ 0.61% EUR/BRL 5.95 ▲ 1.01% BRENT 88.88 ▼ 0.03% WTI 83.11 ▼ 0.11% IRON ORE 161.91 — — COPPER 6.61 ▲ 0.03% GOLD 4,461 ▲ 1.78% SILVER 65.59 ▲ 1.26% SOY 1,184 ▲ 3.20% CORN 480.50 ▲ 10.02% WHEAT 655.00 ▲ 3.93% COFFEE 317.25 ▼ 5.51% SUGAR 16.43 ▼ 1.79% ORANGE JUICE 138.55 ▼ 0.47% COTTON 85.03 ▲ 2.33% COCOA 5,719 ▲ 3.18% BEEF 223.60 ▼ 3.93% CATTLE 339.10 ▼ 3.16% LITHIUM 75.20 ▲ 1.47% PETR4 41.64 ▼ 0.05% VALE3 72.97 ▲ 0.83% ITUB4 38.60 ▼ 1.03% BBDC4 16.85 ▲ 0.36% ABEV3 14.89 ▼ 0.80% BBAS3 19.37 ▲ 0.47% B3SA3 14.26 ▼ 0.21% WEGE3 47.59 ▲ 0.49% PRIO3 59.14 ▼ 0.19% SUZB3 41.33 ▲ 2.35% RENT3 34.68 ▼ 0.09% AZZA3 15.89 ▼ 2.63% CSAN3 3.22 ▼ 1.83% RAIZ4 0.25 — 0.00% PCAR3 2.75 ▼ 0.36% GMAT3 3.65 ▼ 1.08% PSSA3 48.13 ▼ 0.54% CVCB3 1.33 ▼ 2.92% POSI3 3.36 ▲ 2.44% SLCE3 13.34 ▲ 0.30% NATU3 8.14 ▼ 0.73%
since 2009
Sunday, August 23, 2026

Every year the Pacific Ocean gets smaller, and the Atlantic Ocean gets bigger

By · October 10, 2022 · 2 min read

Daily Brief

The morning intel from across Latin America. Free.

By subscribing you agree to our privacy policy. We never share your email.

Every year, the Pacific Ocean gets a little smaller, and the Atlantic Ocean gets a little bigger.

Even if it is only a difference of a few centimeters, the fact is that the American continent is moving away from Europe and Africa but also closer to Asia.

Even if this geological process is not visible now, it will become more apparent in hundreds of millions of years when the next supercontinents form on Earth.

RT
Ask Rio Times
17 years of Latin America reporting, on demand.
Open the full Ask Rio Times →
One-stop reference
Company Intelligence
Every listed company in Latin America — financials, ownership and structure for 1,450+ companies across 26 exchanges, in one place.
Browse the directory →

PLATE TECTONICS: RESPONSIBLE FOR CHANGES IN THE EARTH’S CRUST

Even if we don’t realize it, the Earth constantly changes shape. That is due to the slow but constant shifting of tectonic plates and vast chunks of oceanic and continental crust located in the outermost part of the planet (lithosphere).

The Earth’s crust consists of seven major tectonic plates (African, Antarctic, Eurasian, Indo-Australian, North American, Pacific, and South American).

There are also smaller tectonic plates, such as the Nazca and Cocos plates.

And here’s the important part: the Earth’s metamorphism is determined by what happens at the boundaries between plates.

When these plate boundaries converge, one plate sinks onto the other, causing the crust to disappear.

These places are called subduction zones. On the other hand, if the edges between the plates are divergent, both move away from each other, and new crust or new plates are formed. These are called expansion zones.

The Pacific is shrinking, and the Atlantic is widening because there are more subduction zones in the Pacific and a large expansion zone in the Atlantic known as the Mid-Atlantic Ridge.

This submarine ridge, formed where the North and South American plates collide with the African and Eurasian plates, is 1,500 kilometers wide and extends 16,000 kilometers from southern Iceland to southern Africa.

The Mid-Atlantic Ridge is so long that it is twice as long as the Andes, the longest mountain range on the Earth’s surface, estimated at 7,000 kilometers.

It is also so high in elevation that it gives rise to islands such as the Azores (Portugal) or Tristan da Cunha (United Kingdom).

The Pacific Ocean, on the other hand, is surrounded by a horseshoe-shaped chain of subduction zones that extends for 40,000 kilometers and is known as the Pacific Ring of Fire because of the intense seismic and volcanic activity in the areas it surrounds.

According to Australian authorities, the Pacific Ocean shrinks by about two to three centimeters yearly, while the Atlantic Ocean widens by about five centimeters over the same period.

With information from Latina Press

This article was produced by The Rio Times’ automated newsroom system. How we use AI · Report an error

Read More from The Rio Times

The Rio Times · Power Map
See who really holds power in Latin America
Click to open the Power Map

Rotate for Best Experience

This report is optimized for landscape viewing. Rotate your phone for the full experience.