When and how were the Galapagos Islands formed?

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We spent 10 days in the Galapagos. There’s so much to learn and enjoy there — especially when it comes to Galapagos animals — but we thought we’d start with how the Galapagos were formed.

The Galapagos are a set of islands right on the equator, off the coast of Ecuador. They were undiscovered by humans until about 500 years ago. Volcanoes formed the islands by erupting underneath the ocean, slowly building up enough lava to create land above the level of the ocean.

In a previous post, we talked a little bit about plate tectonics, and how that results in earthquakes (one of which we felt in Arequipa). Tectonic plates are huge pieces of rock that make up the outer layer of the earth, called the crust. They fit together kind of like a jigsaw puzzle. Sometimes whole continents are on one piece of the jigsaw puzzle.

The Galapagos are on the edge of the Nazca plate. The Nazca plate is moving slowly east — it moves about 2 ½ inches per year. The Nazca plate slides under the South America plate, pushing against it. All this pushing actually created the Andes Mountains (which are still being pushed up higher due to the movement of the Nazca plate).

Hot Spots and Sliding Islands

There’s something called a hot spot underneath the Galapagos, which is kind of a hole that goes down toward the center of the earth. Lava bubbles up from this hot spot and comes to the surface in volcanoes. As the volcanoes erupt, they create islands — the Galapagos Islands. But since these islands are sitting on the Nazca plate, they are slowly sliding east – 2 1/2 inches per year.

Since islands form, and then slide east, the islands farthest east are the oldest ones (they are several million years old). The newest islands, the ones to the west, are “only” about 500,000 years old — and are still over the hot spot (which doesn’t move). We created a little video to show what happens.

As a result, different Galapagos islands can have completely different biomes, based on how old they are, their elevation, and the effect of different ocean currents. Islands that are not far away from each other can look completely different, and have different types of animals and plants living on them.

This picture is of the highlands of Santa Cruz island — there are lots of green plants, similar to a rainforest biome.

Here’s a landscape that seems to come from the moon, from Santiago Island.

And here are mangrove forests from another part of Santa Cruz Island. We explored them by paddling on inflatable boats, called pangas, like the one you see in the photo below.

Evolution

All these different biomes created an amazing laboratory for evolution (the idea that animals and plants change over long periods of time). The Galapagos actually helped Charles Darwin to develop his theory of evolution while visiting here in 1832. In the Galapagos, different animals evolved in different ways depending on which island they lived on, and Darwin observed these differences.

For example, many of the islands have little finches on them, which once were all the same. Now, finches from different islands are completely different species, because they’ve changed over long periods of time to adapt to their surroundings. The same goes for the giant tortoises found on different islands. We’ll talk more about Galapagos animals soon!

The Galapagos are a group of around 20 islands located far off the shore of Ecuador and home to an astonishingly beautiful and diverse collection of landscapes, flora and wildlife like nowhere else on Earth. Cruising the islands, you’ll immediately be struck by just how unique each one of them is. From lush dense forests and mature mountainous landscapes of some, through to steaming volcanic peaks and otherworldly lava fields found on others. But just how did these isolated islands come to be? And what explains the captivating geological and natural diversity that we see today?

When and how were the Galapagos Islands formed?

Las Grietas “Crack”

Plate Tectonics and Volcanism

The Galapagos Islands are situated on the Nazca tectonic plate which is gradually shifting towards the South American plate at the rate of around 5 cm per year. As the plates move and collide, the resulting friction creates weak spots where mantle plumes emerge from below to melt parts of the Earth’s crust. In some cases, lava reaches the surface, creating volcanoes and continuous eruptions that eventually form islands above the ocean’s surface.

Its position on the border between two plates explains the long and turbulent volcanic history of the Galapagos. In fact, the region has been subject to around 50 eruptions over the last two centuries alone. Whilst these eruptions can all too easily threaten the fragile flora and fauna of the islands, this is how new land and eventually entire islands are continually created over millennia.

Such high levels of volcanic activity, involving the repeated layering and lifting of the Earth’s surface, as created islands rising above the Pacific ocean. All of the Galapagos Islands consist of one single shield-type volcano, with the exception of the largest island Isabela, which was formed by no less than six volcanoes merging together. Most have a distinctive conical shape, along with steep slopes rising dramatically from sea level.

So tectonic plate activity explains the volcanism and island formation, but how was an entire archipelago created, and why in such a distinctive pattern?

When and how were the Galapagos Islands formed?

The lava field of Fernandina

Hot Spots and the Creation of an Archipelago

Not all tectonic plate divides are characterized by such intense volcanic activity as is found in the Galapagos. This is because the Galapagos Islands are located above “hotspots” which, as the name suggests, are particularly hot areas of the Earth’s mantle that create rising thermal plumes. These plumes easily burn and melt through the Earth’s crust, creating magma that erupts to the surface.

As the name also implies, these “hotspots” are stationary. But because the tectonic plates they are situated beneath are continually moving – however slowly – islands arise in different spots on the Earth’s surface, creating the false impression that it is the hotspots themselves that are moving.

When and how were the Galapagos Islands formed?

Geological Erosion

The Old and the New

The combination of static hot spots beneath shifting plates explains how an entire archipelago was created, as well as the distinctive landscapes and unique ecology of each island. The layout of the islands reflects the speed and direction of the tectonic plate movement. The plates are moving in an east-southeast direction like a conveyor belt, so the more easterly islands were formed first and are millions of years older than the western islands. The Galapagos hot spot is located in the north-western part of the archipelago. It is currently beneath Fernandina and Isabela islands, which were both formed less than a million years ago and are subject to recent volcanic activity.

Eastern islands (including Genovesa, Floreana, San Cristobal, and Espanola) have had more time to develop vegetation and are therefore much more verdant than those to the west (such as Isabela, Santiago, and Bartolome) that are rockier, barer, and more otherworldly by comparison. The more easterly islands are also smaller and some have even been partially or completely lost under the ocean through erosion by the sea. Meanwhile, the younger islands to the West are larger because they have witnessed volcanic eruptions much more recently, including up to the present day.

The stunning Galapagos are not only well worth visiting for their world-famous flora and fauna, which makes them the perfect destination for vacations. The formation and evolution of these islands over millions of years is a fascinating microcosm of the Earth’s internal geological processes, as well as a testament to the awe-inspiring power and beauty that results. Read our previous blog post to find out Who Discovered the Galapagos Islands. For more information about booking a Galapagos Tour, contact us or call 1-888-215-3555.

How was Galapagos Islands formed?

Geologic History Galapagos is located on the Nazca tectonic plate. This perpetually moving plate is heading eastward over the Galapagos hot spot and has formed the chain of islands. The islands were formed through the layering and lifting of repeated volcanic action.

How long ago did the Galapagos Islands form?

The majority of the islands were formed less than one million years ago. The most recently formed island is Fernandina, which is about 500,000 years old, making it the nearest island to the Galápagos Hot Spot. Since Fernandina is still very young its volcano has recently erupted. An eruption took place in 1998.

What is the history of the Galapagos Islands?

Galapagos Islands Discovery The Galapagos Islands were discovered in 1535 when father Tomas Berlanga, the bishop of Panama sailed to Peru to settle a dispute between Francisco Pizarro and his lieutenants after the conquest of the Incas. The bishop's ship stalled strong currents carried him out to the Galapagos.

What type of plate boundary is the Galapagos Islands?

The Galapagos Rise is a divergent boundary located between the South American coast and the triple junction of the Nazca Plate, the Cocos Plate, and the Pacific Plate. The volcanically active Galapagos Islands exist on the Galápagos hotspot above the Galapagos Rise.