Look at a map. Any map. Usually, you’ll see the Canary Islands tucked into a tiny little box in the corner of a map of Spain, right next to the Balearics. It’s misleading. Honestly, it drives locals crazy because it makes these islands look like they’re floating somewhere off the coast of Valencia. They aren't. If you look at a real, unedited map of Canary Islands, you’ll see they are geographically part of Africa, sitting roughly 100 kilometers off the coast of Morocco and the Western Sahara.
They are volcanic. They are rugged. And they are way more spread out than most people realize.
When you’re planning a trip, the map is your best friend, but only if you know how to read between the lines. We’re talking about an archipelago shaped by the "hotspot" theory—the same geological quirk that built Hawaii. As the African tectonic plate drifted slowly northeast, a stationary magma plume under the Earth’s crust punched through, creating islands one by one. This is why the map looks like a chronological timeline. The islands to the east, like Fuerteventura and Lanzarote, are the old souls. They’ve been eroded by wind and time for over 20 million years, leaving them flat and desert-like. Move west toward La Palma and El Hierro, and you’re looking at the "babies" of the family—steep, jagged, and still very much active. Just ask anyone who watched the Cumbre Vieja eruption in 2021.
The East-West Divide on the Map of Canary Islands
If you draw a vertical line down the center of the map of Canary Islands, you’re basically splitting two different worlds. To the east, you have the sun-scorched landscapes. Fuerteventura and Lanzarote feel like Mars met the Sahara. Because they lack high mountains, they don't trap the trade winds' moisture. The result? Endless dunes and volcanic plains.
Then you have the western islands.
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Tenerife, Gran Canaria, La Palma, La Gomera, and El Hierro. These are the giants. Because they have massive central peaks—Teide on Tenerife is the highest point in all of Spain at 3,715 meters—they create their own weather. The "Mar de Nubes" or sea of clouds happens when the moisture-rich Alisios winds hit these mountains. The north stays lush and green; the south stays dry and sunny. If you're looking at a map and wondering why one side of an island looks like a rainforest and the other looks like Arizona, that's why.
It’s about microclimates. You can literally drive from a pine forest into a desert in forty-five minutes.
Why Scale Matters More Than You Think
People look at the distance between islands on a map and think, "Oh, I’ll just hop over for lunch."
Don't do that.
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While Fred Olsen and Armas ferries are fast, the Atlantic isn't a lake. The "Canary Current" is a powerful thing. Between the islands, the wind gets funneled and accelerated—a phenomenon known as the Venturi effect. This is great news for windsurfers in Pozo Izquierdo (Gran Canaria) but can make for a bumpy boat ride for the unprepared.
- Lanzarote: The northernmost and easternmost. It’s defined by Timanfaya National Park. The map shows a pockmarked landscape of craters.
- Fuerteventura: Just south of Lanzarote. It’s the second-largest island but has the lowest population density. Look for the "Jandía" peninsula on the bottom—it’s basically one giant beach.
- Gran Canaria: Often called a "miniature continent." The map reveals a circular shape with deep ravines (barrancos) radiating out from the center like spokes on a wheel.
- Tenerife: The big one. The central feature is the massive caldera of Las Cañadas.
- La Gomera: Almost perfectly circular but incredibly rugged. There are no highways circling the island because the terrain is too steep.
- La Palma: Shaped like a heart or a flint axe. The "Caldera de Taburiente" dominates the northern half.
- El Hierro: The smallest of the main seven. It’s the edge of the world—or at least it was until Columbus sailed past it.
Navigation and the "Eighth" Island
Look closely at the north of Lanzarote on a high-resolution map of Canary Islands. You’ll spot a tiny speck of land. That’s La Graciosa. It only recently became officially recognized as the eighth inhabited island. There are no paved roads there. Just sand. If you want to disappear, that’s where you go.
But the map is changing. Not just because of politics, but because of the ocean floor. To the southwest of El Hierro, there are underwater volcanoes that might one day break the surface. We are watching the birth of new islands in slow motion. The 2011 underwater eruption at La Restinga almost gave us a ninth island. It stopped just a few meters short of the surface.
Practical Insights for Your Trip
Stop using Google Maps as your only guide for hiking. The terrain here is vertical. A two-kilometer walk on a flat map can be a grueling 600-meter vertical ascent in reality. Use OpenStreetMap or specialized topographical maps like those provided by Instituto Geográfico Nacional (IGN).
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Check the "Calima" forecasts. Occasionally, a weather pattern blows dust from the Sahara over the islands. On a map, you can see this massive yellow plume swallowing the archipelago. When this happens, visibility drops and temperatures spike. It's not the time for a long hike in the midlands.
If you’re driving in Gran Canaria or Tenerife, ignore the "estimated time" on your GPS. The roads are "carreteras de montaña"—winding, narrow, and often hair-raising. A distance that looks like 20 minutes on a map will take you an hour. Local drivers are fast; tourists are slow. Be the polite tourist and pull over to let the locals pass.
Understand the ferry hubs. You can't easily get from Lanzarote to La Palma in a straight line. The map of ferry routes usually funnels through the "central" islands. Usually, you’ll have to go Lanzarote -> Gran Canaria -> Tenerife -> La Palma. It’s often easier and faster to take a "Binter" or "Canaryfly" prop plane. These short flights are basically the bus system of the islands. Seeing the archipelago from 10,000 feet gives you a perspective the map never can—you see the turquoise fringes of the reefs and the stark contrast of the volcanic rock against the deep Atlantic blue.
Next Steps for Your Journey:
Download the Offline Maps for the specific island you are visiting, as signal drops to zero the moment you enter a volcanic ravine. Locate the nearest Centro de Visitantes (Visitor Center) upon arrival; they provide physical topographical maps that highlight "senderos" (trails) which are often more accurate than digital versions for mountainous terrain. If you're planning on inter-island travel, check the Naviera Armas or Fred Olsen websites to see which ports (like Los Cristianos vs. Santa Cruz) actually connect to your next destination, as using the wrong port can add three hours to your travel day.