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Posted on April 26, 2022 (Updated on July 24, 2025)

Where is the Valles Marineris?

Space & Navigation

Valles Marineris: Mars’s Jaw-Dropping Grand Canyon (Times a Thousand!)

Location, Location, Location (and Size!)

You’ll find Valles Marineris hanging out near the Martian equator, just east of this massive bulge called Tharsis. But let’s talk scale. This isn’t just a crack in the ground; it’s a planetary-scale scar. Over 4,000 kilometers long (that’s 2,500 miles for us here on Earth), and in some spots, it’s a whopping 200 kilometers (120 miles) wide! And the depth? Forget about it! We’re talking down to 10 kilometers (6 miles) deep. I mean, you could practically lose a mountain in there.

It all starts with this crazy, maze-like area called Noctis Labyrinthus in the west. Then, it carves its way eastward through a series of mind-boggling canyons – Tithonium, Ius, Melas, Candor, Ophir, Coprates, Ganges, Capri, Eos… try saying that five times fast! Finally, it spills out into a chaotic mess of terrain and eventually empties into the Chryse Planitia basin. It’s like Mars’s version of a river delta, only instead of water, it’s… well, we’re not entirely sure what carved it!

Grand Canyon? More Like “Tiny Canyon”!

Seriously, let’s put this in perspective. The Grand Canyon is impressive, no doubt. I’ve been there, hiked it, loved it. But it’s a baby compared to Valles Marineris. The Grand Canyon clocks in at about 800 kilometers long, 30 kilometers wide, and a measly 1.6 kilometers deep. Valles Marineris? Almost ten times the length, twenty times the width, and five times the depth. It’s like comparing a kiddie pool to the Pacific Ocean.

How Did This Monster Form?

So, how did this colossal canyon come to be? The leading theory points to the Tharsis Bulge, that huge volcanic region I mentioned earlier. Imagine pumping a ton of molten rock into one area of the planet. The crust gets stressed, right? It cracks and fractures. That’s basically what happened with Valles Marineris.

Most scientists think it started as a tectonic feature – a giant crack caused by the strain from the Tharsis Bulge. Then, over billions of years, erosion widened the crack. Maybe water played a role, or even carbon dioxide. Some researchers even think there might have been lakes hiding down in those canyons at some point! You see layered materials on the canyon floors, which could have formed when the canyons were filled with water.

Why Should We Care?

Valles Marineris isn’t just a pretty (or, well, dramatically scarred) face. It’s a treasure trove of Martian history. Those canyon walls expose layers of rock that go back billions of years, giving us clues about how Mars evolved. And, because we’ve found evidence of past water activity, there’s even a chance that life might have once existed down there. Plus, the canyon floor offers some advantages for future Martian settlements – relatively higher air pressure and some protection from radiation. So, yeah, Valles Marineris is kind of a big deal. It’s a place that could unlock secrets about Mars’s past, and maybe even its future.

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