The Largest Mountains and Canyons in the Solar System

Largest Mountains and Canyons in the Solar System

Earth’s landmarks are dwarfed by the staggering scale of the Solar System’s megastructures. From the 13-mile high peaks of Olympus Mons on Mars to the 2,500-mile long chasm of Valles Marineris, the geometry of other worlds defies terrestrial logic. Use our Landmark Scale Simulator below to compare Earth’s greatest wonders against the true giants of the cosmos.

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Coordinates Mars
Scale Metric 13.6 MI
Earth Factor 2.5x

Geological Intelligence Archive

Tactical Reconnaissance of the Solar System’s Greatest Megastructures

Volcanic Giant
TARGET_ID: MARS_VOL_01

Olympus Mons

Standing at a staggering 13.6 miles high, Olympus Mons is the undisputed king of volcanoes, towering nearly three times higher than Mt. Everest.

Visual Paradox: The volcano is so massive and its slope so gentle that if you were standing on its peak, you wouldn’t know you were on a mountain—the base would be hidden far beyond the Martian horizon.

The Arizona Baseline

The base of Olympus Mons is roughly 370 miles wide. That is the same size as the entire state of Arizona, or the distance from London to Germany.

Atmospheric Piercing

The peak of the volcano is so high that it sits above 80% of the Martian atmosphere, reaching into the thin vacuum where the sky turns black.

Gravity Efficiency

Mars’s lower gravity (38% of Earth’s) is what allows these structures to grow so massive without collapsing under their own immense weight.

Static Crust Physics

Unlike Earth’s volcanoes which shift due to plate tectonics, Mars has a static crust. A single lava vent can erupt in the same spot for billions of years.
Continental Chasm
TARGET_ID: MARS_CAN_02

Valles Marineris

The Grand Canyon of Mars is a 2,500-mile long tectonic crack that would stretch from New York City to Los Angeles if placed on Earth.

Scale Comparison: The entire Grand Canyon of Arizona could fit inside just one small “side valley” of the Valles Marineris system.

Vertical Extremes

The walls of the canyon drop up to 23,000 feet (4.3 miles). That is four times deeper than the Grand Canyon’s deepest point.

Tectonic Origin

Unlike Earth’s canyons carved by water, this chasm was formed by the planet’s crust literally ripping open as the nearby Tharsis volcanoes grew.

Atmospheric Traps

The canyon is so deep that it often traps water-ice clouds in its floor, creating a visible “river” of white mist in satellite photos.

The Width Mystery

In some sectors, the canyon is 120 miles wide. From the center of the floor, you wouldn’t even be able to see the walls in either direction.
The Long Fall
TARGET_ID: MIRANDA_CLI_03

Verona Rupes

Located on Uranus’s moon Miranda, Verona Rupes is the highest cliff in the solar system—a vertical drop of 12 miles straight down into the void.

Physics Warning: Because Miranda has such low gravity, if you jumped off the top of this cliff, it would take you roughly 12 minutes to reach the bottom.

Impact Reconstruction

Scientists believe Miranda was once shattered by a massive impact and then pulled back together by gravity, creating these chaotic cliffs.

Terminal Velocity

Even with the 12-minute fall time, you would be traveling at over 120 mph when you hit the surface. Air resistance cannot slow you down.

Scarp Height

The cliff face is so high that it is ten times taller than the walls of the Grand Canyon and higher than Mt. Everest’s peak.

Observation Status

We have only seen this structure once, when Voyager 2 flew past Uranus in 1986. Most of the cliff remains unmapped.
04
TARGET_ID: VENUS_MTN_04

Rhea Mons

Rising 4.3 miles from the toxic plains of Venus, Rhea Mons is a massive shield volcano similar in footprint to the island of Hawaii.

Lethal Ascent: While nearly as high as Mt. Everest, a human could never climb it; the 900°F heat and crushing atmospheric pressure would melt a spacesuit.

Acid Weathering

The rock of Rhea Mons is constantly bathed in sulfuric acid mist, creating a landscape that is chemically unlike anything on Earth.

Radar Mapping

We only know the height of this peak because of the Magellan mission, which used radar to “see” through the planet’s opaque clouds.

Tectonic Armor

Venus lacks plate tectonics, meaning its mountains are formed by “blobs” of hot magma pushing the crust upward into huge shields.

Atmospheric Weight

Standing at the base of Rhea Mons, the air is so thick it would feel like walking through water, with pressure 90 times higher than Earth.
05
TARGET_ID: CERES_CRY_05

Ahuna Mons

Rising 2.5 miles from the surface of the dwarf planet Ceres, Ahuna Mons is a “Cryovolcano” that erupts muddy ice instead of molten rock.

Solar System Outlier: This is the only world in the inner solar system where we have confirmed the presence of an active ice volcano.

Cryolava Composition

The “lava” from Ahuna Mons is a mix of water ice and salts like sodium carbonate. It flows like thick, salty slush before freezing solid.

Young Surface

Ahuna Mons is estimated to be only 200 million years old—geologically “new” compared to the 4.5 billion-year-old surface of Ceres.

Internal Heating

The existence of this mountain proves that Ceres was geologically active in the recent past, likely possessing a warm, briny interior.

Dwarf Scale

While only half the height of Everest, Ahuna Mons is massive relative to its parent world—it would be like having a 50-mile high mountain on Earth.

Planetary Geography FAQ

DATA_ID: MARS_VOL_MAX 🌋 What is the largest volcano in the solar system?
The largest volcano in the solar system is Olympus Mons on Mars. It stands at a massive 13.6 miles (22 km) high and spans roughly 370 miles (600 km) in diameter. For comparison, it is nearly three times taller than Mount Everest and roughly the size of the state of Arizona.
DATA_ID: MARS_CAN_MAX 🏜️ What is the longest canyon in the solar system?
Valles Marineris on Mars is the longest canyon system in the solar system. Stretching over 2,500 miles (4,000 km) long and reaching depths of 4.3 miles (7 km), it is ten times longer and four times deeper than Earth’s Grand Canyon.
DATA_ID: CLIFF_MAX 🧗 What is the highest cliff in the solar system?
The highest cliff in the solar system is Verona Rupes, located on Uranus’s moon, Miranda. It features a vertical drop of approximately 12 miles (20 km). Due to the moon’s extremely low gravity, a human would take roughly 12 minutes to fall from the top to the bottom.
DATA_ID: SCALE_PHYSICS 🏔️ Why are mountains on Mars so much bigger than on Earth?
Mountains on Mars grow much larger than those on Earth due to lower surface gravity and a lack of plate tectonics. Mars has only 38% of Earth’s gravity, meaning the planet’s crust can support more weight. Furthermore, the Martian crust is stationary, allowing lava to build up in one spot for billions of years.
DATA_ID: VENUS_MTN ☁️ Are there mountains on Venus?
Yes, Venus has massive mountains, with the highest being Maxwell Montes. Rising nearly 7 miles (11 km) above the surface, it is taller than Mount Everest. Another major peak is Rhea Mons, a shield volcano that stands 4.3 miles high.
DATA_ID: ICE_VOLCANO ❄️ What is a cryovolcano?
A cryovolcano (or ice volcano) is a structure that erupts volatiles such as water, ammonia, or methane instead of molten rock. The most famous example in the inner solar system is Ahuna Mons on the dwarf planet Ceres, which stands 2.5 miles tall and erupts salty ice slush.
DATA_ID: DEEP_MOON 🌑 What is the largest crater on the Moon?
The largest impact feature on the Moon is the South Pole-Aitken Basin. It is approximately 1,600 miles (2,500 km) in diameter and 8 miles deep. It is one of the largest, oldest, and deepest known impact basins in the entire solar system.
DATA_ID: EARTH_BASELINE ⚖️ How does Olympus Mons compare to Mt. Everest?
Olympus Mons is 2.5 times taller than Mount Everest. While Everest rises 5.5 miles (8.8 km) above sea level, Olympus Mons towers 13.6 miles (22 km) above the Martian plains. Visually, Everest would appear as a minor foothill if placed at the base of Olympus Mons.