Mars Regions Alba Mons
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Alba Mons

The widest volcano in the solar system — flat as a shield, vast as a nation.

Alba Mons sprawls roughly 1,600 km across the northern edge of the Tharsis rise, dwarfing every other volcano in footprint. Yet it stands only about 6.5 km tall, so its flanks slope by mere fractions of a degree.

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40.5°N · 109.6°W · Alba Mons
Key facts

Alba Mons at a glance

Width
~1,600 km
largest volcano by area, solar system
Height
~6.5 km
very low, gentle profile
Slope
<1°
almost imperceptibly flat flanks
Type
Low shield volcano
Formed
Hesperian, ~3.5 billion yrs
Location
North of Tharsis
The story

How Alba Mons came to be

Alba Mons is a volcanic giant unlike any other. While Olympus Mons is famous for height, Alba wins on sheer spread — its lava flows and fracture systems reach some 1,600 km end to end, an area larger than that of any terrestrial volcano. Its extreme flatness likely reflects very fluid, low-viscosity lava and possibly eruptions influenced by ground ice.

The mountain is ringed by concentric fractures and graben, including the Alba Fossae and Tantalus Fossae, carved as the crust flexed under the load and stress of the Tharsis bulge. Long, branching lava channels lace its flanks, recording repeated effusive eruptions over hundreds of millions of years during the Hesperian period.

Put it in perspective

Just how big is it?

vs Olympus Mons

Olympus is far taller, but Alba covers a much larger area — a low dome the size of the western United States.

vs Earth volcanoes

No volcano on Earth comes close in footprint; Alba's spread would blanket a large European country.

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FAQ

Alba Mons, answered

Is Alba Mons the biggest volcano on Mars?
By surface area, yes — it is the largest volcanic construct on Mars and the solar system. Olympus Mons is taller, but Alba is far wider.
Why is Alba Mons so flat?
Its very low slopes came from highly fluid lava spreading over great distances, possibly aided by interaction with ground ice.
How old is Alba Mons?
It formed mainly in the Hesperian period, roughly 3.5 billion years ago, north of the main Tharsis volcanoes.
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