Mars Regions Viking 1 — Chryse
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Viking 1 — Chryse

The mission that proved Mars has weather, seasons and a story to tell.

Chryse Planitia — the "Plains of Gold" — is the broad lowland where NASA's Viking 1 became the first spacecraft to land and operate successfully on Mars in 1976. From here, Viking 1 watched Martian seasons turn and measured the composition of the thin, cold atmosphere for the first time.

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22.27°N · 49.97°W · Viking 1 — Chryse
Key facts

Viking 1 — Chryse at a glance

Region
Chryse Planitia
northern lowlands
Mission
Viking 1
orbiter + lander
Arrived
July 20, 1976
first success at Mars
Discovery
Seasonal changes
atmosphere + weather
Air
~95% CO₂
measured in situ
Terrain
Ancient flood plain
carved by water
The story

How Viking 1 — Chryse came to be

Chryse Planitia sits at the mouth of enormous outflow channels, a lowland scoured long ago by catastrophic floods of liquid water. Viking 1's cameras and weather sensors ran for years, recording daily temperature swings, wind, atmospheric pressure changes, and the seasonal ebb and flow of the Martian year — the first long-term weather record from another world.

The lander confirmed the air was almost entirely carbon dioxide, thin and frigid, and documented dust and frost cycles across the seasons. Its biology experiments searched the soil for life and returned puzzling, still-debated results. Together with its orbiter, Viking 1 transformed Mars from a telescope blur into a real, weather-driven planet.

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FAQ

Viking 1 — Chryse, answered

Where is Chryse Planitia?
It is a low, smooth plain in Mars' northern hemisphere, at the outflow of major flood channels — the Viking 1 landing region.
What did Viking 1 prove?
It confirmed Mars has seasons and daily weather, measured its carbon-dioxide atmosphere, and returned the first sustained surface data.
Why is it called the Plains of Gold?
Chryse means "golden" in Greek; the plain was named for its bright appearance, not for actual gold.
What is Chryse Planitia's terrain like?
It is an ancient flood plain, shaped by huge releases of liquid water that carved channels feeding into the lowland.
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