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Tuesday, 22 September 2026 · PlanetaryFormation.com

Two scars

Valles Marineris is a rift beside that rise.

Mars

Valles is a rift beside a rise. Mariana is a trench.

Valles Marineris runs about 4,000 kilometres east of Tharsis. Typical width is about 200 kilometres; locally it opens toward 600. Usual depth is about 7 kilometres; some walls drop near 10. Mariana is shorter, narrower, and deeper. Challenger Deep is about 10.94 kilometres. As a fraction of each planet’s radius the two scars are close. As factories they are not.

One is a rift beside a plume load. The other is a slab going down. Earth’s nearest living match is a rift beside a swell — East Africa, not the Andes.

This site reads Io through Mars as consecutive stages of one kind of planet, with living Earth as the present chapter. A crack of this length next to that load is what a stagnant lid does when the rise is too heavy. The missions do not prove the handoff.

Figure 1. Valles Marineris east of Tharsis. Image: NASA / MOLA context.

The ordinary view

The usual reading ties the trough to the load of Tharsis: the bulge flexed the crust and the canyon opened as a rift, later widened by collapse and landslides. Yin and others have also read strike-slip. Nothing below voids those papers. The comparison here is only scale and factory.

What was measured

Valles MarinerisMariana Trench
Length~4,000 km~2,550 km
Typical width~200 km (locally to ~600)~69 km
Maximum depth~7 km usual; up to ~10 km~10.94 km (Challenger Deep)
Share of the world’s girth~19% of Mars~6% of Earth
What it isRift east of TharsisSubduction trench
Table 1. Valles is longer and wider. Mariana is deeper and steeper. One is a rift. The other is a trench.
RatioVallesMariana
Depth / length (at 7 km for Valles)1 in 5701 in 233
Depth / length (at 10 km for Valles)1 in 4001 in 233
Depth / planetary radius~0.21%~0.17%
Table 2. Depth against length favours Mariana. Depth against planetary radius is close.
Earth featureWhy it is closer than MarianaWhy it is still not Valles
East African Rift / AfarCrack beside a plume swellUsually 1–2 km deep; a family of rifts
Dead Sea TransformStrike-slip and pull-apart basins~1,000 km; a fault zone, not a canyon
Baikal RiftDeepest open continental riftHundreds of km, not thousands
Red Sea / Gulf of AdenA rift after it goes to oceanAlready a young sea, not an open land trough

Table 3. Earth’s nearer cousins are rifts beside swells. Mariana is the wrong factory.

What would move a clock

Table 4. Collapse-only Valles, or a subduction trench along the same line, would take the rift-beside-rise reading off the table.
RowWhat would move itWhat would not
Rift beside TharsisMostly collapse and erosion, little tectonic openingA new name for the same trough
Depth-to-radius coincidenceA new map that puts maximum depth near 3 kmChoosing 7 km vs 10 km inside the same trough
Not a trenchMariana-style subduction along VallesEast Africa remaining the closer living cousin

On this reading

This site reads Mars as the last window before living Earth. A lid that does not walk can keep a volcanic load the size of a small continent. A crack of this length next to that load is what that lid does. Earth later adds ocean floor and moving plates. Some rifts become edges. That is lid behaviour.

What would weaken this

If Valles is shown to be mostly collapse and erosion with little tectonic opening, the rift analog shrinks. If a new map puts maximum depth near 3 kilometres, the depth-to-radius coincidence with Mariana goes away. If Mariana-style subduction is demonstrated along the trough, the factory changes. Neither result would prove a handoff.

What this page holds

Valles is longer and wider. Mariana is deeper and steeper. As a fraction of each planet they are close. One is a rift beside Tharsis. The other is a slab going down. This site reads that as lid behaviour on consecutive stages. The missions do not prove the handoff.

Sources

NASA Science; ESA Mars Express. Valles dimensions and the Tharsis-adjacent rift reading.

Challenger Deep compilations (GEBCO; 2021 acoustic/pressure). Mariana length ~2,550 km; depth ~10,935 m.

Yin, A. (2012). Strike-slip reading of Valles compared with the Dead Sea fault system.

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