Where does a volcano begin?

Where does a volcano begin?

Mauna Loa doesn't stop at the shoreline—or even at the seafloor.

≈4.17 km above sea level · about 17 km from geological base to summit

Its weight has pushed the seafloor down beneath it.

Depends on the measurement reference

Why this is interesting

The part of Mauna Loa you can see is only the top of the volcano.

USGS describes its flanks continuing about 5,000 m below sea level to the seafloor. Below that, the volcano's enormous weight has pressed the seafloor down by roughly another 8,000 m. Measure from that true base, and Mauna Loa is about 17 km tall.

How this measurement works

Mauna Loa's elevation — its summit above sea level — is about 4,170 m.

The 17 km figure is something different: total relief from the volcano's geological base to its summit. It is not an elevation.

The extra depth comes from crustal depression (geologists also call it isostatic loading). A sufficiently massive volcano pushes down the crust beneath it, so its structure extends below the ordinary seafloor. USGS seismologists found the boundary beneath the crust bowed downward by as much as 8 km under Mauna Loa.

That makes 17 km an approximate geological figure, not a surveyed one.

See the math

Summit above sea level
≈4,170 mSource value
Flanks below sea level to the seafloor
≈5,000 mSource value
Seafloor depressed beneath the volcano
≈8,000 mSource value
Inferred from seismic studies
Total
4,170 + 5,000 + 8,000 ≈ 17,170 mCalculated
Published
about 17 km from geological baseResult
Approximate — not an elevation

How certain is this?

Authoritative approximate geological reference. USGS gives about 17,170 m from true base to summit; the depressed-seafloor portion is inferred from seismic studies, so treat it as approximate.

The ~17 km figure includes geological structure below the seafloor and must not be represented as summit elevation. The geological base-to-summit display value is approximate.

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