When a mountain becomes a volume problem

When a mountain becomes a volume problem

The 1980 Mount St. Helens landslide was about a million Olympic pools of debris.

≈2.5 km³ ≈ 1 million Olympic-pool reference volumes

USGS puts the debris avalanche at about 2.5 km³.

Approximate calculated comparison

Why this is interesting

The 1980 eruption didn't just make Mount St. Helens shorter. The collapsed summit and north side became an enormous debris avalanche — that's part of where the missing mountain went.

How this measurement works

USGS gives the total avalanche volume as about 2.5 km³ (3.3 billion cubic yards), and itself compares that with about 1 million Olympic swimming pools.

Our own Olympic-pool reference is 2,500 m³, which gives the same answer: 2.5 km³ is 2.5 billion m³, divided by 2,500 m³ is about 1 million.

This is a volume comparison. No pools held the debris, and real Olympic pools don't all hold the same amount of water.

See the math

Debris avalanche volume
≈2.5 km³Source value
USGS estimate
In cubic metres
2,500,000,000 m³Calculated
Olympic-pool reference
2,500 m³Reference value
Scaleidoscope's 50 × 25 × 2 m reference
Pools
2,500,000,000 ÷ 2,500 = 1,000,000Calculated
Published
≈1 million reference poolsResult
Matches USGS's own comparison

How certain is this?

Approximate calculated comparison. 2.5 km³ is a USGS estimate, and the Olympic pool is a stated reference volume rather than one fixed real-world amount.

USGS gives the debris avalanche as approximately 2.5 km³; the displayed result is rounded.

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