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📘 Guam, before sunrise

Before dawn on 23 January 1960, Trieste waited in rough Pacific water off Guam. Jacques Piccard and Don Walsh were about to enter a steel sphere and let the ocean carry them toward Challenger Deep — a depth no human had reached.

3
lessons
~15 min
to learn
Adults
level
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What you’ll learn

  1. Building a vehicle for the abyssExplain how buoyancy, ballast, and a spherical pressure vessel made Trieste's dive possible.A bathyscaphe separated the problem of floating from the problem of surviving pressure.
  2. The descent and the decisionTrace Project Nekton's preparation, the descent, the crack, and the brief stay on the seafloor.The record was a chain of tests and judgments made inside a machine that could not be quickly rescued.
  3. What the first descent changedAssess what Trieste proved, what it could not do, and why measurement and observation still matter.Reaching Challenger Deep turned an unreachable boundary into a destination for future ocean science.

Questions this course answers

Why did Trieste use aviation gasoline in its large float?

The gasoline displaced seawater to provide lift and remained comparatively incompressible at depth.

What happened at about 32,400 feet?

A shudder and crack were later associated with a temperature-related crack in the free-flooded entrance tube's viewing port.

Why was the stay on the seafloor shorter than planned?

Sediment raised by the vehicle clouded the observation area after about twenty minutes.

Why did the original depth reading change?

Later calculations corrected the gauge's 37,800-foot reading to roughly 35,797 feet.

What lasting change did Trieste help demonstrate?

The dive proved human-rated vehicles could reach and return from Challenger Deep, opening a path for later deep-ocean exploration.

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