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An icebreaker doesn’t smash through ice. It bends it until it snaps. Sea ice is strong in compression and weak in flexure. Crushing a metre-thick floe head-on demands several megapascals; bending the same sheet until it fractures takes roughly 0.5 MPa. Every line of an icebreaker’s hull exists to exploit that asymmetry. The bow does the work. Where a cargo ship has a near-vertical stem, an icebreaker’s is raked to around 20–30 degrees from horizontal. Driven forward, the hull climbs onto the ice sheet and the ship’s own weight becomes the tool. Thousands of tonnes bear down on the unsupported edge until it fails in bending, throwing out radial and circumferential cracks. The broken floes then roll under the flared sides and are pushed beneath the surrounding sheet. Staying unstuck is the harder problem: - An ice belt of high-tensile plating, up to 50 mm thick, in alloys selected for fracture toughness at −40 °C, because ordinary ship steel turns brittle in the cold - Low-friction e...

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