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Lehmann discontinuity

Lehmann discontinuity

Geologic boundary.

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  1. Inge Lehmann

    Danish seismologist (1888–1993).

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    Highly viscous, ductile, and mechanically weak region of Earth's mantle.

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    Level representing a mechanical difference between layers in Earth's inner structure.

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    In geometry, property of being directionally dependent.

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Readers come from

Share of the 579 readers arriving from another article

  1. Inge Lehmann

    Danish seismologist (1888–1993).

    34%

  2. Mohorovičić discontinuity

    Boundary between the Earth's crust and the mantle.

    31%

  3. Internal structure of Earth

    11%

  4. Earth's outer core

    Fluid layer between Earth's solid inner core and its mantle.

    8.6%

  5. Earth's inner core

    Innermost part of Earth, a solid ball of iron-nickel alloy.

    8.5%

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