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  2. Vine–Matthews–Morley hypothesis - Wikipedia

    en.wikipedia.org/wiki/Vine–Matthews–Morley...

    Marine magnetic anomalies were found later to span the vast flanks of the ridges. [9] Drillcores into the crust on these ridge flanks allowed dating of the early and of the older anomalies. This in turn allowed design of a predicted geomagnetic time scale. [ 9 ]

  3. 50 Times People Found Such Strange Things On Google ... - AOL

    www.aol.com/76-times-people-found-strange...

    One place where you can do this is the popular ‘Google Earth, Structures and Anomalies’ group on Fa 50 Times People Found Such Strange Things On Google Earth, They Had To Share Them (New Pics)

  4. Seafloor spreading - Wikipedia

    en.wikipedia.org/wiki/Seafloor_spreading

    In the 1960s, the past record of geomagnetic reversals of Earth's magnetic field was noticed by observing magnetic stripe "anomalies" on the ocean floor. [9] [10] This results in broadly evident "stripes" from which the past magnetic field polarity can be inferred from data gathered with a magnetometer towed on the sea surface or from an ...

  5. Geomagnetic reversal - Wikipedia

    en.wikipedia.org/wiki/Geomagnetic_reversal

    Through analysis of seafloor magnetic anomalies and dating of reversal sequences on land, paleomagnetists have been developing a Geomagnetic Polarity Time Scale. The current time scale contains 184 polarity intervals in the last 83 million years (and therefore 183 reversals). [9] [10]

  6. Paleomagnetism - Wikipedia

    en.wikipedia.org/wiki/Paleomagnetism

    Apparent polar wander paths provided the first clear geophysical evidence for continental drift, while marine magnetic anomalies did the same for seafloor spreading. Paleomagnetic data continues to extend the history of plate tectonics back in time, constraining the ancient position and movement of continents and continental fragments ( terranes ).

  7. Seafloor depth versus age - Wikipedia

    en.wikipedia.org/wiki/Seafloor_depth_versus_age

    The depth of the seafloor on the flanks of a mid-ocean ridge is determined mainly by the age of the oceanic lithosphere; older seafloor is deeper.During seafloor spreading, lithosphere and mantle cooling, contraction, and isostatic adjustment with age cause seafloor deepening.

  8. Mid-ocean ridge - Wikipedia

    en.wikipedia.org/wiki/Mid-ocean_ridge

    Mid-ocean ridge cross-section (cut-away view) A mid-ocean ridge (MOR) is a seafloor mountain system formed by plate tectonics.It typically has a depth of about 2,600 meters (8,500 ft) and rises about 2,000 meters (6,600 ft) above the deepest portion of an ocean basin.

  9. List of reportedly haunted locations - Wikipedia

    en.wikipedia.org/wiki/List_of_reportedly_haunted...

    The Joelma Building (now the Praça da Bandeira Building) in São Paulo is allegedly haunted by victims of the fire that started on 1 February 1974, after an air conditioning unit on the twelfth floor overheated; centered on the "Mystery of the Thirteen Souls", individuals who died within an elevator as they were trying to escape the fire, and ...