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  2. South Pole - Wikipedia

    en.wikipedia.org/wiki/South_Pole

    The South Pole is at an altitude of 9,200 feet (2,800 m) but feels like 11,000 feet (3,400 m). [34] Centripetal force from the spin of the planet throws the atmosphere toward the equator. The South Pole is colder than the North Pole primarily because of the elevation difference and for being in the middle of a continent. [35]

  3. Amundsen's South Pole expedition - Wikipedia

    en.wikipedia.org/wiki/Amundsen's_South_Pole...

    The first ever expedition to reach the Geographic South Pole was led by the Norwegian explorer Roald Amundsen. He and four other crew members made it to the geographical south pole on 14 December 1911, [n 1] which would prove to be five weeks ahead of the competitive British party led by Robert Falcon Scott as part of the Terra Nova Expedition ...

  4. Vine–Matthews–Morley hypothesis - Wikipedia

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

    Magnetic anomalies off west coast of North America. Dashed lines are spreading centers on mid-ocean ridges. The Vine–Matthews-Morley hypothesis correlates the symmetric magnetic patterns seen on the seafloor with geomagnetic field reversals. At mid-ocean ridges, new crust is created by the injection, extrusion, and solidification of magma.

  5. Harry Hammond Hess - Wikipedia

    en.wikipedia.org/wiki/Harry_Hammond_Hess

    In 1960, Hess made his single most important contribution, which is regarded as part of the major advance in geologic science of the 20th century. In a widely circulated report to the Office of Naval Research , he advanced the theory, now generally accepted, that the Earth's crust moved laterally away from long, volcanically active oceanic ridges .

  6. Plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Plate_tectonics

    Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.

  7. Earth's magnetic field - Wikipedia

    en.wikipedia.org/wiki/Earth's_magnetic_field

    As an approximation, it is represented by a field of a magnetic dipole currently tilted at an angle of about 11° with respect to Earth's rotational axis, as if there were an enormous bar magnet placed at that angle through the center of Earth. The North geomagnetic pole (Ellesmere Island, Nunavut, Canada) actually represents the South pole of ...

  8. Phantom of the Poles - Wikipedia

    en.wikipedia.org/wiki/Phantom_of_the_Poles

    This would have invalidated Reed's premise that the poles cannot be reached. Although Peary's claim was, in its day, and continues to be controversial, on December 14, 1911, Roald Amundsen undisputedly reached the South Pole. Subsequent expeditions to and flights over the south pole have conclusively demonstrated that there are no large holes ...

  9. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    Each boundary type is associated with different geological marine features. Divergent plates are the cause for mid-ocean ridge systems while convergent plates are responsible for subduction zones and the creation of deep ocean trenches. Transform boundaries cause earthquakes, displacement of rock, and crustal deformation. [8] [27] [26] [28]