Super W
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1916 Florida Gators football team
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Davey Dodds
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abstract: David "Davey" Dodds (1 March 1971 – 20 August 2017) was a professional English darts player who played in Professional Darts Corporation events. He qualified for the 2012 UK Open, but was on the wrong end of a nine darter by Gary Anderson. Dodds secured a two-year PDC Tour Card at Q-School in 2014, by finishing 16th on the Order of Merit. Dodds passed away on 20 August 2017, at the age of 46.
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BirdValiant
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Tom.Reding
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List of urban local bodies in Telangana
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Ted Lasso
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Ekkehard von Kuenssberg
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Promising Young Woman
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Hebrides
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Electric Reliability Council of Texas
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Sparta, Laconia
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Moonraker
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Beverly B. Martin
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Plate tectonics
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abstract: Plate tectonics (from the Late Latin: tectonicus, from the Ancient Greek: τεκτονικός, lit. 'pertaining to building') is a scientific theory describing the large-scale motion of plates of Earth's lithosphere since tectonic processes began on Earth between 3.3 and 3.5 billion years ago. The model builds on the concept of continental drift, an idea developed during the first decades of the 20th century. The geoscientific community accepted plate-tectonic theory after seafloor spreading was validated in the late 1950s and early 1960s. The lithosphere, which is the rigid outermost shell of a planet (the crust and upper mantle), is broken into tectonic plates. The Earth's lithosphere is composed of seven or eight major plates (depending on how they are defined) and many minor plates. Where the plates meet, their relative motion determines the type of boundary: convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries (or faults). The relative movement of the plates typically ranges from zero to 100 mm annually. Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction, or one plate moving under another, carries the edge of the lower one down into the mantle; the area of material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total geoid surface area of the lithosphere remains constant. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories, since disproven, proposed gradual shrinking (contraction) or gradual expansion of the globe. Tectonic plates are able to move because the Earth's lithosphere has greater mechanical strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection; that is, the slow cre[cell cut: 2715 characters, first 2000 kept]
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comment: Plate tectonics (from the Late Latin: tectonicus, from the Ancient Greek: τεκτονικός, lit. 'pertaining to building') is a scientific theory describing the large-scale motion of plates of Earth's lithosphere since tectonic processes began on Earth between 3.3 and 3.5 billion years ago. The model builds on the concept of continental drift, an idea developed during the first decades of the 20th century. The geoscientific community accepted plate-tectonic theory after seafloor spreading was validated in the late 1950s and early 1960s.

Rodw
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Battle of Arakere
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KingSkyLord
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Bender the Bot
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