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Unfinished Earth History and modern continuation of planetary accretion and The Origin of Crust Earth’s Early History • • • • • Hadean Eon – Earth’s first 500 Ma Intense bombardment by bolides (meteors, comets, etc.) No permanent crust – destroyed by impacts Little direct evidence on Earth Excellent evidence on Moon, Mars and other terrestrial planets Craters on the Moon – Hadean and later bombardment Earth – the water planet Earth – the water planet • Presently, Oceans cover 71% of Earth’s surface • Odds of impact on land are 29% • Water and oxygen weather rocks and destroy evidence of impacts Crater Preservation Australian “Outback” Quebec, Canada • Arid climate is more likely to preserve craters than humid climate • Less weathering • Less erosion Location of Craters on Earth Craters in North America Gene and Carolyn Shoemaker • Gene Shoemaker, geologist • Pioneer in study of impact structures worldwide • Studied Berringer Crater, AZ • Well-respected in geology, but not in astronomy • Until Shoemaker-Levy 9! Berringer Crater, Arizona • Young impact structure • Approximately 40,000 years old • Arid climate – excellent preservation • Remnants of meteorite found in crater and in ejecta Planetary Accretion Today: Shoemaker-Levy 9 Significance of Shoemaker-Levy 9 • Convinced astronomers that such events were still possible • Focused attention on near-Earth objects • Showed how little we know of such objects • Showed how completely unprepared we are A Focus on Earth Why the Gap: 4.6 – 3.98 Ga? • Asteroids, meteorites, comets, planetesimals collide as Earth accretes to form homogeneous protoplanet • Intense bombardment during continued accretion destroyed primeval crust (if there was any) • Inertial heating from impacts and radioactive decay may have liquified the entire planet • This afforded mobility for the start of density differentiation Earth’s Layered Structure • Gravity caused Earth’s interior to differentiate into layers • Layers are arranged according to density • Most dense material sank to the center – core • Density decreases outward • Density layering includes the hydrosphere (oceans) and atmosphere Evidence for Earth’s Internal Structure • • • • • Refraction of seismic waves Density of the entire planet Gravity (mass) of entire planet Composition of meteorites Existence of magnetic field Earth: The Unfinished Planet • Earth continues to lose heat • Volcanism brings material to Earth’s surface • Other processes (subduction) return more dense material to interior • Conclusion: Earth is still under construction! Theory of Plate Tectonics • Plates move as a result of heat inside the Earth • Plates interact to cause: – Earthquakes – Volcanos – Mountain systems Earth’s lithosphere (crust +uppermost mantle) is divided into plates What makes the plates move? • Uneven distribution of heat in the upper mantle (Asthenosphere) causes heat to rise in some places (e.g., Mid-ocean ridges) • Differences in density cause colder, more dense Lithosphere to sink back into the asthenosphere (subduction) • This Convection drives the motion of the plates Plate Tectonics and the Origin of Crust • Direct link with formation of oceanic crust (sea floor spreading) • Less obvious connections with continental crust (continental accretion) Plate Tectonics and the Origin of Crust • Archean convection may have caused earliest crust to float to surface as “scum” • Subduction returned more dense material to interior • Less dense components were scraped off or returned to surface via volcanism • Plate interactions added continental crust to margins of continents • Quantity of continental crust has increased through time