28.solar system origin

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    The origin of the Solar System

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    Small planets beyond PlutoSedna, ~1,3001750 km dia.

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    Our Solar System is about 16

    billion km, or 10 billion miles, or15 light hours across.

    Light travels ~ 300,000 km/sec or

    ~1.1 billion km/hour

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    Our galaxy, the Milky Way

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    A galactic center: More than 1 Million stars are visible here!

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    Edge-on view of a spiral galaxy. Our galaxy, the Milky Way, would

    look very much like it to an outside visitor

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    Our galaxy, the Milky Way

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    IRAS telescope

    image of

    Pictoris, a solarsystem in the

    making? Red =

    solid material.

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    Star nurseries in the constellation Sagittarius

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    The Big Picture The Big Bang, the birth of the Universe ~ 13 Gy ago,

    produced H and He. These elements formed stars

    which cluster in galaxies with billions of stars; our

    galaxy, the Milky Way, formed ~ 10 Gy ago.

    Other elements are synthesized in the interiors of stars

    such as Red Giants and Supernovae.

    Upon ejection into interstellar space from dying stars,

    some elements condense into dust grains (presolar

    grains) and amorphous dust, either in stellar

    atmospheres or in interstellar space.

    Gas and dust collect into giant, cold molecular clouds.

    Dense cores collapse into stars, such as the Sun 4.56 Gy

    ago and planets, asteroids and comets form.

    Asteroids collide and fragments fall on Earth as

    meteorites

    We study meteorites and the presolar grains which

    some of them contain. These tell us about the complex

    nucleosynthetic processes that are going on in stars,

    such as Supernovae, AGB stars, etc.

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    The origin of the Solar System

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    The critical role of Earths Moon in helping life start and be

    sustained on Earth

    Moon adds stability to

    Earths rotation, so

    less extreme seasons

    Moon provides ocean

    tides on Earth

    promotes early life in

    shallow pools

    Moon slows Earths

    rate of rotationlonger days

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    Growth of continents with time

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    Old parts of the Moon are very

    heavily cratered. This indicates

    that early in the history of the

    Solar System the Moon and, by

    inference, Earth were very

    heavily bombarded by highly

    destructive bullets from space

    (asteroids; comets)

    Oldest rocks on Earth are ~3.85

    Gy old. Older rocks were

    destroyed by impacts anderosion: There is nothing left of

    the earliest period of Earth

    history!

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    The atomic bomb dropped on Hiroshima was ~ 20 kt (1 kt = 1,000 t of TNT; 1 mt = 1,000 kt).

    Meteor Crater Arizona = 3 mt = 150 Hiroshima bombs.

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    How long does life exist on Earth

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    Earth is unique: Do not mess it up!

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    Planets outside our Solar System, orbiting other stars, in multiples of

    Jupiter masses (Mj). Conclusion: Most planets have masses equal to,

    or a few times, the mass of Jupiter

    Pl t t id S l S t biti th t l tt d

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    Planets outside our Solar System, orbiting other stars, plotted as a

    function of the distance of their star. Conclusion: Most planets orbit

    extremely closely to their stars!