Astronomy Test 2 Test Answers – Flashcards

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Early astronomers knew:
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Sun, Moon, Stars, Mercury, Venus, Jupiter, Saturn, comets, and meteors
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Now we know the solar system has:
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one star, eight planets (added Uranus and Neptune), 135+ moons, asteroids, comets, and meteoroids.
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Pluto was added as a planet then
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reduced to a Dwarf Planet
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Orbital period
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can be observed
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Distance from the Sun
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known by Kepler's laws
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Radius known from
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angular size
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Masses from Kepler's 3rd Law as modified by
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Newton
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Rotation period from
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observations
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Density can be calculated knowing
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radius and mass
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terrestrial planets - Atmospheres and surface conditions
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are very dissimilar
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only earth has
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oxygen in atmosphere and liquid water on surface
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earth and mars rotate
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at about the same rate
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venus and mercury are
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much slower
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venus rotates in
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the opposite direction
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earth and mars have
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moons
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mercury and venus do not have
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moons
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earth, mars, and mercury have
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magnetic fields
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venus does not have
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magnetic fields
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asteroids and meteoroids are
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rocky
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asteroids are
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bigger
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asteroid eros is 34 Km long
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...
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comets are
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icy, with some rocky parts
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comet hale - bopp
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...
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mariner 10 flew by
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mercury, 1974-1975
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soviey venera probes landed on
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venus from 1970-1978
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viking landers arrived at
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mars in 1976
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pioneer and voyager flew through
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outer solar system.
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cloud of gas and dust contracts due to
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gravity
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conservation of angular momentum means it
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spins faster and faster as it contracts
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condensation theory
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interstellar dust grains help cool the cloud, and act as condensation nuclei to produce flakes
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local temperature in the
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condensing cloud determines where various materials condense
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overall structure
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mantle two-part core thin crust hydrosphere (oceans) atmosphere
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the blue curve shows the
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temperature at each altitude
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troposphere is where
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convection takes place - responsible for weather
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ionosphere is
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ionized by solar radiation, and is a good conductor
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the atmosphere reflects
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radio waves in the AM range
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but transparent to
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FM and TV
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ozone layer is between
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ionosphere and mesosphere
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the ozone layer absorbs
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ultraviolet radiation
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it is reported that man-made chloro-fluoro-carbons (CFCs) have been
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damaging the ozone layer, resulting in an ozone hole
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sunlight that is not reflected is
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absorbed by earth's surface, warming it
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surface reradiates as
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infrared thermal radiation
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atmosphere absorbs much of the
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infrared thus warming it
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the atmosphere scatters
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short wavelengths (blue), but not the longer wavelengths (red), making the sky appear blue
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secondary atmosphere came from
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volcanic activity, mostly nitrogen
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primary atmosphere was
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hydrogen, helium ; these escaped earth's gravity
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life appeared,
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creating atmospheric oxygen
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the construction of the earth is determined by
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studying the seismic waves generated by earthquakes
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mantle is much less dense than
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the core
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mantle is
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rocky;
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core is
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metallic - iron and nickel
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outer core is
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liquid
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inner core is
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solid; due to pressure
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volcanic lava comes from
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mantle; allows analysis of composition
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contintental drift:
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entire earth's surface is covered with crustal plates, which can move independently
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earthquakes and volcanoes occur at
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plate boundaries
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plates can also slide along each other, creating
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faults where many earthquakes occur
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a subduction zone is where
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one plate slides below another
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plates can move away from each other creating
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rifts
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the new crust created at rift zones preserves the
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magnetic field present at the time it solidified
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from this we can tell that field reversals occur about every
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500,000 years
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tectonic plate motion is
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drive by convection currents in the liquid mantle below the crust
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if we follow the continental drift backwards,
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the continents merge into one, which is called pangaea
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the magnetosphere is the
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magnetic field around the earth where charged particles from the solar wind are deflected and some are trapped
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the magnetosphere - the charged particles are
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trapped in areas called he van allen belts, where they spiral around the magnetic field lines
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near the poles, the van allen belts
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intersect the atmosphere.
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the charged particles can interact with
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air molecules; when they do, they create glowing light called an aurora
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many authors say that tides are due to
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gravitational force on earth from the moon
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force on near side of earth is greater than force on far side.
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greater than force on far side.
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water can flow
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freely in response
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the sun has less effect, but it does modify the
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lunar tides and produces neap tides and spring tides
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a more reasonable explanation of the tides if called the
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dynamic theory
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the earth and moon revolve around a
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common center of gravity (barycenter)
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the tide on the moon side is due to
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tidal force
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the tide on the opposite side is due to
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centrifugal force
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tides tend to exert a
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"drag" force on the earth, slowing it's rotation
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this also causes the moon to
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speed up in its orbit and "fall" away from the earth
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the sidereal day is
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one orbital period with respect to the stars
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one synchronous day is measured from
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full moon to the next full moon which is 29.5 days
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the experiment package being deployed here is the
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ALSEP
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the lunar interior was determined from
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moon quakes as measured by the five seismographs deployed on the moon
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the surface of the moon is covered with
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dust and debris from meterorite impacts called Regolith
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the moon is still being bombarded by
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"micro-meteorites" that tend to soften crater edges
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highlands
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meteorite impact
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craters
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meteorite impact
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maria & basins
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impact & vulcanism
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rays
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meteorite impact
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domes
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vulcanism
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rills
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vulcanism
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craters, highlands, maria, and basins were all made during the
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latter part of "creation", after the earth-moon system formed.
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the created record w have on the moon, mercury, etc. is from
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the "early intense bombardment"
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small craters have
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round bottoms
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larger craters have
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lumps in the bottom
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the largest craters have
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flat bottoms
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the lumps are due to
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compressed material relaxing
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the flat bottoms were filled by
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liquid rock from inside
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a meteorite strikes
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moon, ejecting material
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explosion ejects
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more material
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result of meteorites strikes:
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crater, lips (rim) and ejecta
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although most of the features on the mooon are due to impact there are some that come from
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vulcanism
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the GIANT IMPACT theory of the moon's origin says that
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two differentiated planetesmals collided. their crusts splashed and their interiors merged.
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the merged interiors formed
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the earth
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the splash formed
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the moon
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viewed from earth, mercury is
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never far from the sun
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phases of mercury can be seen best when
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mercury is at its maximum elongation
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mercury was long thought to be
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tidally locked to the sun; measurements in 1965 showed this to be false
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rather, mercury's day and year are in a
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3:2 resonance; mercury rotates three times while going around the sun twice
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caloris basin (very large maria) is a
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very large impact feature imaged by mariner 10.
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the weird terrain on opposite side of planet comes from
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convergence of the impact shock wave
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mercury formed about
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4.6 billion yars ago.. as did the earth and moon
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they melted due to
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compression heating, then cooled slowly.
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the iron core of mercury
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shrank... crumpling the crust.
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mercury has a weak
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magnetic field so much of the soar wind is shunted around the e.t
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never-the-less some of the solar wind particles plane do
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strike the planet surface
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more than 80% of the side seen by mariner 10, most disturbing are the
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long curved cliffs
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the possible explanation is that the
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crust crumpled as the iron core cooled
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mercuy was visited in
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1974 by mariner 10 for three quick fly-bys
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this year messenger went into a
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near polar orbit around mercury to do some intense studies
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most of the sensing time is going into
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geological and meteorological measurements.
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two important date points for dr.einstein and the theory of relativity
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1 - explained orbit precession 2 - demonstrated bending of light around a mass
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brightest object in the sky, after the sun and moon
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venus
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venus is also called
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morning or evening star, as it is also "tied" to sun
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venus is much brighter than
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mercury, both because it is bigger and it is closer to the earth. and it is father from the sun than mercury
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mass of venus
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4.9 x 10^24 kg
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density of venus
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5200 kg/m^3 = 5.2 x density of water
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rotation period of venus
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243 days, retrograde
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radius of venus
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6000 km
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dense atmosphere and thick clouds make
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venus' surface impossible to see
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surface temperature of venus is
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about 730 k - hotter than mercury
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venus and earth outgassed in a similar way. essentially all of the nitrogen and carbon dioxide remain
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above the surface.
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venus is too hot for
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liquid water, so oceans could not form
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venus' surface is
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relatively smooth
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there are two continent-like features,
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ishtar terra and aphrodite terra
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there is no apparent
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plate tectonics on venus
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there are very few mountains, a few impact craters, many colvanoes, and large lava flows
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...
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venus' largest impact crater named after
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margaret mead
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venus does not have a
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magnetic field, probably because it rotates too slowly
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venus very likely has an
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iron core
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there are several missions on their way to study
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the atmosphere in more detail
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mars' orbit is
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fairly eccentric - affects amount of sunlight reaching it
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mars can be either in the direction of
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the sun (conjunction) or not (opposition)
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long-distance observation of mars shows that you can see
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polar ice caps that grow and shrink with the seasons
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the hubble space telescope and other good telescopes can see
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much detail on mars.
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the different sides of mars provide different
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aspects and images of different terrain
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early observers before photography struggled to
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see and display martian details
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percival lowell
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in the years from about 1890 to 1910 lowell firmly believed that the canali that schiaparelli saw were canals. he believed in canals and the intelligent life forms needed to dig them.
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long-distance telescopic observations of mars have shown:
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- shifting dust cover makes surface look like it is changing -changing polar ice cas are frozen carbon dioxide; water ice is permanently frozen -frequent dust storms, with high winds -no canals
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martian atmosphere is mostly
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carbon dioxide, and very thin.. too thin to retain much heat; temperature drops sharply at night
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martian internal structure
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-from behavior of crust, it is estimated to be 100 km thick -no seismic studies have been done -no magnetic field, so core is probably non-metallic, non-liquid, or both
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the northern hemisphere (left) of mars is
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rolling volcanic terrain
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the southern hemisphere (right) of mars is
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heavily cratered highlands
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the average altitude in mars is
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5 km above northern
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the assumption is that northern surface is
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younger than southern
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this means that the northern hemisphere must have been
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lowered in elevation and then flooded with lava
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the major feature of the northern hemisphere of mars is the
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tharsis bulge
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the tharsis bulge is the size of
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north america and is 10 km above the surroundings
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associated with the bulgeis the
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great grand canyon named the valle marinaris
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other features of note are the
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giant volcanoes. they are the largest in the solar system
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because of the minimal cratering seen, this surface is
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the youngest surface on mars
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mars has the largest
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volcano in the solar system : olympus mons
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(size) olympus mons is
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25 km high, the caldera is 80 km in diameter, it is 700 km diameter at base
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three other martian volcanoes are only slightly
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smaller
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the mars global surveyor (MGS) was designed to
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image the entire surface of mars in visible and infrared wavelengths every sol for one entire mars year.
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there is no water on the surface of mars today
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but there are two apparent water features whose images were captured by the MGS.
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impact craters less than 5 km across have
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mostly been eroded away in the northern hemisphere
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recently, gullies have been seen that seem to indicate
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the recent presence of liquid water; interpretation is still in being debated
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much of mars' northern hemisphere may have been
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ocean.
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both viking landers landed in
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low-latitude northern plains. care was taken to find a location where the rocks were small
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the rocky surface of mars was analyzed and the red color was due to
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iron content
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one of the trickiest parts of the mars exploration mission is
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actually getting the rovers to mars in working condition.
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the pathfinder carried
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the first US rover on mars.
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the rover that went on mars was named
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sojourner. it analyzed the element content of rocks
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both the pathfinder and the sojourner were active for
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more than three months
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spirit's landing place was similar to the
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vikings'
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the opportunity went down into
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the victoria crater.. it has now left the victoria crater to search of another crater to explore.
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intrepid geologists * discoveries
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- layering as if by water deposit - spherical pebbles such as in a stream - rust (color) same as the red iron oxide as in southern utah
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intrepid geologists * adventures
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- stuck in sand dune - covered by dust in a storm - uncovered by a whirl wind -lived through a long mars winter -are still going strong (four times as long as expected)
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each rover has become
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bigger and more complex as we have learned how to build them and use them
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mars pathfinder and mars global surveyor
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success
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mars polar lander and mars atmosphere observer
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failed
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2011 mars odyssey
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- arrived october 24, 2001 - gathering data today
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landers
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future - biology and geology laboratory - to gather rocks and return them to earth
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phobos (fear) is the
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larger of the two. they are both tiny and badly scarred by impacts but phobos looks like it was nearly shattered
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the japanese are planning to send
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a robot to pick up dirt and rock samples from diemos (terror) to return them to earth
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