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Day
One rotation of Earth relative to the Sun (~24 hours)
Lunar month
One full cycle of Moon phases (~29.5 days)
Year
One complete orbit of Earth around the Sun (~365.25 days)
Seasons
Caused by Earth’s axial tilt combined with its orbit around the Sun
Eclipse cycle
Repeating alignment of Sun, Earth, and Moon (~18 years, Saros cycle)
Astronomy and food
Predicts seasons and planting times
Astronomy and water
Predicts floods and seasonal rainfall
Astronomy and navigation
Uses stars and the Sun to determine direction
Astronomy and timekeeping
Creates calendars and predictable schedules
Astronomy and safety
Tracks eclipses, comets, and space hazards
Sundial
Uses the Sun’s shadow to track hours
Lunar calendar
Uses Moon phases to define months
Solar calendar
Tracks the Sun’s yearly path to define the year
Star calendar
Rising and setting of stars mark seasons
Water clock
Steady water flow measures time intervals
Stone alignments
Structures aligned with solstices and equinoxes
Moon phases
Caused by changing viewing angle of the Sun-lit Moon
New moon
Moon is between Earth and Sun
Full moon
Earth is between Sun and Moon
Solar eclipse
Moon blocks sunlight from reaching Earth
Lunar eclipse
Earth’s shadow falls on the Moon
Summer warmth
Sun is higher in the sky and sunlight is more direct
Winter cold
Sun is lower and sunlight is less direct
Longer summer days
Earth’s tilt keeps one hemisphere facing the Sun longer
Solstice
Sun reaches highest or lowest position in the sky
Equinox
Day and night are equal length
Retrograde motion
Apparent backward motion of a planet against the stars
Geocentric explanation
Planets move on epicycles around Earth
Heliocentric explanation
Relative motion as Earth passes other planets
Parallax
Apparent shift in an object’s position due to viewpoint change
Observer separation
Greater distance between observers gives larger parallax
Nearby objects
Show large parallax
Distant objects
Show little or no parallax
Tycho’s conclusion
Comets and supernovae are farther than the planets
Copernican model
Heliocentric (Sun-centered) system
Earth’s motion
Earth rotates daily and orbits the Sun yearly
Retrograde explanation
Apparent motion caused by Earth’s movement
Importance of Copernicus
Simplified planetary motion and challenged geocentrism
Kepler’s First Law
Planets orbit in ellipses with the Sun at one focus
Kepler’s Second Law
Planets sweep out equal areas in equal times
Kepler’s Third Law
Orbital period² is proportional to orbital distance³
Galileo: Imperfect heavens
Moon mountains and sunspots
Galileo: Not everything orbits Earth
Moons orbit Jupiter
Galileo: Evidence for heliocentrism
Full phases of Venus
Galileo: Falling objects
Inertia keeps Earth’s motion
Galileo: Stellar parallax
Stars too distant to detect at the time