☀️ Astronomy · Solar System

Astronomy tricks that make the solar system click

Planets, moons, Kepler's laws, and solar system formation — mastered.

☀️ Solar System

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Proven mnemonics — fast to learn, hard to forget.

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Planet Order
My Very Educated Mother Just Served Us Nachos — Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune
Planet Mnemonics
Eight planets in order — plus how to remember which are rocky and which are gas giants
Rocky (terrestrial) planets: Mercury, Venus, Earth, Mars — small, dense, inner solar system. Gas/Ice giants: Jupiter, Saturn (gas), Uranus, Neptune (ice giants, mostly water/ammonia/methane). Pluto: reclassified as dwarf planet 2006 (IAU). Planet definition: orbits Sun, spherical by gravity, cleared its orbital neighborhood. Dwarf planets: Pluto, Eris, Ceres, Makemake, Haumea. Asteroid belt between Mars and Jupiter. Kuiper Belt beyond Neptune.
Mercury
Closest, no atmosphere, extreme temps
Venus
Hottest (greenhouse effect), retrograde
Earth
Largest rocky, only known life
Mars
Red, thin CO₂ atmosphere, Olympus Mons
Jupiter
Largest, Great Red Spot, 95 moons
Saturn
Rings, least dense, 146 moons
Uranus
Tilted 98°, ice giant
Neptune
Windiest, Triton retrograde moon
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Alex breaks down My Very Educated Mother Just Served Us Nachos — 1:50.
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🃏 Planet Order
My Very Educated Mother Just Served Us Nachos
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🃏 Answer
My Very Educated Mother Just Served Us Nachos — Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune
MercuryClosest, no atmosphere, extreme temps
VenusHottest (greenhouse effect), retrograde
EarthLargest rocky, only known life
MarsRed, thin CO₂ atmosphere, Olympus Mons
JupiterLargest, Great Red Spot, 95 moons
SaturnRings, least dense, 146 moons
UranusTilted 98°, ice giant
NeptuneWindiest, Triton retrograde moon
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Planet Types
Terrestrial (rocky): Mercury Venus Earth Mars. Jovian (gas): Jupiter Saturn. Ice giants: Uranus Neptune.
Terrestrial vs Giant Planets
Why the inner planets are rocky and the outer planets are enormous — the frost line explains everything
Frost line (~2.7 AU from Sun): water ice stable beyond this point. Inner solar system: only rocky, refractory materials could condense → small terrestrial planets. Beyond frost line: ice added to rocky cores → grew large → captured hydrogen and helium → gas giants. Jupiter and Saturn: ~90% H and He. Uranus and Neptune (ice giants): ~15–20% H/He surrounding water, ammonia, methane ice mantle. Planetary migration: Jupiter likely formed further out and migrated inward — shaped the solar system.
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🃏 Planet Types
Terrestrial vs gas giants vs ice giants?
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🃏 Answer
Terrestrial (rocky): Mercury Venus Earth Mars. Jovian (gas): Jupiter Saturn. Ice giants: Uranus Neptune.
Terrestrial vs Giant Planets — Frost line (~2.7 AU from Sun): water ice stable beyond this point. Inner solar system: only rocky, refractory materials could condense → small terrestrial planets. Beyond frost line: ice added to rocky cores → grew large → captured hydrogen and helium → gas giants. Jupiter and Saturn: ~90% H and He. Uranus and Neptune (ice giants): ~15–20% H/He surrounding water, ammonia, methane ice mantle. Planetary migration: Jupiter likely formed further out and migrated inward — shaped the solar system.
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Kepler's Laws
Kepler's 3 laws: 1) Ellipses, 2) Equal areas in equal times (faster near Sun), 3) T² ∝ a³
Kepler's Three Laws of Planetary Motion
The mathematical rules governing how every planet (and satellite) orbits
First law: planets orbit in ellipses with the Sun at one focus. Second law: line from Sun to planet sweeps equal areas in equal times → faster at perihelion (closest), slower at aphelion. Third law: T² ∝ a³ — orbital period squared is proportional to semi-major axis cubed. Example: Earth (1 AU, 1 yr) vs Mars (1.52 AU, 1.88 yr): 1.88² ≈ 1.52³. Newton derived these from his law of gravitation. Used to calculate masses of planets from moon orbits.
1st
Elliptical orbits — Sun at one focus
2nd
Equal areas — faster near Sun
3rd
T² ∝ a³ — outer = slower orbit
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🃏 Kepler's Laws
Kepler's three laws?
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🃏 Answer
Kepler's 3 laws: 1) Ellipses, 2) Equal areas in equal times (faster near Sun), 3) T² ∝ a³
1stElliptical orbits — Sun at one focus
2ndEqual areas — faster near Sun
3rdT² ∝ a³ — outer = slower orbit
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Orbital Mechanics
v = √(GM/r) — orbital velocity; T = 2π√(r³/GM) — orbital period; v_esc = √(2GM/r) — escape velocity
Orbital Velocity, Period & Escape Velocity
How to actually calculate orbital speed, period, and escape velocity — not just describe them
Gravity supplies the centripetal force for a circular orbit, giving v = √(GM/r) — notice the orbiting object's own mass cancels out entirely. Period follows from circumference ÷ speed: T = 2π√(r³/GM). Escape velocity is always exactly √2 times the circular orbital velocity at that radius: v_esc = √(2GM/r). Example: the ISS at 400 km altitude (r = 6,771 km from Earth's center) orbits at ~7.67 km/s with a ~92.4 minute period. Earth's surface escape velocity is ~11.2 km/s.
v
√(GM/r) — circular orbital velocity
T
2π√(r³/GM) — orbital period
v_esc
√(2GM/r) — escape velocity (= v × √2)
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🃏 Orbital Mechanics
Orbital velocity, period and escape velocity — the formulas?
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🃏 Answer
v = √(GM/r) — orbital velocity; T = 2π√(r³/GM) — orbital period; v_esc = √(2GM/r) — escape velocity
v√(GM/r) — circular orbital velocity
T2π√(r³/GM) — orbital period
v_esc√(2GM/r) — escape velocity (= v × √2)
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Jupiter
Jupiter: largest planet (318× Earth mass). Great Red Spot storm. 95 moons including Ganymede (larger than Mercury).
Jupiter
The solar system's dominant planet — its gravity shaped everything else
Mass: 318× Earth — more than all other planets combined. Composition: ~90% H, 10% He — no solid surface. Great Red Spot: anticyclonic storm, 1.3× Earth wide, observed for 350+ years (shrinking). Galilean moons: Io (most volcanically active body in solar system), Europa (subsurface ocean, potential life), Ganymede (largest moon in solar system, larger than Mercury), Callisto (heavily cratered). 95 moons total. Magnetosphere: largest in solar system. Jupiter as solar system's 'vacuum cleaner' — deflects comets.
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🃏 Jupiter
Jupiter — the key facts?
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🃏 Answer
Jupiter: largest planet (318× Earth mass). Great Red Spot storm. 95 moons including Ganymede (larger than Mercury).
Jupiter — Mass: 318× Earth — more than all other planets combined. Composition: ~90% H, 10% He — no solid surface. Great Red Spot: anticyclonic storm, 1.3× Earth wide, observed for 350+ years (shrinking). Galilean moons: Io (most volcanically active body in solar system), Europa (subsurface ocean, potential life), Ganymede (largest moon in solar system, larger than Mercury), Callisto (heavily cratered). 95 moons total. Magnetosphere: largest in solar system. Jupiter as solar system's 'vacuum cleaner' — deflects comets.
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Saturn's Rings
Saturn's rings: 270,000 km wide but only 10–200 m thick. Water ice particles. May be <400 million years old.
Saturn's Rings
The most spectacular structure in the solar system — surprisingly thin and possibly temporary
Rings span 270,000 km (wider than Earth-Moon distance) but only 10–200 m thick — proportionally thinner than a sheet of paper at that scale. Composition: ~90% water ice particles, 1 cm to 10 m in size. Cassini Division: 4,800 km gap — orbital resonance with Dione. Ring age: Cassini data suggests <400 million years old (dinosaur era). All giant planets have rings. Titan: Saturn's largest moon, thick nitrogen atmosphere, methane lakes — most Earth-like surface in solar system.
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🃏 Saturn's Rings
Saturn's rings — size, thickness, material?
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🃏 Answer
Saturn's rings: 270,000 km wide but only 10–200 m thick. Water ice particles. May be <400 million years old.
Saturn's Rings — Rings span 270,000 km (wider than Earth-Moon distance) but only 10–200 m thick — proportionally thinner than a sheet of paper at that scale. Composition: ~90% water ice particles, 1 cm to 10 m in size. Cassini Division: 4,800 km gap — orbital resonance with Dione. Ring age: Cassini data suggests <400 million years old (dinosaur era). All giant planets have rings. Titan: Saturn's largest moon, thick nitrogen atmosphere, methane lakes — most Earth-like surface in solar system.
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The Moon
Moon: 1/4 Earth's diameter. Formed from giant impact (~4.5 bya). Stabilizes Earth's axial tilt.
The Moon
Earth's companion — its origin, effects on Earth, and key features
Giant impact hypothesis: Mars-sized body (Theia) struck early Earth → debris coalesced → Moon. Evidence: Moon's composition matches Earth's mantle, low iron content, no water originally. Synchronous rotation: Moon rotates at same rate as it orbits → always same face toward Earth. Tidal locking: caused by Earth's tidal forces over billions of years. Effects: stabilizes Earth's axial tilt (~23.5°) → stable seasons. Tides: Moon's gravity stretches Earth. Recession: Moon moves ~3.8 cm farther away per year.
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🃏 The Moon
The Moon — size, origin, effect on Earth?
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Moon: 1/4 Earth's diameter. Formed from giant impact (~4.5 bya). Stabilizes Earth's axial tilt.
The Moon — Giant impact hypothesis: Mars-sized body (Theia) struck early Earth → debris coalesced → Moon. Evidence: Moon's composition matches Earth's mantle, low iron content, no water originally. Synchronous rotation: Moon rotates at same rate as it orbits → always same face toward Earth. Tidal locking: caused by Earth's tidal forces over billions of years. Effects: stabilizes Earth's axial tilt (~23.5°) → stable seasons. Tides: Moon's gravity stretches Earth. Recession: Moon moves ~3.8 cm farther away per year.
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Mars
Mars: thin CO₂ atmosphere, largest volcano (Olympus Mons, 22 km), evidence of ancient liquid water.
Mars
The Red Planet — its geology, past water, and prospects for life
Olympus Mons: 22 km high, 600 km wide — largest volcano in solar system. Valles Marineris: 4,000 km long canyon system. Evidence of ancient water: river valleys, delta deposits, clay minerals. Current water: polar ice caps (CO₂ + water ice), subsurface brine. Atmosphere: 95% CO₂, ~1% Earth pressure → cannot support liquid water at surface. Missions: Curiosity (still operational), Perseverance (collecting samples), Ingenuity helicopter. Moons: Phobos and Deimos (captured asteroids). Mars was warmer and wetter ~3–4 bya.
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🃏 Mars
Mars — the key facts?
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🃏 Answer
Mars: thin CO₂ atmosphere, largest volcano (Olympus Mons, 22 km), evidence of ancient liquid water.
Mars — Olympus Mons: 22 km high, 600 km wide — largest volcano in solar system. Valles Marineris: 4,000 km long canyon system. Evidence of ancient water: river valleys, delta deposits, clay minerals. Current water: polar ice caps (CO₂ + water ice), subsurface brine. Atmosphere: 95% CO₂, ~1% Earth pressure → cannot support liquid water at surface. Missions: Curiosity (still operational), Perseverance (collecting samples), Ingenuity helicopter. Moons: Phobos and Deimos (captured asteroids). Mars was warmer and wetter ~3–4 bya.
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Solar System Formation
Solar nebula hypothesis: collapsing gas cloud → protoplanetary disk → accretion → differentiation.
Solar System Formation
How the Sun and planets formed from a spinning cloud of gas and dust 4.6 billion years ago
Solar nebula hypothesis: cloud of gas and dust collapsed under gravity ~4.6 bya. Conservation of angular momentum → disk formed. Sun ignited at center. Planetesimals: dust grains stuck together → pebbles → km-sized objects → planets via runaway accretion. Differentiation: rocky planets melted, dense iron sank to core. Grand Tack hypothesis: Jupiter migrated inward then outward — explains asteroid belt depletion. Late Heavy Bombardment: ~4 bya, Jupiter's migration sent asteroids/comets into inner system. Isotopic dating of meteorites: 4.568 billion years.
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🃏 Solar System Formation
Solar nebula hypothesis — the steps?
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🃏 Answer
Solar nebula hypothesis: collapsing gas cloud → protoplanetary disk → accretion → differentiation.
Solar System Formation — Solar nebula hypothesis: cloud of gas and dust collapsed under gravity ~4.6 bya. Conservation of angular momentum → disk formed. Sun ignited at center. Planetesimals: dust grains stuck together → pebbles → km-sized objects → planets via runaway accretion. Differentiation: rocky planets melted, dense iron sank to core. Grand Tack hypothesis: Jupiter migrated inward then outward — explains asteroid belt depletion. Late Heavy Bombardment: ~4 bya, Jupiter's migration sent asteroids/comets into inner system. Isotopic dating of meteorites: 4.568 billion years.
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Asteroids and Comets
Asteroids: rocky, inner solar system (asteroid belt). Comets: icy, from Kuiper Belt or Oort Cloud. Tails always point away from Sun.
Asteroids, Comets, and Meteors
The small bodies of the solar system — leftover building blocks and impact hazards
Asteroids: rocky/metallic, mostly in asteroid belt (2–3.3 AU). Ceres: largest (dwarf planet). Near-Earth asteroids (NEAs — asteroids whose orbits bring them close to Earth): tracked for impact risk. Comets: icy (water, CO₂, dust) from Kuiper Belt (short-period) or Oort Cloud (long-period). Tails: dust tail (curved, sunlight pressure) + ion tail (straight, solar wind) — both always point away from Sun. Meteor: streak of light. Meteorite: reaches ground. Chicxulub impact (~66 mya): K-Pg extinction, killed non-avian dinosaurs. Planetary defense: DART mission (2022) successfully deflected Dimorphos.
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🃏 Asteroids and Comets
Asteroids vs comets?
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🃏 Answer
Asteroids: rocky, inner solar system (asteroid belt). Comets: icy, from Kuiper Belt or Oort Cloud. Tails always point away from Sun.
Asteroids, Comets, and Meteors — Asteroids: rocky/metallic, mostly in asteroid belt (2–3.3 AU). Ceres: largest (dwarf planet). Near-Earth asteroids (NEAs — asteroids whose orbits bring them close to Earth): tracked for impact risk. Comets: icy (water, CO₂, dust) from Kuiper Belt (short-period) or Oort Cloud (long-period). Tails: dust tail (curved, sunlight pressure) + ion tail (straight, solar wind) — both always point away from Sun. Meteor: streak of light. Meteorite: reaches ground. Chicxulub impact (~66 mya): K-Pg extinction, killed non-avian dinosaurs. Planetary defense: DART mission (2022) successfully deflected Dimorphos.
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Pluto and Dwarf Planets
Pluto: reclassified as dwarf planet 2006. Failed to 'clear orbital neighborhood.' Kuiper Belt Object.
Pluto and Dwarf Planets
Why Pluto lost planet status — and what the dwarf planet family looks like
IAU 2006 definition: planet must (1) orbit the Sun, (2) be spherical by gravity, (3) clear its orbital neighborhood. Pluto fails #3 — shares orbit with many Kuiper Belt Objects. Dwarf planets: Pluto, Eris, Haumea, Makemake, Ceres. New Horizons flyby (2015): heart-shaped nitrogen ice plain (Tombaugh Regio), mountains of water ice, surprisingly geologically active. Charon: Pluto's moon, half Pluto's size — barycenter outside Pluto. Kuiper Belt: ~30–55 AU, icy bodies. Oort Cloud: ~2,000–200,000 AU, source of long-period comets.
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🃏 Pluto and Dwarf Planets
Why was Pluto reclassified?
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🃏 Answer
Pluto: reclassified as dwarf planet 2006. Failed to 'clear orbital neighborhood.' Kuiper Belt Object.
Pluto and Dwarf Planets — IAU 2006 definition: planet must (1) orbit the Sun, (2) be spherical by gravity, (3) clear its orbital neighborhood. Pluto fails #3 — shares orbit with many Kuiper Belt Objects. Dwarf planets: Pluto, Eris, Haumea, Makemake, Ceres. New Horizons flyby (2015): heart-shaped nitrogen ice plain (Tombaugh Regio), mountains of water ice, surprisingly geologically active. Charon: Pluto's moon, half Pluto's size — barycenter outside Pluto. Kuiper Belt: ~30–55 AU, icy bodies. Oort Cloud: ~2,000–200,000 AU, source of long-period comets.
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The Sun
Sun: G-type main sequence star, 99.86% of solar system mass. Core: 15 million K, nuclear fusion. Magnetic cycle: 11 years.
The Sun
Our star — its structure, energy source, and activity cycle
Structure: core (fusion) → radiative zone → convection zone → photosphere (5,778 K) → chromosphere → corona (1–3 million K — the coronal heating problem). Energy source: proton-proton chain, converts 4H → He-4 + energy (E=mc²), loses ~4 million tons/sec. Solar wind: stream of charged particles. Sunspots: cooler regions (~4,000 K), magnetic inhibition. Solar cycle: 11-year activity cycle (sunspot minimum/maximum). Solar flares and CMEs: can disrupt Earth's magnetosphere (aurora, satellite damage). Lifetime: ~5 billion years remaining.
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🃏 The Sun
The Sun — type, mass share, core, cycle?
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Sun: G-type main sequence star, 99.86% of solar system mass. Core: 15 million K, nuclear fusion. Magnetic cycle: 11 years.
The Sun — Structure: core (fusion) → radiative zone → convection zone → photosphere (5,778 K) → chromosphere → corona (1–3 million K — the coronal heating problem). Energy source: proton-proton chain, converts 4H → He-4 + energy (E=mc²), loses ~4 million tons/sec. Solar wind: stream of charged particles. Sunspots: cooler regions (~4,000 K), magnetic inhibition. Solar cycle: 11-year activity cycle (sunspot minimum/maximum). Solar flares and CMEs: can disrupt Earth's magnetosphere (aurora, satellite damage). Lifetime: ~5 billion years remaining.
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Exoplanets
Exoplanets: 5,500+ confirmed. Detection: transit (Kepler/TESS), radial velocity, direct imaging, microlensing.
Exoplanets
Planets around other stars — and the search for worlds like Earth
First confirmed (1992, pulsar; 1995 51 Peg b, Nobel 2019). Kepler Space Telescope: found 2,600+ — most planets in multi-planet systems. Methods: transit (brightness dip — measures size), radial velocity (Doppler wobble — measures mass), direct imaging (young/large planets), microlensing (single events). Demographics: hot Jupiters surprising, super-Earths common, small rocky planets common. Habitable zone (HZ): liquid water possible. TRAPPIST-1: 7 rocky planets, 3 in HZ (habitable zone — the range where liquid water could exist). JWST: atmospheric characterization — CO₂ detected in exoplanet atmospheres.
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🃏 Exoplanets
Exoplanets — how are they detected?
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🃏 Answer
Exoplanets: 5,500+ confirmed. Detection: transit (Kepler/TESS), radial velocity, direct imaging, microlensing.
Exoplanets — First confirmed (1992, pulsar; 1995 51 Peg b, Nobel 2019). Kepler Space Telescope: found 2,600+ — most planets in multi-planet systems. Methods: transit (brightness dip — measures size), radial velocity (Doppler wobble — measures mass), direct imaging (young/large planets), microlensing (single events). Demographics: hot Jupiters surprising, super-Earths common, small rocky planets common. Habitable zone (HZ): liquid water possible. TRAPPIST-1: 7 rocky planets, 3 in HZ (habitable zone — the range where liquid water could exist). JWST: atmospheric characterization — CO₂ detected in exoplanet atmospheres.
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Terrestrial vs Jovian
MVEM — My Very Energetic Mother — inner rocky planets; JSUN — Jupiter Saturn Uranus Neptune — outer giants
MERCURY VENUS EARTH MARS | JUPITER SATURN URANUS NEPTUNE
Inner four are small and rocky; outer four are massive gas or ice giants
Terrestrial planets (Mercury, Venus, Earth, Mars): rocky surfaces, iron cores, few moons, no rings, slow rotation. Jovian planets (Jupiter, Saturn, Uranus, Neptune): gas/ice composition, rapid rotation, ring systems, many moons, low density. Saturn is less dense than water — it would float! The asteroid belt at ~2.7 AU marks the boundary between the two groups.
My Very Energetic Mother
Mercury Venus Earth Mars — terrestrial, rocky, inner
JSUN
Jupiter Saturn Uranus Neptune — giant, gaseous or icy, outer
Asteroid belt
Boundary at ~2.7 AU separating rocky and giant planets
Saturn density
Less dense than water — would float in a giant bathtub
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🃏 Terrestrial vs Jovian
MVEM
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🃏 Answer
MVEM — My Very Energetic Mother — inner rocky planets; JSUN — Jupiter Saturn Uranus Neptune — outer giants
My Very Energetic MotherMercury Venus Earth Mars — terrestrial, rocky, inner
JSUNJupiter Saturn Uranus Neptune — giant, gaseous or icy, outer
Asteroid beltBoundary at ~2.7 AU separating rocky and giant planets
Saturn densityLess dense than water — would float in a giant bathtub
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Kepler's Laws — E-E-P
ELLIPSE then EQUAL AREAS then PERIOD SQUARED — the three laws in order, easy to recall as E-E-P
ELLIPSES AND EQUAL AREAS AND PERIOD PROPORTIONAL TO SEMI-MAJOR AXIS CUBED
Law 3: P² = a³ (AU/years) — Earth: 1²=1³; Mars: 1.88²=1.52³
Law 1: Orbits are ellipses with the Sun at one focus — not circles. Law 2: A line from Sun to planet sweeps equal areas in equal times — planet moves faster near perihelion. Law 3: P² = a³ where P is in years and a is in AU. These replaced circular orbit models and enabled accurate planetary predictions centuries before Newton explained why.
Law 1 — Ellipses
Orbits are ellipses; Sun at one focus, not the center
Law 2 — Equal areas
Faster near perihelion, slower at aphelion
Law 3 — P² = a³
Period squared equals semi-major axis cubed (AU and years)
Perihelion speed
Earth moves 3.3 km/s faster in January than in July
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🃏 Kepler's Laws — E-E-P
Kepler's three laws — E-E-P
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🃏 Answer
ELLIPSE then EQUAL AREAS then PERIOD SQUARED — the three laws in order, easy to recall as E-E-P
Law 1 — EllipsesOrbits are ellipses; Sun at one focus, not the center
Law 2 — Equal areasFaster near perihelion, slower at aphelion
Law 3 — P² = a³Period squared equals semi-major axis cubed (AU and years)
Perihelion speedEarth moves 3.3 km/s faster in January than in July
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