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Our Solar System
Our Solar System

... •A star with a planet will move in its own small orbit in response to the planet's gravity. The goal now is to measure variations in the speed with which the star moves toward or away from Earth. •In other words, the variations are in the radial velocity of the star with respect to Earth. The radial ...
The formation of the Solar System I. Stellar context
The formation of the Solar System I. Stellar context

... then water ice (<160 K) then ammonia and methane ice (<100K) ...
1 Timeline 2 Geocentric model
1 Timeline 2 Geocentric model

... • Sometimes the eccentric was slightly off center from the center of the Earth Ptolemy’s Geocentric Model • Uniform circular motion could not account for speed of the planets thus Ptolemy used a device called the equant • The equant was placed the same distance from the eccentric as the Earth, but o ...
Some Physics of the Kepler Laws and Orbits Kepler`s First Law
Some Physics of the Kepler Laws and Orbits Kepler`s First Law

... open orbits, while the elliptical and circular orbits are closed bounded orbits. An open orbit simply means that that an object will orbit a star and then go far away from the star. A closed orbit returns to itself in our case (in general it doesn’t do this but we will not worry about that). ...
From the Everett and Seattle Astronomical
From the Everett and Seattle Astronomical

... Mercury is the closest planet to our Sun, and the least explored of the socalled terrestrial planets, which are the four rocky inner planets that also include Venus, Earth, and Mars. Other than 3 flybys by Mariner 10 in 1974 and ’75, no other spacecraft have yet explored the first rock from the Sun. ...
08Moon - NMSU Astronomy
08Moon - NMSU Astronomy

... of the Milky Way B. reflex motion from Earth rotating on its axis C. the 23.5 degree tilt of the Earth’s axis D. reflex motion from Earth revolving around the Sun E. intrinsic motion of the stars around the center of the Milky Way ...
Cycles: Earth, Sun, Moon by MTDavis
Cycles: Earth, Sun, Moon by MTDavis

... http://www.vendian.org/mncharity/dir3/solarsystem/ Great info and images www.space.com www.spaceweather.com ...
PPT - El Camino College
PPT - El Camino College

... – Collisions can destroy small planetesimals. – What’s left at the end? – What’s the temperature like near the Sun? • Gases won’t stay on the planets ...
stars and planets
stars and planets

... Supernovas are explosions generated by large stars when they come to the end of their lifespan. ...
Introducing Astronomy
Introducing Astronomy

... The slowly-rotating NCP causes the dates of Equinoxes, etc. to change Also, the dates of Earth’s aphelion (farthest distance from sun) and perihelion (closest approach to sun) change ...
Name________________ Final Ms. Bailey Period ______ October
Name________________ Final Ms. Bailey Period ______ October

... 12. Which two factors cause the perpendicular rays of the Sun to move between 23.5 o N and 23.5o S? 1. tilt of Earth's axis and Earth's revolution 3. eccentricity of Earth's orbit and Earth's revolution 2. tilt of Earth's axis and Earth's rotation 4. eccentricity of Earth's orbit and Earth's rotatio ...
ExoplanetWorksheet
ExoplanetWorksheet

... *There are two ways to plot the data on each axis (linear and logarithmic). For ‘planet mass’ do you get better detail when you plot with linear or logarithmic data points? __________________________________ *All of the rocky planets in our Solar System are at least 3 times more dense than Jupiter. ...
SPACE Jeopardy
SPACE Jeopardy

... planet to have liquid water. ...
8th GRADE SCIENCE - Norwin School District
8th GRADE SCIENCE - Norwin School District

... 11. Quarterly Curriculum Assessment # 2 ...
the brochure
the brochure

... Saturn Saturn would float if you could throw it in a bucket of water. The fascinating ring system observed by Galileo in 1610 is only beginning to be understood. First thought to be moons of Saturn, it is now known that the rings comprise trillions of ice and rock chunks ranging in size from dust pa ...
Solutions
Solutions

... Orbits are ellipses: this one would have been the same. All that’s necessary for this is a “Keplerian” system, where all (or at least the vast majority) of the mass in the system is concentrated towards the center (inside the orbit of the innermost planet you’re considering). Equal areas in equal ti ...
SciNot Scale Metric 102
SciNot Scale Metric 102

... To get the rate at which the pressure increases with depth: (1) Draw in a line that fits the data points the best (2) Get the coordinates of two arbitrary points on the line ...
1 The Synodic and Orbit Periods of the Planets
1 The Synodic and Orbit Periods of the Planets

... Calculate the percent difference between your Voyager observations and these accepted S values. Make a graph of accepted S vs. planet number (Mercury = 1, Venus = 2, etc.). Is this relationship monotonic? ___________ Is this relationship linear? _____________ Describe the curve in words. (Do not try ...
The Synodic and Orbit Periods of the Planets
The Synodic and Orbit Periods of the Planets

... Calculate the percent difference between your Voyager observations and these accepted S values. Make a graph of accepted S vs. planet number (Mercury = 1, Venus = 2, etc.). Is this relationship monotonic? ___________ Is this relationship linear? _____________ Describe the curve in words. (Do not try ...
Contributions of astronomy to all of science
Contributions of astronomy to all of science

... into the underlying upper mantle.  Over very long time scales, this movement refreshes the surface of the earth and its atmosphere, and is responsible for volcanic activity, earthquakes, and the formation of mountains.  The rate at which the plates move across the surface of the earth is now being ...
ASTRO OTTER (for secondary students)
ASTRO OTTER (for secondary students)

... including the orbital characteristics and any other significant or unusual features of each planet. Particular emphasis is made to describe the differences between the terrestrial and the Jovian planets and how they formed. This program contains moderately enhanced vocabulary including; elliptical a ...
WARM-UP # 32 Which planets are the terrestrial planets and which
WARM-UP # 32 Which planets are the terrestrial planets and which

... meteor, meteorite, meteoroid? The Quick Trick: Oids are outside the atmosphere, ites are inside it, and meteors are in between. ...
the young astronomers newsletter
the young astronomers newsletter

... European experts saw one of the faintest asteroids common stars in the universe) are prime targets in the ever found - a chunk of space rock about 65 miles in search for extraterrestrial life. But new research diameter beyond the orbit of Mars. It had been seen indicates some such planets may not be ...
Lecture 2 - Physics and Astronomy
Lecture 2 - Physics and Astronomy

... On modern star charts, the entire sky is divided into 88 regions Each is a constellation Most stars in a constellation are nowhere near one another They only appear to be close together because they are in nearly the same direction as seen from Earth ...
10_origin_life
10_origin_life

... effect to raise temp. above 0 C. Mars has since lost most of its atmosphere for unknown reasons, perhaps absorption in rocks. ...
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Comparative planetary science

Comparative planetary science or comparative planetology is a branch of space science and planetary science in which different natural processes and systems are studied by their effects and phenomena on and between multiple bodies. The planetary processes in question include geology, hydrology, atmospheric physics, and interactions such as impact cratering, space weathering, and magnetospheric physics in the solar wind, and possibly biology, via astrobiology.Comparison of multiple bodies assists the researcher, if for no other reason than the Earth is far more accessible than any other body. Those distant bodies may then be evaluated in the context of processes already characterized on Earth. Conversely, other bodies (including extrasolar ones) may provide additional examples, edge cases, and counterexamples to earthbound processes; without a greater context, studying these phenomena in relation to Earth alone may result in low sample sizes and observational biases.
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