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Our Solar System
Our Solar System

... • Surface: Mercury has many flat plains and many craters on its surface. ...
How to Use This Presentation
How to Use This Presentation

... are separated from the inner planets by a ring of debris called the asteroid belt. ...
Chapter 15 The Formation of Planetary Systems
Chapter 15 The Formation of Planetary Systems

... • Orbits mostly between Mars and Jupiter • Jupiter’s gravity kept them from condensing into a planet, or accreting onto an existing one • Fragments left over from the initial formation of the solar system ...
Europa
Europa

... Io, and distort Io’s orbit into ellipse • Io’s long axis “nods” back and forth half degree • The tidal stress that Jupiter exerts on Io varies periodically • The varying tidal stresses alternatively squeeze and flex Io • This tidal flexing is aided by the 1:2:4 ratio of orbital periods among the inn ...
The Solar System
The Solar System

... • between Mars & Jupiter • thousands of rock fragments that orbit around the sun • Too small to be spherical or clear a path • Largest asteroids have been reclassified; now called Dwarf planets – Ceres! ...
Jupiter
Jupiter

... • After the discovery of Uranus, it was noticed that its orbit was not as it should be in accordance with Newton's laws. • It was therefore predicted that another more distant planet must be perturbing Uranus' orbit. • Neptune was first observed by Johan Galle and Heinrich d'Arrest on 1846 Sept 23 v ...
Comets, Asteroids, and Meteorites
Comets, Asteroids, and Meteorites

... They leave behind in their orbits, gravel and rocky debris that Earth may encounter from time to time as orbits cross. We see these encounters as 'meteor showers'. Because they orbit the Sun, we can see them come back from time to time. Halley's Comet ...
The solar system - LemoineHPCScience
The solar system - LemoineHPCScience

... Jupiter has a mass that is 2 ½ times greater than the mass of all the other planets and moons combined, yet the sun is 800 times larger than Jupiter. Structure of Jupiter: Jupiter’s hydrogen-helium atmosphere also contains small amounts of methane, ammonia, water, and sulfur compounds. The wind syst ...
Chapter 12 section 3
Chapter 12 section 3

... The atmosphere of Uranus is made up of hydrogen, helium, and some methane. Methane gives the planet a bluish-green color. A few clouds and storms can be seen on Uranus. There may be liquid water under its atmosphere. Uranus has an unusual rotation. It is tilted on its side. The axes of rotation of t ...
Astronomy 110 Announcements: Chapter 8 Jovian Planet Systems
Astronomy 110 Announcements: Chapter 8 Jovian Planet Systems

... • Jupiter and Saturn – mostly H, He • Uranus and Neptune – H compounds mixed w/ metal and rock. • Originated from ice-rich planetesimals of about the same size, but captured different amounts of hydrogen and helium gas from the solar nebula. ...
The Inner Planets
The Inner Planets

... Just beyond the orbit of Mars is a belt of small bodies called asteroids. This asteroid belt separates the inner planets from the outer planets, Jupiter, Saturn, Uranus, Neptune, and Pluto. The first four of these planets, called the Jovian, or Jupiter-like, planets, are considerably larger than Ear ...
Comets & Meteors (10)
Comets & Meteors (10)

... Asteroids & their Belt (10) ...
Solar System Origin II
Solar System Origin II

... • An obvious question: Why didn't proto-Uranus and proto-Neptune grow as fast as proto-Jupiter and proto-Saturn? • Leading hypothesis: – Farther out in the nebula, the timescales between planetesimal collisions were much longer. – Longer orbital periods, larger volume, lower number of planetesimals ...
Document
Document

... Pluto: why not a planet? •Pluto is a special case – An outer planet, but smaller than any of the terrestrial planets – Intermediate average density of about 1900 kg/m3 – Density suggests it is composed of a mixture of ice and rock – Its orbit has large eccentricity and inclination angle – It is now ...
Earth 110 – Exploration of the Solar System Assignment 5
Earth 110 – Exploration of the Solar System Assignment 5

... Due in class Tuesday, Feb. 24, 2015 ...
Earth 110 – Exploration of the Solar System Assignment 4
Earth 110 – Exploration of the Solar System Assignment 4

... Due in class Tuesday, Feb. 23, 2016 ...
Click www.ondix.com to visit our student-to
Click www.ondix.com to visit our student-to

... large, gaseous, rarefied, and hydrogen-rich, while the inner planets are small rocky, dense, and hydrogen-poor. Because the giant planets consist mostly of hydrogen and helium, they resemble the universe at large. The inner planets are distinctly different: Though the universe consists mostly of hyd ...
Why is Pluto no longer a planet
Why is Pluto no longer a planet

... A dwarf planet is a celestial body that is in orbit around the Sun, is massive enough for its own gravity to make it round, is not a moon but has not cleared the neighbourhood around its orbit. The latter point means that there are bodies of a similar size in the orbit of the dwarf planet. For examp ...
Pocket Solar System - Skynet Junior Scholars
Pocket Solar System - Skynet Junior Scholars

... 2. Do you know anything about the physical properties of the ones that are spread out versus the ones that are crowded in close to the Sun? All the inner ones are small and rocky and the outer ones are gassy giants (except small, icy Pluto). 3. Given this spacing, why do you think little, rocky Venu ...
Solar System Model and
Solar System Model and

... Our Solar System is made up of eight planets, their moons, and our sun. The planets and their moons revolve around, or orbit the sun. The orbits are not round. They are elliptical ( E-lip-tih-cul). Elliptical means egg-shaped. The first four planets are called the inner planets. They are closest to ...
The Solar System
The Solar System

... • Io is stretched more, then less, then more, then less…etc for each and every 42 hr orbit. • This converts orbital kinetic energy into thermal energy, heating the interior above the melting point of sulfur (239F or 115C), and it burbles up through cracks to make volcanoes. • Constant volcanic erupt ...
17.4 NOTES What are the other moons in the solar system
17.4 NOTES What are the other moons in the solar system

... Objective: Compare the moons of the different planets in the solar system ...
source - UC Berkeley Astronomy w
source - UC Berkeley Astronomy w

... are "aligned" by Coriolis forces (rotation). Aurorae – Charged particles can only travel along magnetic field lines. When solar wind particles reach the vicinity of a planet, they are captured by the magnetic field and funneled towards the poles (where the field lines originate). Eventually they hit ...
Astronomy 12 Final Review Sheet Sun
Astronomy 12 Final Review Sheet Sun

... are "aligned" by Coriolis forces (rotation). Aurorae – Charged particles can only travel along magnetic field lines. When solar wind particles reach the vicinity of a planet, they are captured by the magnetic field and funneled towards the poles (where the field lines originate). Eventually they hit ...
Jupiter - pridescience
Jupiter - pridescience

... when Jupiter passes directly in front of the sun. They are made of small rocks and dust, and they are dark in color. ...
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Jumping-Jupiter scenario

The jumping-Jupiter scenario specifies an evolution of giant-planet migration described by the Nice model, in which an ice giant (Uranus, Neptune, or an additional Neptune-mass planet) encounters first Saturn and then Jupiter, causing the step-wise separation of their orbits. The jumping-Jupiter scenario was proposed by Ramon Brasser, Alessandro Morbidelli, Rodney Gomes, Kleomenis Tsiganis, and Harold Levison after their studies revealed that the smooth divergent migration of Jupiter and Saturn resulted in an inner Solar System significantly different from the current Solar System. The sweeping of secular resonances through the inner Solar System during the migration excited the eccentricities of the terrestrial planets beyond current values and left an asteroid belt with an excessive ratio of high- to low-inclination objects. The step-wise separation of Jupiter and Saturn described in the jumping-Jupiter scenario allows these resonances to quickly cross the inner Solar System without altering orbits excessively. The jumping-Jupiter scenario also results in a number of other differences with the original Nice model. The fraction of lunar impactors from asteroid belt during the Late Heavy Bombardment is significantly reduced, most of the Jupiter trojans are captured via an alternative mechanism, and Jupiter acquires its population of irregular satellites via the same process as the other planets. The frequent ejection of an ice giant during simulations of the jumping-Jupiter scenario has led some to propose an additional giant planet in the early Solar System.
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