WHAT IS a PLANET? ●➔ by Steven Soter
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Geological Timeline
Geological Timeline In this pack you will find information and activities to help your class grasp the concept of geological time, just how old our planet is, and just how young we, as a species, are. Planet Earth is 4,600 million years old. We all know this is very old indeed, but big numbers like this are always difficult to get your head around. The activities in this pack will help your class to make visual representations of the age of the Earth to help them get to grips with the timescales involved. Important EvEnts In thE Earth’s hIstory 4600 mya (million years ago) – Planet Earth formed. Dust left over from the birth of the sun clumped together to form planet Earth. The other planets in our solar system were also formed in this way at about the same time. 4500 mya – Earth’s core and crust formed. Dense metals sank to the centre of the Earth and formed the core, while the outside layer cooled and solidified to form the Earth’s crust. 4400 mya – The Earth’s first oceans formed. Water vapour was released into the Earth’s atmosphere by volcanism. It then cooled, fell back down as rain, and formed the Earth’s first oceans. Some water may also have been brought to Earth by comets and asteroids. 3850 mya – The first life appeared on Earth. It was very simple single-celled organisms. Exactly how life first arose is a mystery. 1500 mya – Oxygen began to accumulate in the Earth’s atmosphere. Oxygen is made by cyanobacteria (blue-green algae) as a product of photosynthesis. -
The Planetary Report Page 23 -Help Design a Mars Rover Planetary Society
A Publication of THEPLANE~ SOCIETY o o • o -e ¢ 0 0 Board of Directors FROIVI THE CARL SAGAN BRUCE MURRAY EDITOR President Vice President Director. Laboratory for Planetary Professor of Planetary Studies, Cornell University Science, California InsUtute of Technology LOUIS FRIEDMAN Executive Director HENRY TANNER California Institute THOMAS O. PAINE of Technology s we go to press, the Phobos 2 space proach to Earth provided opportunities to Former Administrator; NASA Chairman, National JOSEPH RYAN A craft is orbiting Mars, preparing to ren re-examine its familiar face, and to recall Commission on Space O'Mefveny & Myers dezvous with the moon Phobos. This com the work of earlier observers. Board of Advisors plex craft will send two landers to Phobos' Page 13 -The Concept of Extraterres DIANE ACKERMAN JOHN M. LOGSDON surface, irradiate it with a laser to measure trial Intelligence: An Emerging Cosmol poet and author Director. Space Policy Institute George Washington University its composition and conduct many other ogy?-Is the search for extraterrestrial in ISAAC ASIMOV author HANS MARK experiments that should greatly expand our telligence a truly scientifIc endeavor or an Chancellor. RICHARD BERENDZEN University of Texas System understanding of this strange, asteroid-like exercise in metaphysics? A new cosmology, President, American University JAMES MICHENER satellite. JACQUES BLAMONT aurhor based on centuries of thinking about the Scientific Consultant, Centre National dEludes Spa/isles, MARVIN MINSKY As our readers know, Phobos is the fIrst universe, may be unfolding as we search for France Donner Professor of Science. Massachusetts Institute mission in an ambitious Soviet program to signs of other civilizations. -
Introduction to Astronomy from Darkness to Blazing Glory
Introduction to Astronomy From Darkness to Blazing Glory Published by JAS Educational Publications Copyright Pending 2010 JAS Educational Publications All rights reserved. Including the right of reproduction in whole or in part in any form. Second Edition Author: Jeffrey Wright Scott Photographs and Diagrams: Credit NASA, Jet Propulsion Laboratory, USGS, NOAA, Aames Research Center JAS Educational Publications 2601 Oakdale Road, H2 P.O. Box 197 Modesto California 95355 1-888-586-6252 Website: http://.Introastro.com Printing by Minuteman Press, Berkley, California ISBN 978-0-9827200-0-4 1 Introduction to Astronomy From Darkness to Blazing Glory The moon Titan is in the forefront with the moon Tethys behind it. These are two of many of Saturn’s moons Credit: Cassini Imaging Team, ISS, JPL, ESA, NASA 2 Introduction to Astronomy Contents in Brief Chapter 1: Astronomy Basics: Pages 1 – 6 Workbook Pages 1 - 2 Chapter 2: Time: Pages 7 - 10 Workbook Pages 3 - 4 Chapter 3: Solar System Overview: Pages 11 - 14 Workbook Pages 5 - 8 Chapter 4: Our Sun: Pages 15 - 20 Workbook Pages 9 - 16 Chapter 5: The Terrestrial Planets: Page 21 - 39 Workbook Pages 17 - 36 Mercury: Pages 22 - 23 Venus: Pages 24 - 25 Earth: Pages 25 - 34 Mars: Pages 34 - 39 Chapter 6: Outer, Dwarf and Exoplanets Pages: 41-54 Workbook Pages 37 - 48 Jupiter: Pages 41 - 42 Saturn: Pages 42 - 44 Uranus: Pages 44 - 45 Neptune: Pages 45 - 46 Dwarf Planets, Plutoids and Exoplanets: Pages 47 -54 3 Chapter 7: The Moons: Pages: 55 - 66 Workbook Pages 49 - 56 Chapter 8: Rocks and Ice: -
Science in Nasa's Vision for Space Exploration
SCIENCE IN NASA’S VISION FOR SPACE EXPLORATION SCIENCE IN NASA’S VISION FOR SPACE EXPLORATION Committee on the Scientific Context for Space Exploration Space Studies Board Division on Engineering and Physical Sciences THE NATIONAL ACADEMIES PRESS Washington, D.C. www.nap.edu THE NATIONAL ACADEMIES PRESS 500 Fifth Street, N.W. Washington, DC 20001 NOTICE: The project that is the subject of this report was approved by the Governing Board of the National Research Council, whose members are drawn from the councils of the National Academy of Sciences, the National Academy of Engineering, and the Institute of Medicine. The members of the committee responsible for the report were chosen for their special competences and with regard for appropriate balance. Support for this project was provided by Contract NASW 01001 between the National Academy of Sciences and the National Aeronautics and Space Administration. Any opinions, findings, conclusions, or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the sponsors. International Standard Book Number 0-309-09593-X (Book) International Standard Book Number 0-309-54880-2 (PDF) Copies of this report are available free of charge from Space Studies Board National Research Council The Keck Center of the National Academies 500 Fifth Street, N.W. Washington, DC 20001 Additional copies of this report are available from the National Academies Press, 500 Fifth Street, N.W., Lockbox 285, Washington, DC 20055; (800) 624-6242 or (202) 334-3313 (in the Washington metropolitan area); Internet, http://www.nap.edu. Copyright 2005 by the National Academy of Sciences. -
An Overview of New Worlds, New Horizons in Astronomy and Astrophysics About the National Academies
2020 VISION An Overview of New Worlds, New Horizons in Astronomy and Astrophysics About the National Academies The National Academies—comprising the National Academy of Sciences, the National Academy of Engineering, the Institute of Medicine, and the National Research Council—work together to enlist the nation’s top scientists, engineers, health professionals, and other experts to study specific issues in science, technology, and medicine that underlie many questions of national importance. The results of their deliberations have inspired some of the nation’s most significant and lasting efforts to improve the health, education, and welfare of the United States and have provided independent advice on issues that affect people’s lives worldwide. To learn more about the Academies’ activities, check the website at www.nationalacademies.org. Copyright 2011 by the National Academy of Sciences. All rights reserved. Printed in the United States of America This study was supported by Contract NNX08AN97G between the National Academy of Sciences and the National Aeronautics and Space Administration, Contract AST-0743899 between the National Academy of Sciences and the National Science Foundation, and Contract DE-FG02-08ER41542 between the National Academy of Sciences and the U.S. Department of Energy. Support for this study was also provided by the Vesto Slipher Fund. Any opinions, findings, conclusions, or recommendations expressed in this publication are those of the authors and do not necessarily reflect the views of the agencies that provided support for the project. 2020 VISION An Overview of New Worlds, New Horizons in Astronomy and Astrophysics Committee for a Decadal Survey of Astronomy and Astrophysics ROGER D. -
Rev 06/2018 ASTRONOMY EXAM CONTENT OUTLINE the Following
ASTRONOMY EXAM INFORMATION CREDIT RECOMMENDATIONS This exam was developed to enable schools to award The American Council on Education’s College credit to students for knowledge equivalent to that learned Credit Recommendation Service (ACE CREDIT) by students taking the course. This examination includes has evaluated the DSST test development history of the Science of Astronomy, Astrophysics, process and content of this exam. It has made the Celestial Systems, the Science of Light, Planetary following recommendations: Systems, Nature and Evolution of the Sun and Stars, Galaxies and the Universe. Area or Course Equivalent: Astronomy Level: 3 Lower Level Baccalaureate The exam contains 100 questions to be answered in 2 Amount of Credit: 3 Semester Hours hours. Some of these are pretest questions that will not Minimum Score: 400 be scored. Source: www.acenet.edu Form Codes: SQ500, SR500 EXAM CONTENT OUTLINE The following is an outline of the content areas covered in the examination. The approximate percentage of the examination devoted to each content area is also noted. I. Introduction to the Science of Astronomy – 5% a. Nature and methods of science b. Applications of scientific thinking c. History of early astronomy II. Astrophysics - 15% a. Kepler’s laws and orbits b. Newtonian physics and gravity c. Relativity III. Celestial Systems – 10% a. Celestial motions b. Earth and the Moon c. Seasons, calendar and time keeping IV. The Science of Light – 15% a. The electromagnetic spectrum b. Telescopes and the measurement of light c. Spectroscopy d. Blackbody radiation V. Planetary Systems: Our Solar System and Others– 20% a. Contents of our solar system b. -
Should Earth Get Demoted from Planet Status Just Like Pluto?
IOSR Journal of Applied Physics (IOSR-JAP) e-ISSN: 2278-4861.Volume 10, Issue 3 Ver. I (May. – June. 2018), PP 15-19 www.iosrjournals.org Should Earth Get Demoted From Planet Status Just Like Pluto? Dipak Nath Assistant Professor, HOD, Department of Physics, Sao Chang Govt College, Tuensang;Nagaland, India. Corresponding Author: Dipak Nath Abstract: Clyde.W. Tombough discovered Pluto on march13, 1930. From its discovery in 1930 until 2006, Pluto was classified as Planet. In the late 20th and early 21st century, many objects similar to Pluto were discovered in the outer solar system, notably the scattered disc object Eris in 2005, which is 27% more massive than Pluto. On august-24, 2006, the International Astronomical Union (IAU) defined what it means to be a Planet within the solar system. This definition excluded Pluto as a Planet added it as a member of the new category “Dwarf Planet” along with Eris and Ceres. There were many reasons why Pluto got demoted to dwarf planet status, one of which was that it couldn't clear its orbit of asteroids and other debris. But Earth's orbit is also crowded...too crowded for Earth to be a planet? Earth is indeed in a very crowded orbit, surrounded by tens of thousands of asteroids and other objects. The presence of so many asteroids seems like a serious problem for Earth's claim that it has cleared its neighborhood. And Earth isn't alone in this problem - Jupiter is surrounded by some 100,000 Trojan asteroids, and there's similar clutter around Mars and Neptune. -
Planetarian Index
Planetarian Cumulative Index 1972 – 2008 Vol. 1, #1 through Vol. 37, #3 John Mosley [email protected] The PLANETARIAN (ISSN 0090-3213) is published quarterly by the International Planetarium Society under the auspices of the Publications Committee. ©International Planetarium Society, Inc. From the Compiler I compiled the first edition of this index 25 years ago after a frustrating search to find an article that I knew existed and that I really needed. It was a long search without even annual indices to help. By the time I found it, I had run across a dozen other articles that I’d forgotten about but was glad to see again. It was clear that there are a lot of good articles buried in back issues, but that without some sort of index they’d stay lost. I had recently bought an Apple II computer and was receptive to projects that would let me become more familiar with its word processing program. A cumulative index seemed a reasonable project that would be instructive while not consuming too much time. Hah! I did learn some useful solutions to word-processing problems I hadn’t previously known exist, but it certainly did consume more time than I’d imagined by a factor of a dozen or so. You too have probably reached the point where you’ve invested so much time in a project that it’s psychologically easier to finish it than admit defeat. That’s how the first index came to be, and that’s why I’ve kept it up to date. -
Elements of Astronomy and Cosmology Outline 1
ELEMENTS OF ASTRONOMY AND COSMOLOGY OUTLINE 1. The Solar System The Four Inner Planets The Asteroid Belt The Giant Planets The Kuiper Belt 2. The Milky Way Galaxy Neighborhood of the Solar System Exoplanets Star Terminology 3. The Early Universe Twentieth Century Progress Recent Progress 4. Observation Telescopes Ground-Based Telescopes Space-Based Telescopes Exploration of Space 1 – The Solar System The Solar System - 4.6 billion years old - Planet formation lasted 100s millions years - Four rocky planets (Mercury Venus, Earth and Mars) - Four gas giants (Jupiter, Saturn, Uranus and Neptune) Figure 2-2: Schematics of the Solar System The Solar System - Asteroid belt (meteorites) - Kuiper belt (comets) Figure 2-3: Circular orbits of the planets in the solar system The Sun - Contains mostly hydrogen and helium plasma - Sustained nuclear fusion - Temperatures ~ 15 million K - Elements up to Fe form - Is some 5 billion years old - Will last another 5 billion years Figure 2-4: Photo of the sun showing highly textured plasma, dark sunspots, bright active regions, coronal mass ejections at the surface and the sun’s atmosphere. The Sun - Dynamo effect - Magnetic storms - 11-year cycle - Solar wind (energetic protons) Figure 2-5: Close up of dark spots on the sun surface Probe Sent to Observe the Sun - Distance Sun-Earth = 1 AU - 1 AU = 150 million km - Light from the Sun takes 8 minutes to reach Earth - The solar wind takes 4 days to reach Earth Figure 5-11: Space probe used to monitor the sun Venus - Brightest planet at night - 0.7 AU from the -
Outer Planets: the Ice Giants
Outer Planets: The Ice Giants A. P. Ingersoll, H. B. Hammel, T. R. Spilker, R. E. Young Exploring Uranus and Neptune satisfies NASA’s objectives, “investigation of the Earth, Moon, Mars and beyond with emphasis on understanding the history of the solar system” and “conduct robotic exploration across the solar system for scientific purposes.” The giant planet story is the story of the solar system (*). Earth and the other small objects are leftovers from the feast of giant planet formation. As they formed, the giant planets may have migrated inward or outward, ejecting some objects from the solar system and swallowing others. The giant planets most likely delivered water and other volatiles, in the form of icy planetesimals, to the inner solar system from the region around Neptune. The “gas giants” Jupiter and Saturn are mostly hydrogen and helium. These planets must have swallowed a portion of the solar nebula intact. The “ice giants” Uranus and Neptune are made primarily of heavier stuff, probably the next most abundant elements in the Sun – oxygen, carbon, nitrogen, and sulfur. For each giant planet the core is the “seed” around which it accreted nebular gas. The ice giants may be more seed than gas. Giant planets are laboratories in which to test our theories about geophysics, plasma physics, meteorology, and even oceanography in a larger context. Their bottomless atmospheres, with 1000 mph winds and 100 year-old storms, teach us about weather on Earth. The giant planets’ enormous magnetic fields and intense radiation belts test our theories of terrestrial and solar electromagnetic phenomena. -
The Solar System Cause Impact Craters
ASTRONOMY 161 Introduction to Solar System Astronomy Class 12 Solar System Survey Monday, February 5 Key Concepts (1) The terrestrial planets are made primarily of rock and metal. (2) The Jovian planets are made primarily of hydrogen and helium. (3) Moons (a.k.a. satellites) orbit the planets; some moons are large. (4) Asteroids, meteoroids, comets, and Kuiper Belt objects orbit the Sun. (5) Collision between objects in the Solar System cause impact craters. Family portrait of the Solar System: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune, (Eris, Ceres, Pluto): My Very Excellent Mother Just Served Us Nine (Extra Cheese Pizzas). The Solar System: List of Ingredients Ingredient Percent of total mass Sun 99.8% Jupiter 0.1% other planets 0.05% everything else 0.05% The Sun dominates the Solar System Jupiter dominates the planets Object Mass Object Mass 1) Sun 330,000 2) Jupiter 320 10) Ganymede 0.025 3) Saturn 95 11) Titan 0.023 4) Neptune 17 12) Callisto 0.018 5) Uranus 15 13) Io 0.015 6) Earth 1.0 14) Moon 0.012 7) Venus 0.82 15) Europa 0.008 8) Mars 0.11 16) Triton 0.004 9) Mercury 0.055 17) Pluto 0.002 A few words about the Sun. The Sun is a large sphere of gas (mostly H, He – hydrogen and helium). The Sun shines because it is hot (T = 5,800 K). The Sun remains hot because it is powered by fusion of hydrogen to helium (H-bomb). (1) The terrestrial planets are made primarily of rock and metal. -
Moons, Planets, Solar System, Stars, Galaxies, in Our Universe - an Introduction by Rick Kang Education/Public Outreach Coord
Moons, Planets, Solar System, Stars, Galaxies, in our Universe - An introduction by Rick Kang Education/Public Outreach Coord. Oregon Astrophysics Outreach HIERARCHY: one within another n Moons ORBIT Planets n Planets ORBIT Stars (Suns) n Stars orbited by Planets are Solar Systems (all Stars?) n Solar Systems form from Nebulas and recyle back into Nebulas (dust & gas) n Nebulas and Solar Systems ORBIT within Galaxies (huge Star Cities) n Many Galaxies fill our Universe Moons Our Solar System’s Planets Our Star (the Sun) Our Galaxy (Milky Way) edge-on from within the pancake (STAR CITY) Stars: distant Suns – Birth, Life, Death (Nebulas, Clusters) Solar System Formation Recycling Stars Heavy Duty Recycling: SUPERNOVA – elements galore DRAWING of our Milky Way Galaxy Looking toward Cygnus and toward galactic center Reality Check: n Visualize SOLAR SYSTEM vs. GALAXY Reality Check: n Visualize SOLAR SYSTEM vs. GALAXY n A Solar System is a VERY TINY DOT within a GALAXY…microscopic! n A ¼” paper punchout vs. a huge disk about 150 MILES WIDE (Coast to Bend or Portland to Roseburg!) Our Sister Galaxy, Andromeda, M31 Other Galaxies in Deep Space The HUBBLE ULTRA-DEEP FIELD a tiny swatch of sky-galaxies galore Hundreds of Billions of GALAXIES in our UNIVERSE n We don’t have enough data to figure out where we are within the UNIVERSE nor how big our Universe might be…evidence is it’s expanding! n We are a member of a cluster and a supercluster of galaxies. How do we know that? n If you leave from a place, how far could you travel in a given amount of time? How old is our Universe, how would that relate to its size? .