The Terrestrial Planets

Slides:



Advertisements
Similar presentations
Great Ideas in Science: Lecture 9 – Earth as a Planet Professor Robert Hazen UNIV 301 Great Idea: Earth, one of the planets that orbits the Sun, formed.
Advertisements

Chapter 7 Our Planetary System Earth, as viewed by the Voyager spacecraft.
Our Solar System.
Structure & Formation of the Solar System
WHAT IS THE CURRENT SCIENTIFIC THEORY FOR THE FORMATION OF THE UNIVERSE?
Astronomy Astronomy the study of the planets, stars, galaxies, and all other objects in space. Horsehead Nebula.
The Planets. Mercury The Messenger God 0 Closest planet to the Sun AU 0 Main gases: Na, O, He -300 °F at night 800 °F during the day No moons 0.
1. L ist the 9 planets in our solar system. Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Pluto (dwarf planet)
The Universe. The Milky Way Galaxy, one of billions of other galaxies in the universe, contains about 400 billion stars and countless other objects. Why.
1 The Solar System An Inventory. 1 What is the Solar System? Answer: The system of objects in the solar neighborhood (near the Sun) The sun –Has a luminosity.
Copyright © 2012 Pearson Education, Inc. The Formation of the Solar System.
THE PRIMORDIAL EARTH Hadean and Archean Eons Solar System Includes: Sun Planets Moons Asteroids Comets.
Solar System Formation. Age of the Solar System The oldest rocks found on Earth are about 4.55 billion years old, not native but meteorites which fall.
An Introduction to Astronomy Part VI: Overview and Origin of the Solar System Lambert E. Murray, Ph.D. Professor of Physics.
Chapter 27 – The Planets and the Solar System Page 586 Do you think it is possible to count the rings of Saturn? The rings look solid in the image, do.
The Jovian Planets Chapter 7. Topics Jupter, Saturn, Uranus, Neptune How do we know? Why do we care? What is common about the outer planets? What is peculiar.
Seconds Remaining: What makes up the solar system?
The Solar System.
Comparative Planetology I: Our Solar System
Eight Planets A Write On Activity.
Space Ch 3 Notes. Bell Work 2/23/10 Draw a diagram showing the orbit of Earth and the orbit of Earth’s Moon. Label the Sun, Earth, the Moon, Earth’s orbit,
The Planets in our Solar System
Our Solar System. Our solar system in order from the sun 1.Mercury 2.Venus 3.Earth 4.Mars 5.Asteroid Belt 6.Jupiter 7.Saturn 8.Uranus 9.Neptune 10.Kuiper.
There are two broad categories of planets: Earthlike and Jupiter like
Ch 27 Review Planets & the Solar System. Name the inner planets.
Nine Planets A Write On Activity In this activity you will:  Learn about the solar system.  Practice your knowledge in an interactive game.  Select.
Comparative Planetology I: Our Solar System Chapter Seven.
Solar System All masses that orbit the sun plus the sun!
Solar System. MILKY WAY 200 billion stars Diameter LY Height at center LY Solar System is LY from center.
Terrestrial Planets Earthlike Worlds of Rocks and Metals.
Review 2 What was the solar nebula? What was it made of? How did gravitational collapse affect the Solar nebula? How does conservation of energy and angular.
Solar System Review Game. 1.Which planet’s day is longer than its year? 2.Which planet has two moons? What are their names? 3.Which planet has six thin.
Big Bang theory Parts of our solar system Planet characteristics Galaxies Constellations Nebulas.
Phys141 Principles of Physical Science Chapter 15 The Solar System Instructor: Li Ma Office: NBC 126 Phone: (713)
A Survey of the Solar System. Geocentric vs. Heliocentric.
Chapter 11 The Structure of the solar system. Distances in Space Distances are sol large in the Solar System that you can’t just use meters or kilometers.
NEW CHAPTER Our Solar System CHAPTER the BIG idea Planets and other objects form a system around our Sun. Planets orbit the Sun at different distances.
Solar System Notes Solar System - An area that normally has one star with planets, moons, asteroids and comets orbiting the star. Our solar system has.
Origins of the Planets and Moons Our sun was the center of a nebula (cloud of dust and gas). Planets formed when bits of matter first collided and aggregated.
Universe Eighth Edition Universe Roger A. Freedman William J. Kaufmann III CHAPTER 7 Our Solar System CHAPTER 7 Our Solar System.
It is estimated that our solar system is 5 billion years old.
WARM UP Can you list the planets in order?. Our Solar System.
Formation of our solar system: The nebular hypothesis (Kant, 1755) Hydrogen (H), He (He) and “stardust” (heavier elements that were formed in previous.
HNRS 227 Fall 2005 Chapter 13 The Solar System presented by Dr. Geller 27 October 2005.
Question 1 Which of the following are terrestrial planets? 1)only Earth 2)the Earth, Moon, and Venus 3)Mercury, Venus, Earth, and Mars 4)Mercury, Venus,
The Inner Planets Chapter Terrestrial Planets Mercury, Venus, Earth, Mars Mostly solid rock with metallic cores Impact craters.
ORIGINS Oceans & Continents Crust Earth Solar System Universe.
ORIGINS Oceans & Continents Crust Earth Solar System Universe.
The Sun & The Solar System. Structure of the Sun The Sun has layers which can be compared to the Earth’s core, mantle, crust, and atmosphere All of these.
The Solar System. The Solar System Contains: One star (the sun). Nine planets (well now there’s eight planets and 3 dwarf planets). 157 moons (at last.
The Solar System.
NEW CHAPTER Our Solar System CHAPTER the BIG idea Planets and other objects form a system around our Sun. Planets orbit the Sun at different distances.
1. The Universe and the Solar System 2 © Zanichelli editore 2015.
Planetary Chart PlanetAUMassTypeAtmosphereMoons Mercury Venus Earth Mars Inner Planets Jupiter Saturn Uranus Neptune *Pluto.
Tour of the Solar System. General Properties of the Solar System There are two classes of planets:  The Terrestrial planets are small, solid bodies (rocks.
Hosted by Type your name here Choice1Choice 2Choice 3Choice
The Solar System.
Our Solar System Planets and other stuff!. The Sun Produces energy through nuclear fusion. ( 2 hydrogen nuclei fusing to make helium. Very hot: up to.
Cosmic address The astronomical unit and the light year Dark matter and dark energy Atoms Matter Forces.
Thought Question What does the solar system look like as a whole? Why does the solar system look the way it does? Can we explain how the solar system.
The Solar System What is our little corner of the Milky Way Galaxy like?
The Formation of Our Solar System The Nebular Hypothesis.
1 Earth and Other Planets 3 November 2015 Chapter 16 Great Idea: Earth, one of the planets that orbit the Sun, formed 4.5 billion years ago from a great.
Terrestrial Planets (Chapter 17). Student Learning Objectives Identify & describe each Terrestrial Planet Compare & contrast the Terrestrial planets with.
Planets. The terrestrial planets and some large moons.
EARTH AND THE SOLAR SYSTEM
Our Solar System.
Notes: Our Solar System
The Terrestrial Planets
Presentation transcript:

The Terrestrial Planets Chapter 6 Getting to know our first cousins

Topics Solar System--the big picture Earth, Moon, Mercury, Venus, Mars How do we know? Why do we care? What is common about the terrestrial planets? What is peculiar to each of these planets?

Models The test of all knowledge is experiment. We use models to understand how we think the Solar System, including the Sun and planets, formed. Models can be used to make predictions. Ultimately the accuracy of the predictions reveal the efficacy of our models. As we discuss “what happened” remember that these are based on models. Perhaps at some point, experiments will point us to new models.

Contents of the Solar System All masses that orbit the Sun plus the Sun! One star - called the Sun nine planets Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune, and Pluto more than 60 moons (often called natural satellites) tens of thousands of asteroids countless comets dust and gas Our Sun constitutes nearly 99.44% of the mass of the Solar System

Terrestrial planets (Earth-like): Mercury, Venus, Earth, Mars

What makes them similar? small--1/100 radius of the Sun Size orbit at 0.4 to 1.5 AU Location Moons few none Rings composition dense rock and metal

Density density = mass/volume Density of water = 1.0 g/cm3 Density of wood = 0.5 g/cm3 Density of silicate rock = 3.0 g/cm3 Density of iron = 7.8 g/cm3

Composition? Density Mercury 5.4 g/cm3 Venus 5.2 g/cm3 Earth 5.5 g/cm3 Mars 3.9 g/cm3 So what are these planets mostly made of?

Earth Mass and radius give mass/volume = bulk density, about 5.5 times water Key to composition, internal structure, verified by seismic waves Metals: bulk density about 8 g/cm3; rocks: about 3 g/cm3; earth: about 50-50 metals/rocks

How do we measure density? Mass & spherical shape (Newton’s law of gravitation) Radius (from angular size and distance) Bulk density (mass/volume) => infer general composition

Evolution of a planet - internal effects Energy flow from core to surface to space Source: Stored energy of formation, radioactive decay Results in volcanism, tectonics

Evolution of a planet - external effects Impact cratering: Solid objects from space Bomb-like explosion; many megatons (H-bomb!) Creates circular impact craters on solid surfaces

Earth Composition Volcanism Plate tectonics Atmosphere Craters Magnetic field

Aurora caused by charged particles emitted from the Sun interacting with the Earth’s atmosphere charged particles are most highly concentrated near the poles due to their motion in the earth’s magnetic field.

Craters Barringer meteor crater Largest, most well-preserved impact crater Fist crater recognized as an impact crater (~1920s) 49,000 years old

Earth’s layers Core (metals) Mantle (dense rocks) Crust (less dense rocks) Partially or fully melted material separates by density (differentiation) Age of earth ~ 4.6 Gy ~age of meteorite material and lunar material Astronomy: The Evolving Universe, Michael Zeilik

Earth’s age Radioactive dating: Decay of isotopes with long half-lives; for example, uranium-lead, rubidium-strontium, potassium-argon. Gives elapsed time since rock last melted and solidified (remelting resets clock) Oldest rocks about 4 Gy + 0.5 Gy for earth’s formation => about 4.5 Gy for earth’s age

Earth’s Tides due to the variation of the gravitational force of the moon on the earth two tides per day

Tides The Sun also has an effect on the tides. Eventually the earth and moon will slow down and the moon will recede.

Moon Origin maria craters fission? capture? condensation? ejection of a gaseous ring? maria craters similar in density to Earth’s mantle but proportion of elements is not exactly like the Earth’s

Mercury rotational period is 2/3 of its orbital period -- hot and cold hard to view from Earth highly elongated orbit iron core small magnetic field thin atmosphere, mostly sodium it looks like the Moon

Venus ...where the skies are cloudy all daayyyy. dense atmosphere, mostly CO2 high surface pressure and temperature rotation (117 E-days), revolution (225 E-days) rotates about its axis in the “wrong direction” similar density and size as Earth two continents, one continental plate no moons

Mars small in size two moons thin atmosphere, mostly CO2 4 seasons (why?) smaller density (what would this mean?) polar caps (mostly CO2, some water) canyons (evidence of flowing water?)

What’s important? similarities of terrestrial planets peculiarities of terrestrial planets how we know things like the period of rotation, composition, and age of a planet, to name a few

For Practice Looking through this chapter, make a list of similar features and different features of the terrestrial planets. Identify each instant where the book described something we know about a planet and how we know it.