Download presentation
Presentation is loading. Please wait.
Published byBridget Bradley Modified over 8 years ago
1
SOLAR SYSTEM
2
Spheres and Orbits Gravity causes planets To be roughly spherical To orbit in ellipses To hold onto their matter Evidence for round Earth Pictures Horizon Logic Measurements
3
Eratosthenes 200 B.C. calculations
4
Gravity Force of attraction between all objects Affected by mass and distance More mass more gravity Farther apart less gravity Weight changes; mass does not You weigh less on Mt. Everest You weigh more on Jupiter
7
Magnetism Swirling of liquid metal creates electricity Outer core is liquid iron and nickel Electricity creates a magnetic field Magnetic field protects Earth from solar wind Magnetic poles roughly line up with geographic poles
9
Rotation Earth rotates every 24 hours Causes day and night cycles Creates need for time zones Confirmed by Leon Foucault’s pendulum
10
The rotation of the Earth
12
Revolution Earth revolves around the Sun once every year Causes the seasons Shorter days during winter Seasons and day length are affected by tilt of Earth’s axis 23.5°
16
What is the season?
17
Moon Studied directly 1969-1972 Larger than any other moon of the inner planets Formed by impact of small planet with Earth
20
Moon Rotates and revolves every 27.3 days No atmosphere Daily temperatures range from 250° to - 350° F Some water mixed in with the soil No weather no weathering
21
Giant Impact Hypothesis 4.5 billion years ago Planets collide debris orbits Earth eventually comes together to form Moon Slowly moving away from Earth
24
Interior of the moon Divided into layers like Earth No tectonic activity because the interior has cooled too much
26
Satellite Any body that orbits a larger body Mix of falling and moving forward results in round orbits
31
Sun 99.8% of all matter in the solar system Average star Made Hydrogen and Helium in a plasma state
36
Solar Layers Core 27,000,000°C Nuclear fusion releases energy Radiation zone Energy moves away from the core Convection zone Hot particles rise and cooler particles sink Convection: transfer of heat through the movement of heated particles
37
Solar Layers Photosphere Layer that we see Radiates visible light Chromosphere Glows red with heat from the inner layers Corona Millions of miles thick Only visible when photosphere is blocked
41
Solar Layers The sun has no surface Layers and zones can be detected but there are no clear lines Like fire
42
Sunspots Loops of magnetic energy make the Sun cooler in places Form solar flares when the loops break Solar flares release energy and particles Solar wind Produces aurora in Earth’s thermosphere Solar prominence: plasma flows along the loop
47
Earth’s Rotation Spin is counterclockwise when viewed from the North Pole Sun, Moon, stars rise in the East and set in the West
48
Day-Night Cycles Day: time required to rotate once Length determined by whether the North or South is tilted toward the Sun Longer days + Direct Sun = Summer Shorter days + Indirect Sun = Winter Equator: equal day length all year Poles: six months day, six months night
52
Seasons Length of day changes with seasons Angle of sunlight changes with seasons Sun directly overhead = More direct light More direct light = More heat Longer days + Direct Sun = Summer Shorter days + Indirect Sun = Winter
54
The path of the sun in the sky
56
Solar Eclipse Moon moves between the Earth and Sun Photosphere is blocked Corona becomes visible Earth gets dark for a few seconds Aug. 21, 2017
59
Lunar Eclipse Earth between Sun and Moon Moon goes dark because it does not make its own light Shadow of Earth can be seen on the Moon Proof that Earth is round Sep 28, 2015
62
Phases of the Moon Moon reflects sunlight We only see the part of the Moon that is both facing the Sun and the Earth This means the visible portion of the Moon is constantly changing
64
The phases of the Moon
66
Tides Caused by the pull of the Moon on the oceans Sun also affects the tides Spring tide Extreme tides; higher high, lower low Neap tide Moderate tides; lower high, higher low
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.