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Terrestrial Planets. Mercury. Similar Bodies. Moon. Mercury. Discovery Scarf. Scarf Formation. Movie. Caloris Basin. Mercury’s Interior. Mercury’s Formation. Mercury Formation. Venus. Sif Mons Active volcano. Coronae Collapsed volcanic domes. Pancake Volcanoes
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Similar Bodies Moon Mercury
Scarf Formation Movie
Mercury’s Formation Mercury Formation
Sif Mons Active volcano Coronae Collapsed volcanic domes Pancake Volcanoes Eruptions of very thick lava
The Surface of Venus Venus 2 Venus 1
Seismic Waves in the Earth S Waves (transverse) Epicenter P Waves Inner Core Outer Core P Waves (longitudinal) Mantle S Waves
Interior of the Earth Outer Core Inner Core Mantle Crust
Basalts Lunar Maria
Breccias Lunar Highlands
Lunar Origin • Fission Earth-Moon formed as one, rapidly rotating body. Moon spun off of Earth • Pro • Average density matches • Volume of Moon = Volume of Pacific Ocean basin • Con • Can’t account for differences in composition
Lunar Origin • Capture Moon formed elsewhere and was captured on close approach • Pro • can account for composition differences • Con • very difficult to capture in a nearly circular orbit
Lunar Origin • Binary Accretion Earth and Moon formed together but as separate bodies • Pro • might be able to explain differences in composition • Con • most models are stretched to accommodate this idea
Lunar Origin • Collisional Accretion (Giant Impact) Mars-sized body collided with the Earth. The collision spun off part of the mass which became the Moon.
Life on Mars? • In 1996, a team of U.S. scientists said they had discovered evidence of ancient, single-cell life on Mars in remains from a meteorite that plunged to Earth 13,000 years ago.
1997 1976 Face on Mars?
Moons of Mars Phobos Deimos