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22.3 Earth’s Moon

Earth science 22.3

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Page 1: Earth science 22.3

22.3 Earth’s Moon

Page 2: Earth science 22.3

Crater • The depression at the summit of a volcano or

that which is produced by a meteorite impact.

Page 3: Earth science 22.3

Ray• Any of a system of bright elongated streaks,

sometimes associated with a crater on the moon.

Page 4: Earth science 22.3

Mare• The Latin name for smooth areas of the moon

formerly thought to be seas.

Page 5: Earth science 22.3

Rille• Long channel associated with lunar maria; a

rille looks similar to a trench or a valley.

Page 6: Earth science 22.3

Lunar Regolith• A thin, gray Layer

on the surface of the moon, consisting of loosely compacted, fragmented material believed to have been formed by repeated impacts of meteorites.

Page 7: Earth science 22.3

Key Concept

• Most craters were produced by the impact of rapidly moving debris.

Page 8: Earth science 22.3

Key Concept

• Maria, ancient beds of basaltic lava, originated when asteroids punctured the lunar surface, letting magma bleed out.

Page 9: Earth science 22.3

Key Concept

• The most widely accepted model for the origin of the moon is that when the solar system was forming, body the size of mars impacted Earth.