You will be able to… - LWC Earth Sciencelwcearthscience.yolasite.com/resources/Ch22.3...
Transcript of You will be able to… - LWC Earth Sciencelwcearthscience.yolasite.com/resources/Ch22.3...
You will be able to… •Describe how the physical features of the lunar surface were created. •Explain the history of the moon.
22.3 Earth’s Moon
22.3 Craters
• A crater is the depression at the summit of a volcano or a depression produced by a meteorite impact.
• Rays are any of a system of bright, elongated streaks,
sometimes associated with a crater on the moon.
Formation of a Crater
• This is a view of the Aristarchus and Herodotus craters
taken from orbit during the Apollo 15 mission
Barringer Meteor Crater, Arizona
• Diameter: 1.186 kilometers (.737 miles); age: 49,000 years
22.3 Earth’s Moon Formation
When the solar system was forming, a body the size
of Mars impacted Earth. The resulting debris was
ejected into space, began orbiting around Earth, and
eventually united to form the moon.
22.3 The Lunar Surface
• Most of the lunar surface is made up of densely pitted, light-colored areas known as highlands.
Highlands
Highlands
22.3 The Lunar Surface
• The dark areas on the moon.
• Ancient beds of basaltic lava, originated when asteroids punctured the lunar surface, letting magma bleed out.
• Younger than the Highlands
Maria – Latin for sea
• A rille is a long channel associated with lunar maria. A rille looks similar to a valley or a trench.
Highlands
Maria
22.3 The Lunar Surface
Regolith
• The lunar regolith is 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.
The Moon’s Surface
Mare Tranquillitatus
(Sea of Tranquility)
Mare Imbrium
(Sea of Rains)
Kepler
Crater
Copernicus
Crater
Major Topographic Features of the Moon