Planet Processes
Impact Craters
Instruction:
We
will be using the Exploring the Planets Software for this lesson.
This page will provide you notes and comments on what we cover in the program.
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Slide Number
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Canada's Manacovagan Crater, gives us an example
of cratering on the Earth. Hundreds of craters have been discovered
on Earth. Many are buried by sediments, others are so large they
can only be seen from satellites.
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The Manacovagan crater is 65 km across. A short
video shows how over time it has eroded down into a circular lake.
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Barringer Crater in Arizona is probably the most
famous. This aerial view shows the floor below the surface level
and the circular rim.
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This 1 km wide crater is small compared to most craters
but would need 20 million tons of TNT to be created today.
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This slide shows a close up view of the rocks making
the rim. One of the boulders has a man standing next to it showing
that it is several stories tall and as big as a building.
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The formation of a crater step by step. First
the approaching asteroid hits while traveling at nearly 10 km/s
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Next the energy of motion is converted into heat.
Most of the original meteor is vaporized. A shock wave starts compressing
the surface rock layers downward.
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The compressional shock wave shatters the surrounding
layers of rock.
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Like a balloon that has been pushed in, the compressed
layers of rock rebound, throwing fragmented rock, dust and dirt into the
air.
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Loose material along the sides collapses into the
crater forming Breccia.
In class we observed samples of volcanic and sedimentary breccia.
Breccia is a rock composed of the jagged fragments
and pieces of other rock.
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This slide shows a video of impact studies.
It can be played in slow motion to see the steps of an impact.
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There has also been an observed impact of a comet
on Jupiter in 1994.
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The Jupiter impacts created fireballs larger than
the size of the Earth. The comets hit at 60 Km/sec.
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Various pictures of the comet impact sites.
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An upclose view of a young fresh crater.
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Activity: Asteroid Impacts on the Moon.
This sldie provides data fot the size and depth of asteroid impacts.
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Activity: Continued. Graphing the relationship
between size and depth.
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Answer: For every km in crater width
the crater is .2km deep.
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This relationship does not work for giant craters
which often show central peaks, terraced walls, and flat floors.
This is the end of the Planet Processes Impact
Cratering Notes. Click here
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