Craters Investigation

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Craters Investigation

 

In this experiment I am going to investigate one factor that causes craters to be different sizes. I am going to do this by dropping a ball bearing with a mass of 63.7g, from varying heights into a tub of sand and then measuring the width of the crater it made.

Research

 

On the Moon, craters usually measure up to 200 (320 miles) or more in diameter. Meteorites hitting the lunar surface at high velocity produced most of the large craters. Many of the smaller ones - those measuring less than 1km (0.6 mile) across could have been formed by explosive volcanic activity.

Many craters have a surrounding ring: this is usually quite low although a typical one may be about 1500m (4920 feet) above the surrounding landscape. In many cases, there is a central peak or several peaks within a crater.

The darker areas of the Moon, known as Maria, have relatively few craters. They are thought to be huge lava flows that spread over an area after most of the craters have already been formed.

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Apparatus

· 1 Tub of sand

· 1 Ruler

· 1 Metal Ball Bearing (63.7g)

· 1 Metre Ruler

Method

 

1. Set up the apparatus (as shown in the diagram)

2. Lift the Ball Bearing to a height of 10cm and drop into the tub of sand.

3. Place the end of the ruler at one edge of the crater and measure to the other side. This gives the width of the ...

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