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Soil is formed from decayed vegetable matter (dead leaves and plants),
mineral grains, and larger pieces of rock. Creatures, such as earthworms,
help the decomposition process by mixing the soil. The process by which
rocks are often broken down into smaller pieces is called weathering .
Chemical weathering occurs when minerals are dissolved by water. Some
minerals break down or dissolve quickly. Others, such as quartz, are not
dissolved but stay behind in the soil as stones. The action of burrowing
animals, animals, insects, and growing plants is called physical weathering.
Attrition (grinding down) is another kind of physical weathering and it
occurs when wind-blown particles rub against each other. This kind of
weathering occurs mainly in dry areas, such as deserts. You can see how
attrition works simply by shaking some sugar cubes together in a glass
jar.
Fill the gap with layers of soil and sand to the top. Press the soil down
lightly. Gently place the worms on top of the soil, and cover them with
rotting leaves.
Cover the sides with black paper. Keep the soil moist. After a few days,
remove the paper to see how the worms have tunneled away and dragged leaves
into their burrows.
Put on a pair of gardening gloves and place a trowel full of soil into
the sieve. Shake the sieve over a piece of paper for about a minute or
so. Tap the side of the sieve gently, to help separate the different parts
of the soil. Are there chunks that will not go through the sieve? Can
you see if any of the chunks are rock?
Use a pair of scissors to cut the top off a large, clear plastic bottle.
Ask an adult to help, if you need to. You can throw away the top part
of the bottle. Use a spoon to scoop some gravel, earth, and sand into the bottom of the
bottle. Add water to the mixture, until it nearly reaches to the top of
the bottle. Stir vigorously to mix the stones, earth, and sand with the water. In a
river, soil and rock particles are mixed together and carried along by
the moving water.
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