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Sedimentary Rocks - Weathering and Erosion.
Sediments have come from the weathering and erosion of surface
rocks.
The original surface rocks were
igneous rocks,
formed from the cooling of molten magma.
Surface rocks today are igneous, sedimentary or metamorphic.
Weathering breaks a
rock down into small pieces.
The two main
processes are exfoliation and
freeze-thaw
weathering.
Exfoliation occurs when rocks are heated and
expand in the heat of the day
and then cool and contract in the cold
of night.
Thin slithers of rock tend to flake
off the surface,
and these can then be broken further
into tiny pieces.
Think of exfoliation as flaking.
Freeze-thaw
weathering occurs when water
gets into cracks in rock
and then freezes (below 0 °C) in
cold weather.
Water expands when it freezes and turns to ice,
and the expansion can cause the
rock to split and fragment.
In warmer weather (above 0 °C) the ice melts (called
thawing),
and new cracks are exposed allowing the process to repeat
itself.
Erosion is a slow
process of wearing away
weathered rock
by action of the wind, rivers and
waves.
What happens to the small pieces of rock after weathering and erosion?
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Copyright © 2008 Dr. Colin France. All Rights Reserved.