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Sedimentary Rocks - Transport and Compaction.
Small
pieces of weathered rock
(sediments) are
transported by rivers.
This means that the rock pieces are moved
along
as the river flows towards the
sea.
During transportation, the sediments are sorted according to size.
The largest pieces tend to be deposited
first.
Sand is next to settle out of the water. The smallest
particles are mud or
clay,
and these are moved furthest by the
river and deposited last.
With the passing of time, the
deposits of sediment get thicker
and thicker.
Sediment underneath becomes
increasingly crushed
by the weight of new sediment above.
This is called compaction.
It is this process of compaction
which eventually gives rise to the
sedimentary rock.
The process may take millions of
years.
The largest rock pieces will produce conglomerate.
Sand will produce sandstone.
Mud or clay will produce mudstone or shale.
Younger
sedimentary rocks are usually
found on top of older rocks.
Rock layers generally get older the deeper down
you go.
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