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Children's Corner Sedimentary Rocks
A Special Place for Junior Rock Hounds

  Sedimentary Rocks
The earth's surface is constantly being eroded. This means that rocks are broken up into
smaller pieces by weathering. Conditions such as wind, water, and ice turn small pieces
of rock turn into pebbles, gravel, sand, and clay. They tumble down rivers and streams.
These pieces settle in a new place and begin to pile up and the sediments form flat
layers. Over a long period of time, the pieces become pressed together and form solid
rock called sedimentary rock. Most sedimentary rocks form under water. Most of the
earth has been covered by water some time in the past. 70% of the earth is currently
covered by water. Sedimentary rocks are very common all over the world. It is also
interesting that 70% of all rocks on earth are classified as sedimentary rocks. Fossils are
found most often in Sedimentary rocks. Fossils are the remains of plants and animals
from millions of years ago that got mixed in the sedimentary process.

Clastic sedimentary rock Clastic sedimentary rocks are the group of rocks most people
think of when they think of sedimentary rocks. Clastic sedimentary rocks are made up of
pieces (clasts) of pre-existing rocks. Pieces of rock are loosened by weathering, then
transported to some basin or depression where sediment is trapped. If the sediment is
buried deeply, it becomes compacted and cemented, forming sedimentary rock. Clastic
sedimentary rocks may have particles ranging in size from microscopic clay to huge
boulders. Their names are based on their clast or grain size. The smallest grains are
called clay, then silt, then sand. Grains larger than 2 millimeters are called pebbles. Shale
is a rock made mostly of clay, siltstone is made up of silt-sized grains, sandstone is made
of sand-sized clasts, and conglomerate is made of pebbles surrounded by a matrix of
sand or mud.

Organic sedimentary rock Organic sedimentary rocks form when large numbers of living
things die, pile up, and are compressed and cemented to form rock. Accumulated carbon-
rich plant material may form coal. Deposits made mostly of animal shells may form
limestone, coquina, or chert.

Chemical sedimentary rock Chemical sedimentary rocks are formed by chemical
precipitation. The
Stalactites and Stalagmites you see in caves form this way, so does
the rock salt that table salt comes from. This process begins when water traveling
through rock dissolves some of the minerals, carrying them away from their source.
Eventually these minerals can be redeposited, or precipitated, when the water
evaporates away or when the water becomes over-saturated with minerals.
Here is a "trick" to remember the differences between Stalactites and Stalagmites:
Stalac
tites hang tight to the ceiling; Stalagmites make mounds on the floor.

Here are some things to look for in sedimentary rocks.
-texture and composition are layered
-Often contains fossils
-Often has layers, flat or curved
-Usually composed of pieces cemented or pressed together
-Has great color variety
-Particle size may be the same or vary
-Usually has pores between pieces
-May have cross-bedding, mud cracks, worm burrows, raindrop impressions

Here are some photographs of some common sedimentary rocks. Look for these same
forms, patterns and structure in the rocks you find during your rock hunting trips.
See…you have made another step on the road to  becoming a genuine rockhound. When
you find your rocks, you can number them as we do and make a list to remember their
names.

Common Sedimentary Rocks
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Stalactites hang from
above and point down
Stalagmites form on
the ground and point
up