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Compaction and cementation are two common processes associated with
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
Wind moved layers of sand along as ancient sand dunes. These sand dunes were preserved as rock. This is an example of how sedimentary rock can record information about
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
Sedimentary rocks usually form around
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
These types of rocks form by weathering processes which break down rocks into pebble, sand, or clay particles by exposure to wind, ice, and water.
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
These types of rocks are formed when minerals precipitate out of water
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
The limestone towers in Mono Lake, Ca, formed when dissolved minerals re-formed. These towers are made of
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
Coal is made from the remains of
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
Material that settles out of wind or water
Non-Clastic Sedimentary Rocks
past climate conditions
sedimentation.
plants
Clastic Sedimentary Rocks
sediment
sedimentary rock
near water
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