1. Rocks made of bits & pieces of other rocks.
Sedimentary Rocks
Rocks made of bits & pieces of other rocks.

2. Sedimentary Rocks
Igneous rocks are the most common rocks on Earth, but because most of them exist below the surface you might not have seen too many of them.
75 percent of the rocks exposed at the surface are sedimentary rocks.

3. What is sediment?
Sediments are loose materials such as rock fragments, mineral grains, and bits of shell that have been moved by wind, water, ice, or gravity.
Sediments come from already-existing rocks that are weathered and eroded.
Sedimentary rock forms when sediments are pressed and cemented together, or when minerals form from solutions.

4. already-existing rocks that are weathered and eroded
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded

5. Stacked Rocks Sedimentary rocks often form as layers.
The older layers are on the bottom because they were deposited first.
Sometimes, forces within Earth overturn layers of rock, and the oldest are no longer on the bottom.

6. Classifying Sedimentary Rocks
Sedimentary rocks can be made of just about any material found in nature.
Sediments come from weathered and eroded igneous, metamorphic, and sedimentary rocks.
Sediments also come from the remains of some organisms.
The composition of a sedimentary rock depends upon the composition of the sediments from which it formed.

7. Classifying Sedimentary Rocks
Sedimentary rocks are classified by their composition and by the manner in which they formed.
The three types of sedimentary rocks are
Detrital
Chemical
Organic.

8. already-existing rocks that are weathered and eroded
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical

9. Detrital Sedimentary Rocks
Detrital sedimentary rocks are made from the broken fragments of other rocks.

10. Organic Detrital Chemical
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
Broken fragments of other rocks

11. Weathering & Erosion helps to get the materials to make detrital sedimentary rocks.
When rock is exposed to air, water, or ice, it breaks down chemically and mechanically.
This process, which breaks rocks into smaller pieces, is called weathering.
The movement of weathered material is called erosion.

12. Organic Detrital Chemical erosion weathering
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
Broken fragments of other rocks
weathering
erosion

13. Compaction helps form detrital sedimentary rocks
Where sediments are deposited, layer upon layer builds up.
Pressure from the upper layers pushes down on the lower layers.
If the sediments are small, they can stick together and form solid rock. This process is called compaction.

14. Organic Detrital Chemical erosion weathering compaction
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
compaction
Broken fragments of other rocks
weathering
erosion

15. Cementation also helps form detrital sedimentary rocks.
If sediments are large, like sand and pebbles, pressure alone can’t make then stick together
Large sediments have to be cemented together.
As water moves through soil and rock, it picks up materials released from minerals during weathering.
The resulting solution of water and dissolved materials moves through open spaces between sediments.

16. Detrital Sedimentary Rock Classification
Detrital Sedimentary Rocks are named according to the shapes and sizes of the sediments that form them.
Conglomerate and breccia both form from large sediments.

17. Organic Detrital Chemical erosion weathering compaction
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
compaction
Broken fragments of other rocks
Examples: Sandstone & conglomerate
cementation
weathering
erosion

18. Chemical Sedimentary Rocks
Chemical sedimentary rocks form when dissolved minerals come out of solution.
Minerals collect when seas or lakes evaporate. The deposits of minerals that come out of solution form sediments and rocks.
Chemical sedimentary rocks are not made from pieces of preexisting rocks.

19. Organic Detrital Chemical erosion weathering compaction cementation
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
compaction
Broken fragments of other rocks
Dissolved minerals come out of solution
cementation
weathering
erosion

20. Example of Chemical Sedimentary Rock
Calcium carbonate is carried in solution in ocean water.
When calcium carbonate (CaCO3) comes out of solution as calcite and its many crystals grow together, limestone forms.
Limestone also can contain other minerals and sediments, but it must be at least 50 percent calcite.
Limestone usually is deposited on the bottom of lakes or shallow seas.

21. Example of Chemical Sedimentary Rock
Large areas of the central United States have limestone bedrock because seas covered much of the country for millions of years.
It is hard to imagine Kansas being covered by ocean water, but it has happened several times throughout geological history.

22. Example of Chemical Sedimentary Rock
When water that is rich in dissolved salt evaporates, it often deposits the mineral halite.
Halite forms rock salt.
Rock salt deposits can range in thickness from a few meters to more than 400 m.
Companies mine these deposits because rock salt is an important resource.

23. Organic Detrital Chemical erosion weathering compaction cementation
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
compaction
Broken fragments of other rocks
Dissolved minerals come out of solution
cementation
Halite
limestone
weathering
erosion

24. Organic Sedimentary Rock
Rocks made of the remains of once-living things are called organic sedimentary rocks.
One of the most common organic sedimentary rocks is fossil-rich limestone.
Like chemical limestone, fossil-rich limestone is made of the mineral calcite.
Fossil-rich limestone mostly contains remains of once-living ocean organisms.

25. Organic Detrital Chemical erosion weathering compaction cementation
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
compaction
Broken fragments of other rocks
Made of the remains of once living things
Dissolved minerals come out of solution
cementation
Halite
limestone
weathering
erosion

26. Example of Organic Sedimentary Rock
Chalk is another organic sedimentary rock that is made of microscopic shells.
When you write with
naturally occurring
chalk, you’re crushing
and smearing the calcite-shell remains of once-living ocean organisms.

27. Example of Organic Sedimentary Rock
Another useful organic sedimentary rock is coal.
Coal forms when pieces of dead plants are buried under other sediments in swamps.
These plant materials are chemically changed by microorganisms.
The resulting sediments are compacted over millions of years to form coal, an important source of energy.

28. Organic Detrital Chemical coal erosion chalk weathering compaction
forms when sediments are pressed and cemented together, or when minerals form from solutions
already-existing rocks that are weathered and eroded
Organic
Detrital
Chemical
compaction
Broken fragments of other rocks
Made of the remains of once living things
Dissolved minerals come out of solution
cementation
chalk
coal
Halite
limestone
weathering
erosion

29. How a little bit of heat & pressure transform rocks!
Metamorphic Rocks
How a little bit of heat & pressure transform rocks!

30. What is a metamorphic rock?
The term "metamorphic" means "to change form."
Any rock (igneous, sedimentary, or metamorphic) can become a metamorphic rock. If rocks are buried deep in the Earth at high temperatures and pressures, they form new minerals and textures all without melting. If melting occurs, magma is formed, starting the rock cycle all over again.

31. To change form
Other rocks are exposed to high heat & pressure

32. Metamorphic Rock Types
There are two types of metamorphic rocks.
Each is classified according to its composition and texture.
Foliated
Nonfoliated.

33. Non-Foliated Foliated To change form
Other rocks are exposed to high heat & pressure
Foliated
Non-Foliated

34. Foliated Metamorphic Rocks
FOLIATED metamorphic rocks are those in which the minerals have been flattened and pushed down into parallel layers. The bands in foliated metamorphic rock look like pages in a book.
Examples of foliated rocks are slate, shale, and gneiss.

35. Flattened & pushed into parallel layers
To change form
Other rocks are exposed to high heat & pressure
Foliated
Non-Foliated
Flattened & pushed into parallel layers
slate
gneiss
shale

36. Non-foliated
NON-FOLIATED metamorphic rocks do not display layers. Rather, they are massive structures with no obvious banding. The mineral grains grow and rearrange, but they don’t form layers.
A good example of non-foliated rock is quartzite, the smooth-textured, metamorphosed form of the mineral quartz.
A coarse-textured non-foliated rock is marble.
Anthracite, or hard coal, is a non-foliated rock that forms when intense pressure drives gases out of soft coal, causing it to harden.

37. Flattened & pushed into parallel layers
To change form
Other rocks are exposed to high heat & pressure
Foliated
Non-Foliated
layers
Anthracite coal
Flattened & pushed into parallel layers
Quartzite
slate
gneiss
marble
shale