1. Rocks, Minerals & the Rock Cycle

2. Objectives Chapter 16 Define the term mineral.
Section 1 Minerals and Mineral Resources
Chapter 16
Objectives
Define the term mineral.
Explain the difference between a metal and a nonmetal, and give two examples of each.
Describe three processes by which ore minerals form.

3. Mineral Resources
We depend on the use of mineral resources in almost every aspect of our daily life.
However, our dependence on minerals has not come without a price.
The current challenge is to obtain the minerals that an ever-increasing world population demands at minimal cost to the environment.

4. Mineral Consumption per Person (U.S.)

5. What Is a Mineral?
A mineral is a naturally occurring, usually inorganic solid that has a characteristic chemical composition, an orderly internal structure, and a characteristic set of physical properties.
Minerals are made up of atoms of a single element, or of compounds. A compound consists of atoms of two or more elements chemically bonded together.
The atoms that make up minerals are arranged in regular, repeating geometric patterns.

6. What Is a Mineral? Chapter 16
Section 1 Minerals and Mineral Resources
Chapter 16
What Is a Mineral?
The arrangement of the atoms, along with the strength of the chemical bonds between them, determine the physical properties of minerals,
Some elements, called native elements, are considered minerals. These include the elements gold, silver, and copper.
Most minerals, however, are compounds.
The mineral quartz is made up of silica, which consists of one silicon atom and two oxygen atoms.

7. Section 1 Minerals and Mineral Resources
Chapter 16
Ore Minerals
An ore mineral is a mineral that contains one or more elements of economic value.
During the mining process, gangue minerals, minerals with no commercial value, are extracted along with ore minerals.
Ore minerals, once separated from the gangue minerals, are refined using various methods to extract the valuable elements they contain.
For mining to be profitable, the price of the final product must be greater than the costs of extraction and refining.

8. Section 1 Minerals and Mineral Resources
Chapter 16
Ore Minerals

9. Metallic Minerals Chapter 16
Section 1 Minerals and Mineral Resources
Chapter 16
Metallic Minerals
Ore minerals are either metallic or nonmetallic.
Metals have the following characteristics:
can conduct electricity
have shiny surfaces
are opaque
Many valuable metallic minerals are native elements, such as gold, silver, and copper.
Other important ore minerals are compounds of metallic minerals with nonmetallic elements.

10. Nonmetallic Minerals Chapter 16
Section 1 Minerals and Mineral Resources
Chapter 16
Nonmetallic Minerals
Nonmetals have the following characteristics:
tend to be good insulators
may have shiny or dull surfaces
may allow light to pass through
Nonmetallic minerals can also be native elements or compounds.

11. How Do Ore Minerals Form?
Section 1 Minerals and Mineral Resources
Chapter 16
How Do Ore Minerals Form?
Economically important ore deposits form in a variety of ways, both on and beneath Earth’s surface.
The types of mineral that form depend on the environment in which they form.

12. Mineral Environments Chapter 16
Section 1 Minerals and Mineral Resources
Chapter 16
Mineral Environments

13. Hydrothermal Solutions
Section 1 Minerals and Mineral Resources
Chapter 16
Hydrothermal Solutions
Hot, subsurface waters that contain dissolved minerals are called hydrothermal solutions.
Hydrothermal solutions dissolve minerals as they flow through cracks in rocks.
New minerals crystallize out of these solutions and then fill fractures to form ore deposits called veins.
Many economically valuable metallic ores form in this way.

14. Section 1 Minerals and Mineral Resources
Chapter 16
Evaporites
When water in the seas or lakes evaporate, they leave behind deposits of salts called evaporites.
Evaporites form in arid regions where rates of evaporation are high.
Halite (rock salt) and gypsum are important evaporite minerals.

15. Mineral Resources and Their Uses
Section 1 Minerals and Mineral Resources
Chapter 16
Mineral Resources and Their Uses
Certain metals are of major economic and industrial importance.
Some metals can be pounded or pressed into various shapes or stretched very thinly without breaking. Others conduct electricity well.
Often two or more metals are used to form alloys, which combine the most desirous properties of the metals used to make them.

16. Mineral Resources and Their Uses
Section 1 Minerals and Mineral Resources
Chapter 16
Mineral Resources and Their Uses

17. Rocks And The Rock Cycle

18. Why Are Rocks Important To Us?
Buildings
Roads
Bridges
Concrete
Extract minerals – like iron (Fe) to make steel
Toothpaste
Salt
Sandpaper
Decorations
Jewelry

19. 1. Why is it important to have a basic understanding of the rock cycle?
Rocks contain clues about the environment. Helps us understand the formation of the earth.

20. 2. Rock
Any solid mass of minerals or mineral-like matter

21. 3. Do most rocks occur as one mineral or as a mixture of minerals?

22. 4. Some rocks are made of non-mineral material, can you name one?
Coal

23. Coal - begins as layers of plant matter accumulate at the bottom of a body of water. For the process to continue the plant matter must be protected from biodegradation and oxidization, usually by mud or acidic water. This trapped atmospheric carbon in the ground in immense peat bogs that eventually were covered over and deeply buried by sediments under which they metamorphosed into coal.
Over time, the chemical and physical properties of the plant remains (believed to mainly have been fern-like species antedating more modern plant and tree species) were changed by geological action to create a solid material.
Coal, a fossil fuel, is the largest source of energy for the generation of electricity worldwide.

26. 5. Explain the rock cycle.
A continuous process that causes rock to change from one form to another 2 1 3 5 4

28. The Rock Cycle
The Rock Cycle is a group of changes, this change does not necessarily have to be a chemical change.
Igneous rock can change into sedimentary rock or into metamorphic rock.
Sedimentary rock can change into metamorphic rock or into igneous rock.
Metamorphic rock can change into igneous or sedimentary rock.
Almost all of rock today that we have on earth is made up of all the same stuff as the rocks that dinosaurs and other ancient life forms walked, crawled, or swam over
While the stuff that rocks are made of has stayed the same, the rocks themselves, have not
Over time rocks are recycled into other rocks
Moving tectonic plates are responsible for destroying and forming many types of rocks

29. 6. List the 3 types of rocks
Igneous
Metamorphic
Sedimentary

30. 7. Igneous Rocks
Igneous rock forms when magma cools and makes crystals.
Magma is a hot liquid made of melted minerals. When magma pours onto the earth’s surface it is called lava. The minerals can form crystals when they cool.
Igneous rock can form underground, where the magma cools slowly. Or, igneous rock can form above ground, where the magma cools quickly.
The crystals grow together and form one igneous rocks.

31. 8. What kind of igneous rocks form when molten lava cools and hardens?
Extrusive
Extrusive = forced out while molten through cracks in the earth's surface

32. 9. What is the Latin word that the word igneous comes from and what does it mean?
ignis = fire

33. 10. Intrusive Igneous Rocks
Form from magma below the earth’s surface

34. 11. Extrusive Igneous Rocks
Formed by lava on the Earth’s surface

35. 12. What is the difference between magma and lava?
Lava = molten rock flowing on the earth’s surface
Magma = molten rock below the earth’s surface

36. Silicon, oxygen, aluminum, iron, calcium, sodium, potassium, magnesium
13. What are the 8 elements that make up magma?
Silicon, oxygen, aluminum, iron, calcium, sodium, potassium, magnesium

37. 14. In what ways are the two rocks similar?
Look at the granite rock (A on age 71) and the rhyolite rock (B on page 71)
Granite
Rhyolite
14. In what ways are the two rocks similar?
Both are from melted rock
Their composition is the same

38. 15. In what ways are the two rocks different?
Granite
Rhyolite
Granite – coarse texture, made from magma
Rhyolite – fine texture, made from lava

39. 16. What causes the two rocks to be different?
Granite
Rhyolite
Granite – Slow cooling below the earth’s surface
Rhyolite – Quick cooling on the earth’s surface

40. 17. Why do you think some rocks are heavier than others?
Some are denser – less air space between particles

41. Which rock would have greater density?
Pumice
Granite

42. Classifying Rocks
Rocks can be classified, or put into groups with similar characteristics, by looking at the rocks texture, mineral composition, and color.

43. 18. What is texture? The size, shape, and pattern of the rock’s grain
Glassy
(nice)

44. 19. Composition (what’s it made of?)
The minerals that make up the different parts of a rock
Examples: Quartz Feldspar Magnesium Iron

45. ADD
Rock Color
The apparent color of the rock, on the inside and the outside

46. Metamorphic rocks are rocks that have "morphed" into another kind of rock.
These rocks were once igneous or sedimentary rocks.
How do sedimentary and igneous rocks change?
The rocks are under tons and tons of pressure, which fosters heat build up, and this causes them to change.
If you exam metamorphic rock samples closely, you'll discover how flattened some of the grains in the rock are.

47. The Rock Divisions
Rock divisions occur in three major families based on how they formed: igneous, sedimentary, and metamorphic.
Each group contains a collection of rock types that differ from each other on the basis of the size, shape, and arrangement of mineral grains.
Just remember 3 types of rocks=3 divisions. (igneous, sedimentary, and metamorphic)

48. Texture: the size, shape, and pattern of the rock’s grain.
Classifying Rocks
When classifying a rock sample geologists observe the rock’s color and texture and determine its mineral composition.
Texture: the size, shape, and pattern of the rock’s grain.
Color: the apparent color of the rock, on the inside and the outside.
Mineral composition: The minerals that make up the different parts of a rock.

49. Texture: Grain Size
Often, the grains in a rock are large and easy to see.
Such rocks are said to be coarse-grained. In other rocks, the grains are so small that they can only be seen with a microscope.
These rocks are said to be fine-grained.
Notice the difference in texture between the fine-grained slate and the coarse-grained diorite to the right.

50. Texture: Grain Shape The grains in a rock vary widely in shape
Some grains look like tiny particles of fine sand
Others look like small seeds or exploding stars
In some rocks, such as granite, the grain results from the shapes of the crystals that form the rock
In other rocks, the grain shape results from fragments of other rock
These fragments can be smooth and rounded, like the fragments in conglomerate, or they can be jagged, like the fragments in breccia
You can compare conglomerate and breccia one the next slide

51. Texture : Grain Pattern
The grains in a rock often form patterns. Some grains lie in flat layers that look like a stack of pancakes.
Other grains form wavy, swirling patterns. Some rocks have grains that look like rows of multicolored beads, as in the sample of gneiss shown above.
Other rocks, in contrast, have grains that occur randomly throughout the rock.

52. Different Types of Texture
Fine-Grained, Coarse-Grained, Rounded Grain, Jagged Grain, Nonbanded, Banded

53. 2 Types of Igneous Rocks
INTRUSIVE IGNEOUS ROCKS – When igneous rocks are formed by magma that cools BENEATH Earth’s surface, they are called intrusive igneous rocks
EXTUSIVE IGNEOUS ROCKS – When igneous rocks are formed by LAVA ON Earth’s surface, they are called extrusive igneous rocks

54. Lithification The process by which sediment becomes sedimentary rock
1st step : erosion
2nd step : deposition
3rd step : compaction
4th step : cementation

55. Sedimentary Rocks : Erosion
Destructive forces are constantly breaking up and wearing away all the rocks on Earth’s surface
The forces include heat and cold, rain, waves, and grinding ice
Erosion occurs when running water or wind loosens and carry away the fragments of rock.

56. Sedimentary Rocks: Deposition
 Eventually, the moving water or wind slows and deposits the sediment.
If water is carrying the sediment, rock fragments and other materials sink to the bottom of a lake or ocean.
Deposition is the process by which sediment settles out of the water or wind carrying it.
After sediment has been deposited, the processes of compaction and cementation change the sediment into sedimentary rock.
In addition to particles of rock, sediment may include shells, bones, leaves, stems, and other remains of living things.
Over time, any remains of living things in the sediment may slowly harden and change into fossils trapped in the rock.

57. Sedimentary Rocks: Compaction
 At first the sediments fit together loosely. But gradually, over millions of years, thick layers of sediment build up.
These layers are heavy and press down on the layers beneath them.
Then compaction occurs.
Compaction is the process that presses sediments together.
Year after year more sediment falls on top, creating new layers.
The weight of the layers further compacts the sediments, squeezing them tightly together.
The layers often remain visible in the sedimentary rock.

58. Sedimentary Rocks: Cementation
 While compaction is taking place, the minerals in the rock slowly dissolve in the water.
The dissolved minerals seep into the spaces between particles of sediment.
Cementation is the process in which dissolved minerals crystallize and glue particles of sediment together.
It often takes millions of years for compaction and cementation to transform loose sediments into solid sedimentary rock.

59. Sedimentary Transformations
Point A: water or wind deposits sediments
Point B: The heavy sediments press down on the layers beneath
Point C: Dissolved minerals flow between the particles and cement them together

60. Metamorphic Rock Pictures
Granite, Gneiss, Shale, Slate, Sandstone, and Quartzite are good examples of metamorphic rocks.

61. Bet Cha’ Weren’t Expecting A…. POP QUIZ!!!!!*
What are the three types of rock?
Which type of rock has been formed by magma or lava?
What do we classify rocks by?
How do sedimentary rocks form (in order)?
Metamorphic rocks are rocks that have
?(fill in the blank)
What is the process of sediments forming a sedimentary rock?
What does “ignis” mean in the word igneous?
*Answers are on next slide!

62. ANSWERS!!!! Igneous, Sedimentary, and Metamorphic Igneous
Texture, Color, and Mineral Composition
Erosion, Deposition, Compaction, Cementation
Morphed
Lithification
“ignis” means fire

63. Bibliography www.dlese.com Earth Science Textbook
Google Images ( I KNOW THIS DOESN’T COUNT IM JUST TELLING YOU!!)

64. Sedimentary Rocks
Sedimentary rocks form from particles deposited by water and wind
If you have ever walked along a beach (which I am sure you have) you may have noticed tiny sand grains, mud, and pebbles.
These are some sediments that eventually form into sedimentary rocks
Sedimentary Rocks can form in 4 ways by:
Erosion
Deposition
Compaction
Cementation