1. MINERALS AND ROCKS THE TREASURES OF OUR EARTH! REVIEW THIS POWERPOINT OFTEN— IT IS EVERYTHING YOU NEED TO KNOW!

2. MINERAL: A. Naturally occurring B. Inorganic, Solid C. Crystalline structure D. Definite chemical and physical properties E. Definite molecular structure (internal arrangement of atoms)

3. Minerals are identified based on their physical properties 1. Color Most visible property, but least reliable. Many minerals have the same color and some have more than one color.

4. 2. Streak Color of a mineral in its powder form

5. 3. Luster The way in which light is reflected from the surface a. Metallic - shines like polished metals, rust, heavy b. Nonmetallic - no metallic luster 1) glassy, clear 2) pearly, white 3) greasy 4) dull 5) earthy nonmetallic metallic

6. 4. Hardness a. the resistance of a mineral is compared to glass by scratching it against a glass plate (5.5) b. hardness of a mineral is determined by Moh's Scale of Hardness (1 – 10)

8. 5. Cleavage The tendency of a mineral to split along flat, even surfaces.

9. Fracture -Uneven breakage of a mineral. (minerals that do not have cleavage have this!)

10. Other Properties: a. Magnetic b. React with dilute hydrochloric acid by effervescing bubbles c. Taste (salty) d. Fluorescence e. Double refraction f. Radioactive

11. Minerals Relationship to Rocks: Minerals form rocks. Most rocks are composed of one or more minerals Monominerallic - composed of one mineral Polyminerallic - composed of more than one mineral 10 - 15 minerals form most all of the rocks on Earth, they are called rock-forming minerals.

12. Silicates minerals (SiO 4 )– two minerals combine to form a compound. When they combine they create a structure called the Silicon-Oxygen Tetrahedron

13. 3 Rock Types: IgneousSedimentary Metamorphic Rocks are classified based on their: Origin In other words, what environment did they form in??? Crystals Sediments Recrystallized crystals

14. Igneous Rocks Formed by cooling and solidification of lava or magma. Lava: extrusive Magma: intrusive

16. Igneous Rocks A. Igneous Rocks Intrusive- cools and solidifies from magma (beneath Earth’s surface), making larger crystals due to slow cooling. Granite (coarse crystal texture)

17. Extrusive – cools and solidifies from lava (at or near Earth’s surface), making smaller crystals due to faster cooling. Obsidian (glassy texture)Pumice (glassy texture with vesicles)

18. Igneous Rock Characteristics Felsic- forms light-colored rocks that are high in Al, low density. Mafic- forms dark-colored rocks that are high in Mg and Fe, high density. Vesicular- gas bubbles or air pockets.

19. Cooling Time Graph (the longer it takes to cool, the bigger the crystals!) As time increases, crystal size increases.

20. IGNEOUS ROCKS

21. Crystal size Description Grain Size

22. Igneous rocks have “Intergrown Crystals” – crystals that form as the rock forms.

23. Intergrown Crystals Not Intergrown Crystals

24. Where the rock formed Outside the volcano: Extrusive (lava) Inside the Earth: Intrusive (magma)

25. Air Bubbles in the rock? Yes= Vesicular

26. No Air Bubbles? No = Non-vesicular

27. Color LightDark Lightest Darkest

28. Density Low Density High Density

29. What Minerals Are in the Rocks? First, identify the rock, then go straight down the column for the minerals.

30. This is the amount of Potassium Feldspar in the rock.

31. This is the amount of Quartz in the rock.

32. This is the amount of Plagioclase Feldspar in the rock.

33. Use tick marks on a scrap paper to measure the percentage. Potassium Feldspar 25% Quartz 40%

34. Practice Name a light-colored, fine-grained rock with no bubbles.

35. Name a coarse-grained, dense rock.

36. Name a very light-colored, glassy, extrusive rock with bubbles.

37. Metamorphic Rocks Form from metamorphism (change) that is caused by heat and pressure. Usually form deep in the Earth's crust Causes a change in the rocks 1. makes the rock more dense 2. separates the rock into layers (banding)

38. Metamorphic rocks have been changed from a pre-existing rock. Caused by extreme heat and/or pressure. (regional) Happens over wide “regions.” Caused by contact with extreme heat from a nearby volcano (contact). Occurs when the rock is in close contact with volcanic heat.

39. Types of Metamorphic Rocks: 1. Contact Metamorphic - Rocks that form from being close to a heat source (magma) 2. Regional Metamorphic a. caused mainly by pressure b. usually cover large areas c. form during tectonic activity d. most metamorphic rocks are formed from regional metamorphism

40. Metamorphism happens where lava or magma touches other rocks. What will this limestone rock metamorphose into?

41. Classification of Metamorphic Rocks Non-foliated - no visible layers (distorted crystals) Marble

42. Foliated Metamorphic Rock – mineral alignment a. visible layers in the rock b. form from extreme pressure which flattens the minerals into layers c. different mineral densities may produce alternating light and dark bands of minerals (banding) A “GNEISS” ROCK 

43. Sedimentary Rocks: Rocks formed from sediments on Earth’s surface.

44. Sedimentary Rocks form from sediments that go through cementation & compaction EXAMPLES OF SEDIMENT SIZE FROM LARGEST TO SMALLEST

45. Three main types 1. Clastic - made from other existing rock fragments. Clastic rocks are identified by the size of the fragments. 2. Chemical - form from minerals once dissolved in water. 3. Organic - formed from once living organisms.

46. Features of Sedimentary Rocks: Stratification - layering of rocks caused by different types of sediments being deposited

47. Fossils – only found in Sedimentary Rocks. These are the imprints left by a once-living organism.

48. 1. Made from sediments or rock material that has been broken down in some way. 2. Sedimentary rocks are usually formed under water. 3. Often layered. 4. Are the only rocks that contain fossils! Key Features of Sedimentary Rock

49. 5.Clastic (fragmental) – made by compaction and cementation of sediments. See Earth Science References Tables

50. Mixed

51. Conglomerate Rock has rounded fragments Rocks become rounded when they are exposed to water over long periods of time, such as rocks formed at the bottom of a river bed.

52. Breccia Rock has angular fragments

53. Chemically formed rocks: Evaporites 1. Formed when water carrying minerals evaporates and leaves the minerals behind. 2. Are identified by the minerals present (such as halite forms Rock Salt) See Earth Science Reference Tables

55. Bioclastic- bio= life clastic= fragments Made from accumulated shells (limestone) or plants (coal) See Earth Science Reference Tables

56. Formation of Coal

58. The Rock Cycle Any rock can change into another type of rock!

59. EARTH SCIENCE REFERENCE TABLES CHART – PAGE 6

60. Earth Science Rocks!!! FOR YOUR TEST: *Know the rock & minerals vocab *Know the ESRT charts *Practice Castle Learning questions!