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Minerals, Rocks and the Rock Cycle

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Presentation on theme: "Minerals, Rocks and the Rock Cycle"— Presentation transcript:

1 Minerals, Rocks and the Rock Cycle

2 What is a mineral? Occurs naturally Is a solid
Definite chemical composition Atoms arranged in orderly pattern

3 May Be Elements or Compounds
Gold at Fort Knox Native Minerals Form uncombined in nature Au, Ag, Cu, S, C Gold, silver, copper, sulfur, diamond Most are compounds Form from magma Form as evaporites Changed by heat, pressure, or water Flash: Minerals, Gems and Ores

4 Silicates 90% minerals on Earth Si, O, and 1 or more metallic ions
Most common Si, O, and 1 or more metallic ions Si04 Tetrahedron shape

5 How can I tell what this is?
Identifying Minerals Over 200 known Can be identified from physical properties How can I tell what this is?

6 Identification Properties
COLOR Least useful Many have similar colors Other elements may change color Beryl (emerald)

7 Colors of Quartz

8 Identification Properties
LUSTER The shine in reflected light LUSTER TERM DESCRIPTION adamantine very brilliant - as in diamond resinous looks like resin or hardened tree sap vitreous glassy, but not as shiny as diamond metallic looks like metal silky has a smooth and fibrous sheen pearly smooth and iridescent greasy looks like it's coated with oil earthy looks like dirt

9 LUSTER Glassy Adamantine Greasy

10 Identification Properties
CRYSTAL SHAPE Hard to find Must have room to grow Crystal Systems Cubic Orthorhombic Tetragonal Triclinic Hexagonal Monoclinic

11 Identification Properties
STREAK Color of its powder Does not change Metallic: as dark as sample Nonmetallic: white to colorless Streak Plate ↑

12 Identification Properties
CLEAVAGE Tendency to split easily or break along flat surfaces Mica – 1 direction FRACTURE Break on uneven surfaces Conchoidal - obsidian

13 Identification Properties
HARDNESS Resistance to being scratched Mohs’ Scale of Hardness

14 Mohs’ Scale of Hardness
1 - Talc – fingernail scratches it easily 2 - Gypsum – fingernail scratches it 3 - Calcite – copper penny just scratches it 4 - Fluorite – steel knife scratches it easily 5 – Apatite – steel knife scratches it 6 – Feldspar – steel knife does not scratch it easily; it scratches window glass

15 Mohs’ Scale of Hardness
7 – Quartz – hardest common mineral; it scratches steel and hard glass easily 8 – Topaz – harder than any common mineral 9 – Corundum – it scratches topaz 10 – Diamond – hardest of all minerals

16 Special Identification Properties
Fluorescence

17 Special Identification Properties
Magnetism Magnetite

18 Special Identification Properties
Taste This will quickly identify the mineral halite (salt). If you are new to this process you must use this one with caution, as you never know what the unknown may be. Often, you may need to resort to this method (until you more fully understand other identifying traits) to differentiate halite from calcite. If you do taste the sample (especially in a class environment) you should realize that it has been handled by and probably tasted by hundreds of others.

19 Rocks & the Rock Cycle James Hutton – uniformitarianism
“The present is the key to the past” Geologic processes that happen today happened in the past Earth’s present physical features were formed by these processes Flash: Rock Cycle 19:41

20

21 Igneous Rocks 2 kinds of magma Formed by cooling & hardening of magma
Plutonic – intrusive, forms underground Volcanic – extrusive, forms on surface 2 kinds of magma high SiO2%, light colored, thick, slow moving low SiO2%, dark colored called mafic

22 Igneous Rocks Grain size and texture depends on how quick cooled
Slow = large crystals Fast = small crystals

23 Igneous Rocks Grouped based on mineral composition Light = granite
Dark = gabbro

24 Enormous mass of intrusive igneous rock (rock made of once-molten material that has solidified below the earth's surface). Granite, have steep walls, no visible floors, and extend over thousands of square miles. Form either as one large mass or many smaller masses at great depths and are exposed only after considerable erosion. Associated with plate boundaries.

25 Sedimentary Rock Form from sediments hardening into rock
From pieces of other rocks clastic, sandstone, shale Precipitating out of a solution chemical, limestone, rock salt From remains of plants & animals organic, coal, limestone

26 Conglomerate Conglomerate is a sedimentary rock that contains large (greater than two millimeters in diameter) rounded clasts (pieces of rock). The space between the clasts is generally filled with smaller particles and/or a chemical cement that binds the rock together.

27 Sandstone

28 Limestone

29 Shale

30 The Law of Superposition
Sedimentary Rock Most formed under water, but also in deserts/dunes Cemented together by SiO2, CaCO3, or FeO The Law of Superposition

31 Sedimentary Rock Some contain fossils

32 Sedimentary Rock Almost all show strata (layers)

33 Sedimentary Rock

34 Some show ripple marks or mud cracks
Sedimentary Rock Some show ripple marks or mud cracks

35 Metamorphic Rock “changed” by heat & pressure From mountain building
Contact with magma

36 Metamorphic Rock

37 Metamorphic Rock

38 Metamorphic Rock Shale  slate  schist (if more H&P are added)
Shale or granite  gneiss Limestone  marble

39 Shale to Slate Metamorphism
Metamorphic Rock Shale to Slate Metamorphism

40 Metamorphic Rock

41 Marble

42 Poster Project: Draw and color the Rock Cycle on a large Poster board. Cut out pictures of the different kinds of rock shown and paste them to the drawing in the appropriate places. Due in 1 week.


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