1. I. Minerals Definitions – Earth Materials A. Rock: naturally occurring aggregate of one or more minerals B. Mineral: naturally occurring solid with a definite chemical composition and an orderly internal structure. Natural: synthetic gems and other substances created by chemists are not minerals Solid Definite chemical composition: consists of one or more chemical elements in specific proportions Orderly internal structure: elements are arranged in a systematic way that is the same in every sample of that particular mineral Minerals

2. Rocks and Minerals At one time or another, you have probably held a rock in your hand Recall the color. Recall the size. The word rock refers to solid mineral deposits. Rocks are minerals, but not all minerals are rocks. Minerals are all substances that can't be classified as "animal" or "vegetable."

3. Minerals Metals ores found in the earth, like gold and silver, are minerals. Crystalline substances, like salt and quartz, are minerals. Homogeneous natural substances, like water and gas, are also minerals. These non-solid minerals?" Rock: an aggregate of one or more minerals

4. Minerals (a) atomic structure and chemical reactions: a review (b) What is a mineral? (c) Classification of minerals (d) Silicate minerals

5. What is a mineral? First we need to understand atomic structure of elements. Atomic structure and chemical reactions STRUCTURE OF ATOMS: Atom is the smallest unit of an element that retains the physical and chemical properties of that element.

6. Atom: the smallest particles of an element that retain all of the element’s chemical properties Chemical Compounds: specific combinations of one or more elements. Atoms bond together to form compounds a.SiO 2, NaCl, PbS, Fe 2 SiO 4, CaAl 2 Si 2 O 8 All of the above are chemical formulas of minerals b. Minerals are essentially chemical compounds; elements, in certain proportions, bonded together

7. A. Relative abundances of elements Of the 92 naturally occurring elements, 8 make up >98% of the Earth’s continental crust Most minerals in the crust are O and Si based rocks (silicates) Most minerals in the mantle are O-Si-Fe-Mg based rocks Composition of Earth Crust Entire Earth 1. Oxygen (O)45.2% 29.3% (2) 2. Silicon (Si) 27.2% 14.7% (3) 3. Aluminum (Al) 8.0 1.2% (8) 4. Iron (Fe) 5.8% 34.8% (1) 5. Calcium (Ca) 5.1% 1.4% (7) 6. Magnesium (Mg) 2.8% 11.3% (4) 7. Sodium (Na) 2.3% 8. Potassium (K) 1.7% Sulfur (S) 3.3% (5) Nickel (Ni) 2.4% (6) Total 98.1% 98.4%

8. CHEMICAL REACTIONS and TYPES OF CHEMICAL BONDS Ions = atoms that gained and lost electrons: Ions -- after gain or loss of an electron, atoms are no longer electrically neutral. When Na loses an electron it becomes a Na ion. Positive ions = cations, Negative ions = anions.

9. CHEMICAL REACTIONS TYPES OF CHEMICAL BONDS Relative sizes and charges of these elements’ atoms and ions 1. Given two elements of equal abundance, the element that will contribute more readily in a mineral is the one that “fits” better with the other elements. 2. Ions pack together as closely as possible (large negative ions with small positive ions in the “holes”. 3. If amount of one element runs low, it may be replaced by another.

10. TYPES OF CHEMICAL BONDS One type of atomic bond is: Ionic substitution: ions of similar size and shape (charge) replace one another within a crystal structure For example Mg and Fe 2+ in olivine: (Fe, Mg) 2 SiO 4 ) Na (+1) and Cl (-1), + and – attract, so Na loses an electron and Cl gains an electron

11. Ionic substitution Ions of similar size and shape (charge) replace one another within a crystal structure Ca and Mg can substitute each other O and Ca can not replace another

12. The temperature and pressure at the time of formation (Structural Variation) Polymorphs : minerals with the same composition, but different structures because they formed under different conditions of heat and pressure For example, diamond and graphite are both pure carbon, one very hard & one soft. Diamond needs high pressure (>90 miles) Graphite more stable at Earth’s surface

13. III. Identifying Minerals Identifying minerals is the key to geology. We ID the minerals to know what rock it is and where it came from. The minerals tell us a story about where the rock formed and under what conditions A.Color: first thing you notice, but least reliable, can vary greatly (quartz, calcite, salt) Color depends on the composition and structure. Corundum = clear Chromium = red rubies Titanium & Iron = blue sapphires Lithium = pink Copper = green

14. III. Identifying Minerals B. Luster; how its surface reflects light- - its shininess Metallic Silky Vitreous (glassy) Earthy (dull) C. Streak—the color of a mineral in its powered form. Scrape the mineral across an unglazed porcelain tile (streak plate) Different color powder than how the mineral looks alone

15. III. Identifying Minerals D. Hardness: how hard it is - resistance to scratching or abrasion Scale from 1-10 Diamond 10 Steel 6.5 Glass 5-6 Copper penny 3.5 Fingernail 2.5 Graphite 1-2 E. Smell and Taste Sulfur- rotten eggs Halite- salty Sylvite- bitter F. Effervescence Rocks containing CO 3 react with HCl to form CO 2 gas

16. III. Identifying Minerals F. How they break 1.Cleavage: tendency to break consistently along distinct planes in the crystal structure due to weak bonds---break along flat surfaces called cleavage planes 1. cubic—halite 2. sheets—micas 3. rhombus—calcite 2. Fracture—breaks are jagged and irregular conchoidal fracture: breaks like glass - curved, shell shaped surface

18. Int-A.02b Dr. Kent Ratajeski, Department of Geology and Geophysics, University of Wisconsin, Madison

20. Analytical techniques X-Ray Diffraction Nobel Prize for determining the structure of halite (salt) Microprobe Ion Probe