1 / 37

Earth Science, 10e

Earth Science, 10e. Edward J. Tarbuck & Frederick K. Lutgens . Minerals: Building Blocks of Rocks Chapter 1. Earth Science, 10e Stan Hatfield and Ken Pinzke Southwestern Illinois College. Minerals: the building blocks of rocks . Definition of a mineral Natural Inorganic Solid

zalman
Télécharger la présentation

Earth Science, 10e

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Earth Science, 10e Edward J. Tarbuck & Frederick K. Lutgens

  2. Minerals: Building Blocks of RocksChapter 1 Earth Science, 10e Stan Hatfield and Ken Pinzke Southwestern Illinois College

  3. Minerals: the building blocks of rocks • Definition of a mineral • Natural • Inorganic • Solid • Possess an orderly internal structure of atoms • Have a definite chemical composition • Mineraloid - lacks an orderly internal structure

  4. Composition and structure of minerals • Elements • Basic building blocks of minerals • Over 100 are known • Atoms • Smallest particles of matter • Have all the characteristics of an element

  5. Periodic table of the Elements

  6. How atoms are constructed • Nucleus – central part of an atom that contains • Protons – positive electrical charges • Neutrons – neutral electrical charges • Energy levels, or shells • Surround nucleus • Contain electrons – negative electrical charges

  7. Simplified view of the atom

  8. How atoms are constructed • Atomic number is the number of protons in an atom's nucleus • Bonding of atoms • Forms a compound with two or more elements • Ions are atoms that gain or lose electrons • Isotopes • Have varying number of neutrons

  9. How atoms are constructed • Isotopes • Have different mass numbers – the sum of the neutrons plus protons • Many isotopes are radioactive and emit energy and particles

  10. Minerals • Physical properties of minerals • Crystal form • Luster • Color • Streak • Hardness • Cleavage

  11. The mineral quartz often exhibits good crystal form

  12. Pyrite (fool’s gold) displays metallic luster

  13. Three examples of perfect cleavage – fluorite, halite, and calcite

  14. Minerals • Physical properties of minerals • Fracture • Specific gravity • Other properties • Taste • Smell • Elasticity • Malleability

  15. Conchoidal fracture

  16. Minerals • Physical properties of minerals • Other properties • Feel • Magnetism • Double Refraction • Reaction to hydrochloric acid

  17. Minerals • A few dozen minerals are called the rock-forming minerals • The eight elements that compose most rock-forming minerals are oxygen (O), silicon (Si), aluminum (Al), iron (Fe), calcium (Ca), sodium (Na), potassium (K), and magnesium (Mg) • Most abundant atoms in Earth's crust are oxygen (46.6% by weight) and silicon (27.7% by weight)

  18. Minerals • Mineral groups • Rock-forming silicates • Most common mineral group • Contain the silicon-oxygen tetrahedron • Four oxygen atoms surrounding a much smaller silicon atom • Combines with other atoms to form the various silicate structures

  19. The silicate (SiO4)-4 molecule

  20. Common silicate minerals

  21. Minerals • Mineral groups • Rock-formingsilicates • Groups based upon tetrahedral arrangement • Olivine – independent tetrahedra • Pyroxene group – tetrahedra are arranged in chains • Amphibole group – tetrahedra are arranged in double chains

  22. Hornblende – a member of the amphibole group

  23. Minerals • Mineral groups • Rock-formingsilicates • Groups based upon tetrahedral arrangement • Micas – tetrahedra are arranged in sheets • Two types of mica are biotite (dark) and muscovite (light) • Feldspars - Three-dimensional network of tetrahedra

  24. Minerals • Mineral groups • Rock-formingsilicates • Groups based upon tetrahedral arrangement • Feldspars • Two types of feldspar are Orthoclase and Plagioclase • Quartz – three-dimensional network of tetrahedra

  25. Potassium feldspar

  26. Plagioclase feldspar

  27. Minerals • Mineral groups • Rock-formingsilicates • Feldspars are the most plentiful mineral group • Crystallize from molten material • Nonsilicate minerals • Major groups • Oxides • Sulfides

  28. Minerals • Mineral groups • Nonsilicate minerals • Major groups • Sulfates • Carbonates • “Native” elements

  29. Native Copper

  30. Minerals • Mineral groups • Nonsilicate minerals • Carbonates • A major rock-forming group • Found in the rocks limestone and marble • Halite and gypsum are found in sedimentary rocks • Many have economic value

  31. Some common non-silicate minerals

  32. Minerals • Mineral resources • Reserves are already identified deposits • Ores are useful metallic minerals that can be mined at a profit • Economic factors may change and influence a resource

  33. An underground halite (salt) mine

  34. The Bingham copper mine in Utah

  35. End of Chapter 1

More Related