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Earth Materials: Silicate Minerals & Igneous Rocks

Earth Materials: Silicate Minerals & Igneous Rocks. Introduction to Rocks and Minerals (Continued): Common rock-forming “silicate” minerals (Chapter 5) Introduction to rocks & the rock cycle (Prelude A) Igneous Rocks (Chapter 6). Today’s Lecture:. Question: What minerals would

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Earth Materials: Silicate Minerals & Igneous Rocks

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  1. Earth Materials: Silicate Minerals & Igneous Rocks

  2. Introduction to Rocks and Minerals (Continued): • Common rock-forming “silicate” minerals (Chapter 5) • Introduction to rocks & the rock cycle (Prelude A) • Igneous Rocks (Chapter 6) Today’s Lecture:

  3. Question: What minerals would you expect to be most abundant on Earth? Percent of elements by WEIGHT Average composition of the Earth’s crust.

  4. The Common Rock-forming Minerals Earth’s Crust Primarily Si & O followed in abundance by Fe, Mg, Ca, Na, K, etc. Dark-colored silicates (mantle and oceanic crust) Olivine (Si, O, Fe, Mg) Pyroxene(Si, O, Fe, Mg, Ca) Amphibole (Si, O, Fe, Mg) Light-colored silicates (crust, esp. continental crust) Quartz (SiO2) - Hard, transparent Feldspar (Si, O, Al, K, Na, Ca) - Hard, white, gray, pink Clay (Mostly come from weathering feldspar) Calcite (CaCO3, shells) Limestone - Used for cement

  5. 4- SiO 4 4+ 2- 2- 2- 2- O O Si O O Basic Building Block of Silicate Minerals: The Silicon-Oxygen Tetrahedron An anion with charge of -4 1 silicon (Si) atom 4 oxygen (O) atoms Silicon tetrahedron has An overall charge of -4

  6. Silicates: The Common Rock-forming Minerals Basic Building Block: The Silicon-Oxygen Tetrahedron Tetrahedra link up by forming covalent bonds between oxygen atoms: Two tetrahedra can join by sharing an electron between adjacent oxygen atoms Single silicon tetrahedron: A silicon atom covalently- bonded to four oxygens. Oxygen atom Silicon atom

  7. The Common rock-forming minerals Silicates Silicon-oxygen tetrahedra can be arranged into: Double chains: Amphibole Sheets: Micas Single chains: Pyroxene

  8. Balancing Charges in Silicates: Role of Metal Cations Silicate chains and sheets Not electrically neutral! Unsatisfied negative charges on oxygen atoms located at the edges of chains, or between sheets, are neutralized by coordinating metallic ions at those sites. Iron (Fe) Magnesium (Mg) Potassium (K) Sodium (Na) Aluminum (Al) Calcium (Ca)

  9. Ionic Substitution Ions of similar size (ionic radius) and charge can substitute for one another in a mineral.

  10. Prelude Chapter: Rocks Definition of a rock: A rock is: 1) Comprised of one or more minerals 2) Naturally occurring There are three types of rocks: Igneous (formed by cooling from magma) Sedimentary (formed by the breakdown of other rocks) Metamorphic (formed when preexisting rocks are heated under pressure.

  11. Prelude Chapter: Rocks Rocks and minerals • Some rocks composed entirely of one mineral • limestone (calcite) • Most rocks have more than one kind of mineral • granite • Some rocks contain non-mineral matter • coal (has organic debris) • obsidian (volcanic glassy rock -> not crystalline)

  12. Prelude Chapter: Rocks rock

  13. Prelude Chapter: Rocks collection of one or more minerals rock

  14. Prelude Chapter: Rocks minerals rock mineral

  15. Prelude Chapter: Rocks So far we have: minerals rock mineral collection of one or more minerals A collection of one or more types of atoms

  16. Prelude Chapter: Rocks • Example: • Granite & its constituent minerals: • Quartz • Amphibole (hornblende) • Feldspar

  17. The Rock Cycle • Rocks may be classified into three types: • Igneous: • Formed by the crystallization of • molten rock material called magma • Sedimentary: • Formed from pre-existing rocks by • weathering (chemical and physical breakup) • and erosion (transport). • Metamorphic: • Formed by textural and compositional changes • that occur when pre-existing rocks are buried • and subjected to increased temperatures and • pressures. • Rock Cycle (see accompanying slide/MOV): Connects the three rock groups to each other by process. The rock cycle is embedded within the hydrological and the plate cycles discussed previously,

  18. Focus: Interlude A & Chapter 6. Igneous Rocks Molten rock • In the Earth is called magma. Magma is buoyant, rises to surface, & sometimes breaks through as volcanic eruptions. • When magma reaches thesurface it • is called lava.

  19. Igneous Rocks Anigneousrock is formed when magma or lavacools and solidifies.

  20. Igneous rocks Why care? • Igneous rocks make up bulk of Earth’s crust. • Earth’s mantle is composed entirely of igneous rock! • Igneous rocks are important economically as building stones and as host rocks for a variety of mineral (ore) deposits. • Volcanic activity is a well-known geological hazard, and the associated igneous rocks hold the secrets for understanding both the nature of past volcanic eruptions and the potential for future eruption hazards.

  21. Volcanic Igneous Rocks • Igneous rocks that form by the eruption of magma at the surface are called volcanic(or extrusive). • Magma erupted at the surface iscalled lava. • Fragmented materials are called pyroclastic and consist of ash & cinders.

  22. In igneous rocks, texture is controlled by the cooling rate of the magma. Cooling Rate Crystal Size Slow cooling larger crystals Fast cooling small or no crystals

  23. Plutonic Igneous Rocks Igneous rocks that form deep below the surface are called plutonic(intrusive) igneous rocks. To see them, they must be uplifted to surface and the overlying rock eroded away.

  24. As a magma cools, atoms arrange themselves • into orderly crystalline structures called • minerals. This process is called: • Crystallization

  25. Again, the rate of cooling controls the grain size of the rock formed. Plutonic igneous rocks cool slowly at depth and are therefore coarser grained! Microscopic views of plutonic igneous rocks

  26. Subsurface intrusion called a dike

  27. ALL ROCKS ARE CLASSIFIED ACCORDING TO THEIR: TEXTURE AND MINERAL COMPOSITION Texture involves a consideration of : a. Size b. Shape c. Arrangement of the minerals making up a rock.

  28. Types of Igneous Textures Fine-grained Coarse-grained Glassy Porphyritic

  29. fast cooling magma/lava • forms at or near surface • sometimes gas holes present • hard to see individual crystals • forms deep below the surface • slow cooling • crystals are corase and intergrown • magma cooled slowly for a while then erupted • minerals crystallized at different temperatures and or rates over a period of time • rapid cooling (quenching) at surface • amorphous: atoms unable to form orderly crystalline structures Types of Igneous Textures Fine-grained Coarse-grained Porphyritic Glassy

  30. Devil’s Postpile

  31. Plutonic or volcanic? A C B D

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