Rock Cycle & Igneous Rocks

1. Rock Cycle & Igneous Rocks

2. The Rock Cycle

3. Differences between rocks and minerals

4. The Rock Cycle-Types of Rocks • Rocksare any solid mass of mineral or mineral-like matter occurring naturally as part of our planet. • Types of Rocks 1. Igneous rock is formed by the crystallization of molten magma.

5. Rock Cycle-Types of Rocks 2. Sedimentary rock is formed from the weathered products of preexisting rocks that have been transported, deposited, compacted, and cemented. 3. Metamorphicrock is formed by the alteration of pre-existing rock deep within Earth (but still in the solid state) by heat, pressure, and/or chemically active fluids.

6. The Rock Cycle • Rock Cycle: shows the interrelationships among the three rock types(igneous, sedimentary, and metamorphic) • Magma is molten material that forms deep beneath the Earth’s surface. • Lava is magma that reaches the surface. • Weathering is a process in which rocks are broken down by water, air, and living things. • Sediment is weathered pieces of Earth elements.

7. The Rock Cycle

8. Energy that drives the Rock Cycle Earth’s Interior (Internal Processes): Igneous & Metamorphic Rocks Sun (External processes): Sedimentary rocks.  Weathering and the movement of weathered materials are external processes powered by energy from the sun.

9. Igneous Rocks & Magma

10. Igneous Rocks • Named for the Latin ‘Ignis’=Fire • Occurrence • Found globally • Found in discrete geologic locations • Convergent plate boundaries • Divergent plate boundaries • Mantle plumes • Formed by the crystallization of magma or lava

11. The Nature of Igneous Rocks • Form from Magma[Greek=“paste”] • Hot, partially molten mixture of solid, liquid, and gas • Gases: H2O, CO2, etc. • less dense than solid rock • solidifies upon cooling

12. Magma Vs. Lava (again) • Magma vs. Lava • Magma: molten rock beneath the surface • Lava: molten rock that has reached the surface • Magma: form intrusive igneous rocks • Lava: form extrusive igneous rocks

13. Igneous Rocks in NM- Cornudas Peak

14. Magma Composition • Composition varies widely • Oxygen plus major elements • Generally a silica (SiO2) melt • Silica and water content control viscosity • Silica content used in classification

15. Mafic Magmas • Silica content ~ 50% • High Fe, Mg and Ca (Iron, Magnesium, and Calcium) • High temperature molten magma • 1000o to 1200oC (1800-2200oF) • Major minerals: • Olivine - Ca Plagioclase • Pyroxene

16. Rocks formed from Mafic Magmas

17. Felsic Magma • Silica content: 65-77% • High Al, Na and K (Aluminum, Sodium, Potassium) • Lower temperature magmas • Less than 850oC (1575 oF) • Major minerals: • Feldspars - Micas • Quartz

19. Magma Viscosity Viscosity: resistance to flow High Viscosity= HIGH resistance, SLOWER flow Low Viscosity=LOW resistance=FASTER flow

20. Magma Viscosity • Controlled by silica and water content, and temperature • As magma cools-silica tetrahedron form links • Linkages control viscosity

21. Magma Viscosity • High Silica=high viscosity (slow) • Low Silica=low viscosity (fast) • Cooler Temperatures=higher viscosity • Higher Temperatures=lower viscosity • More Links=higher viscosity • Fewer Links=lower viscosity • Water=lower viscosity

22. Plate Tectonic Setting of Igneous Rocks • Divergent Plate Boundaries • Partial melting of mantle produces basaltic magma (MAFIC) • Convergent Plate Boundaries • Subduction produces partial melting of basalt, sediments, parts of mantle • Andesitic and rhyoliticmagma (INTERMEDIATE & FELSIC) • Ascending magma assimilates lower crustal material

23. Plate Tectonic Setting of Igneous Rocks • Mantle Plumes • Partial melting of plumes of mantle material • Basaltic magma is produced (MAFIC) • Rising magma produce • Intraplate island chains • Flood basalt [Columbia River Basalts]

25. Igneous Rocks-Classification • Igneous Rocks are classified by 3 main factors: • Formation (by magma or lava) • Texture • Composition

26. Igneous Rocks: Classification • Formation • Intrusive Igneous Rocks: • formed when magma hardens beneath Earth’s surface. • See these after erosion occurs • Ex: Granite • Extrusive Igneous Rocks: • Formed when lava hardens above Earth’s surface • Ex: Rhyolite

27. Granite

28. Rhyolite

29. Igneous Rocks: Classification • Texture • the size, shape and relationship of minerals in the rock • Cooling history of the magma or lava • Crystal size increases as rate of cooling slows • There are 5 main textures: coarse, fine, glassy, porphyritic, pyroclastic

30. Igneous Rocks: Classification • Coarse (Phaneritic)Texture • Slow cooling rate • Large Crystals • Equigranular, interlocking crystals • Ex. Granite

31. Igneous Rocks: Classification • Fine (Aphanitic)Texture • Fast cooling rate • Smaller, interconnected crystals • Few crystals visible in hand specimen • Ex. Rhyolite

32. Igneous Rocks: Classification • Glassy Texture • Very fast cooling rate • No visible crystals • Volcanic Glass • Ex. Obsidian

33. Igneous Rocks: Classification • Porphyritic Texture • Complex cooling history • Different cooling rates throughout the rock • Different sized crystals • Ex. Andesite

34. Igneous Rocks: Classification • Pyroclastic Texture • forms as an explosive volcanic eruption mixes fragments of the volcano with hot ash in the atmosphere • As this hot combination of tiny ash particles and larger, angular fragments settles to the ground, they blanket the Earth's surface and weld together • Appear porphyritic with visible crystals • A generic term for all these rocks is “tuff”

36. Igneous Rocks: Classification • Composition • Which types of minerals make up the rock • Composition determined by Bowen’s reaction series (later) • Range from light colored (felsic) to very dark colored (ultramafic)

37. Igneous Rocks: Classification • Felsic Composition • Also called silicic or granitic composition • Light colored rocks • White to pink in color • Mostly composed of quartz and potassium feldspar • Very High amounts of: Si, Na, K • Very Low amounts of: Fe, Mg, Ca • Examples: Granite (I) Rhyolite (E)

38. Felsic Rocks

39. Igneous Rocks: Classification • Intermediate Composition • Also called andesitic composition • Combination of light and dark colored minerals • Salt and Pepper OR gray coloration • Mostly composed of amphibole, plagioclase feldspar, quartz, pyroxene • High amounts of: Si, Na, K • Low amounts of: Fe, Mg, Ca • Examples: Diorite (I) Andesite (E)

40. Intermediate Rocks

41. Igneous Rocks: Classification • Mafic Composition • Also called basaltic composition • Dark colored minerals • Mostly composed of pyroxene, plagioclase feldspar, olivine • Low amounts of: Si, Na, K • High amounts of: Fe, Mg, Ca • Examples: Gabbro (I) Basalt (E)

42. Mafic Rocks

43. Igneous Rocks: Classification • Ultramafic Composition • Very Dark colored minerals (usually has dark greens) • Mostly composed of pyroxene and olivine • Very Low amounts of: Si, Na, K • Very High amounts of: Fe, Mg, Ca • Examples: Peridotite (I) Komatiite (E)

44. Ultramafic Rocks

45. Classification of Igneous Rocks

46. Classification of Igneous Rocks

48. Bowen’s Reaction Series • Chemical Evolution of Igneous Rocks proposed by Norman Bowen in the early 1900s. • Proposed mafic magmas may evolve by cooling and crystallization to produce more silica-rich magmas • Found the following through experiment: • There is a regular sequence of silicate mineral crystallization • Minerals common to mafic rocks crystallize at the highest temperatures • Minerals common to felsic rocks crystallize at the lowest temperatures

49. Bowen’s Reaction Series Once a mineral forms, it will undergo a chemical reaction with the surrounding melt to produce the next  lower temperature mineral in the sequence Example: Olivine undergoes a reaction with the surrounding melt to form pyroxene. Pyroxene reacts with the surrounding melt to form amphibole, etc.

50. Bowen’s Reaction Series • There are two important parts of the reaction series: • The discontinuous series - includes minerals with differing arrangement of Si-O tetrahedra; (olivine, pyroxene, amphibole, biotite) • The continuous series - includes plagioclase feldspar minerals, all of which are framework silicates; (Ca-rich plagioclase (anorthite), Na-rich plagioclase (albite))