2. Rocks and Rock Cycle Intro.

3. The Rock Cycle Illustrates relationships between 3 rock types & their methods of formation Illustrates relationships between 3 rock types & their methods of formation 1. Igneous – forms from cooling & crystallizing magma 2. Sedimentary – forms from sediments compacted & cemented together 3. Metamorphic – intense heat and pressure changes rock Rocks are continuously changing Rocks are continuously changing Processes go in NO particular order Processes go in NO particular order

4. Sedimentary Rock Igneous Rock eg granite eg basalt large crystals small crystals very high temperatures causing melting cooling and crystallisation (solidification) weathering and erosion fast cooling slow cooling very hot! mudstone Magma (molten rock) Sediment mud sand shells sediment is compacted (squashed) and particles get cemented Metamorphic Rock limestone eg chalk sandstone marble slate heat and pressure Any rock can be weathered or eroded to mud or sand

5. The Rock Cycle

6. Causes of Change Causes of rocks to change from one type to another. Causes of rocks to change from one type to another. Weathering Weathering Erosion Erosion Compaction Compaction Cementation Cementation Heat & Pressure Heat & Pressure Melting and cooling Melting and cooling

7. Causes of Change

8. Igneous Rocks Earth’s original!!

9. Igneous Types Intrusive (magma) Slow cooling Slow cooling Large crystals (course-grained) Large crystals (course-grained) Extrusive (Lava) Fast cooling Fast cooling Small Crystals (fine- grained) Small Crystals (fine- grained)

10. Magma Composition Composition Contains the same elements/compounds of earth’s crust Contains the same elements/compounds of earth’s crust Therefore silica & oxygen most abundant Therefore silica & oxygen most abundant Categorized by the amount of silica & oxygen content Categorized by the amount of silica & oxygen content

11. Magma Origins Minerals begin melting between 800- 1200 o C Minerals begin melting between 800- 1200 o C Factors that affect melting Factors that affect melting 1. Temperature Increases w/depth (geothermal gradient) Increases w/depth (geothermal gradient) 2. Pressure Increases w/depth & prevents melting Increases w/depth & prevents melting 3. Water content More water lower melting point More water lower melting point

12. How Rocks Melt Partial melt Partial melt Some minerals melt faster than others Some minerals melt faster than others Creates a magma slush Creates a magma slush Fractional crystallization Fractional crystallization Some minerals cool at lower temps Some minerals cool at lower temps Cools in reverse order of melt Cools in reverse order of melt

13. Crystal Settling

14. Bowen’s Reaction Series 14 15 16

15. Bowen’s Reaction Series Bowen’s Reaction Series Illustrates the relationship between cooling magma and mineral formation Illustrates the relationship between cooling magma and mineral formation 2 main branches 2 main branches Continuous Feldspar group Continuous Feldspar group Discontinuous iron-magnesium group Discontinuous iron-magnesium group

16. Bowen’s Reaction Series Bowen’s Reaction Series Continuous Feldspar Branch As magma cools composition gradually changes As magma cools composition gradually changes Calcium-rich cools first @ high temps. Calcium-rich cools first @ high temps. Sodium-rich cools last @ lowest temps. Sodium-rich cools last @ lowest temps. This means the previously cooled minerals react with the magma to form new (different) minerals

17. Bowen’s Reaction Series Bowen’s Reaction Series Discontinuous Iron-rich Branch Minerals change suddenly at dif. Temps Minerals change suddenly at dif. Temps Olivine cools 1 st @ 1800 o C using up iron & magnesium Olivine cools 1 st @ 1800 o C using up iron & magnesium When too little Iron & magnesium is left for olivine formation, pyroxene will form When too little Iron & magnesium is left for olivine formation, pyroxene will form As more iron & magnesium get used the minerals that follow are more silica & oxygen rich As more iron & magnesium get used the minerals that follow are more silica & oxygen rich Therefore rocks abundant in silicate minerals form last (Quartz) Therefore rocks abundant in silicate minerals form last (Quartz)

18. Chemical Makeup Granitic (also known as Felsic) Light color & low density Light color & low density Make up most of the continental crust. Make up most of the continental crust. Ex/ granite & rhyolite Ex/ granite & rhyolite

19. Chemical Make-Up or Basaltic (also known as Mafic) Dark colored and high in density Dark colored and high in density Main type of rocks in the oceanic crust. Main type of rocks in the oceanic crust. Ex/ Gabbro & Basalt Ex/ Gabbro & Basalt Ultramafic –very low silica and high iron & magnesium Extremely dark in color Extremely dark in color

20. Coarse Texture Coarse textures have mineral crystals large enough to be clearly seen Slow cooling deep within Earth’s crust

21. Fine Grained Texture Fine grains and crystal are not able to be distinguished w/the naked eye Fast cooling close to, or at Earth’s surface

22. Glassy Texture No crystal shapes because it cooled incredibly fast, so crystals become compact glass

23. Vesicular Texture Spongy appearance due to gases (bubbles) trapped in magma Spongy appearance due to gases (bubbles) trapped in magma

24. Porphyritic Textures Course-grained crystals surrounded by fine- grained Course-grained crystals surrounded by fine- grained Two cooling histories: slowly deep within the crust then forced upward & cooled quickly Two cooling histories: slowly deep within the crust then forced upward & cooled quickly

25. Igneous Classification