2. Sedimentary Rocks

3. All places on Earth are, at any moment, either EROSIONAL or DEPOSITIONAL High places are erosional Low places are depositional

4. Sedimentary Rocks Are made of pieces of other rock cemented together. Cover about 75% of Earth’s surface, BUT- Account for only about 5% of Earth’s crust (They make a very thin layer.) Are the key to Earth’s history.

5. I. Nature of Sediments A. Clastic = fragments of rock from weathering B. Chemical = dissolved rocks that crystallize C. Organic = once living materials (shells & leaves)

6. II. Types of sedimentary rocks A. Subclass clastic - Classified based on size of fragments (clasts).166

7. 1. Gravel - size fragments (or larger = >2mm) Require a lot of energy to transport, for example: fast rivers, glaciers, land slides –a. rounded = Conglomerate - transported a long distance by fast-flowing water (= fast fluvial) –b. angular = Breccia - transported a short distance by: Glaciers - deposited when ice melts Gravity - an alluvial environment or talus (scree)

8. 2. Sand-sized pieces (.166-2mm) = Sandstone Usually majority quartz. The farther it has been transported - the closer it will be to pure quartz. –a. river bank (fluvial) –B. beaches –C. windblown

9. Silt & Clay - sized pieces ( <.166mm) = Shale Products of feldspars & micas weathering Deposited: –a. where mud piles up (flood plains, basins, deltas, offshore) –b. quiet water - slow rivers

10. B. Subclass Chemical From dissolved minerals Often single mineral rocks (so rocks are not always mixtures of minerals.) Two ways for formation: –E–Evaporites –P–Precipitates –(–(see next two slides)

11. 1.Evaporites - water totally gone: A. halite (NaCl) - forms Rock Salt B. gypsum (CaSO 4 ) - Rock Gypsum

12. 2. Precipitates - minerals crystallize out of solution (without body of water drying up) a. calcite (CaCO 3 ) - Limestone –1. deep ocean (cold!!) –2. underground - stalactites & stalagmites) –3. at surface - Travertine (Tonto Natural Bridge or Havasupai Canyon) b. quartz (SiO 2 ) - requires hydrothermal (hot) water! 1. small hollow sphere = Geode 2. veins in cracks with secondary minerals

13. C. Subclass Organic - once living organisms 1. Ocean critters (Clams, oysters, snails, etc.) - Limestone 2. Leaves, wood, swamp material: –a. solid, soft - Coal –b. liquid, viscous - Petroleum –c. volatile gasses - Natural Gas

14. III. Sedimentary Environments:

15. Oceans:

16. IV. Sedimentary Structures: A. Stratification = continuous horizontal layers. Most often deposited in water. –1. Small scale - lakes, riverbeds, deltas –2. Grand (large) scale - ocean basins

17. C. Graded Bedding (storm layers)

18. D. Surface impressions: 1. Ripple marks - 2. Mud Cracks - 3. Tracks -