1. THE LANGUAGE OF THE EARTH – PART II SEDIMENTARY ROCKS

3. Principles applied to Sedimentary Rocks Uniformitarianism: The Present is the Key to the Past

4. Principles applied to Sedimentary Rocks Superposition Original Horizontality Faunal Succession Time

5. Siccar Point, Scotland UNCONFORMITIES “Looking into the Abyss of Geological Time”

6. Definition SEDIMENTARY ROCK - Compacted and cemented accumulations of sediment, which can be of two general types - clastic and chemical. Clastic - composed of fragments of pre-existing rock that have been weathered, eroded and transported by wind, water, ice, or mass movement to a site of deposition. Chemical -composed of minerals precipitated from water (usually ocean water) due to evaporation or to the metabolic action of organisms (biogenic).

7. Sedimentary Rocks: Definition and General Types Sediment Sedimentary Rock SEDIMENTARY ROCK SEDIMENTARY ROCK - Compacted and cemented accumulations of sediment, which can be of two general types - clastic and chemical. Clastic Clastic - composed of fragments of pre-existing rock that have been weathered, eroded and transported by wind, water, ice, or mass movement to a site of deposition. Chemical Chemical -composed of minerals precipitated from water (usually ocean water) due to evaporation or to the metabolic action of organisms (biogenic).

8. Clastic Sedimentary Rocks Composed of fragments of pre-existing rock that have been weathered,... Mechanical Weathering

9. Chemical Weathering Clastic Sedimentary Rocks Composed of fragments of pre-existing rock that have been weathered,...

10. Clastic Sedimentary Rocks Composed of fragments of pre-existing rock that have been weathered, transported... by Ice (Glaciers)

11. Continental Glaciation Till  Tillite

12. Clastic Sedimentary Rocks Composed of fragments of pre-existing rock that have been weathered, transported,... by Water

13. The Work of Rivers – Transport Sediment to the Sea

14. 4 Mature Rivers – Floodplains and Meanders

15. Effects of Changing Base Levels due to tectonic uplift or changing sea level

16. Clastic Sedimentary Rocks Composed of fragments of pre-existing rock that have been weathered, transported,... by Wind Cross-bedding

17. Clastic Sedimentary Rocks Composed of fragments of pre-existing rock that have been weathered, eroded, and transported to a site of deposition

18. Deltaic Environments deposition of sediment due to loss of transport energy

19. Near-shore Environments of Deposition

20. Deep-water Deposition

21. Distinguishing Characteristics of Clastic Sediments: Grain Size - mud/clay, silt ( 256mm); particle size reflects energy (velocity) of the transport and depositional system.

22. Distinguishing Characteristics of Clastic Sediments (cont.): Sorting - Well-sorted sediment indicates prolonged reworking by wind or water; poorly sorted sediment may indicate rapid deposition, or deposition by ice or mass movement. Angularity/Roundness and Shape – Well rounded sediment also indicate prolonged reworking by transporting agent; the shape of grains often indicates the transport system, but also may be related to the type of mineral or rock fragment

23. Distinguishing Characteristics of Clastic Sediments (cont.): Compositional Maturity - mature sediment contains only Quartz and Clay and reflects prolonged weathering of the source rocks. Immature sediment contains other minerals or rock fragments that may imply mostly mechanical weathering in the source region and short transport distance.

24. Distinguishing Characteristics of Clastic Sediments (cont.): Bedding/Stratification - Sediments transported by water and wind are typically bedded (or stratified) due to fluccuations in the velocity of transport and sediment load. Graded bedding is a gradual change from coarse particles at the base to fine particles at the top of a bed that reflects a gradual decrease in the energy of the depositional environment. Cross-bedding forms by dune migration in fluvial (stream), marine, or eolian environments. Sediment transported by ice or mass movement are typically unbedded (massive).

25. Lithification Transformation of Sediment into Sedimentary Rock Compaction and Cementation of Clastic Sediments Common Cementing Agents: Quartz, Calcite, Hematite Gravel Conglomerate

26. Lithification Compaction and Cementation of Clastic Sediments

27. Basic Types of Clastic Sedimentary Rocks MUDSTONE/SHALE - Well-sorted, mature, clay-sized particles ; generally implies deposition into quiet water SANDSTONE - Well-sorted, mature, commonly bedded, sand-sized particles typically transported by wind or moderate water movement (e.g. rivers, beaches) GREYWACKE - Moderately sorted, immature, clay- to sand-sized particles commonly showing graded bedding. Commonly deposited in deep waters off mountainous coasts. CONGLOMERATE - Poorly sorted, immature, clay to boulder-sized particles transported only a short distance from their source and typically deposited by fast moving water. TILL - Very poorly sorted, clay to boulder-sized particles; non-bedded; deposited from glaciers.

28. Environments of Deposition of Clastic Sedimentary Rocks

29. Chemical Sedimentary Rocks composed of minerals precipitated from water (usually ocean water) due to evaporation or to the metabolic action of organisms (biogenic) From Plummer and Carlson

30. IRON-FORMATION - Iron oxide minerals, usually magnetite (taconite ore) or hematite (natural ore), interlayered with chert (microcrystalline quartz) and clay minerals. Common chemical sedimentary rock biogenically formed in shallow marine environments older than about 1.8 billion years. Chemical Sedimentary Rocks

31. LIMESTONE - Calcium carbonate (calcite) commonly containing abundant marine fossils. Most common type of chemical sediment forming today by evaporation and biogenic processing of seawater. Dolomite (or dolostone) is created by replacement of calcium by magnesium after shallow burial of limestone. Forms in tropical shallow marine environments. Chemical Sedimentary Rocks Non-fossiliferous LimestoneFossiliferous Limestone

32. Chemical Sedimentary Rocks Fossiliferous Limestone Non-fossiliferous Limestone Oolitic Limestone Oolitic LS Dunes, Bahamas BiogenicInorganic, ~clastic

33. CHERT – Microcrystalline quartz (SiO 2 ) ; commonly found interbedded with iron oxide in iron formation or as replacement nodules in limestone Chemical Sedimentary Rocks White and red chert interlayered with hematite, Soudan Iron Formation Chert nodules in Limestone

34. Chemical Sedimentary Rocks EVAPORITE DEPOSITS (Gypsum, Halite, Anhydrite) – minerals precipitated from saline water in arid environments with high evaporation rates (e.g., playa lakes)

35. PEAT/COAL – Carbonaceous material created by the accumulation, compaction and heating of organic matter. Forms in temperate to tropical, low energy, terrestrial environments (lagoons, floodplains). Organic Sedimentary Rocks

36. Environments of Chemical Sedimentation Evaporites Coal Limestone