Sedimentary Rocks— The Archives of Earth History

1. Chapter 6 Sedimentary Rocks—The Archives of Earth History

2. Sedimentary Rocks • Are formed at or near the surface at relatively low temperatures. • Are formed from sediments which include boulders, cobbles, gravels, sands, silts, and clay particles. • Also included as sediments are particles which are suspended and dissolved in water. • Sedimentary rocks • preserve evidence of surface depositional processes • also, many contain fossils • These things give clues to the depositional environment • Depositional environments are specific areas • or environments where sediment is deposited

3. Depositional environments are specific areas or environments where sediment is deposited • How do we know whether sedimentary rocks were deposited on • continents—river floodplains or desert sand dunes? • at the water's edge? • in the sea?

4. Beach Environment • Sand deposition • Sand-size particles are deposited on a beach along the Pacific coast of the United States • After many years and layers of deposition, sand is compacted, and eventually cemented to form sandstone. • Many ancient sandstones • possess features that indicate they were also deposited on beaches • Present day despositional environments are used as models to help decode the rocks of the past. (uniformitarianism)

5. Sedimentary rocks • Sedimentary rocks may be • detrital • or chemical, including biochemical • and all preserve evidence • of the physical, chemical and biological processes • that formed them • Some sedimentary rocks are a natural resource for • phosphorous • liquid petroleum • natural gas

6. Investigating Sedimentary Rocks • Observation and data gathering • carefully examine • textures • composition • fossils (if present) • thickness • relationships to other rocks • Preliminary interpretations in the field • For example: • red rocks may have been deposited on land • whereas greenish rocks are more typical of marine deposits • (caution: exceptions are numerous)

7. Detrital Rocks • Very common minerals in detrital rocks: • quartz, feldspars, and clay minerals • Detrital rock composition tells • about source rocks, • not transport and deposition • Quartz sand may have been deposited • in a river system • on a beach or • in sand dunes • Quartz is durable and can withstand water and wind transport

8. Grain Size • Detrital grain size gives some indication • of the energy conditions • during transport and deposition • High-energy processes • such as swift-flowing streams and waves • are needed to transport gravel • Conglomerate must have been deposited • in areas where these processes prevail • Sand transport also requires vigorous currents • Silt and clay are transported • by weak currents and accumulate • only under low-energy conditions • as in lakes and lagoons

9. Chemical Sedimentary Rocks • Composition of chemical sedimentary rocks • is more useful in revealing environmental information • Limestone is deposited in warm, shallow seas • although a small amount also originates in lakes or caves • Evaporites such as rock salt and rock gypsum • indicate arid environments where evaporation rates were high • Coal originates in swamps and bogs on land

10. Sorting and Rounding • Sorting and rounding are two textural features • Sorting refers to the variation in size of particles • “well sorted” – particles are similarly sized • “poorly sorted” – particles vary in size within a rock • Well-sorted material implies transport by water or wind. • Poorly sorted material implies transport by ice, or debris flow • Some sediments are not transported; they remain where deposited until lithified

11. Rounding • Rounding is the degree to which sediments have their sharp corners and edges worn away by abrasion • Gravel in transport is rounded very quickly as the particles collide with one another • Sand becomes rounded with considerably more transport

12. Rounding and Sorting • A deposit • of well rounded • and well sorted gravel • Angular, poorly sorted gravel

13. Sedimentary Structures • Sedimentary structures are • features visible at the scale of an outcrop • that formed at the time of deposition or shortly thereafter • and are manifestations of the physical and biological processes that operated in depositional environments • Structures • seen in present-day environments • help provide information about depositional environments of rocks with similar structures

14. Bedding • Sedimentary rocks generally have bedding orstratification • Individual layers less than 1 cm thick are laminations • common in mudrocks • Beds are thicker than 1 cm • common in rocks with coarser grains

15. Graded Bedding • Graded bedding is common in turbidity current deposits • which form when sediment-water mixtures flow along the seafloor • Some beds show an upward gradual decrease • in grain size, known as gradedbedding • As they slow, • the largest particles settle out then smaller ones

16. Cross-Bedding • Cross-bedding forms when layers come to rest • at an angle to the surface • upon which they accumulate • as on the downwind side of a sand dune • Cross-beds result from transport • by either water or wind • The beds are inclined or dip downward • in the direction of the prevailing current • They indicate ancient current directions, • or paleocurrents • They are useful for relative dating • of deformed sedimentary rocks

17. Cross-Bedding • Tabular cross-bedding forms by deposition on sand waves • Tabular cross-bedding in the Upper Cretaceous Two Medicine Formation in Montana

18. Cross-Bedding • Trough cross-bedding formed by migrating dunes • Trough cross-beds in the Pliocene Six Mile Creek Formation, Montana

19. Ripple Marks • Small-scale alternating ridges and troughs • known as ripple marks are common • on bedding planes, especially in sandstone • Current ripple marks • form in response to water or wind currents • flowing in one direction • and have asymmetric profiles allowing geologists • to determine paleocurrent directions • Wave-formed ripple marks • result from the to-and-fro motion of waves • tend to be symmetrical • Useful for relative dating of deformed sedimentary rocks

20. Current Ripple Marks • Ripples with an asymmetrical shape • In the close-up of one ripple, • the internal structure • shows small-scale cross-bedding • The photo shows current ripples • that formed in a small stream channel • with flow from right to left

21. Wave-Formed Ripples • As the waves wash back and forth, • symmetrical ripples form • The photo shows wave-formed ripple marks • in shallow seawater

22. Mud Cracks • When clay-rich sediments dry, they shrink • and crack into polygonal patterns • bounded by fractures called mud cracks • Mud cracks require wetting and drying to form, • as along a lakeshore • or a river flood plain • or where mud is exposed at low tide along a seashore

23. Ancient Mud Cracks • Mud cracks in ancient rocks • in Glacier National Park, Montana • Mud cracks typically fill in • with sediment • when they are preserved • as seen here

24. Biogenic Sedimentary Structures • Biogenic sedimentary structures include • tracks • burrows • trails • called trace fossils • Extensive burrowing by organisms • is called bioturbation • It may alter sediments so thoroughly • that other structures are disrupted or destroyed

25. Bioturbation • U-shaped burrows • Vertical burrows

26. Bioturbation • Vertical, dark-colored areas in this rock are sediment-filled burrows • Could you use burrows such as these to relatively date layers in deformed sedimentary rocks?

27. No Single Structure Is Unique • Sedimentary structures are important • in environmental analyses • but no single structure is unique to a specific environment • Example: • Current ripples are found • in stream channels • in tidal channels • on the sea floor • Environmental determinations • are usually successful with • associations of a groups of sedimentary structures • taken along with other sedimentary rock properties

28. Geometries • Some Sediments are extensive “sheets” deposited during marine transgressions or regressions. • Delta deposits tend to be lens shaped • when viewed in cross profile or long profile • but lobate when observed from above • Buried reefs are irregular • but many are long and narrow • or rather circular

29. Fossils—The Biological Content of Sedimentary Rocks • Fossils • are the remains or traces of prehistoric organisms • can be used in stratigraphy for relative dating and correlation • are constituents of rocks, sometimes making up the entire rock • and provide evidence of depositional environments • Many limestones are composed • in part or entirely of shells or shell fragments • Much of the sediment on the deep-seafloor • consists of microscopic shells of organisms

30. Fossils Are Constituents of Sedimentary Rocks • This variety of limestone, • known as coquina, • is made entirely of shell fragments

31. Fossils in Environmental Analyses • Did the organisms in question live where they were buried? • Or where their remains or fossils transported there? • Example: • Fossil dinosaurs usually indicate deposition • in a land environment such as a river floodplain • But if their bones are found in rocks with • clams, corals and sea lilies, • we assume a carcass was washed out to sea

32. Environmental Analyses • What kind of habitat did the organisms originally occupy? • Studies of a fossil’s structure • and its living relatives, if any, • help environmental analysis • For example: clams with heavy, thick shells • typically live in shallow turbulent water • whereas those with thin shells • are found in low-energy environments • Most corals live in warm, clear, • shallow marine environments where • symbiotic bacteria can carry out photosynthesis

33. Depositional Environments • A depositional environment • is anywhere sediment accumulates • especially a particular area • where a distinctive kind of deposit originates • from physical, chemical, and biological processes • Three broad areas of deposition include • continental • transitional • marine • each of which has several specific environments

34. Depositional Environments Transitional environments Continental environments Marine environments

35. Continental Environments • Deposition on continents (on land) might take place in • fluvial systems – rivers and streams • deserts • areas covered by and adjacent to glaciers • Deposits in each of these environments • possess combinations of features • that allow us to differentiate among them

36. Fluvial • Fluvial refers to river and stream activity • and to their deposits • Fluvial deposits accumulate in either of two types of systems • One is a braided stream system • with multiple broad, shallow channels • in which mostly sheets of gravel • and cross-bedded sand are deposited • mud is nearly absent

37. Braided Stream • The deposits of braided streams are mostly • gravel and cross-bedded sand with subordinate mud

38. Braided Stream Deposits • Braided stream deposits consist of • conglomerate • cross-bedded sandstone • but mudstone is rare or absent

39. Fluvial Systems • The other type of system is a meandering stream • with winding channels • mostly fine-grained sediments on floodplains • cross-bedded sand bodies with shoestring geometry • point-bar deposits consisting of a sand body • overlying an erosion surface • that developed on the convex side of a meander loop

40. Meandering Stream • Meandering stream deposits • are mostly fine-grained floodplain • sediments with subordinate sand bodies

41. Meandering Stream Deposits • In meandering stream deposits, • mudstone deposited in a floodplain is common • sandstones are point bar deposits • channel conglomerate is minor

42. Desert Environments • Desert environments contain an association of features found in • sand dune deposits, • alluvial fan deposits, • and playa lake deposits • Windblown dunes are typically composed • of well-sorted, well-rounded sand • with cross-beds meters to tens of meters high • land-dwelling plants and animals make up any fossils

43. Associations in Desert Basin • A desert basin showing the association • of alluvial fan, • sand dune, • and playa lake deposits • In the photo, • the light colored area in the distance • is a playa lake deposit in Utah

44. Dune Cross-Beds • Large-scale cross-beds • in a Permian-aged • wind-blown dune deposit in Arizona

45. Alluvial Fans and Playa Lakes • Alluvial fans form best along the margins of desert basins • where streams and debris flows • discharge from mountains onto a valley floor • They form a triangular (fan-shaped) deposit • of sand and gravel • The more central part of a desert basin • might be the site of a temporary lake, a playa lake, • in which laminated mud and evaporites accumulate

46. Glacial Environments • All sediments deposited in • glacial environments are collectively called drift • Till is poorly sorted, nonstratified drift • deposited directly by glacial ice • mostly in ridge-like deposits called moraines • Outwash is sand and gravel deposited • by braided streams issuing from melting glaciers • The association of these deposits along with • scratched (striated) and polished bedrock • is generally sufficient to conclude • that glaciers were involved

47. Moraines and Till • Moraines and poorly sorted till • Origin of glacial drift

48. Glacial Varves • Glacial lake deposits show • alternating dark and light laminations • Each dark-light couplet is a varve, • representing one year’s accumulation of sediment • light layers accumulate in summer • dark in winter • Dropstones • liberated from icebergs • may also be present • Varves with a dropstone

49. Transitional Environments • Transitional environments include those • with both marine and continental processes • Example: • Deposition where a river or stream (fluvial system) • enters the sea • yields a body of sediment called a delta • with deposits modified by marine processes, especially waves and tides • Transitional environments include • deltas • beaches • barrier islands and lagoons • tidal flats

50. Transitional Environments Transitional environments