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FROM INTO SEDIMENTARY

Objectives

• Identify three types of . • Explain where and how chemical and biogenic sediments form. • Explain three processes that lead to the lithification of sediments. • Explain how features such as ripples, cracks, and tell geologists about the environment in which a rock originated. • Identify plate tectonics that are favorable for the accumulation of sediments.

Sediments and Sedimentation

– The laying down of sediment • Sediment separated into three broad categories – Clastic – Chemical – Biogenic

1 Sediments and Sedimentation

Sediments and Sedimentation

• Clastic sediment – Sediment formed from fragmented rock and mineral debris – Produced by and – Described by particle shape, angularity, and size

• Clastic sediment – Volcaniclastic sediments • Volcanic in origin • Pyroclasts – Distinguished by size » Bombs » Lapilli » Ash

2 Clastic sediment

Clastic sediment

Clastic sediment

Glacial : poorly sorted Well sorted, well rounded, quartz

3 Sediments and Sedimentation • Chemical sediment – Sediment formed by the precipitation of minerals dissolved in lake water, water, or water – Plants and animals alter chemical balance • – Shallow sea water evaporation causes dissolved salts to precipitate

Sediments and Sedimentation

• Biogenic sediment – Sediment that is primarily composed of plant or animal remains • Shells, bones, teeth • Wood, roots, leaves – Or, precipitates as a result of biologic processes: foraminifer in the head of a pin

Sedimentary Rocks • Lithification – The processes by which loose sediment is transformed into • Bedding – The layered arrangement of strata in sediment/sedimentary rock • Bedding surface – The top or bottom surface of a rock stratum or bed

4 Lithification Processes

Lithification Processes

Lithification Processes

– Reduction of pore space in a sediment as a result of the weight of overlying sediments • Cementation – Substances dissolved in pore water precipitate out and form a matrix in which grains of sediments are joined together

5 Lithification Processes • Recrystallization – The formation of new crystalline mineral grains

What kind of sediment?

• How do you know? • How do you know?

Compare textures of a sedimentary rock with an igneous rock (granite)

6 Types of Sedimentary Rocks • Clastic sedimentary rock – • Has large fragments in a finer grained matrix – • Medium grained, where clasts are typically, but not necessarily, dominated by quartz grains – Mudstone • A very fine grained sedimentary rock of the same composition as but without fissility – Shale • A very fine grained fissile or laminated sedimentary rock, consisting primarily of sized particles

Conglomerate

Figure 7.6

Quartz sandstone

Figure 7.4

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Figure 7.7

Shale with plant remains

Figure 7.2

Types of Sedimentary Rocks

• Chemical sedimentary rocks – • Formed by the evaporation of lake water or sea water, followed by lithification of the resulting salt deposit – Banded iron formation • A type of chemical sedimentary rock rich in iron minerals or silica

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Bedrock of Lower Michigan

http://www.deq.state.mi.us/documents/deq-glm-rcim-geology- 1987_Bedrock_Geology_Map.Pdf

9 Travertine-Mammoth Hot Springs, Yellowstone NP

Banded Iron Formation (BIF)

Types of Sedimentary Rocks

• Biogenic sedimentary rocks – Limestone • A sedimentary rock that consists primarily of the mineral • Formed from the accumulation and compaction of plant remains – • A combustible rock formed from the lithification of plant-rich sediment

10 Coquina

Figure 7.9

Chalk

White Cliffs of Dover

11 Depositional Environments

• Interpreting environmental clues – Patterns formed by air and water moving over sediments • Preserved and later exposed – Ripple marks – Fossils – Mud cracks

Characteristics-fossils

Fossiliferous limestone

12 Mud cracks

Depositional Environments on Land

Depositional Environments on Land • Streams • Lakes – Delta • A sedimentary deposit, commonly triangle shaped, that forms where a stream enters a standing body of water – – Wind • Eolian sediment – Sediments that are carried and deposited by the wind

13 Depositional Environments on Land

Delta Old Lake bed

Lacustrine sediments-Lake Michigan Bluffs

Depositional environments in and near the ocean • Delta • – Semi-enclosed body of coastal water, in which fresh water mixes with sea water • Beaches • Shelves • Carbonate platforms and reefs Green beach due to olivine

14 Chesapeake Bay: An Estuary

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Depositional environments in and near the ocean

Carbonate platform in the Bahamas

16 Depositional environments in and near the ocean • – A turbulent, gravity driven flow consisting of a mixture of sediment and water, – Conveys sediment from the continental shelf to the deep sea • http://www.youtube.com/watch?v=tfNLI2JW7mg&NR=1 • Seafloor – Rich in nutrients • ooze •

Deep sea sediments deposited by ()

How Plate Tectonics Affect Sedimentation

• Divergent plate boundaries – Rift valleys • A linear, -bounded valley along a divergent plate boundary or spreading center • Convergent plate boundaries – Collisional type – Subduction type • Back-arc basin • Accretionary wedges • Ophiolites (slabs of oceanic lithosphere)

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