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Sedimentary Rocks

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Title: Sedimentary Rocks


1
Sedimentary Rocks The Archives of Earth History
?
Disconformity
2
There are actually 3 types of rocks
  • Igneous cool from liquid (magma or lava)
  • Metamorphic pre-existing rocks that have been
    altered by intense temperature or pressure
  • Sedimentary form mainly from deposition of
    sediments

3
Historical geology focuses on sedimentary rocks
Why???
  • Only rocks that contain fossils
  • Indicate ancient depositional environments

4
What is a sediment?
  • Fragment of pre-existing rock (or animal shell)
  • Why does water off Galveston look murky, while
    water off Florida looks clear?

5
What kind of rocks do we find around Houston?
  • Not many rocks!
  • Lots of unlithified sediment
  • Why do many houses in Houston have foundation
    problems?

6
What is a sedimentary rock?
  • Rock that forms at or near Earths surface
  • 3 types
  • Clastic
  • Chemically-precipitated
  • Biogenic

7
How do clastic sedimentary rocks form?
  • Weathering
  • Transport
  • Deposition
  • Lithification

8
How do other sedimentary rocks form?
  • Chemical precipitation of dissolved materials
  • Biogenic (organic) accumulations of organic
    material

9
Environments of Deposition
  • At or near surface of Earth
  • Marine
  • Continental
  • Transitional (deltas, barrier islands, beaches)

10
Marine
  • Coastal
  • Shelf
  • Deep water

www.ngdc.noaa.gov/mgg/image/sedthick.jpg
11
Continental
  • Fluvial
  • Meandering
  • Braided
  • Desert
  • Lacustrine
  • Glacial

www.uoregon.edu/millerm/depenv.html
12
Continental
  • Fluvial
  • Meandering
  • Braided
  • Desert
  • Lacustrine
  • Glacial

www.uoregon.edu/millerm/depenv.html
13
Continental
  • Fluvial
  • Meandering
  • Braided
  • Desert
  • Lacustrine
  • Glacial

www.uoregon.edu/millerm/depenv.html
14
Dune Cross-Beds
  • Large-scale cross-beds in a Permian-aged
    wind-blown dune deposit in Arizona

15
Continental
  • Fluvial
  • Meandering
  • Braided
  • Desert
  • Lacustrine
  • Glacial

www.mikelevin.com/DLBlissParkTahoe.jpg
16
Continental
  • Fluvial
  • Meandering
  • Braided
  • Desert
  • Lacustrine
  • Glacial

www.peakware.com/encyclopedia/peaks/photos/everest
7.htm
17
Moraines and Till
  • Origin of glacial drift
  • Moraines and poorly sorted till

18
Delta
  • Form in oceans or lakes (marine and non-marine)

www.uoregon.edu/millerm/depenv.html
19
Stream/River-Dominated Deltas
  • Stream/river-dominated deltas
  • long distributary channels extending far seaward
  • Mississippi River delta

20
Where would you find different sedimentary rocks?
21
Where would you find different sedimentary rocks?
22
Where would you find different sedimentary rocks?
  • Grain size is controlled by energy
  • High energy
  • River
  • Beach
  • Low energy
  • Lake
  • Deep ocean

Large grains
Small grains
23
Sorting, Rounding
  • If the size range is not very great,
  • the sediment or rock is well sorted
  • If they have a wide range of sizes,
  • they are poorly sorted
  • Wind has a limited ability to transport sediment
    so dune sand tends to be well sorted
  • Glaciers can carry any sized particles because of
    their transport power, so glacier deposits are
    poorly sorted
  • Grains more rounded with longer transport

24
Rounding and Sorting
  • A deposit of well rounded and well sorted gravel
  • Angular, poorly sorted gravel

25
Cross-Bedding
  • Tabular cross-bedding forms by deposition on sand
    waves
  • Tabular cross-bedding in the Upper Cretaceous Two
    Medicine Formation in Montana

26
Current Ripple Marks
  • form in response to water or wind currents
    flowing in one direction
  • asymmetric profiles allowing geologists to
    determine paleocurrent directions

http//www3.interscience.wiley.com8100/legacy/col
lege/levin/0470000201/chap_tutorial/ch03/chapter03
-5sedstr.html
27
Wave-Formed Ripple Marks
  • As the waves wash back and forth, symmetrical
    ripples form
  • Wave-formed ripple marks in shallow seawater

28
Modern Deposition near Houston
  • Fluvial
  • Brazos, Colorado, Trinity, San Jacinto Rivers
  • Transitional
  • Deltas, barrier islands
  • Marine
  • Gulf of Mexico

29
Ancient Environments
  • Important for historical geology
  • Important for oil companies (need to know where
    sand was deposited)

Why are we looking at modern depositional
environments?
30
Present is the key to the past
  • Study modern depositional environments to learn
    about ancient ones
  • Knowledge of ancient environments helps oil
    companies and historical geologists

31
Brazos River
  • Longest river in Texas 1450 km
  • Highest sediment supply of any Texas river
  • Originates in New Mexico

32
Where does deposition occur?
www.uwsp.edu/geo/courses/geog391/toriv/Diagrams.ht
m
33
Point Bars
  • Sediment deposited within the inside bank of a
    meander loop
  • Fining upward sequence (grain size decreases)
  • Coarsest sediment deposited by highest energy

34
Brazos River Point Bar
35
Brazos River Cut Bank
36
Coastal Galveston Island
37
Barrier Islands
  • Formed during sea level rise
  • Rate of SL rise and rate of sediment deposition
    approximately equal
  • Wave-dominated environment

38
Barrier Islands
  • On broad continental margins with abundant sand,
    long barrier islands lie offshore separated from
    the mainland by a lagoon
  • Barrier islands are common along the Gulf and
    Atlantic Coasts of the United States
  • Subenvironments of a barrier island complex
  • beach sand grading offshore into finer deposits
  • dune sands contain shell fragments (not found in
    desert dunes)
  • fine-grained lagoon deposits

39
Barrier Island Complex
  • Subenvironments of a barrier island complex

40
Texas Coast
  • Most Texas beaches relatively fine-grained
  • Low gradient of rivers like Brazos
  • Why is this a problem?

41
Brazos Delta
gulf.rice.edu
42
Environmental Interpretations and Historical
Geology
  • Present-day gravel deposits by a swiftly-flowing
    stream
  • (Most transport and deposition takes place when
    the stream is higher)
  • Nearby gravel deposit probably less than a few
    thousand years old

43
Environmental Interpretations and Historical
Geology
  • Conglomerate more than 1 billion years old
  • shows similar features
  • We infer that it too was deposited by a braided
    stream
  • Why not deposition by glaciers or along a
    seashore?
  • No evidence for either glacial activity or
    transitional environment
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