Title: Sedimentary Rock:
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2Sedimentary Rock Clastic - particles deposited,
cemented like sandstone, shale Chemical -
precipitation out of solution like salt,
gypsum, some limestone Organic - accumulation of
parts of plants and animals - swamps (coal),
shells (limestone)
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5Sandstone
6Conglomerate
7Breccia
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9Coquina (ko-KE-na)
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15Graded bedding
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25Playa (dry basin salt flat)
26Salt mine
27Bonneville Salt Flats
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36MAJOR FACTORS IN METAMORPHISM 1) Composition of
Parent Rock 2) Temperature 3) Pressure 4) Time 5)
Effects of fluids (water)
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46Sandstone to quartzite
47Limestone to marble
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50Start of Sun-driven part of Rock Cycle
WEATHERING ? Two forms Mechanical, Chemical
51Q? Why are the streets of Chicago much worse than
those of Houston each Spring?
52Q? Why are the streets of Chicago much worse than
those of Houston each Spring? Answer Frost
Action
53Q? Why are the streets of Chicago much worse than
those of Houston each Spring? Answer Frost
Action Q? Why are the streets of Chicago much
worse than those of northern Sweden?
54Q? Why are the streets of Chicago much worse than
those of Houston each Spring? Answer Frost
Action Q? Why are the streets of Chicago much
worse than those of northern Sweden? Answer
More freezing and thawing.
55Mechanical Weathering (1) Frost Wedging
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57Mechanical Weathering (2) Plant growth
58Mechanical Weathering (3) Pressure release
59Mechanical Weathering (4) Large Temperature
changes (also forest fires)
60Mechanical Weathering (5) Growth of salt crystals
61- Chemical Weathering
- Dissolution
- Hydrolysis
- Oxidation
- More significant than Mechanical Weathering (in
volume of rock affected) - Especially dominant in wet climates
62Chemical Weathering (1) Dissolution First
CARBONIC ACID is produced as H2O CO2 --gt
H2CO3 Then the carbonic acid dissolves calcite
as H2CO3 CaCO3 --gt Ca2 2(HCO3)-
(Carbonic acid) (calcite) (dissolved
calcium bicarbonate)
63Q? (to be answered on field trip) Why are these
basins here?
64Chemical Weathering (2) Hydrolysis Addition of
water (often as OH- hydroxyl) to a rock to form a
new rock Turns FELDSPAR into CLAYS Greatly
affects Basalt and Granite (Feldspar is the
most abundant mineral in cont. crust, and clay is
the most abundant sediment in ocean and
continental crust)
65HYDROLYSIS First CARBONIC ACID is produced.
Then the carbonic acid dissolves the feldspar as
(for example) 4NaAl3Si3O8 4H2CO3 18H2O --gt
4Na 4(HCO3)- 8H4SiO4 Al4Si4O10(OH)8 (Na-pla
g.) carb. acid water (dissolved
components) clay Provides the clays
that form shale, the most abundant sedimentary
rock Provides the sodium for all the ocean
salt
66Hydrolysis Greatly accelerated in the presence
of acidic rain
67Chemical Weathering (3) Oxidation Addition of
oxygen to a mineral to form a new mineral Most
common is with iron gtgt RUST Minerals start as
OLIVINE, PYROXENE, AMPHIBOLE Minerals end up as
HEMATITE and LIMONITE Ex/ 2Fe2SiO4 4H2O O2
---gt 2Fe2O3 2H4SiO4 (olivine)
(hematite) (dissolved silicic
acid)
68This dissolved silica is deposited in the form of
cryptocrystalline forms of quartz such as chert,
which can form either inorganically, or
biochemically as the shells of diatoms or
radiolaria.
69Mechanical and Chemical Weathering work together.
701.
712.
723.
73Weathering stability of minerals is the reverse
of the Bower reaction cycle, for the same reason
strength of covalent bonds of silica tetrahedra.
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76An end product of weathering is SOIL.
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78Soil varies as a function of latitude because of
climate differences.
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80Soil Affected by bedrock type
81Soil Affected by slope.
82Soil Affected by vegetation
83Q? Why is cutting down rain forests to grow crops
a bad idea?
84A. Tropical regions have the worst soils in the
world (all nutrients have been washed down
through the soils by high rainfall.
85MASS WASTING The removal of weathered rock and
soil.
861st Rule of Geology Rocks Fall Downhill
87Rockfall
88Rockfall
89Landslide
90Landslide
91Landslide
92Landslide
93Slump
94Slump
95Slump
96Slump
97Mudflow
98Mudflow
99Mudflow
100Mudflow (lahar)
101Creep
102Creep
103Creep
104Underwater flows
105Weathering/Mass Wasting Responsible for the
appearance of the land surface.
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