Laboratory 2 - Sedimentary Rocks 2013
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Transcript of Laboratory 2 - Sedimentary Rocks 2013
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Sedimentary rocks
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Weathering is the general process by which rocksand soils are broken down at Earth's surface(through contact with the Earth's atmosphere,biota and waters) to produce sediment particles.
-in takes place in-situ (in place no mo ement)
!here are two types of weathering
mechanical or physical weathering chemical weathering
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Physical weathering thermal stress - e"pansion and contraction of rock, caused by
temperature changes
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Physical weathering frost weathering
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Physical weathering pressure release
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Physical weathering pressure release
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Physical weathering bio-mechanical
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#io-mechanical weathering
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$hemical weathering
$hemical weathering changes the composition ofrocks.
water interacts with minerals to create ariouschemical reactions.
-is a gradual and ongoing process as the mineralogyof the rock adjusts to the near surface en ironment.
%ew or secondary minerals de elop from theoriginal minerals of the rock. &n this the processesof oxidation and hydrolysis are most important.
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umidity
!emperature !opography !ime Surface area
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Erosion Erosion is the process by which soil and rock
are removed from the Earth s surface bye"ogenetic processes such as wind or waterflow, and then transported and deposited inother locations.
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!ransport agents - *ra ity
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!ransport agents - ind
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!ransport agents - ind
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!ransport agents &ce
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!ransport agents ater- +lu ial
transport
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!ransport agents ater- $ostal
transport
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aterial transport in a ri er
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Sediments s.Sedimentary rocks
sand Sand stone
uart grains cement
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$ementation of soils
/ores ( oids)
$lasts (soil particles)
$ement precipitation
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Sand stone
onglomerate
$lay stoneSilt stone
Sedimentary rocksclassification
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/article Shape
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/article shape - Spherisity
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$onglomerate#recia
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/article sorting 0 uniformity ofparticles
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$lay minerals
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!etraedric layer
!
"ctaedric layer
"trioctaedric dioctaedric
$lay minerals
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#$# %!-"&$lay minerals
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'$# %!-"-!& $lay minerals
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