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1/22/2015 1 Origin of Soils The Geological Cycle
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01 - Origin of Soils - University of Memphis for Students/01 - Origin of Soils (2... · Alluvial Soil (Alluvial Fan) ... 1/22/2015 12 Alluvial Soil (River Delta) ... Microsoft PowerPoint

Jul 10, 2018

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Page 1: 01 - Origin of Soils - University of Memphis for Students/01 - Origin of Soils (2... · Alluvial Soil (Alluvial Fan) ... 1/22/2015 12 Alluvial Soil (River Delta) ... Microsoft PowerPoint

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Origin of Soils

The Geological Cycle

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Igneous Rocks

Igneous Rocks

Intrusive magma cools slowly, producing coarse-grained

rocks such as GRANITE

Extrusive magma cools quickly, producing fine-grained

rocks such as BASALT

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Physical Weathering

Wind

Water

Earthquakes

Landslides

Freeze/Thaw Cycles

Growth of Ice, Salt Crystals

Growth of Plant Roots

Chemical Weathering

Oxidation – chemical addition of oxygen

Reduction – addition of hydrogen or removal of oxygen

Hydration – chemical addition of water

Carbonation – dissolution by carbonic acid

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Products of Weathering

Rock Type

Granite

Basalt

Shale / Slate

Sandstone

Limestone

Soil Type

Silty Sands

Clayey Soil

Clay / Silt

Sand

Clay / Silt

Transportation / Deposition

Transporting Agent

Gravity

WaterStreams

Rainfall

Ice

Wind

Soil Type

Colluvial

AlluvialFluvial

Pluvial

Glacial

Aeolian

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Sedimentary Rocks

www.docstoc.com

Detrital Sedimentary Rocks

Formed when sediment consolidates under the weight of overlying soil or is cemented in place by minerals (SiO2, CaCO3, FeO, MgO)

Gravel = conglomerate (rounded) or breccia (angular)

Sand = sandstone

Silt = siltstone

Clay = shale (foliated) or mudstone (massive)

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Biochemical Sedimentary Rocks

Formed by biological / chemical processes

Limestone – CaCO3 deposited by organic or inorganic processes

Chalk – CaCO3 deposited by single-cell animals in ocean environment

Gypsum – CaSO4 precipitate formed by the evaporation of seawater

Rock salt – NaCl precipitate formed by the evaporation of seawater

Coal – Carbon formed from decomposing plant and animal matter

Metamorphic Rocks

Produced when rocks are changed by combination

of heat, pressure, shearing stresses

Granite Gneiss

Basalt Schist

Shale Slate Schist

Sandstone Quartzite

Limestone Marble

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Soil Deposits

Residual Soils

http://echo2.epfl.ch/VICAIRE/mod_3/chapt_1/main.htm

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Colluvial Soils (Talus Slope)

GeologyCafé.com

Braided Streams

http://www.mccullyweb.com/glossary/defs/braided.jpg

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Meandering Streams

http://www.scienceclarified.com/landforms/images/ueol_03_img0108.jpg

Youthful Streams

http://www.personal.kent.edu/~cschweit/Stark/Romaniastream.gif

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Mature Streams

http://faculty.ccc.edu/cdl/Courses/geology201/labs/streams/Streams.htm

Meander Topography

http://www.ohiodnr.com/Portals/7/pubs/fs_gifs/stfs03fig4.gif

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Old Age Streams

http://notendur.hi.is/oi/Siberia%20photos/Meandering%20river%20on%20the%20Yamal%20tundra.jpg

Alluvial Soil (Alluvial Fan)

http://www.rmnp.com/RMNP-Areas-HorseshoePark-AlluvialFan.html

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Alluvial Soil (River Delta)

http://www.alaska-in-pictures.com/data/media/19/kenai-river-delta_1958.jpg

Lacustrine Soil (Varved Clay)

http://www.anr.state.vt.us/DEC/GEO/images/varveswaterbury.jpg

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Glacial Soils

coxclasses.com

Glacial Till

http://polar3.home.att.net/northpole-pics/thule/thule-glacial-rubble.jpg

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Glacial Till

http://jesse.usra.edu/articles/iceagemodule/resources/images/moraine_till_svalbard.jpg

Glacial Till

http://www.sfu.ca/geog351fall02/gp2/geography/PROJECT/till.jpg

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Outwash Plains

coxclasses.com

Outwash Plains

http://imgarcade.com/1/glacial-outwash-diagram/

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Aeolian Soil (Dust Storm)

Aeolian Soil (Sand Storm)

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Aeolian Soil (Volcanic Ash)

Origins of Loess

http://esp.cr.usgs.gov/info/eolian/14.gif

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Loess in the US

http://esp.cr.usgs.gov/info/eolian/1213.gif

Loess

http://www.outreach.canterbury.ac.nz/resources/geology/glossary/loess.jpg

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Loess

http://www.uamont.edu/facultyweb/francis/soilprofiles/WIowaLoessBluffs.jpg

Organic Soils

• Found in low-lying areas where water table is near or above the surface

• Water promotes plant growth which decomposes to form organic soils

• Tend to have a high water content

• Tend to be highly compressible

• Consolidate over time as water is expelled due to loads applied to the soil

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Organic Soils (Peat Bog)

https://www.flickr.com/photos/14716771@N05/8281432745/