Geology 1403 EXAM 2 focuses on weathering processes, illustrating the chemical formation of clay minerals, the role of frost wedging, and soil characteristics in various climates. It assesses understanding of geological weathering and its environmental implications.
Less humus is produced in the tropical rainforest because the B-horizon is so poorly developed
Less humus is produced in the cool, temperate forest but the rate of decay and oxidation is slower than in a tropical rainforest.
More humus is produced in the tropical rainforest but it is quickly washed away by the heavy rains
In a tropical rainforest, the forest-floor litter is offen burned during the dry season
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Tropical literates
Talus slopes
C soil horizons
Mature pedalfers
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The unfractured interior
The edges and corners
The crack surfaces not including edges and corners
All of the above show equal rate
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Soil bacteria produce organic acids that precipitate calcium carbonate in the B-horizon
Iron oxides and aluminum-rich clays are precipitated in the B-horizon
Humus accumulates below the solum in the C-horizon
Clays are eluviated upward from the C-horizon
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A) north-facing slopesreceivemoresunlightin the summer;snow meltsfaster and moresoilmoisture is availablefor thetrees
B)south-facingslopesreceivemoremoisfureandstrnlight;rock weatheringis slower
North-facingslopesreceive about thesameamountof precipitationassouth-facingslopes;lessmoisture evaporatesfrom north-facingslopes
South-facingslopesreceive less moisture, yetrockweatheringis faster
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Chemicalweatheringof olivine and plagioclase feldspar
Mechanicalweatheringof graniteandrhyolite
Chemicalweatheringof orthoclase feldspar
Differentialmechanical weathering of micas
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Low temperatures; very dry
Low temperatures;very moist
High temperatures; very dry
warm temperatures; very moist
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Corn; rows trending straight down the slope,frequent cultivation
Apples;land between the treesis planted in grass and not cultivated
Winterwheat;after the harvest,thefieldis plowed and left idle until next fall
Bean,rows are sPaced wider thanon a levelfield
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0, A, E, B, C,bedrock
A, B,C,D, E, bedrock
E, A, B,C,0, bedrock
D, E, C, B, A, bedrock
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Reduces grain sizes of rock particles
Allows for faster rates of chemical weathering
Is important in the formation of talus slopes
Involves a major change in the mineral composition of theweatheredmaterial
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Mechanical weathering of very fine-grained,blue-gray clays
Chemical weathering of quartz and feldspars
Precipitation of iron oxides during the chemical weatheringprocess
Mechanical weathering of the feldspars and micas in granit and rhyolite
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Transformational
Residual
Relict
Transported
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The long drought preceding the Irish potato famine of the 1840s
The area covered by volcanic ash around Mt. pinatubo,1991
Areas of severe wind erosion on the creat plains,1930s
A New Year's Day invitational soccer match in Tripoli, Libya
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Oxidation
Eluviation
Hydrologic cycling
Fros twedging
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Thermal expansion cracks
Sheetingfractures
Hydrolytic failures
Columnar joints
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water expands as it melts,causing the crack walls to bepushedapart
Water shrinks asit freezes,causing thecrack walls to bedrawn closer together
water expands asit freezes,causing the crack walls to bepushedapart
Water shrinks asit melts,causingthecrackwallsto bep.,it.a closertogether
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disintegration and decomposition of rocks and minerals at the surface
Movement of weathered rock and regolith toward the base of a slope'
The process by which weathered rock and mineral paricles are removed from one area and transported
The combined processes of leaching, eluviation,and mass wasting
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