Weathering and Soil Flashcards
(32 cards)
Weathering
The process by which larger rocks get broken down into smaller pieces
The means by which rocks can be weathered
physical means, chemical means, or both
Erosion
The removal of weathered products
Soil
A mixture of mineral and organic matter
Soil horizons
The distribution of soil layers
What are the Soil horizons
O Horizon
A Horizon
B Horizon
C Horizon
R Horizon
O Horizon
The organic zone containing dead and decaying plant and animal remains; it’s normally dark in colour because of the large amount of humus
Humus
Organic material (in the O Horizon)
A Horizon
The surface layer of soil
Contains a mixture of organic material and mineral matter and is darker than the O Horizon
The most productive and nutrient-rich portion of the soil horizon
The A horizon
E horizon
A zone of leaching below the A horizon (only in some soils) where nutrients move out of it down toward the bedrock leaving behind iron; it’s generally lighter in colour
B horizon
The “subsoil” or “zone of accumulation,” which consists of a variety of substances (organics, clay, small rocks)
C horizon
The substratum
The parent material. Its composition is highly dependent on the type of bedrock below and usually contains fragments of the bedrock
Loam
a soil that contains approximately equal amounts of clay, silt, and sand
The desirable consistency of the A horizon
Loam
The R horizon
Bedrock
The rock unit underlying the soil
chemical weathering
when a rock disintegrates due to chemical reactions that happen within the environment
The main process at work in caves
carbonic acid dissolving calcite in limestone
The result of rocks rusting if iron is present
iron oxides like hematite or limonite
mechanical weathering
the breakdown of rocks by physical or mechanical processes
frost wedging
water gets into cracks in rocks, freezes, and expands, making the cracks in the rocks even bigger
root wedging
roots from plants force open small fractures in rocks, which opens the door for other weathering processes
pressure release/unloading
a type of mechanical weathering in which a rock
fractures because of expansion due to a heavy overlying pressure being removed.
isostatic rebound
occurs when something heavy like glacial ice or large amounts of rock are removed from an area, the landscape underneath will respond by expanding upward (in pressure release mechanical weathering)