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Weathering
weathering information for BSC
| Question | Answer |
|---|---|
| frost wedging | process where freezing and thawing eventually breaks water apart. |
| salt crystal growth | salt crystals grow in rocky shore lines and arid regions, as the water evaporate the salt crystals form, pushing apart the surrounding rock |
| talus slopes | large piles at bases of steep rocky cliffs |
| exfoliation domes | large, dome-shaped structure, usually composed of granite, formed by sheeting |
| abrasion | not in the chapter |
| oxidation | Fe2+ + H202 + 2H+ = 2Fe3+ +2H20 examples: rust |
| dissolution | co2 + H20 = H2CO3 dissolve in water |
| Hydrolysis | Mg2SiO4 +4H+ + 4OH- = 2Mg2+ +4OH- + H4SiO4 |
| hydration | Mg2+(g) + H20 = Mg2+(aq) |
| name two characteristics that effect the rate of weathering | 1. rock characteristics- mineral composition, solubility, and physical features 2. climate- mechanical weathering frost freeze cycle, chemical weathering warm temperatures and abundant moisture |
| regolith | layer of rock and mineral fragments produced by weathering |
| soil | combination of mineral and organic matter, water and air four components always are present to some extent 1/4 disintegrated and decomposed rock 1/4 humus decay remains animal and plant 1/2 pore space air and water circulate |
| loam | no single particle predominates best suited for supporting plant life because best moisture and nutrient storage |
| horizons | vertical zones in soil |
| O-horizon | largely organic material upper part plant litter, lower part humus, microscopic life. |
| A- horizon | mineral matter mixed with some humus |
| top soil | O and A make up top soil |
| E - horizon | light-colored, layer little organic finer particles carried away by water |