Weathering - when rocks are exposed to air, water, certain chemicals, or biological agents that degrade the rock  Physical weathering - the mechanical.

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Presentation transcript:

Weathering - when rocks are exposed to air, water, certain chemicals, or biological agents that degrade the rock  Physical weathering - the mechanical breakdown of rocks and minerals Chemical weathering - the breakdown of rocks and minerals by chemical reactions Weathering and Erosion

Erosion - the physical removal of rock fragments from a landscape or ecosystem –Wind, water, ice, and living organisms can erode materials Deposition - the accumulation or depositing of eroded material such as sediment, rock fragments, or soil Erosion & Deposition

Soil is important because it: Is a medium for plant growth Serves as a filter for water A habitat for living organisms Serves as a filter for pollutants Soil

Factors that determine the formation of soil: Parent material - what the soil is made from influences soil formation Climate - what type of climate influences soil formation Topography - the surface and slope can influence soil formation Organisms - plants and animals can have an effect on soil formation Time - the amount of time a soil has spent developing can determine soil properties The Formation of Soil

O horizon - (organic layer) composed of leaves, needles, twigs, and animal remains on the surface A horizon - (topsoil) the zone of organic material and minerals mixed together Soil Horizons

B horizon - (subsoil) composed primarily of mineral material with very little organic matter C horizon - (parent material) the least weathered horizon and is similar to the parent material Soil Horizons

Texture - the percentage of sand, silt, and clay the soil contains Physical Properties of Soil

Porosity - how quickly the soil drains (which depends on its texture) Physical Properties of Soil

Chemical Properties of Soil Cation exchange capacity - the ability of a soil to adsorb and release cations (positively charged mineral ions) Soil bases - calcium, magnesium, potassium, and sodium Soil acids - aluminum and hydrogen Base saturation - the proportion of soil bases to soil acids

Many organisms are found in the soil including fungi, bacteria, protozoans, rodents, and earthworms Biological Properties of Soil

Elemental Composition of the Earth’s Crust 12

Ore – concentrated accumulations of minerals that can be economically extracted Rare earths – materially important elements that are not typically found concentrated in economically exploitable ores Mineral Resources

Reserves - the known quantity of a resource that can be economically recovered Reserves

Surface mining - removing minerals that are close to Earth’s surface Strip mining - removing strips of soil and rock to expose ore Open pit mining - the creation of a large pit or hole in the ground that is visible from the surface Mountain top removal - removing the entire top of a mountain with explosives Placer mining - looking for metals and stones in river sediments Types of Mining

Subsurface mining - mining for resources that are 100 m below Earth’s surface Types of Mining

Shaft mining – done by use of a mine shaft (a vertical passageway used to access an underground mine) Subsurface Mining

Slope mining – a sloping access shaft travels downwards towards the deposit Slope mines differ from shaft and drift mines, which access resources by tunneling straight down or horizontally Subsurface Mining

Drift mining – accessing deposits by cutting into the side of the earth, rather than tunneling straight downwards Subsurface Mining

Auger mining – a low-cost method of recovering coal from horizontal seams by drilling into the side of a wall Subsurface Mining

Reclamation Before After