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Chapter 4 - Weathering & Soil Formation

AB
weatheringThe chemical and physical processes that break down rock at Earth’s surface.
erosionThe process by which water, ice, wind, or gravity moves fragments of rock and soil.
mechanical weatheringThe type of weathering in which rock is physically broken into smaller pieces.
abrasionThe grinding away of rock by other rock particles carried in water, ice, or wind.
Mechanical weathering breaks rock into pieces byfreezing and thawing, release of pressure, growth of plants, actions of animals, and abrasion.
ice wedgingProcess that splits rock when water seeps into cracks, then freezes and expands.
chemical weatheringThe process that breaks down rock through chemical changes.
The agents of chemical weathering includewater, oxygen, carbon dioxide, living organisms, and acid rain.
The most important factors that determine the rate at which weathering occurs aretype of rock and climate.
permeableCharacteristic of materials such as sand and gravel that allow water to pass easily through them.
soilThe loose, weathered material on Earth’s surface in which plants can grow.
bedrockThe solid layer of rock beneath the soil.
Soil is a mixture ofrock particles, minerals, decayed organic material, air, and water.
humusDark-colored organic material in soil
loamRich, fertile soil that is made up of about equal parts of clay, sand, and silt.
soil horizonA layer of soil that differs in color and texture from the layers above or below it.
top soilMixture of humus, clay, and other minerals that forms the crumbly, topmost layer of soil
subsoilThe layer of soil beneath the topsoil that contains mostly clay and other minerals.
litterThe loose layer of dead plant leaves and stems on the surface of the soil.
Fertile soil isrich in nutrients that plants need, such as nitrogen and phosphorus.
decomposerAn organism that breaks down wastes and dead organisms.
Three uses that change the land areagriculture, development, and mining.
developmentThe construction of buildings, roads, dams, and other structures.
Soil is one of Earth’s most valuable resourcesbecause everything that lives on land depends directly or indirectly on soil.
desertificationThe advance of desertlike conditions into areas that previously were fertile.
sodA thick mass of grass roots and soil.
Dust BowlThe area of the Great Plains where wind erosion caused soil loss during the 1930s.
soil conservationThe management of soil to prevent its destruction.
Ways that soil can be conserved includecontour plowing, conservation plowing, leaving the soil to lie fallow, and crop rotation
contour plowingPlowing fields along the curves of a slope to prevent soil loss.
conservation plowingSoil conservation method in which the dead stalks are left in the ground to hold the soil in place.
fallowLeft unplanted with crops.
crop rotationThe planting of different crops in a field each year.
land reclamationThe process of restoring land to a more natural state.
municipal solid wasteWaste produced in homes, businesses, and schools.
Three methods of handling solid waste areto bury it, to burn it, or to recycle it.
leachateWater that has passed through buried wastes in a landfill.
sanitary landfillA landfill that holds nonhazardous waste such as municipal solid waste and construction debris.
incinerationThe burning of solid waste.
recyclingThe process of reclaiming and reusing raw materials.
Most recycling involves four major categories of products:metal, glass, paper, and plastic.
to help control the solid waste problem. These actions are sometimes called the “three R’s”reduce, reuse, and recycle.
hazardous wasteA material that can be harmful if it is not properly disposed of.
There are four categories of hazardous waste:toxic, explosive, flammable, and corrosive.
Long-term exposure to hazardous wastes may causediseases such as cancer, and may damage body organs, including the brain, liver, kidneys, and lungs.


Life Science & Physical Science Teacher
Elko Middle School
Sandston, VA

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