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Published byJean Anthony Modified over 9 years ago
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Weathering- the breakdown of rock into smaller and smaller pieces. Mechanical weathering- is simply the breakdown of rock into smaller pieces by physical means. Chemical weathering- the chemical breakdown of rocks and minerals into new substances.
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There are three different layers of soil. Topsoil- contains more humus than any soil horizon. Subsoil- Where clays and dissolved substances from the topsoil collect. Bedrock- consists of partially weathered bedrock.
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Different types of rock weather at different rates. Differential weathering is the process by which softer, less weather-resistant rocks wear away, leaving harder, more weather-resistant rocks behind. Rates of Weathering
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Soil conservation consist of the various methods by which humans take care of the soil. Soil provides minerals and other nutrients for plants.
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Erosion is the process by which wind and water transport soil and sediment from one location to another.
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Tropical Climates- the air is very humid and the land receives a large amount of rain. Desert Climates- doesn’t receive much of any water. Temperate Climates- rich soil, which allows a good place to farm. Arctic Climates- little precipitation Climates
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Soil provides a place for animals to live. The Importance of Soil Earthworms, grubs, spiders, moles, and prairie dogs all live in soil.
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A cover crop is a crop that is planted between harvests to reduce soil erosion. A Crop rotation is a common way to keep soils nutrient-rich.
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Over all, chapter ten defines all the different types of weathering. It describes the layers of soil. Talks about the importance of soil, and describes erosion. And it describes different types of climates.
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