Weathering, Erosion, and River Systems

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This set of vocabulary flashcards covers the processes of physical, chemical, and biological weathering, the distinctions between erosion and deposition, and the characteristics of river courses.

Last updated 8:41 PM on 8/19/26
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24 Terms

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Weathering

The slow breakdown of rocks, soil, and minerals into smaller pieces in situ, meaning there is no movement of the weathered material.

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Physical weathering

A process where rocks break into smaller pieces without changing their chemical composition.

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Granular disintegration

A type of physical weathering where rocks break into small grains or pieces, such as sand or gravel, often caused by expansion and contraction.

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Exfoliation

A weathering process where rocks are peeled off in layers due to repeated heating and cooling causing outer layers to expand and break away.

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Block separation

Physical weathering where rocks break into large blocks along cracks or joints, often expanded by temperature changes or water.

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Chemical weathering

The breakdown of rocks into particles with a different chemical composition from the original rock, involving agents like water, oxygen, and CO2CO_2.

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Solution

A type of chemical weathering where minerals, such as salt, dissolve in water.

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Hydration

A chemical weathering process where minerals absorb water and expand, which can contribute to the physical breaking of the rock.

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Hydrolysis

A chemical reaction between minerals and hydrogen ions in rainwater that can change rock-forming minerals into clay minerals.

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Oxidation

A chemical process where rock minerals react with dissolved oxygen to form red/yellow oxides, similar to rusting; common in tropical areas.

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Carbonation

A process where CO2CO_2 dissolves in water to form a weak carbonic acid that weathers rocks like limestone and chalk.

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Biological weathering

The breakdown of rocks caused by living organisms, such as plant roots growing into cracks or animals digging.

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Mining

A human activity that speeds up weathering by digging up and breaking large rocks, exposing more surfaces to the elements.

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Burning fossil fuels

A human impact that releases chemicals into the atmosphere, contributing to acid rain which weathers limestone and buildings.

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Building roads

A human activity where rocks are blasted with explosives and broken into smaller pieces, facilitating faster weathering.

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Erosion

The process by which soil and rock are removed from the Earth's surface and transported to another location by agents like water, wind, or glaciers.

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Deposition

The process where eroded material is dropped or deposited in a new location once the movement stops.

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Gravity

The underlying force behind many types of erosion that causes materials, rocks, and rivers to move downhill from higher elevations.

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Upper Course

The beginning of a river (upstream) characterized by steep slopes, fast-moving water, vertical erosion, and VV-shaped valleys.

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Rapids

Fast-flowing parts of a river caused by steep slopes, typically found in the upper course.

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Middle Course

The stage of a river with more gradual slopes, wider valleys, lateral erosion, meanders, and UU-shaped valleys.

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Meanders

Bends or curves in a river that typically develop during the middle and lower courses.

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Lower Course

The stage close to the mouth (downstream) where water flows slowly, meanders are frequent, and deposition is the dominant process.

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Oxbow Lake

A UU-shaped lake formed in the lower course when a river bend is cut off from the main river channel.