ERTH2404 Lecture Notes Review

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A set of vocabulary flashcards based on key concepts from the ERTH2404 lecture notes on permafrost, groundwater, and earth resources.

Last updated 1:53 AM on 4/21/26
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20 Terms

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Permafrost

Ground (soil or rock) that remains at a temperature of 0°C or lower for at least two consecutive years.

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Active layer

The near-surface layer of permafrost that thaws in summer and freezes in winter, usually 0.5 m to 2 m thick.

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Suprapermafrost

The layer above the permafrost that includes the active layer and taliks.

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Gelifluction

Mass movement linked to the thawing of the active layer, where saturated soil flows down slopes.

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Solifluction

The slow flow of water-saturated soil down a slope due to thawing permafrost.

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Thermokarst

Geological processes resulting from the thawing of permafrost containing ground ice, causing subsidence and landslides.

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Hydrologic cycle

The continuous movement of water on, above, and below the surface of the Earth, operating for over 4 billion years.

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Unsaturated zone

The zone near the Earth's surface where the soil pores contain both air and water; also called the vadose zone.

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Saturated zone

The zone in which all spaces in a rock or soil are filled with water.

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Recharge

The process of water seeping into an aquifer or saturated zone from the surface.

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Aquitard

A geological formation that restricts the flow of groundwater from one aquifer to another.

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Darcy’s Law

An equation describing the flow of groundwater through porous media, stating that flow velocity is proportional to the hydraulic gradient.

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Hydraulic conductivity

A measure of how easily water can flow through a porous material or rock.

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Permeability

The ability of a material to transmit fluids, affected by the size and connectivity of pores.

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Aquifer

A geologic formation that can yield significant amounts of groundwater.

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Groundwater discharge

The flow of groundwater to the surface, contributing to streamflow and lakes.

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Cone of depression

An area around a well where the water table has been lowered due to excessive water extraction.

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Saltwater intrusion

The movement of saline water into freshwater aquifers, often due to over-extraction of groundwater.

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Fossil fuels

Natural fuels formed from the remains of living organisms, primarily including coal, oil, and natural gas.

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Bitumen

A thick, viscous form of petroleum that is found in oil sands and requires special methods for extraction.