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Geology · Year 13

Active learning ideas

Water Resources and Hydrogeology

Hydrogeology is the study of how water moves through the Earth's crust, a topic of increasing importance as global water demand rises. Students learn to distinguish between aquifers and aquitards, and how geological properties like porosity and permeability control the yield of a well. The curriculum covers the dynamics of the water table, the formation of cones of depression, and the risks of saline intrusion in coastal areas. This topic links directly to environmental management and the UK's own water security challenges.

National Curriculum Attainment TargetsA-Level Geology (Eduqas) 5.3: Water supplyA-Level Geology (OCR) 7.1.3: Hydrogeology
25–50 minPairs → Whole Class3 activities

Activity 01

Inquiry Circle45 min · Small Groups

Inquiry Circle: The Aquifer Model

Using clear containers filled with different materials (gravel, sand, clay), groups 'drill' wells (straws) and measure how fast they can pump water out. They observe how the 'water table' drops and how quickly it recovers in each material.

What geological properties determine the yield of an aquifer?
AnalyzeEvaluateCreateSelf-ManagementSelf-Awareness
Generate Complete Lesson

Activity 02

Simulation Game50 min · Small Groups

Simulation Game: Contamination Plume Tracking

Students are given a map of a town with a leaking underground storage tank. Using data from several 'monitoring wells', they must map the spread of the pollution plume and predict which residential wells are at risk of being contaminated.

How does a cone of depression form around a pumping well?
ApplyAnalyzeEvaluateCreateSocial AwarenessDecision-Making
Generate Complete Lesson

Activity 03

Think-Pair-Share25 min · Pairs

Think-Pair-Share: Managing Water Scarcity

Students read about a region facing over-abstraction (e.g., the Chalk aquifer in SE England). They brainstorm three ways to reduce demand or increase recharge, then pair up to select the most geologically sound solution to present to the class.

What are the primary sources of groundwater contamination?
UnderstandApplyAnalyzeSelf-AwarenessRelationship Skills
Generate Complete Lesson

A few notes on teaching this unit


Watch Out for These Misconceptions

  • Groundwater flows in underground rivers.

    Except in limestone caves, groundwater moves very slowly through the tiny pores and fractures in solid rock. Using 'permeability races' with different sediments helps students visualize the slow, steady movement of water through an aquifer.

  • An aquifer is an endless supply of water.

    Aquifers can be 'mined' if water is taken out faster than it is recharged by rain. Peer discussion about 'sustainable yield' helps students understand that groundwater is a finite resource that needs careful management.


Methods used in this brief