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ESO Y4A · Biology and Geology
The dynamic Earth · The history of the Earth

Relief and landscape

A mountain range and the canyon that cuts through it seem like opposites: one pushes up, the other digs out. In reality they are two sides of the same coin: relief always arises from the tug-of-war between forces that build and forces that wear away.

Before you start, make sure you know: The shaping of relief (3rd ESO)
Before you start, make sure you know: The uses of rocks and minerals (1st ESO)

Relief is born from two types of forces

The steep profiles of the Picos de Europa contrast with the gentle, worn-down hills of the Montes de Toledo: why do some parts of the Earth keep their jagged peaks while others gradually flatten out over time?

Cross-section of a mountain range. Internal processes (plate collision) raise it from below, and external processes (weathering, rain, wind, erosion, transport and deposition) wear it down and shape it from the surface. plate collision uplift Internal processes (tectonics): raise relief External processes: wear down and shape weathering wind rain erosion and transport deposition
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Name four external geological agents that shape the relief and give an example of a landform created by each one.

Name four external geological agents that shape the relief and give an example of a landform created by each one.

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Explain the difference between erosion, transport and deposition, and order them as they occur in landform shaping.

Explain the difference between erosion, transport and deposition, and order them as they occur in landform shaping.

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Relief has scientific and scenic value

Two views of relief: on the left, a cross-section with folded strata and a fossil that record geological history; on the right, a canyon landscape with a hiker, representing scenic value and geotourism. Scientific value record of geological history Scenic value heritage and geotourism folded strata fossil canyon
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State whether these landforms were mainly shaped by water, ice or wind: a U-shaped valley, a dune, a river canyon and a moraine.

State whether these landforms were mainly shaped by water, ice or wind: a U-shaped valley, a dune, a river canyon and a moraine.

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Two regions with the same climate have very different landscapes because one consists of limestone rock and the other of granite. Explain how lithology (rock type)…

Two regions with the same climate have very different landscapes because one consists of limestone rock and the other of granite. Explain how lithology (rock type) influences landform development and what characteristic relief limestone typically creates.

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Relief as an economic resource

The concrete and bricks of our homes, the sand used to make glass, the water from wells and the crops of the river plains all come from geological shaping: in what ways do we make use of the structures of the terrain in our daily lives?

Cross-section of a landscape showing the resources of relief: a stepped quarry on a mountain slope, a fertile valley with crops and a river, an aquifer beneath the valley from which water is drawn by a well, and a tourist viewpoint at the top of a hill. aquifer quarry rocks and minerals fertile valley soil and crops well tourism scenery
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Relief is also a resource. Describe two economic uses of relief (for example, tourism or agriculture) and a risk associated with each.

Relief is also a resource. Describe two economic uses of relief (for example, tourism or agriculture) and a risk associated with each.

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Look at the cross-sectional profiles of the two valleys in the diagram, marked with ?. Identify which is a river valley and which is a glacial valley, explain which…

Look at the cross-sectional profiles of the two valleys in the diagram, marked with ?. Identify which is a river valley and which is a glacial valley, explain which agent shaped each one, and what differences in shape allow them to be distinguished.

Valley A ? Valley B ?
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Managing relief sustainably

An abandoned quarry leaves scars on the hillside that can cause deadly rockfalls or contaminate nearby aquifers: how can we extract the raw materials we need without ruining the environment or endangering neighbouring communities?

Cross-section of a limestone slope at two moments: above, an active quarry with bare rock benches, risk of rockfalls, an extraction pit and rubble; below, the same place restored with the slope stabilised and replanted, the rubble removed and a lake in the former pit, without recovering the original profile of the mountain. 1. Active quarry Risk of rockfalls Original profile Bare rock benches Extraction pit Rubble Limestone Environmental restoration 2. Restored area Original profile (not recovered) Stabilised slope with replanted vegetation Lake Rubble removed
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A municipality with an old mining basin in economic decline has a unique karst landscape with prehistoric caves, tectonic folds of great educational value, and several…

A municipality with an old mining basin in economic decline has a unique karst landscape with prehistoric caves, tectonic folds of great educational value, and several threatened botanical species. The city council is debating between two protection designations:

  • Option A: Declare the area a National Park with strictly restricted access for scientific research.

  • Option B: Apply for its declaration as a UNESCO Global Geopark.

  1. a) Justify why the Geopark model is better suited to this case than the National Park model if the goal is to reconcile the protection of geological heritage with the socioeconomic development of the local population.
  2. b) Design two specific geotourism management measures that the geopark should implement so that public visits do not alter or degrade the karst cavities.
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In Las Médulas (León), Roman mining transformed the landscape through the technique of ruina montium* (violent injection of pressurised water into galleries to collapse…

In Las Médulas (León), Roman mining transformed the landscape through the technique of ruina montium (violent injection of pressurised water into galleries to collapse hillsides), generating alluvial fans of boulders, mudflats, and the natural dam of Lake Carucedo. Today it is a protected landscape designated as a UNESCO World Heritage site.

  1. a) Analyse human intervention as an external geological agent in Las Médulas, identifying the stages of erosion, transport, and sedimentation artificially caused by the mining technique.
  2. b) A current mining company requests permission to open-pit mine a nearby pristine valley, arguing that "human activity creates landscapes that in the future will also be considered historical heritage like Las Médulas". Technically refute this argument by comparing the rate of landscape alteration, the toxicity of modern techniques, and the possibility of ecological regeneration.
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Summary

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