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The dynamic Earth · The history of the Earth

Landforms and Landscape

A mountain range that rises and the canyon that cuts through it seem like opposite processes: one builds, the other excavates. Think of Popocatépetl or the Sierra Madre and the ravines that slice through them. In reality they are two sides of the same phenomenon: every landform results from a permanent tug-of-war between forces that lift and forces that wear away.

Relief: A Balance Between Internal and External Processes

When we look at a mountain range, we see rugged peaks next to deep ravines and slopes covered in fallen blocks. What forces lift millions of tons of rock while the atmosphere and water relentlessly try to break it down?

Cross section of a mountain range. The collision of plates folds and lifts the rocks, which are internal processes. Rain, weathering, erosion, transport, and deposition wear down and shape the relief, which are external processes. folds plate collision uplift rain weathering erosion transport deposition Internal processes: lift External processes: wear down

External processes follow an order. First, weathering breaks down or alters the rock in place. Then erosion loosens and wears away the material. Next, transport moves it (water, ice, wind, gravity), and finally deposition leaves it where the agent loses strength.

The external geological agents are water (rivers, rain, sea), ice (glaciers), wind, and gravity, as well as living things and, today, humans. Examples of landforms: canyons and deltas (water), U-shaped valleys and moraines (ice), dunes (wind), landslides (gravity).

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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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Lithology Conditions the Shaping of Relief

Comparison of two cross sections of the terrain: in limestone, water seeps through the fractures and forms a sinkhole, a shaft, and a cave with stalactites and stalagmites; in granite, the joints isolate rounded blocks that remain on the surface. Limestone · karst relief Granite · blocks water sinkhole shaft cave blocks joints

Why? Rainwater carries dissolved $\mathrm{CO_2}$ and is slightly acidic: it reacts with the calcium carbonate in limestone and carries it away in solution. Granite barely dissolves and wears down mainly by mechanical means.

In Mexico you can see this clearly on the Yucatán Peninsula: its ground is limestone, and that is why there are almost no surface rivers, but instead caves, flooded sinkholes (the cenotes), and underground rivers.

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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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Shaping Agents: River and Glacial Landforms

Two agents can shape the same mountain and leave very different valleys: some narrow and deeply cut, like the ravines of the Sierra Madre, and others wide with a flat floor. Why?

Compared cross-section profiles: at the top, a narrow V-shaped river valley with steep walls and the river cut into the bottom by vertical erosion; at the bottom, a wide U-shaped glacial valley with a flat floor, showing the former glacier, lateral and bottom erosion, lateral moraines, and an erratic boulder. River valley (V-shaped profile) vertical erosion steep walls river channel Glacial valley (U-shaped profile) former glacier lateral and bottom erosion lateral moraine lateral moraine wide, flat floor erratic boulder

In Mexico, small glaciers remain on Iztaccíhuatl, Popocatépetl, and Pico de Orizaba; in past cold periods they were larger and left U-shaped valleys and moraines on those mountains.

Now test what you know with two unlabeled profiles. Pay attention to the width, the floor, and the walls of each valley marked with "?".

Two unlabeled valley profiles, each marked with a question mark: the one on the left is wide with a flat floor; the one on the right is narrow with a pointed bottom. ? ? Valley 1 Valley 2
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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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The Value of Relief: Scientific, Scenic, and Economic

Relief is not only something to look at: it is also put to use. Agricultural terraces, mines, and tourism at cenotes or volcanoes depend on the shape of the terrain and the rocks that make it up.

Profile landscape with a mountain of layered rocks on whose flank a terraced quarry is excavated with a truck, a valley with fertile soil, crops, and a river, and on the right a landform with a unique rock formation and a lookout with an information sign for geotourism. i quarry rocks and minerals fertile valley fertile soils geotourism landscape and heritage strata: record of geological history

Each use brings a risk. Farming on slopes promotes soil erosion; quarries and mines leave holes and unstable slopes; mass tourism at cenotes or caves pollutes the water and damages the formations.

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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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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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Humans as a Geological Agent and Sustainable Management

Today people move more sediment than all the rivers combined: we open pit mines, flatten hills, drain lakes. Mexico City is built on the former Lake Texcoco, which was drained, and that is why it is sinking from groundwater extraction. How can we analyze that intervention using the ideas in this section?

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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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Imagine a geological and topographical cross-section running across the Iberian Peninsula from north to south: the Cantabrian Mountains, the Douro Basin, the Central…

Imagine a geological and topographical cross-section running across the Iberian Peninsula from north to south: the Cantabrian Mountains, the Douro Basin, the Central System, the Tagus Basin, and the Betic Cordillera.

  1. a) During the Alpine orogeny, why did the ancient Hercynian basement of the central peninsula respond by fracturing into uplifted blocks (horsts) and down-dropped blocks (grabens), whereas on the edges (Cantabrian and Betic ranges) large folded mountain chains formed? Justify your answer based on the mechanical behavior of the materials in each area.
  2. b) Predict the origin and geometric arrangement (horizontal or folded) of the materials that fill the Douro and Tagus basins, deducing which mountain ranges they come from and what geological process caused their accumulation.
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Summary

See all the exercises in this section