---
title: "Geomorphological Processes | World Geography"
description: "Geomorphological processes are the natural forces that shape landforms through uplift, weathering, erosion, and deposition in World Geography."
canonical: "https://fiveable.me/world-geography/key-terms/geomorphological-processes"
type: "key-term"
subject: "World Geography"
unit: "Unit 4"
---

# Geomorphological Processes | World Geography

## Definition

Geomorphological processes are the natural processes that shape Earth's landforms, including tectonic uplift, weathering, erosion, and deposition. In World Geography, they explain why mountains, valleys, plains, and coasts look the way they do.

## What It Is

Geomorphological processes are the physical processes that build, wear down, and reshape landforms in World Geography. They include forces coming from inside the Earth, like tectonic uplift and folding, and forces acting at the surface, like weathering, erosion, and sedimentation.

A simple way to think about them is that the Earth is always being built up and worn down at the same time. Internal forces raise land or deform it into mountains and plateaus. External forces break rock apart, move the broken material, and drop it somewhere else. That is why a mountain range can exist for millions of years and still slowly shrink, round off, and feed sediment into nearby rivers and basins.

This term shows up a lot in landform questions because geography is not just about where features are located, it is about how they formed. The Appalachian Mountains are a good example. They formed through ancient tectonic collision, but long periods of weathering and erosion have lowered and smoothed them. That is the geomorphological story behind their shape today.

Exogenic processes are especially visible at the surface. Rivers carve valleys, glaciers scrape bedrock and leave moraines, wind moves fine sediment in dry regions, and waves reshape coastlines. In areas like the Great Lakes region, glaciers left behind basins and deposits that still affect drainage, soils, and settlement patterns. In places with active tectonics, like near the San Andreas Fault, land can change faster because faults can trigger uplift, earthquakes, landslides, and sudden changes in the landscape.

Human activity can speed these processes up or change their direction. Clearing land for farming, building roads on steep slopes, or expanding cities can increase erosion and sedimentation. Climate change matters too, because shifts in rainfall, temperature, and ice cover can change how fast rock breaks down, how much sediment rivers carry, and how stable slopes remain.

## Why It Matters

Geomorphological processes are the reason World Geography connects physical landforms to human life instead of treating them like a static map. Once you know how landforms are made, you can explain why some places have rich soils, why others are prone to landslides or flooding, and why transportation routes often follow valleys, passes, or river corridors.

This term also gives you the vocabulary for reading physical maps and landform diagrams. If you see a steep mountain front, a broad delta, or a glacial valley, you are not just naming a feature, you are identifying the process that created it. That is the move geography asks you to make: connect shape to formation.

It also links directly to natural resources and settlement. Areas shaped by erosion and deposition can have fertile floodplains, while uplifted regions may expose mineral resources or create barriers to movement. In class discussion or written responses, geomorphological processes let you explain why people farm, build, mine, or avoid certain landscapes.

## Connections

### Erosion

Erosion is one of the main surface processes inside geomorphological change. It moves weathered material away by water, wind, ice, or gravity, which is why it can carve valleys, steepen slopes, and reshape coastlines. When you describe a canyon, a river bank, or a worn-down mountain range, erosion is usually part of the explanation.

### Weathering

Weathering breaks rock down before erosion carries it away. That makes it the starting point for many landform changes, especially in places with freeze-thaw cycles, chemical breakdown, or plant roots prying apart rock. In World Geography, weathering helps explain how bedrock becomes sediment that can later be moved and deposited elsewhere.

### Sedimentation

Sedimentation is the laying down of material after it has been transported. It is the other side of erosion, because landforms like deltas, floodplains, sandbars, and many coastal features are built by deposited sediment. If a question asks how a flat, layered landform formed, sedimentation is often the process to identify.

### [fluvial processes](/world-geography/key-terms/fluvial-processes)

Fluvial processes are river-related geomorphological processes, so they are one major branch of the larger term. Rivers erode their channels, transport sediment, and deposit material along bends, floodplains, and deltas. When a geography question focuses on valleys, meanders, or river deltas, fluvial processes give the specific mechanism behind the broader landform change.

## On the AP Exam

A map question or landform ID item often asks you to match a landscape to the process that created it. You might see a mountain chain and explain uplift and folding, or see a river delta and connect it to sediment deposition. For visual prompts, look for clues like rounded peaks, U-shaped valleys, layered deposits, or steep fault lines.

Short response questions often want cause and effect: what process shaped the landform, and how does that shape affect people? You could explain that erosion carved a valley that later became a travel route, or that tectonic uplift made a mountain barrier that influences climate and settlement. In a case study, you can trace how farming, logging, or urban growth changes erosion and sedimentation rates.

If you are given a diagram, the move is to name the process, describe the direction of material movement, and tie it to the landform you see.

## geomorphological processes vs Weathering

Weathering and geomorphological processes are related, but they are not the same level of idea. Weathering is one process that breaks rock down in place, while geomorphological processes is the bigger umbrella that includes weathering plus erosion, deposition, uplift, and other land-shaping forces.

## Key Takeaways

- Geomorphological processes are the natural forces that create and change landforms in World Geography.
- They include both internal forces, like tectonic uplift, and surface forces, like weathering, erosion, and sedimentation.
- A landform tells a process story, so shape, slope, and sediment all give clues about how the landscape formed.
- Glaciers, rivers, wind, waves, and moving plates can all reshape the Earth, sometimes very slowly and sometimes quickly.
- Human activity and climate change can speed up erosion, change sediment movement, and make landforms less stable.

## FAQs

### What is geomorphological processes in World Geography?

Geomorphological processes are the physical processes that shape Earth's surface into landforms like mountains, valleys, plains, and deltas. In World Geography, the term covers both forces from inside the Earth, such as tectonic uplift, and surface processes like erosion and deposition.

### What are the main types of geomorphological processes?

The main types are endogenic and exogenic processes. Endogenic processes come from inside the Earth and include tectonic movement, folding, and uplift. Exogenic processes happen at the surface and include weathering, erosion, transport, and sedimentation.

### How are geomorphological processes different from weathering?

Weathering is just one part of geomorphological change. It breaks rock down in place, while geomorphological processes include the whole chain of landform change, from breaking rock down to moving it and depositing it somewhere else.

### Can humans affect geomorphological processes?

Yes. Farming, construction, logging, and road building can increase erosion and sediment runoff. In World Geography, this matters because human land use can speed up slope failure, fill rivers with sediment, and change how stable a landscape is over time.

## Related Study Guides

- [4.1 Landforms and Geological Features](/world-geography/unit-4/landforms-geological-features/study-guide/GR8CUTMNWX6jnUO7)

## About This Document

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