What you'll learn

• How to describe distribution — where features are found — for higher, steeper uplands and lower, gentler lowlands across the United Kingdom (UK).
• How past ice created glaciated landscapes — landscapes shaped by glaciers and ice sheets.
• How geology — rock type and structure — and climate — long-term weather patterns — help explain landscape differences.
• How human activity — the ways people use land — varies between upland, lowland and glaciated areas.

1. The starting point: what is a landscape?

A physical landscape is the visible shape and character of the land, including hills, valleys, rivers, rocks, soils and landforms. In GCSE Geography, you also consider how people use that land, because farming, settlement, tourism and transport often respond to the physical setting.

A useful way to think about this topic is: rocks help make the shape of the land, climate affects water and vegetation, and people use the land in ways that fit the opportunities and limits of that landscape.

2. The big UK pattern: north and west versus south and east

At a national scale, the UK has a clear pattern. The main upland and formerly glaciated landscapes are mostly in the north and west, while the main lowland landscapes are mostly in the south and east. The map below shows this simplified overview.

This pattern is not random. It reflects the UK’s geological history, its position next to the Atlantic Ocean, and the effects of the last ice age.

Worked example: describing a national distribution

3. Upland landscapes

Upland landscapes are areas of higher altitude, often with steep slopes, thin soils and exposed conditions. There is no single height that makes somewhere an upland; the key idea is that uplands are higher and more rugged than the surrounding lowlands.

Important UK upland areas include the Scottish Highlands, Grampian Mountains, Southern Uplands, Lake District, Pennines, Snowdonia/Eryri, Cambrian Mountains, Dartmoor and Exmoor.

Geology of uplands

Many UK uplands are made of older, harder rocks, including igneous rocks and metamorphic rocks. Igneous rocks form when molten rock cools and solidifies. Metamorphic rocks are rocks changed by heat and pressure. These rocks are often more resistant to erosion, so they can form high, rugged relief.

Some uplands also include hard sedimentary rocks, such as limestone or sandstone. Sedimentary rocks form from layers of material such as sand, mud, shells or organic matter that become compacted over time.

Climate of uplands

Uplands are generally cooler, wetter and windier than lowlands. Temperature falls with altitude, so higher places tend to be colder. Uplands in the west are especially wet because moist air arrives from the Atlantic Ocean.

The UK’s prevailing wind — the most common wind direction — is from the south-west. When this moist air is forced to rise over mountains, it cools, condenses and produces rain. This is called relief rainfall.

Human activity in uplands

Upland landscapes often have low population density, meaning fewer people live there per square kilometre. Farming is usually limited by steep slopes, thin soils and wetter conditions, so pastoral farming — farming animals rather than crops — is common. Sheep farming is especially important in upland Wales, northern England and Scotland.

Other common activities include:

• Tourism and recreation, such as walking, climbing and mountain biking in National Parks like the Lake District and Snowdonia/Eryri.
• Forestry, where conifer plantations are grown in wetter upland areas.
• Reservoirs, because uplands receive high rainfall and have valleys suitable for storing water.
• Quarrying, where valuable rock is extracted.
• Wind energy, because exposed uplands can be windy.

4. Lowland landscapes

Lowland landscapes are areas of lower altitude with gentler relief. They often have deeper soils, broader valleys and more accessible land, so they are usually more suitable for settlement, transport and intensive farming.

Major UK lowland areas include East Anglia, the London Basin, the Vale of York, the Cheshire Plain, the Severn Vale and the Central Lowlands of Scotland.

Geology of lowlands

Lowlands are often made from younger, softer sedimentary rocks such as clay, chalk, sandstone and limestone. Softer rocks are more easily eroded, which helps create gentler slopes and lower relief.

However, lowland does not always mean completely flat. Some lowland areas include rolling hills, scarps and gentle ridges, especially where more resistant rocks such as chalk form higher ground.

Climate of lowlands

Lowlands, especially in the south and east of England, are usually warmer and drier than uplands. East Anglia is one of the driest parts of the UK because it is further from the Atlantic and is partly sheltered by uplands to the west.

The south-east also tends to be warmer because it is generally lower, closer to continental Europe, and less exposed to cool Atlantic air than western uplands.

Human activity in lowlands

Lowlands are often the most intensively used parts of the UK. Arable farming — growing crops — is common where soils are fertile and slopes are gentle. East Anglia, for example, is important for crops such as wheat, barley, sugar beet and vegetables.

Lowlands also contain many of the UK’s largest towns and cities. This is because flatter land makes it easier to build houses, roads, railways, airports and industry. The London Basin is a good example of a lowland area with very dense settlement and major transport links.

5. Glaciated landscapes

A glaciated landscape is an area shaped by glaciers or ice sheets. A glacier is a moving mass of ice. During the Pleistocene ice ages — cold periods ending about 11,700 years ago — ice covered large parts of northern and western Britain.

The strongest glacial landscapes are found in upland areas such as the Scottish Highlands, Lake District, Snowdonia/Eryri and parts of Northern Ireland. Ice also left deposits across some lower areas, but the most dramatic glacial scenery is usually found in the mountains.

Characteristics of glaciated landscapes

Glaciated landscapes often have:

• U-shaped valleys, which are wide, steep-sided valleys carved by ice.
• Ribbon lakes, which are long, narrow lakes found in over-deepened glacial valleys.
• Corries, which are bowl-shaped hollows on mountainsides where glaciers formed.
• Arêtes, which are narrow ridges between corries or glacial valleys.
• Moraines, which are ridges or piles of rock material deposited by ice.

You do not need to explain all these landforms in detail for this overview section, but you should recognise that they make glaciated landscapes distinctive: steep, rugged, scenic and often wet.

Human activity in glaciated areas

Glaciated uplands often attract tourism because of their dramatic scenery. The Lake District, for example, is famous for mountains, lakes and walking routes. Snowdonia/Eryri attracts visitors for hiking, climbing and mountain views.

But these areas can also be challenging places to live and work. Steep slopes restrict building and farming, thin soils limit crop growth, and narrow valley roads can become congested during tourist seasons.

6. Comparing the three landscape types

7. Linking geology, climate and people

The strongest answers do not treat geology, climate and human activity as separate facts. They link them together.

For example, in the Lake District, hard rocks and past glaciation create steep mountains, deep valleys and lakes. The high relief leads to wet conditions because of relief rainfall. These conditions limit arable farming but create opportunities for reservoirs, sheep farming and tourism.

In East Anglia, lower relief, gentler slopes and fertile soils support large-scale arable farming. The drier climate helps crop production, and the flatter land makes transport, settlement and mechanised farming easier.