Much of the scenery of Scotland, Wales, northern England and Northern Ireland was carved by ice. Glacial landscapes are one of the UK physical landscape options in several GCSE Geography specifications (AQA 8035, for example, lets schools choose two of coasts, rivers and glacial landscapes), and this material covers the option from the ice itself to the people who live, work and holiday in glaciated uplands today.
You begin with the extent of the ice. At the height of the last glacial period, ice covered about two-thirds of Britain and Ireland, including all of Scotland and most of Wales and northern England, while southern England stayed ice-free. You then learn the processes: freeze-thaw weathering, erosion by abrasion and plucking, movement by rotational slip, bulldozing, and deposition of unsorted till and sorted outwash.
The landform questions ask you to recognise and explain corries, arêtes, pyramidal peaks, truncated spurs, glacial troughs, ribbon lakes and hanging valleys, and then the features of transport and deposition: erratics, drumlins (and how their shape shows the direction of ice movement) and lateral, medial, terminal and ground moraine. Distractors deliberately mix in river and coastal landforms, so you practise telling them apart.
The human part looks at economic activities in glaciated uplands (tourism, sheep farming, forestry and quarrying) and the conflicts between them and conservation. Tourism questions cover what attracts visitors, the social, economic and environmental impacts of large visitor numbers, and management strategies such as footpath repair and park-and-ride schemes.
The material offers a quiz with explanations, flashcards for every landform and process, a printable written sheet of eight exam-style tasks (explaining the formation of landforms, comparing till and outwash, and evaluating tourism management) and an oral exam in which an examiner asks you one question at a time and gives short feedback at the end. Add named examples from the upland area your class studied, such as the Lake District or Snowdonia (Eryri), to strengthen longer answers.
Practice material written by Zestly, based on the DfE GCSE geography subject content (landscapes and physical processes) and board specifications such as AQA GCSE Geography 8035, section 3.1.3 (glacial landscapes in the UK).
A small tributary valley ends much higher than the floor of a main glacial trough, and its stream drops down the valley side as a waterfall. Why was the tributary valley left hanging?
The smaller tributary glacier eroded its valley floor less deeply than the large main glacier
The main glacier was much larger and more powerful, so it eroded its trough far deeper than the small tributary glacier eroded its own valley. When the ice melted, the tributary valley was left hanging high on the side of the main valley, and its stream now falls as a waterfall.
GCSEs are awarded by AQA, Pearson Edexcel, OCR, WJEC/Eduqas and CCEA, and regulated by Ofqual, Qualifications Wales and CCEA Regulation, the regulators for England, Wales and Northern Ireland. Zestly is not affiliated with or endorsed by Ofqual or any awarding body. These materials are our own and reproduce no past-paper content.