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  1. The formation of a glacial trough involves two processes abrasion and plucking. Abrasion is when pieces of debris in the glacier wear away at the rocks below, a bit like sandpaper. The sharper...

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  2. Aug 9, 2024 · Learn about the formation of glacial landforms from corries to troughs, along with examiner tips and worked examples for the AQA GCSE Geography exam.

  3. These are valleys formed by the glacial processes of weathering, erosion and transportation. They have steep sides and flat floors. Unlike V-shaped river valleys, glacial troughs are straight as they have truncated any interlocking spurs which existed prior to glacial advance.

  4. Oct 3, 2024 · Deep U-shaped valleys or troughs. Features of deposition and erosion - striations left behind on rocks, tell the direction of ice travel. Outwash plains and braided rivers etc. Glaciated landscapes can be divided into an active (current) or relict (past) landscapes.

  5. Jan 1, 2014 · The glacial trough is also called “U” shaped valley, relatively straight, flat-bottomed, deeper, and steep-sided valley formed by glacial erosion (Figure 1). Originally the valley would have in existence as stream/river valley prior to occupation by a glacier.

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  6. May 28, 2023 · The equatorward region of any meander is called a trough (pronounced like “troff”) and is associated with low pressure or low geopotential height. The poleward portion of a meander is called a ridge, and has high pressure or height.

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  8. Apr 3, 2020 · Abstract. A novel method is introduced to identify and track the life cycle of upper-level troughs and ridges. The aim is to close. the existing gap between methods that detect the initiation ...

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