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WorldGeo0083 — Landforms of Erosion and Deposition: Rivers, Glaciers, Coasts and Deserts

Rivers, ice, waves, and wind never stop shaping the land. Each one carves its own signature landforms, and each leaves clues an exam question can test.

This article names the key landforms of erosion and deposition, from river gorges to desert dunes.

A crescent-shaped barchan sand dune in the Sperrgebiet desert, Namibia
A barchan dune in the Sperrgebiet desert, Namibia. Barchans form where wind direction stays steady and sand supply is limited. Photo: Plastic pony, via Wikimedia Commons, CC BY-SA 4.0.
MCQ QuestionsMCQ Questions
WorldGeo0083
5

Geomorphic agents, each building its own family of landforms.
Running Water
Meanders, Deltas
Gorges, oxbow lakes, floodplains
Groundwater
Karst Caves
Sinkholes, stalactites, stalagmites
Glaciers
Cirques, Moraines
Horns, aretes, eskers, drumlins
Wind
Sand Dunes
Barchan, seif, longitudinal, transverse
The exam angle: exams love asking you to match a landform name to its correct geomorphic agent. Learn each feature grouped by the agent that made it, not as one long mixed list.
📑 Contents
🏛️ Must Know
Fluvial Landforms: Rivers at Work
  • Gorge vs Canyon A gorge is a deep, steep-sided valley of similar width top to bottom. A canyon looks similar but is wider at the top than the bottom, in step-like layers.(NCERT 11)
  • Meanders and Oxbow Lakes Rivers on gentle slopes curve into loops called meanders. When a loop gets cut off from the main channel, it becomes a stranded, curved oxbow lake.(NCERT 11)
  • Floodplains and Levees A floodplain forms where a river deposits fine sediment beyond its banks during floods. Natural levees are low ridges of coarser deposits that build up right along the riverbank.(NCERT 11)
  • Alluvial Fans and Deltas An alluvial fan forms where a river drops its coarse load suddenly, on reaching flatter ground. A delta is the same idea, but where a river meets the sea, with sediment sorted finer as it spreads.(NCERT 11)
  • River Terraces These are old floodplain or valley-floor surfaces, left standing above the river’s current level. They mark a former, higher position of the same river.(NCERT 11)
  • Youth, Mature, Old A river landscape ages through three stages. In youth, streams are few, with shallow V-shaped valleys. In maturity, many streams cut deep valleys with sharp divides between them. In old age, few streams remain, floodplains grow wide, and the land wears down nearly flat.(NCERT 11)
Karst Topography: Groundwater’s Underground Sculptures
  • What Karst Needs Karst topography develops only in soluble rock, like limestone, where groundwater dissolves the rock over time. It is named after the Karst region of the Balkans.(NCERT 11)
  • Sinkholes These are the most common karst feature: circular depressions where the rock has dissolved from below. Some are simple solution features; others form when a cave roof collapses.(NCERT 11)
  • Caves and Their Contents Caves form along bedding planes where limestone dissolves away. Inside, stalactites hang down from the ceiling, and stalagmites rise up from the floor below them.(NCERT 11)
  • Lapies and Polje Lapies are the jagged, grooved ridges left after heavy solution activity. A polje is the largest karst depression of all, far bigger than a sinkhole or uvala.(NCERT 11)
Glacial Landforms: Carved and Dumped by Ice
  • Cirque This is a deep, steep-walled basin cut by ice at the head of a glacial valley. A cirque often holds a small lake, called a tarn, once the glacier melts.(NCERT 11)
  • Horn and Arete Where three or more cirques cut back into a single peak, a sharp horn forms. Mount Everest and the Matterhorn are both horns. A narrow, saw-toothed ridge between two cirques is called an arete.(NCERT 11)
  • Moraines These are ridges of debris dropped by a glacier. A terminal moraine sits at the glacier’s furthest point; lateral moraines run along its sides; a medial moraine runs down the middle, where two glaciers meet.(NCERT 11)
  • Eskers and Drumlins An esker is a long, winding ridge left by a stream that once flowed under the ice. A drumlin is a smooth, oval hill of till, shaped like an upturned spoon pointing in the direction the ice moved.(NCERT 11)
  • Fjords These are deep glacial valleys that flooded with seawater after the ice retreated. Norway’s coastline is famous for them.(NCERT 11)

Test Yourself

1. A crescent-shaped sand dune with its points trailing downwind is called a:

 

📘 Good to Know
Coastal Landforms: Where Waves Meet Land
  • Cliffs and Wave-Cut Terraces Waves pounding a rocky coast carve steep sea cliffs. As the cliff retreats, it leaves a flat wave-cut terrace of rock debris in front of it.(NCERT 11)
  • Caves and Sea Stacks Wave action hollows out sea caves in a cliff. When a cave’s roof collapses, an isolated pillar of rock left standing offshore is a sea stack.(NCERT 11)
  • Bars, Spits, and Lagoons A bar is a ridge of sand or shingle parallel to the coast. A spit is a bar attached at one end to the land. When a spit or bar closes off a bay, it traps a lagoon behind it.(NCERT 11)
  • India’s Two Coasts India’s west coast is a high, rocky, retreating coast, so erosion features dominate there. The east coast is low and sedimentary, so depositional features like deltas dominate instead.(NCERT 11)
Desert Landforms and the Five Dune Types
  • Pediments and Inselbergs A pediment is a gently sloping rock floor at the foot of a mountain, cut back by erosion. As pediments grow and the mountain shrinks, an isolated rocky remnant called an inselberg is left standing.(NCERT 11)
  • Playas These are shallow desert lakes at the centre of an enclosed basin. They hold water only briefly, and often leave behind a crust of salt called an alkali flat.(NCERT 11)
  • Barchan A crescent-shaped dune with its points trailing downwind. It forms where wind direction is steady and the original ground is fairly flat and even.(NCERT 11)
  • Seif and Parabolic A seif is like a barchan with only one wing, formed when wind direction shifts. A parabolic dune is the reverse shape of a barchan, its points anchored by patchy vegetation instead of trailing free.(NCERT 11)
  • Longitudinal and Transverse Longitudinal dunes form as long, low ridges running parallel to a steady wind, where sand supply is scarce. Transverse dunes instead run perpendicular to the wind, where sand is abundant.(NCERT 11)
📝 Exam Point of View
Exam Point of View: Karst and Lake Types
  • Real PYQ CAPF ACs 2020, General Ability asked which karst landform is largest: a polje, uvala, swallow hole, or sink hole. The answer is polje, a depression far bigger than the others.
  • Real PYQ CDS I 2018, General Knowledge tested a statement pair on sinkholes: both statements were true, but the depth-range statement did NOT explain why sinkholes are the most common karst form.
  • Real PYQ CAPF ACs 2020 also matched lake types to real Indian lakes: Bhimtal is a lake formed by landslide, and Ashtamudi is a lagoon, testing whether you can tell these landform-linked lake types apart.
  • The Pattern Karst questions test the size hierarchy (sinkhole < uvala < polje) and cause-effect reasoning, not just definitions. Learn the size order as a ladder, not a list.

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