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Study Guide: CUET UG Geography Physical Geography Landforms Fluvial Glacial Coastal Arid Landforms
Source: https://www.fatskills.com/cuet/chapter/cuet-ug-geography-physical-geography-landforms-fluvial-glacial-coastal-arid-landforms

CUET UG Geography Physical Geography Landforms Fluvial Glacial Coastal Arid Landforms

By Fatskills Exam Guides Team — the exam nerds behind 28,500+ quizzes and 2.1M practice questions across 500+ global exams.

⏱️ ~5 min read

Must-Know (15–20 detailed bullets)

  • Fluvial landforms are created by erosion, transportation, and deposition of sediments by running water in rivers. Example: Ganga River forms alluvial fans and floodplains.
  • Vertical erosion dominates in the upper course of a river, leading to V-shaped valleys and gorges. Example: Grand Canyon formed by the Colorado River.
  • Waterfalls form when a river flows over alternating bands of hard and soft rock; the soft rock erodes faster. Example: Niagara Falls (USA-Canada border).
  • Rapids develop where there are sudden changes in gradient or resistant rock bands in a river channel. Example: Rapids on the Narmada River near Jabalpur.
  • Potholes are circular depressions formed by the abrasive action of pebbles and sand in swirling eddies at the riverbed. Process: Corrasion.
  • Meanders are sinuous bends in a river in its middle course due to lateral erosion and deposition. Example: Meanders in the Kaveri River.
  • Ox-bow lakes form when a meander neck is cut off due to erosion and deposition, isolating a curved lake. Example: Ox-bow lakes in the floodplain of the Brahmaputra.
  • Delta formation occurs at river mouths where sediment deposition exceeds wave removal. Example: Sundarbans Delta (Ganga-Brahmaputra).
  • Estuaries form when river mouths are submerged due to rising sea levels or land subsidence; no significant delta. Example: Narmada Estuary.
  • Glacial landforms result from glacial erosion and deposition in high-altitude or high-latitude regions. Example: Himalayan glaciers shaping cirques and U-shaped valleys.
  • Cirque (or corrie) is a bowl-shaped depression formed by glacial erosion at the head of a glacial valley. Example: Cirques in the Pir Panjal Range.
  • Hanging valleys form when a smaller tributary glacier joins a larger one, leaving the tributary valley elevated. Example: Hanging valleys in Kashmir Valley.
  • Moraines are accumulations of glacial till (unsorted debris) deposited directly by ice. Types: lateral, medial, terminal, ground moraine.
  • Drumlins are elongated, teardrop-shaped hills formed by glacial deposition; steeper on the upstream side. Example: Drumlins in Ireland.
  • Coastal landforms arise from wave erosion and deposition along shorelines. Key processes: abrasion, attrition, hydraulic action.
  • Sea caves form by wave erosion along weak rock zones; when two caves meet, they form an arch. Example: Arches in the Andaman Islands.
  • Stacks are isolated pillars of rock left after the collapse of a sea arch. Example: The Old Man of Hoy in Scotland.
  • Beaches are depositional landforms made of sand, gravel, or shingle deposited by waves. Example: Marina Beach, Chennai.
  • Bars and spits are ridge-like depositional features; spits are attached at one end and project into water. Example: Neelankarai Spit in Tamil Nadu.
  • Arid landforms are shaped by wind erosion and deposition in deserts with sparse vegetation. Example: Thar Desert landforms.

Difficulty Level

Intermediate — Requires understanding of geomorphic processes and ability to distinguish between landforms formed by different agents (river, glacier, wind, waves), with specific examples.

Common CUET Traps

  • Trap: Confusing ox-bow lakes with meanders or assuming all river bends become lakes.
    Avoid: Ox-bow lakes result only after cutoff of a meander loop due to neck erosion — not all meanders evolve into lakes.

  • Trap: Believing that all deltas are triangular; some are bird’s foot or estuarine.
    Avoid: Deltas are classified based on shape and sediment supply; e.g., Mississippi has a bird’s-foot delta, while Narmada has no delta (forms estuary).

  • Trap: Assuming wind is the only agent in arid regions; ignoring water action (flash floods).
    Avoid: Though wind dominates, ephemeral streams and sheet wash also shape arid landforms like wadis and bajadas.

Practice MCQs

  1. Question: Which of the following landforms is primarily associated with the depositional activity of glaciers?

    A. Cirque

    B. Hanging valley

    C. Moraine

    D. Arete
    Answer: C
    Explanation: Moraines are formed by the deposition of glacial till.
    Why others fail: Cirque, hanging valley, and arete are erosional glacial landforms.

  2. Question: An ox-bow lake is formed when:

    A. A glacier retreats and leaves a lake in a cirque

    B. A meander is cut off from the main river channel

    C. Waves erode a headland to form a stack

    D. River deposits sediment at its mouth
    Answer: B
    Explanation: Ox-bow lakes form due to meander cutoff in fluvial systems.
    Why others fail: Option A describes a tarn, C describes coastal erosion, D refers to delta formation.

  3. Question: Which feature is NOT typically found in the upper course of a river?

    A. V-shaped valley

    B. Waterfall

    C. Delta

    D. Gorge
    Answer: C
    Explanation: Deltas form at the river mouth (lower course), not upper course.
    Why others fail: V-shaped valleys, waterfalls, and gorges are all upper-course features.

  4. Question: The Sundarbans delta is formed by the combined action of which rivers?

    A. Indus and Jhelum

    B. Godavari and Krishna

    C. Ganga and Brahmaputra

    D. Narmada and Tapti
    Answer: C
    Explanation: The Sundarbans is the world’s largest delta formed by the Ganga and Brahmaputra rivers.
    Why others fail: Indus forms a small delta in Pakistan; Narmada and Tapti form estuaries.

  5. Question: Which of the following coastal landforms results from the collapse of a sea arch?

    A. Stack

    B. Bar

    C. Spit

    D. Beach
    Answer: A
    Explanation: A stack is the remnant pillar of rock left after an arch collapses.
    Why others fail: Bar, spit, and beach are depositional features, not erosional remnants.

Last‑Minute Revision

  • ⚠️ V-shaped valley – fluvial erosion in upper course.
  • ⚠️ U-shaped valley – glacial erosion (e.g., Himalayas).
  • ⚠️ Potholes – formed by abrasion in riverbeds.
  • ⚠️ Meander – lateral erosion in middle course; inner bank has slip-off slope, outer has undercut slope.
  • ⚠️ Delta vs. Estuary: Delta forms with high sediment, low wave energy; estuary when river mouth is submerged.
  • ⚠️ Ganga forms Sundarbans Delta; Narmada forms estuary.
  • ⚠️ Cirque – bowl-shaped glacial hollow; may contain tarn after ice melts.
  • ⚠️ Hanging valley – tributary glacial valley above main valley; often forms waterfall.
  • ⚠️ Moraine – unsorted glacial deposit; lateral, medial, terminal types.
  • ⚠️ Drumlins – glacial depositional feature; streamlined hills aligned with ice flow.
  • ⚠️ Sea cave → arch → stack sequence due to coastal erosion.
  • ⚠️ Stack – isolated pillar after arch collapse (e.g., Old Man of Hoy).
  • ⚠️ Spit – depositional feature extending from coast into sea; one end attached.
  • ⚠️ Bar – connects two headlands, closing off lagoon.
  • ⚠️ Arid regions: wind erosion forms yardangs and ventifacts; deposition forms sand dunes.
  • ⚠️ Barchan dune – crescent-shaped with horns facing windward; found in Thar Desert.
  • ⚠️ Flash floods in deserts cause wadis (ephemeral streams).
  • ⚠️ Deflation hollows – formed by wind removal of fine particles.
  • ⚠️ NCERT term: "Fluvial" refers to river-related processes and landforms.
  • ⚠️ Glacial till – unsorted, unstratified material deposited directly by ice.


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