Full Chapter Summary & Detailed Notes - Geomorphic Processes Class 11 NCERT
Overview & Key Concepts
- Chapter Goal: Understand geomorphic processes shaping earth's surface through endogenic (internal) and exogenic (external) forces. Exam Focus: Definitions of processes like weathering, mass wasting, erosion; differences between endogenic/exogenic; soil formation factors; diagrams (e.g., Figure 5.1 Denudational processes). 2025 Updates: Emphasis on climate change impacts on processes like accelerated erosion. Fun Fact: Earth's surface is uneven due to constant battle between building (endogenic) and wearing (exogenic) forces. Core Idea: Geomorphic agents (water, wind, ice) transport materials; gradation levels surface. Real-World: Himalayan landslides due to tectonic activity and heavy rains. Ties: To next chapter on landforms evolution. Expanded: Processes operate over long periods; human activities accelerate degradation, affecting biodiversity and resources. Sustainability: Preserve through understanding to minimize damage.
- Wider Scope: Diastrophism, volcanism as endogenic; denudation includes weathering/erosion/transportation. Variations due to climate, rock structure.
- Expanded Content: Earth's crust dynamic; internal forces build, external wear. Humans overuse resources, diminishing potential. Processes: Physical/chemical/biological weathering; mass movements (creep/slide/flow); agents controlled by climate (wind/liquid/solid). Soil: Pedogenesis from weathering mantle colonized by organisms.
Introduction
After earth's origin, crust/layers evolution, plate movements, earthquakes/volcanism, rocks/minerals, now detail earth's surface. Why uneven? Crust dynamic, moved/moves vertically/horizontally. Internal forces built variations; external (sunlight) wear down. Endogenic (internal) build; exogenic (external) degrade/aggrade. Gradation: Erosion wears relief. Variations persist as forces oppose. Endogenic land building; exogenic wearing. Surface sensitive; humans use intensively, damaging environment. Use sustainably for future. Shaped over long periods; understand processes/materials to minimize harm. Expanded: All organisms sustain; humans overused. Precautions preserve posterity. Geomorphic: Changes configuration via physical/chemical actions.
- Examples: Degradation elevations; aggradation basins. Depth: Diastrophism/volcanism endogenic; weathering/mass wasting/erosion/deposition exogenic.
- Point: Agents (water/ice/wind) mobile due to gradients; remove/transport/deposit.
- Expanded: Process force on materials; agent mobile medium. Gravity directional; stresses activate currents/winds. No gravity/gradients, no mobility/erosion.
Extended: Distinguish agents/processes? Gravity stresses important as others.
Geomorphic Processes
Endogenic/exogenic cause stresses/actions changing surface configuration. Diastrophism/volcanism endogenic (Unit II). Weathering/mass wasting/erosion/deposition exogenic (detailed here). Agent: Mobile exogenic element (water/ice/wind) acquiring/transporting materials. Process/agent same unless stated. Gravity: Downslope movements/stresses. Indirect: Wave/tide currents/winds. Gradients: Higher to lower levels/pressure. Expanded: Energy from within (radioactivity/rotation/tidal friction/primordial heat) drives endogenic. Geothermal gradients/heat flow induce diastrophism/volcanism. Variations in gradients/thickness/strength make crustal surface uneven.
- Examples: Orogenic (mountain building/folding); epeirogenic (uplift/warping); earthquakes (minor); plate tectonics (horizontal).
- Point: Orogeny severe folds; epeirogeny simple deformation. Faulting/fracturing cause PVT changes/metamorphism.
- Expanded: Volcanism: Magma movement; intrusive/extrusive forms (Unit II/igneous rocks).
Extended: Words volcanism/volcanoes: Movement molten rock; forms.
Endogenic Processes
Energy from within: Radioactivity/rotation/tidal/primordial. Geothermal gradients/heat flow induce diastrophism/volcanism. Crustal thickness/strength variations make surface uneven. Diastrophism: Move/elevate/build crust. Orogenic: Mountain building/folds narrow belts. Epeirogenic: Uplift/warping large parts. Earthquakes: Minor local. Plate tectonics: Horizontal plates. Orogeny deforms folds; epeirogeny simple. Processes cause faulting/fracturing; PVT changes metamorphism. Expanded: Differences epeirogeny/orogeny: Continental vs mountain building.
- Examples: Severe folding long/narrow; uplift large parts.
- Point: Volcanism magma surface/forms (detailed prior).
- Expanded: Endogenic mainly building; oppose exogenic wearing.
Extended: Tectonically controlled original surface uneven.
Exogenic Processes
Energy from atmosphere (sun) and tectonic gradients. Gravity downslope; produce movement. Stress: Force/area; shear (separating). Breaks rocks; angular displacement. Molecular stresses: Temperature/crystallisation/melting. Chemical: Loosen bonds/dissolve/cement. Stresses basic reason weathering/mass movements/erosion. Temperature/precipitation control. Denudation: Strip/uncover; weathering/mass wasting/erosion/transportation. Figure 5.1: Processes/driving forces. Expanded: Climatic regions vary processes; vegetation influences indirectly. Local variations: Altitude/aspect/insolation. Intensity depends rock type/structure (folds/faults/joints/hardness/permeability).
- Examples: Wind velocities/directions; precipitation/evaporation; freeze-thaw; frost penetration.
- Point: Sole driving force: Sun's heat/climatic elements.
- Expanded: Rocks resistant one process/non-resistant another; varying climates different resistances. Effects small/slow but cumulative fatigue.
Extended: Differences surface originally crustal evolution; persist due materials/processes/rates.
Weathering
Action weather/climate over materials. Mechanical disintegration/chemical decomposition. In-situ/on-site; little/no motion. Conditioned geological/climatic/topographic/vegetative. Climate important; differs climate to climate; depth mantle (Figure 5.2). Groups: Chemical (solution/carbonation/hydration/oxidation/reduction); physical (gravitational/expansion/water pressures); biological. Rarely alone; dominance one. Expanded: Chemical: Decompose/dissolve/reduce clastic; oxygen/water/acids/heat. CO2 air/decomposition increases. Reactions similar lab.
- Examples: Solution dissolve; oxidation rust.
- Point: Physical: Applied forces (overburden/expansion/wetting-drying). Thermal expansion/pressure release fracture.
- Expanded: Biological: Minerals/ions removal/growth/movement organisms. Burrowing/wedging expose; humic/carbonic acids enhance.
Extended: Motion weathering vs transportation? Not synonymous; weathering in-situ.
Mass Movements
Transfer rock debris down slopes gravity. No agents carry; debris may carry air/water/ice. Slow/rapid; shallow/deep; creep/flow/slide/fall. Weathering aids but not pre-requisite. Active weathered slopes. Aided gravity; no erosion but shift. Materials resist; yield when force > resistance. Factors: Weak materials/faults/steep slopes/precipitation/scarcity vegetation. Activating: Support removal/gradient increase/overloading/rainfall/seepage/earthquakes/vegetation removal. Expanded: Heave/flow/slide forms (Figure 5.5 relationships rates/moisture).
- Examples: Slump backward rotation; debris slide no rotation; rockslide bedding/joint.
- Point: Landslides rapid/perceptible; dry materials.
- Expanded: Himalayas frequent: Tectonic/sedimentary/steep/heavy rain. Nilgiris/Western Ghats: Stable/hard rocks but avalanches; steep cliffs/rainfall.
Extended: Mass wasting vs movements? Appropriate wasting; solifluction rapid flow? Yes saturated soil flow.
Erosion and Deposition
Erosion: Acquisition/transportation debris. Breaks fragments; agents remove/transport. Abrasion aids. Relief degrades; weathering aids but not pre-condition. Degradational. Kinetic energy controls. Agents: Wind/running water/glaciers/waves/groundwater. Climatic: Gaseous/liquid/solid. Waves: Coastal interface; groundwater: Lithological/permeable/soluble. Deposition: Agents lose velocity/energy gentler slopes; materials settle. Coarser first/finer later. Depressions fill. Expanded: Compare agents? Climate controls first three; others location/lithology.
- Examples: Karst soluble rocks/water.
- Point: Erosion changes surface; elaborated next chapter landforms.
- Expanded: Shift mass movements/erosion; both same? No; erosion agents active.
Extended: Erosion without weathering? Appreciable no.
Soil Formation
Dynamic medium chemical/physical/biological activities. Decay/growth; fluctuates seasons. Cold/dry slows; organic increases leaves/grasses die. Pedogenesis: Weathering mantle input. Colonised bacteria/mosses/lichens; organisms shelter; dead remains humus. Grasses/ferns/bushes/trees grow; roots penetrate; animals mix; porous/sponge retain water/air. Mature soil mineral/organic. Expanded: Weathering solely? No; factors control.
- Examples: Parent material passive; residual/transported.
- Point: Factors: Parent/topography/climate/biological/time.
- Expanded: Parent: Texture/structure/mineral/chemical. Topography: Exposure/sunlight/drainage; thin steep/thick flat.
Extended: Separate process/factors? Necessary; time/topography/parent passive.
Summary
- Geomorphic: Endogenic build/exogenic wear; weathering types; mass movements; erosion/deposition agents; soil factors/process.
Why This Guide Stands Out
Complete: All subtopics, examples, Q&A, quiz. Geography-focused. Free 2025. Verified correctness from NCERT text.
Key Themes & Tips
- Aspects: Dynamic, opposing forces, climatic variations.
- Thinkers: None specific; processes focus.
- Tip: Diagrams explain; differences compare; human impact discuss.
Exam Case Studies
Himalayan landslides, soil erosion agriculture, weathering tropical climates.
Project & Group Ideas
- Observe local topography/weathering/soil.
- Debate human role in accelerating processes.
60+ Questions & Answers - NCERT Based (Class 11)
Part A (1 mark short), B (4 marks medium), C (8 marks long). Based on NCERT, exercises. Answer lengths: 1 mark ~2 lines, 4 marks ~5 lines, 8 marks ~10 lines. Expanded with more Qs.
Part A: 1 Mark Questions
1. Why is earth's surface uneven?
1 Mark Answer: Due to internal forces building variations and external forces wearing them down. Endogenic build; exogenic degrade.
2. What are endogenic forces?
1 Mark Answer: Forces from within earth; mainly land building. Examples: Diastrophism and volcanism.
3. Define geomorphic processes.
1 Mark Answer: Physical stresses and chemical actions changing earth's surface configuration. Endogenic and exogenic.
4. What is a geomorphic agent?
1 Mark Answer: Mobile medium like water, wind, ice that removes, transports, deposits materials. Due to gradients.
5. Define diastrophism.
1 Mark Answer: Processes that move, elevate or build earth's crust. Includes orogenic and epeirogenic.
6. What is volcanism?
1 Mark Answer: Movement of molten magma toward or onto earth's surface. Forms intrusive/extrusive.
7. Define denudation.
1 Mark Answer: General term for weathering, mass wasting, erosion and transportation. Means to strip or uncover.
8. What is gradation?
1 Mark Answer: Wearing down of relief variations through erosion. Levels the surface.
9. Define weathering.
1 Mark Answer: Mechanical disintegration and chemical decomposition of rocks in-situ. Action of weather/climate.
10. What is chemical weathering?
1 Mark Answer: Processes like solution, carbonation, hydration, oxidation, reduction. Decomposes/dissolves rocks.
11. Define physical weathering.
1 Mark Answer: Depends on applied forces like gravitational, expansion, water pressures. Causes fractures.
12. What is biological weathering?
1 Mark Answer: Contribution or removal by organisms; burrowing, wedging, acids. Exposes new surfaces.
13. Define exfoliation.
1 Mark Answer: Flaking off curved sheets from rocks. Result of unloading/thermal expansion/salt.
14. What is mass movement?
1 Mark Answer: Transfer of rock debris down slopes under gravity. No agents like water/ice.
15. Define slump.
1 Mark Answer: Slipping of rock debris with backward rotation. Type of landslide.
16. What is erosion?
1 Mark Answer: Acquisition and transportation of rock debris by agents. Wears down landscape.
17. Define deposition.
1 Mark Answer: Settling of materials when agents lose velocity/energy. Fills depressions.
18. What is pedogenesis?
1 Mark Answer: Process of soil formation from weathering mantle. Colonised by organisms.
19. Name a soil-forming factor.
1 Mark Answer: Climate; controls moisture and temperature. Active factor.
20. What is humus?
1 Mark Answer: Finely divided organic matter in soil. From decaying plants/animals.
21. Define orogenic processes.
1 Mark Answer: Mountain building through severe folding. Affects narrow belts.
22. What is epeirogenic?
1 Mark Answer: Uplift or warping of large crustal parts. Continental building.
23. Define stress in geomorphology.
1 Mark Answer: Force per unit area; shear stresses break rocks. Induces deformation.
24. What is enrichment?
1 Mark Answer: Concentration of valuable materials by weathering/leaching. Economic ores.
25. Define debris slide.
1 Mark Answer: Rapid rolling/sliding earth debris without rotation. Type of landslide.
Part B: 4 Marks Questions
1. Explain why earth's surface is uneven.
4 Marks Answer: Crust dynamic; internal forces built variations, external wear down/fill up. Endogenic elevate/build; exogenic degrade/aggrade. Gradation wears relief but endogenic oppose, variations persist. Surface sensitive; humans overuse, damage environment. Sustain for future; shaped long periods, understand to minimize harm.
2. Define geomorphic processes and agents.
4 Marks Answer: Processes: Physical/chemical actions changing surface configuration. Endogenic/exogenic. Agents: Mobile mediums like water/ice/wind acquiring/transporting/depositing materials. Due gradients; same as processes unless stated. Gravity directional/stresses; no mobility without.
3. Describe endogenic processes.
4 Marks Answer: Energy from within: Radioactivity/rotation/tidal/primordial. Induce diastrophism/volcanism via gradients/heat flow. Crust uneven due variations thickness/strength. Diastrophism: Orogenic folds/epeirogenic uplift/earthquakes/plates. Volcanism: Magma movement/forms.
4. Differentiate orogeny and epeirogeny.
4 Marks Answer: Orogeny: Mountain building severe folding narrow belts. Deforms crust folds. Epeirogeny: Continental building uplift/warping large parts. Simple deformation. Both diastrophism; cause faulting/fracturing/PVT changes/metamorphism.
5. Explain exogenic processes.
4 Marks Answer: Energy atmosphere/sun/tectonic gradients. Gravity downslope movement/stresses. Shear breaks; molecular temperature/crystallisation. Chemical loosen/dissolve. Temperature/precipitation control; denudation weathering/mass/erosion/transport.
6. How do climatic factors affect exogenic processes?
4 Marks Answer: Variations thermal gradients create regions; processes vary. Vegetation density/type/distribution influence indirectly. Local: Altitude/aspect/insolation; wind/precipitation intensity/relation evaporation/freeze-thaw/frost depth.
7. Why is rock type/structure important in exogenic processes?
4 Marks Answer: Intensity depends type/structure: Folds/faults/joints/hardness/chemical susceptibility/permeability. Resistant one/non-resistant another; varying climates different resistances. Effects small/slow but cumulative fatigue.
8. Define weathering and its importance.
4 Marks Answer: Disintegration/decomposition rocks weather/climate actions in-situ. Breaks smaller; prepares regolith/soils/erosion/mass movements. Aids biomes/biodiversity/forests; enriches ores economic.
9. Describe chemical weathering processes.
4 Marks Answer: Solution/carbonation/hydration/oxidation/reduction decompose/dissolve/reduce clastic. Oxygen/water/acids/heat speed; CO2 air/decomposition increases. Reactions similar lab; fine state.
10. Explain physical weathering.
4 Marks Answer: Applied forces: Gravitational overburden/shearing; expansion temperature/crystal/animal; water wetting-drying. Fracture rocks surface/within; thermal expansion/pressure release cause. Fatigue repetition.
11. What is biological weathering?
4 Marks Answer: Organisms contribute/remove minerals/ions; physical changes growth/movement. Burrowing/wedging expose chemical/moisture/air. Decaying produce humic/carbonic acids enhance solubility.
12. Explain exfoliation.
4 Marks Answer: Flaking curved sheets rocks/bedrock; smooth rounded. Due expansion/contraction temperature/unloading/salt. Result not process; domes/tors unloading/thermal.
13. Describe mass movements.
4 Marks Answer: Debris down slopes gravity; no agents carry. Slow/rapid; creep/flow/slide/fall. Aided gravity; no erosion but shift. Resist until force > resistance.
14. What activates mass movements?
4 Marks Answer: Support removal/gradient increase/overloading/rainfall saturation/seepage/earthquakes/explosions/vegetation removal. Heave/flow/slide forms; rates/moisture (Figure 5.5).
15. Explain landslides.
4 Marks Answer: Rapid/perceptible; dry materials. Size/shape depend discontinuities/weathering/slope. Slump rotation; debris slide no; rockslide bedding/joint/fast destructive.
16. Why frequent landslides in Himalayas?
4 Marks Answer: Tectonically active; sedimentary/unconsolidated; steep slopes; heavy rainfall. Nilgiris/Western Ghats stable/hard but avalanches; steep cliffs/rainfall/temperature weathering.
17. Define erosion and deposition.
4 Marks Answer: Erosion: Acquisition/transport debris agents; abrades/degrades. Deposition: Settle lose velocity; coarser first/fills depressions. Aggradational.
18. Compare climatically controlled erosion agents.
4 Marks Answer: Wind gaseous; running water liquid; glaciers solid. Kinetic energy controls. Waves coastal; groundwater lithological/permeable/soluble.
19. Explain soil formation process.
4 Marks Answer: Pedogenesis weathering mantle colonised bacteria/mosses/lichens/organisms. Dead humus; grasses/ferns/bushes/trees grow; roots/animals mix porous/retain water/air. Mature mineral/organic.
20. Describe parent material in soil formation.
4 Marks Answer: Passive; residual/transported. Texture/structure/mineral/chemical composition. Weathering rate/depth important. Young soils link bedrock; limestone peculiar weathering.
21. How does topography affect soil?
4 Marks Answer: Passive; sunlight exposure/drainage. Thin steep; thick flat/gentle. Slow erosion/percolation favourable; organic accumulation dark colour.
22. Explain climate's role in soil formation.
4 Marks Answer: Active; moisture precipitation/evaporation/humidity; temperature seasonal/diurnal. Excess eluviation/illuviation/desilication; dry hardpans/kanker. Higher temperatures increase activity; freezing stops.
23. Describe biological activity in soil.
4 Marks Answer: Vegetation/organisms add organic/moisture/nitrogen/humus/acids. Bacterial intense tropical/oxidised; cold accumulates/peat. Nitrogen fixation rhizobium; mechanical reworking ants/earthworms.
24. What is time's role in soil formation?
4 Marks Answer: Length processes operate; maturation/profile development. Young alluvium/glacial till no/poor horizons. No absolute time; mature all act long.
25. Why passive factors in soil formation?
4 Marks Answer: Time/topography/parent material; act union affect others. Passive as not active like climate/biological. Why? Time/topography/parent.
Part C: 8 Marks Questions
1. Discuss "Our earth is a playfield for two opposing groups of geomorphic processes."
8 Marks Answer: Endogenic internal build/elevate surface; exogenic external wear down/fill up. Endogenic diastrophism/volcanism oppose exogenic weathering/erosion/deposition. Variations persist as forces continue; endogenic land building, exogenic wearing. Gradation wears relief but endogenic elevate. Surface dynamic; humans overuse damage balance. Sustain posterity; processes long periods. Understand materials/precautions minimize detrimental effects.
2. Explain exogenic geomorphic processes derive ultimate energy from sun's heat.
8 Marks Answer: Atmosphere determined sun; gradients tectonic. Gravity downslope/stresses but sun drives temperature/precipitation control processes. Denudation weathering/mass/erosion/transport. Climatic regions vary due thermal gradients latitudinal/seasonal/land-water. Vegetation influences indirectly. Local variations altitude/aspect/insolation/wind/precipitation/evaporation/freeze-thaw/frost. Intensity rock type/structure folds/faults/joints/hardness/permeability. Effects small/slow cumulative fatigue.
3. Are physical and chemical weathering processes independent? Explain with examples.
8 Marks Answer: Not independent; often together dominance one. Physical applied forces gravitational/expansion/water; fracture thermal/pressure release. Chemical solution/carbonation/hydration/oxidation/reduction decompose/dissolve oxygen/water/acids. Examples: Physical unloading exfoliation; chemical oxidation rust. Rarely alone; biological aids both burrowing/acids. Conditioned climate/geological/topographic/vegetative; depth mantle varies (Figure 5.2). Importance breaks/regolith/soils/erosion/biomes/enrichment ores.
4. How distinguish process soil formation and soil-forming factors? Role climate/biological as controls.
8 Marks Answer: Process pedogenesis weathering mantle colonised bacteria/mosses/lichens/organisms humus/grasses/trees roots/animals porous/retain mature mineral/organic. Factors control: Parent passive residual/transported texture/structure/composition; topography exposure/drainage thin steep/thick flat. Climate active moisture precipitation/eluv/illuv/desilication/hardpans/kanker; temperature increases/reduces/stops activity. Biological vegetation/organisms organic/moisture/nitrogen/humus/acids bacterial intense tropical/cold accumulates/peat fixation rhizobium mechanical. Time maturation/profile young no horizons. Act union; climate/biological important controls.
5. Describe endogenic and exogenic processes with examples.
8 Marks Answer: Endogenic within energy radioactivity/rotation/tidal/primordial gradients/heat diastrophism/volcanism crust uneven. Diastrophism orogenic folds narrow/epeirogenic uplift large/earthquakes/plates faulting/PVT metamorphism. Volcanism magma intrusive/extrusive. Exogenic atmosphere/sun/gradients gravity stresses shear/molecular chemical loosen. Denudation weathering/mass/erosion/transport Figure 5.1. Examples endogenic mountains/volcanoes; exogenic rivers/glaciers/wind erode/deposit. Climatic vary regions vegetation indirect local altitude/wind/precipitation/frost.
6. Explain significance of weathering.
8 Marks Answer: Breaks rocks fragments prepares regolith/soils aids erosion/mass movements. Biomes/biodiversity forests depend mantle depth. Erosion insignificant without; aids wasting/reduction relief/landforms changes consequence. Enrichment concentrations ores iron/manganese/aluminium/copper economic national. Soil formation important; leaching concentrates valuable. Examples exfoliation smooth/domes/tors; biological roots pressure/humic acids.
7. Describe types of mass movements and causes.
8 Marks Answer: Transfer debris gravity no agents; slow/rapid shallow/deep creep/flow/slide/fall. Weathering aids active weathered. Resist > force; weak materials/faults/steep/precipitation/scarcity vegetation favour. Causes support removal/gradient increase/overloading/rainfall/seepage/earthquakes/vegetation removal. Heave/flow/slide forms Figure 5.5 rates/moisture. Landslides rapid dry; slump rotation/debris slide no/rockslide fast. Himalayas frequent tectonic/sedimentary/steep/rain; Nilgiris stable hard avalanches cliffs/rainfall.
8. Explain erosion and deposition with agents.
8 Marks Answer: Erosion acquisition/transport debris agents abrade/degrade kinetic. Agents wind/water/glaciers/waves/groundwater climatic gaseous/liquid/solid. Waves coastal; groundwater lithological permeable/soluble karst. Deposition lose velocity gentler coarser first finer later fills. Not agent work aggradational. Examples running water valleys; glaciers moraines; wind dunes. Compare agents climate controls first three; others location/lithology. Shift mass/erosion but erosion agents active.
9. Discuss soil-forming factors with examples.
8 Marks Answer: Five: Parent/topography/climate/biological/time act union. Parent passive residual/transported texture/structure/composition weathering rate/depth young link bedrock limestone peculiar. Topography passive exposure/sunlight/drainage thin steep/thick flat gentle slow erosion/percolation organic dark. Climate active moisture precipitation/eluv/illuv/desilication wet hardpans/kanker dry temperature increase/reduce/stop. Biological add organic/moisture/nitrogen humus/acids bacterial tropical oxidised/cold accumulates/peat fixation rhizobium mechanical ants/earthworms. Time maturation/profile young alluvium no horizons no absolute.
10. Explain process of soil formation.
8 Marks Answer: Pedogenesis weathering mantle colonised bacteria/inferior plants mosses/lichens organisms shelter dead humus minor grasses/ferns grow bushes/trees seeds birds/wind. Roots penetrate burrowing animals particles mass porous sponge retain water/permit air mature complex mineral/organic. Weathering not solely but pre-requisite. Dynamic chemical/physical/biological fluctuates seasons cold/dry slows organic increases leaves/grasses. Is weathering responsible biodiversity? Yes aids biomes/forests.
11. Describe types of weathering with examples.
8 Marks Answer: Chemical: Solution/carbonation/hydration/oxidation/reduction decompose/dissolve oxygen/water/acids/heat CO2 decomposition. Physical: Gravitational overburden/expansion temperature/crystal/animal water wetting-drying fracture thermal/pressure. Biological: Remove/add minerals growth/movement burrowing/wedging expose humic/carbonic acids enhance. Rarely alone dominance; conditioned geological/climatic/topographic/vegetative depth mantle Figure 5.2. Examples chemical rust oxidation; physical exfoliation unloading; biological roots pressure.
12. Discuss mass movements that are real rapid and perceptible.
8 Marks Answer: Landslides: Rapid/perceptible dry materials size/shape discontinuities/weathering/slope. Slump slipping units backward rotation; debris slide rolling/sliding no rotation; debris fall free vertical/overhanging; rockslide individual masses bedding/joint/fault fast destructive; rock fall free blocks steep. Planar failures discontinuities. Himalayas frequent tectonic/sedimentary/steep/rain; Nilgiris stable hard avalanches cliffs/temperature/rainfall. Solifluction rapid flow saturated.
13. What are various mobile and mighty exogenic geomorphic agents and their job?
8 Marks Answer: Running water/groundwater/glaciers/wind/waves/currents acquire/transport/deposit. Job: Erosion degrade/transport; deposition aggrade. Climatic gaseous wind/liquid water/solid glacier. Waves coastal interface; groundwater lithological permeable/soluble karst. Lose velocity gentler coarser/finer settle fill depressions. Examples water valleys; wind dunes; glaciers moraines. Kinetic energy controls; changes surface landforms.
14. Is weathering essential as pre-requisite in soil formation? Why?
8 Marks Answer: Yes; weathering mantle basic input pedogenesis colonised organisms humus/plants/roots/animals porous mature soil. But not solely; factors parent/topography/climate/biological/time control. Weathering breaks fragments; aids but soil complex mixture. Examples young alluvium poor horizons; mature long time. Passive time/topography/parent; active climate/biological.
15. Explain role of gravity in geomorphic processes.
8 Marks Answer: Directional force downslope movements matter/stresses materials. Indirect activates wave/tide currents/winds. No gravity/gradients no mobility/erosion/transport/deposition. Keeping contact surface/switches movement; gradients higher/lower levels/pressure. Examples mass movements gravity aided; stresses shear break rocks angular/slippages.
16. Describe significance of weathering in biodiversity and economy.
8 Marks Answer: Breaks rocks prepares regolith/soils aids erosion/mass; biomes/biodiversity forests depend mantle depth. Erosion consequence; reduction relief/landforms changes. Enrichment ores iron/manganese/aluminium/copper economic national. Examples leaching concentrates valuable; without insufficient exploit/refine.
17. Discuss human impact on geomorphic processes.
8 Marks Answer: Overuse resources damage environment diminish potential. Accelerate degradation; e.g., vegetation removal activates mass movements. Understand nature use effectively without disturbing balance. Sustain life future; shaped long periods misuse fast rate. Precautions minimize detrimental.
18. Explain variations in exogenic processes due to climate and rock type.
8 Marks Answer: Climatic regions thermal gradients latitudinal/seasonal/land-water; processes vary vegetation indirect. Local altitude/aspect/insolation/wind/precipitation/evaporation/freeze-thaw/frost. Intensity rock type/structure folds/faults/joints/hardness/susceptibility/permeability. Resistant one/non-resistant another; climates different degrees give topography differences.
19. Describe types of landslides with examples.
8 Marks Answer: Slump backward rotation; debris slide no rotation; debris fall free vertical; rockslide bedding/joint; rock fall superficial blocks. Planar failures discontinuities. Examples Himalayan scars steep (Figure 5.5); Nilgiris avalanches cliffs/escarpments mechanical temperature/rainfall.
20. Discuss role of climate in soil formation with examples.
8 Marks Answer: Active moisture intensity/frequency/duration precipitation evaporation/humidity; temperature seasonal/diurnal. Excess eluviation/illuviation desilication wet equatorial silica removed. Dry evaporation > precipitation capillary salts crust hardpans. Tropical higher temperatures deeper profiles; tundra mechanically broken freezing. Examples wet calcium/sodium removed; intermediate kanker; humid bacterial intense low humus.
Tip: Use diagrams; compare types; explain examples; sustainability link.