SlideShare une entreprise Scribd logo
1  sur  12
SUBMITTED TO :

DR SUNITA SINGH
Mass Wasting
What is mass wasting?
Mass wasting refers to several processes that have the following in
common:
1. Downslope movement of rock or weathered material
2. Movement is due to pull of gravity
3. There is no flowing medium (water, air or ice) that carries the
material

Why is mass wasting important?
1.
Processes represent a significant hazard to property and people
2.
Need to identify where and under what conditions these
processes occur
3.
Avoid construction in areas prone to mass wasting or attempt to
prevent mass wasting
*Generally, mass wasting occurs when gravitational forces exceed
frictional or shear forces (strength) of material.
Shear stress is the downslope pulling causing mass movement related to the mass
of the material and the angle of the slope.
Shear strength is the counteraction of the force of shear stress (i.e., friction).
If stress is greater than strength, then mass movement occurs.
Possibly triggered by:
1. Earthquake
2. Construction work (blasting)
3. Flooding
Driving force behind Mass Wasting:
1. Downslope pull of gravity
2. Depends on weight (amount) of material on slope.
3. Increasing amount of material can lead to mass wasting.
4. Depends on steepness of slope.
5. Over steepening slopes can lead to mass wasting.
Clays provide cohesion to unconsolidated materials.
Mineral cements hold rock together
Role of Water in Mass Wasting
1. Small amount of water can increase strength.
2. Surface tension of water helps hold material together.
3. Saturation with water weakens material.
4. Hydrostatic pressure can act to push grains apart.
Role of Vegetation in Mass Wasting
1.
Roots add strength to material by binding loose material together.
2.
In semi-arid and arid regions, forest fires can remove vegetation from hill
slopes, leaving surface materials vulnerable to mass wasting.
Planes of Weakness in Material

Planes of weakness in the material can facilitate mass wasting if the planes are
oriented parallel to the slope.

Planes of weakness include bedding planes in sedimentary rocks and foliation
planes in metamorphic rocks.
Mass Wasting Processes
Processes can be classified based on
1. Type of material that moves
2. Nature of movement (flow or slide)
3. How fast material moves; e.g. rock falls/slides, slump, debris flows/earth
flows/mud flows, creep
Slope Stability is influenced by:
1. Steepness
2. Angle of repose
3. Fluid effects
4. Expansive clays presence
5. Vegetation present
6. Earthquakes
7. Quick clays presence
Types of mass movement:
1. Fall -- rocks fall from great distances as a result of gravity
2. Slide -- mostly coherent unit slides on a slope or bedding plane
3. Slump -- rock unit falling a short distance due to rotation
4. Flow -- landslides involving an unconsolidated mass that moves in a
chaotic fashion
5. Solifluction -- soil component moving over permafrost layers, analogous
to a hockey puck sliding on ice
6. Creep -- extremely slow movement due to gravity
Slumps
Movement of coherent block of material along a curved surface.
More likely to occur when slope is undercut from below, material is saturated.
Common on river banks where stream erosion over steepens banks.

Example of slump
Creep
Extremely slow movements downslope
Rates of creep are 1-10 mm/year
Bent tree trunks, fence posts, and utility poles; gravestones tilted downslope
indicate that creep has occurred.
Creep damages buildings, roads

Debris flows, earth flows, mud flows
Flows are movements in which the material deforms chaotically as it moves.
Debris flows -- contains large boulders, gravels
Earth flows -- sandy material
Mudflow -- mud with considerable water
Most common
mass wasting
types
Avalanche

Creep

Flow

Slump

Rockslide
Fall

Avalanche

Slide

Flow

Slump

Creep
Deposits of Mass Wasting
Mass wasting produces sediment deposits.
These deposits commonly contain a wide range of sizes of particles (they
are "unsorted").

The deposits do not show layering (they are "unstratified")
How do we prevent landslides and mass wasting? This is NOT possible.
A better question is “how do we lessen the effects” of mass wasting?
 1.

Remove weight from slope

 2.

Engineering controls

 3.

Vegetation and GeofabricTM

 4.

Cables and anchoring systems

 5.

Tunnels built over highways thus reducing weight
THANK YOU
NASEER AHMAD KHAN

Contenu connexe

Tendances

weathering - meaning and effects
weathering - meaning and effectsweathering - meaning and effects
weathering - meaning and effectssubham12
 
Aeolian processes and landforms
Aeolian processes and landformsAeolian processes and landforms
Aeolian processes and landformsPramoda Raj
 
Geography fluvial landforms
Geography fluvial landformsGeography fluvial landforms
Geography fluvial landformsvusumuzingwane1
 
Fluvial landforms
Fluvial landformsFluvial landforms
Fluvial landformsMs Geoflake
 
Crustal Deformation and Orogeny
Crustal Deformation and OrogenyCrustal Deformation and Orogeny
Crustal Deformation and OrogenyJoemar Cabradilla
 
Weathering, erosion, and mass wasting
Weathering, erosion, and mass wastingWeathering, erosion, and mass wasting
Weathering, erosion, and mass wastingljeffreys
 
Weathering, Erosion, and Deposition
Weathering, Erosion, and DepositionWeathering, Erosion, and Deposition
Weathering, Erosion, and Depositionrebelbrindley
 
Causes of Landslide
Causes of LandslideCauses of Landslide
Causes of LandslideAkash Tikhe
 
Geologic Processes on Earth
Geologic Processes on EarthGeologic Processes on Earth
Geologic Processes on EarthHanna Elise
 
Models of landscape evolution and slope development by king
Models of landscape evolution and slope development by kingModels of landscape evolution and slope development by king
Models of landscape evolution and slope development by kingCharu Jaiswal
 

Tendances (20)

weathering - meaning and effects
weathering - meaning and effectsweathering - meaning and effects
weathering - meaning and effects
 
Aeolian processes and landforms
Aeolian processes and landformsAeolian processes and landforms
Aeolian processes and landforms
 
Geological landforms
Geological landformsGeological landforms
Geological landforms
 
Landforms unit 11
Landforms unit 11Landforms unit 11
Landforms unit 11
 
Fluvial Geomorphology
Fluvial GeomorphologyFluvial Geomorphology
Fluvial Geomorphology
 
Erosion
ErosionErosion
Erosion
 
Mass Movement
Mass MovementMass Movement
Mass Movement
 
Weathering
Weathering Weathering
Weathering
 
Erosion and deposition
Erosion and depositionErosion and deposition
Erosion and deposition
 
Mass wasting processes
Mass wasting processesMass wasting processes
Mass wasting processes
 
Geography fluvial landforms
Geography fluvial landformsGeography fluvial landforms
Geography fluvial landforms
 
Fluvial landforms
Fluvial landformsFluvial landforms
Fluvial landforms
 
Crustal Deformation and Orogeny
Crustal Deformation and OrogenyCrustal Deformation and Orogeny
Crustal Deformation and Orogeny
 
Weathering, erosion, and mass wasting
Weathering, erosion, and mass wastingWeathering, erosion, and mass wasting
Weathering, erosion, and mass wasting
 
Weathering, Erosion, and Deposition
Weathering, Erosion, and DepositionWeathering, Erosion, and Deposition
Weathering, Erosion, and Deposition
 
Causes of Landslide
Causes of LandslideCauses of Landslide
Causes of Landslide
 
Geologic Processes on Earth
Geologic Processes on EarthGeologic Processes on Earth
Geologic Processes on Earth
 
Models of landscape evolution and slope development by king
Models of landscape evolution and slope development by kingModels of landscape evolution and slope development by king
Models of landscape evolution and slope development by king
 
3.2 understanding tsunami
3.2 understanding tsunami3.2 understanding tsunami
3.2 understanding tsunami
 
Sinkholes
SinkholesSinkholes
Sinkholes
 

En vedette

3.4.2 Human Causes And Consequences Of Mass Movement V2
3.4.2 Human Causes And Consequences Of Mass Movement V23.4.2 Human Causes And Consequences Of Mass Movement V2
3.4.2 Human Causes And Consequences Of Mass Movement V2tudorgeog
 
Physical Causes And Consequences Of Mass Movement
Physical Causes And Consequences Of Mass MovementPhysical Causes And Consequences Of Mass Movement
Physical Causes And Consequences Of Mass Movementtudorgeog
 
Presentation on mass wasting
Presentation on mass wastingPresentation on mass wasting
Presentation on mass wastingUmer Bhatti
 
Atuação do Instituto Geológico na Prevenção aos Desastres Naturais
Atuação do Instituto Geológico na Prevenção aos Desastres NaturaisAtuação do Instituto Geológico na Prevenção aos Desastres Naturais
Atuação do Instituto Geológico na Prevenção aos Desastres NaturaisInstituto de Pesquisas Ambientais
 
Geography M2 Landslide
Geography M2 LandslideGeography M2 Landslide
Geography M2 LandslideeLearningJa
 
Trabalho de geologia
Trabalho de geologia   Trabalho de geologia
Trabalho de geologia biomaniacas
 
Geography M2 Soil Creep
Geography M2 Soil CreepGeography M2 Soil Creep
Geography M2 Soil CreepeLearningJa
 
All about mass wasting
All about mass wastingAll about mass wasting
All about mass wastingPrasil Koirala
 
Reducing the impacts of volcanoes
Reducing the impacts of volcanoesReducing the impacts of volcanoes
Reducing the impacts of volcanoesVictoriahoo1996
 
Erosion, Weathering And Mass Movement
Erosion, Weathering And Mass MovementErosion, Weathering And Mass Movement
Erosion, Weathering And Mass MovementMr Cornish
 
Presentation on natural disaster - avalanche
Presentation on natural disaster - avalanchePresentation on natural disaster - avalanche
Presentation on natural disaster - avalancheSiddhant Singh
 
Geology powerpoint
Geology powerpointGeology powerpoint
Geology powerpointerikaramos23
 
Volcano powerpoint
Volcano powerpointVolcano powerpoint
Volcano powerpointStacey
 
Landslides
LandslidesLandslides
Landslidesbreimajo
 
Volcanoes powerpoint
Volcanoes powerpointVolcanoes powerpoint
Volcanoes powerpointLavalittle
 

En vedette (20)

3.4.2 Human Causes And Consequences Of Mass Movement V2
3.4.2 Human Causes And Consequences Of Mass Movement V23.4.2 Human Causes And Consequences Of Mass Movement V2
3.4.2 Human Causes And Consequences Of Mass Movement V2
 
Physical Causes And Consequences Of Mass Movement
Physical Causes And Consequences Of Mass MovementPhysical Causes And Consequences Of Mass Movement
Physical Causes And Consequences Of Mass Movement
 
Presentation on mass wasting
Presentation on mass wastingPresentation on mass wasting
Presentation on mass wasting
 
Atuação do Instituto Geológico na Prevenção aos Desastres Naturais
Atuação do Instituto Geológico na Prevenção aos Desastres NaturaisAtuação do Instituto Geológico na Prevenção aos Desastres Naturais
Atuação do Instituto Geológico na Prevenção aos Desastres Naturais
 
Mass Wasting
Mass WastingMass Wasting
Mass Wasting
 
Edu290 ppt1koch
Edu290 ppt1kochEdu290 ppt1koch
Edu290 ppt1koch
 
Geography M2 Landslide
Geography M2 LandslideGeography M2 Landslide
Geography M2 Landslide
 
Trabalho de geologia
Trabalho de geologia   Trabalho de geologia
Trabalho de geologia
 
Geography M2 Soil Creep
Geography M2 Soil CreepGeography M2 Soil Creep
Geography M2 Soil Creep
 
All about mass wasting
All about mass wastingAll about mass wasting
All about mass wasting
 
Reducing the impacts of volcanoes
Reducing the impacts of volcanoesReducing the impacts of volcanoes
Reducing the impacts of volcanoes
 
Erosion, Weathering And Mass Movement
Erosion, Weathering And Mass MovementErosion, Weathering And Mass Movement
Erosion, Weathering And Mass Movement
 
Presentation on natural disaster - avalanche
Presentation on natural disaster - avalanchePresentation on natural disaster - avalanche
Presentation on natural disaster - avalanche
 
Weathering & it's types
Weathering & it's typesWeathering & it's types
Weathering & it's types
 
Avalanche
AvalancheAvalanche
Avalanche
 
Geology powerpoint
Geology powerpointGeology powerpoint
Geology powerpoint
 
Volcano powerpoint
Volcano powerpointVolcano powerpoint
Volcano powerpoint
 
Landslides
LandslidesLandslides
Landslides
 
Volcanoes
VolcanoesVolcanoes
Volcanoes
 
Volcanoes powerpoint
Volcanoes powerpointVolcanoes powerpoint
Volcanoes powerpoint
 

Similaire à MASS MOVEMENT

Chapter 8 section 1 (erosion by gravity)
Chapter 8 section 1 (erosion by gravity)Chapter 8 section 1 (erosion by gravity)
Chapter 8 section 1 (erosion by gravity)Mr. Motuk
 
Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2Mr. Motuk
 
Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2Mr. Motuk
 
AS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENT
AS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENTAS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENT
AS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENTGeorge Dumitrache
 
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSES
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSESCAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSES
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSESGeorge Dumitrache
 
earth and life 5.pptx
earth and life 5.pptxearth and life 5.pptx
earth and life 5.pptxShella69
 
Igcse coastal geomorph
Igcse coastal geomorphIgcse coastal geomorph
Igcse coastal geomorphWill Williams
 
Causes of gEOLOGIC hAZARDS.docx
Causes of gEOLOGIC hAZARDS.docxCauses of gEOLOGIC hAZARDS.docx
Causes of gEOLOGIC hAZARDS.docxBalaoroDheoLubang
 
Exogenic Processes
Exogenic ProcessesExogenic Processes
Exogenic ProcessesJonalyn Asi
 
DRRR - Earthquake Hazards
DRRR - Earthquake HazardsDRRR - Earthquake Hazards
DRRR - Earthquake HazardsDexter Cargullo
 
Landslides A Major Threat
Landslides A Major ThreatLandslides A Major Threat
Landslides A Major ThreatKhanImran5975
 
Geomorphology Presentation 1.pptx
Geomorphology Presentation 1.pptxGeomorphology Presentation 1.pptx
Geomorphology Presentation 1.pptxAdnanKhan153072
 

Similaire à MASS MOVEMENT (20)

Lecture 11 landslides
Lecture 11 landslidesLecture 11 landslides
Lecture 11 landslides
 
Mass wasting
Mass wastingMass wasting
Mass wasting
 
Chapter 8 section 1 (erosion by gravity)
Chapter 8 section 1 (erosion by gravity)Chapter 8 section 1 (erosion by gravity)
Chapter 8 section 1 (erosion by gravity)
 
Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2
 
Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2Chapter 7 Section 1 And 2
Chapter 7 Section 1 And 2
 
Landslide fr
Landslide frLandslide fr
Landslide fr
 
AS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENT
AS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENTAS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENT
AS GEOGRAPHY - ROCKS AND WEATHERING: SLOPE PROCESSES AND DEVELOPMENT
 
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSES
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSESCAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSES
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.3 SLOPE PROCESSES
 
chapter 3.ppt
chapter 3.pptchapter 3.ppt
chapter 3.ppt
 
Landslide
LandslideLandslide
Landslide
 
MASS WASTING
MASS WASTINGMASS WASTING
MASS WASTING
 
earth and life 5.pptx
earth and life 5.pptxearth and life 5.pptx
earth and life 5.pptx
 
Mass wasting.pptx
Mass wasting.pptxMass wasting.pptx
Mass wasting.pptx
 
Igcse coastal geomorph
Igcse coastal geomorphIgcse coastal geomorph
Igcse coastal geomorph
 
Slops
SlopsSlops
Slops
 
Causes of gEOLOGIC hAZARDS.docx
Causes of gEOLOGIC hAZARDS.docxCauses of gEOLOGIC hAZARDS.docx
Causes of gEOLOGIC hAZARDS.docx
 
Exogenic Processes
Exogenic ProcessesExogenic Processes
Exogenic Processes
 
DRRR - Earthquake Hazards
DRRR - Earthquake HazardsDRRR - Earthquake Hazards
DRRR - Earthquake Hazards
 
Landslides A Major Threat
Landslides A Major ThreatLandslides A Major Threat
Landslides A Major Threat
 
Geomorphology Presentation 1.pptx
Geomorphology Presentation 1.pptxGeomorphology Presentation 1.pptx
Geomorphology Presentation 1.pptx
 

Dernier

Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)eniolaolutunde
 
Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104misteraugie
 
Key note speaker Neum_Admir Softic_ENG.pdf
Key note speaker Neum_Admir Softic_ENG.pdfKey note speaker Neum_Admir Softic_ENG.pdf
Key note speaker Neum_Admir Softic_ENG.pdfAdmir Softic
 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactdawncurless
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Disha Kariya
 
Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfciinovamais
 
Web & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfWeb & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfJayanti Pande
 
1029-Danh muc Sach Giao Khoa khoi 6.pdf
1029-Danh muc Sach Giao Khoa khoi  6.pdf1029-Danh muc Sach Giao Khoa khoi  6.pdf
1029-Danh muc Sach Giao Khoa khoi 6.pdfQucHHunhnh
 
Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17Celine George
 
9548086042 for call girls in Indira Nagar with room service
9548086042  for call girls in Indira Nagar  with room service9548086042  for call girls in Indira Nagar  with room service
9548086042 for call girls in Indira Nagar with room servicediscovermytutordmt
 
social pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajansocial pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajanpragatimahajan3
 
Arihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdfArihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdfchloefrazer622
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingTeacherCyreneCayanan
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphThiyagu K
 
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...fonyou31
 
Grant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingGrant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingTechSoup
 
A Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy ReformA Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy ReformChameera Dedduwage
 
Beyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactBeyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactPECB
 

Dernier (20)

Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)Software Engineering Methodologies (overview)
Software Engineering Methodologies (overview)
 
Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104Nutritional Needs Presentation - HLTH 104
Nutritional Needs Presentation - HLTH 104
 
Key note speaker Neum_Admir Softic_ENG.pdf
Key note speaker Neum_Admir Softic_ENG.pdfKey note speaker Neum_Admir Softic_ENG.pdf
Key note speaker Neum_Admir Softic_ENG.pdf
 
Accessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impactAccessible design: Minimum effort, maximum impact
Accessible design: Minimum effort, maximum impact
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..
 
Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdf
 
Web & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfWeb & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdf
 
1029-Danh muc Sach Giao Khoa khoi 6.pdf
1029-Danh muc Sach Giao Khoa khoi  6.pdf1029-Danh muc Sach Giao Khoa khoi  6.pdf
1029-Danh muc Sach Giao Khoa khoi 6.pdf
 
Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17Advanced Views - Calendar View in Odoo 17
Advanced Views - Calendar View in Odoo 17
 
9548086042 for call girls in Indira Nagar with room service
9548086042  for call girls in Indira Nagar  with room service9548086042  for call girls in Indira Nagar  with room service
9548086042 for call girls in Indira Nagar with room service
 
Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1
 
social pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajansocial pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajan
 
Advance Mobile Application Development class 07
Advance Mobile Application Development class 07Advance Mobile Application Development class 07
Advance Mobile Application Development class 07
 
Arihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdfArihant handbook biology for class 11 .pdf
Arihant handbook biology for class 11 .pdf
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writing
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot Graph
 
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
Ecosystem Interactions Class Discussion Presentation in Blue Green Lined Styl...
 
Grant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy ConsultingGrant Readiness 101 TechSoup and Remy Consulting
Grant Readiness 101 TechSoup and Remy Consulting
 
A Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy ReformA Critique of the Proposed National Education Policy Reform
A Critique of the Proposed National Education Policy Reform
 
Beyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global ImpactBeyond the EU: DORA and NIS 2 Directive's Global Impact
Beyond the EU: DORA and NIS 2 Directive's Global Impact
 

MASS MOVEMENT

  • 1. SUBMITTED TO : DR SUNITA SINGH
  • 2.
  • 3. Mass Wasting What is mass wasting? Mass wasting refers to several processes that have the following in common: 1. Downslope movement of rock or weathered material 2. Movement is due to pull of gravity 3. There is no flowing medium (water, air or ice) that carries the material Why is mass wasting important? 1. Processes represent a significant hazard to property and people 2. Need to identify where and under what conditions these processes occur 3. Avoid construction in areas prone to mass wasting or attempt to prevent mass wasting *Generally, mass wasting occurs when gravitational forces exceed frictional or shear forces (strength) of material.
  • 4. Shear stress is the downslope pulling causing mass movement related to the mass of the material and the angle of the slope. Shear strength is the counteraction of the force of shear stress (i.e., friction). If stress is greater than strength, then mass movement occurs. Possibly triggered by: 1. Earthquake 2. Construction work (blasting) 3. Flooding Driving force behind Mass Wasting: 1. Downslope pull of gravity 2. Depends on weight (amount) of material on slope. 3. Increasing amount of material can lead to mass wasting. 4. Depends on steepness of slope. 5. Over steepening slopes can lead to mass wasting. Clays provide cohesion to unconsolidated materials. Mineral cements hold rock together
  • 5. Role of Water in Mass Wasting 1. Small amount of water can increase strength. 2. Surface tension of water helps hold material together. 3. Saturation with water weakens material. 4. Hydrostatic pressure can act to push grains apart. Role of Vegetation in Mass Wasting 1. Roots add strength to material by binding loose material together. 2. In semi-arid and arid regions, forest fires can remove vegetation from hill slopes, leaving surface materials vulnerable to mass wasting. Planes of Weakness in Material  Planes of weakness in the material can facilitate mass wasting if the planes are oriented parallel to the slope.  Planes of weakness include bedding planes in sedimentary rocks and foliation planes in metamorphic rocks. Mass Wasting Processes Processes can be classified based on 1. Type of material that moves 2. Nature of movement (flow or slide) 3. How fast material moves; e.g. rock falls/slides, slump, debris flows/earth flows/mud flows, creep
  • 6. Slope Stability is influenced by: 1. Steepness 2. Angle of repose 3. Fluid effects 4. Expansive clays presence 5. Vegetation present 6. Earthquakes 7. Quick clays presence Types of mass movement: 1. Fall -- rocks fall from great distances as a result of gravity 2. Slide -- mostly coherent unit slides on a slope or bedding plane 3. Slump -- rock unit falling a short distance due to rotation 4. Flow -- landslides involving an unconsolidated mass that moves in a chaotic fashion 5. Solifluction -- soil component moving over permafrost layers, analogous to a hockey puck sliding on ice 6. Creep -- extremely slow movement due to gravity
  • 7. Slumps Movement of coherent block of material along a curved surface. More likely to occur when slope is undercut from below, material is saturated. Common on river banks where stream erosion over steepens banks. Example of slump
  • 8. Creep Extremely slow movements downslope Rates of creep are 1-10 mm/year Bent tree trunks, fence posts, and utility poles; gravestones tilted downslope indicate that creep has occurred. Creep damages buildings, roads Debris flows, earth flows, mud flows Flows are movements in which the material deforms chaotically as it moves. Debris flows -- contains large boulders, gravels Earth flows -- sandy material Mudflow -- mud with considerable water
  • 11. Deposits of Mass Wasting Mass wasting produces sediment deposits. These deposits commonly contain a wide range of sizes of particles (they are "unsorted"). The deposits do not show layering (they are "unstratified") How do we prevent landslides and mass wasting? This is NOT possible. A better question is “how do we lessen the effects” of mass wasting?  1. Remove weight from slope  2. Engineering controls  3. Vegetation and GeofabricTM  4. Cables and anchoring systems  5. Tunnels built over highways thus reducing weight

Notes de l'éditeur

  1. NASEER AHMAD KHAN