Gravity pulls the rocks, soils and debris on a downward slope, naturally, without any chemical change. This downward movement is called as mass -movement or mass-wasting.
Landslides, mudflows and rockfalls are all belonging to this category of geomorphic processes.
Mass-wasting may lead to severe natural disasters by affecting the life and building structures in different places. Understanding of mass-wasting will certainly help to mitigate the impacts of these hazards and plan the development activities.
Geologic time scale, Uniformitarianism, Catastrophic concept, Geomorphic process-agent cause and product, Hutton's concept, Davis Concept, Darwin's concept, Gilbert's concept
Geomorphology at a glance: Major landformsP.K. Mani
Geomorphology, Major landforms, Genetic landform classifications, Volcanic landforms, River Systems and Fluvial Landforms, Aeolian Landforms, Glacial Landforms
Geologic time scale, Uniformitarianism, Catastrophic concept, Geomorphic process-agent cause and product, Hutton's concept, Davis Concept, Darwin's concept, Gilbert's concept
Geomorphology at a glance: Major landformsP.K. Mani
Geomorphology, Major landforms, Genetic landform classifications, Volcanic landforms, River Systems and Fluvial Landforms, Aeolian Landforms, Glacial Landforms
The reason for the occurrence of such a huge mass of water on the globe, is still a myth and reality. The reason goes back to the Origin of Earth itself. The exact mode of origin is not precisely known. Scientists assume, both Primary and secondary sources would have given rise to all both air and water on the earth. Two possible sources as internal source (or) external source have been proposed so far. Some of them are attributed towards the theories of origin of the earth.
After attending this lesson, the user would be able to understand the nature and causative factors of landslides, their characteristics, classifications, triggering mechanisms, and effects. The methods of controlling the effects of landslides, and avoiding their menace are also highlighted. Disaster management methods are to be adopted to mitigate the never ending natural hazards. This lesson is an important topic in disaster management.
The reason for the occurrence of such a huge mass of water on the globe, is still a myth and reality. The reason goes back to the Origin of Earth itself. The exact mode of origin is not precisely known. Scientists assume, both Primary and secondary sources would have given rise to all both air and water on the earth. Two possible sources as internal source (or) external source have been proposed so far. Some of them are attributed towards the theories of origin of the earth.
After attending this lesson, the user would be able to understand the nature and causative factors of landslides, their characteristics, classifications, triggering mechanisms, and effects. The methods of controlling the effects of landslides, and avoiding their menace are also highlighted. Disaster management methods are to be adopted to mitigate the never ending natural hazards. This lesson is an important topic in disaster management.
A grain started journey from a source area and in the way it become weathered, eroded, transported and finally deposited. It is a gross geologic description of grain's journey.
E-content is a Comprehensive package of teaching material put into hypermedia format. Hypermedia is multimedia with internet deplorability. E-content can not be created by a teaching faculty alone . It needs the role of teacher, Video editor, production assistants, web developers (HTML 5 or Adobe captivate, etc). Analyze the learner needs and goals of the instructional material development, development of a delivery system and content, pilot study of the material developed, implementation, evaluating, refining the materials etc. In designing and development of E-content we have to adopt one of the instructional design models based on our requirements.
Pedagogy is the most commonly understood approach to teaching. It refers to the theory and practice of learning. Pedagogy is often described as the act of teaching. Pedagogy has little variations between traditional teaching and online teaching. Online teaching pedagogy is a method of effective teaching practice specifically developed for teaching via the internet. It has a set of prescribed methods, strategies, and practices for teaching academic subjects in an online (or blended) environment, where students are in a physical location separate from the faculty member.
Technology has changed the possibilities within teaching and learning. Classes, which prior to the digital era were restricted to lectures, talks, and physical objects, no longer have to be designed in that manner. Training in a synchronous virtual classroom can only be successful with the active participation and engagement of the learners. Explore the Virtual Classroom’s features and see how they can support and enhance your tutoring style.
• The monitoring and evaluation of the institutional processes require a carefully structured system of internal and external review. The NAAC expects the Institutions to undertake continuous Academic and Administrative Audits (AAA). This presentation is intended to serve as advisory to all accredited HEIs who volunteer to undertake AAA. The pros and cons of this process are also highlighted. Academic and Administrative Audit is the process of evaluating the efficiency and effectiveness of the administrative procedure. It includes assessment of policies, strategies & functions of the various administrative departments, control of the overall administrative system, etc. This checklist gives an overview what the audit committee members may look into while visiting an institution for this purpose. It invariably follows the Quality Indicators Framework prescribed by Accreditation Council in India.
• The monitoring and evaluation of the institutional processes require a carefully structured system of internal and external review. The NAAC expects the Institutions to undertake continuous Academic and Administrative Audits (AAA). This presentation is intended to serve as advisory to all accredited HEIs who volunteer to undertake AAA.
Chemical analysis data of water samples can not be used directly for understanding. They are to be used for various calculations in order to determine the quality parameters that have a lot of significances. A. Balasubramanian and D. Nagaraju, of the Department of Studies in Earth Science, Centre for Advanced Studies, University of Mysore, Mysore-570006, Karnataka, India have recently brought out a software and its application manual as a good book for reference and execution. The Name of the software is WATCHIT meaning Water Chemistry Interpretation Techniques. This software computes more than 100 parameters pertaining to water quality interpretations. The software follows its own method of approach to determine the required results. Systems International Units are used. Limited input parameters are required. This is suitable for all scientific research, government water quality data interpretations and for understanding the quality of water before using it.
Water conservation refers to reducing the usage of water and recycling of waste water for different purposes like domestic usage, industries, agriculture etc. This technical article highlights most of the popular methods of water conservation. A special note on rainwater harvesting is also provided.
This module gives an overview of general applications of current hydrogeological aspects. It is for the basic understanding of students and research scholars.
Climate Extreme (extreme weather or climate event) refers to the occurrence of a value of a weather or climate variable above (or below) a threshold value near the upper (or lower) ends of the range of observed values of the variable. Extreme weather and climate events, interacting with exposed and vulnerable human and natural systems, can lead to disasters.
WATER RESOURCES PLANNING AND MANAGEMENT POSSIBILITIES IN CHAMARAJANAGAR TALUK...Prof. A.Balasubramanian
Any unplanned development and utilization of water resources with result in water scarcity. In many parts of the developing world. Such a situation exists. In order to do proper planning and
management of water resources, it is necessary to conduct detailed analyses of the factors, which influence the water availability and its uses. In the present study, a comprehensive analysis have been undertaken for proper utilization of water resources in Chamarajanagar Taluk, which has been identified as one of the drought hit districts of Karnataka, in India. The factors analysed in this work are, surface and groundwater availability, land use, cropping pattern, recharge potential of soils and the rainfall pattern in typical areas of Taluk. It is observed that the problem of water scarcity is mainly due to the lack of irrigation planning and management. Hence, a
modified cropping pattern is suggested by taking into consideration of all available water resources and other conditions.
In broad terms, cultural geography examines the cultural values, practices, discursive and material expressions and artefacts of people, the cultural diversity and plurality of society.
It also emphasizes on how cultures are distributed over space, how places and identities are produced, how people make sense of places and build senses of place, and how people produce and communicate knowledge and meaning.
Minerals are formed by changes in chemical energy in systems which contain one fluid or vapor phase. In nature, minerals are formed by crystallisation or precipitation from concentrated solutions. These solutions are called as ore-bearing fluids. Ore-bearing fluids are characterised by high concentration of certain metallic or other elements.
Fluids are the most effective agents for the transport of material in the mantle and the Earth's crust.
Soils are complex mixers forming the skin of the earth's surface. Soil is a dynamic layer in which many complex chemical, physical and biological activities are going on constantly. Soils become adjusted to conditions of climate, landform and vegetation, and will change internally when those controlling conditions change. Soils are products of weathering. Soils play a dominant role in earth's geomorphic processes in a cyclic manner. The characteristics of soils are very essential for several reasons. This module highlights these characteristics.
GIS TECHNIQUES IN WATER RESOURCES PLANNING AND MANAGEMENT IN CHAMARAJANAGAR ...Prof. A.Balasubramanian
The over-exploitation and contamination of groundwater continue to threaten the long-term sustainability of our precious water resources, in spite of the best efforts made by various agencies.
This has many serious implications to the economic development of a country like India. Lack of
judicious planning and integration of environmental consideration to ground water development
projects are primarily responsible for such a state of affair in the ground water sector. Geographical Information Systems could be of immense help in planning sustainable ground water management strategies, especially in hard rock areas with limited ground water potential. Data collected from
Satellite Imagery and through field investigations have been integrated, on a GIS platform, for demarcation and prioritization of areas suitable for ground water development and ground water augmentation. An attempt has also been made to assess the vulnerability of the area to ground water
contamination. This paper demonstrates the utility of GIS in planning judicious management of ground water resources in a typical hard rock area of Chamarajanagar Taluk, Karnataka, state India.
Nanobiomaterials are very effective components for several biomedical and pharmaceutical studies. Among the metallic, organic, ceramic and polymeric nanomaterials, metallic nanomaterials have shown certain prominent biomedical applications. Enormous works have been done to synthesize, analyse and administer the metallic nanoparticles for various kinds of medical and therapeutic applications, during the last forty years. In these analyses, the prominent biomedical applications of ten metallic nanobiomaterials have been reviewed from various sources and works. It has been found that almost nine of them are used in a very wide spectrum of medical and theranostic applications.
A variety of Nano-biomaterials are synthesised, characterised and tested to find out their potentialities by global scientific communities, during the last three decades. Among those, nanostructured ceramics, cements and coatings are being considered for major use in orthopaedic, dental and other medical applications. The development of novel biocompatible ceramic materials with improved biomedical functions is at the forefront of health-related applications, all over the world. Understanding of the potential biomedical applications of ceramic nanomaterials will provide a major insight into the future developments. This study reviews and enlists the prominent potential biomedical applications of ceramic nanomaterials, like Calcium Phosphate (CaP), Tri-Calcium Phosphate (TCP), Hydroxy-Apatite(HAP), TCP+HAP, Si substituted HAP, Calcium Sulphate and Carbonate, Bioactive Glasses, Bioactive Glass Ceramics, Titania-Based Ceramics, Zirconia Ceramics, Alumina Ceramcis and Ceramic Polymer Composites.
The present forest and tree cover of the country is 78.37 million ha in 2007 which is 23.84% of the geographical areas and it includes 2.82% tree cover. This becomes 25.25%, if the areas above tree line i.e., 4000m are excluded from the total geographical area. The forest cover is classified into 3 canopy density classes.
1. Very Dense Forest (VDF) with canopy density more than 70%
2. Moderately Dense Forest (MDF) with Canopy density between 40-70% and
3. Open Forest (OF) with Canopy density between 10-40%
Nutraceutical market, scope and growth: Herbal drug technologyLokesh Patil
As consumer awareness of health and wellness rises, the nutraceutical market—which includes goods like functional meals, drinks, and dietary supplements that provide health advantages beyond basic nutrition—is growing significantly. As healthcare expenses rise, the population ages, and people want natural and preventative health solutions more and more, this industry is increasing quickly. Further driving market expansion are product formulation innovations and the use of cutting-edge technology for customized nutrition. With its worldwide reach, the nutraceutical industry is expected to keep growing and provide significant chances for research and investment in a number of categories, including vitamins, minerals, probiotics, and herbal supplements.
Richard's aventures in two entangled wonderlandsRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Deep Behavioral Phenotyping in Systems Neuroscience for Functional Atlasing a...Ana Luísa Pinho
Functional Magnetic Resonance Imaging (fMRI) provides means to characterize brain activations in response to behavior. However, cognitive neuroscience has been limited to group-level effects referring to the performance of specific tasks. To obtain the functional profile of elementary cognitive mechanisms, the combination of brain responses to many tasks is required. Yet, to date, both structural atlases and parcellation-based activations do not fully account for cognitive function and still present several limitations. Further, they do not adapt overall to individual characteristics. In this talk, I will give an account of deep-behavioral phenotyping strategies, namely data-driven methods in large task-fMRI datasets, to optimize functional brain-data collection and improve inference of effects-of-interest related to mental processes. Key to this approach is the employment of fast multi-functional paradigms rich on features that can be well parametrized and, consequently, facilitate the creation of psycho-physiological constructs to be modelled with imaging data. Particular emphasis will be given to music stimuli when studying high-order cognitive mechanisms, due to their ecological nature and quality to enable complex behavior compounded by discrete entities. I will also discuss how deep-behavioral phenotyping and individualized models applied to neuroimaging data can better account for the subject-specific organization of domain-general cognitive systems in the human brain. Finally, the accumulation of functional brain signatures brings the possibility to clarify relationships among tasks and create a univocal link between brain systems and mental functions through: (1) the development of ontologies proposing an organization of cognitive processes; and (2) brain-network taxonomies describing functional specialization. To this end, tools to improve commensurability in cognitive science are necessary, such as public repositories, ontology-based platforms and automated meta-analysis tools. I will thus discuss some brain-atlasing resources currently under development, and their applicability in cognitive as well as clinical neuroscience.
What is greenhouse gasses and how many gasses are there to affect the Earth.moosaasad1975
What are greenhouse gasses how they affect the earth and its environment what is the future of the environment and earth how the weather and the climate effects.
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...University of Maribor
Slides from:
11th International Conference on Electrical, Electronics and Computer Engineering (IcETRAN), Niš, 3-6 June 2024
Track: Artificial Intelligence
https://www.etran.rs/2024/en/home-english/
Earliest Galaxies in the JADES Origins Field: Luminosity Function and Cosmic ...Sérgio Sacani
We characterize the earliest galaxy population in the JADES Origins Field (JOF), the deepest
imaging field observed with JWST. We make use of the ancillary Hubble optical images (5 filters
spanning 0.4−0.9µm) and novel JWST images with 14 filters spanning 0.8−5µm, including 7 mediumband filters, and reaching total exposure times of up to 46 hours per filter. We combine all our data
at > 2.3µm to construct an ultradeep image, reaching as deep as ≈ 31.4 AB mag in the stack and
30.3-31.0 AB mag (5σ, r = 0.1” circular aperture) in individual filters. We measure photometric
redshifts and use robust selection criteria to identify a sample of eight galaxy candidates at redshifts
z = 11.5 − 15. These objects show compact half-light radii of R1/2 ∼ 50 − 200pc, stellar masses of
M⋆ ∼ 107−108M⊙, and star-formation rates of SFR ∼ 0.1−1 M⊙ yr−1
. Our search finds no candidates
at 15 < z < 20, placing upper limits at these redshifts. We develop a forward modeling approach to
infer the properties of the evolving luminosity function without binning in redshift or luminosity that
marginalizes over the photometric redshift uncertainty of our candidate galaxies and incorporates the
impact of non-detections. We find a z = 12 luminosity function in good agreement with prior results,
and that the luminosity function normalization and UV luminosity density decline by a factor of ∼ 2.5
from z = 12 to z = 14. We discuss the possible implications of our results in the context of theoretical
models for evolution of the dark matter halo mass function.
Richard's entangled aventures in wonderlandRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
This pdf is about the Schizophrenia.
For more details visit on YouTube; @SELF-EXPLANATORY;
https://www.youtube.com/channel/UCAiarMZDNhe1A3Rnpr_WkzA/videos
Thanks...!
1. MHRD
NME-ICT
Course Title: Earth Science
Paper Title: The Dynamic Earth
Mass-wasting ProcessesMass-wasting Processes
By
Prof.A. Balasubramanian
Centre for Advanced Studies in Earth Science
University of Mysore, India
2. MHRD
NME-ICT
Introduction
Mass-wasting and its causes
Types of mass movements
Types of mass wasting
Factors influencing mass wasting
Geology and Slope Stability
Conclusion
Table of ContentsTable of Contents
3. MHRD
NME-ICT
After attending this module, the user should be able
to comprehend the importance of mass-wasting
processes on the planet earth.
It is one of the silent processes that is happening on
the surface of the earth.
The module also highlights the various kinds of mass-
movements and their impacts on land.
Objectives
4. MHRD
NME-ICT
Earth’s geomorphological processes are never ending
activities. The landforms are formed due to various
endogenous and exogenous processes. The endogenous
processes are generated by the internal forces of the
earth.
They are the tectonic processes like earthquakes,
deformation, volcanic eruptions, metamorphism and sea-
floor spreading. The exogenous processes are activated
by the geological agents acting on the surface like
running water, moving glaciers, blowing wind and
washing sea waves. (…Contd)
Introduction
5. MHRD
NME-ICT
In addition to these, there are some natural geomorphic
processes acting on the surface of the earth. They are
the weathering and mass-wasting processes. These two
processes are very active on the surface of the earth.
They are responsible for many morphological
modifications of rock bodies existing on land. Among
these, mass-wasting is a unique geomorphological
process destabilizing the surface rocks and soil mass.
Introduction
6. MHRD
NME-ICT
Gravity pulls the rocks, soils and debris on a downward
slope, naturally, without any chemical change.
This downward movement is called as mass -movement
or mass-wasting.
Landslides, mudflows and rockfalls are all belonging to
this category of geomorphic processes.
Moving Mass on the Earth’s surface
(…Contd)
7. MHRD
NME-ICT
Mass-wasting may lead to severe natural disasters by
affecting the life and building structures in different
places.
Understanding of mass-wasting will certainly help to
mitigate the impacts of these hazards and plan the
development activities.
Moving Mass on the Earth’s surface
(…Contd)
8. MHRD
NME-ICT
In this lesson, the following aspects of mass-wasting
are highlighted:
Mass-wasting and its causes
Types of mass-movements
Triggers of mass-wasting
Factors influencing mass-wasting
Importance of mass-movements.
Moving Mass on the Earth’s surface
9. MHRD
NME-ICT
The term mass-wasting is used for a broad category of
processes whereby the earth’s surface materials are
pulled down on a slope by the force of gravity.
Mass wasting is a geomorphic process by which soil,
regolith, and rock move down a slope under the force
of gravity.
It is also called as mass-movement.
Mass-wasting and its causes
(…Contd)
10. MHRD
NME-ICT
It happens on a standing rock body or regolith.
It is closely related to weathering, which is the
breakdown of minerals or rocks at or near Earth's
surface through physical, chemical, or biological
processes.
It is also related to erosion because the transport of
material is done through a variety of agents like wind
or flowing water.
Mass-wasting and its causes
11. MHRD
NME-ICT
There are two forces involved in a mass standing on a
slope.
One is the driving force and the other one is the
resisting force.
The standing mass has the driving force due to its weight.
The slope and substratum have the resisting force.
Forces for movements
(…Contd)
12. MHRD
NME-ICT
When the driving force exceeds the resisting force,
then the mass becomes unstable and moves down or
falls.
When the gravitational force acting on a slope
exceeds its resisting force, failure of slope occurs in
holding the mass.
Forces for movements
13. MHRD
NME-ICT
The slope material's strength and cohesion and the
amount of internal friction between material help in
maintaining the slope's stability.
These are collectively known as the slope's shear
strength.
The steepest angle that a cohesion less slope can
maintain the mass without losing its stability is known as
its angle of repose.
Slope materials
(…Contd)
14. MHRD
NME-ICT
When a slope possesses this angle, its shear strength
perfectly counterbalances the force of gravity acting
upon it and the mass will not leave.
When the angle of repose is more, with a little trigger
or disturbance, the mass moves down rapidly.
Slope materials
15. MHRD
NME-ICT
Mass wasting may occur at a very slow rate,
particularly in areas that are very dry or those areas
that receive sufficient rainfall such that vegetation has
stabilised the surface.
It may also occur at very high speed, such as in rock
slides or landslides, with disastrous impacts.
Slow rate
(…Contd)
16. MHRD
NME-ICT
Varieties of mass wasting happen based on the type of
mass involved, type of movement involved and the type
of effect they create on a region.
These movements are classified according to the speed
and force of the process, from extremely slow creep to
very rapid, dramatic slide or fall.
Slow rate
17. MHRD
NME-ICT
The factors that can change the potential of mass
wasting include:
1.change in the slope angle
2.weakening of the material by weathering
3.increased water content
4.changes in the vegetation cover and
5.overloading.
Factors responsible
18. MHRD
NME-ICT
Mass-wasting occurs both on terrestrial slopes and
submarine slopes. Inside the seas and oceans also such
mass-movements happen.
Mass-movement have also been observed in Mars,
Venus, and Jupiter's moon Io.
Examples of rapid mass wasting include landslides and
avalanches, which can be the cause of widespread death
and destruction when they occur in populated areas.
Terrestrial slopes
19. MHRD
NME-ICT
Water plays a typical role in mass-movements.
Water can increase or decrease the stability of a slope
depending on the amount present not only on the
overlying mass but also on the slope.
Water may help to create a slippery phase on the
slope.
Role of water
(…Contd)
20. MHRD
NME-ICT
Small amounts of water can strengthen soils because
the surface tension of water gives the soil a lot of
cohesion.
This allows the soil to resist erosion better than if it
were dry.
If too much water is present the water may act as a
lubricant, accelerating the erosion process and resulting
in different types of mass wasting like mudflows and
landslides.
Role of water
21. MHRD
NME-ICT
A good example of this is to think of a sand castle, which
may collapse at any time.
Water must be mixed with sand in order to form the
castle to keep its shape.
If too much water is added the sand washes away, if
enough water is not added, the sand falls and cannot
keep its shape.
Sand castle
22. MHRD
NME-ICT
Types of mass movement are distinguished based on
how the soil, regolith or rock moves down slope as a
whole.
The process involves two major factors as type of mass
and type of movement.
The type of mass involved may be bedrocks or soils.
The type of movement may be a fall, slide, flow or
creep.
Types of mass movements
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NME-ICT
Types of movement involved
Types of movementTypes of movement
involved involved
Type of mass involved Type of mass involved
Bedrock Soils
Falls Rock fall Soil fall
Slides
Slums, slides and
glides
Slums, slides and glides
Flows Fragment flow
Earth flow, debris flow,
mudflow
Complex Complex type of movements
24. MHRD
NME-ICT
In addition to these, sub-categories of mass-movements
are classified based on the type of movement involved as
1.Planar movement or
2.Rotational movement.
Sub - categories of Mass-movements
25. MHRD
NME-ICT
Types of mass wasting include creep, slides, flows, topples,
and falls, each with its own characteristic features, and
taking place over timescales from seconds to years.
The down-slope movement of material, whether it be
bedrock, regolith, or a mixture of these, is commonly
referred to as a landslide.
Under a complex situation, all of these processes
generally grade into one another, so classification of such
complex processes is very difficult.
Types of Mass wasting
27. MHRD
NME-ICT
Creep is a long term mass-wasting process on a
downhill.
In this process, the combination of small movements of
soil or rock occurs in different directions over time.
Creep is directed by gravity gradually downslope.
The steeper the slope, the faster the creep.
Creeps
(…Contd)
28. MHRD
NME-ICT
The creep makes trees and other shrubs bend and
curve to reach the sun light.
These often trigger landslides because the dirt
underneath is not very strong.
The trees most of the times die out because of lack of
water and sun, and these rarely happen in wet climates.
Creeps
(…Contd)
29. MHRD
NME-ICT
Caused by freezing and then thawing, or hot and then
cold temperature, it causes surface soils to move up
then down.
Creep happens at a rate that is not noticeable to the
naked eye, and it also happens in the tropical regions.
Creeps
30. MHRD
NME-ICT
Slides are sudden downhill movement of masses of rock
or sediment or soils.
Slides are also called Translational Slides, as they involve
only straight movement along a direction.
Rock slides and debris slides result when rocks or
debris slide down a pre-existing surface, such as a
bedding plane, foliation surface, or joint surface.
Slides
(…Contd)
31. MHRD
NME-ICT
Piles of talus are common at the base of a rock slide
or debris slide.
Slides differ from slumps in that there is no rotation
of the sliding rock mass along a curved surface.
Slides
32. MHRD
NME-ICT
Landslide is a general term used to describe the
downslope movement of soil, rock, and organic
materials under the effects of gravity and also the
landform that results from such movement.
Landslides can be classified into different types on the
basis of the type of movement and the type of material
involved.
The material in a landslide may be either a rock or soil
(or both).
Landslides
33. MHRD
NME-ICT
The term slump refers to a slipping of coherent rock
material along the curved surface of a decline.
Slumps are also called as Rotational Slides due to the
type of movement involved.
These are special category slides wherein the downward
rotation of rock or regolith occurs along a concave-
upward curved surface.
Slump
(…Contd)
34. MHRD
NME-ICT
The upper surface of each slump block remains
relatively undisturbed, as do the individual blocks.
Slumps leave arcuate scars or depressions on the hill
slope.
Slumps may be isolated or may occur in large
complexes covering thousands of square meters.
They often happen due to human activities.
Slump
(…Contd)
35. MHRD
NME-ICT
Slumps are common along the roads where slopes
have been over steepened during construction.
They are also common along the river banks and sea
coasts, where erosion has under-cut the slopes.
Heavy rains, tectonic disturbances, tremors and
earthquakes can also trigger slumps.
Slump
36. MHRD
NME-ICT
Movement of soil and regolith resembling like a fluid
behavior is called as a flow.
These include avalanches, mudflows, debris flows, earth
flow, lahars and sturzstroms.
Water, air and ice are often involved in enabling this fluid
like motion of the material.
Flows
37. MHRD
NME-ICT
Sediment flows occur when sufficient force is applied
to rocks and regolith that they begin to flow down
slope.
A sediment flow is a mixture of rock, and/or regolith
with some water or air.
They can be broken into two types depending on the
amount of water present as Slurry flows and granular
flows.
Sediment Flows
38. MHRD
NME-ICT
Slurry Flows- are sediment flows that contain between
about 20 and 40% water. As the water content
increases above 40%, the slurry flows grade into
streams. Slurry flows are considered as water-saturated
flows.
The Slurry Flows are further classified into:
Solifluction
Debris flows and
Mudflows.
Slurry Flows
39. MHRD
NME-ICT
Granular Flows - are sediment flows that contain
between 0 and 20% water. Granular flows are possible
with little or no water.
Fluid-like behavior is given to these flows by mixing
with air. Granular flows are not saturated with water.
Each of these classes of sediment flows can be further
subdivided on the basis of the velocity at which flowage
occurs.
Granular Flows
40. MHRD
NME-ICT
Solifluction is a flowage of soil mass at rates measured
on the order of centimeters per year of regolith
containing water.
Solifluction produces distinctive lobes on the hill slopes.
These occur in areas where the soil remains saturated
with water for long periods of time.
Solifluction
41. MHRD
NME-ICT
Debris Flows occur at higher velocities than solifluction.
The velocities may range between 1 meter/hr to 100
meters/hr.
It often results due to heavy rains causing saturation of
the soil and regolith with water.
They sometimes start with slumps and then flow
downhill forming lobes with an irregular surface
consisting of ridges and furrows.
Debris Flows
42. MHRD
NME-ICT
Mudflows are very different type of mass-movements.
These are a highly fluid, high velocity mixture of
sediment and water that has a consistency ranging
between soup-like and wet concrete.
They move at velocities greater than 1 km/hr and tend
to travel along valley floors.
Mudflows
(…Contd)
43. MHRD
NME-ICT
These usually result due to heavy rains in areas where
there is an abundance of unconsolidated sediment that
can be picked up by the streams.
Thus after a heavy rain streams can turn into mudflows
as they pick up more and more loose sediments on the
way.
Mudflows
(…Contd)
44. MHRD
NME-ICT
Mudflows can travel for long distances over gently
sloping stream beds.
Because of their high velocity and long distance of
travel they are potentially very dangerous types of
mass-movements.
Mudflows
(…Contd)
45. MHRD
NME-ICT
Mudflows can also result from volcanic eruptions
that cause melting of snow or ice on the slopes of
volcanoes, or draining of crater lakes on volcanoes.
Volcanic mudflows are often referred to as lahars.
Some lahars can be quite hot, if they are generated
as a result of eruptions of hot tephra.
Mudflows
46. MHRD
NME-ICT
Granular Flows are yet another type of mass-
movements.
Creep is a very slow, usually continuous movement of
regolith down slope.
Creep occurs on almost all slopes, but the rates vary.
Evidence for creep is often seen in bent trees, offsets in
roads and fences, and inclined utility poles.
Granular Flows
47. MHRD
NME-ICT
Earth flows are usually associated with heavy rains
and move at velocities between several cm/yr and
100s of m/day.
They usually remain active for long periods of time.
They generally tend to be narrow tongue-like
features that begin at a scarp or small cliff.
Earth flows
48. MHRD
NME-ICT
Grain Flows are usually formed in relatively dry material,
such as a sand dune, on a steep slope.
A small disturbance sends the dry unconsolidated grains
moving rapidly down slope.
Grain flows
49. MHRD
NME-ICT
Debris Avalanches are yet another type of mass-
movement.
These are very high velocity flows of large volume
mixtures of rock and regolith that result from
complete collapse of a mountainous slope.
They move down slope and then can travel for
considerable distances along relatively gentle slopes.
They are often triggered by earthquakes and volcanic
eruptions.
Debris Avalanches
50. MHRD
NME-ICT
Topple are unique instances when huge blocks of rock
pivot and fall away from a slope.
Topple failures involve the forward rotation and
movement of a mass of rock, earth or debris out of a
slope.
This kind of slope failure generally occurs around an
axis (or point) at or near the base of the block of rock.
Topple
(…Contd)
51. MHRD
NME-ICT
A topple often results in the formation of debris or a
debris cone at the base of the slope; this pile is called a
talus cone.
New talus cones don't have any plants growing on
them. Old talus cones can have weeds and even trees
on them.
Topple
52. MHRD
NME-ICT
Falls are major categories of mass-wasting.
Falls are further categorized into two types as rock falls
or debris falls.
Rock falls occur when a piece of rock on a steep slope
becomes dislodged and falls down the slope.
Debris falls are similar, except they involve a mixture of
soil, regolith, vegetation, and rocks.
Falls
(…Contd)
53. MHRD
NME-ICT
A rock fall may be a single rock or a mass of rocks, and
the falling rocks can dislodge other rocks as they collide
with the cliff.
A fall, including rock fall, is where regolith cascades
down a slope, but is not of sufficient volume or
viscosity to behave as a flow.
Falls are promoted in rocks which are characterized by
presence of vertical cracks or joints.
Falls
(…Contd)
54. MHRD
NME-ICT
Falls also occur due the undercutting action of water as
well as undercutting of waves near coastal regions.
They usually occur at very steep slopes such as a cliff or
escarpments.
The rock material may be loosened by tremors or
earthquakes, rain, plant-root wedging and expanding
ice.
Falls
55. MHRD
NME-ICT
The accumulation of rock material that has fallen down
will reside at the base of the structure.
It is known as talus. Because this process involves the
free fall of material, falls commonly occur where there
are steep cliffs.
At the base of most cliffs we get the accumulation of
fallen material called as talus.
Talus
57. MHRD
NME-ICT
Mass-wasting is a geomorphic process happening due to a
triggering mechanism.
Soil and regolith remain on a hillslope only while the
gravitational forces are unable to overcome the frictional
forces keeping the material in place.
They are stable and the factor is called as Slope stability.
Other Factors that reduce the frictional resistance
relative to the downslope forces initiate the mass –
movement.
Triggers of mass wasting
(…Contd)
58. MHRD
NME-ICT
They are:
seismic shaking
increased overburden from structures
increased soil moisture and infiltration of water
reduction of roots holding the soil to bedrock
undercutting of the slope by excavation or erosion
weathering by frost heave and
bioturbation.
Triggers of mass wasting
59. MHRD
NME-ICT
The most common triggering mechanisms are strong
vibrations from earthquakes and excessive amounts of
water from a winter snow melt or a heavy rainstorm.
Volcanic eruptions, explosions, and even loud claps of
thunder may also be enough to trigger a landslide if the
slope is sufficiently unstable.
Tectonic causes
(…Contd)
60. MHRD
NME-ICT
Many avalanches, which are rapid movements of snow
and ice down steep mountain slopes, are triggered by
the sound of a loud gunshot, a sonic boom from a
supersonic airplane, or in rare cases, even a person's
shout.
Tectonic causes
61. MHRD
NME-ICT
Mass wasting is fully related to gravity. Creep, slides,
and flows all of these processes share one thing in
common, namely, that they are caused by the incessant
downward pull of gravity, which moves all loose slope
material downwards.
Gravity-driven mass wasting processes are a subset of
larger set of processes that transport weathered and
unweathered earth materials.
Role of gravity
(…Contd)
62. MHRD
NME-ICT
The trigger for mass-movement may come due to
micro-seismic activities, tectonic dislocations and
shaking of the ground by neo-tectonic forces.
Such incidences may be common in places where there
is an active fault on a hill slope.
Role of gravity
63. MHRD
NME-ICT
Active faults will always create the trigger. Even if the
movement is very small, the effect will be more.
Huge volume of mass existing on a hill slope will be moved
down within a fraction of a second after trigger. It is the
most dangerous situation which is not known and
unpredictable by any normal methods.
Continuous seismological observations using seismometers
and earth stations may help in monitoring the situations.
Active faults
64. MHRD
NME-ICT
The second triggering mechanism is the increase in the
weight by a overburden.
It may be a new structure created on the slope
involving a heavy weight.
Sometimes cutting the slopes for laying roads and
dumping the excavated mass on another slope may
increase the weight.
Over weight
(…Contd)
65. MHRD
NME-ICT
Overloading is almost always the result of human
activity and typically results from dumping, filling, or
piling up of material.
The additional weight created by overloading increases
the water pressure within the material, which in turn
decreases its shear strength, thereby weakening the
slope material.
Over weight
66. MHRD
NME-ICT
Water has hydraulic pressure. When water enters into
the soil, it fills the pore spaces of soils and weathered
zones.
Due to this accumulation of water molecules on the
regolith and soils, the weight increases.
It also starts moving down through the pores.
Role of water
(…Contd)
67. MHRD
NME-ICT
Water can create slippery phases between the bedrock
and the overburden.
The amount of water in rock or soil influences slope
stability.
Large quantities of water from melting snow or heavy
storms greatly increase the likelihood of slope failure.
Role of water
(…Contd)
68. MHRD
NME-ICT
The additional weight that water adds to a slope can be
enough to cause mass movement.
The mass-movement may occur after any slow and
steady rainfall.
Throughout the world, the water-induced mass-
movements are more in number. Rainfall is the major
triggering mechanism.
Role of water
69. MHRD
NME-ICT
Vegetation affects slope stability in several ways. By
absorbing the water from a rainstorm, vegetation
decreases water saturation of a slope's material and
the resultant loss of shear strength that frequently
leads to mass wasting.
Role of Vegetation
(…Contd)
70. MHRD
NME-ICT
The removal of vegetation by either natural or human
activity is a major cause of many mass movements.
Removal of trees may affect the binding mechanism
between overburden and the bedrock.
Roots of trees have the ability to keep the mass in-tact
on a slope.
Role of vegetation
71. MHRD
NME-ICT
Growth of trees is a slow and steady natural process
and hence it never triggers a mass-movement, but does
the opposite.
It binds the mass with the bedrock. Due to incidences
like forest fires, such unexpected conditions arise.
Erosion is a major triggering mechanism. It forcefully
removes the mass down a slope.
Growth of trees
(…Contd)
72. MHRD
NME-ICT
Sometimes, the under-cutting action of flowing water
along a slope, may move the surrounding rock bodies
and regolith downwards.
Similarly, cutting of slopes for highways or
constructions may also lead to this situation.
Weathering is another process enacting mass-
movements.
Growth of trees
(…Contd)
73. MHRD
NME-ICT
Weathering has the ability to disintegrate the overburden
and decompose the mass both physically and chemically.
These physical disintegration processes may loosen the
mass.
Once the compactness is disturbed, then the other factors
like water saturation takes a lead role to move the mass.
Though weathering is a slow process, it induces the mass
to move even on a gentle slope.
Growth of trees
74. MHRD
NME-ICT
Root wedging is a different process.
Through cracks and fractures, the roots penetrate and
destabilize the rock block below.
Such actions may encourage rock falls and debris falls.
Root wedging
75. MHRD
NME-ICT
Bioturbation is yet another factor for mass-wasting.
The role played by microorganisms may loosen the
compactness of the mass on a slope.
Bioturbation
76. MHRD
NME-ICT
When the gravitational force acting on a slope exceeds
its resisting force, slope failure (mass wasting) occurs.
The resisting forces helping to maintain slope stability
include the slope material's strength and cohesion, the
amount of internal friction between grains, and any
external support of the slope.
These factors collectively define a slope's shear
strength.
Slope failure
77. MHRD
NME-ICT
Opposing a slope's shear strength is the force of gravity.
Gravity operates vertically but has a component acting
parallel to slope, thereby causing instability.
All slopes are in a state of dynamic equilibrium, which
means that they are constantly adjusting to new
conditions.
Slope angle
(…Contd)
78. MHRD
NME-ICT
The greater a slope's angle, the greater the chance for
mass wasting.
A number of processes can over steepen a slope. One
of the most common is undercutting by stream or
wave action.
This removes the slope's base, increases the slope
angle, and thereby increases the gravitational force
acting parallel to the slope.
Slope angle
(…Contd)
79. MHRD
NME-ICT
Excavations for road cuts and hillside building sites are
another major cause of slope failure.
Grading the slope too steeply, or cutting into its side,
increases the stress in rock or soil until it is no longer
strong enough to remain at the steeper angle and
mass wasting ensues.
Slope angle
80. MHRD
NME-ICT
Mass wasting is more likely to occur in loose or poorly
consolidated slope material than in solid bedrock.
As soon as solid rock is exposed at the Earth's surface,
weathering begins to disintegrate and decompose it,
thereby reducing its shear strength and increasing its
susceptibility to mass wasting.
The deeper the weathering zone extends, the greater the
likelihood of some type of mass movement.
Weathering and Climate
81. MHRD
NME-ICT
Geology and Slope Stability are to be considered.
The relationship between topography and the geology
of an area is important in determining slope stability.
If the rocks underlying a slope dip in the same direction
as the slope, mass wasting is more likely to occur than
if the rocks are horizontal or dip in the opposite
direction.
Geology and Slope Stability
82. MHRD
NME-ICT
Mass-wasting is an important part of the erosional
process, as it moves material from higher elevations
to lower elevations where transporting agents like
streams and glaciers can then pick up the material
and move it to even lower elevations.
Importance of mass movements
(…Contd)
83. MHRD
NME-ICT
Mass-wasting processes are occurring continuously on
all slopes; some act very slowly, others occur very
suddenly, often with disastrous results.
Any perceptible down slope movement of rock or
regolith is often referred to in general terms as a
landslide.
Importance of mass movements
(…Contd)
84. MHRD
NME-ICT
Landslides, however, can be classified in a much more
detailed way that reflects the mechanisms responsible for
the movement and the velocity at which the movement
occurs.
As human populations expand and occupy more and more
of the land surface, mass-wasting processes become more
likely to affect humans.
The table below shows the impact of mass-wasting
processes on human life over the last century.
Importance of mass movements
85. MHRD
NME-ICT
Rapid mass wasting events such as massive landslides or
debris flows are typically triggered by events that
destabilize material that resides on steep slopes.
Such events include earthquakes, volcanic eruptions, rain
or melting snow, and poorly planned landscape
alterations by humans.
The road cuts or developments that require the
removal of material at the bases of slopes may lead to
slope failures.
Conclusion
(…Contd)
86. MHRD
NME-ICT
The impacts of mass-wasting could be seen only on the hill
stations and roads along the Ghat sections. Landslides are
serious hazards along these roads.
Frequent maintenance of these roads becomes an
expensive affair for any government.
Knowledge about the relationships between local geology
and mass-wasting processes can lead to better planning of
a region that can reduce the vulnerability of such natural
hazards.
Conclusion