Environment Geology
Environment Geology
The creation of heat island; Materials like concrete, asphalt, bricks etc
absorb and reflect energy differently than vegetation and soil.Cities remain
warm in the night when the countryside has already cooled.
Erosion and other changes in land quality; Rapid development can result
in very high levels of erosion and sedimentation in river channels
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Flow of Water into Streams; Natural vegetation and undisturbed soil are
replaced with concrete, asphalt, brick, and other impermeable surfaces. This
means that, when it rains, water is less likely to be absorbed into the ground
and, instead, flows directly into river channels.
Flow of Water through Streams; Higher, faster peak flows change streams
channels that have evolved over centuries under natural conditions. Flooding can
be a major problem as cities grow and stream channels attempt to keep up with
these changes
Degraded Water Quality; The water quality has degraded with time due
to urbanization that ultimately leads to increased sedimentation there by also
increasing the pollutant in run-off.
Creation of New Habitats; New habitats are also created for some native
and non-native species. Cities also create habitats for some species considered
pests, such as pigeons, sparrows, rats, mice, flies and mosquitoes. Urbanization
has, for example, eliminated many bat colonies in caves, but has provided sites
such as bridges for these species to nest.
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The expansion of housing developments, businesses, industry, infrastructure and
agriculture all necessitated by an unprecedented population explosion over recent
years accounts for humans modifying over 50 percent of the earth’s topsoil It can
also simply be degradation from transforming the land by clearing it so that
beneficial organisms can no longer provide services supporting growth and
protect it from further erosion. This human activity appears more than a little
reckless when considering that it takes 500 years to naturally produce 2.5 cm
topsoil in ideal conditions, absent of ecological changes.
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fish eat more of the tinier prey, so that the meal can be quite toxic by the time the
fish makes it to our dinner plate.It is not just direct pollution of toxic chemicals
that can cause these problems. Nor is the problem confined to abandoned lots or
illegal dumpsites
Deforestation
In the Amazon rain forest in Brazil, an area the size of a football field is clear-cut
by loggers every second [9]. The removal of plant cover not only eliminates
wildlife habitats and food for wildlife, but it also degrades the soil by leaving it
barren and without the roots of plants to hold it in place, vulnerable to erosion.
Agriculture
The world population increase and increased demand for a food supply is causing
forests and grasslands to be converted to farmland. Natural vegetation has deep
roots that hold the soil in its place. Many of the replacement plants, like cotton,
coffee, wheat and soybeans do not have deep roots and allow soil erosion. This
means that flooding is worsened as the land no longer has the ability to absorb
excess rainfall.
Industry
Industrial activities often release toxic and material wastes onto the land or into
the atmosphere where they settle onto the land. While most developed countries
now regulate land dumping and emissions, the regulations balance the costs to
industry and do not necessarily adequately safeguard the integrity of our
biosphere or more specifically, human health.
Mining
Forty percent of the world’s mines are strip mines. This is where the earth is
either scraped or blasted to get to the mineral seams. The balance of mining is
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done underground, where pillars support the earth while work is performed
underground and at the end, removed or simply left to collapse. Strip mines
obviously remove the topsoil and contribute to erosion. In many developed
countries, regulations now require land reclamation when the project is over.
Urbanization
Urbanization contributes to land degradation in a number of ways, including the
negative impact of construction on soil, the displacement and destruction of
animal and species habitat and the greater demand for waste disposal, generally
meaning larger landfills removed from the city.
We must be diligent in insuring that tough laws are enacted that require the very
best pollution control technologies imaginable, pass strict pollution emission
standards and make sure they are enforced. This applies too to regulations
governing mining and industrial waste and disposal of solid and hazardous waste.
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being involved. Only by possessing adequate knowledge we can focus on the
necessary prevention of land and global pollution overall .
Greenhouse effect
The greenhouse effect is the process by which radiation from a planet's
atmosphere warms the planet's surface to a temperature above what it would be
without this atmosphere
Earth’s natural greenhouse effect is critical to supporting life, and initially was a
precursor to life moving out of the ocean onto land. Human activities, however,
mainly the burning of fossil fuels and clearcutting of forests, have accelerated the
greenhouse effect and caused global warming.
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Atmosphere as warming up is the simplest way for the climate to get rid of the
extra energy. However, a small rise in temperature will induce many other
changes, for example, cloud cover and wind patterns. Some of these changes may
act to enhance the warming (positive feedbacks), others to counteract it
(negative feedbacks). Using complex climate models, the "Intergovernmental
Panel on Climate Change" in their third assessment report has forecast that
global mean surface temperature will rise by 1.4℃ to 5.8℃ by the end of 2100.
This projection takes into account the effects of aerosols which tend to cool the
climate as well as the delaying effects of the oceans which have a large thermal
capacity. However, there are many uncertainties associated with this
projection such as future emission rates of greenhouse gases, climate
feedbacks, and the size of the ocean delay
How are humans impacting the greenhouse effect?
Human activities are changing Earth's natural greenhouse effect. Burning fossil
fuels like coal and oil puts more carbon dioxide into our atmosphere. NASA has
observed increases in the amount of carbon dioxide and some other greenhouse
gases in our atmosphere. Too much of these greenhouse gases can cause Earth's
atmosphere to trap more and more heat. This causes Earth to warm up .
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constant loud music in or near commercial venues
industrial sounds like fans, generators, compressor, mills
train stations traffic
household sounds, from the television set to music playing on the stereo or
computer, vacuum cleaners, fans and coolers, washing machines,
dishwashers, lawnmowers etc.
events involving fireworks, firecrackers, loudspeakers etc.
conflicts generate noise pollution through explosions, gunfire etc. The
dysfunctions, in this case, are likely caused by the conflict and insecurity
and less by the noise pollution in itself, although that compounds stress
levels too.
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Sleep disturbances are usually caused by constant air or land traffic at
night, and they are a serious condition in that they can affect everyday
performance and lead to serious diseases
DISASTER
A catastrophe, mishap, calamity or grave occurrence in any area, arising from
natural or manmade causes, or by accident or negligence which results in
substantial loss of life or human suffering or damage to and destruction of,
property or damage to and degradation of , environment, and is of such a nature or
magnitude as to be beyond the coping capacity of the community of the affected
area.
DISASTER MANAGEMENT
A continuous and integrated process of planning, organising, coordinating and
implementing measures which are necessary or expedient for prevention of danger
or threat of any disaster, mitigation or reduction of risk of any disaster or its
severity or consequences, capacity building, preparedness to deal with any disaster,
prompt response to any threatening disaster situation or disaster, assessing the
severity or magnitude of effects of any disaster, evacuation, rescue and relief, and
rehabilitation and reconstruction.
EARTHQUAKES
Earthquake is one of the most destructive natural hazard. They may occur at any
time of the year, day or night, with sudden impact and little warning. They can
destroy buildings and infrastructure in seconds, killing or injuring the inhabitants.
Earthquakes not only destroy the entire habitation but may de-stabilize the
government, economy and social structure of the country.
Ground Shaking
Ground shaking is a term used to describe the vibration of the ground during
an earthquake. Ground shaking is caused by body waves and surface waves. As a
generalization, the severity of ground shaking increases as magnitude increases and
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decreases as distance from the causative fault increases. Although the physics of
seismic waves is complex, ground shaking can be explained in terms of body
waves, compressional, or P, and shear, or S, and surface waves, Rayleigh and
Love.
Surface Faulting
Surface faulting is the differential movement of the two sides of a fracture at the
Earth's surface and can be strike-slip, normal, and reverse (or thrust).
Combinations of the strike-slip type and the other two types of faulting can be
found. Although displacements of these kinds can result from landslides and other
shallow processes, surface faulting, as the term is used here, applies to differential
movements caused by deep-seated forces in the Earth, the slow movement of
sedimentary deposits toward the Gulf of Mexico, and faulting associated with salt
domes.
Landslides
Past experience has shown that several types of landslides take place in
conjunction with earthquakes. The most abundant types of earthquake induced
landslides are rock falls and slides of rock fragments that form on steep slopes.
Shallow debris slides forming on steep slopes and soil and rock slumps and block
slides forming on moderate to steep slopes also take place, but they are less
abundant. Reactivation of dormant slumps or block slides by earthquakes is rare.
Tsunamis
Tsunamis are water waves that are caused by sudden vertical movement of a large
area of the sea floor during an undersea earthquake. Tsunamis are often called tidal
waves, but this term is a misnomer. Unlike regular ocean tides, tsunamis are not
caused by the tidal action of the Moon and Sun. The height of a tsunami in the
deep ocean is typically about 1 foot, but the distance between wave crests can be
very long, more than 60 miles. The speed at which the tsunami travels decreases as
water depth decreases. In the mid-Pacific, where the water depths reach 3 miles,
tsunami speeds can be more than 430 miles per hour. As tsunamis reach shallow
water around islands or on a continental shelf; the height of the waves increases
many times, sometimes reaching as much as 80 feet. The great distance between
wave crests prevents tsunamis from dissipating energy as a breaking surf; instead,
tsunamis cause water levels to rise rapidly along coast lines.
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EARTHQUAKE HAZARDS IN INDIA
India has had a long history of earthquake occurrences. About 65% of the total area
of the country is vulnerable to seismic damage of buildings in varying degrees. The
most vulnerable areas, according to the present seismic zone map of India, are
located in the Himalayan and sub-Himalayan regions, Kutch and the Andaman and
Nicobar Islands. Depending on varying degrees of seism city, the entire country
can be divided into the following seismic regions:
Kashmir and Western Himalayas - Covers the states of Jammu and Kashmir,
Himachal Pradesh and sub-mountainous areas of Punjab
Central Himalayas - Includes the mountain and sub-mountain regions of
Uttar Pradesh and the sub-mountainous parts of Punjab
North-east India - Comprises the whole of Indian territory to the east of
north Bengal
Indo-Gangetic basin and Rajasthan - This region comprises of Rajasthan,
plains of Punjab, Haryana, Uttar Pradesh and West Bengal
Cambay and Rann of Kutch
Peninsular India, including the islands of Lakshwadeep
The Andaman and Nicobar Islands
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various roles, is considered essential for immediate and effective response after
an earthquake occurrence. The major action points are highlighted in the
following paragraphs.
TSUNAMI
What is a tsunami?
A tsunami is a series of waves with a long wavelength and period (time between
crests). Time between crests of the wave can vary from a few minutes to over an
hour. Tsunamis are often incorrectly called tidal waves; they have no relation to
the daily ocean tides.
Tsunamis and earthquakes happen after centuries of energy build up within the
earth. A tsunami (in Japanese ‘tsu’ means harbor and ‘nami’ means wave) is a
series of water waves caused by the displacement of a large volume of a body of
water, usually an ocean. In the Tamil language it is known as “Aazhi Peralai”.
Seismicity generated tsunamis are result of abrupt deformation of sea floor
resulting vertical displacement of the overlying water. Earthquakes occurring
beneath the sea level, the water above the reformed area is displaced from its
equilibrium position. The release of energy produces tsunami waves which have
small amplitude but a very long wavelength (often hundreds of kilometer long). It
may be caused by non-seismic event also such as a landslide or impact of a meteor.
Some Historical Tsunamis Prior to the Tsunami of 26 December 2004, the most
destructive Pacific-wide Tsunami of recent history was generated along the coast
of Chile on May 22, 1960. No accurate assessment of the damage and deaths
attributable to this Tsunami along the coast of Chile can be given; however, all
coastal towns between the 36th and 44th S (latitude) parallels either were
destroyed or heavily damaged by the action of the waves and the quake. The
combined Tsunami and earthquake toll included 2,000 killed, 3000 injured
2,000,000 homeless and $550 million damages. Off Corral, the waves were
estimated to be 20.4 meters (67 feet) high. The Tsunami caused 61 deaths in
Hawaii, 20 in the Philippines, and 100 or more in Japan. Estimated damages were
$50 million in Japan, $24 million Hawaii and several millions along the west coast
of the United States and Canada. Wave heights varied from slight oscillations in
some areas to range of 12.2 meters (40 feet) at Pitcairn Islands; 10.7 meters (35
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feet) at Hilo, Hawaii and 6.1 meters (20 feet) at various places in Japan. The
hydrographic survey in Japan after the great Kwato earthquake of September 1,
1923 showed that vertical displacements of the order of 100 meters had occurred
over a large area of sea floor. Tsunamis are very common in the Pacific Ocean
because it is surrounded on all sides by a seismically active belt. In the Hawain
Islands, Tsunamis approach from all directions, namely, from Japan, the Aleutian
Islands and from South America. Tsunamis in India The Indian coastal belt has not
recorded many severe tsunamis in the past. Waves accompanying earthquake
activity have been reported over the North Bay of Bengal. During an earthquake in
1881 which had its epicenter near the Andamans in the Bay of Bengal, tsunamis
were reported. The earthquake of 1941 in Bay of Bengal caused some damage in
Andaman region. This was unusual because most Tsunamis are generated by
shocks which occur at or near the flanks of continental slopes. During the
earthquakes of 1819 and 1845 near the Rann of Kutch, there were rapid
movements of water into the sea. There is no mention of waves resulting from
these earthquakes along the coast adjacent to the Arabian sea, and it is unlikely that
Tsunamis were generated. Further west, in the Persian Gulf, the 1945 Mekran
earthquake (magnitude 8.1) generated Tsunami of 12 to 15 metres height. This
caused a huge deluge, with considerable loss of life and property at Ormara and
Pasi. The estimated height of Tsunami at Gulf of Kutchch was 15m but no report
of damage is available. The estimated height of waves was about 2 metres at
Mumbai, where boats were taken away from their moorings and casualties
occurred. A list showing the Tsunami that affected Indian coast in the past is given
in Table-3.2. The information given in the Table for the first three events is
sketchy and authenticity cannot be confirmed except the Tsunami of 26th
December 2004. Above facts indicate the coastal region of Gujarat is vulnerable to
Tsunamis from great earthquakes in Mekran coast. Earthquake of magnitude 7 or
more may be dangerous. It may be noted that all earthquake do not generate
Tsunami.
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effective action on the ground is a longer project. Sound strategies and careful
work right down to community level will be needed to make sure that projects such
as the early warning system actually do make people safer. Planners and managers
of tsunami responses should consider the following suggestions
COASTAL EROSION
Coastal erosion is a common problem faced in almost all coastal areas. Only the
magnitude and nature of erosion changes from place to place. Along the Karnataka
coast much of the erosion observed is only seasonal in nature, that is, beach gets
eroded during monsoon and regains its original profile during fair weather season.
Only in a few pockets, erosion of permanent nature has been observed (KREC
Study Team, 1994). To understand the process ofcoastal erosion one should know
about the beach profiles.
Beach profile changes frequently in response to winds, waves and tides. Profiles
are also affected by Civil Engineering activities in and along the shore which
influence the long shore transport ofsand. The most notable rapid arrangement of a
profile is by storm waves. During monsoon season because of high wave activity
beach gets eroded due to off-shore movement of sediments. This profile is called
storm profile. During fair weather season because of swell wave activity, beach
regains its original profile by the on-shore movement ofsediments. Fig 2.1 shows
the storm and swell profiles.
1. Geological factors
3. Waves
5. Tides
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6. Off-shore relief
7. Sand mining.
Geological Factors
In geologically old areas the coastline would have achieved a state of equilibrium.
In contrast, in geologically younger areas, there will be readjustment processes and
hence erosion or deposition is felt predominantly. The West coast ofIndia is
geologically younger and has not yet attained an equilibrium condition. Hence it is
prone to minor adjustments (erosion)
Sea level changes may be due to eustatic sea level change or due to the shifting
ofshoreline because oflocal tectonic movements. Eustatic sea level rise contributes
to the process of erosion at a slow but gradual rate. It has been estimated that the
present day sea level rise is at a rate of 1.2 mm/year due to deglaciation and with
every millimetre rise in the sea level 1 to 1.5 meters ofland gets submerged (Bruun,
1962, 1990). As a result of this, the wave breaker zone and shoreline move
landwards
Waves
1. Steep waves cause the beach erosion by taking away the material.
Due to this wave orthogonals may converge or diverge on the beach. At places of
divergence, a relatively calm water exists and gradual deposition takes place. At
places of convergence, energy gets concentrated and erosion occurs. It also
depends on grain size, wave steepness and beach slope.
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Tides
Tides increase the zone over which destructive waves can erode the beach. The
high tide prevents the premature breaking ofthe waves on the off-shore sand bars
which dissipate some oftheir energy at that location. So the waves break closer to
the shore which is responsible for eroding the beach material. Hence, places with
high tidal range are more susceptible to erosion.
Off-shore
Relief Off-shore reliefaffects wave refraction and diffraction pattern ,thus the
energy received by a section of the beach may be different. In case of mudbanks
the shoreward side ofthe sea will be calm and traps the littoral material. The
downdrift side due to the lack oflittoral material starts eroding. In Karnataka coast
there is no mudbank formation and hence the erosion observed in this area may be
attributed to other factors.
The major river mouths along the D. K. Coast, as one moves from the South to the
North are the Netravathi - Gurpurrivers near Mangalore, Pavanje - Mulki rivers
near Mulki and Udiyavara river near Malpe. These river mouths, particularly sand
spits on either side show strong tendencies ofmigration. These movements do not
follow any regular pattern. Some ofthese sand spits ofunconsolidated sand extend
for long distances with river on one side and the sea on the other side. These long
and narrow sand spits are highly vulnerable areas since they consits ofsand which
can be easily worked by waters ofboth the sea and the river. The KREC Study
Team (1994) concludes that the beaches in these places are more vulnerable to
erosion due to the high water table caused by the flood flows in the adjoining rivers
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erosion strategies refer to temporary options of slowing the effects of erosion.
These options, including Sandbag and beach nourishment, are not intended to be
long term solutions or permanent solutions
FLOODS
A flood is an overflow of a large amount of water beyond its normal limits,
especially over what is normally dry land.Flooding may occur as an overflow of
water from water bodies, such as a river , lake, or ocean, in which the water
overtops or breaks leeves , resulting in some of that water escaping its usual
boundaries
Causes of Floods
Floods are caused by many factors: heavy precipitation, severe winds over water,
unusual high tides, tsunamis, or failure of dams, levels, retention ponds, or other
structures that contained the water. Periodic floods occur on many rivers, forming
a surrounding region known as the flood plain. During times of rain or snow, some
of the water is retained in ponds or soil, some is absorbed by grass and vegetation,
some evaporates, and the rest travels over the land as surface runoff. Floods occur
when ponds, lakes, riverbeds, soil, and vegetation cannot absorb all the water.
Water then runs off the land in quantities that cannot be carried within stream
channels or retained in natural ponds, lakes, and man-made reservoirs. About 30
percent of all precipitation is in the form of runoff small and that amount might be
increased by water from melting snow. River flooding is often caused by heavy
rain, sometimes increased by melting snow. Aflood that rises rapidly, with little or
no advance warning, is called a flash flood. Flash floods usually result from intense
rainfall over a relatively small area, or if the area was already saturated from
previous precipitation.
Effects of Floods
Flooding has many impacts. It damages property and endangers the lives of
humans and other species. Rapid water runoff causes soil erosion and concomitant
sediment deposition elsewhere (such as further downstream or down a coast). The
spawning grounds for fish and other wildlife habitats can become polluted or
completely destroyed. Some prolonged high floods can delay traffic in areas which
lack elevated roadways. Floods can interfere with drainage and economic use of
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lands, such as interfering with farming. Structural damage can occur in bridge
abutments, bank lines, sewer lines, and other structures within floodways.
Waterway navigation and hydroelectric power are often impaired. Financial losses
due to floods are typically millions of dollars each year.
(iv) ensuring the incorporation of flood resistant features in the design and
construction of new structures in the flood prone areas; (v) drawing up time-bound
plans for the flood proofing of strategic and public utility structures in flood prone
areas
(vi) improving the awareness and preparedness of all stakeholders in the flood
prone areas
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Landslides
A landslide is the rapid mass movement of soil, mud and/or rocks downhill due to
the pull of gravity. Landslides are very common and occur in a variety of forms.
Land may topple off in a big chunk, or slip down in bits. Landslide may be
composed of mud or may contain rocks and other debris. Most landslides occur
gradually, but some may be sudden.
Deforestation is the removal or cutting down of trees and other types of vegetation
from the land. The firm roots of the trees also help to keep the soil in place, even
when it absorbs water, thus diminishing the effects that gravity has on the soil. It is
when these trees are removed that the bare and exposed soil is left defenceless
against the pulling force of gravity when saturated since trees help to keep soil
firmly in place. Soil movement takes place more easily and rapidly resulting in
deadly landslides.
Quarrying or rock mining refers to the cutting away or excavation of hilly or
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mountainous areas so that rocks and minerals can be extracted from the land.
Quarrying is rampant in the Northern Range and results in the land being left
devoid of trees and vegetation. Without trees to hold the soil in place, soil
movement occurs easily and rapidly.
Mitigation of Landslides
Frequency of landslide hazards and type of human activity as well as location
determine impact
• Land use policies and regulations should also be in place in areas prone to
landslides
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Man made hazards
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4) Fukushima Meltdown, Japan:
5) Global Warming, Third Planet from the Sun:
Mass wasting
Mass wasting, also known as slope movement or mass movement, is
the geomorphic process by which soil, sand, regolith, and rock move
downslope typically as a solid, continuous or discontinuous mass,
largely under the force of gravity, frequently with characteristics of a
flow as in debris flows and mudflows.[1] 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
hundreds of years.
When the gravitational force acting on a slope exceeds its resisting
force, slope failure (mass wasting) occurs. The slope material's strength
and cohesion and the amount of internal friction within the material help
maintain the slope's stability and are known collectively as the
slope's shear strength. The steepest angle that a cohesionless slope can
maintain without losing its stability is known as its angle of repose.
When a slope made of loose material possesses this angle, its shear
strength counterbalances the force of gravity acting upon it.
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 stabilized the surface. It may also occur at very high
speed, such as in rockslides or landslides, with disastrous consequences,
both immediate and delayed, e.g., resulting from the formation
of landslide dams. Factors that change the potential of mass wasting
include: change in slope angle, weakening of material by weathering,
increased water content; changes in vegetation cover, and overloading.
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Role of water
Water can increase or decrease the stability of a slope depending on the
amount present. Small amounts of water can strengthen soils because
the surface tension of water increases soil cohesion. This allows the soil
to resist erosion better than if it were dry. If too much water is present
the water may act to increase the pore pressure, reducing friction, and
accelerating the erosion process and resulting in different types of mass
wasting (i.e. mudflows, landslides, etc.). A good example of this is to
think of a sand castle. Water must be mixed with sand for the castle to
keep its shape. If too much water is added the sand washes away, if not
enough water is added the sand falls and cannot keep its shape. Water
also increases the mass of the soil, this is important because an increase
in mass means that there will be an increase in velocity if mass wasting
is triggered. Saturated water, however, eases the process of mass wasting
in that the rock and soil debris are easily washed down-slope.
Creep
Soil creep is a slow and long term mass movement. The combination of small movements of soil or rock in
different directions over time is directed by gravity gradually downslope. The steeper the slope, the faster the
creep. The creep makes trees and shrubs curve to maintain their perpendicularity, and they can trigger
landslides if they lose their root footing. The surface soil can migrate under the influence of cycles of freezing
and thawing, or hot and cold temperatures, inching its way towards the bottom of the slope forming terracettes.
Landslides are often preceded by soil creep accompanied with soil sloughing — loose soil that falls and
accumulates at the base of the steepest creep sections. [2]
Landslide
A landslide, also called a landslip, is a slow or rapid movement of a
large mass of earth and rocks down a hill or a mountainside. Little or no
flowage of the materials occurs on a given slope until heavy rain and
resultant lubrication by the same rainwater facilitate the movement of
the materials, causing a landslide to occur.
In particular, if the main feature of the movement is a slide along a
planar or curved surface, the landslide is termed slump, earth slide,
debris slide or rock slide, depending on the prevailing material.
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Movement of soil and regolith that more resembles fluid behaviour is
called a flow. These include avalanches, mudflows, debris flows, earth
flow, lahars and sturzstroms. Water, air and ice are often involved in
enabling fluid-like motion of the material.
A fall, including rockfall and debris fall occurs 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 the
presence of vertical cracks. Falls can also result from undercutting by
running water as well as by waves. They usually occur at very steep
slopes such as a cliff face. The rock material may be loosened by
earthquakes, rain, plant-root wedging and expanding ice, among other
things. The accumulation of rock material that has fallen and resides at
the base of the structure is known as talus.
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What is the environmental impact of Dams?
Habitat fragmentation: Unless specifically engineered to allow fish to pass
through them, dams present a barrier to fish that need to migrate to spawn and
reproduce downstream and upstream along a river. This not only impacts the
populations of the fish themselves, but it can negatively impact other species in
the food chain that either eat that fish or are preyed upon by that fish.
Flooding and the destruction of surrounding habitat: Dammed rivers create a
reservoir upstream from the dam, which spills out into the surrounding
environments and floods ecosystems and habitats that once existed there. Such
flooding can kill or displace many different organisms, including plants, wildlife,
and humans.
Greenhouse gases: The flooding of surrounding habitat around dams kills trees
and other plant life that then decomposes and releases large amounts
of carbon into the atmosphere. Because the river is no longer flowing freely, the
water becomes stagnant and the bottom of the reservoir becomes becomes
depleted of oxygen. This lack of oxygen creates a situation where methane (a
very potent greenhouse gas) is produced from the decomposition of the plant
materials at the bottom of the reservoir that eventually gets released into the
atmosphere, contributing to global climate change.
Sediment builds up behind the dam: Because a dammed river no longer flows
freely, the sediment that would have otherwise been deposited naturally
downstream begins to build up behind the dam, forming new riverbanks, river
deltas, alluvial fans, braided rivers, oxbow lakes, levees and coastal shores. These
changes in sedimentation can lead to dramatic alterations in plant life and animal
life and how they are distributed.
Downstream sediment erosion: Due to the restrictions in the sediment flow
above a dam, the lack of sediment that would have once flowed downstream
ultimately leads to a deficiency in sediment load, and therefore, leads to
an increase in downstream erosion. This lack of sediment load causes the
riverbed to deepen and narrow over time, a compromised water table, the
homogenization of the river’s flow, reduced wildlife support, and a reduction in
sediment that reaches coasts and deltas.
Negative impacts on local fish populations: Typically, local fish species will
not be adapted to the new environment that is present after a dam is built and
do not survive, leading to the extirpation of local populations. Many factors
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impact their survival, including the blockage of migration routes, a disconnection
from the river’s flood plain, changes in a river’s flow, changes in temperature,
turbidity, dissolved oxygen, and changes in local plant life.
o Organic materials from within and outside the river that would normally wash
downstream get built up behind dams and start to consume a large amount of
oxygen as they decompose. In some cases this triggers algae blooms which, in
turn, create oxygen-starved “dead zones” incapable of supporting river life of
any kind.
o Also, water temperatures in dam reservoirs can differ greatly between the
surface and depths, further complicating survival for marine life evolved to
handle natural temperature cycling. And when dam operators release oxygen-
deprived water with unnatural temperatures into the river below, they harm
downstream environments as well.
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Pollution
Roads can also be a conduit for pollutants into the environment. The
debris from tires on the road can decrease the time to metamorphosis of
wood frogs.20 Deicing salts that run off from roads into adjacent ponds
can decrease survivorship of wood frogs and spotted
salamanders.21 Frogs have been shown to have higher skeletal
abnormalities closer to roads, possibly as a result of contamination.19 In
addition to causing mortality, deicing salts can alter the behavior of
frogs and decrease locomotor performance. This can impact fitness, as
they may be less adept at catching prey or eluding predators. 22 Roads
also carry oils from cars that travel across them, which have the potential
to harm wildlife when they enter the environment.
Pollution from roads extends beyond just chemicals, as light and noise
pollution from roads can be detrimental as well. Noise from cars can
impact birds by disrupting acoustic communication and interfering with
warning signals, leading to bird population declines in the proximity of
roads.23 Not all birds are equally affected, however, as those that have
song frequencies similar to car frequencies are more likely to be absent
from roadside areas. In addition to decreasing the numbers of birds, road
noise can alter the community composition of birds as certain species are
differentially excluded.24 Similarly, roads can interfere with the calling
of frogs and make it difficult for them to find a mate.25
Mitigation
A number of mitigation strategies have been developed to decrease the
harmful impacts of roads on wildlife. In cases where patterns of
mortality are predictable during certain times of the year, road closures
or speed limit reductions during these times may decrease mortality
rates.10 Road closures during breeding migrations have been used to
successfully decrease mortality of the Jefferson's salamander in Ontario.
Since many gravid reptiles are killed while trying to find a nesting site,
the construction of artificial nesting sites may prohibit them from
needing to cross the road. For snakes, artificial hibernacula can also be
29
constructed to reduce distance traveled and the chances of road
mortality.
Decreasing traffic volume is not likely to be effective when animals
avoid the physical surface of the road. In such cases, constructing
alternative ways of crossing the road can be more successful. For
smaller animals, culverts that pass under roads can allow for safe
passage. Barriers along the road are also constructed to guide animals to
the culverts. This has shown to be extremely effective in reducing road
mortality in some cases. A drawback of culverts is that they primarily
facilitate crossing by smaller animals. For larger animals, wildlife
overpasses have been used to allow crossing. They sometimes have
vegetation planted over them to mimic the natural habitat. Studies have
shown that red deer and wild boar will use such structures to cross the
road and usage may increase over time as animals become accustomed
to them.31
Erosion
Erosion of exposed hillsides, mine dumps, tailings dams and
resultant siltation of drainages, creeks and rivers can significantly impact
30
the surrounding areas, a prime example being the giant Ok Tedi
Mine in Papua New Guinea. In wilderness areas mining may cause
destruction of ecosystems and habitats, and in areas of farming it may
disturb or destroy productive grazing and croplands
Sinkholes
A sinkhole at or near a mine site is typically caused from the failure of a
mine roof from the extraction of resources, weak overburden or
geological discontinuities.[3] The overburden at the mine site can
develop cavities in the subsoil or rock, which can infill with sand and
soil from the overlying strata. These cavities in the overburden have the
potential to eventually cave in, forming a sinkhole at the surface. The
sudden failure of earth creates a large depression at the surface without
warning, this can be seriously hazardous to life and
property.[4] Sinkholes at a mine site can be mitigated with the proper
design of infrastructure such as mining supports and better construction
of walls to create a barrier around an area prone to sinkholes. Back-
filling and grouting can be done to stabilize abandoned underground
workings.
Water pollution
Mining can have harmful effects on surrounding surface and
groundwater. If proper precautions are not taken, unnaturally high
concentrations of chemicals, such as arsenic, sulfuric acid,
and mercury over a significant area of surface or subsurface
water.[5] With large amounts of water used for mine drainage, mine
cooling, aqueous extraction and other mining processes, increases the
potential for these chemicals to contaminate ground and surface water.
As mining produces copious amounts of waste water, disposal methods
are limited due to contaminates within the waste water. Runoff
containing these chemicals can lead to the devastation of the
surrounding vegetation. The dumping of the runoff in surface waters or
in a lot of forests is the worst option. Therefore, submarine tailings
disposal are regarded as a better option (if the waste is pumped to great
31
depth).[6] Land storage and refilling of the mine after it has been depleted
is even better, if no forests need to be cleared for the storage of debris.
The contamination of watersheds resulting from the leakage of
chemicals also has an effect on the health of the local population.[7]
In well-regulated mines, hydrologists and geologists take careful
measurements of water to take precaution to exclude any type of water
contamination that could be caused by the mine's operations. The
minimization of environmental degradation is enforced in American
mining practices by federal and state law, by restricting operators to
meet standards for the protection of surface and groundwater from
contamination.[8] This is best done through the use of non-toxic
extraction processes as bioleaching.
Acid rock drainage
Sub-surface mining often progresses below the water table, so water
must be constantly pumped out of the mine in order to prevent flooding.
When a mine is abandoned, the pumping ceases, and water floods the
mine. This introduction of water is the initial step in most acid rock
drainage situations.
Acid rock drainage occurs naturally within some environments as part of
the rock weathering process but is exacerbated by large-scale earth
disturbances characteristic of mining and other large construction
activities, usually within rocks containing an abundance of sulfide
minerals. Areas where the earth has been disturbed (e.g. construction
sites, subdivisions, and transportation corridors) may create acid rock
drainage. In many localities, the liquid that drains from coal stocks, coal
handling facilities, coal washeries, and coal waste tips can be highly
acidic, and in such cases it is treated as acid mine drainage (AMD). The
same type of chemical reactions and processes may occur through the
disturbance of acid sulfate soils formed under coastal or estuarine
conditions after the last major sea level rise, and constitutes a similar
environmental hazard.
The five principal technologies used to monitor and control water flow
at mine sites are diversion systems, containment ponds, groundwater
32
pumping systems, subsurface drainage systems, and subsurface barriers.
In the case of AMD, contaminated water is generally pumped to a
treatment facility that neutralizes the contaminants.[10] A 2006 review of
environmental impact statements found that "water quality predictions
made after considering the effects of mitigation largely underestimated
actual impacts to groundwater, seeps, and surface water"
33
Mitigation
To ensure completion of reclamation, or restoring mine land for future
use, many governments and regulatory authorities around the world
require that mining companies post a bond to be held in escrow until
productivity of reclaimed land has been convincingly demonstrated,
although if cleanup procedures are more expensive than the size of the
bond, the bond may simply be abandoned. Since 1978 the mining
industry has reclaimed more than 2 million acres (8,000 km²) of land in
the United States alone. This reclaimed land has renewed vegetation and
wildlife in previous mining lands and can even be used for farming and
ranching.
1. Coal dust
Dust inhalation or coal dust is one of the most common concerns for
miners.
Even though measures to prevent black lung have been legally enforced
for many years now, new cases still occur among coal miners.
2. Noise
Mines are noisy places, with the constant of drilling and heavy
machinery, and the potential for hearing damage is quite serious.
“It can be easy for you to mentally get used to loud noises, but that
doesn’t mean that damage isn’t still being done. Many people don’t
notice the damage to their hearing until long after they were first
exposed to the noisy environment, as most damage occurs very slowly.
35
3. Whole body vibration
Whole body vibration (WBV) is a slow forming physical hazard that
occurs in mining workers and other occupations that work with heavy
machinery.
“Some forms of vibration are ok, but they become dangerous when they
involve uneven surfaces, vehicle activity such as ripping versus pushing
material in a bulldozer, and engine vibrations.
Again, reducing exposure also reduces the health risks and should be the
first step that mining companies take. This might include filling in
potholes on unmade roads, minimising the transport of goods or
materials, or replacing manned with unmanned machines such as
remotely controlled conveyors.
Where risks cannot be avoided, supervisors should reduce the time for
which the employee uses the machine each day. Instruction and training
are critical, and symptoms of back pain in employees should be closely
monitored.
4. UV Exposure
For open-pit miners, understanding the risk of over-exposure to UV
(ultraviolet) radiation in sunlight is essential.
“Over exposure of ultraviolet rays can put you at risk of skin cancer, of
which Australia has the highest rate in the world. Not only can UV rays
36
cause melanomas to form, but they can cause serious damage to your
eyes if you are not wearing protective eye wear.
5. Musculoskeletal disorders
Musculoskeletal disorders (MSDs) refer to any problems affecting your
bones, muscles, blood vessels and nerves.
“Mine workers are exposed to a variety of potential health risks that fall
under this broad category. While musculoskeletal damage can occur due
to a trip, fall or heavy lift, the more serious ones occur slowly over time.
This could be due to ongoing heavy lifting or repetitive strains,” says
Clark.
6. Thermal stress
A common health risk that miners face is thermal – or heat – stress.
“Mining environments are often very hot and humid, particularly those
in outback Australia, which over time can cause thermal stress in
workers.
38
Furthermore, companies should provide training for workers, especially
new and young employees, and monitor the health of workers at risk.
7. Chemical hazards
Mine workers are often exposed to harmful chemicals.
39
Waste can be solid, liquid, or gas and each type has different methods of
disposal and management. Waste management deals with all types of
waste, including industrial, biological and household. In some cases,
waste can pose a threat to human health.[2] Waste is produced by human
activity, for example, the extraction and processing of raw
materials.[3] Waste management is intended to reduce adverse effects of
waste on human health, the environment or aesthetics.
Waste management practices are not uniform among countries
(developed and developing nations); regions (urban and rural areas),
and residential and industrial sectors can all take different approaches.[4]
A large portion of waste management practices deal with municipal
solid waste (MSW) which is the bulk of the waste that is created by
household, industrial, and commercial activity
Principles of waste management
Waste hierarchy
The waste hierarchy refers to the "3 Rs" Reduce, Reuse and Recycle,
which classifies waste management strategies according to their
desirability in terms of waste minimisation. The waste hierarchy is the
cornerstone of most waste minimisation strategies. The aim of the waste
hierarchy is to extract the maximum practical benefits from products and
to generate the minimum amount of end waste; see: resource
recovery.[6] The waste hierarchy is represented as a pyramid because the
basic premise is that policies should promote measures to prevent the
generation of waste. The next step or preferred action is to seek
alternative uses for the waste that has been generated i.e. by re-use. The
next is recycling which includes composting. Following this step is
material recovery and waste-to-energy. The final action is disposal, in
landfills or through incineration without energy recovery. This last step
is the final resort for waste which has not been prevented, diverted or
recovered.[7] The waste hierarchy represents the progression of a product
or material through the sequential stages of the pyramid of waste
40
management. The hierarchy represents the latter parts of the life-cycle
for each product.
Life-cycle of a product
The life-cycle begins with design, then proceeds through manufacture,
distribution, and primary use and then follows through the waste
hierarchy's stages of reduce, reuse and recycle. Each stage in the life-
cycle offers opportunities for policy intervention, to rethink the need for
the product, to redesign to minimize waste potential, to extend its
use.[7][ Product life-cycle analysis is a way to optimize the use of the
world's limited resources by avoiding the unnecessary generation of
waste.
Throughout most of history, the amount of waste generated by humans
was insignificant due to low levels of population
density and exploitation of natural resources. Common waste produced
during pre-modern times was mainly ashes and human biodegradable
waste, and these were released back into the ground locally, with
minimum environmental impact. Tools made out of wood or metal were
generally reused or passed down through the generations.
However, some civilizations do seem to have been more profligate in
their waste output than others. In particular, the Maya of Central
America had a fixed monthly ritual, in which the people of the village
would gather together and burn their rubbish in large dumps.
Waste handling and transport
Waste collection methods vary widely among different countries and
regions. Domestic waste collection services are often provided by local
government authorities, or by private companies for industrial and
commercial waste. Some areas, especially those in less developed
countries, do not have formal waste-collection systems.
41
Curbside collection is the most common method of disposal in most
European countries, Canada, New Zealand, United States, and many
other parts of the developed world in which waste is collected at regular
intervals by specialised trucks. This is often associated with curb-side
waste segregation. In rural areas waste may need to be taken to a transfer
station. Waste collected is then transported to an appropriate disposal
facility. In some areas, vacuum collection is used in which waste is
transported from the home or commercial premises by vacuum along
small bore tubes. Systems are in use in Europe and North America.
Disposal methods
Landfill
A landfill is a site for the disposal of waste materials by burial.
Landfill is the oldest form of waste treatment, although the burial of the
waste is modern; historically, refuse was simply left in piles or thrown
into pits. Historically, landfills have been the most common method of
organized waste disposal and remain so in many places around the
world.
Incineration
Incineration is a disposal method in which solid organic wastes
are subjected to combustion so as to convert them into residue and
gaseous products. This method is useful for disposal of both municipal
solid waste and solid residue from waste water treatment. This process
reduces the volumes of solid waste by 80 to 95 percent.[18] Incineration
and other high temperature waste treatment systems are sometimes
described as "thermal treatment". Incinerators convert waste materials
into heat, gas, steam, and ash.
Incineration is carried out both on a small scale by individuals and on a
large scale by industry. It is used to dispose of solid, liquid and gaseous
waste. It is recognized as a practical method of disposing of
42
certain hazardous waste materials (such as biological medical waste).
Incineration is a controversial method of waste disposal, due to issues
such as emission of gaseous pollutants.
Incineration is common in countries such as Japan where land is more
scarce, as the facilities generally do not require as much area as
landfills. Waste-to-energy (WtE) or energy-from-waste (EfW) are broad
terms for facilities that burn waste in a furnace or boiler to generate heat,
steam or electricity. Combustion in an incinerator is not always perfect
and there have been concerns about pollutants in gaseous emissions
from incinerator stacks. Particular concern has focused on some very
persistent organic compounds such as dioxins, furans, and PAHs, which
may be created and which may have serious environmental
consequences.
Recycling
Recycling is a resource recovery practice that refers to the
collection and reuse of waste materials such as empty beverage
containers. The materials from which the items are made can be
reprocessed into new products. Material for recycling may be collected
separately from general waste using dedicated bins and collection
vehicles, a procedure called kerbside collection. In some communities,
the owner of the waste is required to separate the materials into different
bins (e.g. for paper, plastics, metals) prior to its collection. In other
communities, all recyclable materials are placed in a single bin for
collection, and the sorting is handled later at a central facility. The latter
method is known as "single-stream recycling."
The most common consumer products recycled include aluminium such
as beverage cans, copper such as wire, steel from food and aerosol cans,
old steel furnishings or equipment,
rubber tyres, polyethylene and PET bottles, glass bottles and
jars, paperboard cartons, newspapers, magazines and light paper,
and corrugated fiberboard boxes.
PVC, LDPE, PP, and PS (see resin identification code) are also
recyclable. These items are usually composed of a single type of
43
material, making them relatively easy to recycle into new products. The
recycling of complex products (such as computers and electronic
equipment) is more difficult, due to the additional dismantling and
separation required.
The type of material accepted for recycling varies by city and country.
Each city and country has different recycling programs in place that can
handle the various types of recyclable materials. However, certain
variation in acceptance is reflected in the resale value of the material
once it is reprocessed. In July 2017, the Chinese government announced
an import ban of 24 categories of recyclables and solid waste, including
plastic, textiles and mixed paper, placing tremendous impact on
developed countries globally, which exported directly or indirectly to
China.
Energy recovery
Energy recovery from waste is the conversion of non-
recyclable waste materials into usable heat, electricity, or fuel through a
variety of processes, including combustion, gasification, pyrolyzation,
anaerobic digestion, and landfill gas recovery.[22] This process is often
called waste-to-energy. Energy recovery from waste is part of the non-
hazardous waste management hierarchy. Using energy recovery to
convert non-recyclable waste materials into electricity and heat,
generates a renewable energy source and can reduce carbon emissions
by offsetting the need for energy from fossil sources as well as reduce
methane generation from landfills.[22] Globally, waste-to-energy
accounts for 16% of waste management.[23]
The energy content of waste products can be harnessed directly by using
them as a direct combustion fuel, or indirectly by processing them into
another type of fuel. Thermal treatment ranges from using waste as a
fuel source for cooking or heating and the use of the gas fuel (see
above), to fuel for boilers to generate steam and electricity in
a turbine. Pyrolysis and gasification are two related forms of thermal
treatment where waste materials are heated to high temperatures with
limited oxygen availability. The process usually occurs in a sealed vessel
44
under high pressure. Pyrolysis of solid waste converts the material into
solid, liquid and gas products. The liquid and gas can be burnt to
produce energy or refined into other chemical products (chemical
refinery). The solid residue (char) can be further refined into products
such as activated carbon. Gasification and advanced Plasma arc
gasification are used to convert organic materials directly into a
synthetic gas (syngas) composed of carbon monoxide and hydrogen. The
gas is then burnt to produce electricity and steam. An alternative to
pyrolysis is high temperature and pressure supercritical water
decomposition (hydrothermal monophasic oxidation).
Resource recovery
Resource recovery is the systematic diversion of waste, which was
intended for disposal, for a specific next use.[29] It is the processing of
recyclables to extract or recover materials and resources, or convert to
energy.[30] These activities are performed at a resource recovery
facility.[30] Resource recovery is not only environmentally important, but
it is also cost-effective.[31] It decreases the amount of waste for disposal,
saves space in landfills, and conserves natural resources.[31]
Resource recovery (as opposed to waste management) uses LCA (life
cycle analysis) attempts to offer alternatives to waste management. For
mixed MSW (Municipal Solid Waste) a number of broad studies have
indicated that administration, source separation and collection followed
by reuse and recycling of the non-organic fraction and energy and
compost/fertilizer production of the organic material via anaerobic
digestion to be the favoured path.
As an example of how resource recycling can be beneficial, many items
thrown away contain metals that can be recycled to create a profit, such
as the components in circuit boards. Wood chippings in pallets and other
packaging materials can be recycled to useful products for horticulture.
The recycled chips can cover paths, walkways, or arena surfaces.
Application of rational and consistent waste management practices can
yield a range of benefits including:
45
1. Economic – Improving economic efficiency through the means of
resource use, treatment and disposal and creating markets for
recycles can lead to efficient practices in the production and
consumption of products and materials resulting in valuable
materials being recovered for reuse and the potential for new jobs
and new business opportunities.
2. Social – By reducing adverse impacts on health by proper waste
management practises, the resulting consequences are more
appealing civic communities. Better social advantages can lead to
new sources of employment and potentially lifting communities
out of poverty especially in some of the developing poorer
countries and cities.
3. Environmental – Reducing or eliminating adverse impacts on the
environment through reducing, reusing and recycling, and
minimizing resource extraction can result in improved air and
water quality and help in the reduction of greenhouse
gas emissions.
4. Inter-generational Equity – Following effective waste management
practises can provide subsequent generations a more robust
economy, a fairer and more inclusive society and a cleaner
environment.[7]
46
1. Most useful from point of view of economic demands
Decision making process in that case is aimed at the best way of land
use from point of view of nation-wide or regional economic
requirements. So, the first demand covers possible collisions of interests
in a territory.
The last point calls for designs in harmony with nature. It means that
interventions into the geoenvironment and landscape must be technically
and ecologic sound and aesthetic suitable.
From listed above results that the concept rational use of the
geoenvironment includes also its protection. Why than we speak
47
separately of the geoenvironment protection? It is mainly in connection
with old objects of techno-sphere, which were not built up in accordance
with requirements of the geoenvironment rational use, in case of old
ecologic loads, on the chance of accidents and in case of unstable
territories (slope movements, erosion, subsidence, sagging a. o.). In
general we distinguish the geoenvironment protection against pollution
and against stability, integrity and structure failure, which bring about
instability of a territory.
In the case of the protection against pollution we basically use four
methods:
49
An environmental geologist has in geology similar position as a general
practitioner in medicine. This has to know something of all problems of
medicine (internal medicine, paediatrics, surgery, etc.) and must know
when he is competent to deal with problem alone and when to send the
patient to a specialist. There is necessary to subjoin that environmental
geologists, when comparing them with physicians, should be included
among the better ones, which take care of the health of the population
mainly on the basis of prevention.
Some of the efforts and programmes that are being implemented in the
protection of environment are as follows:
50
1. Forest Conservation
Forest plays the vital role for the environment conservation. The
Ministry of Forest and Soil Conservation has launched various
programmes for the conservation of forest and environment. Community
Forest Programme is one of the examples of conservation programmes
that help to protect the land, water and other components of the
environment. Afforestation must be done for the conservation of forest.
Laws about forest protection and awareness generation help in the
conservation programme
2. Soil Conservation
Soil conservation is an important work of environmental conservation.
Control of landslides, flood, soil erosion helps to protect the land.
Afforestation, tree plantation, protection of pasture land help to conserve
the soil. Terrace farming on slope land, use of compost fertilizer and
minimizing the use of chemicals also helps to protect the soil. Ministry
of Forest and Soil Conservation, Ministry of Agriculture, etc. are
conducting various programmes to protect the soil.
3. Waste Management
House, market area, industry, settlement area, etc. are the sources of
solid wastes. Proper management of solid wastes helps to keep the
surrounding healthy. Local level authorities like municipalities, VDC,
etc. have been conducting various programmes for the management of
solid wastes. Construction of toilets in every house and management of
enough public toilet also help to keep the environment healthy
4. Public Awareness
People should be aware of the consequences of their activities. There are
various means to aware people by conducting rally and drama. Media
should also play the active role to aware the people.
51
5. Pollution Control
Industries and vehicles emit the smoke, dust and harmful gases that
pollute the environment. Chemical fertilizer and chemical poisons like
insecticides, herbicides, pesticides, etc. also pollute the environment.
Pollution must be controlled to keep the environment healthy. The
government of Nepal is making an effort to control the pollution.
6. Conservation of Heritage
Temple, gumba, chaityas, Dharamshala, parties and pauwas are our
cultural heritage. They are our identity. They must be preserved for
future generation. We must keep the areas of cultural heritage free from
pollution.
53