[Geography Notes] on Hot Spring Pdf for Exam

Hot springs are also known as the thermal springs, which spurts water that has higher temperatures which are moreover higher than the air temperature of that region that is surrounding the spring. The hot springs are a discharge of the groundwater that is heated by shallow intrusions of the magma. 

However, these thermal springs are not related to volcanic activity. In the cases of hot springs, the water is heated by the convective circulation of groundwater which percolates downward and then reaches the depths of a kilometre or even more where the temperature of rocks is quite high because of the normal temperature that is the gradient of the crust of the earth. 

Hot Spa

A hot spa is formed by a hot tub, which is typically used to refer to the above-ground portable spa. A hot tub or this portable spa is a total self-contained vessel. All kinds of plumbing works, and also the electrical control system and other such components, are built inside the hot tub. Extra plumbing is not required here.

The contrast between these two is their actual use and their location. A hot tub does have spa-like qualities like spas are often a standalone establishment or this is an in-ground structure that also provides all the health treatments. Whereas, a hot tub is portable and has plumbing and other electrical control systems.

Asin Hot Springs 

Asin Hot Spring is located 16 kilometres away from Baguio City. The hot spring is set in between the tall mountains.

Passing through the Naguilian Road, which comes before Cooyeesan Hotel Plaza after a few minutes, we can find Woodcarving Village. Woodcrafts are here displayed along the roadsides, where we can stop and watch the villagers carve beautiful images from the wood. The travellers travelling in the Asin, usually enjoy the whole trip because of the beautiful mountain scenery that is displayed throughout this trip. There are two waterfalls which catch the attention of the travellers. The travellers need to pass two tunnels after which they can finally reach Asin. 

There are 5 resorts to choose from, depending on the preference, budget and availability. The entrance fee to the resorts starts from Rs. 40-60 for the kids and Rs. 80-100 for adults. All the resorts have great amenities like restaurants, hotels and souvenir shops.

People with minimal budgets choose to go to the river instead. The water is clean and clear there, with no rules, so that they can enjoy nature at its best. People can also bring their fishing rods with them. Here the travellers come and enjoy with fewer restrictions and entry fee, they also carry picnic mats with them.  

Hot Spring Bath 

The hot spring bath is a steamy and sulphur-smelling tradition that spans the ages and continues to be a luxury requirement for spas, resorts and campgrounds around the world. People around the globe talk much about the rejuvenating powers of the sulphur springs. So, we can say that the hot spring bath causes many health benefits.

  • Hot Spring Baths are friendly to the skin.

  • This relaxes the mind.

  • A hot Spring bath increases blood circulation.

  • Hot Spring Bath proves to be a natural painkiller

Hot Springs Resort and Spa

Hot Springs are located in the mountains of Western North Carolina and are located along the banks of the Spring Creek and in the French Broad River, this is a town with rich history and with beaming natural charm. This town is an intersection along the historic Appalachian Trail and they are the part of the Southern Appalachian Mountains.

There is a Hot Spring Resort and Spa located in the heart of Hot Springs, North Carolina, this is a 100-acre Resort & Spa. In this resort we can find jetted hot tubs, that are positioned outside along the tranquil banks of the Spring Creek and the French Broad River; these tubs are supplied with a continuous flow of the World Famous Natural Hot Mineral Water. The resorts also have a nationally certified and state-licensed staff of massage therapists to compliment the same. 

Hot Springs Resort & Spa also offers other lodging options for those looking for a relaxing time to spend. These resorts have four luxury suites that have a jetted tub with mineral water in the room. This resort also has a deluxe cabin along with a full size outdoor jetted tub.

[Geography Notes] on Indicator Species Pdf for Exam

The word “bioindicator” is used to refer to all sources of biotic and abiotic responses to environmental changes. Taxa are used to display the effects of natural surrounding changes, or environmental change, rather than simply as gauges of natural change. They are used to detect changes in the natural environment and to show negative or positive effects. They can also detect changes in the ecosystem caused by pollutants, which can have an effect on the environment’s biodiversity as well as the animals that live there.

In various species occupying various types of habitats, natural, biological, and biodiversity markers can be identified. Air pollution is often monitored using lichens and bryophytes (liverworts). Since they have no roots, no fingernail skin, and obtain all of their nutrients from immediate exposure to the climate, lichens and bryophytes are important bioindicators of air quality. Their high surface area to volume ratio adds to the hypothesis that they could be used as a bioindicator or to capture contaminants from the air. Cyanophyta, a form of phytoplankton, is a powerful bioindicator that can indicate rapid eutrophication of water bodies such as rivers, lakes, and other bodies of water by forming bloom formations.

Not all biological processes, plants, or populations, on the other hand, can be used as bioindicators. Environments differ in terms of physical, chemical, and biological influences. Populations develop strategies to optimise growth and reproduction within a limited range of environmental factors over time. Individuals’ physiology and/or behaviour can be adversely affected outside of their environmental optima, or tolerance range, decreasing their overall fitness. Reduced fitness can cause population dynamics to shift and the society as a whole to change. Because of their moderate tolerance for environmental variability, bioindicator species effectively show the condition of the environment. Rare species (or species assemblages) with narrow tolerances, on the other hand, are often too sensitive to environmental change or too uncommon to represent the general biotic response. Similarly, widespread species with broad tolerances are less vulnerable to environmental changes that would otherwise disrupt the population. The use of bioindicators, on the other hand, is not limited to a single species with a narrow range of environmental tolerance. In a “biotic index” or “multimetric” approach, whole populations may serve as bioindicators and represent various sources of data to measure environmental conditions, encompassing a wide range of environmental tolerances.

Types of Indicator Species

Indicator species come in a variety of types. Bacteria to more complex organisms like plants and animals may all be used as indicator species. Although all have evolved to exist within certain limits, all species are indicators of something; many are especially sensitive and provide an early indication of changes in environmental conditions.

1. The Wood Stork 

The absence of wood storks in everglade habitats indicates that the climate is not conducive to abundant wading birdlife. Wood storks used to live in these wetlands by consuming small freshwater fish. Wood storks are held up as a model for the health of the Everglades by conservationists. The success of water-management restoration efforts on wood stork populations will help determine whether efforts are improving overall everglade conditions to support all bird, fish, animal, and plant life.

2. River Otters 

Crayfish and fish are the main foods of river otters, but they also eat other invertebrates, amphibians, and smaller mammals. Otters are one of the most common keystone species and apex predators, so if there is a problem lower down the food chain, they are usually the first to suffer. River otter reintroduction effectiveness has been used to evaluate the health of freshwater habitats. The health of river otters has also been used to assess mercury emissions in the ecosystem. Chemicals or heavy metals accumulate in an organism over time, which is known as bioaccumulation. River otters will likely be the first to show signs of mercury poisoning because they are at the top of the food chain.

3. Frogs

Frogs have semi-permeable skin that needs to stay moist in order to breathe. Since they are susceptible to consuming chemical pollutants in their water, their skin makes them bioindicators for the health of their environment. Many frogs have life cycles that use both terrestrial and freshwater habitats, making them vulnerable to environmental stressors including temperature changes and UV radiation.

4. Buck’s Horn Plantain 

Salt exclusion and cellular osmotic adjustment are two mechanisms evolved by some plant species to cope with salt in the soil. Plants that lack these mechanisms would be unable to thrive in high-salinity environments. Buck’s horn plantain is a good ecological indicator of salt levels in Australian soils because its leaves turn redder as the salt level rises.

5. Algal Blooms are Water Pollution Indicator Species

Algal blooms may be a sign of a changing climate. Algal blooms may be caused by a rise in nutrients from sedimentation runoff. Natural seasonal changes in nutrient availability can also be linked to algal blooms. The abundance of algae in a given area can also be used to detect nutrient availability gradients in a body of water.

6. Lichens as Bioindicators

Lichens are pollution indicators. Lichens are made up of a variety of fungi, algae, and bacteria. Lichens exhibit a variety of functional traits and responses in response to air pollution and temperature, making them a bioindicator of air pollution. As a result, the presence of various forms of lichens may be used to determine the environmental effects of urbanisation. For example, lichens made of chloro coccoid green algae and those with foliose narrow lobes are associated with medium to high levels of urbanisation. Low-density urbanised areas, on the other hand, have more cyanolichens and Trentepohlia algae lichens that have a crustose formation.

Bioaccumulator Indicator Species

Bioaccumulator indicator organisms are those that can avoid and accumulate different pollutant substances in their tissues, allowing them to be detected at very low levels in the atmosphere. The main disadvantage is that a variety of biotic and abiotic variables will influence the rate at which the pollutant accumulates, necessitating both laboratory and field testing to identify the effects of extraneous parameters.

Mollusks, especially bivalves, have long been the most common species used to detect the presence and quantity of toxic substances. Because of their sessile existence, vast geographical range, and capacity to absorb toxic substances in their tissues and detoxify when pollution ceases, individuals of the genera Mytilus, for example, have been considered ideal in many works to detect the concentration of toxic substances in the atmosphere.

Similarly, polychaete species such as Nereis diversicolor, Neanthes arenaceodentata, Glycera alba, Tharix marioni, or Nephtys hombergii are thought to be capable of accumulating toxic substances. Because of their bioaccumulative potential and the current relationship between pathologies experienced by any benthic fish and the existence of polluting substances, several fish species have also been used in various works focusing on the effects of toxic contamination of the marine environment.

Heavy metals, chemicals, and radionuclides have all been detected in algae, with Fucus, Ascophyllum, and Enteromorpha being the most commonly used taxa.

Bioindicators of Water Pollution

Plankton is responsible for a considerable amount of biological production in many water bodies, including oceans, lakes, streams, and swamps. Planktons are made up of chlorophyll-producing species. These planktons are made up of populations that move along with the rivers and tides, fusing and cycling large amounts of energy that is then passed on to higher trophic levels.

Planktons were studied in Indian lentic ecosystems in the mid-twentieth century. These studies showed that the dominant planktons and their regularity vary greatly in different water bodies depending on supplement status, age, morphometry, and other location factors. As a result, they’re often used as markers of lake trophic status. Planktons respond quickly to environmental changes and are regarded as excellent indicators of water quality and trophic conditions due to their short lifespan and rapid reproduction rate. The resistance range in relation to abiotic ecological components (Temperature, Oxygen fixation, and pH) as well as biotic connections among organisms are used to identify the occurrence of planktonic organisms in natural conditions. The changes that occur within planktonic populations provide the foundation for determining the trophic condition of water bodies.

Benefits and Disadvantages of Bioindicators

Bioindicators’ various advantages have prompted regulatory requirements for their use in countries all over the world, as well as their inclusion in a number of international agreements. Bioindicators, however, are not without flaws. We depend on the sensitivity of certain bioindicators to act as early-warning signals, just like the canaries in the coal mine. We can’t always tell the difference between natural variations and changes caused by humans, which limits the applicability of bioindicators in complex ecosystems. As a result, factors other than disturbance or stress may have an effect on indicator species populations, complicating our understanding of the causal mechanisms of transition. The ability of bioindicators to serve as indicators is scale-dependent, according to the second criticism of their use. A large vertebrate indicator, for example, may not accurately represent the biodiversity of the local insect population. The habitat requirements of bioindicator species are invariably different from those of other species in their environment. Ecosystem management based on a bioindicator’s habitat requirements which fail to protect rare species with different requirements. The ultimate objective of bioindicators is to determine the nature of an ecosystem and how it evolves over time using a single species or a small group of species, but this can be a gross oversimplification of a complex system.

We must be aware of its shortcomings, as with all management methods. Bioindicators’ drawbacks, on the other hand, are obviously outweighed by their advantages. Bioindicators may be used to assess the health of an environment at a variety of scales, from the cellular to the ecosystem level. They put together data from our world’s biological, physical, and chemical components to show how changes in human fitness, population density, community structure, and ecosystem processes manifest themselves. In terms of management, bioindicators help us determine what is and is not biologically viable. We do not understand the effect of our disruptions until it is too late to avoid them without the moss in the tundra, the cutthroat in the mountain stream, and the canary in the coal mine.

Conclusion

There are three different definitions for the word “indicator species.” They are a species (or a group of species) that represent the biotic or abiotic state of an ecosystem, show evidence for, or the effects of, environmental change, or indicate the diversity of other species, taxa, or entire communities within a given region. The first two uses of indicator species are very similar, with the only difference being that organisms must be sampled more than once in the same location and in the same way to show change. Detecting emissions to tracking the regeneration of formerly damaged ecosystems, using species to show the condition of, and changes in, the ecosystem has various tried and tested applications at many scales, from local to global. The use of indicator species to estimate the diversity of other, unstudied taxa for scientific or conservation purposes is much more controversial, and it may prove difficult to do so with any degree of accuracy.

[Geography Notes] on Land, Soil, Water, Natural Vegetation, and Wildlife Resources Pdf for Exam

The resources that occur and exist in nature and lead to the existence of others are termed as natural resources which can be renewable or non – renewable as well. Some resources will be entirely exhausted one day but we can slow the pace of their complete exhaustion and extinction by looking out the issues and adopting measures to conserve them. In this article, we will be discussing major natural resources such as land soil water natural vegetation and wildlife resources and their related important concepts. We will learn what kind of resource is soil or how to conserve wildlife or the importance of land and water and other related concepts. These notes will be helpful for the students of Class 6 studying Geography and Environment and also students of upper classes. 

Natural Resources & Their Significance

The resources that exist on our planet in different forms in a natural way without any help or action of humans are called natural resources. They exist independently in nature without the help or interaction of humans. For example, air, water, land, sunlight, minerals, fossil fuels, animals, plants, etc. The major significance of these resources is that they maintain ecological and environmental balance on the Earth because humans usually create unbalance on the Earth. They provide an environment here that makes the possibility for life to exist on the planet. The major five natural resources are land soil water natural vegetation and wildlife resources. 

Land & Soil

Land and soil are two of the most important resources on our planet. The former is considered as the upper lithosphere part of the Earth whereas the latter is a kind of loose and organic material that lies on the land. Both serve as an important resource of Earth but is there any difference between land and soil? Let’s see.

Difference between Land and Soil

Land

Soil

It is the outer and lithospheric part of the Earth. 

It is a part of land and kind of organic material that lies on land. 

It is considered a 2-dimensional resource because we measure the length and width of the land.

It is considered a 3-dimensional resource because we measure the length, width, and depth of the soil. 

It is a broader term. 

It is a narrow term.

Significance 

The importance of soil and land natural resources are mentioned below:

  • They both are reasons for the survival of living organisms on the planet.

  • Where one side, the land provides space to reside, the other provides food to live.

  • The land is home to human beings and animals and other land species whereas soil is also home to various microorganisms.

  • They both serve as the base for agriculture activities.

Factors Affecting Land

Following are the factors that can affect land and its productivity:

  • The rapid increase in the global population put major stress on land.

  • The different types of cultivation patterns can affect the land.

  • The quality of the land can also affect its productivity level.

  • Excessive use of land and excessive stress can affect its productivity.

  • The occurrence of natural disasters such as landslides or earthquakes can affect the land in a large amount.

  • Different types of irrigation methods and excessive use of these methods can also affect their health.

Factors Affecting Soil

The following mentioned factors can affect the soil and its productivity:

  • The wrong agricultural practices can affect the soil and its fertility can be lost.

  • Land pollution can affect it as well.

  • The excessive use of chemical fertilizers or pesticides or insecticides can harm the quality of the soil.

  • Heavy rainfall, cloud outburst, floods, tsunamis, etc. can harm a large amount of good soil and lead to soil erosion.

  • Heavy deforestation directly affects the soil.

Conservation of Soil

Following measures can be taken for its conservation:

  • The use of good agricultural activities such as crop rotation or terrace farming, mulching, etc.

  • Leaving the soil vacant for some time say years so that it can regain its sufficient fertility level.

  • Less use of harmful chemical agricultural products.

  • The adoption of organic farming will help conserve the soil.

  • Growing more and more trees also helps in their conservation.

Water as a Natural Resource

It is one of the unique features of our planet that lead to the presence of life on it because it consists of liquid water which is essential for survival. Water as a Natural Resource serves various functions but only 2.5 % of the total water that we found on Earth is freshwater that is usable for survival purposes for humans or animals and the rest of the water is saltwater. The list of its various sources includes rivers, lakes, ponds, wetlands, glaciers, oceans, etc.

Factors Affecting Water

The various factors that can affect this natural resource are mentioned below:

  • It is used as a raw material in both agricultural and industrial activities, thus putting great stress on this resource.

  • Excessive use of irrigation activities can affect the availability of groundwater in some areas.

  • Pollution is a major source that is affecting not only its quality but also producing several water-borne diseases.

  • Throwing garbage or industrial waste in water affects it.

Conservation of Water Resources

It is very important to conserve this resource which can be done in the following ways:

  • Best irrigation practices should be adopted in the agriculture sector such as drip irrigation or sprinkler system etc.

  • Recycling industrial water or household water will help in conserving water.

  • Rainwater harvesting is a good method to be adopted by everyone.

  • Adopting water conservation measures by the households in their homes will lead to a major impact.

Natural Vegetation and Wildlife Resources

These are flora and fauna that exist in nature without any kind of humanitarian aid. The flora that grows naturally is called natural vegetation whereas the several species of fauna kingdom that live on Earth are called wildlife resources. Various factors are there which are affecting their existence on Earth such as increasing temperature and deforestation, damaging the home of the animals, killing them for food and other industrial products, etc.

Conservation of Natural Vegetation and Wildlife Resources

The various measures can be taken to conserve natural resources vegetation and wildlife which are mentioned below:

  • Various projects are launched by the National and international organizations for their conservation in which everyone should participate.

  • By knowing the status of any wildlife species through the IUCN list, conservation should be done on a priority basis of species that lie in critical endangered, endangered and vulnerable categories.

Conclusion

To conclude what we have discussed above we can say that these natural resources are the gift of nature and these are the gifts that help in the existence of life on the Earth but due to several factors they are deteriorating and for that right conservation measures are required to be taken to save them. In this article, we have covered necessary topics of land soil water natural vegetation and wildlife such as the meaning of the resources, water as a natural resource, the difference between land and soil, etc. As we discussed above, we should take appropriate measures to conserve these natural resources and do whatever is in our hands. These notes will help the students of Class 6 and upper classes to understand the resources and their various issues and how to conserve them.

[Geography Notes] on Mafic Rocks Pdf for Exam

The Earth, by weight, mostly consists of mafic or ultramafic rocks, but silicic rocks are considered to be more abundant on the surface of the Earth. The common type of mafic rocks is basalt, pyroxene, biotite, etc. In this article, we will talk about this type of rock. We will learn about what are mafic rocks, mafic minerals, their meaning, definitions, features, and examples, etc. This topic will be helpful to understand one of the types of igneous rocks which are formed from magma and which we usually study in Geography, Geography, Earth Sciences, Physical Geography, etc.

Introduction

Rocks are said to be the hard matter which forms after the solidification of the magma and because of various other geographical phenomena. These are generally of three main types which include igneous rocks, sedimentary rocks, and metamorphic rocks. Among these, igneous rocks are said to be the primary rocks because they occur first and then sedimentary rocks form and then the formation of metamorphic rocks happens because of geological processes on the above two types of rocks. If we talk about Igneous rocks, these are formed after the solidification of magma and can be of two types i.e. Intrusive and Extrusive. These are being divided on the basis of where they actually occur. If rock formation is done below the surface of the Earth is known as intrusive igneous whereas if it occurs above the surface of the Earth, it is known as Extrusive rocks. Mafic rock is an example of Intrusive igneous rock.

Meaning of Mafic

It is a portmanteau term that is made up of magnesium and ferric. On the basis of silica content, igneous rocks can be classified into various types. Silica is found in abundance in igneous rocks because of which is considered the basis of classification. On this basis, igneous rocks can be divided into four major types i.e felsic, intermediate, mafic, and ultramafic ( written as per the silica content in decreasing order). Mafic is a kind of igneous rock which are rich in magnesium and iron. This type of rock contain 45 to 55 % silica content and 4 mafic igneous rocks minerals are pyroxene, amphibole, olivine, and mica. Mafic word is sometimes also used as a synonym for dark coloured minerals. 

Definitions

Some of the standard definitions are given below:

  • “In Geology, of or relating to rocks rich in dark, ferromagnesian minerals.” – dictionary

  • “Mafic describes rocks containing more dark-coloured substances and iron than other rocks.” – Cambridge dictionary.

  • “It is Relating to or denoting a group of dark-coloured, mainly ferromagnesian minerals such as pyroxene and olivine and often contrasted with felsic. ( Geology ). – Lexico definition.

  • “Mafic is a collective term for minerals present in igneous rocks Or “relating to igneous rocks or silicate minerals.” Or “( Geology ) of or pertaining to igneous rocks that are rich in dark-coloured minerals and that contain magnesium and iron and a comparatively low level of silica.” – Collins Dictionary.

Features

The basic features of mafic rocks are given below:

  • This is one of the important types of igneous rocks that are classified on the basis of silica content.

  • It is a type of rock that crystallizes from silicate minerals at high temperatures. Sometimes, these rocks are also called basaltic. 

  • Olivine, pyroxene, amphibole, and biotite are common rock-forming minerals of mafic.

  • Common examples of mafic rocks are basalt, gabbro, diabase, etc.

  • They are dark in colour ( whereas felsic rocks are light in colour).

  • Chemically, these rocks are consist of magnesium, iron, and calcium.

  • Mafic magma has a low content of silica because of which before cooling, mafic lava has a low viscosity.

  • The volcanic eruptions consist of mafic lava are less explosively violent as compared to felsic volcanic eruptions.

Additional Information

On the basis of the texture of rocks, different names of mafic rocks are given below in the table:

Different Names of Mafic Rocks

Texture

Name of Mafic Rocks

Pegmatitic

Gabbro pegmatite

Coarse grained – Phaneritic

Gabbro

Coarse grained – Porphyritic

Porphyritic Gabbro

Fine grained – aphanitic

Basalt

Fine grained – Porphyritic

Porphyritic basalt

Puroclastic

Basalt tuff or breccia

Vesicular

Vesicular basalt

Amygdaloidal

Amygdaloidal basalt

Small vesicles

Scoria

Glassy

Tachylyte, Sideromelane, and Palagonite

Conclusion

To sum up we can say that mafic is a term which is made up of magnesium and ferric thus used to describe the rocks which are rich in two whereas now it is also used to describe the igneous rocks which are rich in high content of magnesium as well as iron. It is a dark coloured rock that consists of silica content less than felsic and intermediate whereas more than ultramafic igneous rocks. On the basis of the texture of the rocks, different names of mafic rocks can be there. This topic is useful to study whenever we talk about igneous rocks and their types.

[Geography Notes] on Methods of Reducing Earthquake Hazards Pdf for Exam

An earthquake can be defined as the trembling or shaking of the earth’s surface resulting due to the friction caused by the tectonic plates. These plates are found in the Earth’s crust and are separated by plate boundaries. Any friction in these edges or boundaries results in the formation of seismic waves causing the earth’s surface and the ground to move.

The after-effects of an earthquake are huge resulting in the formation of seismic waves. The movements of these waves shake the surface of the earth and result in earthquakes. 

The aftermath of an earthquake is huge. It destroys several buildings, infrastructure and even loss of life on a severe level. The level of damage caused depends on the intensity of the earthquake. Therefore, many scientists do a study on understanding the ground motions of an earthquake and recording it with the help of a seismograph. This awareness of earthquake geology is very important to predict any future earthquakes and mitigate the hazards caused by them.

In this article, we provided information on the causes of an earthquake and also some methods for reducing earthquake hazards. This article can be referred to by the students as a reference to prepare for their examination.

What Causes an Earthquake?

An earthquake occurs due to the friction caused by two blocks of the earth. These blocks are known as the tectonic plates. The edges of these plates are separated by plate boundaries and the movement of these plates causes a planar fracture in the earth’s crust (also known as fault), thus, resulting in an earthquake.  This surface of friction is also called the fault plane. 

The surface of the earth where the earthquake originated is known as the epicentre. It is a location above the earth’s surface. While the area of origin below the surface of the earth is called the hypocentre of the earthquake. 

An earthquake can be followed by aftershocks. These are occurrences of small earthquakes after a regular interval of time. This occurs mostly after a larger earthquake having a high intensity. The aftershocks of an earthquake may continue for several hours to days or even years depending upon the intensity of the main earthquake.  The location below the earth’s surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter.

Methods of Reducing Earthquake Hazards

Over the several years, scientists have been trying their best to record the ground motions and do a study on earthquake geology. These studies help scientists to detect the earthquake-prone areas of the world and makes people aware of the occurrence of an earthquake in the near future. The geology of an earthquake is studied through seismograph. This gives the appropriate information on the epicentre and intensity of the earthquake. The size of an earthquake is provided on the Richter scale and the severity of damages caused by earthquakes totally depends on the magnitude of it. Every year, several lifeforms, infrastructures and natural habitats are destroyed due to the consequences of earthquakes. Henceforth, it is important for us to be aware of the precautionary measures to reduce the hazards.

Given below are Some of the Methods of Reducing Earthquake Hazards:

  1. To understand and evaluate the damages caused by the strong shaking of the ground.

  2. To evaluate and improve the infrastructure and design strategies of the buildings for making them more resistant to earthquakes.

  3. To introduce new methods to predict and study the seismic performance of buildings and structures.

  4. Improving earthquake provisions of building codes, and

  5. Assessing building safety immediately following a damaging quake.

  6. To improve the system and methods of seismic monitoring, especially in earthquake-prone areas. 

  7. Attaching sensors in the buildings to make people aware and safeguard them from any future earthquake.

Although earthquakes occur in an unpredictable manner, following these methods will somehow reduce the damages caused by earthquakes and will safeguard the people beforehand.

[Geography Notes] on Noctilucent Cloud Pdf for Exam

Noctilucent clouds or night-shining clouds are the highest clouds found in the Earth’s atmosphere located in the mesosphere at an altitude around 76 to 85 km (249,000 to 279,000 ft). The cloud consists of ice crystals and is only visible during astronomical twilight. In Latin, the term Noctilucent means “night-shining”. The clouds are most visible during the summer month and when the Sun is below the horizon from latitude between ±50° and ±70°.

The clouds are too faint to be observed during daylight and are visible only when illuminated by sunlight from below the horizon while lower levels of the atmosphere are in Earth’s shadow.

Noctilucent Meaning

The term Noctilucent means “night-shining” and is an indicator as to what makes them special.  Most clouds are dark at night, but night-shining clouds appear to glow a brilliant white or electric blue. Nlc clouds can reflect the light of the sun as shown in the figure given below as they are the highest clouds in the Earth’s atmosphere. The Nlc clouds are located in the mesosphere at an altitude of around 76 to 85 km (249,000 to 279,000 ft).

Noctilucent Clouds Definition

Noctilucent clouds, also known as polar mesospheric clouds, are very thin clouds of water ice crystals located in the Mesosphere at a height of about 75 km to 90 km.

Noctilucent Cloud Discovery 

Noctilucent or night-shining clouds were first observed in 1885, two years after the 1883 eruption of Krakatoa in the straits of Java. 

It is not confirmed whether their appearance had anything to do with the volcanic eruptions or whether their occurrence was due to more people observing the incredibly vibrant sunset caused by volcanic debris into the upper atmosphere by eruptions and contributing to their formation.  

Subsequent studies have shown that noctilucent clouds are not solely caused by volcanic activity, although dust and water vapour could be inserted in the Earth’s atmosphere by a volcanic eruption and contributed to their formation.

The assumption was made by the scientist at that time that clouds were another phenomenon of volcanic ash, but the cloud persisted after the ash liquidated out of the atmosphere.

In 1972, Nlc clouds were first observed from space by an instrument on the OGO – satellite. 

Noctilucent Cloud Formation

The night-shining clouds are made up of small crystals of water ice up to 10 mm in diameter and exist at a height of about 76 to 85 km, higher than any other cloud in the Earth’s atmosphere. Similar to the other clouds. Clouds in the Earth’s lower atmosphere form when water collects on particles, but mesospheric clouds or clouds in the mesosphere may come directly from the water vapour as well as forming on dust particles. 

Nlc clouds required water vapour dust, and very cold temperature to form. The source of both dust and water vapour in Earth’s atmosphere is not known with certainty. The dust was expected to come from micrometres, although particles from volcanoes and dust from the troposphere are also possibilities. Scientists believe that moisture could be lifted through the gas in the tropopause, as well as forming the reaction of methane with hydroxyl radicals in the stratosphere. Noctilucent clouds form mostly in the polar regions because the mesosphere is the coldest in that region. 

Noctilucent Cloud Observation

Nlc clouds are mostly found colourless or pale blue, but occasionally other colours such as red and green are also observed. The attributes of blue colour come from absorption by ozone in the path of sunlight brightening the Nlc clouds. The Nlc clouds appear as featureless bands, but frequently show different patterns such as streaks,  waves, and wavelike undulations.

The Noctilucent occurs during summer from mid-May to mid-August in the northern hemisphere and between mid-November to mid-February in the southern hemisphere. The clouds are very faint and tenuous and may be observed only in twilight around sunrise and sunset when the clouds of the lower atmosphere are in the shadow, but the Nlc clouds are brightened by the Sun.  The clouds are best observed when the Sun is between 6° and 16° below the horizon.

Although night-shining clouds are found in both the hemisphere, they have been observed thousands of times during the northern hemisphere and fewer than 100 times during the southern hemisphere. 

Also, Nlc clouds are made up of small crystals which are not noticeable to the viewer on the ground because they cannot disperse enough light. The size of the crystals may be 30 mm or less.

Noctilucent Cloud  Forms

The noctilucent cloud comes in different forms and patterns. As per the identification scheme introduced by Fogle in 1970, the clouds are classified in five different terms. This classification is further modified and subdivided. In view of the recent research, the World Meteorological Organization now observed four major forms that can be subdivided. The four major forms are:

  • Type 1 veils are very fragile and lack definite structure, similar to cirrostratus or inadequately defined cirrus.  

  • Type 2 bands are long streaks that rarely appear in roughly parallel groups, usually more widely spaced than the bands or elements seen with cirrocumulus clouds. 

  • Type 3 billows are arranged in a closed-space, roughly parallel short streaks that most often look like cirrus. 

  • Type 4 whorls are more partial, or more often complete rings of cloud with dark centres. 

Did You Know?

  • NLC clouds are the highest cloud in the sky, growing at the edge of space 50 miles above the Earth’s surface.

  • Nlc clouds exist in the atmosphere mesosphere layer.

  • Nlc clouds are the newest clouds that we all have observed. Scientists first observed the Nlc clouds in 1885 after the same famous explosion of the Krakatoa volcano.

  • Nlc clouds occur during summer from mid-May to mid-August in the northern hemisphere and between mid-November and mid – February in the southern hemisphere.