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Tuesday, 14 July 2015

NATURAL DISASTERS



Natural Disaster
                “Any natural phenomenon which may cause loss of life and property for man is called Natural disaster”. Volcanism, landslides, desertification, floods, cyclones, earthquakes and forest fires are such natural phenomena which cause destruction for mankind. Let us have a look on these natural disasters.
1.     Volcanism
        The formation of molten rock material (Magma) inside the earth and the process of its coming out on the earth surface is called Volcanism. The magma when comes on the surface of earth is called lave and it burns and destroys everything that comes in its way. Sometimes it comes out with an explosion and causes an earthquake. Sometimes volcanic ash also comes out with lava and gases during volcanism. This ash may rise in the atmosphere up to several miles and causes environmental pollution.
Volcanism in Pakistan
        Pakistan is fortunate that even lying in an active vibrant region, no dangerous and active volcano lies within its boundaries. However some volcanic activates have been traced in some places of Hindu Kush mountain ranges and Baluchistan.
Safety measures
        To mitigate loss of life and property in areas vulnerable to volcanism, an integrated monitoring system of volcanoes has been adopted throughout the world. In case of emergency, a warning is declared in the hazard zone to make people prepared to combat the disaster.
2.     Landslides
        Down slope movement of soil and weathered rock material under the influence of gravity is called landslide”. It may create an impact in many ways. It may cause loss of life and property. It may damage the construction severely. It may damage the construction severely. It may block the roads and damage the communication lines. It may block the flow of rivers i.e. the creation of Arababad Lake in Gilgit is the result of river blockade by landslides. It may disturb the agricultural productivity in the affected areas.
Landslides in Pakistan
        The northern areas of Pakistan are affected by landslides during the rainy season. Due to the construction of roads the slopes become unstable and vulnerable to landslides. Karakoram highway which connects Pakistan to China often remains blocked due to landslides. The unchecked tree cutting in mountainous areas of Pakistan is also a main cause of landslides.
Safety measures
        Methods of slope stabilization can be adopted in areas vulnerable to landslides to reduce their effects. Impacts of landslides can also be reduced by lowering the water table underground, by improving the irrigation system, by avoiding construction, by stopping unchecked tree cutting and by growing trees in the affected areas.
3.     Desertification
        The extension of deserts at the expense of cultivable lands is called desertification. Although climate chances have always favored the process of desertification, but human induced activities, especially after the industrial revolution are very much responsible for increasing desertification. Due to this menace, agricultural production and usable water resources are depleting and migration of humans and wildlife from the affected areas in increasing. As a result shortage of food, drought and increase in poverty at local level may occur.
Desertification in Pakistan
        Pakistan is situated in warm and dry climatic region where the annual amount of rainfall is less than 25 centimeters. Arid to semi-arid weather conditions prevail in almost 80% area of Pakistan. The main cause of desertification in Pakistan is unsafe and poor ways of cultivation which result in soil erosion, lapse of fertility, and continuous drop in biodiversity.
Safety measures
        To combat desertification, tree plantation can favor in two ways. Firstly, it reduces desertification by keeping weather conditions moderate. Secondly it acts as hurdle to stop the spread of desertification towards cultivable areas. The use of organic fertilizers can enhance the fertility of land. People can be made aware about desertification and methods to stop it. Unchecked cutting of trees should be discouraged and modern ways of cultivation and irrigation should be adopted to stop desertification.
4.     Floods
        An overflow of river water out of its channel, which may cause damage to the nearby settlements, is called flood. It is considered a natural disaster because it may be a cause of social and environmental degradation. It can damage any constructional frame work, uncommented housing and buildings without deep foundations. It may destroy bridges, roads, communication lines, crops, farms, orchards, livestock and cultural monuments as well. Loss of lives especially of women, children and aged can occur, along with the spread of diseases and epidemics.
Floods in Pakistan
        Pakistan has a natural system of rivers flowing out of the northern mountain ranges. These mountain ranges are a home of huge glaciers outsides the polar areas. Melt-water streams from glaciers feed these rivers. The upper plains of these rivers are situated in the rainy monsoon region. In summers the monsoon rains along with the melt water streams from glaciers cause heavy flooding in the rivers of Pakistan.
Safety measures
        Awareness about the flood risks should be given to the people of areas vulnerable to floods. Evacuation plan should be prepared to get people out of the area safely. Electricity and gas supplies should be disconnected to avoid any accident. Camps should be established in safe areas to provide shelter and food to the affecters. Proper arrangements should be made for the return of affecters to their homes. Efforts should be made on governmental and non-governmental side for reconstruction of houses and rehabilitation of the affecters.
5.     Cyclones
        Cyclone is a system of swirling winds which has low pressure area in the center. The winds tend to circulate toward the center and produce rain with thunder and lightning. Wind speed exceeds up to 200 kilometers per hours. The winds have erosive power which destroys everything that comes in their way. Cyclones produce continuous rainfall in a short period of time which may cause flooding and loss of life and property. In coastal areas huge sea waves called storm surges are generated which may cause destruction on a large scale.
Cyclones in Pakistan
        Arabian Sea lies in the south of Pakistan. In Indian Ocean, this is an important area of the origin of tropical cyclones. These cyclones affect the coastal areas of Pakistan. Thatta and Badin in sindh, while jeewani, Gwadar and Lasbela in Balochistan are the main areas affected by the cyclones. Inadequate construction methods and inferior construction material, absence of laws of land use, lack of awareness of the local people, lack of education and poverty are the main causes of destruction caused by cyclones.
Safety measures
        Construction of resistant houses should be made possible. Forecast management system should be established in areas vulnerable to cyclones. As soon as the warning is given, arrangements should be made to shift the livestock and house hold items to safe places. Evacuation system should be established and mobilization of volunteers in the affected areas should be made possible. In case of evacuation, the house should be sealed after disconnecting power supplies. A risk map should be prepared about the estimation of extent and storage of drinking water, food, candles, matches and first aid material should be made possible. Keep in touch with radio and report to emergency rescue centers established by the government.

6.     Earthquakes
        Sudden and intense vibration of the earth crust is called Earthquake. As this is a sudden movement without any pre-occurring symbols, prediction of earthquake is not possible. Earthquakes destroy human settlements, buildings and infrastructure i.e. bridges, roads, railway lines, pipelines, water tanks and communication etc. indirect damages include fire, loss of water reservoirs, and landslides etc. the most unrecoverable damage caused by the earthquake is the loss of valuable lives.
Earthquakes in Pakistan
        Geologically Pakistan lies in an active zone at the margin of three tectonic plates. Indian plate is converging with the Eurasian plate in the north and Arabian plate in the west. The geologic result of this convergence is the formation of Karakoram, Himalayas and the Hindu Kush mountain ranges in the north and northwest. This convergent boundary is also responsible for the occurrence of earthquakes in Pakistan and adjacent areas.





       


       
       
       

Topic Ocean and Seas,,, Movement of ocean water



Movement of ocean water
        Ocean water never remains stagnant. It tends to move. Main causes of this movement are waves, currents and tides. Let us have a look on nature and causes of these movements.
1.     Waves
        The movement of surface water is called wave. Waves in an ocean are generated due to different natural factors. Actually it is the movement of energy which is transferred in water particles from one to another.
Nature
        The top of the wave is called crest and the bottom is called Trough. The vertical distance between crest and trough is called wave height. While the horizontal distance between two crests or troughs is called wave length. As the wave travels towards the shallow waters of the coast, its height increases and length decreases. The crest gets narrower and sharp. This called Breaker. The sharp pointed crest travels ahead of the bottom part and breaks to make foam. This is called surf.
Causes
        Winds are the main cause of generating waves. Cyclones and tornadoes which originate and travel across the ocean also create waves. An earthquake near coastal areas or beneath the ocean floor can also generate huge waves.
2.     Currents
        Rivers flow on land. Similarly when the ocean water moves permanently in a specific direction, it is called current.
Nature
        The currents which flow from equator to polar areas are called Warm currents. They increase the temperatures of coastal areas e.g. Gulf Stream along the eastern coast of North America in the Atlantic Ocean is a warm current. The currents which flow form polar areas to equator are called cold currents e.g. Labrador Current in Atlantic and Kamchatka current in the Pacific Ocean are cold currents. Currents move clockwise in the northern hemisphere and anti-clock wise in the southern. A larger current forming by the joining of two currents is called Drift. Where warm currents meet cold currents, fog is produced which is harmful for the sailing ships.
Causes
        Following are the major causes of current circulation.
i)      Permanent winds
        The most important cause of current circulation is winds. Winds force the ocean water to circulate in their general direction e.g. trade winds blow from east to west, while western winds blow from west to east. So the currents move eastwards under trade winds and vice versa under western wind.
ii)     Temperature of the ocean water
        Temperature difference id another cause of current circulation. Warmer water of equatorial regions moves upwards, while colder water of Polar Regions sinks downwards due to greater density.
iii)    Salinity of ocean water
        Salinity variation also causes the ocean water to circulate. Water of inland seas is more saline than the water of open seas and oceans. So more saline water due to its greater density sinks do downwards while less saline water moves upward.
3.     Tides
        There is a continuous rise and fall in sea level. Twice a day, the level rises and twice a day the level falls as well. This is called tides.
Causes
        The basic cause of tides is the gravitation of moon. This reality was presented by Newton in his “Theory of Gravitation” in the seventeenth century. According to this theory every two celestial bodies attract each other. So the moon, which is nearest to the earth, creates tides on earth inspire of its lesser mass as compared to the sun. Sun, as compared to moon, is 390 times more distant from the earth. So the effect of sun’s gravitation is 46% of the moon’s gravity on the earth.
Nature
        According to nature, there are two types of tides.
i)      Daily tides
        Daily tides occur twice with the interval of 12 hours 25 minutes. The effect of gravitation is maximum on the other side. But the centrifugal forces of the earth maintain balance of tides on the other side too. So the effect of gravitation is equal on both sides of the earth.
ii)     Monthly Tides
        These are of two types.
        Spring tides
        The earth revolves around the sun and the moon revolves around the earth. During this revolution it happens twice on the 1st and 14th date in a lunar month that the moon, earth and sun are in the same plane. The combined gravitation of sun and moon create very high tides. These are called spring tides.
        Neap tides
        Twice in the lunar month on the 7th and 21st date, it happens that the moon and sun are perpendicular to each other with reference to the earth. Gravitation of both bodies counteracts each other resulting in the creation of low tides. These are called Neap tides.

Ocean and Seas, Configuration of Ocean Floor



Configuration of Ocean Floor

Like the earth, the surface of ocean floor is not uniform as well. The undulation ocean floor is divided into following parts.
i)      Continental shelf
        The shallow part of sea which lies adjacent to the coastal areas is called continental shelf. This part of ocean is of vital importance form the geographical, political and economic point of view. A country’s maritime borders, rights of mining and fishing, trade routes and strategic planning depends upon continental shelf.
ii)     Continental slope
        The gentle sloping continental shelf ends at a steep slope which descends into the deep ocean. This is called continental slope.
iii)    Submarine trenches/canyons
        The continental slope merges into the deepest part of the ocean which comprise of narrow and deep v-shaped canyons called trenches. These trenches descend up to 10 kilometers under water.
iv)    Ocean Basin and Mid- Oceanic Ridges
        The mid portion of ocean is usually comprised of vast undulation plain. This part has an average depth of 4500 to 6000 meters. Volcanoes are also found in this portion in a series of a non-ending very long ridge. This is called Mid-Oceanic ridge formed by the eruption of magma at divergent plate boundary.