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Descargar WinRar Full Espa EARTHQUAKES AND VOLCANOES - Brainy Key. An earthquake is a sudden movement of the Earth, caused by the abrupt release of strain that has accumulated over a long time. For hundreds of millions of years the forces of plate tectonics have shaped the Earth as the huge plates that form the Earth’s surface slowly move over, under, and past each other. Sometimes the movement is gradual. At other times, the Plates are locked together, unable to release the accumulating energy. When the accumulated energy grows strong enough, the plates break free. The magnitude or intensity of energy released by an earthquake is measured on the Richter scale. The place of the origin of an earthquake is called focus which is hidden inside the earth. The Place on the ground surface which is perpendicular to the buried focus is called . Seismic waves are recorded by an instrument called . But most naturally occurring earthquakes are caused by movement of Pieces of the earth’s surface, which are called tectonic plates. DIFFERENT THEORIES THAT EXPLAIN THE ORIGIN OF EARTHQUAKESFaulting and Elastic Rebound Theory: . In fact, sudden dislocation of rock blocks caused by both tensile and compressive forces trigger immediate earth tremor due to sudden maladjustment of rock blocks. According to the theory, the underground rocks are elastic like rubber and expand when stretched and pulled. The stretching and pulling of crustal rocks due to tensile forces is a slow process. The rocks continue to be stretched so long as the tensile forces do not exceed the elasticity of the rocks but as the tensile forces exceed the rocks elasticity they are broken and broken rock blocks try immediately to occupy their previous positions so that they may adjust themselves. All these Processes occur so rapidly that the equilibrium of the concerned crustal surface is suddenly disturbed and hence earth tremors are caused. Hydrostatic Pressure and Anthropogenic Causes: . A place, which is the seat of an active volcano, is often prone to earthquakes as well. Earthquakes are also caused after a volcanic eruption since the eruption also leads to a disturbance in the position of plates, which either move further or resettle and can result into severe or light tremors. Plate Tectonic Theory. Finally, in the mid- 1. United States and Great Britain came up with a theory that explained why the Earth shook. The theory, called Plate tectonics, is that the Earth’s crust, or lithosphere, is comprised of many Plates that slide over a lubricating asthenosphere layer. Plate tectonics confirms that there are four types of seismic zones. The first follows the line of mid- ocean ridges. Activity is low, and it occurs at very shallow depths’ The Point is that the lithosphere is very thin and weak at these boundaries, so the strain cannot build up enough to cause large earthquakes. Associated with this type of seismicity is the volcanic activity along the axis of the ridges (for example, Iceland, Azores, Tristan da Cunha). The second type of earthquake associated with plate tectonics is the shallow- focus event unaccompanied by volcanic activity. The, San Andreas fault is a good example, of this, so is the Anatolian fault in Northern Turkey. In these faults, two mature plates are scraping by one another. The friction between the plates can. Nevertheless, activity does not always occur along the entire length of the fault during any one earthquake. Origin of the Bermuda volcanoes and Bermuda Rise: History, Observations. Rise development mostly within a belt of rougher. Impacts of Volcanic Gases on Climate, the Environment. Gases from volcanoes give rise to numerous impacts on climate, the environment. But after last season’s struggles, the Volcanoes’ owner figured it was the ideal strategy to build a. PLATE TECTONICS IN A NUTSHELL! A World Map of Volcanoes, Earthquakes, and Plate Tectonics. As they rise and approach the surface. For instance, the 1. San Francisco event was caused by breakage only along the northern end of the San Andreas fault. The third type of earthquake is related to the collision of oceanic and continental plates. One plate is thrust or subducted under the other plate so that a deep ocean trench is produced. In the Philippines, ocean trenches are associated with curved volcanic is- land arcs on the landward plate, for example the Java trench. Along the Peru – Chile trench, the Nazca plate is being subducted under the South American plate which responds by crumpling to form the Andes. This type of earthquake can be shallow, intermediate, or deep, according to its location on the downgoing lithospheric slab. Such inclined planes of earthquakes are known as Benioff. The fourth type of seismic zone occurs along the boundaries of continental plates. Typical of this is the broad swath of seismicity from Burma to the Mediterranean, crossing the. Himalayas, Iran, Turkey, to Gilbraltar. Within this zone, shallow earthquakes are associated with high mountain ranges where intense compression is taking place. Intermediate- and deepfocus earthquakes also occur and are known in the Himalayas and in the Caucasus. The interiors of continental plates are very complex, much more so than island arcs. For instance, we do not yet know the full relationship of the AIps or the East African rift system to the broad picture of plate tectonics. Effects. Landslides and damming of the rivers in highland regions. Causes depression forming lakes. Mountains, Volcanoes and Earthquakes. Volcanoes Factsheet for teachers PDF The last few years have seen the ground in the area begin to rise again. What causes a volcano to erupt and how do scientists predict eruptions? 1 The Secrets of Supervolcanoes. The Legends, Myths, and Science of Volcanoes Mary Jefferson. Online why the earth quakes the story of earthquakes and volcanoes, why the earth quakes the story of earthquakes and volcanoes PDF. May cause faults, thrusts, folds, etc. Formation of cracks or fissures in the epicenter region and sometimes water, mud, gas are ejected from it. Causes the raising or lowering of parts of the sea floor e. This causes “tsunamis” or tidal waves. May change surface drainage & underground circulation of water like the sudden disappearance of springs in some places. Rising and lowering of crustal regions for example in Alaska in 1. Devastation of cities, fires, diseases, etc. Distribution of Earthquakes. The world maps of the distribution of earthquakes prepared by the seismologists on the basis of computer analysis and simulation of 3. Circum Pacific Belt or Ring of Fire surrounding the Pacific Ocean. It is a junction of continental and oceanic margins; it is a zone of young folded mountains; it is a zone of active volcanoes thus this belt accounts for the 6. Mid- Continental Belt representing Alpine- Himalayan chains of Eurasia and northern Africa and epicenters of east African fault zone. This belt represents the collision or subduction zones of continental plates. About 2. 1 per cent of the total seismic events occur in this belt. Mid- Atlantic Belt representing the earthquakes located along the mid- Atlantic Ridge and its offshoots. This belt records moderate and shallow focus earthquakes which are essentially caused due to creation of transform faults and fractures because of divergent movement of plates. VOLCANOESA volcano is an opening or a vent through which heated materials consisting of gases, water, liquid lava and fragments of rocks are discharged. Magma is molten rock within the Earth’s crust. When magma erupts through the earth’s surface it is called lava. Lava can be thick and slow- moving or thin and fast- moving. Rock also comes from volcanoes in other forms, including ash (finely powdered rock that looks like dark smoke coming from the volcano), cinders (bits of fragmented lava) and pumice (light- weight rock that is full of air bubbles and is formed in explosive volcanic eruptions – this type of rock can float on water). As rock inside the earth melts, its mass remains the same while its volume increases–producing a melt that is less dense than the surrounding rock. This lighter magma then rises towards the surface by virtue of its buoyancy. If the density of the magma between the zone of its generation and the surface is less than that of the surrounding and overlying rocks, the magma reaches the surface and erupts. Types of Vulcanic eruption. The most common type of volcanic eruption occurs when magma (the term for lava when it is below the Earth’s surface) is released from a volcanic vent. Eruptions can be effusive, where lava flows like a thick, sticky liquid or explosive, where fragmented lava explodes out of a vent. In explosive eruptions, the fragmented rock may be accompanied by ash and gases; in effusive eruptions degassing is common but ash is usually not. Volcanologists classify eruptions into several different types. Hawaiian Eruption. In a Hawaiian eruption fluid basaltic lava is thrown into the air in jets from a vent or line of vents (a fissure) at the summit or on the flank of a volcano. The jets can last for hours or even days, a phenomenon known as fire fountaining. The spatter created by bits of hot lava falling out of the fountain can melt together and form lava flows, or build hills called spatter cones. Lava flows may also come from vents at the same time as fountaining occurs, or during periods where fountaining has paused. Because these flows are very fluid, they can travel miles from their source before they cool and harden. Strombolian Eruption. Strombolian eruptions are distinct bursts of fluid lava (usually basalt or basaltic andesite) from the mouth of a magma- filled summit conduit. The explosions usually occur every few minutes at regular or irregular intervals. The explosions of lava, which can reach heights of hundreds of meters, are caused by the bursting of Large bubbles of gas, which travel upward in the magma- filled conduit until they reach the open air. This kind of eruption can create a variety of forms of eruptive products: spatter, or hardened globs of glassy lava; scoria, which are hardened chunks of bubbly lava; lava bombs or chunks of lava a few cm to a few m in size; ash; . Products of an explosive eruption . They are one of the least violent of the explosive eruptions. Strombolian eruptions are named for the volcano that makes up the Italian island of Stromboli, which has several erupting summit vents. These eruptions are particularly spectacular at night, when the lava glows brightly. Vulcanian Eruption. A Vulcanian eruption is a short, violent, relatively small explosion of viscous magma (usually andesite, dacite, or rhyolite). This type of eruption results from the fragmentation and explosion of a plug of lava in a volcanic conduit or from the rupture of a lava dome (viscous lava that piles up over a vent). Vulcanian eruptions create powerful explosions in which material can travel faster than 3. 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