Volcanoes
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Volcanoes form when molten rock flows from fissures in the Earth's surface caused by movement of tectonic plates. Volcanoes are classified as active, extinct, or dormant based on eruption likelihood. Active volcanoes frequently erupt, like Mount Etna and Mount Fujiyama. Extinct volcanoes were once active but will not erupt again, such as Kilimanjaro. Dormant volcanoes erupted in the past but are not currently active, though they could become active again, for example Vesuvius in Italy.
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This document discusses different types of volcanoes and mountains. It describes volcanoes as being caused by molten rock flowing through fissures in the earth's surface. Volcanoes are classified as active, extinct, or dormant based on their eruption patterns. There are four types of mountains based on their origin: fold mountains formed by faulting, block mountains also formed by faulting, relict mountains formed by erosion of old mountains, and volcanic mountains associated with volcanic activity. The document also briefly mentions various landforms caused by erosion from running water like V-shaped valleys, waterfalls, flood plains, and deltas.
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This document appears to be an intervention material for teaching about the three main types of volcanoes: cinder cones, composite volcanoes, and shield volcanoes. It includes descriptions of each type of volcano along with examples. There are also activity and assessment sections that ask students to classify volcanoes and illustrate similarities and differences between the three types in a Venn diagram. The overall goal seems to be helping students learn the distinguishing characteristics of cinder cones, composite volcanoes, and shield volcanoes.
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This document provides information about different types of volcanoes. It describes volcanoes as vents where hot gases, rocks, and lava are ejected from the Earth's surface. Volcanoes form at plate boundaries, and can also form when plates separate under the ocean. The document then classifies volcanoes according to their shape (cinder cone, shield, composite) and activity level (active, dormant, extinct). Specific examples are given for each type of volcano classification.
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This document discusses volcanoes and their characteristics. It describes the four main types of volcanoes: fissure, cinder cone, shield, and composite. Fissure volcanoes erupt through long vents and produce flood lavas. Cinder cone volcanoes have steep sides and short eruptions producing loose cinders. Shield volcanoes have gentle slopes and erupt fluid basaltic lava over long periods. Composite volcanoes are large mountains that erupt tephra and lava, building their size over millions of years. Volcanoes can be active, dormant, or extinct depending on their recent eruption history, and they produce both primary hazards during eruptions and secondary hazards after.
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The document describes different features of two main types of volcanoes: composite volcanoes and shield volcanoes. Composite volcanoes have thick, sticky lava and steep slopes, while experiencing very violent eruptions. Shield volcanoes contain thin, runny lava and have gentle slopes, forming from less violent eruptions. The document includes diagrams of the volcano types and tasks for students to label features and compare the characteristics of composite and shield volcanoes.
Why volcanoes erupt?
Volcanoes erupt due to tremendous pressure from magma building up in magma chambers under the earth's surface. The heat from the earth's core partially melts rock, forming new magma, which rises into magma chambers until the pressure causes it to burst through openings or craters in volcanoes. Eruptions can be violent if the magma is rich in gas and silica, or nonviolent if it contains less gas and silica. Volcanic eruptions can have both beneficial effects such as fertile soil and geothermal power, as well as harmful effects like loss of life from lava flows, damage to aircraft from ash plumes, and impacts on global climate from volcanic gases.
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This document discusses different types of volcanoes. It provides descriptions of cinder cones, shield volcanoes, composite volcanoes, and lava domes. Cinder cones are symmetrical cones up to 1,200 feet tall formed from a single vent. Shield volcanoes are very broad with shallow slopes and can be over 30,000 feet tall. Composite volcanoes are also known as stratovolcanoes, ranging from 1-10 km wide and up to 10,000 feet tall with steep slopes. They have explosive, dangerous eruptions. Lava domes are much smaller formations that occur when lava is too viscous to flow, piling up in a dome shape around 100 feet tall. Examples of each type
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This document discusses different types of volcanoes and mountains. It describes volcanoes as being caused by molten rock flowing through fissures in the earth's surface. Volcanoes are classified as active, extinct, or dormant based on their eruption patterns. There are four types of mountains based on their origin: fold mountains formed by faulting, block mountains also formed by faulting, relict mountains formed by erosion of old mountains, and volcanic mountains associated with volcanic activity. The document also briefly mentions various landforms caused by erosion from running water like V-shaped valleys, waterfalls, flood plains, and deltas.
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This document appears to be an intervention material for teaching about the three main types of volcanoes: cinder cones, composite volcanoes, and shield volcanoes. It includes descriptions of each type of volcano along with examples. There are also activity and assessment sections that ask students to classify volcanoes and illustrate similarities and differences between the three types in a Venn diagram. The overall goal seems to be helping students learn the distinguishing characteristics of cinder cones, composite volcanoes, and shield volcanoes.
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This document discusses volcanoes and their characteristics. It describes the four main types of volcanoes: fissure, cinder cone, shield, and composite. Fissure volcanoes erupt through long vents and produce flood lavas. Cinder cone volcanoes have steep sides and short eruptions producing loose cinders. Shield volcanoes have gentle slopes and erupt fluid basaltic lava over long periods. Composite volcanoes are large mountains that erupt tephra and lava, building their size over millions of years. Volcanoes can be active, dormant, or extinct depending on their recent eruption history, and they produce both primary hazards during eruptions and secondary hazards after.
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The document describes different features of two main types of volcanoes: composite volcanoes and shield volcanoes. Composite volcanoes have thick, sticky lava and steep slopes, while experiencing very violent eruptions. Shield volcanoes contain thin, runny lava and have gentle slopes, forming from less violent eruptions. The document includes diagrams of the volcano types and tasks for students to label features and compare the characteristics of composite and shield volcanoes.
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Volcanoes erupt due to tremendous pressure from magma building up in magma chambers under the earth's surface. The heat from the earth's core partially melts rock, forming new magma, which rises into magma chambers until the pressure causes it to burst through openings or craters in volcanoes. Eruptions can be violent if the magma is rich in gas and silica, or nonviolent if it contains less gas and silica. Volcanic eruptions can have both beneficial effects such as fertile soil and geothermal power, as well as harmful effects like loss of life from lava flows, damage to aircraft from ash plumes, and impacts on global climate from volcanic gases.
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This document discusses different types of volcanoes. It provides descriptions of cinder cones, shield volcanoes, composite volcanoes, and lava domes. Cinder cones are symmetrical cones up to 1,200 feet tall formed from a single vent. Shield volcanoes are very broad with shallow slopes and can be over 30,000 feet tall. Composite volcanoes are also known as stratovolcanoes, ranging from 1-10 km wide and up to 10,000 feet tall with steep slopes. They have explosive, dangerous eruptions. Lava domes are much smaller formations that occur when lava is too viscous to flow, piling up in a dome shape around 100 feet tall. Examples of each type
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The document describes the three main types of volcanoes:
1) Cinder cone volcanoes are the simplest type, forming small, steep conical hills from accumulated cinder around the vent. Examples are Mt. Paricutin in Mexico and Sunset Crater in Arizona.
2) Composite volcanoes have steep, symmetrical cones like Mt. Fuji in Japan and Mt. Hood in Oregon.
3) Shield volcanoes have broad, gently sloping dome shapes resembling a warrior's shield, such as Mauna Loa and Kilauea in Hawaii.
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Volcanoes are cone-shaped landforms with an opening at the top or sides that allow hot, thick clouds of gas, molten rock, and ash to escape. According to PHIVOLCS, volcanoes are classified as either active if they have erupted within the last 600 years or 10,000 years ago based on analysis, or inactive if they have not erupted in over 10,000 years and are being eroded through weathering.
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This document provides information about volcanoes and volcanic eruptions. It begins with a 10 question pre-assessment about volcanic characteristics and types. It then discusses the classification of volcanoes as active or inactive. Key details are provided about iconic Philippine volcanoes like Mayon and Taal. The different types of volcanic eruptions such as Plinian and Strombolian are described. Finally, the document discusses the factors that affect eruption style and provides signs of an impending eruption.
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Volcanoes form when magma rises up through fissures in the Earth's crust caused by movement of tectonic plates. The opening where magma emerges onto the surface is called a vent, and the funnel-shaped depression at the top of an erupting volcano is termed a crater. Active volcanoes frequently erupt, while dormant volcanoes were active in the past but are not currently erupting, though they could become active again. Areas around volcanoes are rich in minerals and some have developed healing hot springs, fertile soil, and tourist attractions.
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Volcanoes form in different types depending on the composition of the magma and tectonic setting, with shield volcanoes being non-explosive and forming from basalt in oceanic settings, composite volcanoes sometimes having explosive eruptions from more viscous magma in continental settings, and cinder cones being the smallest from pyroclastic eruptions.
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The document describes 6 volcanoes - Mt. Kiska, Mt. Iliamna, Carlisle, Kanaga Volcano, Kasatochi Volcano. Mt. Kiska and Mt. Iliamna are described as active stratovolcanoes located in Alaska. Carlisle is described as an inactive volcano located off Alaska's coast consisting of a single symmetric cone. Kanaga Volcano is described as an active composite cone located in the Aleutian Islands built of interbedded lava flows. Kasatochi Volcano is described as an inactive volcano located in the Aleutians represented by a dissected cone with a central crater.
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This document discusses different types of volcanoes and their characteristics. It describes three main types: composite volcanoes, cinder cones, and shield volcanoes. Composite volcanoes are large, steep mountains formed from layers of lava and pyroclastic material. They often have small craters and include volcanoes like Krakatoa. Cinder cones are small, steep mountains composed of hardened volcanic cinders and ash. Shield volcanoes are enormous mountains thousands of kilometers high, like Mauna Loa, formed from numerous mild lava flows. The document provides details on the components and eruptive behaviors of each type.
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Volcanoes form when molten magma forces its way through cracks in the Earth's crust. They can take cone shapes but also other forms. The melted rock that emerges from the volcano's crater is called lava, which destroys everything in its path due to its extreme heat. Most volcanoes occur on land, but some exist on the ocean floor and can emerge from the water if tall enough. Volcanoes erupt when magma and gases find a way to escape through vents to the surface. Eruptions can be gentle or violent.
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Volcanoes are openings in the Earth's crust that eject lava, pyroclasts, and gases during eruptions. They consist of cones formed from accumulated volcanic materials and craters or calderas at the peak. Magma located below ground hardens into lava when it reaches the surface. Volcanoes can be cinder cones, shield cones, or composite cones depending on their composition and shape. They can be active, dormant, or extinct based on activity levels and pose dangers like gases, lava flows, and lahars during eruptions but also provide agricultural, energy, industrial, and tourism benefits.
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This document defines volcanoes as openings in the Earth's crust that allow molten rock and gases to escape. It notes that over half of the world's active volcanoes above sea level are located along the Ring of Fire. Volcanoes form when tectonic plates collide, spread apart, or interact under a plate. The parts of a volcano include the crater, pipe, cone, and vent. There are three main types of volcanoes: composite/strato volcanoes, shield volcanoes, and cinder cone volcanoes. Volcanic eruptions can have both beneficial effects like adding nutrients to soil or creating new islands, and harmful effects like releasing aerosols or abandoning land.
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The document provides information about different types of volcanoes and volcanic features including:
- Shield volcanoes which are built by basalt lava flows and have gentle slopes.
- Lava domes which are built by thick, viscous lava that cools too quickly to flow very far from the eruption.
- Cinder cones which are steep sided hills made of volcanic fragments blown from eruptions of stratovolcanoes.
- Stratovolcanoes which have steep sides and are formed by violent eruptions of lava flows, tephra, and pyroclastic flows from multiple vents.
- Mud volcanoes which form from eruptions of wet
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There are several main types of volcanoes classified based on their shape, eruptive behavior, and composition. Composite volcanoes, also known as stratovolcanoes, are conical mountains built up by viscous lava flows and explosive eruptions, examples being Mount St. Helens and Mount Pinatubo. Shield volcanoes are larger and less steeply sloped, constructed by fluid basaltic lava flows like those of Hawaii. Small cinder cones form from explosive eruptions of pyroclastic material. Fissure eruptions produce fluid lava flows from cracks in the crust along zones of weakness.
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Volcanoes are openings in the Earth's crust that allow magma, ash, and gases to escape from below the surface. There are three types of volcanoes: active, dormant, and extinct. Magma is molten rock underground, while lava is magma that flows out of a volcano. Ash, cinders, and pumice are other materials emitted from volcanoes. Over half of the world's volcanoes are located on the Ring of Fire around the Pacific Ocean. Volcanic eruptions are caused by the movement of tectonic plates, which squeezes magma up in between. Eruptions can endanger people through lava, tsunamis, earthquakes, and toxic gases
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There are three main types of volcanoes that form from different geological processes:
1) Hotspot volcanoes like those in Hawaii form when magma rises from a hotspot in the mantle as a tectonic plate moves over it. Eruptions are less explosive due to fluid magma.
2) Shield volcanoes form at divergent plate boundaries and from hotspots, with low, wide shapes from fluid basaltic magma.
3) Composite volcanoes form at convergent plate boundaries, where one plate subducts under another. They have steep sides due to more viscous magma and explosive eruptions, producing hazards like pyroclastic flows and lahars.
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A supervolcano eruption would have devastating effects. Supervolcanoes emit over 1,000 km3 of material and form calderas, which are large depressions formed by the partial emptying of magma chambers. An eruption of the Yellowstone supervolcano would fling magma 50 km into the air and kill all life within 1,000 km through falling ash, lava flows, and the force of the explosion. 100 km3 of lava would flow from the volcano and ash would block the sun, triggering a freezing cold volcanic winter that could cause crop failure and starvation as economies collapse.
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Volcanoes can cause deadly hazards such as pyroclastic flows that move at 200km/h and contain poisonous gases and rocks. Ash clouds from eruptions can lead to suffocation and building collapses, while volcanic bombs and lava can destroy buildings and crops. Poisonous gases like carbon monoxide and sulfur can cause acid rain. Supervolcanic eruptions eject over 1,000 cubic km of material and form caldera depressions, with the last one occurring 74,000 years ago in Indonesia. Yellowstone sits over a hotspot and has experienced enormous eruptions in the past forming calderas.
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The document describes the three main types of volcanoes:
1) Cinder cone volcanoes are the simplest type, forming small, steep conical hills from accumulated cinder around the vent. Examples are Mt. Paricutin in Mexico and Sunset Crater in Arizona.
2) Composite volcanoes have steep, symmetrical cones like Mt. Fuji in Japan and Mt. Hood in Oregon.
3) Shield volcanoes have broad, gently sloping dome shapes resembling a warrior's shield, such as Mauna Loa and Kilauea in Hawaii.
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Volcanoes are cone-shaped landforms with an opening at the top or sides that allow hot, thick clouds of gas, molten rock, and ash to escape. According to PHIVOLCS, volcanoes are classified as either active if they have erupted within the last 600 years or 10,000 years ago based on analysis, or inactive if they have not erupted in over 10,000 years and are being eroded through weathering.
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This document provides information about volcanoes and volcanic eruptions. It begins with a 10 question pre-assessment about volcanic characteristics and types. It then discusses the classification of volcanoes as active or inactive. Key details are provided about iconic Philippine volcanoes like Mayon and Taal. The different types of volcanic eruptions such as Plinian and Strombolian are described. Finally, the document discusses the factors that affect eruption style and provides signs of an impending eruption.
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Volcanoes form when magma rises up through fissures in the Earth's crust caused by movement of tectonic plates. The opening where magma emerges onto the surface is called a vent, and the funnel-shaped depression at the top of an erupting volcano is termed a crater. Active volcanoes frequently erupt, while dormant volcanoes were active in the past but are not currently erupting, though they could become active again. Areas around volcanoes are rich in minerals and some have developed healing hot springs, fertile soil, and tourist attractions.
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Volcanoes form in different types depending on the composition of the magma and tectonic setting, with shield volcanoes being non-explosive and forming from basalt in oceanic settings, composite volcanoes sometimes having explosive eruptions from more viscous magma in continental settings, and cinder cones being the smallest from pyroclastic eruptions.
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Volcanoes form when molten magma forces its way through cracks in the Earth's crust. They can take cone shapes but also other forms. The melted rock that emerges from the volcano's crater is called lava, which destroys everything in its path due to its extreme heat. Most volcanoes occur on land, but some exist on the ocean floor and can emerge from the water if tall enough. Volcanoes erupt when magma and gases find a way to escape through vents to the surface. Eruptions can be gentle or violent.
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Volcanoes are openings in the Earth's crust that eject lava, pyroclasts, and gases during eruptions. They consist of cones formed from accumulated volcanic materials and craters or calderas at the peak. Magma located below ground hardens into lava when it reaches the surface. Volcanoes can be cinder cones, shield cones, or composite cones depending on their composition and shape. They can be active, dormant, or extinct based on activity levels and pose dangers like gases, lava flows, and lahars during eruptions but also provide agricultural, energy, industrial, and tourism benefits.
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This document defines volcanoes as openings in the Earth's crust that allow molten rock and gases to escape. It notes that over half of the world's active volcanoes above sea level are located along the Ring of Fire. Volcanoes form when tectonic plates collide, spread apart, or interact under a plate. The parts of a volcano include the crater, pipe, cone, and vent. There are three main types of volcanoes: composite/strato volcanoes, shield volcanoes, and cinder cone volcanoes. Volcanic eruptions can have both beneficial effects like adding nutrients to soil or creating new islands, and harmful effects like releasing aerosols or abandoning land.
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The document provides information about different types of volcanoes and volcanic features including:
- Shield volcanoes which are built by basalt lava flows and have gentle slopes.
- Lava domes which are built by thick, viscous lava that cools too quickly to flow very far from the eruption.
- Cinder cones which are steep sided hills made of volcanic fragments blown from eruptions of stratovolcanoes.
- Stratovolcanoes which have steep sides and are formed by violent eruptions of lava flows, tephra, and pyroclastic flows from multiple vents.
- Mud volcanoes which form from eruptions of wet
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There are several main types of volcanoes classified based on their shape, eruptive behavior, and composition. Composite volcanoes, also known as stratovolcanoes, are conical mountains built up by viscous lava flows and explosive eruptions, examples being Mount St. Helens and Mount Pinatubo. Shield volcanoes are larger and less steeply sloped, constructed by fluid basaltic lava flows like those of Hawaii. Small cinder cones form from explosive eruptions of pyroclastic material. Fissure eruptions produce fluid lava flows from cracks in the crust along zones of weakness.
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Volcanoes are openings in the Earth's crust that allow magma, ash, and gases to escape from below the surface. There are three types of volcanoes: active, dormant, and extinct. Magma is molten rock underground, while lava is magma that flows out of a volcano. Ash, cinders, and pumice are other materials emitted from volcanoes. Over half of the world's volcanoes are located on the Ring of Fire around the Pacific Ocean. Volcanic eruptions are caused by the movement of tectonic plates, which squeezes magma up in between. Eruptions can endanger people through lava, tsunamis, earthquakes, and toxic gases
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There are three main types of volcanoes that form from different geological processes:
1) Hotspot volcanoes like those in Hawaii form when magma rises from a hotspot in the mantle as a tectonic plate moves over it. Eruptions are less explosive due to fluid magma.
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3) Composite volcanoes form at convergent plate boundaries, where one plate subducts under another. They have steep sides due to more viscous magma and explosive eruptions, producing hazards like pyroclastic flows and lahars.
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A supervolcano eruption would have devastating effects. Supervolcanoes emit over 1,000 km3 of material and form calderas, which are large depressions formed by the partial emptying of magma chambers. An eruption of the Yellowstone supervolcano would fling magma 50 km into the air and kill all life within 1,000 km through falling ash, lava flows, and the force of the explosion. 100 km3 of lava would flow from the volcano and ash would block the sun, triggering a freezing cold volcanic winter that could cause crop failure and starvation as economies collapse.
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This document outlines a teaching manual for a lesson on Egyptian civilization. It includes details like the name of the teacher, school, subject, unit, and topic. It provides context about Egyptian civilization like its location along the Nile River, use of hieroglyphics for writing, and construction of pyramids to tomb pharaohs. The lesson plan involves introducing the topic, presenting key facts and concepts, and engaging students in activities like discussing hieroglyphics and pyramids in small groups.
Volcanoes
Volcanoes form when molten rock flows from fissures in the Earth's surface caused by movement of tectonic plates. Volcanoes are classified as active, extinct, or dormant based on eruption likelihood. Active volcanoes frequently erupt, like Mount Etna and Mount Fujiyama. Extinct volcanoes were once active but will not erupt again, such as Kilimanjaro. Dormant volcanoes erupted in the past but are not currently active, though they could become active again, for example Vesuvius in Italy.
Innovative
The document is a submission by Sabareesh.P.S for innovative work in physical science. It provides his registration number 13367008 and indicates he is a student at J B M C T C, Kayamkulam.
Parambariyam
This document discusses innovative teaching methods in biology that incorporate local resources and hands-on learning. It provides examples of how various biological components like proteins, lipids, and minerals can be taught about and used to explain their importance in living organisms and the environment. Students are shown experimenting with different biological samples and learning about their structures and roles through discussion. The summary emphasizes hands-on, collaborative learning around real-world examples to help students make deeper connections between biology, their surroundings, and their culture.
Sabareeshpsppt
This PowerPoint presentation summarizes Newton's contributions and laws of motion. Newton developed calculus, proved that white light is composed of rainbow colors, invented the reflecting telescope, and formulated the laws of motion and universal law of gravitation. Newton's First Law, also called the law of inertia, states that an object at rest stays at rest and an object in motion stays in motion with the same speed and in the same direction unless acted upon by an unbalanced force. The presentation explains balanced and unbalanced forces and how inertia increases with increasing mass of an object.
Lesson template of sabareesh.p.s
This document outlines a teaching manual for a physical science lesson on factors affecting acceleration due to gravity. It provides details on the teacher, class, subject, duration, topic, and date. The curricular statement indicates students will generate knowledge on factors affecting gravity through discussion, demonstration, experimentation and evaluation. Learning outcomes include recalling, understanding, applying, analyzing, and creating knowledge related to the topic. The lesson plan follows an inquiry training model in 5 phases from encountering the problem to analyzing thinking strategies.
Innovative work.compressed
This document appears to be a submission for an innovative work project from a student named Sindhya. S. studying Physical Science with a registration number of 13367011 at J B M C T E in Kayamkulam. The document title and student information provide the key details about what is being submitted.
Innovative work
This document appears to be a submission for an innovative work project from a student named Sindhya. S. studying Physical Science with a registration number of 13367011 at J B M C T E in Kayamkulam. The document title and student information provide the key details about what is being submitted.
Lesson template of sabareesh.p.s
This document outlines a teaching manual for a physical science lesson on factors affecting acceleration due to gravity. It provides details on the teacher, class, subject, duration, topic, and date. The curricular statement indicates students will generate knowledge on factors affecting gravity through discussion, demonstration, experimentation, observation and evaluation. Learning outcomes include recalling, understanding, applying, analyzing, and creating knowledge related to the topic. The lesson plan follows an inquiry training model in 5 phases from encountering the problem to analyzing thinking strategies.
Lesson template of sabareesh.p.s
This document outlines a teaching manual for a physical science lesson on factors affecting acceleration due to gravity. It provides details on the teacher, class, subject, duration, topic, and date. It describes the curriculum statement, new terms, facts, concepts, and learning outcomes related to developing different types of knowledge. It outlines the phases of an inquiry training model used in the lesson, including encountering the problem, developing explanations, and analyzing thinking strategies. It also discusses the social system, principles of reaction, support system, and instructional and nurturing effects of the model.
Sabareesh p s ppt
This power point presentation by Sabareesh P.S. summarizes Newton's contributions and laws of motion. Newton developed calculus, demonstrated that white light is composed of rainbow colors, invented the reflecting telescope, and formulated the laws of motion and universal law of gravitation. Newton's First Law, also called the law of inertia, states that an object at rest stays at rest and an object in motion stays in motion with the same speed and in the same direction unless acted upon by an unbalanced force. The presentation provides examples of how friction and gravity cause moving objects to eventually stop due to the unbalanced forces they create.
Lesson template of sabareesh.p.s
This document outlines a teaching manual for a physical science lesson on factors affecting acceleration due to gravity. It provides details on the teacher, class, school, subject, duration, topic, and date. The curricular statement and learning outcomes describe enabling students to generate knowledge on factors affecting gravity through discussion, demonstration, and experimentation. The content analysis lists facts and concepts to be covered. The lesson plan follows an inquiry training model in 5 phases from encountering the problem to analyzing thinking strategies with the goal of developing students' knowledge and process skills related to factors affecting acceleration due to gravity.
Ramya completed
The document discusses the key structures and functions of the human eye. It describes the cornea as a thin protective covering of epithelial cells that protects the eye. It notes that the lens is a transparent, curved structure that focuses light rays onto the retina using refraction. It also explains that the retina is a layer of sensory neurons, including photoreceptors, that respond to light and pass visual impulses to the brain.
Teaching mannuel
This document is a teaching manual for a natural science class on neurons. It provides details on the class such as the teacher's name, school, date, class size and duration. The document outlines the learning outcomes which are to develop students' factual, conceptual, procedural and metacognitive knowledge of neurons. It discusses developing students' process skills like observation and communication. The document also includes an analysis of the content to be covered, pre-requisites, teaching resources and procedures, expected student responses and follow up activities like review questions and assignments.
Teaching manual
The document provides a lesson plan for teaching 8th grade students about the surroundings of Kuttanad in Kerala, India. It includes the name of the teacher, school, subject, unit, topic, learning outcomes, content analysis, concepts, previous student knowledge, and classroom activities. The lesson introduces students to Kuttanad's unique landscape of backwaters, villages on stilts, and way of life. Students learn about Kuttanad's role in Kerala's backwaters network and history as an important trading center. The lesson concludes with a review of key topics and an enrichment activity asking students to research life in Kuttanad or imagine a trip there.
Continents
The document summarizes the seven continents of Earth. It describes the key facts about each continent, such as their relative sizes, countries they contain, and notable geographic features. The seven continents are North America, South America, Europe, Asia, Africa, Australia, and Antarctica.
World religions
Christianity originated around 0 CE and is based on the belief that Jesus Christ was the son of God. The Christian Bible contains both the Old Testament and the New Testament. Islam was founded in the 7th century CE by the prophet Muhammad and believes in one God called Allah. Hinduism originated around 2500 BCE and believes in reincarnation and escaping the cycle of rebirth. Sikhism was founded in the 15th century by Guru Nanak and believes in one powerful God best understood through meditation.
Pendulum
The document is a PowerPoint presentation about the simple pendulum and periodic motion. It defines a simple pendulum as a mass attached to a string that is free to swing back and forth. The motion of the pendulum is periodic, meaning it repeats at regular time intervals. The time taken to complete one full swing from side to side is called the periodic time or period of the pendulum.
Teaching manual sandhy. s
This document outlines a teaching manual submitted by Sindhya S. for a concept attainment model lesson plan. It includes sections on the curriculum statement, learning outcomes in different domains, essential and non-essential attributes, and outlines the three phases of the concept attainment model - presentation of data, testing attainment of the concept, and analysis and thinking strategies. The document provides the framework for a lesson but does not include details on the specific topic, class, or activities.
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Chapter wise All Notes of First year Basic Civil Engineering.pptx
Chapter wise All Notes of First year Basic Civil Engineering
Syllabus
Chapter-1
Introduction to objective, scope and outcome the subject
Chapter 2
Introduction: Scope and Specialization of Civil Engineering, Role of civil Engineer in Society, Impact of infrastructural development on economy of country.
Chapter 3
Surveying: Object Principles & Types of Surveying; Site Plans, Plans & Maps; Scales & Unit of different Measurements.
Linear Measurements: Instruments used. Linear Measurement by Tape, Ranging out Survey Lines and overcoming Obstructions; Measurements on sloping ground; Tape corrections, conventional symbols. Angular Measurements: Instruments used; Introduction to Compass Surveying, Bearings and Longitude & Latitude of a Line, Introduction to total station.
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Chapter 6
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Water Pollution: Water Quality standards, Introduction to Treatment & Disposal of Waste Water. Reuse and Saving of Water, Rain Water Harvesting. Solid Waste Management: Classification of Solid Waste, Collection, Transportation and Disposal of Solid. Recycling of Solid Waste: Energy Recovery, Sanitary Landfill, On-Site Sanitation. Air & Noise Pollution: Primary and Secondary air pollutants, Harmful effects of Air Pollution, Control of Air Pollution. . Noise Pollution Harmful Effects of noise pollution, control of noise pollution, Global warming & Climate Change, Ozone depletion, Greenhouse effect
Text Books:
1. Palancharmy, Basic Civil Engineering, McGraw Hill publishers.
2. Satheesh Gopi, Basic Civil Engineering, Pearson Publishers.
3. Ketki Rangwala Dalal, Essentials of Civil Engineering, Charotar Publishing House.
4. BCP, Surveying volume 1
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Volcanoes
- 1. SUBMITTED BY REMYA. V POWER POINT PRESENTATION
- 3. Volcanoes Volcanoes are causes when molten rock flows out on to the earth’s surface through fissures that are caused due to the movement of plates.
- 4. Based on the chances of eruption the volcanoes are classified in to three 1) Active volcanoes 2) Extinct volcanoes 3) Dormant volcanoes
- 5. ACTIVE VOLCANOES Volcanoes that frequently erupt Eg. Mount Etna Mount Fujiyama
- 7. Extinct volcanoes Volcanoes that active at a time. But with not exrupt again. Eg. Kilimanjaro in Africa
- 8. Dormant Volcanoes Those that have erupted earlier and not acive in the recent past. But can become active Eg. Vesuvius in Italy.