This document contains a science lesson on plate tectonics. It begins with welcome messages and learning objectives. It then reviews concepts about convergent plate boundaries through multiple choice questions and answers. Examples and diagrams are provided to illustrate subduction zones and the three types of convergent boundaries. The document continues with a similar format reviewing concepts about divergent plate boundaries through true/false questions. Examples are used to explain the two types of divergent boundaries and the motion and features associated with each.
Divergent plate boundaries occur when two tectonic plates move away from each other. As the plates separate, new crust is formed in between through volcanic activity and magma solidifying. This results in the creation of geological features such as mid-ocean ridges under the ocean or rift valleys on land. Over millions of years, continued separation at divergent boundaries can lead to the formation of new oceans as the crust spreads out.
This document discusses tectonic plates and transform plate boundaries. It notes that tectonic plates are large pieces of rock that make up Earth's crust, and there are two main types - oceanic and continental plates. At transform boundaries, the plates move horizontally past one another, driven by convection currents in the underlying mantle. When the plates rub together at these boundaries, it causes huge stress that results in earthquakes, faults, and tsunamis.
This tacklesabout locating epicenter,3 typesof plate boundaries hotspot.
A ppt presentation for module 1 in 1st quarter in grade 10sciencein the Philippines.
Feel free tomessage mefor any corrections/suggestions forimprovement.
The document describes the four main types of plate boundaries:
1) Divergent boundaries occur at spreading centers where new crust is created and plates move apart, such as at the Mid-Atlantic Ridge.
2) Convergent boundaries exist where plates collide and one is subducted under the other, forming deep ocean trenches.
3) Transform boundaries result from two plates sliding past each other horizontally, such as along the San Andreas Fault.
4) Continent-continent collisions buckle and uplift massive mountain ranges, as when India collided with Asia to form the Himalayas.
This document discusses plate tectonics and how it relates to mountains, earthquakes, and volcanoes. It begins by providing an overview of plate tectonics and the layers of the Earth. It then describes the three types of plate boundaries (divergent, convergent, and transform) and how each results in different geological features and tectonic activity. Specific examples are given of different types of mountains that form at plate boundaries, including folded mountains, fault-block mountains, and volcanic mountains. The document also discusses earthquakes, volcanic eruptions, and the distribution of volcanoes around the world.
1. The document discusses earthquakes and faults, explaining that the Philippines is prone to earthquakes due to its location along the Ring of Fire.
2. It defines a fault as a break in the earth's crust where significant movement has occurred, and explains how faults produce earthquakes through the buildup and sudden release of energy from inside the earth.
3. The document provides information on earthquake waves, intensity scales, and safety tips for both indoors and outdoors during and after an earthquake.
Divergent plate boundaries occur where tectonic plates are moving away from each other. There are two main types of tectonic plates - continental plates composed of rocks and minerals, and oceanic plates which are thinner and located under seas. As the plates separate, molten lava rises up between them to form new crust. This divergence is driven by convection currents in the Earth's mantle which push the plates apart. New crust forms underwater as seafloor spreading, and volcanoes and mountains can form on the edges of the separating plates.
Divergent plate boundaries occur when two tectonic plates move away from each other. As the plates separate, new crust is formed in between through volcanic activity and magma solidifying. This results in the creation of geological features such as mid-ocean ridges under the ocean or rift valleys on land. Over millions of years, continued separation at divergent boundaries can lead to the formation of new oceans as the crust spreads out.
This document discusses tectonic plates and transform plate boundaries. It notes that tectonic plates are large pieces of rock that make up Earth's crust, and there are two main types - oceanic and continental plates. At transform boundaries, the plates move horizontally past one another, driven by convection currents in the underlying mantle. When the plates rub together at these boundaries, it causes huge stress that results in earthquakes, faults, and tsunamis.
This tacklesabout locating epicenter,3 typesof plate boundaries hotspot.
A ppt presentation for module 1 in 1st quarter in grade 10sciencein the Philippines.
Feel free tomessage mefor any corrections/suggestions forimprovement.
The document describes the four main types of plate boundaries:
1) Divergent boundaries occur at spreading centers where new crust is created and plates move apart, such as at the Mid-Atlantic Ridge.
2) Convergent boundaries exist where plates collide and one is subducted under the other, forming deep ocean trenches.
3) Transform boundaries result from two plates sliding past each other horizontally, such as along the San Andreas Fault.
4) Continent-continent collisions buckle and uplift massive mountain ranges, as when India collided with Asia to form the Himalayas.
This document discusses plate tectonics and how it relates to mountains, earthquakes, and volcanoes. It begins by providing an overview of plate tectonics and the layers of the Earth. It then describes the three types of plate boundaries (divergent, convergent, and transform) and how each results in different geological features and tectonic activity. Specific examples are given of different types of mountains that form at plate boundaries, including folded mountains, fault-block mountains, and volcanic mountains. The document also discusses earthquakes, volcanic eruptions, and the distribution of volcanoes around the world.
1. The document discusses earthquakes and faults, explaining that the Philippines is prone to earthquakes due to its location along the Ring of Fire.
2. It defines a fault as a break in the earth's crust where significant movement has occurred, and explains how faults produce earthquakes through the buildup and sudden release of energy from inside the earth.
3. The document provides information on earthquake waves, intensity scales, and safety tips for both indoors and outdoors during and after an earthquake.
Divergent plate boundaries occur where tectonic plates are moving away from each other. There are two main types of tectonic plates - continental plates composed of rocks and minerals, and oceanic plates which are thinner and located under seas. As the plates separate, molten lava rises up between them to form new crust. This divergence is driven by convection currents in the Earth's mantle which push the plates apart. New crust forms underwater as seafloor spreading, and volcanoes and mountains can form on the edges of the separating plates.
The document discusses different types of volcanoes and volcanic eruptions. It describes composite volcanoes which erupt violently due to sticky magma. Shield volcanoes form gentle slopes from runny lava. Cinder cones are small and formed from ejected fragments. Icelandic eruptions come from long fissures building lava plateaus. Hawaiian eruptions also come from fissures, forming shield volcanoes from fluid lava. Strombolian eruptions involve moderate bursts ejecting lava clots.
This document provides information about earthquakes. It begins by defining key earthquake terms like epicenter, hypocenter, foreshocks, aftershocks, and magnitude. It then explains that earthquakes are caused by the sudden slipping of fault blocks within the earth, as the plates of the earth's crust shift. The document discusses how seismographs are used to measure and locate earthquakes by recording seismic waves. It also describes the different scales used to measure earthquake size and intensity. Finally, it provides references for additional information.
Wegener first proposed continental drift in the early 20th century, suggesting that continents were once joined together in a supercontinent called Pangaea. While evidence like matching coastlines and fossil distributions supported drift, Wegener could not explain the forces driving plate motions. In the 1960s, the new theory of plate tectonics emerged, proposing that Earth's outer layer is broken into rigid plates that move over the mantle. At plate boundaries, plates diverge, converge, or slide past each other, creating geological features like mid-ocean ridges and subduction zones. Paleomagnetic and seafloor spreading evidence confirmed plate tectonics, and mantle convection is now understood to be the primary driver of
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
This document discusses different types of mountains and how they are formed. It defines a mountain and differentiates it from a hill. There are two main types of mountains described - volcanic mountains, which are formed from magma piling up at the Earth's surface, and fault-block mountains, which are formed by stresses in the tectonic plates causing blocks of rock to be thrust upwards. Some major mountain ranges provided as examples are the Alps, Himalayas, Andes and Rocky Mountains. References are also provided with links to images of different mountain types and ranges.
Convergent plate boundaries occur where tectonic plates move towards one another. There are three main types:
1) Oceanic-oceanic, where two oceanic plates collide and one subducts under the other, forming ocean trenches.
2) Oceanic-continental, where an oceanic plate subducts under a continental plate, pushing up mountains.
3) Continental-continental, where collision resists subduction and the plates break and fold, forming mountains.
This document provides an overview of transform plate boundaries, including:
1. Transform boundaries are zones where plates slide horizontally past each other with strong deformation but no new lithosphere is created or consumed.
2. There are three types of transform boundaries: ridge-ridge, ridge-trench, and trench-trench. Oceanic transforms form long fracture zones perpendicular to mid-ocean ridges.
3. Examples of prominent ocean fracture zones include the Romanche Fracture Zone and Clipperton Fracture Zone. Continental transforms like the San Andreas Fault accommodate plate motions but have more complex structures.
The document discusses the theory of plate tectonics, including what plates are, how they move, and the three types of plate boundaries. The three types of boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move towards each other; and transform boundaries, where plates move past each other laterally. Each boundary type results in different geologic features and events due to the stresses caused by the ways plates are pulled, pushed, or sheared at their edges.
Continental drift theory and seafloor spreadingJaehadd Untalan
The document discusses continental drift theory and seafloor spreading. Continental drift theory states that the continents were once joined together in a supercontinent called Pangaea before drifting apart. Evidence for this includes matching fossil and rock formations, as well as coal deposits. Seafloor spreading theory developed by Harry Hess and Robert Dietz proposes that new ocean crust is formed at mid-ocean ridges as the continents separate. Evidence includes the age of ocean rocks decreasing with distance from ridges and magnetic reversals in ocean crust.
Earthquakes occur along fault lines where the earth's crust has cracked, forming weak spots. There are two main types of earthquakes - tectonic earthquakes caused by movement of tectonic plates, and volcanic earthquakes caused by volcanic activity. Faults are classified based on the movement under the crust, such as dip-slip, strike-slip, and oblique-slip faults. Active faults are those likely to produce future earthquakes, as movement has occurred within the past 10,000 years, such as the Philippine West Valley Fault Line and Philippine Fault.
The document discusses "The Big One", a potentially powerful earthquake that could hit Metro Manila. It explains that earthquakes are caused by the movement of tectonic plates underground. The West Valley Fault runs through Metro Manila and could produce a 7.2 magnitude earthquake capable of shaking the entire region. The document provides details on fault types, earthquake measurement scales, seismic waves, and tips for preparing for and surviving earthquakes and typhoons.
Earth's outer shell is divided into tectonic plates that slowly move over the mantle below. Plates interact at boundaries where they either converge and collide, causing volcanoes and earthquakes, diverge and form rift valleys and ocean ridges, or slide past each other along transform boundaries, also producing earthquakes. The movement of these plates over geological time scales shapes the earth's surface features and geography.
Earthquake waves and types of faults caused by earthquake Udayram Patil
unstable movement of ground is known as earthquake . Earthquake is transferred by waves known as Primary waves and secondary waves.
Effect of earthquake includes faults. There are three types of faults caused by earthquake .
Plates and list of all major and minor plates in the worldTahsin Islam Ornee
The definition of plates, Earth's interior, Boundaries and the list of the major and minor plates are included in the presentation with images, videos and information.
Scientists in the 1950s used sonar to map the mid-ocean ridge and discovered it was not flat but contained underwater mountains. This discovery led them to research what the ridge was and how it formed. Evidence from molten rock samples, magnetic stripes in the ocean crust, and the ages of rocks drilled from the ocean floor supported Harry Hess' theory from 1960 of sea-floor spreading, where new crust forms at mid-ocean ridges and spreads outward over time.
The document describes how to locate an earthquake's epicenter using data from three seismograph stations. For each station, the difference in arrival times between the P and S waves is calculated and plotted on a travel-time graph to determine the distance to the epicenter. Triangulation is then used to pinpoint the exact epicenter location where the distance circles from each station intersect.
This document provides an introduction to the structure and composition of the Earth's interior. It discusses how scientists have studied the interior without being able to directly explore or probe it. Seismic waves from earthquakes are used to analyze the different layers of the Earth. There are three main layers - the crust, mantle, and core. The core is further divided into a solid inner core and liquid outer core. Activities are included to help students understand these concepts, such as simulating seismic waves and comparing the Earth's layers to those in a hard boiled egg.
1. The document discusses sea-floor spreading, which is the process where new oceanic crust forms at mid-ocean ridges as tectonic plates move away from each other.
2. Evidence that supports sea-floor spreading includes magnetic stripe patterns in the ocean floor and samples from ocean crust that show it is younger near ridges and older further away.
3. Oceanic crust is basaltic rock that forms at ridges and is then recycled in subduction zones, making it generally younger than continental crust which does not undergo this recycling process.
Convection currents in the earth's mantle cause the movement of tectonic plates. Faults form at the boundaries of these plates where the rocks are weak. When stress builds up along fault lines from the movement of plates, it causes the faults to slip suddenly and generate earthquakes. There are three main types of faults - normal, reverse, and strike-slip - which move in different ways due to tensional, compressional, or shear stresses. Active faults have generated earthquakes within the last 10,000 years and may continue to do so, while inactive faults have not produced quakes recently but could still be capable of generating future seismic activity.
The document provides instructions to analyze the process of volcanic eruption by arranging steps 1-5 in the correct order. It then lists 5 events labeled A-E and asks the reader to write the corresponding number for each event. The events are: A) magma accumulates in the magma chamber, B) gas-charged magma reaches the surface and explodes, C) more highly gas-charged magma reaches the surface and the volcano explodes, D) melting of solid rocks forms magma, and E) magma oozes out through openings to form lava domes without explosions.
The document discusses the theory of plate tectonics. It describes how the Earth's crust is broken into plates that move around on top of the mantle due to convection currents in the mantle. There are three types of plate boundaries: convergent where plates collide, divergent where they move apart, and transform where they slide past each other. Convergent boundaries can result in subduction zones, mountain building, or earthquakes depending on the type of plates involved. Divergent boundaries result in seafloor spreading and volcanic activity at mid-ocean ridges.
The document discusses different types of volcanoes and volcanic eruptions. It describes composite volcanoes which erupt violently due to sticky magma. Shield volcanoes form gentle slopes from runny lava. Cinder cones are small and formed from ejected fragments. Icelandic eruptions come from long fissures building lava plateaus. Hawaiian eruptions also come from fissures, forming shield volcanoes from fluid lava. Strombolian eruptions involve moderate bursts ejecting lava clots.
This document provides information about earthquakes. It begins by defining key earthquake terms like epicenter, hypocenter, foreshocks, aftershocks, and magnitude. It then explains that earthquakes are caused by the sudden slipping of fault blocks within the earth, as the plates of the earth's crust shift. The document discusses how seismographs are used to measure and locate earthquakes by recording seismic waves. It also describes the different scales used to measure earthquake size and intensity. Finally, it provides references for additional information.
Wegener first proposed continental drift in the early 20th century, suggesting that continents were once joined together in a supercontinent called Pangaea. While evidence like matching coastlines and fossil distributions supported drift, Wegener could not explain the forces driving plate motions. In the 1960s, the new theory of plate tectonics emerged, proposing that Earth's outer layer is broken into rigid plates that move over the mantle. At plate boundaries, plates diverge, converge, or slide past each other, creating geological features like mid-ocean ridges and subduction zones. Paleomagnetic and seafloor spreading evidence confirmed plate tectonics, and mantle convection is now understood to be the primary driver of
Plate tectonics is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core. The plates act like a hard and rigid shell compared to Earth's mantle. This strong outer layer is called the lithosphere.
This document discusses different types of mountains and how they are formed. It defines a mountain and differentiates it from a hill. There are two main types of mountains described - volcanic mountains, which are formed from magma piling up at the Earth's surface, and fault-block mountains, which are formed by stresses in the tectonic plates causing blocks of rock to be thrust upwards. Some major mountain ranges provided as examples are the Alps, Himalayas, Andes and Rocky Mountains. References are also provided with links to images of different mountain types and ranges.
Convergent plate boundaries occur where tectonic plates move towards one another. There are three main types:
1) Oceanic-oceanic, where two oceanic plates collide and one subducts under the other, forming ocean trenches.
2) Oceanic-continental, where an oceanic plate subducts under a continental plate, pushing up mountains.
3) Continental-continental, where collision resists subduction and the plates break and fold, forming mountains.
This document provides an overview of transform plate boundaries, including:
1. Transform boundaries are zones where plates slide horizontally past each other with strong deformation but no new lithosphere is created or consumed.
2. There are three types of transform boundaries: ridge-ridge, ridge-trench, and trench-trench. Oceanic transforms form long fracture zones perpendicular to mid-ocean ridges.
3. Examples of prominent ocean fracture zones include the Romanche Fracture Zone and Clipperton Fracture Zone. Continental transforms like the San Andreas Fault accommodate plate motions but have more complex structures.
The document discusses the theory of plate tectonics, including what plates are, how they move, and the three types of plate boundaries. The three types of boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move towards each other; and transform boundaries, where plates move past each other laterally. Each boundary type results in different geologic features and events due to the stresses caused by the ways plates are pulled, pushed, or sheared at their edges.
Continental drift theory and seafloor spreadingJaehadd Untalan
The document discusses continental drift theory and seafloor spreading. Continental drift theory states that the continents were once joined together in a supercontinent called Pangaea before drifting apart. Evidence for this includes matching fossil and rock formations, as well as coal deposits. Seafloor spreading theory developed by Harry Hess and Robert Dietz proposes that new ocean crust is formed at mid-ocean ridges as the continents separate. Evidence includes the age of ocean rocks decreasing with distance from ridges and magnetic reversals in ocean crust.
Earthquakes occur along fault lines where the earth's crust has cracked, forming weak spots. There are two main types of earthquakes - tectonic earthquakes caused by movement of tectonic plates, and volcanic earthquakes caused by volcanic activity. Faults are classified based on the movement under the crust, such as dip-slip, strike-slip, and oblique-slip faults. Active faults are those likely to produce future earthquakes, as movement has occurred within the past 10,000 years, such as the Philippine West Valley Fault Line and Philippine Fault.
The document discusses "The Big One", a potentially powerful earthquake that could hit Metro Manila. It explains that earthquakes are caused by the movement of tectonic plates underground. The West Valley Fault runs through Metro Manila and could produce a 7.2 magnitude earthquake capable of shaking the entire region. The document provides details on fault types, earthquake measurement scales, seismic waves, and tips for preparing for and surviving earthquakes and typhoons.
Earth's outer shell is divided into tectonic plates that slowly move over the mantle below. Plates interact at boundaries where they either converge and collide, causing volcanoes and earthquakes, diverge and form rift valleys and ocean ridges, or slide past each other along transform boundaries, also producing earthquakes. The movement of these plates over geological time scales shapes the earth's surface features and geography.
Earthquake waves and types of faults caused by earthquake Udayram Patil
unstable movement of ground is known as earthquake . Earthquake is transferred by waves known as Primary waves and secondary waves.
Effect of earthquake includes faults. There are three types of faults caused by earthquake .
Plates and list of all major and minor plates in the worldTahsin Islam Ornee
The definition of plates, Earth's interior, Boundaries and the list of the major and minor plates are included in the presentation with images, videos and information.
Scientists in the 1950s used sonar to map the mid-ocean ridge and discovered it was not flat but contained underwater mountains. This discovery led them to research what the ridge was and how it formed. Evidence from molten rock samples, magnetic stripes in the ocean crust, and the ages of rocks drilled from the ocean floor supported Harry Hess' theory from 1960 of sea-floor spreading, where new crust forms at mid-ocean ridges and spreads outward over time.
The document describes how to locate an earthquake's epicenter using data from three seismograph stations. For each station, the difference in arrival times between the P and S waves is calculated and plotted on a travel-time graph to determine the distance to the epicenter. Triangulation is then used to pinpoint the exact epicenter location where the distance circles from each station intersect.
This document provides an introduction to the structure and composition of the Earth's interior. It discusses how scientists have studied the interior without being able to directly explore or probe it. Seismic waves from earthquakes are used to analyze the different layers of the Earth. There are three main layers - the crust, mantle, and core. The core is further divided into a solid inner core and liquid outer core. Activities are included to help students understand these concepts, such as simulating seismic waves and comparing the Earth's layers to those in a hard boiled egg.
1. The document discusses sea-floor spreading, which is the process where new oceanic crust forms at mid-ocean ridges as tectonic plates move away from each other.
2. Evidence that supports sea-floor spreading includes magnetic stripe patterns in the ocean floor and samples from ocean crust that show it is younger near ridges and older further away.
3. Oceanic crust is basaltic rock that forms at ridges and is then recycled in subduction zones, making it generally younger than continental crust which does not undergo this recycling process.
Convection currents in the earth's mantle cause the movement of tectonic plates. Faults form at the boundaries of these plates where the rocks are weak. When stress builds up along fault lines from the movement of plates, it causes the faults to slip suddenly and generate earthquakes. There are three main types of faults - normal, reverse, and strike-slip - which move in different ways due to tensional, compressional, or shear stresses. Active faults have generated earthquakes within the last 10,000 years and may continue to do so, while inactive faults have not produced quakes recently but could still be capable of generating future seismic activity.
The document provides instructions to analyze the process of volcanic eruption by arranging steps 1-5 in the correct order. It then lists 5 events labeled A-E and asks the reader to write the corresponding number for each event. The events are: A) magma accumulates in the magma chamber, B) gas-charged magma reaches the surface and explodes, C) more highly gas-charged magma reaches the surface and the volcano explodes, D) melting of solid rocks forms magma, and E) magma oozes out through openings to form lava domes without explosions.
The document discusses the theory of plate tectonics. It describes how the Earth's crust is broken into plates that move around on top of the mantle due to convection currents in the mantle. There are three types of plate boundaries: convergent where plates collide, divergent where they move apart, and transform where they slide past each other. Convergent boundaries can result in subduction zones, mountain building, or earthquakes depending on the type of plates involved. Divergent boundaries result in seafloor spreading and volcanic activity at mid-ocean ridges.
Plate tectonics explains earthquakes and volcanoes, which occur at plate boundaries where plates are moving together or apart. Earthquakes are caused by seismic waves from faults deep in the earth, while volcanoes form where weaknesses in the crust allow magma to reach the surface. Despite hazards, volcanoes are attractive to live near due to fertile soil and tourism opportunities from hot springs and geysers.
The document describes an earthquake that struck the Iranian city of Bam in 2003. The earthquake, measured at 6.6 on the Richter scale, was caused by the pushing together of the Iranian and Arabian tectonic plates. Over 20,000 people were killed when the earthquake destroyed thousands of homes in Bam. Emergency services struggled to help those injured and trapped in the rubble due to damaged roads and collapsed buildings. The earthquake devastated the historic structures in Bam, including the famous 2,000-year-old citadel.
This document provides an overview of the theory of plate tectonics. It explains that the Earth's crust and upper mantle are broken into plates that move around on top of the mantle. There are three main types of plate boundaries: convergent where plates collide, divergent where they move apart, and transform where they slide past each other. Convection currents in the Earth's mantle cause the plates to move by heating and cooling material in the mantle. As plates interact at boundaries, it causes volcanic activity and mountain building at convergent boundaries and new seafloor at divergent ones.
Dia mundial del agua , el agua es vida .pptxjoseobando36
This document provides information about World Water Day, which is celebrated annually on March 20th. It includes the themes of previous years' celebrations, how water relates to the UN's Agenda 2030 for Sustainable Development, fun facts about water, ways to conserve water, how to celebrate World Water Day, the origin of the day, what water is, and how water is a fundamental human right. It also previews the 2022 theme of "Groundwater: Making the Invisible Visible".
This document provides information about the intensive farming technique for growing vaname shrimp (Litopenaeus vannamei) in Indonesia. It discusses the advantages of vaname shrimp such as fast growth rate, high stocking density, high survival rate, and ability to tolerate a wide range of salinities and temperatures. The purpose of the document is to increase knowledge about vaname shrimp farming and understand the farming process from stocking to harvest and post-harvest handling. It describes preparing the ponds, stocking baby shrimp, monitoring water quality, feeding, pest and disease control, and maintenance observations.
- The Earth's crust is made up of tectonic plates that are constantly moving due to convection currents in the mantle.
- There are three types of plate boundaries: divergent where plates separate and new crust is formed, convergent where plates collide and oceanic plates are subducted, and transform where plates slide past each other.
- Evidence for plate tectonics includes magnetic patterns in ocean crust, matching fossils and rock formations on separated continents, and the fit of continental shelves. Plate movements have caused continents like Pangaea to break apart over millions of years.
This document provides a slide presentation on the topic of self-concept. It includes 17 slides with various types of content such as titles, bullet points, images, diagrams, and tables. The slides cover concepts like who we want to be versus who we are, Carl Rogers' theory of self-concept, using images and diagrams to explain ideas, comparing data in tables, reviewing key concepts, and thanking contributors. The overall document serves as a presentation template on self-concept with different elements to engage an audience.
The broad overview of the Oil and Gas Industry contained in this PowerPoint presentation contains more technical detail than the “Broad Overview for Non-technical Staff”. It is intended for executive staff who lack a background in Geoscience and/or Engineering and/or for new employees to the industry.
1. This document provides instructions for a classroom activity using graham crackers and fruit rollups to model plate tectonic boundaries including divergent, convergent, and transform.
2. Students will create each boundary type using the food items to represent Earth's tectonic plates and layers, record their observations, and answer reflection questions about how the physical models relate to actual geological processes.
3. Questions address how new crust is formed at divergent boundaries, why subduction occurs at convergent boundaries, and how the transform boundary model relates to earthquakes.
This document discusses different types of plate boundaries including divergent boundaries where plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past one another. It provides examples of each boundary type and describes the geological features and processes associated with each, such as the formation of oceanic trenches and volcanic island arcs at convergent boundaries, and the development of rift valleys and oceanic spreading ridges at divergent boundaries. It also discusses examples of hotspots, which are volcanic regions not located along plate boundaries.
automotive industry, all those companies and activities involved in the manufacture of motor vehicles, including most components, such as engines and bodies, but excluding tires, batteries, and fuel. The industry’s principal products are passenger automobiles and light trucks, including pickups, vans, and sport utility vehicles. Commercial vehicles (i.e., delivery trucks and large transport trucks, often called semis), though important to the industry, are secondary. The design of modern automotive vehicles is discussed in the articles automobile, truck, bus, and motorcycle; automotive engines are described in gasoline engine and diesel engine. The development of the automobile is covered in transportation. The history of the automobile industry, though brief compared with that of many other industries, has exceptional interest because of its effects on history from the 20th century. Although the automobile originated in Europe in the late 19th century, the United States completely dominated the world industry for the first half of the 20th century through the invention of mass production techniques. In the second half of the century the situation altered sharply as western European countries and Japan became major producers and exporters. Developments before World War I
Most early automobile companies were small shops, hundreds of which each produced a few handmade cars, and nearly all of which abandoned the business soon after going into it. The handful that survived into the era of large-scale production had certain characteristics in common. First, they fell into one of three well-defined categories: they were makers of bicycles, such as Opel in Germany and Morris in Great Britain; builders of horse-drawn vehicles, such as Durant and Studebaker in the United States; or, most frequently, machinery manufacturers. The kinds of machinery included stationary gas engines (Daimler of Germany, Lanchester of Britain, Olds of the United States), marine engines (Vauxhall of Britain), machine tools (Leland of the United States), sheep-shearing machinery (Wolseley of Britain), washing machines (Peerless of the United States), sewing machines (White of the United States), and woodworking and milling machinery (Panhard and Levassor of France). One American company, Pierce, made birdcages, and another, Buick, made plumbing fixtures, including the first enameled cast-iron bathtub. Two notable exceptions to the general pattern were Rolls-Royce in Britain and Ford in the United States, both of which were founded as carmakers by partners who combined engineering talent and business skill.
Types of plate boundaries include divergent, convergent, and transform. Convergent boundaries occur when plates collide and one plate slides under the other, resulting in volcanic activity and earthquakes. Divergent boundaries occur where plates are moving apart, forming mid-ocean ridges and rift valleys. Transform boundaries occur where plates slide horizontally past each other, causing shallow earthquakes.
1. Convection currents in the Earth's mantle drive the movements of tectonic plates. Hot material rises and spreads out laterally while cooler material sinks.
2. Ridge push and slab pull are two forces that influence plate tectonics. Ridge push results from the weight of new ocean crust pushing older, denser crust towards subduction zones. Slab pull occurs when the dense subducting plate pulls the trailing plate into the subduction zone.
3. Uneven heating of the mantle leads to differences in the density of rocks. Less dense, hot rocks rise while more dense, cooler rocks sink - similar to convection currents in boiling water. This cycling of hot and cold mantle material powers
This document discusses different types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past one another. It focuses on convergent boundaries, describing the processes that occur when an oceanic plate collides with a continental plate or when two oceanic plates collide. These processes include subduction, the formation of volcanoes and mountain ranges, and earthquakes.
The document provides information about ecological concepts and communities. It defines an ecosystem as a collection of populations that live together in an area over time, interacting with each other. A population is defined as a group of living organisms of the same species in one area, while a community is defined as a collection of populations in an area that interact and influence one another. Communities can be named based on their main structure, habitat, or functional characteristics. The document also lists different types of communities such as aquatic and terrestrial, and characteristics used to describe communities such as diversity, relative abundance, and stability.
The document provides definitions and descriptions of various colors:
- Yellow is the color of gold, butter, and ripe lemons. It is located between green and orange on the visible light spectrum.
- Blue is the color of the clear sky and deep sea. It is located between violet and green on the optical spectrum.
- Red is the color of blood and has historically been associated with sacrifice, danger, and courage.
species extinction_07441312344556677.pptxLauriceFrojo3
This document contains a lesson on biodiversity and species extinction. It includes objectives, group activities to identify endangered and extinct species, classify causes of extinction, and evaluate conservation efforts. The lesson teaches students to identify threatened species, understand causes of extinction like habitat loss and pollution, and suggest ways to preserve biodiversity such as protecting wildlife habitats and raising awareness.
Chapter wise All Notes of First year Basic Civil Engineering.pptxDenish Jangid
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.
Levelling: Instrument used Object of levelling, Methods of levelling in brief, and Contour maps.
Chapter 4
Buildings: Selection of site for Buildings, Layout of Building Plan, Types of buildings, Plinth area, carpet area, floor space index, Introduction to building byelaws, concept of sun light & ventilation. Components of Buildings & their functions, Basic concept of R.C.C., Introduction to types of foundation
Chapter 5
Transportation: Introduction to Transportation Engineering; Traffic and Road Safety: Types and Characteristics of Various Modes of Transportation; Various Road Traffic Signs, Causes of Accidents and Road Safety Measures.
Chapter 6
Environmental Engineering: Environmental Pollution, Environmental Acts and Regulations, Functional Concepts of Ecology, Basics of Species, Biodiversity, Ecosystem, Hydrological Cycle; Chemical Cycles: Carbon, Nitrogen & Phosphorus; Energy Flow in Ecosystems.
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
A Visual Guide to 1 Samuel | A Tale of Two HeartsSteve Thomason
These slides walk through the story of 1 Samuel. Samuel is the last judge of Israel. The people reject God and want a king. Saul is anointed as the first king, but he is not a good king. David, the shepherd boy is anointed and Saul is envious of him. David shows honor while Saul continues to self destruct.
Andreas Schleicher presents PISA 2022 Volume III - Creative Thinking - 18 Jun...EduSkills OECD
Andreas Schleicher, Director of Education and Skills at the OECD presents at the launch of PISA 2022 Volume III - Creative Minds, Creative Schools on 18 June 2024.
Philippine Edukasyong Pantahanan at Pangkabuhayan (EPP) CurriculumMJDuyan
(𝐓𝐋𝐄 𝟏𝟎𝟎) (𝐋𝐞𝐬𝐬𝐨𝐧 𝟏)-𝐏𝐫𝐞𝐥𝐢𝐦𝐬
𝐃𝐢𝐬𝐜𝐮𝐬𝐬 𝐭𝐡𝐞 𝐄𝐏𝐏 𝐂𝐮𝐫𝐫𝐢𝐜𝐮𝐥𝐮𝐦 𝐢𝐧 𝐭𝐡𝐞 𝐏𝐡𝐢𝐥𝐢𝐩𝐩𝐢𝐧𝐞𝐬:
- Understand the goals and objectives of the Edukasyong Pantahanan at Pangkabuhayan (EPP) curriculum, recognizing its importance in fostering practical life skills and values among students. Students will also be able to identify the key components and subjects covered, such as agriculture, home economics, industrial arts, and information and communication technology.
𝐄𝐱𝐩𝐥𝐚𝐢𝐧 𝐭𝐡𝐞 𝐍𝐚𝐭𝐮𝐫𝐞 𝐚𝐧𝐝 𝐒𝐜𝐨𝐩𝐞 𝐨𝐟 𝐚𝐧 𝐄𝐧𝐭𝐫𝐞𝐩𝐫𝐞𝐧𝐞𝐮𝐫:
-Define entrepreneurship, distinguishing it from general business activities by emphasizing its focus on innovation, risk-taking, and value creation. Students will describe the characteristics and traits of successful entrepreneurs, including their roles and responsibilities, and discuss the broader economic and social impacts of entrepreneurial activities on both local and global scales.
THE SACRIFICE HOW PRO-PALESTINE PROTESTS STUDENTS ARE SACRIFICING TO CHANGE T...indexPub
The recent surge in pro-Palestine student activism has prompted significant responses from universities, ranging from negotiations and divestment commitments to increased transparency about investments in companies supporting the war on Gaza. This activism has led to the cessation of student encampments but also highlighted the substantial sacrifices made by students, including academic disruptions and personal risks. The primary drivers of these protests are poor university administration, lack of transparency, and inadequate communication between officials and students. This study examines the profound emotional, psychological, and professional impacts on students engaged in pro-Palestine protests, focusing on Generation Z's (Gen-Z) activism dynamics. This paper explores the significant sacrifices made by these students and even the professors supporting the pro-Palestine movement, with a focus on recent global movements. Through an in-depth analysis of printed and electronic media, the study examines the impacts of these sacrifices on the academic and personal lives of those involved. The paper highlights examples from various universities, demonstrating student activism's long-term and short-term effects, including disciplinary actions, social backlash, and career implications. The researchers also explore the broader implications of student sacrifices. The findings reveal that these sacrifices are driven by a profound commitment to justice and human rights, and are influenced by the increasing availability of information, peer interactions, and personal convictions. The study also discusses the broader implications of this activism, comparing it to historical precedents and assessing its potential to influence policy and public opinion. The emotional and psychological toll on student activists is significant, but their sense of purpose and community support mitigates some of these challenges. However, the researchers call for acknowledging the broader Impact of these sacrifices on the future global movement of FreePalestine.
Level 3 NCEA - NZ: A Nation In the Making 1872 - 1900 SML.pptHenry Hollis
The History of NZ 1870-1900.
Making of a Nation.
From the NZ Wars to Liberals,
Richard Seddon, George Grey,
Social Laboratory, New Zealand,
Confiscations, Kotahitanga, Kingitanga, Parliament, Suffrage, Repudiation, Economic Change, Agriculture, Gold Mining, Timber, Flax, Sheep, Dairying,
This presentation was provided by Racquel Jemison, Ph.D., Christina MacLaughlin, Ph.D., and Paulomi Majumder. Ph.D., all of the American Chemical Society, for the second session of NISO's 2024 Training Series "DEIA in the Scholarly Landscape." Session Two: 'Expanding Pathways to Publishing Careers,' was held June 13, 2024.
2. 2
Whiteboard Review Rules
1. Read the question and write your answer on your
whiteboard.
2. You may use your notes, not your other classmates
to answer the question.
3. Do not show your board until I say so.
4. Ready? Let’s go!
3. “
Question #1:
At convergent boundaries, Earth’s plates are
_______:
A. Not moving.
B. Moving towards each other.
C. Moving away from each other.
D. Being created.
3
4. ◍ Question #1 Answer:
B. Moving towards each other.
Convergence of the Nazca and South American Plates
https://pubs.usgs.gov/publications/text/Nazca.html
5. “
◍ Question #2:
When two plates collide, the heavier of
the two is pulled under the lighter plate
in a process called ______:
5
10. “
◍ Question #4 :
What type of Convergent Plate boundary where
in one of the plates such as oceanic crust and
Lithospheric mantle is pushed, or subducted,
under the other forming a subduction zone
10
15. Today’s Learning Objectives:
◍ Explain Divergent Boundaries and their
features.
◍ Identify the two types of divergent plate
boundaries
◍ Determine the movement of the two types
of divergent plate
15
16. Divergent
boundaries
◍ where plates
separate and move
in opposite
directions, allowing
new lithosphere to
form from upwelling
magma.
16
◍ This either occurs at
mid-ocean ridges
(the so-called
seafloor spreading)
or at rifted
continental margins.
18. 1.
Transition headline
Let’s start with the first set of slides
18
Along these
boundaries ,
earthquakes are
common &
magma ( molten
rock) rises from
the Earth’s
mantle to the
surface,
solidifying to
create new
oceanic crust.
19. Questions
◍ The motion
of divergent
plate
boundary is
spreading.
◍ Volcanic
activity is
present in
divergent
boundary.
◍ Oceanic
lithosphere is
formed in
divergent
plate
boundary.
19
(Seafloor
Spreading)
21. Two Types of Divergent
Plate Boundaries
21
◍ Oceanic-Oceanic Plates ◍ Continental-Continental
Plates
22. Divergent Boundaries –
Oceanic Plates
◍ Oceanic ridges are the
result or rising convection
currents that lifts the
lithosphere.
22
23. Divergent Boundaries –
Continental Plates
◍ Continental rifts are the
result of the convection
forces inside the Earth
arching the plate upwards
and fracturing it.
23
24. 24
Divergent boundaries occur where two oceanic
plates move away from one another, this is
where seafloor spreading takes place the most
common example is the mid-ocean ridge.
Fig.1.1. Oceanic- oceanic Fig.1.2. Continental - continental
25. What is being produced from the types
of divergent plate boundaries shown
below?
25
Oceanic –oceanic Continental- continental
Mid-Atlantic ocean ridge
Volcanic activity
Shallow earthquake
faulted valleys - rift
valleys
26. What causes the motion in the two types of
divergent plate boundaries ?
Divergent boundaries occur along spreading centers
where plates are moving apart & new crust is created
by magma pushing up from the mantle.
26
27. 27
True/False – Thumbs Up/Thumbs
Down
For each of the following statements,
put your thumb up or down depending
on if it is true or false.
TRUE = THUMBS UP
FALSE = THUMBS DOWN
28. 28
True/False – Thumbs Up/Thumbs Down
A divergent boundary happens when Earth’s
tectonic plates move away from each other
TRUE = THUMBS UP
FALSE = THUMBS DOWN
29. 29
True/False – Thumbs Up/Thumbs Down
A divergent boundary happens when Earth’s
tectonic plates move away from each other
TRUE = THUMBS UP
FALSE = THUMBS DOWN
1
2
3
4
5
31. 31
True/False – Thumbs Up/Thumbs Down
Ocean ridge and volcanic island are also formed
in the divergent plate boundary.
TRUE = THUMBS UP
FALSE = THUMBS DOWN
32. 32
True/False – Thumbs Up/Thumbs Down
Ocean ridge and volcanic island are also formed
in the divergent plate boundary.
TRUE = THUMBS UP
FALSE = THUMBS DOWN
1
2
3
4
5
34. 34
True/False – Thumbs Up/Thumbs Down
When magma continues to build up, new
mountain ranges are not formed under the sea
creating a mid-ocean ridge.
TRUE = THUMBS UP
FALSE = THUMBS DOWN
35. 35
True/False – Thumbs Up/Thumbs Down
When magma continues to build up, new
mountain ranges are not formed under the sea
creating a mid-ocean ridge.
TRUE = THUMBS UP
FALSE = THUMBS DOWN 1
2
3
4
5
37. 37
True/False – Thumbs Up/Thumbs Down
Earthquakes and volcanoes do not occur in a
divergent plate boundary.
TRUE = THUMBS UP
FALSE = THUMBS DOWN
38. 38
True/False – Thumbs Up/Thumbs Down
Earthquakes and volcanoes do not occur in a
divergent plate boundary.
TRUE = THUMBS UP
FALSE = THUMBS DOWN
1
2
3
4
5
46. 46
True/False – Thumbs Up/Thumbs Down
Plates that are sliding past each other is
characterized by a transform fault boundary.
TRUE = THUMBS UP
FALSE = THUMBS DOWN
47. 47
True/False – Thumbs Up/Thumbs Down
Plates that are sliding past each other is
characterized by a transform fault boundary.
TRUE = THUMBS UP
FALSE = THUMBS DOWN 1
2
3
4
5
60. Let’s review some concepts
Yellow
Is the color of gold, butter and
ripe lemons. In the spectrum of
visible light, yellow is found
between green and orange.
Blue
Is the colour of the clear sky and
the deep sea. It is located
between violet and green on the
optical spectrum.
Red
Is the color of blood, and
because of this it has historically
been associated with sacrifice,
danger and courage.
Yellow
Is the color of gold, butter and
ripe lemons. In the spectrum of
visible light, yellow is found
between green and orange.
Blue
Is the colour of the clear sky and
the deep sea. It is located
between violet and green on the
optical spectrum.
Red
Is the color of blood, and
because of this it has historically
been associated with sacrifice,
danger and courage.
60
61. You can insert graphs from Excel or Google Sheets
61
4000
3000
2000
1000
0
62. Tablet project
Show and explain your
web, app or software
projects using these
gadget templates.
62
63. Desktop project
Show and explain your
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63
64. Credits
Special thanks to all the people who
made and released these awesome
resources for free:
◍ Presentation template by
SlidesCarnival
◍ Photographs by Unsplash
64
65. Presentation design
This presentation uses the following typographies and colors:
◍ Titles: Nixie One
◍ Body copy: Inconsolata
You can download the fonts on these pages:
https://www.fontsquirrel.com/fonts/inconsolata
https://www.fontsquirrel.com/fonts/nixie-one
◍ Purple #432e64
◍ Dark Purple #0e004a
◍ Yellow #ff9900
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◍ Blue #6d9eeb
You don’t need to keep this slide in your presentation. It’s only here to serve you as a design
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PowerPoint®
65
67. Timeline
67
DEC
NOV
OCT
SEP
AUG
JUL
JUN
MAY
APR
MAR
FEB
JAN
Blue is the colour of the
clear sky and the deep
sea
Red is the colour of
danger and courage
Black is the color of
ebony and of outer
space
Yellow is the color of
gold, butter and ripe
lemons
White is the color of milk
and fresh snow
Blue is the colour of the
clear sky and the deep
sea
Yellow is the color of
gold, butter and ripe
lemons
White is the color of milk
and fresh snow
Blue is the colour of the
clear sky and the deep
sea
Red is the colour of
danger and courage
Black is the color of
ebony and of outer
space
Yellow is the color
of gold, butter and
ripe lemons
68. Roadmap
68
1 3 5
6
4
2
Blue is the colour of the
clear sky and the deep
sea
Red is the colour of
danger and courage
Black is the color of
ebony and of outer
space
Yellow is the color of
gold, butter and ripe
lemons
White is the color of milk
and fresh snow
Blue is the colour of the
clear sky and the deep
sea
70. SWOT Analysis
70
STRENGTHS
Blue is the colour of the
clear sky and the deep sea
WEAKNESSES
Yellow is the color of gold,
butter and ripe lemons
Black is the color of ebony
and of outer space
OPPORTUNITIES
White is the color of milk
and fresh snow
THREATS
71. Business Model Canvas
71
Key Activities
Insert your content
Key Resources
Insert your content
Value Propositions
Insert your content
Customer Relationships
Insert your content
Channels
Insert your content
Customer Segments
Insert your content
Key Partners
Insert your content
Cost Structure
Insert your content
Revenue Streams
Insert your content
73. Team Presentation
73
Imani Jackson
JOB TITLE
Blue is the colour of the clear
sky and the deep sea
Marcos Galán
JOB TITLE
Blue is the colour of the clear
sky and the deep sea
Ixchel Valdía
JOB TITLE
Blue is the colour of the clear
sky and the deep sea
Nils Årud
JOB TITLE
Blue is the colour of the clear
sky and the deep sea
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75
77. You can use any emoji as an icon!
And it resizes without losing quality.
How? Follow Google instructions
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