Plate tectonics
•Download as PPTX, PDF•
3 likes•3,822 views
Here are the steps to demonstrate a transform boundary using the snack tectonics materials: 1. Place a small amount of icing along the edge of one piece of wax paper to represent the plate boundary. 2. Hold the two pieces of wax paper next to each other with the icing in between. 3. Slowly slide the pieces of wax paper past each other along the icing, which represents the plates moving horizontally in opposite directions. This demonstrates how transform boundaries form as the plates slide past each other laterally without either plate subducting under the other. The icing represents the fault line where energy is released through earthquakes as the plates shear and grind against each other.
Report
Share
Report
Share
Recommended
Earth interior
This document provides an overview of the layers of the Earth through a series of diagrams and explanations. It discusses the four main layers - the lithosphere, asthenosphere, outer core, and inner core. The lithosphere includes the crust and upper mantle and is broken into tectonic plates. The asthenosphere is below the lithosphere and flows like hot asphalt due to convection currents, allowing the plates to move. Deeper layers get progressively hotter and the immense pressure would crush anything at the Earth's core.
Interior Structure of the Earth
The document summarizes key information about the interior structure and composition of the Earth. It is divided into three main layers:
1) The crust is the outermost solid layer and thinnest, varying between 5-50 km thick. It is broken into tectonic plates that move over time.
2) The mantle, the largest layer, makes up over 80% of the Earth's volume. It is divided into the upper and lower mantle.
3) The core is the innermost layer and has a solid inner core and liquid outer core, composed primarily of iron and nickel.
Theory of Plate Tectonics
The document discusses plate tectonics and the theory that Earth's outer shell is divided into plates that glide over the mantle. It describes three main types of plate boundaries: convergent boundaries where plates collide, divergent boundaries where plates move apart, and transform boundaries where plates slide past each other. Convergent boundaries can involve subduction zones and result in mountain building. Divergent boundaries create new crust and can form undersea ridges or split continents. Transform boundaries cause earthquakes as stress builds up between sliding plates.
Chapter 1 Plate Tectonics Power Point
The document discusses Earth's structure and plate tectonics. It describes how Earth formed layers with different densities, including the inner and outer core, mantle, crust, and lithosphere. The lithosphere is made up of tectonic plates that move over time. There are three types of plate boundaries - divergent where plates move apart, convergent where they push together, and transform where they scrape past each other. Plate tectonics explains how continents have changed positions over billions of years and continue to move today.
Dynamic earth ppt to go with notes
The theory of plate tectonics explains that Earth's outer layer is made up of plates that have moved throughout geological history. These plates float on top of the mantle and move at boundaries where they diverge, converge, or slide past one another. Convection currents in the upper mantle provide the driving force that causes plates to move over time.
Plate Tectonics Earth
Volcanoes are formed from hot spots within the Earth's crust and mantle that allow hot liquid rock to break through weak spots on the surface. Earthquakes are caused by motion within the solid Earth and provide evidence about its interior structure. The Earth's surface is made up of tectonic plates that move over time, as evidenced by matching rock and fossil formations on separated continents and patterns in seafloor ages and magnetism. Plate boundaries include convergent boundaries where plates move toward each other, divergent boundaries where they move apart, and transform boundaries where they slide past each other.
Plate tectonics
The Continental Drift Theory, The Seafloor Spreading Theory and The Plate Tectonics Theory are the three important theories taking place in our planet.
Earth Science. Geosphere, Plate Tectonic Notes
The document discusses plate tectonics and the structure of the Earth. It explains that Earth's outer layer is divided into plates that move over Earth's mantle in a constant state of motion. This motion of plates causes continental drift and is responsible for geological features and events like earthquakes, volcanic eruptions, and mountain building. The theory of plate tectonics developed in the 1960s to explain phenomena like sea floor spreading and the movement of continents over geologic time.
Recommended
Earth interior
This document provides an overview of the layers of the Earth through a series of diagrams and explanations. It discusses the four main layers - the lithosphere, asthenosphere, outer core, and inner core. The lithosphere includes the crust and upper mantle and is broken into tectonic plates. The asthenosphere is below the lithosphere and flows like hot asphalt due to convection currents, allowing the plates to move. Deeper layers get progressively hotter and the immense pressure would crush anything at the Earth's core.
Interior Structure of the Earth
The document summarizes key information about the interior structure and composition of the Earth. It is divided into three main layers:
1) The crust is the outermost solid layer and thinnest, varying between 5-50 km thick. It is broken into tectonic plates that move over time.
2) The mantle, the largest layer, makes up over 80% of the Earth's volume. It is divided into the upper and lower mantle.
3) The core is the innermost layer and has a solid inner core and liquid outer core, composed primarily of iron and nickel.
Theory of Plate Tectonics
The document discusses plate tectonics and the theory that Earth's outer shell is divided into plates that glide over the mantle. It describes three main types of plate boundaries: convergent boundaries where plates collide, divergent boundaries where plates move apart, and transform boundaries where plates slide past each other. Convergent boundaries can involve subduction zones and result in mountain building. Divergent boundaries create new crust and can form undersea ridges or split continents. Transform boundaries cause earthquakes as stress builds up between sliding plates.
Chapter 1 Plate Tectonics Power Point
The document discusses Earth's structure and plate tectonics. It describes how Earth formed layers with different densities, including the inner and outer core, mantle, crust, and lithosphere. The lithosphere is made up of tectonic plates that move over time. There are three types of plate boundaries - divergent where plates move apart, convergent where they push together, and transform where they scrape past each other. Plate tectonics explains how continents have changed positions over billions of years and continue to move today.
Dynamic earth ppt to go with notes
The theory of plate tectonics explains that Earth's outer layer is made up of plates that have moved throughout geological history. These plates float on top of the mantle and move at boundaries where they diverge, converge, or slide past one another. Convection currents in the upper mantle provide the driving force that causes plates to move over time.
Plate Tectonics Earth
Volcanoes are formed from hot spots within the Earth's crust and mantle that allow hot liquid rock to break through weak spots on the surface. Earthquakes are caused by motion within the solid Earth and provide evidence about its interior structure. The Earth's surface is made up of tectonic plates that move over time, as evidenced by matching rock and fossil formations on separated continents and patterns in seafloor ages and magnetism. Plate boundaries include convergent boundaries where plates move toward each other, divergent boundaries where they move apart, and transform boundaries where they slide past each other.
Plate tectonics
The Continental Drift Theory, The Seafloor Spreading Theory and The Plate Tectonics Theory are the three important theories taking place in our planet.
Earth Science. Geosphere, Plate Tectonic Notes
The document discusses plate tectonics and the structure of the Earth. It explains that Earth's outer layer is divided into plates that move over Earth's mantle in a constant state of motion. This motion of plates causes continental drift and is responsible for geological features and events like earthquakes, volcanic eruptions, and mountain building. The theory of plate tectonics developed in the 1960s to explain phenomena like sea floor spreading and the movement of continents over geologic time.
Interior Of Earth
The document discusses what lies within Earth's interior based on indirect evidence from seismic waves. [1] Seismic waves provide information about Earth's layered structure as the waves refract and reflect differently depending on density changes. [2] Earth has a crust, mantle, outer core, and inner core, with increasing temperatures and pressures toward the center. [3] The core generates Earth's magnetic field through its spinning liquid outer layer.
Concept of isostatic adjustment and isostatic models
This document discusses the geological concept of isostasy, which refers to the equilibrium between Earth's crust and mantle such that the crust "floats" at an elevation that depends on its thickness and density. It presents several theories of isostasy, including Airy's theory which proposes that thicker crustal areas sink deeper into the mantle, and Pratt's theory which suggests areas of lower crustal density project higher. The document also discusses isostatic effects from processes like deposition, erosion, and past ice sheets, as well as concepts like phase changes and Heiskanen's modification of Airy's theory.
The structure of the earth and plate tectonics
The Earth is composed of four main layers - the inner core, outer core, mantle, and crust. The crust is divided into tectonic plates that slowly move due to convection currents in the mantle. There are three types of plate boundaries - divergent where plates move apart, convergent where they move together, and transform where they slide past each other. Plate interactions at boundaries cause volcanic and seismic activity, with volcanoes and earthquakes concentrated near plate margins.
Revision plate tectonic (landforms)
This is the summary on gateway 1 on plate tectonic. It discusses about the following:
1) Characteristics of the different structure of the earth.
2) The mechanism leading to plate movement
3) Landforms associated to the different plate movement.
OLM Science6_6
The document summarizes key concepts in plate tectonics. It describes how the Earth is divided into layers including the crust, mantle, and core. It explains that the crust is broken into plates that move around on the asthenosphere. 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. Plate tectonics helps explain geological events like continental drift, mountain building, and volcanic activity.
Isostasy and continental_drift
1) Isostasy refers to the state of gravitational equilibrium between the Earth's lithosphere and asthenosphere. The elevation and thickness of the Earth's crust depends on its density and thickness to maintain balance.
2) Alfred Wegener first proposed the theory of continental drift in 1915, which states that continents slowly drift due to convection currents in the mantle. Wegener provided evidence that all present-day continents were once joined together in a supercontinent called Pangea.
3) Plate tectonics explains continental drift as the movement of tectonic plates across the Earth's surface over geological time, caused by convection currents in the upper mantle. Pangea broke apart into smaller continents that have
Plate tectonics
Plate tectonics describes how the Earth's crust is broken into plates that move around on the mantle. There are two types of plates - ocean plates under the oceans and continental plates under the continents. Plates meet at boundaries where they either move apart, collide together, or slide past one another. The movement of convection currents in the mantle is the driving force behind plate tectonics.
Plate tectonics
The document discusses 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. Plates interact at boundaries where they diverge (move apart), converge (move together), or slide past one another. Convection currents in the mantle provide the driving force for plate tectonics.
The earth’s interior
This document provides an overview of the internal structure of the Earth. It describes the three main layers - crust, mantle, and core. The crust is the outermost layer and is divided into continental and oceanic crust. Beneath the crust is the mantle, which makes up most of the Earth's volume. The core is at the center and has a solid inner core and liquid outer core. Seismic waves and magnetic reversals provide evidence about the composition and movement of materials in the Earth's interior.
Plate tectonics bs 1st year
The document summarizes key concepts about tectonic plates and continental drift. It describes how tectonic plates consist of rigid continental and oceanic crust that moves due to convection currents in the underlying mantle. It outlines Alfred Wegener's early 20th century proposal of continental drift, which provided evidence that continents were once joined together before drifting apart. It also summarizes the three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where they slide past one another.
Plate tectonics ma
Plates are made of rigid lithosphere consisting of crust and upper mantle. Plate tectonics involves the motions and interactions of these rigid plates. There are three main types of plate interactions - divergent boundaries where plates move apart and mid-ocean ridges form, convergent boundaries where plates collide resulting in subduction zones or mountain building, and transform boundaries where plates slide past each other along transform faults.
Plate tectonics slides re
This slide show describes the theory of plate tectonics and explains how the interaction of tectonic plates changes the surface of our earth.
Geology: Plate Tectonics
Plate Tectonic is a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates which move slowly over the underlying mantle.
Plate tectonics & seafloor spreading
1) Seismic studies reveal that the Earth is composed of layers with different chemical compositions and physical properties, including a solid inner core, liquid outer core, soft asthenosphere, and rigid lithosphere.
2) Evidence from seafloor spreading and magnetic stripes on the ocean floor support the theory of plate tectonics, where new ocean crust forms at mid-ocean ridges and spreads outward as the plates move.
3) Paleomagnetic data from rocks show alternating magnetic polarities on either side of ridges, supporting the hypothesis that new crust forms at ridges and cools over time, recording reversals in Earth's magnetic field to reveal the history of plate movements.
5th Grade Ch 9 Lesson 1 What Is The Structure Of Earth
The document discusses the four main layers of Earth's interior:
1. The crust is the outermost layer made of granite or basalt and is the thinnest layer.
2. The mantle is the largest layer made of hot, solid rock that can flow like a liquid. It includes the lithosphere.
3. The outer core is liquid and generates Earth's magnetic field.
4. The inner core is solid and lies at the center of Earth.
Interior of the earth
The document discusses the interior structure of the Earth. It is divided into four major layers:
1) The crust is the outermost solid rock layer and is divided into continental and oceanic crust.
2) Below the crust is the mantle, which makes up most of the Earth's volume. The upper mantle includes the asthenosphere and transition zone.
3) In the Earth's core, seismic waves indicate the outer core is liquid while the inner core is solid.
4) Evidence from earthquake waves, density measurements, and mineral properties help reveal the composition of each layer and boundaries between them like the Mohorovicic discontinuity.
Geosphere.rocks.minerals
The document provides information about Earth's four main systems - the atmosphere, hydrosphere, biosphere, and geosphere. It then focuses on explaining the different types of rocks: igneous rocks form from cooled lava or magma, either underground (intrusive) or above ground (extrusive); sedimentary rocks form through the deposition and cementation of sediments; and metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in Earth's crust. Weathering, erosion, deposition, compaction, and cementation are identified as processes that can transform one rock type into another in the rock cycle.
Plate tectonics
The document discusses evidence that supports the theory of plate tectonics and continental drift. It describes how early in Earth's formation, chemical segregation resulted in layers forming within the planet. Later, the nebular hypothesis proposed that planets accreted from a disk of dust and gases orbiting the sun. Evidence like matching fossil distributions, rock formations, and paleoclimate patterns across separated continents supported Alfred Wegener's idea that continents had drifted apart from an original supercontinent. This helped establish the modern theory of plate tectonics.
Earth Science 4.1 : Inside the Earth
The document summarizes the layers and structure of the Earth's interior. It discusses the three main layers - crust, mantle, and core - based on their chemical compositions. The crust is the outermost layer and thinnest, with continental crust thicker than oceanic crust. The mantle makes up most of the Earth's mass and lies between the crust and core. The core is the central part made mostly of iron. It then describes the physical structure, dividing the interior into lithosphere, asthenosphere, mesosphere, outer core, and inner core based on their properties. Tectonic plates consist of crust and the rigid upper mantle, floating on the asthenosphere. Scientists have mapped the interior using seismic waves from earth
Plate tectonics and various landforms form by plate movements of earth system
a basic information report of plate tectonics activities and formation of volcanoes, series of volcanoes
formation view point of Himalayas, Platue and others valleys
Notes: Continental Drift Plate Tectonics
Here are the answers to the questions:
1. Divergent boundary - Mid-ocean ridge. New ocean floor is created as the plates move apart and magma rises to fill the gap.
2. Convergent boundary - Subduction zone. One plate moves under the other and is recycled back into the mantle. Volcanoes and earthquakes occur above the subducting slab.
3. Transform boundary - San Andreas Fault. The plates slide past each other, causing earthquakes along the fault line.
2016 Pure Geog Chapter 1 living with tectonic hazards complete
This document provides an overview of natural hazards caused by tectonic plate movement, including earthquakes and volcanic eruptions. It discusses the different types of plate boundaries (divergent, convergent, transform) and the associated landforms, such as mid-ocean ridges, trenches, fold mountains and volcanoes. Specific examples like the San Andreas Fault and Himalayas are also mentioned. The text explores the structure of the Earth's interior and explains concepts such as continental drift theory and the movement of tectonic plates.
More Related Content
What's hot
Interior Of Earth
The document discusses what lies within Earth's interior based on indirect evidence from seismic waves. [1] Seismic waves provide information about Earth's layered structure as the waves refract and reflect differently depending on density changes. [2] Earth has a crust, mantle, outer core, and inner core, with increasing temperatures and pressures toward the center. [3] The core generates Earth's magnetic field through its spinning liquid outer layer.
Concept of isostatic adjustment and isostatic models
This document discusses the geological concept of isostasy, which refers to the equilibrium between Earth's crust and mantle such that the crust "floats" at an elevation that depends on its thickness and density. It presents several theories of isostasy, including Airy's theory which proposes that thicker crustal areas sink deeper into the mantle, and Pratt's theory which suggests areas of lower crustal density project higher. The document also discusses isostatic effects from processes like deposition, erosion, and past ice sheets, as well as concepts like phase changes and Heiskanen's modification of Airy's theory.
The structure of the earth and plate tectonics
The Earth is composed of four main layers - the inner core, outer core, mantle, and crust. The crust is divided into tectonic plates that slowly move due to convection currents in the mantle. There are three types of plate boundaries - divergent where plates move apart, convergent where they move together, and transform where they slide past each other. Plate interactions at boundaries cause volcanic and seismic activity, with volcanoes and earthquakes concentrated near plate margins.
Revision plate tectonic (landforms)
This is the summary on gateway 1 on plate tectonic. It discusses about the following:
1) Characteristics of the different structure of the earth.
2) The mechanism leading to plate movement
3) Landforms associated to the different plate movement.
OLM Science6_6
The document summarizes key concepts in plate tectonics. It describes how the Earth is divided into layers including the crust, mantle, and core. It explains that the crust is broken into plates that move around on the asthenosphere. 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. Plate tectonics helps explain geological events like continental drift, mountain building, and volcanic activity.
Isostasy and continental_drift
1) Isostasy refers to the state of gravitational equilibrium between the Earth's lithosphere and asthenosphere. The elevation and thickness of the Earth's crust depends on its density and thickness to maintain balance.
2) Alfred Wegener first proposed the theory of continental drift in 1915, which states that continents slowly drift due to convection currents in the mantle. Wegener provided evidence that all present-day continents were once joined together in a supercontinent called Pangea.
3) Plate tectonics explains continental drift as the movement of tectonic plates across the Earth's surface over geological time, caused by convection currents in the upper mantle. Pangea broke apart into smaller continents that have
Plate tectonics
Plate tectonics describes how the Earth's crust is broken into plates that move around on the mantle. There are two types of plates - ocean plates under the oceans and continental plates under the continents. Plates meet at boundaries where they either move apart, collide together, or slide past one another. The movement of convection currents in the mantle is the driving force behind plate tectonics.
Plate tectonics
The document discusses 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. Plates interact at boundaries where they diverge (move apart), converge (move together), or slide past one another. Convection currents in the mantle provide the driving force for plate tectonics.
The earth’s interior
This document provides an overview of the internal structure of the Earth. It describes the three main layers - crust, mantle, and core. The crust is the outermost layer and is divided into continental and oceanic crust. Beneath the crust is the mantle, which makes up most of the Earth's volume. The core is at the center and has a solid inner core and liquid outer core. Seismic waves and magnetic reversals provide evidence about the composition and movement of materials in the Earth's interior.
Plate tectonics bs 1st year
The document summarizes key concepts about tectonic plates and continental drift. It describes how tectonic plates consist of rigid continental and oceanic crust that moves due to convection currents in the underlying mantle. It outlines Alfred Wegener's early 20th century proposal of continental drift, which provided evidence that continents were once joined together before drifting apart. It also summarizes the three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where they slide past one another.
Plate tectonics ma
Plates are made of rigid lithosphere consisting of crust and upper mantle. Plate tectonics involves the motions and interactions of these rigid plates. There are three main types of plate interactions - divergent boundaries where plates move apart and mid-ocean ridges form, convergent boundaries where plates collide resulting in subduction zones or mountain building, and transform boundaries where plates slide past each other along transform faults.
Plate tectonics slides re
This slide show describes the theory of plate tectonics and explains how the interaction of tectonic plates changes the surface of our earth.
Geology: Plate Tectonics
Plate Tectonic is a theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithospheric plates which move slowly over the underlying mantle.
Plate tectonics & seafloor spreading
1) Seismic studies reveal that the Earth is composed of layers with different chemical compositions and physical properties, including a solid inner core, liquid outer core, soft asthenosphere, and rigid lithosphere.
2) Evidence from seafloor spreading and magnetic stripes on the ocean floor support the theory of plate tectonics, where new ocean crust forms at mid-ocean ridges and spreads outward as the plates move.
3) Paleomagnetic data from rocks show alternating magnetic polarities on either side of ridges, supporting the hypothesis that new crust forms at ridges and cools over time, recording reversals in Earth's magnetic field to reveal the history of plate movements.
5th Grade Ch 9 Lesson 1 What Is The Structure Of Earth
The document discusses the four main layers of Earth's interior:
1. The crust is the outermost layer made of granite or basalt and is the thinnest layer.
2. The mantle is the largest layer made of hot, solid rock that can flow like a liquid. It includes the lithosphere.
3. The outer core is liquid and generates Earth's magnetic field.
4. The inner core is solid and lies at the center of Earth.
Interior of the earth
The document discusses the interior structure of the Earth. It is divided into four major layers:
1) The crust is the outermost solid rock layer and is divided into continental and oceanic crust.
2) Below the crust is the mantle, which makes up most of the Earth's volume. The upper mantle includes the asthenosphere and transition zone.
3) In the Earth's core, seismic waves indicate the outer core is liquid while the inner core is solid.
4) Evidence from earthquake waves, density measurements, and mineral properties help reveal the composition of each layer and boundaries between them like the Mohorovicic discontinuity.
Geosphere.rocks.minerals
The document provides information about Earth's four main systems - the atmosphere, hydrosphere, biosphere, and geosphere. It then focuses on explaining the different types of rocks: igneous rocks form from cooled lava or magma, either underground (intrusive) or above ground (extrusive); sedimentary rocks form through the deposition and cementation of sediments; and metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in Earth's crust. Weathering, erosion, deposition, compaction, and cementation are identified as processes that can transform one rock type into another in the rock cycle.
Plate tectonics
The document discusses evidence that supports the theory of plate tectonics and continental drift. It describes how early in Earth's formation, chemical segregation resulted in layers forming within the planet. Later, the nebular hypothesis proposed that planets accreted from a disk of dust and gases orbiting the sun. Evidence like matching fossil distributions, rock formations, and paleoclimate patterns across separated continents supported Alfred Wegener's idea that continents had drifted apart from an original supercontinent. This helped establish the modern theory of plate tectonics.
Earth Science 4.1 : Inside the Earth
The document summarizes the layers and structure of the Earth's interior. It discusses the three main layers - crust, mantle, and core - based on their chemical compositions. The crust is the outermost layer and thinnest, with continental crust thicker than oceanic crust. The mantle makes up most of the Earth's mass and lies between the crust and core. The core is the central part made mostly of iron. It then describes the physical structure, dividing the interior into lithosphere, asthenosphere, mesosphere, outer core, and inner core based on their properties. Tectonic plates consist of crust and the rigid upper mantle, floating on the asthenosphere. Scientists have mapped the interior using seismic waves from earth
Plate tectonics and various landforms form by plate movements of earth system
a basic information report of plate tectonics activities and formation of volcanoes, series of volcanoes
formation view point of Himalayas, Platue and others valleys
What's hot (20)
Concept of isostatic adjustment and isostatic models
Concept of isostatic adjustment and isostatic models
5th Grade Ch 9 Lesson 1 What Is The Structure Of Earth
5th Grade Ch 9 Lesson 1 What Is The Structure Of Earth
Plate tectonics and various landforms form by plate movements of earth system
Plate tectonics and various landforms form by plate movements of earth system
Similar to Plate tectonics
Notes: Continental Drift Plate Tectonics
Here are the answers to the questions:
1. Divergent boundary - Mid-ocean ridge. New ocean floor is created as the plates move apart and magma rises to fill the gap.
2. Convergent boundary - Subduction zone. One plate moves under the other and is recycled back into the mantle. Volcanoes and earthquakes occur above the subducting slab.
3. Transform boundary - San Andreas Fault. The plates slide past each other, causing earthquakes along the fault line.
2016 Pure Geog Chapter 1 living with tectonic hazards complete
This document provides an overview of natural hazards caused by tectonic plate movement, including earthquakes and volcanic eruptions. It discusses the different types of plate boundaries (divergent, convergent, transform) and the associated landforms, such as mid-ocean ridges, trenches, fold mountains and volcanoes. Specific examples like the San Andreas Fault and Himalayas are also mentioned. The text explores the structure of the Earth's interior and explains concepts such as continental drift theory and the movement of tectonic plates.
Chapter 1 part 1 2 3 and 4
This document provides information about natural hazards caused by tectonic plate movement. It discusses different types of plate boundaries like divergent, convergent and transform boundaries. Key landforms associated with these boundaries are described, such as fold mountains, rift valleys, block mountains, and volcanoes. Specific examples like the Himalayas and Mount Pinatubo are given. The document also explains concepts of tectonic plates, continental drift theory, and the different types of volcanoes.
Sec 3 Elective Geog Unit 1 Tectonics
The document provides information about natural hazards associated with tectonic plate movement, including earthquakes and volcanoes. It discusses the different types of plate boundaries (divergent, convergent, transform) and the landforms created by each, such as rift valleys, fold mountains, and volcanoes. Convergent boundaries are described in more detail, outlining the processes and features of oceanic-oceanic, oceanic-continental, and continental-continental convergence. Hazards of living in areas with active tectonics are also summarized, such as destruction from volcanic eruptions, tsunamis triggered by earthquakes, and landslides.
Chapter 1 living with tectonic hazards complete
This document provides an overview of natural hazards caused by tectonic plate movements, including earthquakes, volcanoes, and tsunamis. It discusses the structure of the Earth and concepts of plate tectonics such as continental drift and the three types of plate boundaries. Specific landforms associated with each boundary type are described, including fold mountains, rift valleys, and volcanoes. The document also covers volcanic eruptions and the risks of living near volcanoes or in earthquake zones.
2.3 theory of plate tectonics
The Theory of Plate Tectonics states that the Earth's outer shell is broken into rigid plates that float on the asthenosphere and interact at their boundaries. The lithosphere consists of oceanic and continental crust plates that move due to convection currents in the mantle. Plates interact at divergent boundaries where new crust is created, convergent boundaries where one plate subducts under another, and transform boundaries where plates slide past each other like the San Andreas Fault.
2.4 tectonic plate boundaries
There are three main types of plate boundaries: divergent boundaries where plates pull apart and new crust is formed, convergent boundaries where plates push together resulting in subduction and volcanic activity, and transform boundaries where plates slide past one another along transform faults. Each boundary has distinct features like mid-ocean ridges, deep trenches, and fracture zones. Plate tectonics can be seen in examples around the world from the Himalayas to the Aleutian Islands.
Sara Arif - EDSC 304 - Teacher Lecture & Guided Notes - Plate Tectonics and E...
The document discusses the theory of plate tectonics and how it explains the formation and movement of continents over time. Around 250 million years ago, all the continents were joined together in a supercontinent called Pangea. Over millions of years, Pangea broke apart and the continents drifted to their current locations, carried by tectonic plates in the Earth's mantle. New crust is formed at mid-ocean ridges as plates move apart, while older crust is recycled at deep ocean trenches as plates converge. The movement of tectonic plates causes earthquakes, particularly at plate boundaries where plates collide, slide past each other, or move apart.
Plate tectonics
This document discusses plate tectonics and the three main types of plate boundaries. It describes how plate tectonics theory states that the lithosphere is made up of rigid plates that move over the asthenosphere. The three types of plate boundaries are divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where they grind past each other. It provides examples of each boundary type and explains the geological features that form as a result of the movements and interactions of tectonic plates.
Living with Tectonic Hazards
This document provides information about natural hazards caused by tectonic plate movements. It discusses the three main types of plate boundaries: divergent where plates move apart, convergent where they move together, and transform where they move past each other. At divergent boundaries, mid-ocean ridges and volcanic islands form through sea floor spreading. Rift valleys and block mountains form when continents split apart. At convergent boundaries, denser plates subduct under lighter ones, creating ocean trenches, volcanic island arcs, and fold mountains through compression. Transform boundaries cause earthquakes along tear faults as plates grind past each other.
Tectonics GW1 Slides (Part 2)
1. There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates move together, and transform boundaries where plates slide past one another.
2. At divergent boundaries, new oceanic crust is formed at mid-ocean ridges. This results in features like rift valleys on land and undersea volcanoes at sea. Convergent boundaries result in ocean trenches from subducting plates and volcanic island arcs. Continental collisions yield fold mountains from compressed crust.
3. Key landforms and phenomena associated with plate tectonics include mid-ocean ridges, rift valleys and block mountains, ocean trenches, volcanic island arcs, and fold mountains. Earthquakes also
Plate Tectonics
This document provides information about natural hazards such as earthquakes and volcanoes. It discusses the different types of plate boundaries including divergent, convergent and transform boundaries. It describes associated landforms such as fold mountains, rift valleys, block mountains and volcanoes. The document explains different types of volcanoes including shield volcanoes and composite volcanoes. It discusses volcanic eruptions and distribution of volcanoes along the Pacific Ring of Fire. The risks of living near volcanoes are outlined, as well as some benefits. Earthquakes are also described, including factors that influence damage and preparedness measures.
Geography Elective/Pure Chapter 1/2: Plate tectonic Gateway 1, 2, 3
This is the notes and slides provided and compiled by teachers from reputable schools. Took me many months to compile this and share with you guys! By the way, the slides with a star usually mean that it will be significant so take note! Sharing with you now is this notes!!! Enjoy and love geography!!!
Elective Gegography Chapter 1 Plate Tectonics
This document provides information about natural hazards such as earthquakes and volcanoes. It discusses the different types of plate boundaries including divergent, convergent and transform boundaries. It describes associated landforms such as fold mountains, rift valleys, block mountains and volcanoes. The document explains different types of volcanoes including shield volcanoes and composite volcanoes. It discusses volcanic eruptions and distribution of volcanoes along the Pacific Ring of Fire. The risks of living near volcanoes are outlined, as well as some benefits. Earthquakes are also described, including factors that influence damage. Overall, the document presents an overview of tectonic hazards and the geology associated with plate tectonics.
Chapter 9 science 3 outline
Wegener's continental drift hypothesis proposed that the continents were once joined together in a supercontinent called Pangaea before breaking apart around 200 million years ago. Evidence for continental drift includes matching fossils found on separate continents, matching rock types and mountain structures that end at one coastline and reappear across an ocean, and indications of ancient shared climates. Plate tectonics theory holds that the lithosphere, the rigid outer layer of Earth, is broken into plates that move over the asthenosphere in the upper mantle. There are three types of plate boundaries: divergent where plates move apart, convergent where they move together, and transform where they grind past each other.
Plates
This document discusses natural hazards caused by tectonic and climate-related events. It provides details on the internal structure of the Earth, including the crust and mantle. It then focuses on plate tectonics, explaining the three main types of plate boundaries and associated landforms. Specific examples are given for each plate boundary type. The document also addresses causes of earthquakes and their impacts, as well as types and characteristics of volcanoes.
Plate Boundary.pptx
There are three main types of plate boundaries: divergent boundaries, transform boundaries, and convergent boundaries. Divergent boundaries occur where plates move apart, and can be oceanic or continental in nature. Transform boundaries occur where plates slide past one another. Convergent boundaries occur where plates collide, and can involve continental-continental, oceanic-continental, or oceanic-oceanic collisions. These boundaries result in different geological features like mid-ocean ridges, rift valleys, subduction zones, and mountain ranges.
Prema
plate tectonic theory,how seafloor spread and how mountain are build,polar wandering, Hot spot, kober's geosynclinal orogen hypothesis
Chapter 3 Plate Tectonics
This document discusses plate tectonics and the evidence that supports the theory. It describes how Alfred Wegener first proposed continental drift in 1912 and how the theory was rejected until the 1950s. The discovery of mid-ocean ridges provided evidence that the ocean floors were spreading and pushing the continents apart. Rocks and fossils found on separated continents matched and indicated they were once joined together in a supercontinent called Pangaea. The theory of plate tectonics emerged, linking continental drift and seafloor spreading to explain how the Earth's crust has evolved over time.
Chapter 3 Plate Tectonics
This document discusses plate tectonics and the evidence that supports the theory. It describes how Alfred Wegener first proposed continental drift in 1912 and how the theory was rejected until the 1950s. The discovery of mid-ocean ridges provided evidence that the ocean floors were spreading and pushing the continents apart. Rocks and fossils found on separated continents matched and indicated they were once joined together in a supercontinent called Pangaea. The theory of plate tectonics emerged, linking continental drift and seafloor spreading to explain how the Earth's crust has evolved over time through the movement of tectonic plates.
Similar to Plate tectonics (20)
2016 Pure Geog Chapter 1 living with tectonic hazards complete
2016 Pure Geog Chapter 1 living with tectonic hazards complete
Sara Arif - EDSC 304 - Teacher Lecture & Guided Notes - Plate Tectonics and E...
Sara Arif - EDSC 304 - Teacher Lecture & Guided Notes - Plate Tectonics and E...
Geography Elective/Pure Chapter 1/2: Plate tectonic Gateway 1, 2, 3
Geography Elective/Pure Chapter 1/2: Plate tectonic Gateway 1, 2, 3
More from Brandi
Speed and Time graphs
This document provides information about distance vs time graphs and speed vs time graphs. It discusses key concepts such as:
- No movement results in a flat line graph for distance vs time and speed vs time
- Constant speed results in a straight line graph for both with the slope equal to the speed
- Acceleration results in a curved line graph for speed vs time with the slope of the line indicating the acceleration
Weather winds, air masses, air pressures, fronts
Here are the quiz questions:
1. What causes convection in the atmosphere?
2. Why does warm air rise and cold air sink?
3. What are the four main air masses that affect the US?
4. What type of front brings clearing conditions after it passes through?
5. What type of front moves slowly with rain developing gradually ahead of it?
Take 5 minutes to answer the questions individually on your paper. Then we'll go over the answers together.
Adaptation and selective breeding
The document discusses how physical features in animals evolve over generations through natural selection to help animals obtain food, stay safe from predators, build homes, withstand weather, and attract mates. It provides examples of physical features like beak shape, number of fingers, fur color and thickness, and nose or ear shape. Defensive adaptations against predators through hiding, camouflage, group defense, fleeing, and warnings are also discussed. Natural selection requires that organisms produce more offspring than can survive, individuals vary in their characteristics, and characteristics are inherited from parents. Through natural selection, characteristics evolve over time to resemble those of better-suited ancestors who survive and reproduce more successfully.
Adaptation and selective breeding
Animals develop physical features over many generations through natural selection that help them obtain food, stay safe from predators, build homes, withstand weather, and attract mates. These features are not acquired during an animal's lifetime but are inherited from parents and include traits like beak shape, number of fingers, fur color and thickness, and nose or ear shape. Many organisms avoid predators through camouflage, hiding, fleeing, or warning signals. The peppered moth example illustrates how a dark color mutation provided camouflage for moths in polluted areas, making the dark form more common than the light form.
Weather - Winds, air masses, air pressures, fronts
Weather occurs due to convection currents in the atmosphere caused by uneven heating from the sun. Warm air rises at the equator forming clouds, while cool air sinks at the poles. High and low pressure systems move across the globe along jet streams, bringing different weather depending on whether air is ascending or descending. Fronts separate air masses and influence whether conditions are sunny or stormy as warm and cold air interact.
Seasons
The seasons are caused by the 23.5 degree tilt of the Earth's axis as it revolves around the sun, resulting in different parts of the Earth receiving more or less direct sunlight over the course of a year. Summer occurs in the northern hemisphere when its axis is tilted toward the sun, producing longer days, and winter happens when the axis is tilted away from the sun for shorter days. The changing position of the Earth relative to the sun's rays is responsible for seasonal variations in weather patterns and daylight hours around the world.
Volcanoes
Volcanoes erupt when pressure from gases and magma built up in the volcano's magma chamber is too great. This is similar to the pressure build up in a balloon until it bursts. When the pressure is released, gases and molten rock (magma) are ejected from the volcano in explosive eruptions or flow out as lava in nonexplosive eruptions. Volcanoes form at boundaries where tectonic plates meet, especially at subduction zones, as well as at hot spots in the mantle.
Classroom pictures from 1st and 2nd nine weeks
The document contains pictures from classrooms during the first and second nine weeks of the school year. Students can be seen working individually and collaboratively on various academic activities and projects. The pictures provide a snapshot into classroom learning and engagement during the early part of the school year.
Unicellular and mulitcellular
This document discusses unicellular and multicellular organisms. Unicellular organisms are made of only one cell and include bacteria, amoebas, and unicellular fungi and yeasts. They are microscopic and need to be seen with a microscope. Multicellular organisms are made of two or more cells and include humans, cats, dogs, insects, trees and more. They can be seen with the naked eye and need all parts to survive. Examples are given of both unicellular and multicellular organisms.
What is a chromosome anyway
Chromosomes are structures that carry genetic information in the form of DNA. They are found in the nucleus of human cells and determine characteristics like eye color and blood type. Each human cell normally contains 23 pairs of chromosomes, for a total of 46.
Viruses
This document summarizes key information about viruses and bacteria from a biology chapter 17 presentation. It defines viruses as non-cellular particles composed of genetic material and protein that can invade living cells. It lists many common viral diseases such as the cold, flu, smallpox, measles, and AIDS. The document also explains that viruses are transmitted through coughing, sneezing, touching contaminated surfaces, and sharing of body fluids.
Genetics introduction
The document introduces key concepts in genetics including chromosomes, DNA, genes, traits, genotypes, phenotypes, alleles, heterozygous, homozygous, and Punnett squares. It explains that chromosomes contain DNA and are found in pairs, with one from each parent. Genes are segments of DNA that determine traits. Genotypes are the genetic makeup and phenotypes are the physical traits. Dominant and recessive alleles and heterozygous and homozygous conditions are also defined. Punnett squares are introduced as a tool to predict the probability of traits in offspring based on the parents' alleles.
Electromagnetic spectrum
The document discusses the electromagnetic spectrum, which includes different types of electromagnetic waves that transfer energy, including visible light, infrared, ultraviolet, microwaves, radio waves, X-rays, and gamma rays. These waves have different wavelengths and frequencies and travel through space at the speed of light. Visible light is the only part of the electromagnetic spectrum that humans can see, but all types are forms of radiation. The document provides examples of how different types of electromagnetic waves are used, such as radio waves for communication, microwaves for cooking, and X-rays for medical imaging.
Extension on wavelenghts and the spectrum
Electromagnetic radiation, including light, comes in a wide range of wavelengths and is used by astronomers to study astronomical objects. Radio waves have the longest wavelengths while gamma rays have the shortest. Astronomers use spectroscopes to separate starlight into colors and study spectra, allowing them to determine properties of stars like their composition, temperature, and luminosity. Looking at objects across different wavelengths provides additional information.
Newton's laws of motion
This document summarizes Newton's three laws of motion:
1) An object at rest stays at rest and an object in motion stays in motion unless acted upon by an unbalanced force. This law is known as the law of inertia.
2) The acceleration of an object as produced by a net force is directly proportional to the magnitude of the net force, in the same direction as the net force, and inversely proportional to the mass of the object. This is expressed by F=ma.
3) For every action, there is an equal and opposite reaction. The forces of action and reaction between two objects always act in opposite directions.
Acceleration
1) Acceleration is the rate of change of velocity with time. It can be positive, indicating an increase in speed or change in direction, or negative, indicating a decrease in speed or change in direction.
2) A car accelerating from 60 mph to 90 mph in 3 seconds has an acceleration of 10 mph/sec. A car braking from 60 mph to a stop in 6 seconds has a negative acceleration of -10 mph/sec.
3) Falling objects near the Earth's surface accelerate at approximately 10 m/s2 due to gravity. Their velocity increases linearly with time until air resistance balances the gravitational force and the object reaches terminal velocity.
Acceleration
Each time you take a step or a vehicle changes speed or direction, it is experiencing acceleration. Acceleration is the rate of change of velocity over time and can be calculated as the change in velocity divided by the time elapsed. For example, a car accelerating from 60 mph to 90 mph in 3 seconds has an acceleration of 10 mph/s. Acceleration can be positive, like the car speeding up, or negative, like when braking and slowing down. Over time, the constant acceleration due to gravity causes objects in free fall to increase their velocity, gaining 10 m/s every second until air resistance balances the downward force.
Acids and bases
This document discusses compounds, acids, and bases. It defines compounds as groups of bonded elements and lists some common chemical compounds along with their elemental compositions. Acids are defined as compounds that donate hydrogen ions in solution and have a low pH, while bases donate hydroxide ions, have a high pH, and are often used for cleaning. Examples of acids and bases are provided. The document also discusses using indicators like litmus paper to determine if a substance is an acid or base based on the color change, and that acids and bases neutralize through reactions that produce water.
Periodic table
The periodic table organizes the elements and provides useful information to chemists. It was developed by Dmitri Mendeleev in the late 1800s by arranging elements in rows by atomic weight and columns by chemical properties. The modern periodic table arranges elements by atomic number and divides them into groups and periods that predict chemical and physical trends. The position of an element on the periodic table reveals its valence electrons and how it will bond and react.
Atomic Theory
The document discusses the classification of elements and the periodic table. It explains that elements are arranged in the periodic table according to their atomic structure and properties, with similar elements grouped together. The periodic table is divided into rows and columns, with each row representing an energy level and each column representing common chemical properties. The position of an element in the table predicts its chemical behavior and reactivity with other elements.
More from Brandi (20)
Weather - Winds, air masses, air pressures, fronts
Weather - Winds, air masses, air pressures, fronts
Recently uploaded
一比一原版(OP毕业证)奥塔哥理工学院毕业证成绩单如何办理
OP毕业证【微信95270640】《如何办理奥塔哥理工学院毕业证认证》【办证Q微信95270640】《奥塔哥理工学院文凭毕业证制作》《OP学历学位证书哪里买》办理奥塔哥理工学院学位证书扫描件、办理奥塔哥理工学院雅思证书！
国际留学归国服务中心《如何办奥塔哥理工学院毕业证认证》《OP学位证书扫描件哪里买》实体公司，注册经营，行业标杆，精益求精！
如果您是以下情况，我们都能竭诚为您解决实际问题：【公司采用定金+余款的付款流程，以最大化保障您的利益，让您放心无忧】
1、在校期间，因各种原因未能顺利毕业，拿不到官方毕业证+微信95270640
2、面对父母的压力，希望尽快拿到奥塔哥理工学院奥塔哥理工学院毕业证学位证；
3、不清楚流程以及材料该如何准备奥塔哥理工学院奥塔哥理工学院毕业证学位证；
4、回国时间很长，忘记办理；
5、回国马上就要找工作，办给用人单位看；
6、企事业单位必须要求办理的；
面向美国乔治城大学毕业留学生提供以下服务:
【★奥塔哥理工学院奥塔哥理工学院毕业证学位证毕业证、成绩单等全套材料，从防伪到印刷，从水印到钢印烫金，与学校100%相同】
【★真实使馆认证（留学人员回国证明），使馆存档可通过大使馆查询确认】
【★真实教育部认证，教育部存档，教育部留服网站可查】
【★真实留信认证，留信网入库存档，可查奥塔哥理工学院奥塔哥理工学院毕业证学位证】
我们从事工作十余年的有着丰富经验的业务顾问，熟悉海外各国大学的学制及教育体系，并且以挂科生解决毕业材料不全问题为基础，为客户量身定制1对1方案，未能毕业的回国留学生成功搭建回国顺利发展所需的桥梁。我们一直努力以高品质的教育为起点，以诚信、专业、高效、创新作为一切的行动宗旨，始终把“诚信为主、质量为本、客户第一”作为我们全部工作的出发点和归宿点。同时为海内外留学生提供大学毕业证购买、补办成绩单及各类分数修改等服务；归国认证方面，提供《留信网入库》申请、《国外学历学位认证》申请以及真实学籍办理等服务，帮助众多莘莘学子实现了一个又一个梦想。
专业服务，请勿犹豫联系我
如果您真实毕业回国，对于学历认证无从下手，请联系我，我们免费帮您递交
诚招代理：本公司诚聘当地代理人员，如果你有业余时间，或者你有同学朋友需要，有兴趣就请联系我
你赢我赢，共创双赢
你做代理，可以帮助奥塔哥理工学院同学朋友
你做代理，可以拯救奥塔哥理工学院失足青年
你做代理，可以挽救奥塔哥理工学院一个个人才
你做代理，你将是别人人生奥塔哥理工学院的转折点
你做代理，可以改变自己，改变他人，给他人和自己一个机会顿时留恋起家乡的小河潺潺活水清凉无比日子就这样孤寂而快乐地过着寂寞之余山娃最神往最开心就是晚上无论多晚多累父亲总要携山娃出去兜风逛夜市流光溢彩人潮涌动的都市夜生活总让山娃目不暇接惊叹不已父亲老问山娃想买什么想吃什么山娃知道父亲赚钱很辛苦除了书籍和文具山娃啥也不要能牵着父亲的手满城闲逛他已心满意足了父亲连挑了三套童装叫山娃试穿山娃有点不想父亲说城里不比乡下要穿得漂漂亮亮爸怎么不穿得漂亮望着父亲山娃可
AadiShakti Projects ( Asp Cranes ) Raipur
Welcome to ASP Cranes, your trusted partner for crane solutions in Raipur, Chhattisgarh! With years of experience and a commitment to excellence, we offer a comprehensive range of crane services tailored to meet your lifting and material handling needs.
At ASP Cranes, we understand the importance of reliable and efficient crane operations in various industries, from construction and manufacturing to logistics and infrastructure development. That's why we strive to deliver top-notch solutions that enhance productivity, safety, and cost-effectiveness for our clients.
Our services include:
Crane Rental: Whether you need a crawler crane for heavy lifting or a hydraulic crane for versatile operations, we have a diverse fleet of well-maintained cranes available for rent. Our rental options are flexible and can be customized to suit your project requirements.
Crane Sales: Looking to invest in a crane for your business? We offer a wide selection of new and used cranes from leading manufacturers, ensuring you find the perfect equipment to match your needs and budget.
Crane Maintenance and Repair: To ensure optimal performance and safety, regular maintenance and timely repairs are essential for cranes. Our team of skilled technicians provides comprehensive maintenance and repair services to keep your equipment running smoothly and minimize downtime.
Crane Operator Training: Proper training is crucial for safe and efficient crane operation. We offer specialized training programs conducted by certified instructors to equip operators with the skills and knowledge they need to handle cranes effectively.
Custom Solutions: We understand that every project is unique, which is why we offer custom crane solutions tailored to your specific requirements. Whether you need modifications, attachments, or specialized equipment, we can design and implement solutions that meet your needs.
At ASP Cranes, customer satisfaction is our top priority. We are dedicated to delivering reliable, cost-effective, and innovative crane solutions that exceed expectations. Contact us today to learn more about our services and how we can support your project in Raipur, Chhattisgarh, and beyond. Let ASP Cranes be your trusted partner for all your crane needs!
What Could Be Behind Your Mercedes Sprinter's Power Loss on Uphill Roads
Unlock the secrets behind your Mercedes Sprinter's uphill power loss with our comprehensive presentation. From fuel filter blockages to turbocharger troubles, we uncover the culprits and empower you to reclaim your vehicle's peak performance. Conquer every ascent with confidence and ensure a thrilling journey every time.
一比一原版(Columbia文凭证书)哥伦比亚大学毕业证如何办理
一模一样【微信：176555708】【(Columbia文凭证书)哥伦比亚大学毕业证成绩单Offer】【微信：176555708】（留信学历认证永久存档查询）采用学校原版纸张、特殊工艺完全按照原版一比一制作（包括：隐形水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠，文字图案浮雕，激光镭射，紫外荧光，温感，复印防伪）行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备，十五年致力于帮助留学生解决难题，业务范围有加拿大、英国、澳洲、韩国、美国、新加坡，新西兰等学历材料，包您满意。
【业务选择办理准则】
一、工作未确定，回国需先给父母、亲戚朋友看下文凭的情况，办理一份就读学校的毕业证【微信：176555708】文凭即可
二、回国进私企、外企、自己做生意的情况，这些单位是不查询毕业证真伪的，而且国内没有渠道去查询国外文凭的真假，也不需要提供真实教育部认证。鉴于此，办理一份毕业证【微信：176555708】即可
三、进国企，银行，事业单位，考公务员等等，这些单位是必需要提供真实教育部认证的，办理教育部认证所需资料众多且烦琐，所有材料您都必须提供原件，我们凭借丰富的经验，快捷的绿色通道帮您快速整合材料，让您少走弯路。
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
→ 【关于价格问题（保证一手价格）
我们所定的价格是非常合理的，而且我们现在做得单子大多数都是代理和回头客户介绍的所以一般现在有新的单子 我给客户的都是第一手的代理价格，因为我想坦诚对待大家 不想跟大家在价格方面浪费时间
对于老客户或者被老客户介绍过来的朋友，我们都会适当给一些优惠。
选择实体注册公司办理，更放心，更安全！我们的承诺：可来公司面谈，可签订合同，会陪同客户一起到教育部认证窗口递交认证材料，客户在教育部官方认证查询网站查询到认证通过结果后付款，不成功不收费！
快速办理(napier毕业证书)英国龙比亚大学毕业证在读证明一模一样
学校原件一模一样【微信：741003700 】《(napier毕业证书)英国龙比亚大学毕业证》【微信：741003700 】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
【主营项目】
一.毕业证【q微741003700】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【q/微741003700】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
一比一原版(AUT毕业证)奥克兰理工大学毕业证成绩单如何办理
AUT毕业证【微信95270640】奥克兰理工大学毕业证购买,办理AUT成绩单,AUT毕业证制作【Q微信95270640】《奥克兰理工大学毕业证》，AUT毕业证购买，AUT学位证，奥克兰理工大学学位证《AUT成绩单制作》【AUT毕业证文凭 AUT本科 澳洲学历认证原版制作《diploma certificate degree transcript 》【留信网认证，本科，硕士，海归，博士，排名，成绩单】代办国外（海外）澳洲、韩国、加拿大、新西兰等各大学毕业证。 ?我们对海外大学及学院的毕业证成绩单所使用的材料，尺寸大小，防伪结构（包括：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。 文字图案浮雕，激光镭射，紫外荧光，温感，复印防伪）都有原版本文凭对照。
[留学文凭学历认证(留信认证使馆认证)奥克兰理工大学毕业证成绩单毕业证证书大学Offer请假条成绩单语言证书国际回国人员证明高仿教育部认证申请学校等一切高仿或者真实可查认证服务。
多年留学服务公司,拥有海外样板无数能完美1:1还原海外各国大学degreeDiplomaTranscripts等毕业材料。海外大学毕业材料都有哪些工艺呢？工艺难度主要由：烫金.钢印.底纹.水印.防伪光标.热敏防伪等等组成。而且我们每天都在更新海外文凭的样板以求所有同学都能享受到完美的品质服务。
国外毕业证学位证成绩单办理方法：
1客户提供办理奥克兰理工大学奥克兰理工大学毕业证成绩单信息：姓名生日专业学位毕业时间等（如信息不确定可以咨询顾问：我们有专业老师帮你查询）；
2开始安排制作毕业证成绩单电子图；
3毕业证成绩单电子版做好以后发送给您确认；
4毕业证成绩单电子版您确认信息无误之后安排制作成品；
5成品做好拍照或者视频给您确认；
6快递给客户（国内顺丰国外DHLUPS等快读邮寄）
— — — — 我们是挂科和未毕业同学们的福音我们是实体公司精益求精的工艺！ — — — -
一真实留信认证的作用(私企外企荣誉的见证):
1：该专业认证可证明留学生真实留学身份同时对留学生所学专业等级给予评定。
2：国家专业人才认证中心颁发入库证书这个入网证书并且可以归档到地方。
3：凡是获得留信网入网的信息将会逐步更新到个人身份内将在公安部网内查询个人身份证信息后同步读取人才网入库信息。
4：个人职称评审加20分个人信誉贷款加10分。
5：在国家人才网主办的全国网络招聘大会中纳入资料供国家500强等高端企业选择人才。电总将小方桌搁在门口看书写作业有一次山娃坐在门口写作业写着写着竟伏在桌上睡着了迷迷糊糊中山娃似乎听到了父亲的脚步声当他晃晃悠悠站起来时才诧然发现一位衣衫破旧的妇女挎着一只硕大的蛇皮袋手里拎着长铁钩正站在门口朝黑色的屋内张望不好坏人小偷山娃一怔却也灵机一动立马仰起头双手拢在嘴边朝楼上大喊：“爸爸爸——有人找——那人一听朝山娃尴尬地笑笑悻悻地走了山娃立马“嘭的一声将铁门锁死心却咚咚地乱跳当山娃跟父亲有
Here's Why Every Semi-Truck Should Have ELDs
Implementing ELDs or Electronic Logging Devices is slowly but surely becoming the norm in fleet management. Why? Well, integrating ELDs and associated connected vehicle solutions like fleet tracking devices lets businesses and their in-house fleet managers reap several benefits. Check out the post below to learn more.
EV Charging at Multifamily Properties by Kevin Donnelly
Kevin Donnelly gave this presentation at the Forth Addressing The Challenges of Charging at Multi-Family Housing webinar on June 11, 2024.
一比一原版(WashU文凭证书)圣路易斯华盛顿大学毕业证如何办理
一模一样【微信：176555708】【(WashU文凭证书)圣路易斯华盛顿大学毕业证成绩单Offer】【微信：176555708】（留信学历认证永久存档查询）采用学校原版纸张、特殊工艺完全按照原版一比一制作（包括：隐形水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠，文字图案浮雕，激光镭射，紫外荧光，温感，复印防伪）行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备，十五年致力于帮助留学生解决难题，业务范围有加拿大、英国、澳洲、韩国、美国、新加坡，新西兰等学历材料，包您满意。
【业务选择办理准则】
一、工作未确定，回国需先给父母、亲戚朋友看下文凭的情况，办理一份就读学校的毕业证【微信：176555708】文凭即可
二、回国进私企、外企、自己做生意的情况，这些单位是不查询毕业证真伪的，而且国内没有渠道去查询国外文凭的真假，也不需要提供真实教育部认证。鉴于此，办理一份毕业证【微信：176555708】即可
三、进国企，银行，事业单位，考公务员等等，这些单位是必需要提供真实教育部认证的，办理教育部认证所需资料众多且烦琐，所有材料您都必须提供原件，我们凭借丰富的经验，快捷的绿色通道帮您快速整合材料，让您少走弯路。
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
→ 【关于价格问题（保证一手价格）
我们所定的价格是非常合理的，而且我们现在做得单子大多数都是代理和回头客户介绍的所以一般现在有新的单子 我给客户的都是第一手的代理价格，因为我想坦诚对待大家 不想跟大家在价格方面浪费时间
对于老客户或者被老客户介绍过来的朋友，我们都会适当给一些优惠。
选择实体注册公司办理，更放心，更安全！我们的承诺：可来公司面谈，可签订合同，会陪同客户一起到教育部认证窗口递交认证材料，客户在教育部官方认证查询网站查询到认证通过结果后付款，不成功不收费！
What do the symbols on vehicle dashboard mean?
Ever been troubled by the blinking sign and didn’t know what to do?
Here’s a handy guide to dashboard symbols so that you’ll never be confused again!
Save them for later and save the trouble!
Digital Fleet Management - Why Your Business Need It?
Fleet management these days is next to impossible without connected vehicle solutions. Why? Well, fleet trackers and accompanying connected vehicle management solutions tend to offer quite a few hard-to-ignore benefits to fleet managers and businesses alike. Let’s check them out!
Hand Gesture Control Robotic Arm using image processing.pptx
Hand Gesture Control Robotic Arm using image processing
一比一原版(UNITEC毕业证)UNITEC理工学院毕业证成绩单如何办理
UNITEC毕业证【微信95270640】☀《UNITEC理工学院毕业证购买》Q微信95270640《UNITEC毕业证模板办理》文凭、本科、硕士、研究生学历都可以做,《文凭UNITEC毕业证书原版制作UNITEC成绩单》《仿制UNITEC毕业证成绩单UNITEC理工学院学位证书pdf电子图》毕业证
全套服务：UNITEC理工学院UNITEC理工学院硕士毕业证成绩单真实回国人员证明 #真实教育部认证。让您回国发展信心十足#铸就十年品质！信誉！实体公司！可以视频看办公环境样板如需办理真实可查可以先到公司面谈勿轻信小中介黑作坊！
可以提供UNITEC理工学院钢印 #水印 #烫金 #激光防伪 #凹凸版 #最新版的毕业证 #百分之百让您绝对满意
印刷DHL快递毕业证 #成绩单7个工作日真实大使馆教育部认证1个月。为了达到高水准高效率
请您先以qq或微信的方式对我们的服务进行了解后如果有UNITEC理工学院UNITEC理工学院硕士毕业证成绩单帮助再进行电话咨询。
国外毕业证学位证成绩单如何办理：
1客户提供办理信息：姓名生日专业学位毕业时间等（如信息不确定可以咨询顾问：我们有专业老师帮你查询）；
2开始安排制作UNITEC理工学院毕业证成绩单电子图；
3毕业证成绩单电子版做好以后发送给您确认；
4毕业证成绩单电子版您确认信息无误之后安排制作成品；
5成品做好拍照或者视频给您确认；
6快递给客户（国内顺丰国外DHLUPS等快读邮寄）。嘿嘿的笑连连说记得记得但别忘了拿奖状进城啊考试一结束山娃就迫不及待地给父亲挂电话：爸我拿奖了三好学生接我进城吧父亲果然没有食言第二天就请假回家接山娃离开爷爷奶奶的那一刻山娃又伤心得泪如雨下宛如军人奔赴前线般难舍和悲壮卧空调大巴挤长蛇列车山娃发现车上挤满了叽叽喳喳的同龄人皆一脸惊喜地四处瞅山娃不认识他们也无暇去套近乎一味地跟着父亲昼夜兼程第二天凌晨就辗转到了父亲的城哇父亲的城真的好大好美哟走出广州有
一比一原版(AIS毕业证)奥克兰商学院毕业证成绩单如何办理
AIS毕业证【微信95270640】《如何办理AIS毕业证奥克兰商学院文凭学历》【Q微信95270640】《奥克兰商学院文凭学历证书》《奥克兰商学院毕业证书与成绩单样本图片》毕业证书补办 Fake Degree做学费单《毕业证明信-推荐信》成绩单，录取通知书，Offer，在读证明，雅思托福成绩单，真实大使馆教育部认证，回国人员证明，留信网认证。网上存档永久可查！
如果您是以下情况，我们都能竭诚为您解决实际问题：【公司采用定金+余款的付款流程，以最大化保障您的利益，让您放心无忧】
1、在校期间，因各种原因未能顺利毕业，拿不到官方毕业证+微信95270640
2、面对父母的压力，希望尽快拿到奥克兰商学院奥克兰商学院毕业证学历书；
3、不清楚流程以及材料该如何准备奥克兰商学院奥克兰商学院毕业证学历书；
4、回国时间很长，忘记办理；
5、回国马上就要找工作，办给用人单位看；
6、企事业单位必须要求办理的；
面向美国乔治城大学毕业留学生提供以下服务:
【★奥克兰商学院奥克兰商学院毕业证学历书毕业证、成绩单等全套材料，从防伪到印刷，从水印到钢印烫金，与学校100%相同】
【★真实使馆认证（留学人员回国证明），使馆存档可通过大使馆查询确认】
【★真实教育部认证，教育部存档，教育部留服网站可查】
【★真实留信认证，留信网入库存档，可查奥克兰商学院奥克兰商学院毕业证学历书】
我们从事工作十余年的有着丰富经验的业务顾问，熟悉海外各国大学的学制及教育体系，并且以挂科生解决毕业材料不全问题为基础，为客户量身定制1对1方案，未能毕业的回国留学生成功搭建回国顺利发展所需的桥梁。我们一直努力以高品质的教育为起点，以诚信、专业、高效、创新作为一切的行动宗旨，始终把“诚信为主、质量为本、客户第一”作为我们全部工作的出发点和归宿点。同时为海内外留学生提供大学毕业证购买、补办成绩单及各类分数修改等服务；归国认证方面，提供《留信网入库》申请、《国外学历学位认证》申请以及真实学籍办理等服务，帮助众多莘莘学子实现了一个又一个梦想。
专业服务，请勿犹豫联系我
如果您真实毕业回国，对于学历认证无从下手，请联系我，我们免费帮您递交
诚招代理：本公司诚聘当地代理人员，如果你有业余时间，或者你有同学朋友需要，有兴趣就请联系我
你赢我赢，共创双赢
你做代理，可以帮助奥克兰商学院同学朋友
你做代理，可以拯救奥克兰商学院失足青年
你做代理，可以挽救奥克兰商学院一个个人才
你做代理，你将是别人人生奥克兰商学院的转折点
你做代理，可以改变自己，改变他人，给他人和自己一个机会的笑连连说记得记得但别忘了拿奖状进城啊考试一结束山娃就迫不及待地给父亲挂电话：爸我拿奖了三好学生接我进城吧父亲果然没有食言第二天就请假回家接山娃离开爷爷奶奶的那一刻山娃又伤心得泪如雨下宛如军人奔赴前线般难舍和悲壮卧空调大巴挤长蛇列车山娃发现车上挤满了叽叽喳喳的同龄人皆一脸惊喜地四处瞅山娃不认识他们也无暇去套近乎一味地跟着父亲昼夜兼程第二天凌晨就辗转到了父亲的城哇父亲的城真的好大好美哟走出广州火车方
原版制作(Exeter毕业证书)埃克塞特大学毕业证完成信一模一样
学校原件一模一样【微信：741003700 】《(Exeter毕业证书)埃克塞特大学毕业证》【微信：741003700 】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
【主营项目】
一.毕业证【q微741003700】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【q/微741003700】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
Recently uploaded (20)
Manual despiece Yamaha fuera de borda pc_e40x_02.pdf
Manual despiece Yamaha fuera de borda pc_e40x_02.pdf
What Could Be Behind Your Mercedes Sprinter's Power Loss on Uphill Roads
What Could Be Behind Your Mercedes Sprinter's Power Loss on Uphill Roads
EV Charging at Multifamily Properties by Kevin Donnelly
EV Charging at Multifamily Properties by Kevin Donnelly
Digital Fleet Management - Why Your Business Need It?
Digital Fleet Management - Why Your Business Need It?
Hand Gesture Control Robotic Arm using image processing.pptx
Hand Gesture Control Robotic Arm using image processing.pptx
Globalfleet - global fleet survey 2021 full results
Globalfleet - global fleet survey 2021 full results
Plate tectonics
- 2. Plate Tectonics • Pieces of the lithosphere that move around • Each plate has a name • Fit together like jigsaw puzzles • Float on top of mantle similar to ice cubes in a bowl of water
- 3. Continental Drift •Alfred Wegener 1900’s Continents were once a single land mass that drifted apart. •Fossils of the same plants and animals are found on different continents •Called this supercontinent Pangea, Greek for “all Earth”
- 4. Pangea
- 7. Sea Floor Spreading • Mid Ocean Ridges – underwater mountain chains that run through the Earth’s Basins • Magma rises to the surface and solidifies and new crust forms • Older Crust is pushed farther away from the ridge Two Volunteers to Demonstrate
- 10. Different Types of Boundaries Animations
- 11. Divergent Boundary – Arabian and African Plates
- 12. Divergent Boundaries • Places where plates are coming apart • Forms a central valley called a rift • Earthquakes occur along the faults • Volcanoes form where the magma reaches the surface. • Plate separation is a slow process. For example, divergence along the Mid Atlantic ridge causes the Atlantic Ocean to widen at only about 2 centimeters per year. Animation
- 13. Divergent Boundary – Iceland
- 14. Divergent Boundary - Oceanic
- 15. Divergent Boundary - Continental
- 16. Convergent Boundary •Places where plates crash or crunch together •Collisions are very slow and last millions of years •Mountains, earthquakes, and volcanoes form where plates collide •Rockies in North America, the Alps in Europe, the Pontic Mountains in Turkey, the Zagros Mountains in Iran, and the Himalayas in central Asia were formed by plate
- 17. Convergent Boundary – Indian and Eurasian Plates Himalayas
- 18. Transform Boundaries •Places where plates slide past each other •Marked in some places by linear valleys where rock has been ground up by the sliding
- 19. Transform Boundary – San Andreas Fault in California
- 20. Subduction Zone • When two oceanic plates collide, the younger of the two plates, because it is less dense, will ride over the edge of the older plate.
- 21. Review • Name the 3 main layers of the Earth. • What is a tectonic plate? • What was Pangea? • What is Sea-Floor spreading? • Name the three different types of plate boundaries and one location on Earth for each one
- 22. 1. In your basket you should have wax paper, a plastic spoon, fruit roll-up and a graham cracker 2. I will come around and put a small amount of icing on your wax paper.
- 23. 1. Divergent Boundary – Notice how the frosting is exposed and pushed up where the plates are separated? – This is how magma comes to the surface where plates are moving apart at divergent boundaries – When plates begin to pull apart
- 24. 1. Continent-Oceanic Convergent Boundary – The graham cracker represents the continental crust, which is thicker and less dense than oceanic crust (fruit roll-up). – After you complete Step 3, the oceanic plate will be subducted below the continental one.
- 25. 1. Continent – Continent Convergent Boundary – This is when two continents collide – Notice how the wet edges crumble? – This is how mountains are made at convergegnt plate boundaries. – When continents move toward each other, there is nowhere for the rock to go but up.
- 26. Snack Tectonics 1. Transform Boundary