Chapter2 principleofgeology1meeting-160409105612
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This document discusses plate tectonics and the three types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. Divergent boundaries occur where plates move apart, like at mid-ocean ridges, convergent boundaries occur where plates move together and one plate subducts under the other, forming mountain ranges. Transform boundaries occur where plates slide past each other horizontally, like at the San Andreas fault. The document provides examples of each boundary type and discusses how the different interactions between oceanic and continental plates result in volcanism, earthquakes, and mountain building.
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The document describes three main types of plate boundaries: convergent boundaries, divergent boundaries, and transform boundaries. Convergent boundaries occur when plates collide and include ocean-ocean, ocean-continent, and continent-continent convergence. Divergent boundaries exist when plates move apart, such as at oceanic spreading ridges and ancient continental rift valleys. Transform boundaries occur when plates slide past each other horizontally along transform faults. Volcanoes form at ocean-ocean convergent boundaries and ocean-continent convergent boundaries where one plate subducts under the other.
Convergent boundaries
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.
Plate boundaries
There are three main types of plate boundaries: 1) transform boundaries where plates slide horizontally past one another like the San Andreas Fault, 2) convergent boundaries where plates collide and one is subducted beneath the other in oceanic trenches or mountain building, and 3) divergent boundaries where plates spread apart like mid-ocean ridges and new crust is formed through volcanic activity.
Convergent plate boundary
Two continental tectonic plates pushing into each other form a convergent boundary, which creates mountain ranges like the Himalayas. Convection currents in the Earth's mantle cause the plates to slowly move towards each other over time, forcing the edges to crumple upwards and form mountain chains along the boundary.
Transform boundary
A transform boundary is a plate boundary where plates move horizontally past each other in opposite directions. Convection currents in the mantle cause plate movement. Transform boundaries collect energy from plate movement that is eventually released through earthquakes and tsunamis, as seen at the San Andreas Fault and from a Pacific Ocean earthquake that caused a major tsunami. While they do not form volcanoes or mountains, transform boundaries can create dangerous earthquakes and tsunamis.
Plate movement and resultant landscape
There are three main types of plate movements that result in different landforms: convergence, divergence, and transform. Convergence occurs when plates collide, forming subduction zones, fold mountains, or continental collisions. Divergence happens when plates move apart, seen at mid-ocean ridges and rifting continents. Transform boundaries are where plates slide past each other, causing earthquakes along faults like the San Andreas. Plate tectonics shapes the Earth's surface through these movements.
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Chapter 1 principle of geology 1 meeting
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Chapter 2 principle of geology 1 meeting
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Ignite
The document describes three main types of plate boundaries: convergent boundaries, divergent boundaries, and transform boundaries. Convergent boundaries occur when plates collide and include ocean-ocean, ocean-continent, and continent-continent convergence. Divergent boundaries exist when plates move apart, such as at oceanic spreading ridges and ancient continental rift valleys. Transform boundaries occur when plates slide past each other horizontally along transform faults. Volcanoes form at ocean-ocean convergent boundaries and ocean-continent convergent boundaries where one plate subducts under the other.
Convergent boundaries
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.
Plate boundaries
There are three main types of plate boundaries: 1) transform boundaries where plates slide horizontally past one another like the San Andreas Fault, 2) convergent boundaries where plates collide and one is subducted beneath the other in oceanic trenches or mountain building, and 3) divergent boundaries where plates spread apart like mid-ocean ridges and new crust is formed through volcanic activity.
Convergent plate boundary
Two continental tectonic plates pushing into each other form a convergent boundary, which creates mountain ranges like the Himalayas. Convection currents in the Earth's mantle cause the plates to slowly move towards each other over time, forcing the edges to crumple upwards and form mountain chains along the boundary.
Transform boundary
A transform boundary is a plate boundary where plates move horizontally past each other in opposite directions. Convection currents in the mantle cause plate movement. Transform boundaries collect energy from plate movement that is eventually released through earthquakes and tsunamis, as seen at the San Andreas Fault and from a Pacific Ocean earthquake that caused a major tsunami. While they do not form volcanoes or mountains, transform boundaries can create dangerous earthquakes and tsunamis.
Plate movement and resultant landscape
There are three main types of plate movements that result in different landforms: convergence, divergence, and transform. Convergence occurs when plates collide, forming subduction zones, fold mountains, or continental collisions. Divergence happens when plates move apart, seen at mid-ocean ridges and rifting continents. Transform boundaries are where plates slide past each other, causing earthquakes along faults like the San Andreas. Plate tectonics shapes the Earth's surface through these movements.
TYPES OF PLATE BOUNDARIES
This document discusses three main types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. It provides examples and describes the geological effects of each boundary type. It also discusses processes at divergent boundaries like mid-ocean ridges and continental rift valleys. Convergent boundaries include oceanic-oceanic convergence forming island arcs, and continental-oceanic convergence forming volcanic mountain ranges. Transform boundaries involve strike-slip faulting along plate edges. Additionally, the document touches on hot spot volcanism unrelated to plate boundaries.
Conservative (Passive) Plate Boundaries
- Conservative (passive) plate boundaries occur where two tectonic plates slide horizontally past one another in opposite directions, causing friction and earthquakes along the fault line where they meet.
- As the plates move, a gap is created behind each one called a fault. The best known example is the San Andreas Fault in California, where the Pacific and North American Plates slide past each other.
- Major earthquakes, like the 1906 San Francisco earthquake, are caused by the built-up friction along the fault line being suddenly released as the plates shift. These earthquakes can cause widespread damage.
Transform plate boundary
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.
When the earth moves
This document discusses plate tectonics and how the earth's crust is made up of moving tectonic plates. It describes how convection currents in the earth's mantle cause the plates to slowly drift via processes such as continental drift. Key terms are defined, including fault, continental drift, subduction zone, convergent boundary, divergent boundary, and transform boundary. Students are tasked to research and investigate plate tectonics using textbooks and include relevant keywords in their explanations of how plate tectonics creates earthquakes and volcanoes.
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The document discusses plate tectonics and the different types of plate boundaries. It explains that tectonic plates are giant pieces of the Earth's crust that are constantly moving. There are three main types of plate boundaries: constructive boundaries where plates move apart and new crust is formed, destructive boundaries where one plate moves under another, and conservative boundaries such as transform faults that offset movement at plate margins. The document also includes quiz questions to test understanding of these concepts.
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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.
Transform Plate Boundaries
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.
Earth science. Plate Tectonics ppt
The document summarizes plate tectonics and the structure and dynamics of the Earth. It describes the four main layers of the Earth and explains that plate tectonics involves the constant motion of tectonic plates due to convection currents in the mantle. It provides evidence that supported the theory of continental drift and discusses how sea floor spreading and subduction at trenches cause the plates to move over time.
Plate boundaries powerpoint
There are three types of plate boundaries: divergent boundaries where plates move apart and new crust is formed at mid-ocean ridges like the Mid-Atlantic Ridge; convergent boundaries where plates move towards each other and ocean crust is destroyed at trenches forming volcanic island arcs; and transform boundaries where plates slide past each other along faults like the San Andreas Fault. Many earthquakes and volcanoes occur on the Ring of Fire around the Pacific Ocean due to the Pacific plate interacting with surrounding plates at their convergent and transform boundaries.
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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.
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This document discusses the different types of plate boundaries including convergent, divergent, and transform boundaries. At convergent boundaries, plates move toward each other forming trenches and volcanic arcs at oceanic-continental boundaries and trenches and island arcs at oceanic-oceanic boundaries. Continental-continental convergent boundaries form mountains. Transform boundaries occur when plates slide past each other, forming tsunamis at oceanic-oceanic boundaries and earthquakes at continental-continental boundaries. Divergent boundaries form when plates move apart, creating mid-ocean ridges at oceanic-oceanic boundaries and rift valleys at continental-continental boundaries.
Tectonic Plates
The document discusses tectonic plates and their movement over time. It explains that tectonic plates are large sections of Earth's crust that are constantly shifting. Approximately 225 million years ago, all the continents were joined together in a supercontinent called Pangea. The plates have since moved apart, forming the current continental configuration. In about 250 million years, the continents are predicted to reconverge into another supercontinent called Pangea Ultima. As plates shift, they interact along boundaries where they can separate, collide, or slide past each other.
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The document provides an overview of mantle plumes and hotspots. It discusses that mantle plumes are columns of hot material rising from deep within the mantle, and hotspots are the surface expression of these plumes seen as volcanic regions. Hotspots have distinct geochemical signatures and are unrelated to tectonic plate boundaries. They can form hotspot tracks as the tectonic plate moves over them, leaving age-progressive volcanic chains. While hotspots were thought to be fixed in the mantle, evidence now suggests they may move slowly relative to each other over geologic timescales. Mantle plumes provide an explanation for various volcanic and tectonic phenomena seen in the interiors of tectonic plates.
Plate Movements Ppt
The document discusses the four spheres of the Earth - atmosphere, hydrosphere, lithosphere, and biosphere. It then describes the layers that make up Earth's interior - crust, mantle, outer core, and inner core. The rest of the document discusses plate tectonic theory, the three types of plate boundaries and movements (divergent, convergent, transform), associated volcanic and earthquake activity, and the impacts of earthquakes and volcanoes.
Divergent plate boundary PPT
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.
Plate Boundaries
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.
Plate Boundaries
The document discusses the structure and composition of the Earth, including the crust, mantle, outer core, and inner core. It also discusses plate tectonics and the different types of plate boundaries: constructive, destructive, conservative, and collision. At destructive boundaries, oceanic plates are subducted under continental plates, forming volcanoes. At collision boundaries, continental plates push together to form mountain ranges. At constructive boundaries, plates move apart and new crust is formed.
Hotspots
Three key points about hotspots:
1) Hotspots are volcanic regions thought to be fed by anomalously hot mantle material rising independently of tectonic plate boundaries. Well-known examples include Hawaii, Iceland, and Yellowstone.
2) There are two hypotheses for the origin of hotspots - one involving mantle plumes rising from the core-mantle boundary, the other involving passive rising of melt from shallow depths.
3) Hotspot tracks provide evidence for the plate tectonics model, as volcanic chains like the Hawaiian Islands can be explained by plates migrating over fixed mantle plumes.
Lesson 4/5 - Natural Processes
The document discusses various landforming processes including:
1. Tectonic processes such as plate tectonics involve convection currents that cause plates to move via diverging, converging, and transform boundaries, creating features like mountains, volcanoes, and faults.
2. Fluvial processes like erosion and deposition by rivers transport and deposit sediment to form landforms.
3. Volcanic processes involve magma rising from convection currents to erupt and form volcanic landforms.
Plate Tectonics Review Answers
1. Plate tectonics describes how the Earth's crust is broken into plates that move relative to each other as magma circulates underneath. Plates can divide, collide, or slide past one another at their boundaries.
2. 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 horizontally.
3. At convergent boundaries, the plates squeeze rock as they move together or subduct one beneath the other.
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This document discusses three main types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. It provides examples and describes the geological effects of each boundary type. It also discusses processes at divergent boundaries like mid-ocean ridges and continental rift valleys. Convergent boundaries include oceanic-oceanic convergence forming island arcs, and continental-oceanic convergence forming volcanic mountain ranges. Transform boundaries involve strike-slip faulting along plate edges. Additionally, the document touches on hot spot volcanism unrelated to plate boundaries.
Conservative (Passive) Plate Boundaries
- Conservative (passive) plate boundaries occur where two tectonic plates slide horizontally past one another in opposite directions, causing friction and earthquakes along the fault line where they meet.
- As the plates move, a gap is created behind each one called a fault. The best known example is the San Andreas Fault in California, where the Pacific and North American Plates slide past each other.
- Major earthquakes, like the 1906 San Francisco earthquake, are caused by the built-up friction along the fault line being suddenly released as the plates shift. These earthquakes can cause widespread damage.
Transform plate boundary
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.
When the earth moves
This document discusses plate tectonics and how the earth's crust is made up of moving tectonic plates. It describes how convection currents in the earth's mantle cause the plates to slowly drift via processes such as continental drift. Key terms are defined, including fault, continental drift, subduction zone, convergent boundary, divergent boundary, and transform boundary. Students are tasked to research and investigate plate tectonics using textbooks and include relevant keywords in their explanations of how plate tectonics creates earthquakes and volcanoes.
Plate Boundaries, Tectonic Plates & Plate Tectonics
The document discusses plate tectonics and the different types of plate boundaries. It explains that tectonic plates are giant pieces of the Earth's crust that are constantly moving. There are three main types of plate boundaries: constructive boundaries where plates move apart and new crust is formed, destructive boundaries where one plate moves under another, and conservative boundaries such as transform faults that offset movement at plate margins. The document also includes quiz questions to test understanding of these concepts.
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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.
Transform Plate Boundaries
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.
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The document summarizes plate tectonics and the structure and dynamics of the Earth. It describes the four main layers of the Earth and explains that plate tectonics involves the constant motion of tectonic plates due to convection currents in the mantle. It provides evidence that supported the theory of continental drift and discusses how sea floor spreading and subduction at trenches cause the plates to move over time.
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There are three types of plate boundaries: divergent boundaries where plates move apart and new crust is formed at mid-ocean ridges like the Mid-Atlantic Ridge; convergent boundaries where plates move towards each other and ocean crust is destroyed at trenches forming volcanic island arcs; and transform boundaries where plates slide past each other along faults like the San Andreas Fault. Many earthquakes and volcanoes occur on the Ring of Fire around the Pacific Ocean due to the Pacific plate interacting with surrounding plates at their convergent and transform boundaries.
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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.
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The document discusses tectonic plates and their movement over time. It explains that tectonic plates are large sections of Earth's crust that are constantly shifting. Approximately 225 million years ago, all the continents were joined together in a supercontinent called Pangea. The plates have since moved apart, forming the current continental configuration. In about 250 million years, the continents are predicted to reconverge into another supercontinent called Pangea Ultima. As plates shift, they interact along boundaries where they can separate, collide, or slide past each other.
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The document provides an overview of mantle plumes and hotspots. It discusses that mantle plumes are columns of hot material rising from deep within the mantle, and hotspots are the surface expression of these plumes seen as volcanic regions. Hotspots have distinct geochemical signatures and are unrelated to tectonic plate boundaries. They can form hotspot tracks as the tectonic plate moves over them, leaving age-progressive volcanic chains. While hotspots were thought to be fixed in the mantle, evidence now suggests they may move slowly relative to each other over geologic timescales. Mantle plumes provide an explanation for various volcanic and tectonic phenomena seen in the interiors of tectonic plates.
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The document discusses the four spheres of the Earth - atmosphere, hydrosphere, lithosphere, and biosphere. It then describes the layers that make up Earth's interior - crust, mantle, outer core, and inner core. The rest of the document discusses plate tectonic theory, the three types of plate boundaries and movements (divergent, convergent, transform), associated volcanic and earthquake activity, and the impacts of earthquakes and volcanoes.
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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.
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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.
Plate Boundaries
The document discusses the structure and composition of the Earth, including the crust, mantle, outer core, and inner core. It also discusses plate tectonics and the different types of plate boundaries: constructive, destructive, conservative, and collision. At destructive boundaries, oceanic plates are subducted under continental plates, forming volcanoes. At collision boundaries, continental plates push together to form mountain ranges. At constructive boundaries, plates move apart and new crust is formed.
Hotspots
Three key points about hotspots:
1) Hotspots are volcanic regions thought to be fed by anomalously hot mantle material rising independently of tectonic plate boundaries. Well-known examples include Hawaii, Iceland, and Yellowstone.
2) There are two hypotheses for the origin of hotspots - one involving mantle plumes rising from the core-mantle boundary, the other involving passive rising of melt from shallow depths.
3) Hotspot tracks provide evidence for the plate tectonics model, as volcanic chains like the Hawaiian Islands can be explained by plates migrating over fixed mantle plumes.
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Plate tectonics is the theory that the Earth's outermost shell is divided into plates that constantly move and interact with one another. Earthquakes, volcanoes, and mountain ranges occur primarily at plate boundaries. 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. Each boundary type results in different geological effects depending on whether oceanic or continental crust is involved in the plate interaction.
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Plate tectonics is the theory that the Earth's outermost shell is divided into plates that constantly move and interact with one another. At plate boundaries, where the plates meet, seismic activity like earthquakes and volcanic eruptions occur. The three main types of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past one another. Each boundary type results in different geological features and phenomena.
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Plate movement
The document describes different types of plate boundaries including divergent boundaries which form grabens and rift valleys, convergent boundaries where oceanic plates subduct under continents (like the Andes) or under other oceanic plates forming island arcs, and transform boundaries where plates slide past each other like the San Andreas Fault. It also discusses examples of each boundary type and how they relate to earthquake and volcanic activity patterns around the world.
Earthquakes
Here are three questions from the section with the answers:
1. What causes convection currents in the mantle?
- Convection currents in the Earth are caused by the Earth's hot inner core heating the magma within the mantle.
2. What is a fault?
- A fault is a fracture, or break, in Earth's lithosphere. Rocks on either side can slide slowly along the fault or stick together, building stress until releasing in an earthquake.
3. Where do most earthquakes occur?
- About 80% of all earthquakes occur in a belt around the edges of the Pacific Ocean, near plate boundaries like the San Andreas Fault where the North American and Pacific plates meet.
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1) Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together and have since drifted apart.
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3) In the 1960s, the theory of plate tectonics was developed, explaining that convection currents in the mantle cause the movement of tectonic plates. Sea floor spreading provided key evidence that the ocean floor continually forms at mid-ocean ridges.
Continental Drift And Plate Tectonics Andie
1) Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together and have since drifted apart.
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Meath Earthquakes 1 1 1 [1]
This document summarizes key concepts of plate tectonics and earthquake formation. Major plate boundaries include convergent boundaries, where plates collide and cause events like mountain building; divergent boundaries, where plates spread apart like at mid-ocean ridges; and transform boundaries like the San Andreas fault, where plates slide past each other. Earthquake waves include P waves and S waves, while surface waves include Love waves and Rayleigh waves. Various plate interactions give rise to different earthquake and volcanic events around the world.
Tectonics: Plate Tectonics
This document discusses the key concepts of plate tectonics including the types of plate boundaries and their associated features and hazards. There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates move together, and conservative boundaries where plates slide past each other laterally. Divergent boundaries form mid-ocean ridges and rift valleys, convergent boundaries involve subduction and result in volcanoes and earthquakes, and conservative boundaries include transform faults like the San Andreas Fault. The document also covers plate tectonic evidence, hotspots, and examples like the Himalayas and Hawaii to illustrate the concepts.
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 Tectonics
This document provides information about plate tectonics and is designed to meet South Carolina science standards. It discusses the layers of the Earth, tectonic plates and their movement, and the three types of plate boundaries - convergent where plates collide, divergent where they separate, and transform where they slide past each other. Specific examples are given for each boundary type, including discussions of sea floor spreading at mid-ocean ridges, subduction zones creating volcanoes and trenches, and the San Andreas Fault as a transform boundary.
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This document discusses suffixes and terminology used in medicine. It begins by listing common combining forms used to build medical terms and their meanings. It then defines several noun, adjective, and shorter suffixes and provides their meanings. Examples are given of medical terms built using combining forms and suffixes. The document also examines specific medical concepts in more depth, such as hernias, blood cells, acromegaly, splenomegaly, and laparoscopy.
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This document is from a textbook on medical terminology. It discusses the basic structure of medical words and how they are built from prefixes, suffixes, and combining forms. Some key points:
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Chapter24 immunology-140105101108-phpapp02
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- 1. Part Two Introduction to Geology Widodo, S.T., M.T. Mining Geology SMK N 1 Balikpapan
- 2. Here comes your footer Page 2 1. Do you know tsunami, volcanism and earthquicke ?. Are they caused by human or natural ? 2. What do you think about crust movement ? Pre Test
- 3. Here comes your footer Page 3 A relatively recent theory that the Earth's crust is composed of rigid plates that move relative to one another. Plate movements are on the order of a few centimeters/year - about the same rate as your fingernails grow! Plate Tectonics There are 3 types of plate boundaries: 1. divergent 2. convergent 3. transform
- 4. Here comes your footer
- 5. Here comes your footer โข Convergent boundaries - plates move together forming a subduction zone and mountain chains. โข Divergent boundaries - plates move apart forming the mid-ocean ridge and seafloor spreading. โข Transform boundaries - plates grind past one another. These boundaries subdivide the mid-ocean ridge and also form the San Andreas fault system.
- 6. Here comes your footer Plate Boundaries: where the real action occurs. The plates are all moving relative to each other. At the boundary between two plates, there must be some motion of one relative to the other. You get three possibilities: Spreading center: Divergent boundary At the top of a rising convection limb. Heat is being brought up. Volcanism. Usually under-ocean. Often associated with a rift valley. Collision zone: Convergent boundary Cold lithosphere bends downward and begins sinking into the mantle (subduction). Mountains are squeezed up here by the collision. Most earthquakes occur here. Parallel plate motion: Transform / Transcurrent / Strike Slip faulting The San Andreas Fault is the most famous transform fault system.
- 7. Here comes your footer
- 8. Here comes your footer Oceanic - Oceanic Convergence - Example: Japan At an ocean-ocean collision, one plate subducts beneath the other, leaving a trace of the process in volcanoes and earthquakes. At the fast collisions (Fiji-Tonga) the subducting plate gets as deep as 700 km while still cool: it is here that you get the deepest (deep focus) earthquakes.
- 9. Here comes your footer Oceanic - Continent Convergence - Example: Andes, Cascades At an ocean-continent collision, the ocean subducts, and the continent rides high. Volcanoes are built on the continental side due to melt which comes off the subducting plate. Nazca-South America is an excellent example.
- 10. Here comes your footer
- 11. Here comes your footer Oceanic Divergent Boundary Example: Mid-Atlantic Ridge
- 12. Here comes your footer Continental Divergent Boundary Example: Red Sea / E. African Rift
- 13. Here comes your footer Continental Divergent Boundary Example: Baja California
- 14. Here comes your footer Page 14 1. Do you know tsunami, volcanism and earthquicke ?. Are they caused by human or natural ? 2. What do you think about crust movement ? Post Test
- 15. Here comes your footer Page 15 1. What do you know about crust movement/plate movement ? 2. There are 3 types of plate boundries. What are they and give the examples area ? Exercises
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