Landforms Of Erosion Ap
•Download as PPT, PDF•
4 likes•2,085 views
This document discusses coastal erosion processes. Hydraulic action involves air being forced into cracks in rock by waves, building enormous pressure that breaks off rock pieces when the water falls. This type of erosion is called hydraulic action. Coastal erosion forms headlands and bays as harder rock headlands project into the sea while softer bays erode back. Arches, stacks and stumps can form from erosion and collapse of the rock structures. Wave cut platforms are formed between high and low tides as waves erode the cliff but not the platform. Longshore drift involves waves carrying sediment up beaches at an angle due to wind direction and then carrying it down coast at 90 degrees due to gravity, moving material along the coast in
Report
Share
Report
Share
Recommended
Landforms Of Erosion Ap
This document discusses coastal erosion processes. Hydraulic action erodes rock when air is forced into cracks by waves, exerting pressure that pulls out rock when the water falls. This type of erosion is called hydraulic action. Coastal erosion forms headlands and bays as harder rock headlands project into the sea while soft rock in between erodes back to form bays. Over time, hydraulic action can form arches, stacks, and stumps in headlands as erosion undercuts the base of cliffs.
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.
The Work of the Sea
The document summarizes various coastal landforms and processes caused by erosion and deposition from ocean waves and currents. It describes how erosion wears away rock and sediments are transported and deposited in different areas, forming features like headlands, bays, cliffs, wave cut platforms, sea caves, arches, stacks, blowholes, beaches, sand dunes stabilized by marram grass, sand spits, bars, lagoons, tombolos, and defenses built to protect the coastline from erosion.
What Happens At A Destructive Plate Boundary Bv
1) At a destructive plate boundary, two plates collide with one another - one plate is oceanic crust and one is continental crust. The denser oceanic crust is pushed under the continental plate at a subduction zone.
2) Fold mountains, volcanoes, and earthquakes occur at destructive plate boundaries due to the subduction process. As the oceanic plate sinks into the mantle, friction causes earthquakes and the continental crust is uplifted to form mountains. Melted material from the sinking slab rises to the surface as volcanoes.
3) Examples of destructive plate boundaries include where the Nazca and South American plates are converging to form the Andes Mountains, with evidence of a subduction zone
Divergent boundary
Convection currents in the mantle cause tectonic plates to move away from each other at divergent boundaries, forming mid-ocean ridges between separating oceanic plates or rift valleys between continental plates. Divergent boundaries include the Mid-Atlantic Ridge and East African Rift, creating new crust and sometimes volcanic activity or lakes as the plates pull apart.
Landforms found-on-the-ocean-floor
The ocean floor contains several key landforms including the continental shelf, a shallow border along continents; the continental slope, a steep drop-off from the shelf; the mid-ocean ridge, an underwater volcanic mountain range dividing the ocean floor; and deep trenches and ocean basins on either side of the ridge.
L2 waves
Waves influence erosion through both constructive and destructive processes. Constructive waves gently build up beaches by spilling water up the shore, while destructive waves strongly erode beaches by crashing waves that remove material. Waves are formed by wind blowing across the surface of the ocean, transferring its energy to the water. As waves approach shore, they steepen and eventually break, providing energy to erode, transport, and deposit coastal materials.
Our changing earth
The document summarizes key concepts about landforms and geological processes. It describes how earthquakes are caused by movement of tectonic plates, and defines focus and epicenter. It explains weathering and erosion in forming landscapes. It also outlines various landforms created by rivers like meanders, ox-bow lakes, floodplains, levees and deltas. Additionally, it summarizes coastal landforms such as sea caves, sea arches, stacks, sea cliffs, beaches and features caused by glaciers, wind and desert processes like sand dunes and loess deposits.
Recommended
Landforms Of Erosion Ap
This document discusses coastal erosion processes. Hydraulic action erodes rock when air is forced into cracks by waves, exerting pressure that pulls out rock when the water falls. This type of erosion is called hydraulic action. Coastal erosion forms headlands and bays as harder rock headlands project into the sea while soft rock in between erodes back to form bays. Over time, hydraulic action can form arches, stacks, and stumps in headlands as erosion undercuts the base of cliffs.
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.
The Work of the Sea
The document summarizes various coastal landforms and processes caused by erosion and deposition from ocean waves and currents. It describes how erosion wears away rock and sediments are transported and deposited in different areas, forming features like headlands, bays, cliffs, wave cut platforms, sea caves, arches, stacks, blowholes, beaches, sand dunes stabilized by marram grass, sand spits, bars, lagoons, tombolos, and defenses built to protect the coastline from erosion.
What Happens At A Destructive Plate Boundary Bv
1) At a destructive plate boundary, two plates collide with one another - one plate is oceanic crust and one is continental crust. The denser oceanic crust is pushed under the continental plate at a subduction zone.
2) Fold mountains, volcanoes, and earthquakes occur at destructive plate boundaries due to the subduction process. As the oceanic plate sinks into the mantle, friction causes earthquakes and the continental crust is uplifted to form mountains. Melted material from the sinking slab rises to the surface as volcanoes.
3) Examples of destructive plate boundaries include where the Nazca and South American plates are converging to form the Andes Mountains, with evidence of a subduction zone
Divergent boundary
Convection currents in the mantle cause tectonic plates to move away from each other at divergent boundaries, forming mid-ocean ridges between separating oceanic plates or rift valleys between continental plates. Divergent boundaries include the Mid-Atlantic Ridge and East African Rift, creating new crust and sometimes volcanic activity or lakes as the plates pull apart.
Landforms found-on-the-ocean-floor
The ocean floor contains several key landforms including the continental shelf, a shallow border along continents; the continental slope, a steep drop-off from the shelf; the mid-ocean ridge, an underwater volcanic mountain range dividing the ocean floor; and deep trenches and ocean basins on either side of the ridge.
L2 waves
Waves influence erosion through both constructive and destructive processes. Constructive waves gently build up beaches by spilling water up the shore, while destructive waves strongly erode beaches by crashing waves that remove material. Waves are formed by wind blowing across the surface of the ocean, transferring its energy to the water. As waves approach shore, they steepen and eventually break, providing energy to erode, transport, and deposit coastal materials.
Our changing earth
The document summarizes key concepts about landforms and geological processes. It describes how earthquakes are caused by movement of tectonic plates, and defines focus and epicenter. It explains weathering and erosion in forming landscapes. It also outlines various landforms created by rivers like meanders, ox-bow lakes, floodplains, levees and deltas. Additionally, it summarizes coastal landforms such as sea caves, sea arches, stacks, sea cliffs, beaches and features caused by glaciers, wind and desert processes like sand dunes and loess deposits.
Coastal processes
The document discusses coastal processes and the coastal zone. It describes the coastal zone as the narrow area between land and sea that is constantly changing due to the actions of the sea, land, and air. Key coastal zone features include cliffs, beaches, sand dunes, salt marshes, ports, and seaside resorts. The three main coastal processes are erosion by waves, the transportation of eroded materials up and down the coast, and deposition that occurs when waves lose energy. Waves are a major force that shapes the coastline, with constructive waves building beaches up and destructive waves eroding them.
Landforms and Oceans Presentation
Natural processes like weathering, erosion, deposition, landslides, volcanic eruptions, earthquakes and floods shape Earth's landforms and oceans in both constructive and destructive ways. Key ocean landforms include the continental shelf, slope, mid-ocean ridge, rift zone, trench, and ocean basin. Waves, currents, tides and storms continually change coastal features such as beaches, barrier islands, estuaries and inlets through erosion and deposition.
Aqa A Coasts 1
Waves are caused by wind dragging on the surface of water, causing ripples that grow into waves as the wind continues. As waves reach shallow water, they slow due to friction and break as the water piles up in an irregular pattern. When waves reach the coast, the crest breaks as it moves faster than the wave base. The swash pushes the wave energy up the beach, then the backwash runs back down. Constructive waves build beaches by carrying material up the beach in low, breaking swashes that deposit material, while destructive waves remove beach material in high, frequent waves where the backwash transports material out to sea.
Coast
This document provides information on coastal geography topics including:
- The coast can be used for industry, transport, tourism, recreation, and nature conservation.
- Destructive waves are associated with storms and erosion while constructive waves are associated with deposition.
- Coastal weathering involves physical, chemical, and biological breakdown of rock, and erosion is the wearing away and transport of material.
- Waves erode coastlines through abrasion, hydraulic action, attrition, and solution. Headlands are eroded to form coastal landforms.
- Material is transported along beaches by swash and backwash. Beaches form through deposition by constructive waves.
- Spits, bars,
Constructive and destructive waves
This lesson aims to teach students about different types of waves and how they impact coastlines. By the end, students should be able to name two types of waves, describe their differences, and explain how each type changes coastlines. Constructive waves are low in height and length with few occurrences per minute, depositing sediment to build wide, flat beaches. Destructive waves are high, short, and frequent, eroding steep beaches by pulling sediment offshore.
Coasts Introduction
The document discusses coastal environments and the processes that impact coastlines. It describes coasts as zones where land and sea interact and are influenced by terrestrial, human, marine and atmospheric factors. Coasts experience rapid change from both short-term processes like storms and long-term processes like sea level rise. Over half the world's population lives near coasts, putting increasing pressure on coastal resources and ecosystems. Coastal management is important given human development and climate change impacts. The document outlines different coastal zone types and diagrams the factors affecting coasts.
The work of the sea a.kearon
The document summarizes various landforms created by coastal erosion and deposition processes. It describes how waves erode coastlines through hydraulic action, abrasion, solution, attrition, and compressed air. This erosion forms bays in soft rock and headlands in hard rock. Cliffs, sea caves, blowholes, beaches, sand dunes, spits, bars, and tombolos are also formed through the interacting processes of erosion, transportation by waves and currents, and deposition.
Destructive plate boundaries
This document summarizes the three types of plate boundaries:
1) When an oceanic plate meets a continental plate, the oceanic plate is subducted beneath the continental plate. This can form deep trenches and volcanic island arcs.
2) When two oceanic plates meet, one plate subducts beneath the other, forming ocean trenches and island arcs offshore.
3) When two continental plates meet, they are forced upwards to form fold mountains rather than subducting. This leads to earthquakes but no volcanic activity. Mountain ranges like the Himalayas and Andes are examples of this type of plate boundary.
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.
land forms formed by seawaves
This document discusses erosional and depositional landforms caused by sea waves. It describes how sea waves erode coastal rocks through cracks and breaking pieces, forming sea cliffs, caves, arches and stacks. Sea caves are formed by wave erosion carving holes in the coastline. Arches are formed when sea caves on either side join together. Stacks remain when arch roofs collapse. Deposition by waves temporarily deposits sand and soil to form beaches. In conclusion, sea waves cause significant morphological changes along the shoreline through both erosional and depositional processes.
GEOG101 Chapt03 lecture
This document provides an overview of earth materials, geologic time, movements of the continents, tectonic forces, and gradational and erosional processes that shape landforms and landform regions. It describes the three main types of rocks - igneous, sedimentary, and metamorphic - and how they are formed. It also explains plate tectonics theory and how the movement of tectonic plates results in diverse landforms and geological phenomena like earthquakes and volcanoes globally.
Coasts Lesson 1
Coasts undergo change due to three main coastal processes: erosion, transportation, and deposition. Waves are a major force in coastal change, as they erode and transport sediment. The size and power of waves depends on factors like wind strength and duration, and fetch - the distance over which the wind blows to generate the waves. Destructive waves in storms can cause significant erosion, while constructive waves in calm weather tend to deposit material and build up beaches.
Nouman Ijaz Divergent Boundary Powerpoint
The document discusses tectonic plates and divergent plate boundaries. It explains that tectonic plates are large, solid pieces of Earth's lithosphere or crust. When two plates move apart at a divergent boundary, new crust is formed by magma from the mantle welling up between the separating plates. There are two main types of divergent boundaries - oceanic-oceanic boundaries which form undersea mountain ridges, and continental-continental boundaries which form rift valleys as the continents move apart.
GEOGRAPHY IGCSE: COASTAL LANDFORMS
This document provides information on coastal landforms found in LEDC and MEDC countries. It describes both depositional landforms like beaches, spits, and tombolos, which are built up by material deposited by waves, and erosional landforms like cliffs and caves, which are shaped by erosion. It discusses processes like longshore drift that form features like spits, and provides examples of different coastal landforms like Chesil Beach in the UK and Spurn Head in England.
Divergent
- The document discusses plate tectonics topics including oceanic-oceanic divergence and continental-continental divergence.
- Oceanic-oceanic divergence involves two oceanic plates moving apart, causing magma to rise and form new sea floor through sea-floor spreading, creating a mid-ocean ridge.
- Continental-continental divergence can form rift valleys as the land between diverging continental plates sinks, such as the East African Rift Valley, and may eventually lead to the formation of new oceans.
Ocean shore zones
Waves, currents, tides, and storms shape the geological features of ocean shore zones. Beaches are formed from sand deposited by waves along shorelines. Longshore currents move sand along beaches from one area to another. Barrier islands block the mainland from wave effects and their shape changes as sand is deposited and moved by currents. Estuaries are where rivers meet the ocean and have a mixture of fresh and salt water, with sediments deposited by waves and sea life nourished by tidal flows. Inlets between barrier islands change shape due to tides, currents, and storms.
EXTERNAL CHANGES
The document outlines 5 agents that change landscapes over time: wind, rivers, sea, underground, and glaciers. It describes the processes of weathering, erosion, transport, and sedimentation caused by these agents, and how they shape specific landforms like deserts, cliffs, beaches, and underground caves. Rivers in particular change landscapes through high, middle, and low courses that involve different combinations of these geological processes.
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.
Constructive Plate Boundaries Conservative Boundaries Bv
Constructive plate boundaries create new crust as plates move apart, such as at the Mid-Atlantic Ridge where the Eurasian and North American plates are diverging. Conservative boundaries involve plates sliding past one another without creating or destroying crust, often causing earthquakes, like at the San Andreas Fault where the Pacific and North American plates slide in the same direction at different speeds.
Coastal erosion processes
This document discusses coastal studies and processes. It describes the different types of waves that impact coasts, including constructive waves that have weaker backwash and destructive waves that strongly erode coasts. The key coastal processes are erosion, transportation, and deposition. Erosional processes include corrasion, attrition, solution, and hydraulic action, which can be remembered with the acronym CASH. Factors influencing the rate of coastal erosion are the type of waves, the nature of coastal rocks, the gradient of the coast, and human activities.
Coastal geography waves, features of erosion and deposition, longshore drift
Waves cause coastal erosion and depositional features through processes like abrasion, hydraulic action, and corrosion. As waves approach shorelines, they can form erosional landforms such as headlands, bays, wave-cut notches, and platforms. Waves also transport sediment via processes like traction, saltation, and suspension, building depositional features along coastlines through longshore drift. This can result in beaches, spits, tombolos, bars, and barrier islands.
L5 headlands
This document provides information on various coastal landforms and erosion processes. It defines key terms like headlands, bays, fetch, corrasion, deposition, longshore drift, backwash, attrition, hydraulic action, and corrosion. It also matches these terms to their meanings. The document discusses how differing rock properties lead to different coastal landform shapes. It specifically examines how headlands, cliffs, and wave-cut platforms are formed through erosion processes acting on resistant and weak rocks over time.
More Related Content
What's hot
Coastal processes
The document discusses coastal processes and the coastal zone. It describes the coastal zone as the narrow area between land and sea that is constantly changing due to the actions of the sea, land, and air. Key coastal zone features include cliffs, beaches, sand dunes, salt marshes, ports, and seaside resorts. The three main coastal processes are erosion by waves, the transportation of eroded materials up and down the coast, and deposition that occurs when waves lose energy. Waves are a major force that shapes the coastline, with constructive waves building beaches up and destructive waves eroding them.
Landforms and Oceans Presentation
Natural processes like weathering, erosion, deposition, landslides, volcanic eruptions, earthquakes and floods shape Earth's landforms and oceans in both constructive and destructive ways. Key ocean landforms include the continental shelf, slope, mid-ocean ridge, rift zone, trench, and ocean basin. Waves, currents, tides and storms continually change coastal features such as beaches, barrier islands, estuaries and inlets through erosion and deposition.
Aqa A Coasts 1
Waves are caused by wind dragging on the surface of water, causing ripples that grow into waves as the wind continues. As waves reach shallow water, they slow due to friction and break as the water piles up in an irregular pattern. When waves reach the coast, the crest breaks as it moves faster than the wave base. The swash pushes the wave energy up the beach, then the backwash runs back down. Constructive waves build beaches by carrying material up the beach in low, breaking swashes that deposit material, while destructive waves remove beach material in high, frequent waves where the backwash transports material out to sea.
Coast
This document provides information on coastal geography topics including:
- The coast can be used for industry, transport, tourism, recreation, and nature conservation.
- Destructive waves are associated with storms and erosion while constructive waves are associated with deposition.
- Coastal weathering involves physical, chemical, and biological breakdown of rock, and erosion is the wearing away and transport of material.
- Waves erode coastlines through abrasion, hydraulic action, attrition, and solution. Headlands are eroded to form coastal landforms.
- Material is transported along beaches by swash and backwash. Beaches form through deposition by constructive waves.
- Spits, bars,
Constructive and destructive waves
This lesson aims to teach students about different types of waves and how they impact coastlines. By the end, students should be able to name two types of waves, describe their differences, and explain how each type changes coastlines. Constructive waves are low in height and length with few occurrences per minute, depositing sediment to build wide, flat beaches. Destructive waves are high, short, and frequent, eroding steep beaches by pulling sediment offshore.
Coasts Introduction
The document discusses coastal environments and the processes that impact coastlines. It describes coasts as zones where land and sea interact and are influenced by terrestrial, human, marine and atmospheric factors. Coasts experience rapid change from both short-term processes like storms and long-term processes like sea level rise. Over half the world's population lives near coasts, putting increasing pressure on coastal resources and ecosystems. Coastal management is important given human development and climate change impacts. The document outlines different coastal zone types and diagrams the factors affecting coasts.
The work of the sea a.kearon
The document summarizes various landforms created by coastal erosion and deposition processes. It describes how waves erode coastlines through hydraulic action, abrasion, solution, attrition, and compressed air. This erosion forms bays in soft rock and headlands in hard rock. Cliffs, sea caves, blowholes, beaches, sand dunes, spits, bars, and tombolos are also formed through the interacting processes of erosion, transportation by waves and currents, and deposition.
Destructive plate boundaries
This document summarizes the three types of plate boundaries:
1) When an oceanic plate meets a continental plate, the oceanic plate is subducted beneath the continental plate. This can form deep trenches and volcanic island arcs.
2) When two oceanic plates meet, one plate subducts beneath the other, forming ocean trenches and island arcs offshore.
3) When two continental plates meet, they are forced upwards to form fold mountains rather than subducting. This leads to earthquakes but no volcanic activity. Mountain ranges like the Himalayas and Andes are examples of this type of plate boundary.
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.
land forms formed by seawaves
This document discusses erosional and depositional landforms caused by sea waves. It describes how sea waves erode coastal rocks through cracks and breaking pieces, forming sea cliffs, caves, arches and stacks. Sea caves are formed by wave erosion carving holes in the coastline. Arches are formed when sea caves on either side join together. Stacks remain when arch roofs collapse. Deposition by waves temporarily deposits sand and soil to form beaches. In conclusion, sea waves cause significant morphological changes along the shoreline through both erosional and depositional processes.
GEOG101 Chapt03 lecture
This document provides an overview of earth materials, geologic time, movements of the continents, tectonic forces, and gradational and erosional processes that shape landforms and landform regions. It describes the three main types of rocks - igneous, sedimentary, and metamorphic - and how they are formed. It also explains plate tectonics theory and how the movement of tectonic plates results in diverse landforms and geological phenomena like earthquakes and volcanoes globally.
Coasts Lesson 1
Coasts undergo change due to three main coastal processes: erosion, transportation, and deposition. Waves are a major force in coastal change, as they erode and transport sediment. The size and power of waves depends on factors like wind strength and duration, and fetch - the distance over which the wind blows to generate the waves. Destructive waves in storms can cause significant erosion, while constructive waves in calm weather tend to deposit material and build up beaches.
Nouman Ijaz Divergent Boundary Powerpoint
The document discusses tectonic plates and divergent plate boundaries. It explains that tectonic plates are large, solid pieces of Earth's lithosphere or crust. When two plates move apart at a divergent boundary, new crust is formed by magma from the mantle welling up between the separating plates. There are two main types of divergent boundaries - oceanic-oceanic boundaries which form undersea mountain ridges, and continental-continental boundaries which form rift valleys as the continents move apart.
GEOGRAPHY IGCSE: COASTAL LANDFORMS
This document provides information on coastal landforms found in LEDC and MEDC countries. It describes both depositional landforms like beaches, spits, and tombolos, which are built up by material deposited by waves, and erosional landforms like cliffs and caves, which are shaped by erosion. It discusses processes like longshore drift that form features like spits, and provides examples of different coastal landforms like Chesil Beach in the UK and Spurn Head in England.
Divergent
- The document discusses plate tectonics topics including oceanic-oceanic divergence and continental-continental divergence.
- Oceanic-oceanic divergence involves two oceanic plates moving apart, causing magma to rise and form new sea floor through sea-floor spreading, creating a mid-ocean ridge.
- Continental-continental divergence can form rift valleys as the land between diverging continental plates sinks, such as the East African Rift Valley, and may eventually lead to the formation of new oceans.
Ocean shore zones
Waves, currents, tides, and storms shape the geological features of ocean shore zones. Beaches are formed from sand deposited by waves along shorelines. Longshore currents move sand along beaches from one area to another. Barrier islands block the mainland from wave effects and their shape changes as sand is deposited and moved by currents. Estuaries are where rivers meet the ocean and have a mixture of fresh and salt water, with sediments deposited by waves and sea life nourished by tidal flows. Inlets between barrier islands change shape due to tides, currents, and storms.
EXTERNAL CHANGES
The document outlines 5 agents that change landscapes over time: wind, rivers, sea, underground, and glaciers. It describes the processes of weathering, erosion, transport, and sedimentation caused by these agents, and how they shape specific landforms like deserts, cliffs, beaches, and underground caves. Rivers in particular change landscapes through high, middle, and low courses that involve different combinations of these geological processes.
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.
Constructive Plate Boundaries Conservative Boundaries Bv
Constructive plate boundaries create new crust as plates move apart, such as at the Mid-Atlantic Ridge where the Eurasian and North American plates are diverging. Conservative boundaries involve plates sliding past one another without creating or destroying crust, often causing earthquakes, like at the San Andreas Fault where the Pacific and North American plates slide in the same direction at different speeds.
Coastal erosion processes
This document discusses coastal studies and processes. It describes the different types of waves that impact coasts, including constructive waves that have weaker backwash and destructive waves that strongly erode coasts. The key coastal processes are erosion, transportation, and deposition. Erosional processes include corrasion, attrition, solution, and hydraulic action, which can be remembered with the acronym CASH. Factors influencing the rate of coastal erosion are the type of waves, the nature of coastal rocks, the gradient of the coast, and human activities.
What's hot (20)
Constructive Plate Boundaries Conservative Boundaries Bv
Constructive Plate Boundaries Conservative Boundaries Bv
Similar to Landforms Of Erosion Ap
Coastal geography waves, features of erosion and deposition, longshore drift
Waves cause coastal erosion and depositional features through processes like abrasion, hydraulic action, and corrosion. As waves approach shorelines, they can form erosional landforms such as headlands, bays, wave-cut notches, and platforms. Waves also transport sediment via processes like traction, saltation, and suspension, building depositional features along coastlines through longshore drift. This can result in beaches, spits, tombolos, bars, and barrier islands.
L5 headlands
This document provides information on various coastal landforms and erosion processes. It defines key terms like headlands, bays, fetch, corrasion, deposition, longshore drift, backwash, attrition, hydraulic action, and corrosion. It also matches these terms to their meanings. The document discusses how differing rock properties lead to different coastal landform shapes. It specifically examines how headlands, cliffs, and wave-cut platforms are formed through erosion processes acting on resistant and weak rocks over time.
Distinctive Coastal Erosional Landforms
The document describes different coastal landforms formed by erosion processes. It discusses how headlands and bays form along coastlines with variations in rock hardness. Headlands project out and are more exposed to wave erosion, while bays form in areas of softer rock. As cliffs erode, waves cut notches and undercut the base, eventually leading to cliff collapse and the formation of wave-cut platforms. Within resistant cliff rocks, erosion enlarges weaknesses like faults to form caves, which can eventually be cut through to form arches or isolate stacks from the headland.
COASTS ENM 142 Lecture 7.pptx
The document discusses coastal landforms and the processes involved in their formation. It covers both erosional and depositional coastal features. Erosional features like cliffs, arches and stacks are formed by processes like wave action, weathering and erosion concentrating on headlands. Depositional features such as beaches, spits and bars are produced by constructive waves depositing sediment transported by longshore drift. The key forces shaping the coast are waves, tides, currents and the underlying geology of the area.
L4 ap erosional landforms
This document discusses various coastal landforms formed by erosion processes. It describes attrition as the breaking down of material into smaller particles when carried by waves. Corrasion and hydraulic action involve material carried by waves wearing away coastlines through impacts or air pressure within cracks. Solution slowly dissolves rocks through chemical reactions with acid in seawater. Headlands project out and are more resistant to erosion, forming bays between them. Cliffs and wave-cut platforms are formed as waves erode the cliff base and notch it, eventually leaving a platform when the cliff collapses. Caves, arches, stacks and stumps form through the continued erosion of weaknesses in the cliff and eventual collapse of eroded sections.
Coastal processes this one
This document provides information about the GCSE Geography course for Mr. Rogers' class, including details on exam dates and percentages of the final mark for different topics. It discusses rivers and coasts, economic geography, settlement and population, and hazards. It provides resources for students, including Mr. Rogers' contact information and links to online materials. Homework is assigned to produce a factfile on a place eroded by the coast.
Lithosphere Coasts
The document discusses various coastal landforms created by wave erosion and deposition along shorelines. It describes how alternating bands of hard and soft rock lead to the formation of headlands and bays through differential erosion. As waves erode the soft rock faster than the hard rock, an irregular coastline develops. Further erosion can form caves, arches, stacks, and stumps. Coves are formed when a stream cuts through a cliff, widening through erosion. Wave-cut platforms are flat terraces exposed when cliffs retreat inland. Longshore drift can build up spits, narrow accumulations of sand and gravel stretching from the shore into the sea.
Ch 3 Our Changing Earth 2.pptx
This document discusses how the Earth's landscape is continuously changed by various forces. It describes how rivers erode landscapes to form landforms like waterfalls, meanders, ox-bow lakes, and deltas. Sea waves erode coastal areas to form sea caves, sea arches, and sea cliffs. Glaciers erode and deposit material as they move, leaving behind moraines and carving out lakes. Wind erosion forms structures like mushroom rocks and deposits materials to create sand dunes and loess. The document provides examples of different landforms shaped by these external, or exogenic, geological processes.
3 e coasts (1)
Coasts are shaped by the dynamic forces of the sea, air, and waves. Waves erode coastlines through hydraulic action, abrasion, attrition, and corrosion. Erosion carves out coastal landforms like cliffs, headlands, and bays. Waves also transport and deposit eroded material, building up beaches and forming depositional landforms such as spits, bars, and sand dunes. Managing coastal change involves either "hard engineering" using structures, or "soft engineering" techniques like beach nourishment and managed retreat that work with natural coastal processes.
Erosion
1. Waves erode coastlines through processes like undercutting cliffs and forming wave-cut platforms. Longshore drift transports sediment along the shoreline and can form extensions like spits and tombolos.
2. Tides are caused by gravitational pull from the sun and moon, producing two high and two low tides daily. Coastal landforms also include barrier islands, deltas, and coral reefs.
3. Wind erosion shapes desert landscapes through abrasion and deflation. Sediment is transported by surface creep and saltation, forming dune types like barchan and parabolic dunes oriented with the wind direction.
The coasts igcse
The coast is a narrow contact zone between land and sea that is constantly changing due to various land, air, and marine processes. Waves are a major force shaping the coastline, with characteristics like height, period, length, and steepness influencing their constructive or destructive power. Coastal landforms like beaches, sand dunes, spits, bars, cliffs, and caves form through the interacting processes of erosion, sediment transport, and deposition that waves and currents bring about.
Coastal land-form evoltion
Formation of different land-forms along the coast due to wave action and other processes are explained here
The sea
The sea constantly changes coastlines through erosion, transportation, and deposition of material. Waves erode the coastline through processes like hydraulic action and abrasion, forming landforms such as cliffs, bays, and sea caves. Material is transported along the shore by swash and backwash and through longshore drift. Deposition by the sea creates beaches, sand dunes, sand spits, and lagoons. People build structures like sea walls, place boulders, and construct groynes to protect coastlines from erosion while also utilizing coastlines for tourism, industry, and recreation.
Works Of The Sea And Development Of The Related Landforms For Presentation
The document discusses various topics related to oceans and coastal landforms including:
- Ocean currents are driven by wind and influence marine climates by transporting warm and cold water.
- Deep ocean circulation is governed by gravity and density differences in water temperature and salinity, circulating water very slowly over 500-2000 years.
- Tides are periodic changes in ocean elevation affected by the Earth's rotation and the moon and sun's gravitational pull.
- Waves are formed by wind across ocean surfaces, with larger waves forming in storms and tsunamis from undersea events.
- Coastal landforms like sea arches, stacks, and barrier islands are formed through erosion from wave action.
Coastal erosion processes
The document provides information about different types of coastal erosion and how they can be represented through "Kung Fu" gestures. It includes descriptions of four erosion processes - hydraulic action, abrasion, attrition, and corrosion. Students are asked to create gestures to symbolize each process. The document also contains sample exam questions about coastal erosion processes and features formed by erosion.
Marine Systems
The document summarizes coastal processes and features. It discusses how waves erode, transport, and deposit material, shaping coastlines. Coastal landforms like cliffs, headlands, bays, beaches, and sand dunes are formed through erosion or deposition. Coastal management considers both human uses of coasts and techniques to address physical processes like erosion.
Coastal Landforms
The document discusses various coastal landforms created by erosion and deposition processes along shorelines. It describes landforms such as headlands and bays, cliffs and wave-cut platforms, caves, arches, stacks, and stumps which are formed by coastal erosion. Beaches and spits are landforms created by coastal deposition, with beaches forming in sheltered areas between high and low tide lines, and spits forming as narrow ridges projecting from the coast due to longshore drift depositing materials.
AS GEOGRAPHY - ROCKS AND WEATHERING: ELEMENTARY PLATE TECTONICS
1. Plate tectonics theory states that the Earth's crust is made up of plates that move over the mantle due to convection currents. As plates move away from mid-ocean ridges, they cool and become denser.
2. At convergent plate boundaries, one plate subducts under the other into the mantle at deep ocean trenches. This causes volcanism and creates island arcs at the surface.
3. Mountain building occurs at plate boundaries, such as the Himalayas formed by the collision of the Eurasian and Indian plates, and the Andes formed at the boundary between the oceanic Nazca Plate and continental South American Plate. Folding and faulting create the mountains.
Coasts 3
The document provides an overview of coastal erosion and transportation processes. It explains the four main types of coastal erosion: hydraulic action, abrasion, attrition, and solution. It then describes how loose materials are transported along coastlines by processes like traction, saltation, and suspension. Longshore drift is identified as the process by which waves transport sand and pebbles parallel to the shoreline. Deposition occurs when constructive waves deposit more material on beaches than they remove.
L3.ap longshore drift and deposition
The document summarizes various coastal erosion processes that shape coastlines:
1) Attrition occurs as waves carry rocks that knock against each other, breaking them down into smaller pieces over time.
2) Abrasion involves the dissolving of limestone by carbonic acid in seawater and the expansion of salt crystals in the rock causing it to disintegrate.
3) Hydraulic action is the wearing away of cliffs by sand, shingle and boulders hurled against them powerfully by wave action.
Similar to Landforms Of Erosion Ap (20)
Coastal geography waves, features of erosion and deposition, longshore drift
Coastal geography waves, features of erosion and deposition, longshore drift
Works Of The Sea And Development Of The Related Landforms For Presentation
Works Of The Sea And Development Of The Related Landforms For Presentation
AS GEOGRAPHY - ROCKS AND WEATHERING: ELEMENTARY PLATE TECTONICS
AS GEOGRAPHY - ROCKS AND WEATHERING: ELEMENTARY PLATE TECTONICS
More from SHS Geog
L2 2015 location of bio and hotspots
Biodiversity hotspots are areas with high levels of endemic species that are under threat. They cover only 1.4% of the Earth's land but contain over 40% of plant species and 35% of animal species. Most hotspots are located in the tropics where optimal conditions exist for growth and diversity. While hotspots have helped protect threatened biodiversity, they leave many ecosystems uncovered and do not address threats facing areas outside their criteria.
L1 ap 2014 defining bio
The document provides information about Edexcel Geography Unit 3: Contested Planet. It discusses the six topics covered in the unit, including how they are linked and the suggested order to teach them. It also provides details about the exam structure, including the format and content of sections A and B. Additionally, it defines key terms related to biodiversity such as ecosystems, biomes, genetic diversity, species diversity, and ecosystem diversity. Finally, it discusses the importance of biodiversity and highlights biodiversity hotspots as areas of very high biodiversity values.
L3 k learn spaces 2014 value of ecosystems
This document discusses how to value ecosystems by examining the economic, cultural, and environmental value they provide. It provides examples of ecosystem services - the benefits ecosystems provide to people - which are broken into supporting, regulating, cultural, and provisioning services. These services have a large impact on human well-being. The document then analyzes two case studies: the Daintree Rainforest in Australia and coral reefs. For the Daintree, it highlights the ecosystem services of carbon sequestration, providing medicine, tourism, cultural value for indigenous people, and its history of logging. For coral reefs, it prompts examining their value through videos and a textbook section.
L6 ap 2014 dangers of mountain env
Mountain environments pose several dangers including cold temperatures, steep terrain, avalanches, and severe weather. Despite these risks, many people are drawn to mountains for recreation like skiing and tourism which provides economic benefits but also puts more lives at risk. When visiting mountains, it is important to be aware of potential hazards from the environment and weather and take proper precautions for protection and survival.
L4 avalanches ap
An avalanche is a rapid flow of snow down a steep mountain slope. Avalanches are typically triggered by heavy snowfall, strong winds, or human activity such as skiing or climbing. When triggered, an avalanche can move at speeds up to 200 km/h, destroying everything in its path. Avalanches pose serious dangers to those caught in their path who may be killed or injured by the force of the moving snow.
L1. introduction to mountain environments ap
This document provides information about mountain environments and includes several learning activities. It begins with an introduction to the key characteristics of mountain environments and includes a virtual field trip. Students are then assigned a mini research project on a particular mountain. The rest of the document outlines several challenge activities for students to complete, including identifying mountain ranges on a map, learning fun facts about mountains, watching a video to describe feelings, and reading an extract about being stranded on a mountain. The overall purpose is to broaden students' knowledge of mountain environments through various learning exercises.
Glacier and corrie formation ap
Glaciers form through the accumulation of snow in mountainous areas. When snow falls during winter and does not melt during cold spring and summer months, it compacts into dense ice over many years under its own weight. Additional layers of snow become compressed into ice, which causes the air to be squeezed out, turning the glacier a blue color. The large mass of ice then flows down the mountain under its own weight, eroding the landscape through two main processes - plucking and abrasion. Plucking involves rocks becoming frozen to the base of the glacier and breaking away as it moves. Abrasion occurs as rocks and debris carried on the glacier's bottom scrape along the valley floor, slowly excavating and shaping the land over
Mountain building
Fold mountains are formed over millions of years when two tectonic plates collide and push material upwards, creating mountain ranges. The largest fold mountains include the Himalayas, Alps, Andes, Rockies, and Urals. Fold mountains are formed through the upward and downward folding of crustal material. Once formed, mountains undergo weathering and erosion that slowly shape the landscape over time.
L2 growth of brighton ap
Brighton has a long history as a popular seaside resort town on the southern coast of England. It was first mentioned in the Doomsday Book in 1086 and saw growth as a fishing and port town in the 16th-17th centuries. In the 18th century, doctors began promoting the health benefits of sea bathing, attracting more visitors. Major growth occurred in the 19th century with the construction of the Brighton Pavilions by the Prince of Wales in 1787 and the arrival of the London to Brighton Railway in 1841, opening the town to day trippers. The development of tourism infrastructure like the two piers further increased visitor numbers. Today, tourism remains a vital part of Brighton's economy.
L4 multiculturism in brighton
Globalization has caused increased migration and a multicultural Britain. It refers to how people and companies are becoming more connected globally through improved transportation like airplanes and container ships. This has made it easier for people to move between countries for work or a better life. As a result, Britain has seen large numbers of migrants come from countries like India, Pakistan, Poland and Ireland, changing the cultural makeup of the country. This has resulted in both positive and negative effects of an increasingly multicultural society in Britain.
L3 rebranding 2014
This document discusses rebranding of places and provides examples. It defines rebranding as redeveloping and marketing a place to give it a new identity to attract new investors and visitors. Examples discussed include Miley Cyrus rebranding herself, and the recent rebranding of Kingston Market. Students are asked to consider why places like towns or seaside resorts may want to rebrand. The document also discusses the proposed rebranding of the West Pier area in Brighton and having students design a questionnaire to collect public opinions on the rebranding.
Food lesson 2 ap
- There are two main types of farming: arable farming, which involves growing crops, and pastoral farming, which involves rearing animals. Some farms practice mixed farming with both crops and livestock.
- Arable farming is more common in southeast England where the land is flat, fertile, and has a warm climate and good transportation. Pastoral farming is found more in southwest England where the climate is warm and wet, even if the land is hilly.
- Organic farming avoids artificial fertilizers and pesticides and uses crop rotation to maintain soil fertility.
Diversification
Farm diversification is when farmers grow multiple crops and agricultural products on their land rather than specializing in one main crop. Traditionally, farms focused on a single product like dairy or livestock but now many farms are diversifying their offerings in response to changing market prices. Diversification allows farms to continue making money by providing a variety of agricultural goods and experiences to attract visitors.
L3 food miles
Food miles refer to the distance food travels from field to plate. Longer food miles contribute significantly to carbon dioxide emissions that cause climate change. The document discusses how most fruit and vegetables in the UK are now imported, having doubled since the 1990s, and imports are predicted to continue rising. It identifies several causes for this increase in food imports and miles, including lower costs, consumer demand for out-of-season foods, some foods not being able to be grown in the UK, supermarket desires for higher profits, and improved transportation technology. Potential positive and negative impacts of increased food miles are also mentioned.
Year 9 rf revision 2015
To revise key topics in geography including physical landscapes, glaciation, population, development, and tourism. The document provides revision materials such as diagrams, videos, exercises, and practice questions to help students review these concepts in preparation for an assessment. Interactive activities include matching processes of glaciation to their order, identifying features in photographs, and playing geography taboo to review terms related to development. The goal is to strengthen students' understanding of these interrelated topics through multi-modal learning and self-testing activities.
L6 tsunami ap
This document provides information about tsunamis, including what causes them, how they occur, and details about the devastating 2004 Indian Ocean tsunami. It aims to teach students about tsunamis through defining key terms, having students watch explanatory videos, modeling a hypothetical tsunami using play dough to demonstrate the wave's destructive power, and role playing a television news script about the 2004 event.
L7 hazard research ap
This document discusses natural hazards and provides information and assignments about them. It defines a natural hazard as an extreme weather event that occurs naturally. Some examples of natural hazards mentioned are tornados, flooding, avalanches, earthquakes, and hurricanes. Students are assigned a project to research a natural hazard of their choice, with success criteria including describing what causes it, its effects on people, how humans respond to it, where it is found, and including an example, maps, photos and diagrams in their project.
Revision presentation 2015pptx blog
This document provides a summary of content for a Year 8 geography exam revision. It includes the following key points:
- Global issues section covers causes and effects of global warming, resource extraction in Congo, food and water access as global issues.
- Europe section covers identity, migration push/pull factors, and a quiz on the content.
- Plate tectonics section explains how the earth's crust is divided and how plates move, with examples of constructive, destructive, and conservative plate boundaries. It also discusses tsunamis and a case study.
- Hazards section provides guidance on a research project about a natural hazard, its causes, effects, responses, locations, and an example.
L5 planning questions
The document discusses anagrams and their corresponding words, including "assess", "discuss", "causes", "evaluate", and "consequences". It then provides potential essay questions about the causes and patterns of food insecurity around the world, asking the reader to discuss whether food insecurity has one primary cause or results from various local and regional factors. A model methodology and framework are mentioned but not described.
L6 planning questions
This document provides guidance on answering questions about data stimuli effectively:
- It warns students to avoid mixing up causes and consequences in their answers.
- It advises brushing up interpretation skills like considering all parts of maps, graphs, data tables and diagrams instead of just one area.
- It explains what makes a good data stimulus answer - correctly interpreting the question, focusing on the specific task like impacts rather than just describing changes, and using evidence from the stimulus instead of just the stimulus.
- It also provides examples of grouping information in the stimulus to more easily see trends and patterns, as well as using examples to add depth instead than just the stimulus.
More from SHS Geog (20)
Recently uploaded
A Deep Dive into ScyllaDB's Architecture
This talk will cover ScyllaDB Architecture from the cluster-level view and zoom in on data distribution and internal node architecture. In the process, we will learn the secret sauce used to get ScyllaDB's high availability and superior performance. We will also touch on the upcoming changes to ScyllaDB architecture, moving to strongly consistent metadata and tablets.
Essentials of Automations: Exploring Attributes & Automation Parameters
Building automations in FME Flow can save time, money, and help businesses scale by eliminating data silos and providing data to stakeholders in real-time. One essential component to orchestrating complex automations is the use of attributes & automation parameters (both formerly known as “keys”). In fact, it’s unlikely you’ll ever build an Automation without using these components, but what exactly are they?
Attributes & automation parameters enable the automation author to pass data values from one automation component to the next. During this webinar, our FME Flow Specialists will cover leveraging the three types of these output attributes & parameters in FME Flow: Event, Custom, and Automation. As a bonus, they’ll also be making use of the Split-Merge Block functionality.
You’ll leave this webinar with a better understanding of how to maximize the potential of automations by making use of attributes & automation parameters, with the ultimate goal of setting your enterprise integration workflows up on autopilot.
How to Interpret Trends in the Kalyan Rajdhani Mix Chart.pdf
A Mix Chart displays historical data of numbers in a graphical or tabular form. The Kalyan Rajdhani Mix Chart specifically shows the results of a sequence of numbers over different periods.
Crafting Excellence: A Comprehensive Guide to iOS Mobile App Development Serv...
Crafting Excellence: A Comprehensive Guide to iOS Mobile App Development Serv...Pitangent Analytics & Technology Solutions Pvt. Ltd
Discover top-tier mobile app development services, offering innovative solutions for iOS and Android. Enhance your business with custom, user-friendly mobile applications."Choosing proper type of scaling", Olena Syrota
Imagine an IoT processing system that is already quite mature and production-ready and for which client coverage is growing and scaling and performance aspects are life and death questions. The system has Redis, MongoDB, and stream processing based on ksqldb. In this talk, firstly, we will analyze scaling approaches and then select the proper ones for our system.
Must Know Postgres Extension for DBA and Developer during Migration
Mydbops Opensource Database Meetup 16
Topic: Must-Know PostgreSQL Extensions for Developers and DBAs During Migration
Speaker: Deepak Mahto, Founder of DataCloudGaze Consulting
Date & Time: 8th June | 10 AM - 1 PM IST
Venue: Bangalore International Centre, Bangalore
Abstract: Discover how PostgreSQL extensions can be your secret weapon! This talk explores how key extensions enhance database capabilities and streamline the migration process for users moving from other relational databases like Oracle.
Key Takeaways:
* Learn about crucial extensions like oracle_fdw, pgtt, and pg_audit that ease migration complexities.
* Gain valuable strategies for implementing these extensions in PostgreSQL to achieve license freedom.
* Discover how these key extensions can empower both developers and DBAs during the migration process.
* Don't miss this chance to gain practical knowledge from an industry expert and stay updated on the latest open-source database trends.
Mydbops Managed Services specializes in taking the pain out of database management while optimizing performance. Since 2015, we have been providing top-notch support and assistance for the top three open-source databases: MySQL, MongoDB, and PostgreSQL.
Our team offers a wide range of services, including assistance, support, consulting, 24/7 operations, and expertise in all relevant technologies. We help organizations improve their database's performance, scalability, efficiency, and availability.
Contact us: info@mydbops.com
Visit: https://www.mydbops.com/
Follow us on LinkedIn: https://in.linkedin.com/company/mydbops
For more details and updates, please follow up the below links.
Meetup Page : https://www.meetup.com/mydbops-databa...
Twitter: https://twitter.com/mydbopsofficial
Blogs: https://www.mydbops.com/blog/
Facebook(Meta): https://www.facebook.com/mydbops/
zkStudyClub - LatticeFold: A Lattice-based Folding Scheme and its Application...
Folding is a recent technique for building efficient recursive SNARKs. Several elegant folding protocols have been proposed, such as Nova, Supernova, Hypernova, Protostar, and others. However, all of them rely on an additively homomorphic commitment scheme based on discrete log, and are therefore not post-quantum secure. In this work we present LatticeFold, the first lattice-based folding protocol based on the Module SIS problem. This folding protocol naturally leads to an efficient recursive lattice-based SNARK and an efficient PCD scheme. LatticeFold supports folding low-degree relations, such as R1CS, as well as high-degree relations, such as CCS. The key challenge is to construct a secure folding protocol that works with the Ajtai commitment scheme. The difficulty, is ensuring that extracted witnesses are low norm through many rounds of folding. We present a novel technique using the sumcheck protocol to ensure that extracted witnesses are always low norm no matter how many rounds of folding are used. Our evaluation of the final proof system suggests that it is as performant as Hypernova, while providing post-quantum security.
Paper Link: https://eprint.iacr.org/2024/257
Session 1 - Intro to Robotic Process Automation.pdf
👉 Check out our full 'Africa Series - Automation Student Developers (EN)' page to register for the full program:
https://bit.ly/Automation_Student_Kickstart
In this session, we shall introduce you to the world of automation, the UiPath Platform, and guide you on how to install and setup UiPath Studio on your Windows PC.
📕 Detailed agenda:
What is RPA? Benefits of RPA?
RPA Applications
The UiPath End-to-End Automation Platform
UiPath Studio CE Installation and Setup
💻 Extra training through UiPath Academy:
Introduction to Automation
UiPath Business Automation Platform
Explore automation development with UiPath Studio
👉 Register here for our upcoming Session 2 on June 20: Introduction to UiPath Studio Fundamentals: https://community.uipath.com/events/details/uipath-lagos-presents-session-2-introduction-to-uipath-studio-fundamentals/
Connector Corner: Seamlessly power UiPath Apps, GenAI with prebuilt connectors
Join us to learn how UiPath Apps can directly and easily interact with prebuilt connectors via Integration Service--including Salesforce, ServiceNow, Open GenAI, and more.
The best part is you can achieve this without building a custom workflow! Say goodbye to the hassle of using separate automations to call APIs. By seamlessly integrating within App Studio, you can now easily streamline your workflow, while gaining direct access to our Connector Catalog of popular applications.
We’ll discuss and demo the benefits of UiPath Apps and connectors including:
Creating a compelling user experience for any software, without the limitations of APIs.
Accelerating the app creation process, saving time and effort
Enjoying high-performance CRUD (create, read, update, delete) operations, for
seamless data management.
Speakers:
Russell Alfeche, Technology Leader, RPA at qBotic and UiPath MVP
Charlie Greenberg, host
Principle of conventional tomography-Bibash Shahi ppt..pptx
before the computed tomography, it had been widely used.
What is an RPA CoE? Session 2 – CoE Roles
In this session, we will review the players involved in the CoE and how each role impacts opportunities.
Topics covered:
• What roles are essential?
• What place in the automation journey does each role play?
Speaker:
Chris Bolin, Senior Intelligent Automation Architect Anika Systems
GraphRAG for LifeSciences Hands-On with the Clinical Knowledge Graph
Tomaz Bratanic
Graph ML and GenAI Expert - Neo4j
High performance Serverless Java on AWS- GoTo Amsterdam 2024
Java is for many years one of the most popular programming languages, but it used to have hard times in the Serverless community. Java is known for its high cold start times and high memory footprint, comparing to other programming languages like Node.js and Python. In this talk I'll look at the general best practices and techniques we can use to decrease memory consumption, cold start times for Java Serverless development on AWS including GraalVM (Native Image) and AWS own offering SnapStart based on Firecracker microVM snapshot and restore and CRaC (Coordinated Restore at Checkpoint) runtime hooks. I'll also provide a lot of benchmarking on Lambda functions trying out various deployment package sizes, Lambda memory settings, Java compilation options and HTTP (a)synchronous clients and measure their impact on cold and warm start times.
inQuba Webinar Mastering Customer Journey Management with Dr Graham Hill
HERE IS YOUR WEBINAR CONTENT! 'Mastering Customer Journey Management with Dr. Graham Hill'. We hope you find the webinar recording both insightful and enjoyable.
In this webinar, we explored essential aspects of Customer Journey Management and personalization. Here’s a summary of the key insights and topics discussed:
Key Takeaways:
Understanding the Customer Journey: Dr. Hill emphasized the importance of mapping and understanding the complete customer journey to identify touchpoints and opportunities for improvement.
Personalization Strategies: We discussed how to leverage data and insights to create personalized experiences that resonate with customers.
Technology Integration: Insights were shared on how inQuba’s advanced technology can streamline customer interactions and drive operational efficiency.
Mutation Testing for Task-Oriented Chatbots
Conversational agents, or chatbots, are increasingly used to access all sorts of services using natural language. While open-domain chatbots - like ChatGPT - can converse on any topic, task-oriented chatbots - the focus of this paper - are designed for specific tasks, like booking a flight, obtaining customer support, or setting an appointment. Like any other software, task-oriented chatbots need to be properly tested, usually by defining and executing test scenarios (i.e., sequences of user-chatbot interactions). However, there is currently a lack of methods to quantify the completeness and strength of such test scenarios, which can lead to low-quality tests, and hence to buggy chatbots.
To fill this gap, we propose adapting mutation testing (MuT) for task-oriented chatbots. To this end, we introduce a set of mutation operators that emulate faults in chatbot designs, an architecture that enables MuT on chatbots built using heterogeneous technologies, and a practical realisation as an Eclipse plugin. Moreover, we evaluate the applicability, effectiveness and efficiency of our approach on open-source chatbots, with promising results.
QA or the Highway - Component Testing: Bridging the gap between frontend appl...
These are the slides for the presentation, "Component Testing: Bridging the gap between frontend applications" that was presented at QA or the Highway 2024 in Columbus, OH by Zachary Hamm.
Apps Break Data
How information systems are built or acquired puts information, which is what they should be about, in a secondary place. Our language adapted accordingly, and we no longer talk about information systems but applications. Applications evolved in a way to break data into diverse fragments, tightly coupled with applications and expensive to integrate. The result is technical debt, which is re-paid by taking even bigger "loans", resulting in an ever-increasing technical debt. Software engineering and procurement practices work in sync with market forces to maintain this trend. This talk demonstrates how natural this situation is. The question is: can something be done to reverse the trend?
[OReilly Superstream] Occupy the Space: A grassroots guide to engineering (an...
The typical problem in product engineering is not bad strategy, so much as “no strategy”. This leads to confusion, lack of motivation, and incoherent action. The next time you look for a strategy and find an empty space, instead of waiting for it to be filled, I will show you how to fill it in yourself. If you’re wrong, it forces a correction. If you’re right, it helps create focus. I’ll share how I’ve approached this in the past, both what works and lessons for what didn’t work so well.
JavaLand 2024: Application Development Green Masterplan
My presentation slides I used at JavaLand 2024
Recently uploaded (20)
Essentials of Automations: Exploring Attributes & Automation Parameters
Essentials of Automations: Exploring Attributes & Automation Parameters
How to Interpret Trends in the Kalyan Rajdhani Mix Chart.pdf
How to Interpret Trends in the Kalyan Rajdhani Mix Chart.pdf
Crafting Excellence: A Comprehensive Guide to iOS Mobile App Development Serv...
Crafting Excellence: A Comprehensive Guide to iOS Mobile App Development Serv...
Must Know Postgres Extension for DBA and Developer during Migration
Must Know Postgres Extension for DBA and Developer during Migration
zkStudyClub - LatticeFold: A Lattice-based Folding Scheme and its Application...
zkStudyClub - LatticeFold: A Lattice-based Folding Scheme and its Application...
Session 1 - Intro to Robotic Process Automation.pdf
Session 1 - Intro to Robotic Process Automation.pdf
Connector Corner: Seamlessly power UiPath Apps, GenAI with prebuilt connectors
Connector Corner: Seamlessly power UiPath Apps, GenAI with prebuilt connectors
Principle of conventional tomography-Bibash Shahi ppt..pptx
Principle of conventional tomography-Bibash Shahi ppt..pptx
GraphRAG for LifeSciences Hands-On with the Clinical Knowledge Graph
GraphRAG for LifeSciences Hands-On with the Clinical Knowledge Graph
High performance Serverless Java on AWS- GoTo Amsterdam 2024
High performance Serverless Java on AWS- GoTo Amsterdam 2024
inQuba Webinar Mastering Customer Journey Management with Dr Graham Hill
inQuba Webinar Mastering Customer Journey Management with Dr Graham Hill
QA or the Highway - Component Testing: Bridging the gap between frontend appl...
QA or the Highway - Component Testing: Bridging the gap between frontend appl...
[OReilly Superstream] Occupy the Space: A grassroots guide to engineering (an...
[OReilly Superstream] Occupy the Space: A grassroots guide to engineering (an...
JavaLand 2024: Application Development Green Masterplan
JavaLand 2024: Application Development Green Masterplan
Landforms Of Erosion Ap
- 1. The force of the waves pushes air into cracks in the rock The compressed air exerts enormous pressure at the tip of the crack. As the water falls back the air pressure is released and rock is pulled out from the crack further enlarging the hole. What is this type of erosion called?
- 2. What features does coastal erosion cause?
- 3. 1) HEADLANDS AND BAYS
- 5. Headlands and bays Why have the bays been eroded more than the headlands? Why are headlands now more vulnerable to erosion than bays? How do headlands protect bays from erosion?
- 10. Arches, stacks and stumps
- 11. Development of a Headland 1
- 12. Development of a Headland 2
- 13. Development of a Headland 3
- 22. Cliffs and wave cut platforms
- 23. Wave cut platform formed between the high and low tides as the waves only attack the cliff and pass over the platform
- 24. TRANSPORTATION