REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DEPOSITIONAL LANDFORMS
•Download as PPT, PDF•
3 likes•329 views
The document contains 4 questions and answers about hydrology and depositional landforms. It discusses how depositional landforms like levees are predominantly found in the lower course of rivers where the velocity decreases, encouraging sediment deposition. It explains that levees are formed through repeated flooding that causes material to build up on river banks. Finally, it lists deltas, alluvial fans, floodplains, oxbow lakes, and point bars as other examples of depositional landforms.
Report
Share
Report
Share
Recommended
GEOGRAPHY IGCSE: DESERT CLIMATE
GEOGRAPHY IGCSE: DESERT CLIMATE. It contains: desert climate and vegetation. Case study: Las Vegas and the Mojave Desert.
GEOGRAPHY IGCSE: WEATHER MEASUREMENTS.
GEOGRAPHY IGCSE: WEATHER MEASUREMENTS. It contains: difference between weather and climate, measuring the weather, what do we measure, temperature, precipitation, wind direction, Beaufort scale, cloud cover, air pressure, glossary.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - CHANNEL EFFICIENCY
Channel efficiency is measured by calculating the hydraulic radius of the channel cross-section, which is the cross-sectional area divided by the wetted perimeter. A higher hydraulic radius results in a more efficient channel that can transfer water downstream at a higher velocity. Some channel shapes are more efficient because they have a higher proportion of water not in contact with bed and bank materials, experiencing less frictional effects. Channel efficiency normally increases downstream as the channel deepens and widens, resulting in less friction from smoothed bed and bank materials despite additional water inputs.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - HJULSTROM CURVE
The Hjulstrom curve shows the relationship between flow velocity and sediment transport, with larger particles being deposited first as velocity decreases due to losing the energy needed to transport heavier sediment, while higher velocities are required to both erode and transport larger particles due to their weight and the cohesion of smaller particles.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - BRAIDED CHANNEL
Braided channels form in areas with large amounts of sediment and highly variable water flow. They consist of multiple interweaving channels separated by small islands called eyots. Eyots typically have a steep upstream end of coarse material that gradually slopes downstream into finer sediments. Braided channels are common in environments recently impacted by glaciers where weathering produces sediment and melting causes discharge fluctuations.
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZON
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZON. It contains: tropical rainforests, average rainfall in Brazil, rainforest ecosystems, disadvantages of human intervention, rainforest water cycle, rainforest nutrient cycle, rainforest soils, vegetation layers, fan palms, buttress roots, lianas, strangler figs, case study, humans and the Amazon.
Farming as a system igcse
Farming can be viewed as a system with inputs, processes, outputs, and feedback. Physical inputs include water, land, and raw materials while human inputs are money, labor, and skills. Processes transform inputs into outputs, which can be positive like crops and meat or negative like waste. Feedback puts money and knowledge back into the system. There are different types of farming like arable, pastoral, and mixed, which can be commercial, subsistence, or plantations. Sustainable agriculture maximizes yields through techniques like crop rotation, irrigation, and limited chemicals. The Green Revolution increased food production but was expensive, water intensive, and relied heavily on chemicals, negatively impacting the environment and farmers.
CAMBRIDGE GEOGRAPHY A2 REVISION - ENVIRONMENTAL MANAGEMENT: ENVIRONMENTAL DEG...
The document discusses several key issues related to environmental degradation and pollution:
1. Pollution and environmental degradation come in many forms and negatively impact land, air, water and human health.
2. The largest polluters are often large-scale industrial operations that tend to cluster together.
3. Exposure to pollution can have varying effects from minor to severe, and sustained pollution usually impacts more people long-term than incidental pollution.
4. Access to clean water is vital for development but water scarcity impacts many people and threatens food supplies, economic growth, and international conflicts.
Recommended
GEOGRAPHY IGCSE: DESERT CLIMATE
GEOGRAPHY IGCSE: DESERT CLIMATE. It contains: desert climate and vegetation. Case study: Las Vegas and the Mojave Desert.
GEOGRAPHY IGCSE: WEATHER MEASUREMENTS.
GEOGRAPHY IGCSE: WEATHER MEASUREMENTS. It contains: difference between weather and climate, measuring the weather, what do we measure, temperature, precipitation, wind direction, Beaufort scale, cloud cover, air pressure, glossary.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - CHANNEL EFFICIENCY
Channel efficiency is measured by calculating the hydraulic radius of the channel cross-section, which is the cross-sectional area divided by the wetted perimeter. A higher hydraulic radius results in a more efficient channel that can transfer water downstream at a higher velocity. Some channel shapes are more efficient because they have a higher proportion of water not in contact with bed and bank materials, experiencing less frictional effects. Channel efficiency normally increases downstream as the channel deepens and widens, resulting in less friction from smoothed bed and bank materials despite additional water inputs.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - HJULSTROM CURVE
The Hjulstrom curve shows the relationship between flow velocity and sediment transport, with larger particles being deposited first as velocity decreases due to losing the energy needed to transport heavier sediment, while higher velocities are required to both erode and transport larger particles due to their weight and the cohesion of smaller particles.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - BRAIDED CHANNEL
Braided channels form in areas with large amounts of sediment and highly variable water flow. They consist of multiple interweaving channels separated by small islands called eyots. Eyots typically have a steep upstream end of coarse material that gradually slopes downstream into finer sediments. Braided channels are common in environments recently impacted by glaciers where weathering produces sediment and melting causes discharge fluctuations.
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZON
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZON. It contains: tropical rainforests, average rainfall in Brazil, rainforest ecosystems, disadvantages of human intervention, rainforest water cycle, rainforest nutrient cycle, rainforest soils, vegetation layers, fan palms, buttress roots, lianas, strangler figs, case study, humans and the Amazon.
Farming as a system igcse
Farming can be viewed as a system with inputs, processes, outputs, and feedback. Physical inputs include water, land, and raw materials while human inputs are money, labor, and skills. Processes transform inputs into outputs, which can be positive like crops and meat or negative like waste. Feedback puts money and knowledge back into the system. There are different types of farming like arable, pastoral, and mixed, which can be commercial, subsistence, or plantations. Sustainable agriculture maximizes yields through techniques like crop rotation, irrigation, and limited chemicals. The Green Revolution increased food production but was expensive, water intensive, and relied heavily on chemicals, negatively impacting the environment and farmers.
CAMBRIDGE GEOGRAPHY A2 REVISION - ENVIRONMENTAL MANAGEMENT: ENVIRONMENTAL DEG...
The document discusses several key issues related to environmental degradation and pollution:
1. Pollution and environmental degradation come in many forms and negatively impact land, air, water and human health.
2. The largest polluters are often large-scale industrial operations that tend to cluster together.
3. Exposure to pollution can have varying effects from minor to severe, and sustained pollution usually impacts more people long-term than incidental pollution.
4. Access to clean water is vital for development but water scarcity impacts many people and threatens food supplies, economic growth, and international conflicts.
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: MEXICAN MIGRATION TO USA
This case study examines migration from Mexico to the US over the past 40 years. It identifies key push and pull factors, including high population growth and economic crises in Mexico, and demand for low-skilled labor in the US. Mexican migrants have concentrated in border states like California and Texas, working mainly in agriculture, construction, and services. While migration rates have declined since the late 1990s, over 12 million Mexican-born individuals lived in the US by 2006. The document also discusses the impacts on both Mexico and the US, such as remittances sent to Mexico and debates over cultural and economic effects in the US.
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY; 1.1. DRAINAGE B...
Introductory presentation of the drainage basin systems in the first chapter of Hydrology and Fluvial Geomorphology, suitable for AS students, consisting in the following: the global hydrological cycle, store, flows, the drainage systems, precipitation, evapotranspiration, interception, infiltration, percolation, drainage patterns, the water balance.
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY: 1.3 RIVER CHANN...
Subchapter 3 in the first chapter of Hydrology and Fluvial Geomorphology, suitable for AS students, consisting in the following: river processes, velocity, flows and Hjulstrom Curve.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.1 LOCAL ENERGY BU...
A comprehensive presentation of subchapter 2.1 Local Energy Budgets, from the second chapter of Physical Geography, AS Cambridge, Atmosphere and Weather.
GEOGRAPHY IGCSE: ALTERNATIVE PAPER 4 - INVESTIGATING
GEOGRAPHY IGCSE: ALTERNATIVE PAPER 4 - INVESTIGATING. It contains: formulating aims and hypotheses, enquiry skills to collect data, questionnaires, observation, counts, measurements, river measurement and beach studies, data presentation techniques, analysis, formation of conclusions.
AS GEOGRAPHY - ROCKS AND WEATHERING: WEATHERING AND ROCKS
Physical weathering breaks rocks into smaller pieces through processes like heating and cooling or wetting and drying. Chemical weathering alters the mineral composition of rocks through reactions with water and acids. Limestone landscapes feature karst topography with features like caves, sinkholes, and limestone pavements formed by the dissolution of calcium carbonate in the rocks. Granite weathers through freeze-thaw action and hydrolysis, forming tors and soil. The rate and type of weathering depends on climate, rock type, relief, vegetation and other factors.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DRAINAGE BASIN
A drainage basin is defined as the area of land drained by a river and its tributaries. Static factors that influence water movement through a basin and do not change over time include rock type, relief, soil type, shape and size of the basin, and drainage density. Dynamic factors that influence water movement through a basin and do vary over time include climate, vegetation, human activities, and previous conditions. All of the factors mentioned influence the amount of water stored in the basin and the rate at which water is transferred between stores.
GEOGRAPHY IGCSE: TOURISM - TRENDS
GEOGRAPHY IGCSE: TOURISM - TRENDS. It contains: trends in tourism, the growth of tourism, trends, infrastructure, reasons behind the trends in tourism.
AS GEOGRAPHY - ATMOSPHERE AND WEATHER - WEATHER PHENOMENA
Atmospheric stability refers to air that does not rise, which can lead to fog, mist or frost formation. Instability occurs when air rises, forming clouds and rain. Clouds are classified by form, height, and whether convection or fronts caused them. Convectional rainfall happens when warm land heats the air above, causing it to rise and condense. Frontal rainfall occurs at boundaries of warm and cold air masses. Orographic rainfall results when air is forced to rise over mountain barriers, cooling and condensing. Hail forms through a process of freezing and melting within cumulonimbus clouds. Dew and radiation fog form on clear nights through surface cooling and condensation. Advection fog
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: ABERFAN MUDFLOW
(1) The document examines the 1966 mudflow disaster in Aberfan, Wales that was caused by the mismanagement of coal waste from nearby mines. (2) Over 100,000 cubic meters of saturated coal waste and debris engulfed parts of the village after heavy rainfall, including a local junior school where 116 children and 5 teachers were killed. (3) An official inquiry found the National Coal Board extremely negligent for irresponsibly dumping large amounts of coal waste on unstable hillsides near a populated area.
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRIC...
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRICULTURAL SYSTEMS AND FOOD PRODUCTION. It contains: ley terms and definitions, topic summary, additional work and suggested websites.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...
This document defines key terms related to weather processes and phenomena. It discusses topics like adiabatic lapse rates, air masses, altitude, clouds, condensation, humidity, instability, precipitation and more. Weather results from changes in atmospheric conditions, such as temperature and moisture levels, which can cause air masses to rise or fall. Various types of precipitation form through different processes, like convectional rainfall from rising warm air or orographic rainfall on the windward sides of mountains. Fog occurs when air is cooled to its dew point through advection or radiation.
Geographical enquiry - Alternative to course work- paper 4 IGCSE
Geographical enquiry - CBD, Rivers and coasts, weather, tourism
IGCSE 2 - Alternative to course work
CAMBRIDGE GEOGRAPHY A2 REVISION - COASTAL ENVIRONMENTS: 8.1 WAVES MARINE AND ...
A2 Geography Revision for Coastal Environments, subchapter 8.1 Waves Marine and Subaerial Processes. It is suitable for Year 13 Geography, Cambridge Examination in November 2016. It contains: key terms and definitions, a topic summary, sketches and descriptions, additional work (6 questions for testing your knowledge) and some suggested websites.
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.1 DR...
A presentation of the first subchapter (Drainage Basin Systems) from the first chapter (Hydrology and Fluvial Geomorphology) of Revision for Geography AS Cambridge exam.
GEOGRAPHY IGCSE: INDUSTRY
The document discusses the four sectors of the economy: primary, secondary, tertiary, and quaternary. The primary sector involves agriculture and extraction of natural resources. The secondary sector processes raw materials into manufactured goods. The tertiary sector provides services. The quaternary sector offers information services. Employment structures have changed over time and differ between countries, with developed nations having more employment in the service sectors than agriculture and industry. Factors like resources, infrastructure, labor, and incentives influence where industries locate.
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM TECTO...
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM TECTONIC PROCESSES. It contains: earthquakes, volcanoes, tsunamis.
CAMBRIDGE GEOGRAPHY AS EXTRA REVISION - EXAM STYLE QUESTIONS 1 - HYDROLOGY AN...
The document contains exam style questions on hydrology and fluvial geomorphology. Section A asks students to define the hydrological cycle, draw a diagram showing its stores and flows, and outline how human activities have modified it. Section B asks students to describe how rivers carry sediment loads, explain river erosion processes, illustrate how waterfalls and oxbows are formed with diagrams, and provide examples of how human activities increase flooding risks.
CAMBRIDGE GEOGRAPHY A2 - PRODUCTION, LOCATION AND CHANGE: THE GREEN REVOLUTION
CAMBRIDGE GEOGRAPHY A2 - PRODUCTION, LOCATION AND CHANGE: THE GREEN REVOLUTION. It contains: green revolution, Norman Bourlag, green revolution in Mexico, India, Brazil, Philippines. Effects on food security, Malthusian criticism, the environmental impact.
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.
Fluvial depositional landform geomorphology
This document summarizes fluvial depositional landforms. It begins with an introduction to stream deposition and fluvial landforms. It then discusses reasons for sediment deposition including changes in slope, flow obstructions, and sediment supply. Major landforms are classified and explained, including alluvial fans/cones, braided streams, meandering belts, point bars, backswamps, floodplains, natural levees, and river deltas. Specific features of each landform like bar formation and channel abandonment are described. The document concludes by noting the geological significance of these landforms and their use for cultivation.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - FLUVIAL EROSION
Fluvial erosion is the wearing away and removal of material by moving water in a river channel. The four main processes of fluvial erosion are abrasion, solution, attrition, and hydraulic action, though attrition does not directly erode the channel bed or banks. The two main factors influencing the rate of fluvial erosion are the rock type and the amount of energy available in the river. Dams reduce fluvial erosion downstream by trapping sediment, giving the river more energy to erode channels.
More Related Content
What's hot
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: MEXICAN MIGRATION TO USA
This case study examines migration from Mexico to the US over the past 40 years. It identifies key push and pull factors, including high population growth and economic crises in Mexico, and demand for low-skilled labor in the US. Mexican migrants have concentrated in border states like California and Texas, working mainly in agriculture, construction, and services. While migration rates have declined since the late 1990s, over 12 million Mexican-born individuals lived in the US by 2006. The document also discusses the impacts on both Mexico and the US, such as remittances sent to Mexico and debates over cultural and economic effects in the US.
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY; 1.1. DRAINAGE B...
Introductory presentation of the drainage basin systems in the first chapter of Hydrology and Fluvial Geomorphology, suitable for AS students, consisting in the following: the global hydrological cycle, store, flows, the drainage systems, precipitation, evapotranspiration, interception, infiltration, percolation, drainage patterns, the water balance.
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY: 1.3 RIVER CHANN...
Subchapter 3 in the first chapter of Hydrology and Fluvial Geomorphology, suitable for AS students, consisting in the following: river processes, velocity, flows and Hjulstrom Curve.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.1 LOCAL ENERGY BU...
A comprehensive presentation of subchapter 2.1 Local Energy Budgets, from the second chapter of Physical Geography, AS Cambridge, Atmosphere and Weather.
GEOGRAPHY IGCSE: ALTERNATIVE PAPER 4 - INVESTIGATING
GEOGRAPHY IGCSE: ALTERNATIVE PAPER 4 - INVESTIGATING. It contains: formulating aims and hypotheses, enquiry skills to collect data, questionnaires, observation, counts, measurements, river measurement and beach studies, data presentation techniques, analysis, formation of conclusions.
AS GEOGRAPHY - ROCKS AND WEATHERING: WEATHERING AND ROCKS
Physical weathering breaks rocks into smaller pieces through processes like heating and cooling or wetting and drying. Chemical weathering alters the mineral composition of rocks through reactions with water and acids. Limestone landscapes feature karst topography with features like caves, sinkholes, and limestone pavements formed by the dissolution of calcium carbonate in the rocks. Granite weathers through freeze-thaw action and hydrolysis, forming tors and soil. The rate and type of weathering depends on climate, rock type, relief, vegetation and other factors.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DRAINAGE BASIN
A drainage basin is defined as the area of land drained by a river and its tributaries. Static factors that influence water movement through a basin and do not change over time include rock type, relief, soil type, shape and size of the basin, and drainage density. Dynamic factors that influence water movement through a basin and do vary over time include climate, vegetation, human activities, and previous conditions. All of the factors mentioned influence the amount of water stored in the basin and the rate at which water is transferred between stores.
GEOGRAPHY IGCSE: TOURISM - TRENDS
GEOGRAPHY IGCSE: TOURISM - TRENDS. It contains: trends in tourism, the growth of tourism, trends, infrastructure, reasons behind the trends in tourism.
AS GEOGRAPHY - ATMOSPHERE AND WEATHER - WEATHER PHENOMENA
Atmospheric stability refers to air that does not rise, which can lead to fog, mist or frost formation. Instability occurs when air rises, forming clouds and rain. Clouds are classified by form, height, and whether convection or fronts caused them. Convectional rainfall happens when warm land heats the air above, causing it to rise and condense. Frontal rainfall occurs at boundaries of warm and cold air masses. Orographic rainfall results when air is forced to rise over mountain barriers, cooling and condensing. Hail forms through a process of freezing and melting within cumulonimbus clouds. Dew and radiation fog form on clear nights through surface cooling and condensation. Advection fog
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: ABERFAN MUDFLOW
(1) The document examines the 1966 mudflow disaster in Aberfan, Wales that was caused by the mismanagement of coal waste from nearby mines. (2) Over 100,000 cubic meters of saturated coal waste and debris engulfed parts of the village after heavy rainfall, including a local junior school where 116 children and 5 teachers were killed. (3) An official inquiry found the National Coal Board extremely negligent for irresponsibly dumping large amounts of coal waste on unstable hillsides near a populated area.
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRIC...
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRICULTURAL SYSTEMS AND FOOD PRODUCTION. It contains: ley terms and definitions, topic summary, additional work and suggested websites.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...
This document defines key terms related to weather processes and phenomena. It discusses topics like adiabatic lapse rates, air masses, altitude, clouds, condensation, humidity, instability, precipitation and more. Weather results from changes in atmospheric conditions, such as temperature and moisture levels, which can cause air masses to rise or fall. Various types of precipitation form through different processes, like convectional rainfall from rising warm air or orographic rainfall on the windward sides of mountains. Fog occurs when air is cooled to its dew point through advection or radiation.
Geographical enquiry - Alternative to course work- paper 4 IGCSE
Geographical enquiry - CBD, Rivers and coasts, weather, tourism
IGCSE 2 - Alternative to course work
CAMBRIDGE GEOGRAPHY A2 REVISION - COASTAL ENVIRONMENTS: 8.1 WAVES MARINE AND ...
A2 Geography Revision for Coastal Environments, subchapter 8.1 Waves Marine and Subaerial Processes. It is suitable for Year 13 Geography, Cambridge Examination in November 2016. It contains: key terms and definitions, a topic summary, sketches and descriptions, additional work (6 questions for testing your knowledge) and some suggested websites.
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.1 DR...
A presentation of the first subchapter (Drainage Basin Systems) from the first chapter (Hydrology and Fluvial Geomorphology) of Revision for Geography AS Cambridge exam.
GEOGRAPHY IGCSE: INDUSTRY
The document discusses the four sectors of the economy: primary, secondary, tertiary, and quaternary. The primary sector involves agriculture and extraction of natural resources. The secondary sector processes raw materials into manufactured goods. The tertiary sector provides services. The quaternary sector offers information services. Employment structures have changed over time and differ between countries, with developed nations having more employment in the service sectors than agriculture and industry. Factors like resources, infrastructure, labor, and incentives influence where industries locate.
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM TECTO...
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM TECTONIC PROCESSES. It contains: earthquakes, volcanoes, tsunamis.
CAMBRIDGE GEOGRAPHY AS EXTRA REVISION - EXAM STYLE QUESTIONS 1 - HYDROLOGY AN...
The document contains exam style questions on hydrology and fluvial geomorphology. Section A asks students to define the hydrological cycle, draw a diagram showing its stores and flows, and outline how human activities have modified it. Section B asks students to describe how rivers carry sediment loads, explain river erosion processes, illustrate how waterfalls and oxbows are formed with diagrams, and provide examples of how human activities increase flooding risks.
CAMBRIDGE GEOGRAPHY A2 - PRODUCTION, LOCATION AND CHANGE: THE GREEN REVOLUTION
CAMBRIDGE GEOGRAPHY A2 - PRODUCTION, LOCATION AND CHANGE: THE GREEN REVOLUTION. It contains: green revolution, Norman Bourlag, green revolution in Mexico, India, Brazil, Philippines. Effects on food security, Malthusian criticism, the environmental impact.
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.
What's hot (20)
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: MEXICAN MIGRATION TO USA
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: MEXICAN MIGRATION TO USA
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY; 1.1. DRAINAGE B...
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY; 1.1. DRAINAGE B...
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY: 1.3 RIVER CHANN...
CAMBRIDGE GEOGRAPHY AS - HYDROLOGY AND FLUVIAL GEOMORPHOLOGY: 1.3 RIVER CHANN...
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.1 LOCAL ENERGY BU...
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.1 LOCAL ENERGY BU...
GEOGRAPHY IGCSE: ALTERNATIVE PAPER 4 - INVESTIGATING
GEOGRAPHY IGCSE: ALTERNATIVE PAPER 4 - INVESTIGATING
AS GEOGRAPHY - ROCKS AND WEATHERING: WEATHERING AND ROCKS
AS GEOGRAPHY - ROCKS AND WEATHERING: WEATHERING AND ROCKS
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DRAINAGE BASIN
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DRAINAGE BASIN
AS GEOGRAPHY - ATMOSPHERE AND WEATHER - WEATHER PHENOMENA
AS GEOGRAPHY - ATMOSPHERE AND WEATHER - WEATHER PHENOMENA
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: ABERFAN MUDFLOW
CAMBRIDGE AS GEOGRAPHY - CASE STUDY: ABERFAN MUDFLOW
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRIC...
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRIC...
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...
Geographical enquiry - Alternative to course work- paper 4 IGCSE
Geographical enquiry - Alternative to course work- paper 4 IGCSE
CAMBRIDGE GEOGRAPHY A2 REVISION - COASTAL ENVIRONMENTS: 8.1 WAVES MARINE AND ...
CAMBRIDGE GEOGRAPHY A2 REVISION - COASTAL ENVIRONMENTS: 8.1 WAVES MARINE AND ...
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.1 DR...
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.1 DR...
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM TECTO...
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM TECTO...
CAMBRIDGE GEOGRAPHY AS EXTRA REVISION - EXAM STYLE QUESTIONS 1 - HYDROLOGY AN...
CAMBRIDGE GEOGRAPHY AS EXTRA REVISION - EXAM STYLE QUESTIONS 1 - HYDROLOGY AN...
CAMBRIDGE GEOGRAPHY A2 - PRODUCTION, LOCATION AND CHANGE: THE GREEN REVOLUTION
CAMBRIDGE GEOGRAPHY A2 - PRODUCTION, LOCATION AND CHANGE: THE GREEN REVOLUTION
Similar to REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DEPOSITIONAL LANDFORMS
Fluvial depositional landform geomorphology
This document summarizes fluvial depositional landforms. It begins with an introduction to stream deposition and fluvial landforms. It then discusses reasons for sediment deposition including changes in slope, flow obstructions, and sediment supply. Major landforms are classified and explained, including alluvial fans/cones, braided streams, meandering belts, point bars, backswamps, floodplains, natural levees, and river deltas. Specific features of each landform like bar formation and channel abandonment are described. The document concludes by noting the geological significance of these landforms and their use for cultivation.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - FLUVIAL EROSION
Fluvial erosion is the wearing away and removal of material by moving water in a river channel. The four main processes of fluvial erosion are abrasion, solution, attrition, and hydraulic action, though attrition does not directly erode the channel bed or banks. The two main factors influencing the rate of fluvial erosion are the rock type and the amount of energy available in the river. Dams reduce fluvial erosion downstream by trapping sediment, giving the river more energy to erode channels.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - FLUVIAL DEPOSITION
Fluvial deposition is the process by which a river deposits the material it carries. A river deposits its load when it loses energy, such as when entering a lake or sea or during periods of drought. The largest materials are deposited first as the river loses velocity. If a river suddenly gains a large additional load from an event like a landslide, it will use all its energy to transport material, but will deposit any excess it cannot carry.
Chapter 6:1 Freshwater at Earth’s Surface - Streams
This document discusses freshwater sources on Earth's surface. It covers streams, including how runoff enters streams, types of streams like meandering and braided streams, and how streams shape the land through erosion and deposition. It also discusses drainage basins, and how flooding can be caused by heavy rain or snowmelt that increases stream discharge beyond the capacity of the channel.
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - MEANDER
The document defines meanders as sinuous wave-like forms in river channels. It then provides answers to 4 questions about meanders: 1) River velocity is fastest on the outside of bends and slowest on the inside. 2) Sinuosity is measured as length of channel divided by straight-line distance, with over 1.5 considered meandering. 3) Meander wavelength is typically 7-10 times the channel width. 4) Meanders usually develop when the bed/bank material is silt/clay and the channel gradient is moderately steep to allow bank erosion.
River
The document summarizes key aspects of river systems, including the hydrologic cycle, stream characteristics, erosion and deposition processes, landforms created in the upper, middle, and lower courses of rivers, and human impacts on rivers. It describes evaporation and precipitation cycles, stream velocity and types, erosion by abrasion and hydraulic action, transportation methods, meander formation, floodplain and levee development, and delta building where rivers enter seas. Finally, it discusses human reliance on and interference with rivers through activities like transportation, agriculture, power generation, and pollution.
our changing earth.pptx
Water, wind and ice are the major agents of erosion that shape the landscape. A seismograph is used to measure earthquakes on the Richter scale. Examples of coastal landforms created by erosion and deposition include sea caves, sea arches, stacks and sea cliffs. Large rivers like the Ganges, Zaire and Amazon form deltas with distributaries that deposit sediment as the river speed decreases entering the sea.
Revision booklet 2015 OCR B Geography
This document provides revision materials for a GCSE Geography exam, including key themes, contact information, and resources. It covers topics like rivers, coasts, and landforms. For rivers, it outlines landforms like V-shaped valleys, waterfalls, meanders, and floodplains. For coasts, it discusses landforms including headlands, bays, wave-cut platforms, and beaches. It also provides case studies, definitions of geographic terms, and exam practice questions.
SDME revision pack 2016
The document provides information about rivers and coasts for a GCSE Geography revision pack. It includes key terms, landforms, and processes related to rivers and coasts, as well as case studies on river and coastal management. Resources for further study are also listed.
Rivers presentation
Rivers and streams begin as small tributaries that merge to form larger rivers as they flow downhill towards areas of lower elevation. They perform erosion by processes such as attrition, corrasion, hydraulic action, and chemical solution, and transport sediment through dissolution, suspension, and along the stream bed. A stream's competence and capacity determine the size of materials it can carry. Channel morphology depends on factors like gradient and sediment load, resulting in narrow channels in steep upper reaches and wider braided or meandering patterns downstream. Within channels, features like bars, point bars, and floodplains form through sediment deposition during times of changing flow.
Revision pack OCR B Geography
The River Zambezi floods of 2009 in Namibia displaced over 50,000 people from their homes and caused over $136 million in economic losses. Heavy rainfall led to river levels rising by 8 meters, inundating villages and agricultural land. Over 700,000 people, a third of Namibia's population, were affected. The floods demonstrated the local authorities' inability to respond adequately, with relief efforts hampered by poor coordination. International aid of $7 million was provided to help establish relief camps and address health and sanitation issues.
Chapter 6 the_work_of_streams[1][1]
Streams transport sediment in three ways: dissolved in water, suspended in water, or along the stream bed. As streams flow, they erode their channels and deposit sediment in other areas, forming features like deltas where streams enter larger bodies of water. Floodplains are areas along streams subject to periodic flooding, which occurs when a stream's discharge exceeds the capacity of its channel and overflows its banks.
Rivers
The document discusses rivers, including their definition, formation, and key processes. It notes that rivers are natural flowing watercourses that drain into oceans, lakes, or other bodies of water. Small rivers may have other names like stream or creek. Rivers form through the hydrological cycle as water collects from precipitation through drainage basins. The main processes in rivers are erosion, transportation, and deposition, which are driven by the river's energy. Erosion can make a river wider, deeper, or longer through various types of erosion. Transported materials are eventually deposited through sedimentation.
The Flow of Fresh Water
This document provides an overview of key concepts about rivers and water systems from an Earth Science textbook. It begins by describing how moving water causes erosion and shapes the landscape. It explains the water cycle and defines important river features like tributaries, watersheds, and gradients. Later sections discuss how rivers deposit sediment to form features like deltas and floodplains. It also explains groundwater systems, describing aquifers, springs, wells, and how erosion can form caves and sinkholes. The document concludes by discussing water pollution, water treatment, and conservation strategies.
Uses of Rivers
The document discusses rivers and the hydrological cycle. It begins by explaining how rivers are an important resource for drinking water, transport, electricity and more. It then describes the three main processes by which rivers shape the land - erosion, transportation, and deposition. Erosion involves wearing away river banks and breaking down rock particles. As rivers transport sediment downstream, larger rocks can be moved in higher energy areas near the source, while finer particles are deposited where energy is lowest at the mouth. The document outlines the typical features of the upper, middle and lower courses of a river as its energy decreases downstream.
River Features Map Task
Rivers create landforms through three main processes:
1) Erosion, such as hydraulic action, abrasion, and attrition which help form landforms like V-shaped valleys, waterfalls, and interlocking spurs in the upper course.
2) Transportation of material which leads to deposition and the formation of landforms like point bars inside river meanders in the middle course.
3) Deposition which is prominent in the lower course, creating large floodplains and deltas near the river mouth.
River Presentation
The document discusses river processes and landforms created by erosion, transportation, and deposition of sediment. Key points include:
- Rivers erode, transport, and deposit sediment through various processes including saltation, traction, suspension, and solution that create landforms such as potholes, rapids, waterfalls, deltas, and floodplains.
- The Hjulstrom curve shows the relationship between sediment size, erosion thresholds, and transportation/deposition based on water velocity.
- Meandering rivers create oxbow lakes through lateral erosion and cut-offs of meander loops over time.
floodplain presentation
This document provides an overview of fluvial geomorphology and floodplains. It discusses how rivers erode, transport, and deposit sediment, forming various fluvial landforms like alluvial fans, floodplains, and deltas. Floodplains are formed through vertical accretion, lateral accretion, and channel abandonment. They support rich ecosystems but also experience flooding that interacts with human settlements. India has several major flood-prone river basins, and floods annually cause billions in damage, affected millions of hectares and thousands of lives.
Fluvial/River Processes
Here are the key points about how isostatic changes have impacted the Irish landscape:
- Isostatic changes refer to vertical movements of the Earth's crust due to adjustments in land masses following the melting of ice sheets during glacial periods.
- During the last ice age, much of Ireland was depressed under thick ice sheets, weighing the land surface down. As the ice melted about 10,000 years ago, the land began to rise again in a process known as isostatic rebound.
- This caused rivers to be elevated above their original base levels. Many rivers underwent rejuvenation as they cut downwards, forming features like waterfalls, incised meanders and terraces along their courses as they
L4 Levees And Floodplains
1) Floodplains form through erosion and deposition as rivers carry large loads of sediment and widen their valleys over thousands of years.
2) Levees are natural embankments that form along rivers when water moving out of the channel loses energy and deposits heavier sediments along the banks during flooding.
3) Repeated flooding and deposition over time cause levees and floodplains to build up layers of nutrient-rich alluvium soil.
Similar to REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DEPOSITIONAL LANDFORMS (20)
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - FLUVIAL EROSION
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - FLUVIAL EROSION
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - FLUVIAL DEPOSITION
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - FLUVIAL DEPOSITION
Chapter 6:1 Freshwater at Earth’s Surface - Streams
Chapter 6:1 Freshwater at Earth’s Surface - Streams
More from George Dumitrache
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE SOURCES
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE
On February 27, 1933, the German parliament (Reichstag) building burned down. The Nazi leadership and its coalition partners used the fire to claim that Communists were planning a violent uprising. They claimed that emergency legislation was needed to prevent this. The resulting act, commonly known as the Reichstag Fire Decree, abolished a number of constitutional protections and paved the way for Nazi dictatorship.
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTX
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTX
Following Hitler’s appointment as chancellor the Nazis were finally in a position of power.
However, this power was limited, as the Nazis were just one party in a three party coalition government, under President Hindenburg.
This topic will explore how the Nazis managed to eliminate their opposition and consolidate ultimate power over Germany, whilst maintaining an illusion of democracy.
It will first explore this topic in chronological order, from the Reichstag Fire through to the death of President Hindenburg, and then explore it thematically in the last section. On the 31 January 1933, Hitler, conscious of his lack of a majority in the Reichstag, immediately called for new elections to try and strengthen his position. The Nazis aimed to increase their share of the vote so that they would have a majority in the Reichstag. This would allow them to rule unopposed and unhindered by coalition governments.
Over the next two months, they launched themselves into an intense election campaign.
On 27 February 1933, as the campaign moved into its final, frantic days, the Reichstag, the German Parliament building, was set on fire and burnt down. An atmosphere of panic and terror followed the event.
This continued when a young Dutch communist, Van der Lubbe was arrested for the crime.
The Nazi Party used the atmosphere of panic to their advantage, encouraging anti-communism. Göring declared that the communists had planned a national uprising to overthrow the Weimar Republic. This hysteria helped to turn the public against the communists, one of the Nazis main opponents, and 4000 people were imprisoned.
The day after the fire, Hindenburg signed the Emergency Decree for the Protection of the German People. On the 28 February 1933, President Hindenburg signed the Emergency Decree for the Protection of the German People. This decree suspended the democratic aspects of the Weimar Republic and declared a state of emergency.
This decree gave the Nazis a legal basis for the persecution and oppression of any opponents, who were be framed as traitors to the republic. People could be imprisoned for any or no reason.
The decree also removed basic personal freedoms, such as the freedom of speech, the right to own property, and the right to trial before imprisonment.
Through these aspects the Nazis suppressed any opposition to their power, and were able to start the road from democracy to a dictatorship. The atmosphere of uncertainty following the Reichstag Fire secured many voters for the Nazi party.
The SA also ran a violent campaign of terror against any and all opponents of the Nazi regime. Many were terrified of voting of at all, and many turned to voting for the Nazi Party out of fear for their own safety. The elections were neither free or fair.
On the 5 March 1933, the elections took place, with an extremely high turnout of 89%.
The Nazis secured 43.9% of the vote.
DEPTH STUDY GERMANY: NAZI REGIME - 04. HITLER BECOMING CHANCELLOR 1933
Hitler was not immediately appointed chancellor after the success of the July 1932 elections, despite being leader of the largest party in the Reichstag. It took the economic and political instability (with two more chancellors failing to stabilise the situation) to worsen, and the support of the conservative elite, to convince Hindenburg to appoint Hitler.
Hitler was sworn in as the chancellor of Germany on the 30 January 1933. The Nazis were now in power.
DEPTH STUDY GERMANY: NAZI REGIME - 03. NAZI'S LITTLE SUCCESS
The document discusses the early success of the Nazi party in Germany. It notes that while the party made progress in organization and membership in its early years after 1919, it had little impact in elections initially. The Nazis received only 6.5% of the vote in their first national election in 1924. Later elections in 1928 saw their support decline further to just 2.6% as the German economy and political situation stabilized under Stresemann. While the Nazis appealed to specific groups frustrated with the Weimar Republic, they remained a small party with less than 30,000 members by 1925.
DEPTH STUDY GERMANY: NAZI REGIME - 02. NAZI PARTY IDEOLOGY IN 1920
The document provides background information on the origins and early development of the Nazi party in Germany during the 1920s. It describes how the party began as the German Workers' Party led by Anton Drexler before Hitler joined in 1919 and became the leader in 1921. It also outlines some of the key aspects of the Nazi party platform outlined in the 25-point program, including nationalism, anti-Semitism, and a desire for more territory. Finally, it discusses Hitler's failed Munich Putsch coup attempt in 1923 and how he wrote Mein Kampf while in prison.
DEPTH STUDY GERMANY: NAZI REGIME - 01. FASCISM
1) Post-war instability and economic crisis weakened established political systems in countries like Germany and Italy. 2) A sense of nationalism was used by fascist leaders to promote unity and scapegoat others for the nation's problems. 3) Charismatic leaders like Hitler and Mussolini were able to gain followers by promoting fascism as an alternative to communism and liberal democracy.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 10. THE FALL OF WEIMAR 1930-1933
The document provides background information on the rise of the Nazi party in Germany between 1930-1933. It discusses how Germany's economic dependence on American loans led to the collapse of German industry following the 1929 Wall Street crash. This caused widespread unemployment, with over 6 million people jobless by 1932. As economic conditions deteriorated, support grew for the Nazis as they promised strong leadership and blamed Jews and communists for Germany's problems. The Nazis increased their Reichstag seats in elections in 1933 after Hitler became Chancellor, and he then used emergency powers to crush opposition and establish a one-party Nazi state in Germany.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 09. TABLES AND CARTOONS
The document discusses the Weimar Republic in Germany through tables and cartoons as part of a Cambridge IGCSE depth study on Germany. It provides information on the political and economic challenges faced by the Weimar Republic between 1919-1933 through statistical tables and illustrations. The depth study uses multiple visual elements to summarize key events and issues like inflation, unemployment, and the rise of extremism during this period of German history.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 08. NAZIS IN THE WILDERNESS
The “Lean Years” (also called the "wilderness" years) of Hitler and the Nazi Party in Germany refer to the period between 1924 and 1928 when the Nazi party did not have high levels of support and still suffered from humiliation over the Munich Putsch. Why where these years “lean”?
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 07. STRESEMMAN ERA 1924-1929
Gustav Stresemann was appointed Chancellor of Germany in 1923 during the Weimar Republic period. As Chancellor and later as Foreign Minister, he implemented policies that helped stabilize Germany's economy and improve its international standing. This included establishing a new currency to end hyperinflation, crushing communist uprisings, and pursuing diplomatic agreements like the Locarno Pact to normalize Germany's relations with other European powers. However, the economic and political stability of the Weimar Republic remained fragile.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 06. THE BEER HALL PUTSCH 1923
The Beer Hall Putsch, also known as the Munich Putsch, was a failed coup d'état by Nazi Party (Nationalsozialistische Deutsche Arbeiterpartei or NSDAP) leader Adolf Hitler, Generalquartiermeister Erich Ludendorff and other Kampfbund leaders in Munich, Bavaria, on 8–9 November 1923, during the Weimar Republic. Approximately two thousand Nazis marched on the Feldherrnhalle, in the city centre, but were confronted by a police cordon, which resulted in the deaths of 16 Nazi Party members and four police officers. Hitler escaped immediate arrest and was spirited off to safety in the countryside. After two days, he was arrested and charged with treason. The putsch brought Hitler to the attention of the German nation for the first time and generated front-page headlines in newspapers around the world. His arrest was followed by a 24-day trial, which was widely publicised and gave him a platform to express his nationalist sentiments to the nation. Hitler was found guilty of treason and sentenced to five years in Landsberg Prison, where he dictated Mein Kampf to fellow prisoners Emil Maurice and Rudolf Hess. On 20 December 1924, having served only nine months, Hitler was released. Once released, Hitler redirected his focus towards obtaining power through legal means rather than by revolution or force, and accordingly changed his tactics, further developing Nazi propaganda.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 05. HYPERINFLATION
Hyperinflation affected the German Papiermark, the currency of the Weimar Republic, between 1921 and 1923, primarily in 1923. It caused considerable internal political instability in the country, the occupation of the Ruhr by France and Belgium, and misery for the general populace.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 04. WEIMAR TURMOIL YEARS 1919-1923
Weimar had faced a series of problems between 1919 and 1923 (hyperinflation, Munich Putsch, Kapp Putsch) but despite the odds had managed to survive.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 03. THE TREATY OF VERSAILLES IMPACT ON...
Thanks to the Treaty of Versailles, Germany's ability to produce revenue-generating coal and iron ore decreased. As war debts and reparations drained its coffers, the German government was unable to pay its debts. Some of the former World War I Allies didn't buy Germany's claim that it couldn't afford to pay.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 02. THE NOVEMBER REVOLUTION 1918
The German Revolution or November Revolution was a civil conflict in the German Empire at the end of the First World War that resulted in the replacement of the German federal constitutional monarchy with a democratic parliamentary republic that later became known as the Weimar Republic. The revolutionary period lasted from November 1918 until the adoption of the Weimar Constitution in August 1919. Among the factors leading to the revolution were the extreme burdens suffered by the German population during the four years of war, the economic and psychological impacts of the German Empire's defeat by the Allies, and growing social tensions between the general population and the aristocratic and bourgeois elite.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 01. THE EFFECT OF WW1 ON GERMANY
The document summarizes the impact of World War 1 on Germany. It discusses how Germany initially found success on the Eastern Front and made advances on the Western Front in 1918 but was eventually overwhelmed as the US joined the war effort. Germany experienced political instability, economic devastation from blockades, widespread hunger and disease, and psychological trauma from defeat. The German people bitterly blamed leaders for the defeat, sowing seeds for the rise of the Nazis in the unstable Weimar Republic that followed the war.
08. LEAGUE OF NATIONS - Questions and Answers.pptx
QUESTIONS AND ANSWERS - LEAGUE OF NATIONS. The League of Nations was an international organization, headquartered in Geneva, Switzerland, created after the First World War to provide a forum for resolving international disputes.
07. LEAGUE OF NATIONS - Abyssinian Crisis.pptx
This cartoon was likely published after the Stresa Pact was signed in early 1935, when Britain and France failed to raise the issue of Abyssinia with Mussolini and were perceived as turning a blind eye to his plans in hopes of keeping Italy as an ally against Germany. The cartoon directly criticizes the British and French policy of appeasing Mussolini, so the purpose was to criticize, not just inform. By criticizing the policy, the hope would be to influence and change the policy by swaying public opinion.
06. LEAGUE OF NATIONS - Manchurian Crisis.pptx
Manchurian Crisis. On September 18, 1931, an explosion destroyed a section of railway track near the city of Mukden. The Japanese, who owned the railway, blamed Chinese nationalists for the incident and used the opportunity to retaliate and invade Manchuria.
05. LEAGUE OF NATIONS - Great Depression and LON.pptx
GREAT DEPRESSION AND THE LEAGUE OF NATIONS. The Great Depression of 1930-33 meant people turned to extremist dictators such as Hitler and Mussolini, who were keen to invade other countries. This made it hard for the League to maintain peace. The League had some very ambitious plans and ideals – to stop war and make the world a better place.
More from George Dumitrache (20)
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE SOURCES
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE SOURCES
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTX
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTX
DEPTH STUDY GERMANY: NAZI REGIME - 04. HITLER BECOMING CHANCELLOR 1933
DEPTH STUDY GERMANY: NAZI REGIME - 04. HITLER BECOMING CHANCELLOR 1933
DEPTH STUDY GERMANY: NAZI REGIME - 03. NAZI'S LITTLE SUCCESS
DEPTH STUDY GERMANY: NAZI REGIME - 03. NAZI'S LITTLE SUCCESS
DEPTH STUDY GERMANY: NAZI REGIME - 02. NAZI PARTY IDEOLOGY IN 1920
DEPTH STUDY GERMANY: NAZI REGIME - 02. NAZI PARTY IDEOLOGY IN 1920
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 10. THE FALL OF WEIMAR 1930-1933
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 10. THE FALL OF WEIMAR 1930-1933
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 09. TABLES AND CARTOONS
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 09. TABLES AND CARTOONS
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 08. NAZIS IN THE WILDERNESS
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 08. NAZIS IN THE WILDERNESS
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 07. STRESEMMAN ERA 1924-1929
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 07. STRESEMMAN ERA 1924-1929
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 06. THE BEER HALL PUTSCH 1923
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 06. THE BEER HALL PUTSCH 1923
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 05. HYPERINFLATION
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 05. HYPERINFLATION
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 04. WEIMAR TURMOIL YEARS 1919-1923
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 04. WEIMAR TURMOIL YEARS 1919-1923
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 03. THE TREATY OF VERSAILLES IMPACT ON...
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 03. THE TREATY OF VERSAILLES IMPACT ON...
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 02. THE NOVEMBER REVOLUTION 1918
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 02. THE NOVEMBER REVOLUTION 1918
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 01. THE EFFECT OF WW1 ON GERMANY
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 01. THE EFFECT OF WW1 ON GERMANY
08. LEAGUE OF NATIONS - Questions and Answers.pptx
08. LEAGUE OF NATIONS - Questions and Answers.pptx
05. LEAGUE OF NATIONS - Great Depression and LON.pptx
05. LEAGUE OF NATIONS - Great Depression and LON.pptx
Recently uploaded
BÀI TẬP DẠY THÊM TIẾNG ANH LỚP 7 CẢ NĂM FRIENDS PLUS SÁCH CHÂN TRỜI SÁNG TẠO ...
BÀI TẬP DẠY THÊM TIẾNG ANH LỚP 7 CẢ NĂM FRIENDS PLUS SÁCH CHÂN TRỜI SÁNG TẠO ...Nguyen Thanh Tu Collection
https://app.box.com/s/qhtvq32h4ybf9t49ku85x0n3xl4jhr15BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...
BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...Nguyen Thanh Tu Collection
https://app.box.com/s/tacvl9ekroe9hqupdnjruiypvm9rdaneThe History of Stoke Newington Street Names
Presented at the Stoke Newington Literary Festival on 9th June 2024
www.StokeNewingtonHistory.com
Mule event processing models | MuleSoft Mysore Meetup #47
Mule event processing models | MuleSoft Mysore Meetup #47
Event Link:- https://meetups.mulesoft.com/events/details/mulesoft-mysore-presents-mule-event-processing-models/
Agenda
● What is event processing in MuleSoft?
● Types of event processing models in Mule 4
● Distinction between the reactive, parallel, blocking & non-blocking processing
For Upcoming Meetups Join Mysore Meetup Group - https://meetups.mulesoft.com/mysore/YouTube:- youtube.com/@mulesoftmysore
Mysore WhatsApp group:- https://chat.whatsapp.com/EhqtHtCC75vCAX7gaO842N
Speaker:-
Shivani Yasaswi - https://www.linkedin.com/in/shivaniyasaswi/
Organizers:-
Shubham Chaurasia - https://www.linkedin.com/in/shubhamchaurasia1/
Giridhar Meka - https://www.linkedin.com/in/giridharmeka
Priya Shaw - https://www.linkedin.com/in/priya-shaw
Your Skill Boost Masterclass: Strategies for Effective Upskilling
Your Skill Boost Masterclass: Strategies for Effective UpskillingExcellence Foundation for South Sudan
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.Philippine Edukasyong Pantahanan at Pangkabuhayan (EPP) Curriculum
(𝐓𝐋𝐄 𝟏𝟎𝟎) (𝐋𝐞𝐬𝐬𝐨𝐧 𝟏)-𝐏𝐫𝐞𝐥𝐢𝐦𝐬
𝐃𝐢𝐬𝐜𝐮𝐬𝐬 𝐭𝐡𝐞 𝐄𝐏𝐏 𝐂𝐮𝐫𝐫𝐢𝐜𝐮𝐥𝐮𝐦 𝐢𝐧 𝐭𝐡𝐞 𝐏𝐡𝐢𝐥𝐢𝐩𝐩𝐢𝐧𝐞𝐬:
- Understand the goals and objectives of the Edukasyong Pantahanan at Pangkabuhayan (EPP) curriculum, recognizing its importance in fostering practical life skills and values among students. Students will also be able to identify the key components and subjects covered, such as agriculture, home economics, industrial arts, and information and communication technology.
𝐄𝐱𝐩𝐥𝐚𝐢𝐧 𝐭𝐡𝐞 𝐍𝐚𝐭𝐮𝐫𝐞 𝐚𝐧𝐝 𝐒𝐜𝐨𝐩𝐞 𝐨𝐟 𝐚𝐧 𝐄𝐧𝐭𝐫𝐞𝐩𝐫𝐞𝐧𝐞𝐮𝐫:
-Define entrepreneurship, distinguishing it from general business activities by emphasizing its focus on innovation, risk-taking, and value creation. Students will describe the characteristics and traits of successful entrepreneurs, including their roles and responsibilities, and discuss the broader economic and social impacts of entrepreneurial activities on both local and global scales.
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
-------------------------------------------------------------------------------
Find out more about ISO training and certification services
Training: ISO/IEC 27001 Information Security Management System - EN | PECB
ISO/IEC 42001 Artificial Intelligence Management System - EN | PECB
General Data Protection Regulation (GDPR) - Training Courses - EN | PECB
Webinars: https://pecb.com/webinars
Article: https://pecb.com/article
-------------------------------------------------------------------------------
For more information about PECB:
Website: https://pecb.com/
LinkedIn: https://www.linkedin.com/company/pecb/
Facebook: https://www.facebook.com/PECBInternational/
Slideshare: http://www.slideshare.net/PECBCERTIFICATION
Temple of Asclepius in Thrace. Excavation results
The temple and the sanctuary around were dedicated to Asklepios Zmidrenus. This name has been known since 1875 when an inscription dedicated to him was discovered in Rome. The inscription is dated in 227 AD and was left by soldiers originating from the city of Philippopolis (modern Plovdiv).
Traditional Musical Instruments of Arunachal Pradesh and Uttar Pradesh - RAYH...
Traditional Musical Instruments of Arunachal Pradesh and Uttar Pradesh
Main Java[All of the Base Concepts}.docx
This is part 1 of my Java Learning Journey. This Contains Custom methods, classes, constructors, packages, multithreading , try- catch block, finally block and more.
Solutons Maths Escape Room Spatial .pptx
Solutions of Puzzles of Mathematics Escape Room Game in Spatial.io
How to Make a Field Mandatory in Odoo 17
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
Leveraging Generative AI to Drive Nonprofit Innovation
In this webinar, participants learned how to utilize Generative AI to streamline operations and elevate member engagement. Amazon Web Service experts provided a customer specific use cases and dived into low/no-code tools that are quick and easy to deploy through Amazon Web Service (AWS.)
Advanced Java[Extra Concepts, Not Difficult].docx
This is part 2 of my Java Learning Journey. This contains Hashing, ArrayList, LinkedList, Date and Time Classes, Calendar Class and more.
Recently uploaded (20)
BÀI TẬP DẠY THÊM TIẾNG ANH LỚP 7 CẢ NĂM FRIENDS PLUS SÁCH CHÂN TRỜI SÁNG TẠO ...
BÀI TẬP DẠY THÊM TIẾNG ANH LỚP 7 CẢ NĂM FRIENDS PLUS SÁCH CHÂN TRỜI SÁNG TẠO ...
B. Ed Syllabus for babasaheb ambedkar education university.pdf
B. Ed Syllabus for babasaheb ambedkar education university.pdf
BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...
BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...
Mule event processing models | MuleSoft Mysore Meetup #47
Mule event processing models | MuleSoft Mysore Meetup #47
Your Skill Boost Masterclass: Strategies for Effective Upskilling
Your Skill Boost Masterclass: Strategies for Effective Upskilling
Philippine Edukasyong Pantahanan at Pangkabuhayan (EPP) Curriculum
Philippine Edukasyong Pantahanan at Pangkabuhayan (EPP) Curriculum
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
Traditional Musical Instruments of Arunachal Pradesh and Uttar Pradesh - RAYH...
Traditional Musical Instruments of Arunachal Pradesh and Uttar Pradesh - RAYH...
Leveraging Generative AI to Drive Nonprofit Innovation
Leveraging Generative AI to Drive Nonprofit Innovation
Film vocab for eal 3 students: Australia the movie
Film vocab for eal 3 students: Australia the movie
REVISION AS CAMBRIDGE GEOGRAPHY: RIVERS - DEPOSITIONAL LANDFORMS
- 2. QUESTION 1 In which part of a river’s course are depositional landforms predominantly found?
- 3. ANSWER In the lower course, sometimes called old course, where the river becomes lazy, loosing its velocity thus encouraging deposition (sediments deposited).
- 4. QUESTION 2 What are levees?
- 5. ANSWER Levees are raised river banks. They can be natural and artificial (reinforced raised banks to protect against flooding).
- 6. QUESTION 3 How are levees formed by rivers?
- 7. ANSWER During flood conditions, water leaves the river channel and loses velocity (speed) as it spreads on to the surrounding area. Deposition occurs and material builds up on the banks. Further flooding causes this to be repeated and the levees to increase in height.
- 8. QUESTION 4 Name three other depositional landforms.
- 9. ANSWER Deltas, alluvial fans, floodplains, oxbow lakes, point bars.