Flowing water has the ability to dissolve the soluble mineral substances available on its way. The processes enacted by streams are called as fluvial processes. The word “fluvius” is derived from the latin word meaning “ river”. The world fluvial is used to denote the running water as streams or rivers. Fluvial processes entail the erosion, transportation, and deposition of earth materials by running water. Fluvial processes and fluvial landforms dominate land surfaces the world over, as opposed to the limited effects of glacial, coastal, and wind processes.
Fluvial processes create distinct landforms over time as a river ages. In the youth stage, the river valley is narrow with steep sides. Meanders begin to form in the maturity stage as the river widens and deepens. In the old stage, the river flows across a flat floodplain as it approaches being a featureless plain. Distinct landforms are produced at each stage as the river's erosional and depositional activities change.
This document discusses hydrogeology, which is the study of groundwater. It begins by explaining the hydrologic cycle, in which water evaporates from bodies of water and transpirates from plants, condenses into clouds and precipitates back to the ground as rain or snow. Some precipitation infiltrates into the ground to become groundwater. The document then discusses groundwater occurrence, movement through aquifers, and factors that influence it like porosity, permeability and lithology. Finally, it describes the vertical distribution of groundwater into the unsaturated zone above the water table and saturated zone below it.
This document discusses different types of erosional and depositional landforms created by river processes. It describes landforms such as V-shaped valleys and waterfalls that are created by erosion, and floodplains and deltas that are formed by deposition. It also explains the factors that influence fluvial erosion and the formation of various erosional features like interlocking spurs, rapids, and potholes.
Glacial processes and their land forms.Pramoda Raj
Glaciers are masses of ice that move due to gravity. They erode the landscape through abrasion and plucking, and transport material large distances. Glaciers deposit this material as till or outwash. Glacial processes form characteristic landforms such as cirques, arêtes, and u-shaped valleys through erosion and landforms like moraines and eskers through deposition. Glacial lakes are also left behind when a glacier melts.
Coastal Geomorphology Landforms Of Wave Erosion & DepositionPRasad PK
This document discusses various coastal landforms and processes. It defines coastal geomorphology and describes how waves, longshore currents, rip currents, and tides shape coastal areas and transport sediment. It then lists and describes specific coastal landforms like headlands, bays, sea cliffs, beaches, bars, spits, tombolos, sand dunes, salt marshes, and more. For each landform, it provides a brief definition and example photo. Coastal erosion processes like abrasion, hydraulic action, corrosion, and attrition are also outlined.
This document provides an overview of karst topography and the geological processes involved in its formation. Karst topography is shaped by the dissolution of soluble bedrock like limestone by mildly acidic water. This causes features like caves, sinkholes, stalactites, stalagmites, and disappearing streams. The water dissolves along fractures in the bedrock, enlarging openings underground and forming drainage systems. Over thousands of years, this process creates characteristic karst landforms.
Flowing water has the ability to dissolve the soluble mineral substances available on its way. The processes enacted by streams are called as fluvial processes. The word “fluvius” is derived from the latin word meaning “ river”. The world fluvial is used to denote the running water as streams or rivers. Fluvial processes entail the erosion, transportation, and deposition of earth materials by running water. Fluvial processes and fluvial landforms dominate land surfaces the world over, as opposed to the limited effects of glacial, coastal, and wind processes.
Fluvial processes create distinct landforms over time as a river ages. In the youth stage, the river valley is narrow with steep sides. Meanders begin to form in the maturity stage as the river widens and deepens. In the old stage, the river flows across a flat floodplain as it approaches being a featureless plain. Distinct landforms are produced at each stage as the river's erosional and depositional activities change.
This document discusses hydrogeology, which is the study of groundwater. It begins by explaining the hydrologic cycle, in which water evaporates from bodies of water and transpirates from plants, condenses into clouds and precipitates back to the ground as rain or snow. Some precipitation infiltrates into the ground to become groundwater. The document then discusses groundwater occurrence, movement through aquifers, and factors that influence it like porosity, permeability and lithology. Finally, it describes the vertical distribution of groundwater into the unsaturated zone above the water table and saturated zone below it.
This document discusses different types of erosional and depositional landforms created by river processes. It describes landforms such as V-shaped valleys and waterfalls that are created by erosion, and floodplains and deltas that are formed by deposition. It also explains the factors that influence fluvial erosion and the formation of various erosional features like interlocking spurs, rapids, and potholes.
Glacial processes and their land forms.Pramoda Raj
Glaciers are masses of ice that move due to gravity. They erode the landscape through abrasion and plucking, and transport material large distances. Glaciers deposit this material as till or outwash. Glacial processes form characteristic landforms such as cirques, arêtes, and u-shaped valleys through erosion and landforms like moraines and eskers through deposition. Glacial lakes are also left behind when a glacier melts.
Coastal Geomorphology Landforms Of Wave Erosion & DepositionPRasad PK
This document discusses various coastal landforms and processes. It defines coastal geomorphology and describes how waves, longshore currents, rip currents, and tides shape coastal areas and transport sediment. It then lists and describes specific coastal landforms like headlands, bays, sea cliffs, beaches, bars, spits, tombolos, sand dunes, salt marshes, and more. For each landform, it provides a brief definition and example photo. Coastal erosion processes like abrasion, hydraulic action, corrosion, and attrition are also outlined.
This document provides an overview of karst topography and the geological processes involved in its formation. Karst topography is shaped by the dissolution of soluble bedrock like limestone by mildly acidic water. This causes features like caves, sinkholes, stalactites, stalagmites, and disappearing streams. The water dissolves along fractures in the bedrock, enlarging openings underground and forming drainage systems. Over thousands of years, this process creates characteristic karst landforms.
This document summarizes geomorphic processes including exogenic processes like weathering, mass wasting, erosion and aggradation that modify the Earth's surface through physical and chemical means. Endogenic processes like volcanism and diastrophism involve subsurface movement of magma or rock. Extra-terrestrial processes include meteorite impacts that also shape landforms. The document discusses various agents and mechanisms of weathering, erosion, transportation and deposition of earth materials.
The document describes William Morris Davis' geographical cycle of erosion, which outlines the evolution of landforms over time through three main stages: youth, mature, and old. The cycle begins with the uplift of a landmass, initiating rapid erosion during the youthful stage as rivers deepen valleys. In the mature stage, erosion shifts to lateral widening of valleys as gradients decrease. Finally, in the old stage valleys become flat as erosion slows, resulting in a peneplain landscape. The cycle may be rejuvenated by drops in sea level or renewed uplift restarting the erosion process.
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
This document summarizes aeolian (wind-related) processes and landforms. It describes the three main aeolian processes of erosion, transportation, and deposition by wind. Erosion occurs through deflation, corrasion/abrasion, and attrition. Transportation is by saltation, suspension, and rolling/traction. Deposition results from decreases in wind velocity. Aeolian landforms include erosional features like ventifacts, yardangs, and desert pavements, as well as depositional landforms such as loess, dunes, and ripples that are formed by the accumulation of wind-blown sediments. Different types of dunes like barchan, transverse, and parabolic d
The document discusses fluvial processes and landforms. It describes various types of erosion caused by water including surface erosion through splash and sheet erosion, and channel erosion through rills, gullies, and streams. It also discusses drainage basins and patterns, explaining how drainage patterns are influenced by geology and reflect the arrangement of river courses. Various landforms resulting from fluvial processes are also mentioned.
Groundwater levels fluctuate due to various factors. Secular variations occur over years due to changes in storage and recharge/discharge amounts. Seasonal variations result from rainfall and irrigation on well-defined cycles. Diurnal variations happen within a day due to tidal effects. Other causes of groundwater level changes include stream flows, evaporation, transpiration, atmospheric pressure, wind, rainfall, ocean tides, earth tides, external loads, earthquakes, urbanization, volcanic eruptions, roads, and continental drift.
The document discusses aeolian (wind-related) landforms and processes. It describes how wind can erode, transport, and deposit materials through various processes like abrasion, deflation, and saltation. Some erosional landforms formed by wind include ventifacts, yardangs, and mushroom rocks. Depositional landforms include loess, sand dunes (which can take various forms like barchan, transverse, parabolic, and longitudinal dunes), and sand ripples. Aeolian processes and landforms are particularly important in arid environments like deserts where wind is a dominant agent of geomorphic change.
Groundwater exists below the Earth's surface within the pore spaces and fractures of rocks and sediments. It originates from rainfall and snowmelt that percolates underground, where it moves slowly through the saturated zone and eventually resurfaces in streams, lakes, or oceans. The movement and storage of groundwater is dependent on the porosity, permeability, and saturation of geological formations. When groundwater is pumped from wells faster than it can recharge, water tables decline and other issues like land subsidence can occur. Groundwater supports various geological features and processes near the surface.
This document provides an overview of key concepts in geomorphology. It defines geomorphology as the study of landforms and discusses how landforms are shaped by tectonic and hydrologic processes. Early theories that invoked supernatural causes are contrasted with modern theories of uniformitarianism and plate tectonics. The roles of various controlling factors - including geomorphic agents, surficial materials, tectonic setting, and climate - are examined. Different types of crustal features like continents, mountain belts, shields, and continental shelves are also introduced.
Glaciers form from accumulated snow that undergoes recrystallization into ice. They flow via gravity from accumulation zones where snowfall exceeds melting to ablation zones where melting exceeds snowfall. Glaciers powerfully erode, transport, and deposit sediment. They carve U-shaped valleys and leave behind landforms like moraines, drumlins, eskers and kettle lakes. Glaciers shape mountain and coastal landscapes through erosion and deposition.
The document discusses 10 key concepts in geomorphology. It begins by defining geomorphology as the study of landforms and their formation and development. It then explains each concept in 1-2 paragraphs with examples. The concepts are: 1) Uniformitarianism, 2) Role of geologic structure, 3) Differential erosion rates, 4) Distinct landforms from geomorphic processes, 5) Geomorphic cycles, 6) Complex geomorphic evolution, 7) Young topography, 8) Impact of Pleistocene climate change, 9) Role of climate on processes, 10) Historical approach. The document concludes with a quick review of the 10 concepts.
Stream capture, also known as river capture or stream piracy, is the process where a river or stream redirects its flow and starts flowing into another river's drainage basin instead of continuing into its own basin. This can occur where two drainage basins are separated by an erosion-resistant divide that is breached by headward erosion of one of the streams. Once the divide is breached, the stream will capture the tributaries of the neighboring basin and divert its entire flow into the new course. Stream capture events can result in changes to drainage patterns over time.
The document summarizes the tectonic framework of India in 3 broad divisions - Peninsular India, Extra-Peninsular India, and the Indo-Gangetic Plain. Peninsular India comprises the Indian shield and its sedimentary basins, and is further divided into the shield areas, mobile belts, and Proterozoic sedimentary basins. Extra-Peninsular India includes the Himalayan mountain ranges, divided into the Lesser Himalayan zone, Central Crystalline zone, and Tethyan zone. The Indo-Gangetic Plain is a deep crustal trough in northern India filled with Quaternary sediments.
Orogenesis is the process of mountain building that occurs during an orogeny. An orogeny involves tectonic processes like subduction and plate convergence that cause deformation and metamorphism of the Earth's crust, forming orogenic belts made of parallel rock structures. Orogenies can take tens of millions of years to build mountains and are associated with the development of foreland basins in front of the growing mountain range.
This document discusses different types of drainage patterns that can form based on topography, geology, climate, and other factors. It describes dendritic, trellis, rectangular, radial, parallel, and annular drainage patterns. The dendritic pattern resembles a tree branch and forms in impervious rock. The trellis pattern has tributaries joining at right angles and forms in folded mountains with parallel hard and soft rocks. The rectangular pattern forms in uniformly resistant and jointed rocks. The radial pattern has streams radiating outward from a central high point. The parallel pattern has straight, swift streams along resistant rock bands with few tributaries. The annular and centripetal patterns form rings around structural domes or basins. Combinations of
1. Drainage patterns are formed by the networks of streams, rivers, and lakes within a drainage basin and are influenced by the topography and geology of the land.
2. The most common drainage pattern is dendritic, where many small streams feed into larger tributaries and ultimately the trunk river. Dendritic patterns form in V-shaped valleys in impermeable rock.
3. Other drainage patterns include parallel, trellis, rectangular, radial, centripetal, annular, and angular - each forming under different geological conditions and rock structures. Discordant drainage does not correlate to the underlying geology.
Concept 1. The same physical processes and laws that operate today operated throughout geologic time, although not necessarily always with the same intensity as now.
Concept 2. Geologic structure is a dominant control factor in the evolution of land forms and is reflected in them.
River rejuvenation occurs when a river's base level changes, altering the gradient of the river channel and increasing its erosive power. This causes the river to cut downward into its channel, forming landforms such as waterfalls, incised meanders, and river terraces. Changes in base level are typically caused by isostatic adjustments to sea level from glacial rebound or eustatic sea level changes.
The document discusses several landforms that can result from river rejuvenation caused by a fall in sea level. Knick points form as steps where the river erodes downward to adjust to the new base level, and may create waterfalls. River terraces are abandoned floodplains left at higher levels after the river cuts down through deposits. Incised or enclosed meanders develop when the river maintains its meandering pattern while increasing vertical erosion.
This document summarizes geomorphic processes including exogenic processes like weathering, mass wasting, erosion and aggradation that modify the Earth's surface through physical and chemical means. Endogenic processes like volcanism and diastrophism involve subsurface movement of magma or rock. Extra-terrestrial processes include meteorite impacts that also shape landforms. The document discusses various agents and mechanisms of weathering, erosion, transportation and deposition of earth materials.
The document describes William Morris Davis' geographical cycle of erosion, which outlines the evolution of landforms over time through three main stages: youth, mature, and old. The cycle begins with the uplift of a landmass, initiating rapid erosion during the youthful stage as rivers deepen valleys. In the mature stage, erosion shifts to lateral widening of valleys as gradients decrease. Finally, in the old stage valleys become flat as erosion slows, resulting in a peneplain landscape. The cycle may be rejuvenated by drops in sea level or renewed uplift restarting the erosion process.
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
This document summarizes aeolian (wind-related) processes and landforms. It describes the three main aeolian processes of erosion, transportation, and deposition by wind. Erosion occurs through deflation, corrasion/abrasion, and attrition. Transportation is by saltation, suspension, and rolling/traction. Deposition results from decreases in wind velocity. Aeolian landforms include erosional features like ventifacts, yardangs, and desert pavements, as well as depositional landforms such as loess, dunes, and ripples that are formed by the accumulation of wind-blown sediments. Different types of dunes like barchan, transverse, and parabolic d
The document discusses fluvial processes and landforms. It describes various types of erosion caused by water including surface erosion through splash and sheet erosion, and channel erosion through rills, gullies, and streams. It also discusses drainage basins and patterns, explaining how drainage patterns are influenced by geology and reflect the arrangement of river courses. Various landforms resulting from fluvial processes are also mentioned.
Groundwater levels fluctuate due to various factors. Secular variations occur over years due to changes in storage and recharge/discharge amounts. Seasonal variations result from rainfall and irrigation on well-defined cycles. Diurnal variations happen within a day due to tidal effects. Other causes of groundwater level changes include stream flows, evaporation, transpiration, atmospheric pressure, wind, rainfall, ocean tides, earth tides, external loads, earthquakes, urbanization, volcanic eruptions, roads, and continental drift.
The document discusses aeolian (wind-related) landforms and processes. It describes how wind can erode, transport, and deposit materials through various processes like abrasion, deflation, and saltation. Some erosional landforms formed by wind include ventifacts, yardangs, and mushroom rocks. Depositional landforms include loess, sand dunes (which can take various forms like barchan, transverse, parabolic, and longitudinal dunes), and sand ripples. Aeolian processes and landforms are particularly important in arid environments like deserts where wind is a dominant agent of geomorphic change.
Groundwater exists below the Earth's surface within the pore spaces and fractures of rocks and sediments. It originates from rainfall and snowmelt that percolates underground, where it moves slowly through the saturated zone and eventually resurfaces in streams, lakes, or oceans. The movement and storage of groundwater is dependent on the porosity, permeability, and saturation of geological formations. When groundwater is pumped from wells faster than it can recharge, water tables decline and other issues like land subsidence can occur. Groundwater supports various geological features and processes near the surface.
This document provides an overview of key concepts in geomorphology. It defines geomorphology as the study of landforms and discusses how landforms are shaped by tectonic and hydrologic processes. Early theories that invoked supernatural causes are contrasted with modern theories of uniformitarianism and plate tectonics. The roles of various controlling factors - including geomorphic agents, surficial materials, tectonic setting, and climate - are examined. Different types of crustal features like continents, mountain belts, shields, and continental shelves are also introduced.
Glaciers form from accumulated snow that undergoes recrystallization into ice. They flow via gravity from accumulation zones where snowfall exceeds melting to ablation zones where melting exceeds snowfall. Glaciers powerfully erode, transport, and deposit sediment. They carve U-shaped valleys and leave behind landforms like moraines, drumlins, eskers and kettle lakes. Glaciers shape mountain and coastal landscapes through erosion and deposition.
The document discusses 10 key concepts in geomorphology. It begins by defining geomorphology as the study of landforms and their formation and development. It then explains each concept in 1-2 paragraphs with examples. The concepts are: 1) Uniformitarianism, 2) Role of geologic structure, 3) Differential erosion rates, 4) Distinct landforms from geomorphic processes, 5) Geomorphic cycles, 6) Complex geomorphic evolution, 7) Young topography, 8) Impact of Pleistocene climate change, 9) Role of climate on processes, 10) Historical approach. The document concludes with a quick review of the 10 concepts.
Stream capture, also known as river capture or stream piracy, is the process where a river or stream redirects its flow and starts flowing into another river's drainage basin instead of continuing into its own basin. This can occur where two drainage basins are separated by an erosion-resistant divide that is breached by headward erosion of one of the streams. Once the divide is breached, the stream will capture the tributaries of the neighboring basin and divert its entire flow into the new course. Stream capture events can result in changes to drainage patterns over time.
The document summarizes the tectonic framework of India in 3 broad divisions - Peninsular India, Extra-Peninsular India, and the Indo-Gangetic Plain. Peninsular India comprises the Indian shield and its sedimentary basins, and is further divided into the shield areas, mobile belts, and Proterozoic sedimentary basins. Extra-Peninsular India includes the Himalayan mountain ranges, divided into the Lesser Himalayan zone, Central Crystalline zone, and Tethyan zone. The Indo-Gangetic Plain is a deep crustal trough in northern India filled with Quaternary sediments.
Orogenesis is the process of mountain building that occurs during an orogeny. An orogeny involves tectonic processes like subduction and plate convergence that cause deformation and metamorphism of the Earth's crust, forming orogenic belts made of parallel rock structures. Orogenies can take tens of millions of years to build mountains and are associated with the development of foreland basins in front of the growing mountain range.
This document discusses different types of drainage patterns that can form based on topography, geology, climate, and other factors. It describes dendritic, trellis, rectangular, radial, parallel, and annular drainage patterns. The dendritic pattern resembles a tree branch and forms in impervious rock. The trellis pattern has tributaries joining at right angles and forms in folded mountains with parallel hard and soft rocks. The rectangular pattern forms in uniformly resistant and jointed rocks. The radial pattern has streams radiating outward from a central high point. The parallel pattern has straight, swift streams along resistant rock bands with few tributaries. The annular and centripetal patterns form rings around structural domes or basins. Combinations of
1. Drainage patterns are formed by the networks of streams, rivers, and lakes within a drainage basin and are influenced by the topography and geology of the land.
2. The most common drainage pattern is dendritic, where many small streams feed into larger tributaries and ultimately the trunk river. Dendritic patterns form in V-shaped valleys in impermeable rock.
3. Other drainage patterns include parallel, trellis, rectangular, radial, centripetal, annular, and angular - each forming under different geological conditions and rock structures. Discordant drainage does not correlate to the underlying geology.
Concept 1. The same physical processes and laws that operate today operated throughout geologic time, although not necessarily always with the same intensity as now.
Concept 2. Geologic structure is a dominant control factor in the evolution of land forms and is reflected in them.
River rejuvenation occurs when a river's base level changes, altering the gradient of the river channel and increasing its erosive power. This causes the river to cut downward into its channel, forming landforms such as waterfalls, incised meanders, and river terraces. Changes in base level are typically caused by isostatic adjustments to sea level from glacial rebound or eustatic sea level changes.
The document discusses several landforms that can result from river rejuvenation caused by a fall in sea level. Knick points form as steps where the river erodes downward to adjust to the new base level, and may create waterfalls. River terraces are abandoned floodplains left at higher levels after the river cuts down through deposits. Incised or enclosed meanders develop when the river maintains its meandering pattern while increasing vertical erosion.
Rivers over long periods of time develop a smooth, concave long profile as they adjust their characteristics to transport water and sediment in a state of dynamic equilibrium with their environment. However, occasional events can destabilize this equilibrium, increasing the river's energy and causing it to actively erode its channel to reestablish its optimal long profile through a process called rejuvenation. Common causes of rejuvenation include changes in base level from tectonic uplift or changes in sea level. During rejuvenation, landforms such as waterfalls from knickpoints, incised meanders, and river terraces may form as the river adjusts to its new gradient.
Streams are smaller bodies of water with a current, while rivers are larger. They are part of a watershed - the area where all water drains. Streams join to form rivers and eventually drain into oceans, lakes, or other bodies of water. Rivers and streams have upper, middle, and lower courses. Organisms in rivers and streams have adaptations like streamlined bodies to deal with currents. Human impacts like dams, channelization, and urbanization disrupt natural river flows and habitats.
Base level is the lowest level to which erosion by running water can take placeKennyboo Brown
Base level is the lowest point a river can erode down to, usually sea level. Changes in base level, from climate or tectonic activity, impact the river valley. A positive change, like rising sea levels, decreases the gradient and causes more deposition, flooding lower areas. A negative change, from falling seas or uplifting land, steepens the gradient and increases erosion rates, rejuvenating the river and creating features like knickpoints and terraces as the river adjusts its profile.
This document discusses strategies for engaging boomer volunteers and adapting volunteer programs. It notes that boomers expect to work past 65 and see retirement as a time for renewal rather than rest. To attract boomers, volunteer opportunities should offer flexibility, a variety of options, engage skills and expertise, and show impact. Meeting structures should move from committees to task forces and project teams. Leadership teams are recommended over boards to provide strategic planning and action. The document provides examples of developing project teams for a membership drive and author event fundraising. It stresses evaluating projects, continuous support for volunteers, and database management.
Geography as revision rivers floods and managementklaudia666
The document discusses key concepts related to physical geography and river flooding. It defines important terms like precipitation, infiltration, overland flow, and hydrographs. It describes the hydrological cycle within a drainage basin and factors that influence flooding, like vegetation, geology, and urbanization. Engineering strategies for flood management are outlined, including soft techniques like reforestation and hard techniques like dams and flood relief channels. Case studies on flooding in Hull, China, and Tewkesbury analyze both physical and human causes and impacts.
Rivers shape the landscape through three main functions: erosion, transportation, and deposition. Erosion occurs via abrasion, attrition, hydraulic action, and solution as a river carries rock and sediment in its flow. Transportation involves traction, saltation, suspension, and solution of materials. Deposition happens when a river's volume or speed decreases as it enters areas like lakes, seas, or plains with gentler slopes. A river's erosional and depositional work depends on its energy, which relates to its volume, flow speed, and gradient of the land.
The document discusses strategies for achieving work-life balance. It begins by outlining common signs of an imbalance like working late hours, feeling stressed or tired due to work responsibilities. It then describes five "dying stages" that can result from being "married to your work", including exhaustion, suffering family and friends, and increased expectations. Several solutions are proposed, such as making lists, being flexible, learning to say no, leaving work at the office, managing time, communicating clearly, and setting aside time for recreation and self-care. The key message is that creating balance is an ongoing process that requires periodically reassessing one's priorities and routines.
As more skilled workers enter the global labor market and companies outsource jobs, employees feel increased pressure to work longer hours and take on more work to protect their jobs. Advances in technology allow people to work anywhere and be available around the clock. Employers commonly require overtime work which can negatively impact employees' physical and mental health as well as their personal lives by causing them to miss important family events. To achieve a better work-life balance, employees should track their time use, communicate clearly with their employers about scheduling needs, set boundaries between work and personal time, prioritize self-care, and leverage social support systems during stressful periods.
The document discusses work-life balance and its importance. It defines work-life balance as the ability to be productive at work while maintaining a happy home life with leisure time. It then discusses six components of achieving work-life balance: self-management, time management, stress management, change management, technology management, and leisure management. The document also discusses causes of imbalance like work pressure and stress, and consequences like health risks, absenteeism, and burnout. Finally, it discusses responsibilities of employers in helping employees achieve better balance through options like telecommuting, job sharing, and flexible scheduling.
This document discusses work-life balance and solutions for achieving it. It begins by defining work-life balance and noting that over 60% of respondents feel unable to balance their personal and professional lives. Competition, career ambitions, and long work hours are cited as reasons for the imbalance. The document then outlines HR solutions like flexible work schedules, family-oriented activities, and leave policies. It discusses benefits like increased productivity, commitment, and reduced stress for both organizations and individuals. Finally, it emphasizes finding the right balance through setting boundaries and priorities.
The Praying Indian town of Megunko in what is now Ashland Massachusetts played a key role in the events and outcome of King Philip's War. This presentation looks at the background of the geographic area, the activity of Rev. John Eliot, and the heroes and villains from Megunko during King Philip's War.
PHP Apps on the Move - Migrating from In-House to Cloud RightScale
RightScale Conference NYC 2012 -- PHP Apps on the Move - Migrating from In-House to Cloud
Kent Mitchell - Sr. Director, Product Management, Zend
It’s a common problem: How to move your PHP system to the cloud without completely overhauling your app. Most existing systems and applications were not designed for the level of elasticity the cloud brings. But many of those apps can still take advantage of all that the cloud offers - while requiring very few modifications.
In this session, we will discuss how one customer leveraged the off-the-shelf capabilities of RightScale and Zend to migrate from a fixed, non-scalable traditional architecture to an elastic, high-availability cloud architecture. Join us for a deeper look at this auto-scaling PaaS solution specifically designed to make it easier for you to deploy and manage cloud-based, highly available PHP server clusters.
The document provides an overview of the Ngaanyatjarra Pitjantjatjara Yankunytjatjara Women’s Council (NPYWC), including its origins, aims to support Aboriginal women and communities in the central desert region, key functions such as advocacy and service delivery programs, organizational structure, and strategic planning processes to guide its work.
The document provides examples of simple past tense verbs in English. It lists affirmative and negative examples of common past tense verbs like "watch", "visit", "play", and "walk". It also provides yes/no question examples using "Did". Finally, it lists common past time expressions like "yesterday", "last week", and "last year" and provides additional verb examples like "study", "eat", "exercise", and "read".
Li & Fung Ltd is a global supply chain company founded in 1906 in Guangzhou, China that coordinates product design, sourcing, production, and quality assurance for major retailers. It has expanded to over 26,000 employees working across 40 countries with a network of over 15,000 suppliers. The company pioneered the philosophy of managing global supply chains and allowing customers to source products closer to various markets. It performs higher value tasks like design and quality control in Hong Kong while outsourcing lower value production to optimal locations around the world.
HTML5 is well-suited for the iPad as it does not require Flash and offers features like CSS3, DOM manipulation, SVG, and Canvas. The document discusses the history of HTML5 and how it emerged as an alternative to Flash. It also covers some of the technical challenges of developing for the iPad like video playback, DOM performance, and leveraging new APIs. Overall, HTML5 is positioned as providing many benefits for building applications for the iPad without Flash.
The document discusses the benefits of meditation for reducing stress and anxiety. Regular meditation practice can help calm the mind and body by lowering heart rate and blood pressure. Making meditation a part of a daily routine, even if just 10-15 minutes per day, can offer improvements to mood, focus, and overall feelings of well-being over time.
This document outlines key features of river erosion and river systems. It begins with a longitudinal profile diagram showing how a river's gradient is steepest at the headwaters and gentlest near the base level. It then discusses drainage patterns like dendritic and trellis. Common river features like meanders and waterfalls are also explained. The document covers the erosional work of rivers through processes like abrasion and hydraulic action. Methods of sediment transportation like suspension and traction are outlined. Stages in river development from youthful to mature to old age are also summarized.
Running water is the most powerful natural agent of erosion. It acts almost everywhere on Earth, carrying rock fragments and breaking down the crust through hydraulic action and abrasion. Streams and rivers form complex drainage systems that collectively drain precipitation from drainage basins. As rivers flow from their headwaters to their mouths, their profiles evolve from steep slopes with deep valleys and gorges to flatter slopes with more deposition. Various landforms such as waterfalls, terraces, and canyons are created through the erosive processes of running water.
Floodplains develop alongside rivers and are subject to periodic flooding. As rivers mature from steep mountain streams to slow, meandering plains rivers, they develop floodplains marked by features like natural levees, backswamps, and oxbow lakes formed from river meanders. Flooding deposits sediment across the floodplain but slows closer to the river, building up levees. Meanders may eventually be cut off, forming oxbow lakes. While flooding is natural, it can be hazardous to human development, so structures like dams, levees, flood walls, and bypasses are used to control floodwaters.
This document discusses river rejuvenation and the landforms it produces. River rejuvenation occurs when a river's base level changes, such as due to sea level change or glacial isostatic adjustment. This decreases the river's gradient, increasing its erosional power. Key landforms produced include waterfalls, incised meanders, river terraces, and knickpoints as the river grade is adjusted to the new base level.
This document discusses river landforms and processes. It begins with a longitudinal profile diagram showing how a river's gradient is steepest at the headwaters and gentlest near the base level. It also includes diagrams of drainage patterns and stream order. Common river features are described such as meanders, floodplains, levees, and the formation of ox-bow lakes. The four main methods of river erosion and three methods of sediment transportation are defined. River landforms like waterfalls and pot holes are also examined. The document concludes with descriptions of the different stages in river development from youth to maturity.
The document describes various fluvial landforms found in the upper course of a river. Vertical erosion dominates and produces V-shaped valleys with interlocking spurs. Rapids and waterfalls form where the gradient suddenly increases, such as at bands of harder rock. Potholes are eroded by spinning pebbles in eddies and widen/deepen through abrasion. Braided channels occur where rivers carry large sand/gravel loads that deposit as shifting bars and islands, dividing the channel.
The document describes various fluvial landforms found in the upper course of a river. Vertical erosion dominates and produces steep V-shaped valleys with interlocking spurs. Rapids and waterfalls form where the gradient suddenly increases, such as at bands of resistant rock. Potholes are formed by abrasion of pebbles rotating in eddies, deepening and widening holes in the rock. Braided channels occur where rivers carry large loads of sediment that deposit as shifting bars and islands, dividing the channel.
The document discusses drainage basins, the storm hydrograph, river erosion processes and landforms, flooding causes and impacts, and flood management strategies. It describes the hydrological cycle within a drainage basin and factors that influence the shape of a storm hydrograph. It outlines river erosion mechanisms and key landforms in the upper, middle and lower courses such as potholes, waterfalls, meanders, and deltas. Causes of flooding include excessive rainfall and development that increases runoff. Impacts are economic, social and environmental. Flood management includes hard and soft engineering approaches.
As a river flows from its source to its mouth, changes take place in its morphology and landforms. In the upper course, waterfalls and rapids form where the gradient suddenly changes. Potholes are carved by turbulent water. Meanders develop from sediment bars and cause lateral stream migration. Oxbow lakes are left when meanders are cut off. In lowlands, flooding leads to levees, floodplains and deltas where deposition exceeds removal of sediment at the river's mouth. A variety of landforms result from erosion and depositional processes along a river's course.
Work's of river, winds, seas and their Engineering ImportanceJohnCarloEdejer
The document summarizes key concepts regarding rivers, wind, and seas and their engineering importance. It describes rivers' erosion, transportation, and deposition functions according to Playfair's Law. It discusses the juvenile, mature, and old stages of river development. It also explains wind erosion through deflation and abrasion and deposition of sediments like sand dunes and loess. Finally, it briefly discusses seas and oceans and the formation of shorelines.
Running water is the primary agent of erosion on Earth's surface, though its role is limited in some glaciated and desert areas. Streams erode through processes like abrasion, attrition, solution, and hydraulic action. As they flow downhill, their kinetic energy is used to transport sediment in suspension, saltation, traction, or solution. When the stream's energy decreases, such as when entering flatter terrain, sediment is deposited in features like point bars, floodplains, levees, meanders, and deltas. Meanders may be cut off over time, forming oxbow lakes.
The document describes the journey of the River Tees from its source in the Pennines to its mouth in the North Sea. It discusses the landforms and processes along the upper, middle, and lower courses of the river. In the upper course, erosion is the main process and landforms include High Force waterfall and gorge formed by the erosion of softer rock from under hard cap rock. Meanders, ox-bow lakes, and levées are formed in the middle to lower courses as erosion gives way to deposition. The river's estuary at its mouth was formed by rising sea levels after the Ice Age.
This document discusses various geological processes and landforms resulting from physical geology. It covers the geological work of rivers including erosion, transportation, deposition and various fluvial landforms. It also discusses the geological work of other agents like wind, groundwater and oceans. Rivers can erode, transport and deposit sediment, forming features like drainage patterns, valleys, waterfalls and terraces over long periods of time. Wind erosion can form dunes and loess deposits, while groundwater can dissolve rock to form sinkholes, caves and valleys. Oceans also erode, transport and deposit material along coastlines.
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.
Streams erode, transport, and deposit sediment as they flow downhill. Their patterns are controlled by geology and climate. Meandering streams form point bars on inside bends as faster flow on outsides erodes the banks. During floods, sediment is deposited in floodplains and deltas form where streams enter standing water. Over geological time, streams deepen valleys and widen them through lateral erosion.
Rivers go through three stages as they flow from their source to the sea - youthful, mature, and old. In the youthful stage, the fast-moving river erodes the landscape, creating V-shaped valleys, interlocking spurs, and waterfalls. During the mature stage, the river transports eroded material and deposits it, forming wider valleys, meanders, and flood plains. In the slow-moving old stage, deposition creates features like ox-bow lakes, levees, and deltas at the river's mouth. Rivers have long been important to people for transportation, water, and more recently, power generation through hydroelectric dams.
Sea level change can occur through two main processes: isostatic and eustatic. Isostatic changes are local and caused by land height changes, while eustatic changes are global and caused by ocean water volume changes. During ice ages, water is stored in glaciers causing eustatic sea levels to drop; melting then causes levels to rise. Coastlines can emerge from isostatic uplift or submerge through subsidence. Emergent coasts may have raised beaches and cliffs, while rias and fjords form in submerged areas. Sea level changes impact coastal ecosystems and infrastructure through flooding and erosion.
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Rivers have distinct features along their upper, middle, and lower courses. In the upper course, the river flows through a V-shaped valley with steep sides, eroding vertically. Meanders begin to form in the middle course as the river erodes more horizontally and widens the valley floor. In the lower course, the river flows through a wide, flat floodplain with features like oxbow lakes formed from abandoned meander loops.
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.
This presentation is a cool resource for doing river revision, especially if you are doing A-levels in Geography.
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Rejuvenation presentation
1.
2. Rejuvenation
Definition = Rejuvenation is the renewal of a
river’s energy in response to a relative fall in
base level.
Rivers are always attempting to reach a
state of dynamic equilibrium* where
erosion, deposition & transportation
are in perfect balance.
3. Base level
• Dynamic & eustatic change affect the base level
of a river.
• This is the lowest point to which a river can flow
& erode (usually sea level)*
• Local base level occurs when a river meets a
larger river, reservoir or lake
5. 1. Dynamic change
• Involves an upward movement of the land
raising the height of the river above sea
level (base level).
• This alters the long profile of the river,
increases the gravitational potential of the
river and therefore increases the energy
available (to erode and transport material)
6. Dynamic change
Why does the land rise?
• Orogenesis (Mountain building)
Compression from plate movement at convergent
boundaries builds mountains (eg. Alps, Andes,
Himalayas). Resultant uplift (usually along fault lines)
raises river (relative to base sea level), steepens river
gradient, and increases energy.*
7. Dynamic change
Why does the land rise?
• Isostatic rebound
18000 years BP (the last glacial maximum*) ice sheets covered
much of the northern & southern land masses.
The weight of this ice was enough to depress the crust beneath.**
The mantle aesthenosphere flowed away under this pressure.
The melting of the ice sheets (10000years BP) removed this
weight. The mantle flowed back & caused uplift. *** This
rejuvenated rivers as they rose up with the land. Its still happening!
8. 2. Eustatic change
Eustatic changes affect the volume of water in the oceans.
• This fits to rejuvenation as an actual fall or rise in global
sea level or base level, linked directly to the temperature
of the Earth.
• In warmer periods there is less ice and the water is
warmer, so expands and sea levels rise.
• In colder periods the ocean water is
colder so contracts and sea levels fall. *
9. How does rejuvenation affect
rivers?
The restart of erosion and reduction in
deposition, provoked by a fall in base
level, leads to the formation of landforms
that would not ‘normally’ be found in rivers.
11. Eustatic effects (landforms)
• Sea level fall = raised beaches, abandoned cliffs,
erosion surfaces created at the coast, and adjustments
made to river valleys:
• Knick points & waterfalls
• River terraces
• Incised & entrenched meanders
These occur as the river attempts to regrade its
long profile to a normal concave shape.
12. Knick Points
• A sudden break or irregularity in the long profile
of a river. Can be sharply defined, (such as
waterfalls) or barely noticeable.
• Erosion at the mouth of the river cuts down into
the land and slowly cuts the profile down to sea
level (base level) from the mouth and
subsequently upstream.
• Knick point is the point at which this process has
reached upstream.*
14. The waterfall at Glen Maye, Isle of Man
This
waterfall on
the
rejuvenated
Rushen river
has been
formed as a
result of the
uplift of the
west coast
of the island
post
glaciation.*
15. River terraces near Kasbeki,
(Caucasus) Georgia
• A river terrace is a remnant of
a former floodplain which has
been abandoned at a higher
level due to renewed
downcutting of a river.
• The terraces will be cut back
as the new valley is widened
by lateral erosion.
• This process may be repeated
a number of times leading to
terraces at a number of levels.
• Terraces provide useful shelter
from floods and are ideal as
natural route ways for road and
rail.
16. Incised Meanders
(NB: These may be entrenched or ingrown)
• If a rejuvenated river
occupies a valley with
well developed
meanders, renewed
downcutting results in
them becoming incised
(deepened).
• If incision is rapid, the
valley will be symmetrical
with steep sides and a
gorge like appearance –
this is known as an
entrenched meander.
The city of Durham and its ‘Bailey’
colleges, ‘trapped’ within this
entrenched meander on the River
Wear.
17. Entrenched Meanders
San Juan River, southeastern Utah
The Goosenecks of the
San Juan River in
southeastern Utah are
textbook examples of
entrenched river
meanders, where a lazy
meandering river was
"trapped" as the
surrounding plateau (the
Monument Upwarp) rose
up over millions of years
while the canyon kept
cutting down.
18. Ingrown Meanders
• When incision is slower and more lateral
erosion is occurring, an ingrown meander
may be produced.
• The valley becomes asymmetrical, with
steep cliffs on the outer bends and more
gentle slip-off slopes on the inner bends.
19. Ingrown Meander on the River
Wye, Tintern Abbey
(Note the asymmetrical valley profile)
River Cliff
Slip-off slope
20. 3. Static change
• Not linked to base level change.
• These are the result of the river’s ability to
erode more due to :
– Changes in load transported by the river
– Increase in discharge due to increased rainfall
– Increased discharge through river capture
21. Static change – changes in load
• In glacial times meltwater streams carried large
volumes of material and deposited them in wide
open valleys.
• Huge discharge and large volume of
unconsolidated debris meant deposits grew
high.
• Post glaciation, deposits fell & rivers’ energy
could be re-deployed for eroding.*
• The lack of load enabled valleys to be slowly
eroded – cutting through the deposits**
22. Static change – increase in discharge
• Climate change may bring increased discharge
• Increased precipitation or rivers merging could
link to a progressive lowering of the long profile
• Additional flow brings additional energy which
resulting in greater erosion and deposition
23. Ok, that’s it – now you really do
know all about rivers!