river delta impact (For Geography)
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The document describes the formation of deltas. As a river reaches the sea, it deposits sediments, building up the river mouth and causing the river to split into distributaries. Over time, accumulated sediments rise above the water level, forming a delta where the river meets the sea. It also discusses how meanders form through a river's winding course as it seeks to avoid obstacles at a low gradient, eroding the outer concave bank and depositing sediments to form slip-off slopes on the inner convex bank. Rivers provide benefits like water and food but can also negatively impact people through flooding and spreading disease.
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River Changes And Landforms
The document provides information about river characteristics and landforms. It describes key features of drainage basins such as tributaries, watersheds and confluences. It explains the changes that occur along a river's long profile from upper to middle to lower course, including differences in gradient, erosion processes and landforms. Specific features of the upper course like interlocking spurs and waterfalls are also outlined. The formation of meanders and oxbow lakes in the middle course through erosion and deposition is detailed.
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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.
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River Landform
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.
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The drainage pattern shown is dendritic. A dendritic drainage pattern occurs in regions where the underlying rock is uniform in its resistance to erosion. It resembles the branching pattern of a tree, with many small tributaries that join together into larger streams and rivers, eventually converging to a single outlet. The branching tributaries meet the main rivers at acute angles. This type of drainage pattern suggests an underlying topography that has a uniform resistance to erosion, allowing the drainage network to develop evenly in all directions without being controlled by the geology.
Geography fluvial landforms
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.
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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.
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The document discusses river channel processes and landforms, including:
1. River processes like erosion, transportation, and deposition shape landforms through sediment movement.
2. Velocity and discharge impact a river's ability to erode, transport, or deposit materials based on the Hjulström curve.
3. Meanders, floodplains, and deltas are examples of landforms formed by fluvial erosion and deposition that impact human settlements.
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This document provides information about river drainage basins. It discusses how drainage basins are defined as the area of land drained by a river and its tributaries. Key points include:
- Rivers flow downhill from highland source areas through three main sections - the upper, middle and lower courses.
- The boundaries of the drainage basin are defined by watershed areas of high land.
- As the river flows downstream, its characteristics change with width, depth, and volume increasing.
- Common exam questions involve locating features on diagrams of river basins and explaining river landforms and processes like erosion and transportation of material.
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genghis khan
Temujin was born around 1165 in Mongolia and later became known as Genghis Khan. As a child, his father was poisoned and he became the chief of his tribe. By 1205, through forming alliances and organizing an army with strict discipline, he had vanquished all rivals. The following year, he was proclaimed Chinggis Khan and united the steppe tribes under one nation. As ruler, Genghis Khan established laws and policies to suppress causes of warfare between tribes and granted religious freedom. Through his military strategy and tactics, he went on to conquer much of Eurasia over the next two decades, creating the largest contiguous land empire in history.
Delta
1. Deltas form where rivers enter bodies of standing water, depositing large amounts of sediment. They are common features where large rivers meet the ocean.
2. Deltas consist of a delta plain, delta front, and prodelta. The delta plain is the subaerial region with distributary channels, the delta front is the shallow underwater region where mouth bars form, and the prodelta is the deepest region where fine sediments settle out.
3. Deltas are classified based on dominant hydrodynamic processes, including river-dominated, tide-dominated, and wave-dominated deltas which have characteristic morphologies and sedimentary structures.
Genghis khan and_mongols
Genghis Khan united the Mongol tribes and built a vast empire through conquest. He was tolerant of different religions and his military strategies of feigned retreat and attacks on horseback allowed him to defeat larger armies. After his death, the Mongol Empire continued expanding under other leaders but grew too large to manage and eventually fractured into khanates. The empire had both positive impacts like increased trade and negative ones as many regions suffered destruction from Mongol invasions.
Genghis Khan
Genghis Khan was born in 1162-1167 in Mongolia and became a powerful tribal leader and king. He united the nomadic tribes of Northeast Asia and created the largest contiguous empire in history. Genghis Khan was a fierce warrior who conquered many lands through military victories but also established schools, cities, and shared his wealth with his people. He is still remembered today through monuments, places named after him, and for transforming Mongolia into a major power.
The Formation Of A Waterfall
AS-Level Geography description of how a waterfall is formed with diagrams and a case study. Step-by-step formation.
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Similar to river delta impact (For Geography)
Fresh Surface Water
Lakes are inland bodies of water formed in depressions where water collects. They are formed through processes like diastrophism, glacial action, and volcanic activity. Lakes provide many benefits like transportation, water storage, hydroelectric power, and recreation. Specific types of lakes include kettle lakes formed in depressions left by melting glaciers, tarn lakes in mountain hollows, and volcanic lakes that form in volcanic craters. Oxbow lakes form from river meanders that are cut off. Swamps occur in low-lying areas and transition between lakes and dry land depending on the season. Rivers are natural freshwater streams that flow towards seas, lakes or other rivers. Meltwater from glaciers feeds streams
Unit 12 River training work.pdf
Rivers carry large amounts of water and sediment. They can be classified based on their topography into upper reach rivers flowing through hills, lower reach rivers flowing through flood plains, and tidal rivers. River training works are constructed to guide and confine river flows, control river beds, and ensure safe flood passage. Methods for river training include embankments/levees, guide banks, groynes, cutoffs, and pitched islands. Guide banks are constructed in pairs to create a waterway and prevent structures from being outflanked by the river.
Sec 2 rivers 2013
Rivers are formed through the hydrological cycle as precipitation falls and flows over land towards the sea. A river's features include its source, mouth, drainage basin, and tributaries. Waterfalls form through erosion of rocks of varying resistance. Meanders form as rivers curve to avoid obstacles, eroding cliffs on outer banks and depositing slip-off slopes on inner banks. Floodplains and levees develop from sediment deposition during floods, with coarser sediments forming raised levees and finer sediments creating flat floodplains. Deltas form at river mouths as sediments accumulate and cause the river to split into distributaries. While rivers provide water and transportation, overflowing can damage property and contaminated water risks disease.
Sec 1 Exp - River System & Drainage
The document discusses key features and processes of river systems, including that a river's drainage basin is the area of land drained by the river and its tributaries, waterfalls form when a river flows over harder and softer rocks at different rates, and sediments deposited at river mouths over time can create deltas with distributaries.
Sec 1 NA - River system & drainage
The document discusses key features and processes related to river systems, including the drainage basin, tributaries, confluence, watershed, waterfalls, meanders, and river mouths. It explains that a river's drainage basin is the area that drains into the river and its tributaries, and that waterfalls form when a river flows over mixed hard and soft rocks, eroding the soft rocks more quickly to form a ledge. It also describes how river meanders and oxbow lakes are formed by rivers and that sediments deposited at river mouths over time create deltas with distributaries.
Lesson plan 13 running water
This document discusses various landforms created by rivers, including V-shaped valleys, canyons, waterfalls, flood plains, meanders, ox-bow lakes, and deltas. It provides definitions and examples of each landform. Experiments are suggested to observe water flow and erosion. Jog Falls in Karnataka is provided as an example of the largest waterfall in India. The document concludes with review questions about jog falls and ox-bow lakes, as well as a suggestion for a follow up activity to create a picture album of river landforms.
River erosion
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.
Depositional landforms
Floodplains form along river banks when flooding deposits sediment. Levees are natural embankments of coarser sediment deposited along river banks during floods. Braided rivers divide into small streams separated by islands of deposited gravel and sand within the channel. Deltas are flat lands formed of sediments deposited at river mouths, with distributaries transporting sediment into the sea.
Environment engineering
The primary source of water on Earth is precipitation. Most precipitation infiltrates into the ground and joins groundwater sources, or runs off into surface water sources like rivers, lakes, and reservoirs. The main surface water sources are rivers, streams, lakes, ponds, and impounding reservoirs. The main groundwater/subsurface sources are springs, infiltration galleries, infiltration wells, and dug or tube wells. Rivers are the most important sources of water supply since they provide large quantities of water throughout the year. Storage reservoirs created by dams are also important since they can regulate water supplies.
Running water-Geomorhology Chapter
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.
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.
Presentation (2)
In the upper course of a river, the river flows swiftly and forms valleys and waterfalls. As the river enters the plains, it moves more leisurely and forms broad S-shaped meander loops and curves due to irregularities in the ground surface. Over time, ox-bow lakes may form when meander loops are cut off from the main river channel. Distributaries form near the river's mouth when sediment buildup blocks the main channel and forces the river to divide into branches, as typically seen in river deltas emptying into the sea.
GEOLOGY.pptx
Runoff occurs when rainwater or snowmelt causes soil to become saturated and unable to absorb more water. Excess water flows as runoff. Gullies form when running water erodes soil, creating ditches or small valleys, especially in hilly areas. Streams are surface waters that flow in channels and are part of the water cycle. Tributaries are rivers that flow into larger rivers or lakes but not the ocean. Rivers differ from tributaries in that they ultimately drain into oceans or seas and typically contain larger volumes of water. Waterfalls form when water falls from a height due to differences in rock resistance and topography. Flood plains are flat lands adjacent to rivers that experience periodic flooding. Meanders are
River 2 waterfall plungepools floodplain n levees
Waterfalls form over time as river water erodes less resistant rock more quickly than more resistant rock, causing the river gradient to change. This leads the river to plunge from a great height, forming a waterfall. Repeated pounding of the river bed at the base of waterfalls creates depressions known as plunge pools. Floodplains are formed along river banks during heavy rainfall as the river's energy decreases and deposits sediments, with coarser sediments accumulating into raised banks called levees and finer sediments creating flat plains further from the river.
Relief
This document discusses different types of landforms on Earth including continental and oceanic relief. It describes how tectonic plates move and collide, forming three main types of plate boundaries. It also explains key landforms shaped by rivers, glaciers, groundwater and lakes. Coastal landforms like cliffs, beaches and estuaries are presented. The document emphasizes how plate tectonics and erosion by water have created the diverse surface features visible around the world today.
GEOGRAPHY IGCSE: RIVER LANDFORMS
This document summarizes the key landforms found in the upper, middle, and lower courses of a river. In the upper course, steep valleys and gorges form due to erosion. Meanders and oxbow lakes develop in the middle course as the gradient decreases. The lower course features wide floodplains and deltas, where deposition exceeds erosion at the river's mouth.
13.4 Stages of a River.ppt
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.
River Landforms
This document discusses rivers and associated landforms. It describes how rivers shape the landscape through erosion and deposition. A river system is divided into three subsystems: the collecting system of tributaries, the transporting trunk stream, and the dispersing distributary network at the river's mouth or delta. Common landforms created by rivers include alluvial fans at mountain bases where sediment is deposited, braided channels in steep areas, meandering patterns on floodplains, and deltas where rivers enter standing bodies of water.
River landforms in middle and lower courses, meanders and oxbow lakes
this is a ppt about two river landforms, meanders and oxbow lakes. In this ppt you can you can find explanations how these two river landforms form and in which part of the river you can find them.
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.
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River landforms in middle and lower courses, meanders and oxbow lakes
River landforms in middle and lower courses, meanders and oxbow lakes
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Mr. Brainwash Beautiful Girl / Mixed Media / signed / Unique
Year: 2023
Format: 96,5 x 127 cm / 37.8 x 50 inch
Material: Fine Art Paper with hand-torn edges.
Method: Mixed Media, Stencil, Spray Paint.
Edition: Unique
Other: handsigned by Mr. Brainwash front and verso.
Beautiful Girl by Mr. Brainwash is a mixed media artwork on paper done in 2023. It is unique and of course signed by Mr. Brainwash. The picture is a tribute to his own most successful work of art, the Balloon Girl. In this new creation, however, the theme of the little girl is slightly modified.
In Mr. Brainwash’s mixed media artwork titled “Beautiful Girl,” we are presented with a captivating depiction of a little girl adorned in a summer dress, with two playful pigtails framing her face. The artwork exudes a sense of innocence and whimsy, as the girl is shown in a dreamy state, lifting one end of her skirt and looking down as if she were about to dance. Through the use of mixed media, Mr. Brainwash skillfully combines different artistic elements to create a visually striking composition. The vibrant colors and bold brushstrokes bring the artwork to life, evoking a sense of joy and happiness. The attention to detail in the girl’s expression and body language adds depth and character to the piece, allowing viewers to connect with the young protagonist on a personal and emotional level. “Beautiful Girl” is a testament to Mr. Brainwash’s unique artistic style, blending elements of street art, pop art, and contemporary art to create a visually captivating and emotionally resonant artwork.
The use of mixed media in “Beautiful Girl” adds an additional layer of complexity to the artwork. By combining different artistic techniques and materials, such as stencils, spray paint, and collage, Mr. Brainwash creates a dynamic and textured composition that grabs the viewer’s attention. The juxtaposition of different textures and patterns adds depth and visual interest to the piece, while also emphasizing the artist’s eclectic and experimental approach to art-making. The inclusion of collage elements, such as newspaper clippings and torn posters, further enhances the artwork’s urban and contemporary feel. Overall, “Beautiful Girl” is a visually captivating and thought-provoking artwork that showcases Mr. Brainwash’s talent for blending different artistic elements to create a truly unique and engaging piece.
Tanjore Painting: Rich Heritage and Intricate Craftsmanship | Cottage9
Explore the exquisite art of Tanjore Painting, known for its vibrant colors, gold foil work, and traditional themes. Discover its cultural significance today!
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The basics of photography in the environment
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8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
【关于价格问题（保证一手价格）】
我们所定的价格是非常合理的，而且我们现在做得单子大多数都是代理和回头客户介绍的所以一般现在有新的单子 我给客户的都是第一手的代理价格，因为我想坦诚对待大家 不想跟大家在价格方面浪费时间
对于老客户或者被老客户介绍过来的朋友，我们都会适当给一些优惠。
➒➌➎➏➑➐➋➑➐➐ Satta Matka Dpboss Matka Guessing
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Dpboss Matka Guessing Satta Matta Matka Kalyan panel Chart Indian Matka Dpbos...
Dpboss Matka Guessing Satta Matta Matka Kalyan panel Chart Indian Matka Dpbos...
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Dpboss Matka Guessing Satta Matta Matka Kalyan panel Chart Indian Matka Dpbos...
Dpboss Matka Guessing Satta Matta Matka Kalyan panel Chart Indian Matka Dpbos...
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Dpboss Matka Guessing Satta Matta Matka Kalyan Chart Indian Matka
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river delta impact (For Geography)
- 1. Formation of Delta • At the river mouth, a river loses energy and starts to deposit its sediments.
- 2. Formation of Delta • As the sediments build up, the mouth will be blocked • The river also split into several small channels called distributaries to flow to the sea.
- 3. DistributariesDelta Over time, the accumulated sediments that rise over the water and the distributaries form a delta.
- 4. Meander • A river that follows a winding course, usually forming hoop-like bends. • River may meander because Lower gradient lower speed lower river energy river turns to avoid obstacles
- 5. Meander Note: Outer Bank = Concave Bank Note: Inner Bank = Concave Bank
- 6. River Cliff • Constant erosion (undercutting) erodes the outer (concave) bank of the meander • forming a river cliff. Slip-off slope River cliff
- 7. Slip-off slope • Constant deposition at the outer (convex) bank deposits sediments • forming a slip- off slope. Slip-off slope River cliff
- 8. Positive Impact of river • Rivers provide water for domestic purposes such as drinking, bathing and washing. • Rivers are a good source of food such as fish and prawns.
- 9. Positive Impact of river • Rivers are important waterways for transporting people and goods.
- 10. Negative Impact of river •River water overflows river bank cause lives to be lost and destroy property and crops.
- 11. Negative Impact of river • Consuming contaminated river water can cause people to fall ill • Eg contract diseases such as cholera.