The River Journey (Years 3-4)_G2PAT15.ppsx
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The document describes a journey down a river from its source to the sea. It divides the river into three sections - the upper, middle, and lower courses. The upper course is narrow with rapids and waterfalls as the river flows over rocky ground. The middle course widens and slows as the ground becomes smoother. The lower course nears the end, where the river meets the sea and deposits sediment to form deltas and estuaries. Key features of rivers mentioned include tributaries, meanders, oxbow lakes, flood plains, and confluences.
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River
The document describes the journey of a river from its source in hills or mountains, where it begins, to its mouth where it empties into the sea. Along the way, the river may encounter waterfalls where it hits layers of rock, tributaries which are smaller streams that join the main river, meandering curves and bends, and sometimes lakes can form in low areas of the river. Eventually all rivers flow to the sea at their final mouth.
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.
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.
How Do Rivers Shape The Land
Rivers shape the land through erosion and deposition as they flow from their sources downstream. In the upper course near the source, the river erodes steep V-shaped valleys due to its high gradient and velocity. In the middle course, meanders and oxbox lakes form as the river erodes the outside of bends and deposits sediment inside bends. In the lower course near the mouth, floodplains and deltas form as the river's velocity decreases and it deposits large amounts of sediment.
River final
The document discusses the course of a river from its source to its mouth. It begins by defining what a river is and explaining that rivers flow downhill via mountains, valleys, or plains towards an ocean or other body of water. It then discusses various river features and landforms created by erosion like waterfalls, V-shaped valleys, and potholes. The document also explains processes that shape the river channel like abrasion, attrition, and solution. Finally, it describes what happens as the river approaches its mouth, including levees, deltas, estuaries, and deposition of sediment.
Erosion
The sediment begins its journey on a mountainside where it undergoes weathering from processes like freezing water and roots. It is eroded slowly by water and sometimes more quickly during landslides, being transported by runoff into rivers that carry it down the mountain and farther into wider valleys. The river eventually slows and deposits the sediment either on a point bar within the river or in a delta where the river meets the ocean, completing the sediment's movement from mountain to sea.
Presentation (9)
A river flows from higher to lower ground, originating from mountains or glaciers and emptying into the sea. It has an upper course with swift flow and erosion, a middle course where speed reduces and meanders form, and a lower course where the river deposits silt and splits into distributaries to form deltas.
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River
The document describes the journey of a river from its source in hills or mountains, where it begins, to its mouth where it empties into the sea. Along the way, the river may encounter waterfalls where it hits layers of rock, tributaries which are smaller streams that join the main river, meandering curves and bends, and sometimes lakes can form in low areas of the river. Eventually all rivers flow to the sea at their final mouth.
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.
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.
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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.
How Do Rivers Shape The Land
Rivers shape the land through erosion and deposition as they flow from their sources downstream. In the upper course near the source, the river erodes steep V-shaped valleys due to its high gradient and velocity. In the middle course, meanders and oxbox lakes form as the river erodes the outside of bends and deposits sediment inside bends. In the lower course near the mouth, floodplains and deltas form as the river's velocity decreases and it deposits large amounts of sediment.
River final
The document discusses the course of a river from its source to its mouth. It begins by defining what a river is and explaining that rivers flow downhill via mountains, valleys, or plains towards an ocean or other body of water. It then discusses various river features and landforms created by erosion like waterfalls, V-shaped valleys, and potholes. The document also explains processes that shape the river channel like abrasion, attrition, and solution. Finally, it describes what happens as the river approaches its mouth, including levees, deltas, estuaries, and deposition of sediment.
Erosion
The sediment begins its journey on a mountainside where it undergoes weathering from processes like freezing water and roots. It is eroded slowly by water and sometimes more quickly during landslides, being transported by runoff into rivers that carry it down the mountain and farther into wider valleys. The river eventually slows and deposits the sediment either on a point bar within the river or in a delta where the river meets the ocean, completing the sediment's movement from mountain to sea.
Presentation (9)
A river flows from higher to lower ground, originating from mountains or glaciers and emptying into the sea. It has an upper course with swift flow and erosion, a middle course where speed reduces and meanders form, and a lower course where the river deposits silt and splits into distributaries to form deltas.
river lesson 1 (6).pptx is saved with agreat presentation very good
The document discusses key features of river drainage basins:
- A drainage basin is the land area drained by a river and its tributaries. It includes the river's source, channel, tributaries, watershed, and mouth.
- The source is where the river begins, usually in highland areas. Tributaries are smaller rivers that flow into the main river. The watershed separates waters flowing to different rivers.
- At the mouth, the main river finally reaches the sea. Together these features make up the river's drainage basin, which channels water throughout the landscape.
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.
River Stages and Delta Formation
This document summarizes the stages of river development from youth to old age. It describes 3 main stages: 1) The youth or initial stage where the river erodes quickly down steep slopes. 2) The mature stage where the river slows and develops landforms like meanders and floodplains through erosion and deposition. 3) The old stage where the river reaches flat land and builds up deltas by depositing sediment in a triangular shape at its mouth before emptying into the sea.
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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.
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Rivers form from rainwater flowing over land and collecting in streams. They flow from high elevations down to oceans, lakes or other bodies of water. Rivers have common structures like watersheds, basins, tributaries and channels. The largest rivers include the Nile, Amazon and Mississippi. Rivers experience flooding when water exceeds capacity. Dams help control flooding but are also used for water collection and power generation. Bridges allow crossing rivers. Life like bears and beavers inhabit rivers, which support surrounding plant growth. Flow rates are measured in cubic meters per second.
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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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The document discusses rivers and their environments. It describes the hydrologic cycle and how water moves between the earth's surface and atmosphere. It then explains the key components of a river system, including the source, tributaries, and mouth. It also defines the drainage basin and describes several landforms created by rivers, such as valleys, waterfalls, meanders, floodplains, and deltas. Finally, it discusses both the positive and negative impacts rivers can have on people, such as providing water, generating power, enabling transport, and causing floods.
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Fluvial processes and 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.
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1. Pennsylvania has 6 major river basins or watersheds that drain the state's land and waterways.
2. Half of Pennsylvania's land area drains into the Susquehanna River watershed.
3. Rivers and streams are important physical features that provide benefits like draining rainwater, generating electricity, and serving as habitats for organisms and travel routes for people.
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This document discusses river landforms and processes. It begins by defining a river and explaining fluvial processes. It then discusses key aspects of river systems such as tributaries, floodplains, and meanders. Different drainage patterns like dendritic, parallel and trellis are described. The document also covers stream discharge, perennial and non-perennial streams, erosion types, sediment load and transportation methods. Finally, it summarizes the landforms created by upper, middle and lower course rivers such as V-shaped valleys, waterfalls, meanders, ox-bow lakes and deltas.
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The document outlines the steps for designing a task to teach students about rivers:
1) Choose a student age/language level and topic about rivers
2) Formulate a real-world guiding question for students, such as "What is a river?" for primary school students
3) Provide details of the task, including authentic texts and videos, scaffolding, developing skills and competencies, and recycling previous knowledge
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Meanders
A meander is a bend or curve in a river's course that develops over time due to erosion on the outside bend and deposition on the inside bend. As the faster moving water on the outside erodes and undercuts the bank, it forms a river cliff. Meanwhile, sediment is deposited along the inner bend, tightening and lengthening the meander loop. This process of erosion on the outside and deposition on the inside causes the meander bend to migrate and become more pronounced.
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river lesson 1 (6).pptx is saved with agreat presentation very good
The document discusses key features of river drainage basins:
- A drainage basin is the land area drained by a river and its tributaries. It includes the river's source, channel, tributaries, watershed, and mouth.
- The source is where the river begins, usually in highland areas. Tributaries are smaller rivers that flow into the main river. The watershed separates waters flowing to different rivers.
- At the mouth, the main river finally reaches the sea. Together these features make up the river's drainage basin, which channels water throughout the landscape.
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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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This document summarizes the stages of river development from youth to old age. It describes 3 main stages: 1) The youth or initial stage where the river erodes quickly down steep slopes. 2) The mature stage where the river slows and develops landforms like meanders and floodplains through erosion and deposition. 3) The old stage where the river reaches flat land and builds up deltas by depositing sediment in a triangular shape at its mouth before emptying into the sea.
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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.
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Rivers form from rainwater flowing over land and collecting in streams. They flow from high elevations down to oceans, lakes or other bodies of water. Rivers have common structures like watersheds, basins, tributaries and channels. The largest rivers include the Nile, Amazon and Mississippi. Rivers experience flooding when water exceeds capacity. Dams help control flooding but are also used for water collection and power generation. Bridges allow crossing rivers. Life like bears and beavers inhabit rivers, which support surrounding plant growth. Flow rates are measured in cubic meters per second.
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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.
Grade 12 notes (Geomorphology) .pdf
This document provides a summary of key concepts in geomorphology. It defines important terms like drainage basin, catchment area, river types and features. It describes different drainage patterns that form based on geology and topography. Factors that influence river discharge and landforms created by fluvial processes like meanders and waterfalls are also outlined. The document also discusses concepts like river grading, rejuvenation, and capture - how rivers gain or lose energy over time.
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The document discusses rivers and their environments. It describes the hydrologic cycle and how water moves between the earth's surface and atmosphere. It then explains the key components of a river system, including the source, tributaries, and mouth. It also defines the drainage basin and describes several landforms created by rivers, such as valleys, waterfalls, meanders, floodplains, and deltas. Finally, it discusses both the positive and negative impacts rivers can have on people, such as providing water, generating power, enabling transport, and causing floods.
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Continental waters include lakes and rivers. Lakes are large bodies of water surrounded by land, while rivers start in mountains and flow to lowlands. Rivers have a course, channel, mouth, and source, and the water flow and speed changes from upriver to mid-river to downriver near the mouth. People build dams on rivers to store water. Subterranean waters are underground until they emerge above ground as fountains. Marine waters consist of seas and oceans. Coastal landscapes have beaches, cliffs, capes, gulfs, peninsulas, and islands, with islands close together forming an archipelago.
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Ronnie Raindrop narrates their journey from precipitation to reaching the sea. Ronnie begins falling as precipitation near a watershed and rolls down a steep, thin valley river. The fast flowing river is rocky in its upper stage before Ronnie falls over a waterfall. After passing through middle passages and an oxbow lake, the flattening river turns everywhere through meanders before reaching the beach, with friends falling onto floodplains along the way. In the lower stage, the river's load is too great for it to hold as it approaches the massive floodplains and expanding meanders leading to the river mouth and sea, where Ronnie and friends have finally reached the end of their journey.
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1) Choose a student age/language level and topic about rivers
2) Formulate a real-world guiding question for students, such as "What is a river?" for primary school students
3) Provide details of the task, including authentic texts and videos, scaffolding, developing skills and competencies, and recycling previous knowledge
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Meanders
A meander is a bend or curve in a river's course that develops over time due to erosion on the outside bend and deposition on the inside bend. As the faster moving water on the outside erodes and undercuts the bank, it forms a river cliff. Meanwhile, sediment is deposited along the inner bend, tightening and lengthening the meander loop. This process of erosion on the outside and deposition on the inside causes the meander bend to migrate and become more pronounced.
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- 2. The River Journey Hey there! I’m Sidney Sediment, but you can call me Sid. I’d like to invite you on a little trip with me today. I’m trying to make my way to the seaside - I’m really in need of a holiday. To get there, we’re going to have to take a journey down the river. What’s that? You’ve never taken the river journey before? Don’t you worry – I know all the stages. Stay by my side!
- 3. The River Journey UPPER MIDDLE LOWER The course of a river can be divided into three sections.
- 4. Upper Course This is the beginning of the river. It’s narrow and has lots of energy as it flows over rocky ground – hold on tight! This is the source. It’s the start of the river. These are tributaries. They are small streams that flow into the main river. This is a waterfall. It’s a steep drop over a rocky ledge, which causes the river water to flow suddenly downward. Source Tributary Waterfall
- 5. Middle Course The river starts to get wider and deeper here. The ground is smoother and the river flows faster and more smoothly. Confluence This is the point where two rivers join to make one. Meander Oxbow Lake This is a U-shaped bend in the river. This is a U-shaped lake that is cut off from the river – it used to be a meander.
- 6. Lower Course Now the river is nearing the end of its journey. We’re almost there! This is where freshwater from the river mixes with saltwater from the sea. This is wetland made up of sediment transported to the end of the river, and divided by channels. Estuary Delta Mouth This is where the river enters the ocean. This is a flat area of land next to the river that is flooded when river level rises. Flood Plain
- 7. Recap Source Tributary Waterfall Confluence Oxbow Lake Meander Flood Plain Mouth Estuary Delta UPPER MIDDLE LOWER We made it! Let’s recap.
- 8. Quiz What is the start of a river called? A) The mouth B) The source C) Oxbow lake D) Ketchup
- 9. Quiz Where does the river meet the sea? A) At a waterfall B) At a confluence C) At a tributary D) At its mouth
- 10. Quiz What is a confluence? A) A U-shaped bend in a river B) A point where two rivers join together
- 11. Quiz Which feature of a river is this? A) Delta B) Estuary C) Meander D) Source
- 12. Quiz Which feature of a river is this? A) Waterfall B) Mouth C) Tributary D) Oxbow lake
- 13. Quiz Which section of a river is this? A) Upper B) Middle C) Lower
- 14. Quiz Which section of a river is this? A) Upper B) Middle C) Lower
- 15. Quiz Which section of a river is this? A) Upper B) Middle C) Lower