registered in England (Company No 02017289) with its registered office at 26 Red Lion The gradient is at it's gentlest, as the river approaches the sea. Any material that is broken away has to be transported and there are four ways in which this can happen: Solution occurs because of the way that soluble materials dissolve when they are in the river. Suspension is slightly different, but it might help you if you imagine that the particles involved in suspension are a tiny bit heavier than soluble particles. For example, if the water becomes shallower, then deposition can occur. The area over which they flood is known as the floodplain, and this often coincides with regions where meanders form. If you feel that the instruction or language is too simplistic or too complex then edit it to suit your learners. There are two ways in which you might be asked to identify a river during your examination, they are long profile and cross profile. The lower course is the last course of a river. Rivers usually have a wide, smooth channel, and water moves at its slowest. Before abrasion can take place, hydraulic action has an important role to play. Square This is where materials are picked up by the river and deposited somewhere else. Useful links- to video clips, websites etc. A PowerPoint version of diagrams and answers. The silt and other materials carried by the river are deposited. If you take a look at a cross profile diagram of a river, then it is easy to see that rivers widen at certain points. If you are offered a cross profile diagram of a V-shaped valley with steep sides and what appears to be a small amount of water in the bottom, then that usually means that you are looking at the upper course of a river, where the gradient is steep. When rivers flood the velocity of water slows. Naturally, the course that a river follows affects the landscape that surrounds the river because of processes like erosion. You will more than likely be asked about why deposition occurs. I have found the resources easy to upload and convert to Google Slides and Google Docs, You will not be able to edit the diagrams, pictures, or visuals included in this resource.

Geography / Geomorphic processes and landforms, Geography / Geomorphic processes and landforms / Rivers. Created: Jun 18, 2018| Updated: Aug 2, 2020. Why not set this as pre-learning so that students can start a lesson from a position of confidence? Huge Primary Geography Knowledge Organisers Bundle! They usually start off narrow in the upper course, so a wide river tells us that we are looking at either the middle course or the lower course. A lesson for the topic of Rivers. This website and its content is subject to our Terms and Typically, a river valley can be divided into three sections; the upper course, the middle course and the lower course.

As rivers flow, they pick up material. If so, you can save yourself a lot of time by downloading our modules below.
OCR A Level Geography Past Papers WJEC A Level Geography Past Papers, River Landscapes GCSE Geography Revision Notes, Compatible with the following exam boards, Measuring and Assessing Volcanic Activity. Huge Primary Geography Knowledge Organisers Bundle! Vertical erosion is really easy to spot because we can see how deep the river valley is when we look at cross profile diagrams. NB: When answering questions on River features, always remember to use the F.E.E.D. They are still carried along in the water, but in a dissolved state. The gradient is steep. River Severn | River Thames. Main activity see's the pupils annotate a diagram of a Levee.

The Lower Course: The last part of a river near its mouth is called the lower course. Completely FREE. AQA GCSE Geography Content- The Geographical knowledge- supported by short activities, images, graphs, diagrams. In the lower course, the river has a high volume and a large discharge. Now that you know what happens during erosion and transportation, it is important to learn what happens to all of these particles and where they actually end up. Teacher PowerPoint with diagrams and answer key provided directly onto the slides or in notes section of each slide. Pre-class flipped learning- The majority of students should be able to access the learning in the resource without teacher support. Previously taught in a 1hr lesson. The course a river takes is split into three stages, the upper, middle and lower stage. In this part the slope of the river bed is not very steep. A word document worksheet that includes step by step descriptions of how the landforms are created.

Solution also occurs in rivers. Geography / Geomorphic processes and landforms, Geography / Geomorphic processes and landforms / Rivers, The Long Profile of a River: Upper, Middle, Lower Course (MINI).

The current is also very slow. You can control the learning objectives, you can add video clips, your own activities etc. A River’s Course. The sheer force of the water in the river breaks rock particles away. River Landforms of the Lower Course- Focusing on Floodplains, Levees, River Deltas. Generally, either erosion or deposition will be a dominant force. Young River - the upper course. The beginning of a river, when it flows quickly with lots of energy, is called a young river. Section 2 is the middle course (where it comes down into the lowlands).

This worksheet is also provided as a PDF.

OCR A Level Geography, AQA A Level Geography Past Papers When we are talking about erosion, abrasion is one of the key factors that plays a prominent role. OCR GCSE Geography, AQA A Level Geography

Upper course of river Middle course of river Lower course of river Source - the point at which the river starts. This deposition leaves a layer of sediment across the whole floodplain. A River’s Course. The cross profile simply shows us a cross-section of the river, while the long profile shows us how the gradient changes over the course of the river. Section 3 is the lower course (where it is at its widest and most powerful and enters the sea). This is where some types of rock are dissolved. These are supported by diagrams and follow-up questions. Introduces 3 types of river delta: cuspate, arcuate and bird’s foot. Deposition can occur for a few different reasons. This means that you can add around this.

The description of each landform is supported by diagrams and key terminology. The course a river takes is split into three stages, the upper, middle and lower stage. Content: This resources describes and explains the formation of flood plains and river deltas. registered in England (Company No 02017289) with its registered office at 26 Red Lion

* Locating river features in the lower, middle or upper course of a river, * Seeing where major rivers are located * Knowing how waterfalls are formed through the use of labelled diagrams, * Building a pop up river basin (template included), * The water cycle * River pollution * and a topic self-assessment. Edexcel A Level Geography Past Papers
Traction involves heavier particles than the ones that we can see in saltation.

We can also see attrition occurring. Rivers flood on a regular basis. Most rivers have upper, middle and lower courses. Locating the world's famous volcanoes - KS2, Identifying the key features of mountains, Volcanoes and other Natural Disasters - Presentation. I have deliberately focused on key knowledge and processes. Eduqas A Level Geography Past Papers CIE IGCSE Geography Use the resource as a framework. This website and its content is subject to our Terms and In class activity- I use this resource to quickly and accurately teach the subject knowledge. Here are some features that you should look for: Erosion shapes the landscape around rivers, but two types of erosion are actually occurring at the same time. Conditions. River Landforms of the Lower Course- Focusing on Floodplains, Levees, River Deltas. Conditions. Section 1 is the upper course (think high up in the mountains). There is a thinking skills activity based on land use on floodplains. To support students who benefit from short, structured activities. Covering KS3, GCSE and A-Level, we provide the most comprehensive GCSE and A-Level revision tools to pass your exams. River Floods.

Tributary- Smaller rivers/streams that join the main river. This material can then scrape along the sides of the channel. This resources describes and explains the formation of flood plains and river deltas. Locating the world's famous volcanoes - KS2, Identifying the key features of mountains, Volcanoes and other Natural Disasters - Presentation. These particles are too heavy to bounce along so they are simply pushed by the force of the water. Meanders support the formation of floodplains through lateral (sideways) erosion. 6.-River-Landforms-of-the-Lower-Course-GRAYSCALE. Review- a plenary, recall activity, AFL, knowledge check. Are you looking for high-quality GCSE Geography resources? Any river, anywhere in the world can be split into three sections. By the time a river reaches the lower stretches of its long profile – and gets closer to base level (usually sea level, though possibly a lake) – the channel can experience an increase in deposition. These river diagrams help to explain the geography topic of rivers. In the upper stage, the river is close to its source and high above its base level (the lowest point the river can erode to 1).In the lower stage the river is far away from its source, close to the mouth and not far above its base level. When we are talking about both vertical erosion and lateral erosion, there are four key factors that come into play: As you can see, one of the main causes of erosion actually occurs because of materials that are being transported downstream.

Ideal for years 7 to 9. We can also see deposition occurring along the course of rivers. Includes application through the consideration of planning on flood plains (zonation). In the upper stage, the river is close to its source and high above its base level (the lowest point the river can erode to 1).In the lower stage the river is far away from its source, close to the mouth and not far above its base level. system.

Deposition can also occur if the amount of material that is present increases or if the volume of water in the river decreases. Lower course features. BASED ON AQA 1-9 GCSE. Activate- a starter, an introduction, a stimulus. We shall examine each section of the river along with their various features in some detail. Saltation involves particles that are too heavy to be simply carried along by the water. You can edit all written passages.

Some features expected in this section of the river are V- shaped valleys, interlocking spurs, a river bed with large rocks and stones,gorges, fast flowing rapids and waterfalls. Post class homework and consolidation- Likewise, the resources could be used to consolidate on in-class teacher instruction.

Nearly all rivers have an upper, middle, and lower course. The former is closest to the source of the river and the latter is closest to the mouth of the river. Tes Global Ltd is