Additional Materials: Ruler Calculator READ THESE INSTRUCTIONS FIRST Write your Centre number, candidate number and name in the spaces provided. The pupils then create annotated diagrams of spits, bars and tombolos. Cliff Retreat. This sand has been transported by longshore drift (material carried along the coast by the prevailing Spits form in bays where rivers prevent the Spit from growing fully across the whole bay. In geography, spit is a landform made by the deposition of sand by the movement of tides. Waves called swash come into the beach at an angle and pick up material (1) They come in at an angle because of wind direction (1) A short video describing what a spit is and how one forms for my geography homework :) . It is formed by the process of long shore drift. Spit B. Stack C. Beach D. Wedge E. Cliff Correct Answer: Option A sand spit is a long, narrow ridge of sand or shingle that is connected to the mainland at one end and extends into the sea at the other end. BUURI EAST STANDARDS . Spit and Hook: A spit is a projected deposition joined at one end to the headland, with the other end free in the sea. U-shaped valley V-shaped valley Waterfall . Candidates can gain full marks for well-annotated diagrams that explain the formation of a sand spit. PHYSICAL GEOGRAPHY. b) Using well-labeled diagram, explain how each of the following features is used formed. Stage in the enquiry process Possible questions Responses for Dawlish Warren fieldwork 1 Explain how you Outline the role of erosion in shaping a headland. A feature of coastal deposition is a sand spit / tombolo. A spit is an extended stretch of beach material that projects out to sea and is joined to the mainland at one end. By the end of this lesson you will be able to: • Name 3 depositional landforms • Describe longshore drift • Explain how longshore drift forms bars, spits and tombolos. Candidates were asked to draw a diagram of a stretch of coastline showing a hooked or recurved spit in Part (a) (i) and to suggest reasons for the development of the recurved ends in Part (ii). Describe the process that leads to the formation of a spit. • Beach - The zone of deposited material that extends from the low water line to the limit of storm waves. 312/1 . Material is pushed up onto beaches at an angle when the swash brings it onto the coastline at a 45 degree angle. top sporting events in the world Use the diagram to identify a landform found in the upper course, middle course and lower course. The process of longshore drift may be explained in greater detail. You should be able to draw annotated diagrams of the features to show how they form as well as knowing named examples of each. (3 marks) Have a go at answering the question in the space below. A tombolo is formed when a spit connects the mainland coast to an island. Landforms created by erosion include headlands and bays, caves, arches, stacks and stumps. Coastal Protection Images. Sediment is pushed up and dragged back down . Curonian Spit, divided between Russia and Lithuania A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. Explain the formation of a spit. BUURI EAST STANDARDS . • The formation of river landforms including waterfall, gorge, v-shaped valley, floodplain, levee, meander, ox-bow lake. The waves then travel at a ninety degree angle back down the beach due to gravity as the backwash. Spit is a landform in geography that is created from the deposition of the sand by the tide movements. Geography Diagrams. JULY, 2019 . Geography OCR B REVISION BOOKLET . Cuspate Foreland Diagram. The Spit Geography is Depicted by the Following Diagram: I m a g e w i l l b e U p l o a d e d S o o n The longshore current generated by the waves spreads out and dissipates at places where the direction of the inland shore re-enters or changes its direction for example at places like headlands. 2. Explain what a drainage basin is in your own words. i) A spit (4mks) ii) A blow hole (2mks) iii) An a toll (5mks) i) Formation of a spit. Use the diagram below to answer the question. The backwash, however carries the material back down the . Diagrams were poorly executed with little attention being paid to its relation to longshore drift or to the trend of the coastline. GEOGRAPHY 0460/11 Paper 1 May/June 2017 1 hour 45 minutes Candidates answer on the Question Paper. 5. A tombolo is a coastal formation that means, when translated from Italian, "mound". A spit is a depositional landform that is a long, narrow beach of sand or shingle attached to the mainland at one end, and possibly across an estuary. Simple river basin diagram. Historical records show that some twenty-nine villages have fallen into the sea since Roman times (Fig. Diagrams may help your answer (4) . Supported by diagrams and key terminology. The prevailing wind pushes constructive waves up the beach at an angle as the swash. Sand or shingle is deposited by long shore drift / oblique waves. We identified it from obedient source. The spit builds up but is often curved by the wind and wave currents. Compound spits exhibit a number of recurved 'spurs' along their length as each . In Section B answer question 6 and any other two. Also, to help illustrate the topic, there is a great coastal diagram and links to more useful geography resources all to help you learn about the geography topic of coasts in a fun and interesting way. The process of longshore drift occurs and this moves material along the coastline. How people use and pollute coastal areas. This island-like landform is actually attached to the coast by a thin sand bar or spit. The combination of clay geology and a high-energy environment has helped make this part of the Yorkshire coast one of the most rapidly eroding coastlines in Europe. It the present example of the natural, coastal deposition area for the material, particularly Pleistocene shingle transported from the cliffs of Christchurch Bay, a coastline which eroded . A lagoon is a salt water lake that is formed when a sand bar extends across a bay, blocking off some of the bay. . Learning Objectives. One end of the spit remains attached to the mainland while the other end is open out in the water. Formation of Caves, Arch, Stack and Stump. Check any diagram(s) for relevant points not present in the text and award marks accordingly. Spits are formed by the movement of sediment (typically sand) along a shore by a process known as longshore drift. spit (Figures 1 and 5) which lies at the mouth of the River Exe, less than 3 km north-east of the south Devon holiday town of Dawlish. Tick ( ) the correct definition below. Diagram showing a spit A spit contrasted with other coastal landforms. The process is shown in the diagram below. Application to real world examples (coastal spit). What is a lagoon? A spit or sandspit is a deposition bar or beach landform off coasts or lake shores. The deposits accumulate forming a spit The continued deposition elongates the spit eventually blocking the mouth of the bay forming a bay bar The bay bar separates part of the sea water from the open sea The enclosed sea water is the lagoon (c) (i) Give three reasons why some lakes in Kenya have saline water. The area behind the Spit is protected from wind and waves. Landforms created by deposition include beaches, spits, tombolos and bars. 2 Complete the table in Figure 12 by calculating the mean sediment size, in cm . Diagram Q2 Sand spit Look at Diagram Q2. The landform is formed by longshore drift in the dominant wind direction, which carries material eroded from the proximal end of the spit to deposit it at the distal end of the landform. If a spit joins another headland, what is it called? Describe with the aid of diagrams, how it was formed 9B. Study Figure 2, a block diagram showing how river landforms change downstream. Instruction: Answer ALL the questions in section A. Describe with the aid of diagrams, how it was formed Name ONE landform formed by Coastal OR Glacial deposition. PAPER 1 . Detailed explanation of how sediment is transported along the coast by the process of long shore drift and then deposited on the sheltered side of a headland. You may wish to use an annotated diagram or diagrams in your answer. Its submitted by government in the best field. Instruction: Answer ALL the questions in section A. Material builds up behind the spit forming mud flats. Also known as sandspit, this type of landform is found off the coasts or the lake shores. This is because rates of deposition are . Write in dark blue or black pen. We then draw an annotated field sketch from a photograph of Dawlish Warren Spit. In geography, a spit is a deposition landform found off coasts. Spit Stack Suspension Swash Traction Transport Triassic period Upland . A spit develops when waves meet the beach at an oblique angle, moving sediment down the beach and into the open waters where it is deposited in a . Geography paper 1 (312/1). • Beach - The zone of deposited material that extends from the low water line to the limit of storm waves. (2mks) b) Give three reasons why it is importance to study geography. 2. (5 marks) (b) Study the following landforms: Ox-bow Lake, rock pedestal, cirque, sand spit, stalagmite Choose ONE erosional and ONE depositional feature and with the aid of diagrams, describe the processes of their . Sand and shingle is moved . (3 marks) State the two causes of vertical movement of the ocean water. If you would like to use these images for commercial purposes please contact us. Erosion. Materials are dragged in a zig-zag manner up the coast by the action of the waves (swash & backwash). Gradually sediment builds up, vegetation begins to establish itself and forms a Salt Marsh. The process of longshore drift may be explained in greater detail. Formation of Headlands and Bays. Figure 12 Longshore drift Longshore drift X Y River estuary N 0 200 400 m Spit Location X Sediment size (cm) Location Y Sediment size (cm) 12 9 10 4 92 15 3 82 13 6 Mean: 11.2 Mean: 03. direction of prevailing wind, direction of longshore drift, deposited sediment extends into the sea, hooked end, change in direction of the coast, salt marsh forming in stagnant water, flowing river prevents spit growing further, temporary wind direction. It appears to be a small island that has not fully separated from the mainland. (3mks) 2. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. Learn how to draw the Spit Diagram. Spits are formed where the prevailing wind blows at an angle to the coastline . A hook or a recurve may form at the end of the spit. . Process. It is easier to remember coastal features having seen them and it is easier to see how the features are formed through looking at and studying coast pictures. Task. Explain the formation of a sand spit. Here are a number of highest rated Cuspate Foreland Geography pictures on internet. Coastal Landforms of Deposition. A mark for a named process should only be If you would like to attempt the question with the aid . (3 marks) GEOGRAPHY . How is a spit different from other landforms? Please remember to credit www.internetgeography.net If you would like to use these images in the public domain. The pupils then label the feature of the spit and fill in the blanks on the paragraph. (2 marks) List three types of ocean tides. A salt marsh begins when mud and silt are deposited along a sheltered part of the coastline. Award a maximum of 4 marks where candidates provide a fully developed explanation of longshore drift. Plus there are ideas for making geography models that make learning about coasts fun. Tombolos are sometimes referred to as "tied islands", because it seems to tethered to . Its submitted by dispensation in the best field. Geography Unit: KGE0 4GE0 Paper: 01 Pearson Edexcel Certificate Pearson Edexcel International GCSE KGE0/01 4GE0/01. Study Figure 12, showing sediment size at two locations along a coastal spit. Detailed explanation of how sediment is transported along the coast by the process of long shore drift and then deposited on the sheltered side of a headland. Diagram showing a spit. Blakeney Point is a spit that extends along the Norfolk coastline. aeolian transportation. Name the features marked X, Y and Z. Longshore Drift - Longshore drift - Formation of a coastal spit - Coastal vocab - The formation of a spit - The formation of a spit, annotated photo 2. Key words • Bar - Where a spit grows across a bay, a bay bar can eventually enclose the bay to create a lagoon. Landforms of deposition. Here are a number of highest rated Cuspate Foreland Diagram pictures on internet. (1) Definition Tick ( ) Create a 3D- model to show several coastal features along a stretch of coastline: cliff, wave-cut platform, headland, bay, cave, arch, stack, spit, bay-bar, tombolo, beach. Lesson Objectives This lesson is about longshore drift and how this process creates depositional landforms. An example of this can be found at Sutton, Co. Dublin. If a spit joins an island, what is it called? Study the map of Yimbo 1:50,000 (sheet 115/1 . Geography paper 1 (312/1). Answer question 6 and any other two questions from this section. Give yourself 5 marks if you wrote in more depth you should have included a detailed diagram or case study: Material is deposited in calmer waters. The formation of spits. Chapter 12: Coastal Processes, Patterns & Associated Landforms, & Human Interaction Sand Spit § A sand spit is a long narrow ridge of deposited sand shingle § It is connected to the coast at one end § Sand spits develop due to longshore drift and deposition § Sand spits form where the process of longshore drift is interrupted § Waves lose . The diagram shows the building of a spit by longshore. Hooked/Recurved spits. PAPER 1 . Spits are narrow and elongated - one end is attached to the mainland and the other is out in open water. These cause the sediment of the Spit to bend inland forming a Hook. In Section B answer question 6 and any other two. Hurst Spit is a hook-shaped shingle spit which extends southeast for 1.4 miles or 2.25 km. 312/1 . [Turn over 8. page 04 A Question 3 . GCSE Geography_Fieldwork Pack_Coasts_June20 9 The material below shows answers prepared by a school whose GCSE Geography students carried out their geographical investigation at Dawlish Warren (a spit on the south coast of England). Historically, the spit has built up as a result of deposition of sand at the mouth of the estuary. 1. from the Hampshire shore into the Solent towards the Isle of Wight.
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