This document provides guidance on answering exam questions about how natural processes interact to shape geographic environments in New Zealand. It discusses key concepts like elements, processes, and features. It focuses specifically on the coastal environment of South Muriwai Beach, describing the natural processes of wave action, aeolian action, and their interactions. It also provides examples of potential exam questions on topics like spatial and temporal variations, and the distribution and formation of natural features as shaped by interacting processes. Diagrams and maps are emphasized as ways to enhance answers.
GEOGRAPHY IGCSE: DUNE FORMATION - MURIWAI BEACH NEW ZEALANDGeorge Dumitrache
This document discusses dune formation and examples of eroded and vegetated dunes at Muriwai Beach in New Zealand. It provides details on:
- How dunes are formed by wind transporting sand and depositing it in sheltered areas behind obstacles.
- Examples of eroded dunes at Muriwai Beach that have been exposed by erosion of dunes in front of them.
- The role of vegetation like pingao sedge in trapping sand and building/stabilizing dunes at Muriwai Beach.
- How the interaction between aeolian sand transport processes and vegetative growth shapes the dunes at Muriwai Beach.
The document provides information and revision notes for a Level 3 Geography exam, including:
- The exam will take place on September 15 from 1:30-4:30pm in Option B hall or M14A. Students should bring specific supplies.
- The exam consists of 3 papers analyzing natural processes, cultural processes, and applying geographic skills.
- Suggested revision focuses on coastal processes at South Muriwai Beach and tourism development in Rotorua, NZ and Waikiki, Hawaii.
- Formats, criteria, and content that could be assessed are outlined for each paper.
This document provides an overview and revision of content for demonstrating understanding of how the cultural process of tourism development shapes geographic environments. It discusses several key parts to the standard, including the operation of the cultural process over time and space, factors that influence changes to the process, and effects on people and places. The document then provides examples of analyzing tourism development in Rotorua, New Zealand, breaking down elements like tourists, attractions, facilities, and how they interact and vary temporally and spatially. It suggests focusing answers on analyzing these elements and their links in order to score well on the exam.
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.2 WEATHERING AND ROCKSGeorge Dumitrache
Weathering is the breakdown of rocks through chemical and mechanical processes. There are two main types of weathering: chemical weathering involves changes to a rock's mineral composition, while mechanical weathering breaks rocks into smaller pieces without changing their composition. The rate and type of weathering depends on factors like climate, rock type, and rock structure. Limestone is particularly susceptible to weathering due to its permeability and solubility, which can form distinctive karst landscapes.
A2 Geography Revision for Coastal Environments, subchapter 8.3 Coral Reefs. It is suitable for Year 13 Geography, Cambridge Examination in November 2016. It contains: key terms and definitions, a topic summary, sketches and descriptions, additional work (6 questions for testing your knowledge) and some suggested websites.
This document provides guidance on answering exam questions about how natural processes interact to shape geographic environments in New Zealand. It discusses key concepts like elements, processes, and features. It focuses specifically on the coastal environment of South Muriwai Beach, describing the natural processes of wave action, aeolian action, and their interactions. It also provides examples of potential exam questions on topics like spatial and temporal variations, and the distribution and formation of natural features as shaped by interacting processes. Diagrams and maps are emphasized as ways to enhance answers.
GEOGRAPHY IGCSE: DUNE FORMATION - MURIWAI BEACH NEW ZEALANDGeorge Dumitrache
This document discusses dune formation and examples of eroded and vegetated dunes at Muriwai Beach in New Zealand. It provides details on:
- How dunes are formed by wind transporting sand and depositing it in sheltered areas behind obstacles.
- Examples of eroded dunes at Muriwai Beach that have been exposed by erosion of dunes in front of them.
- The role of vegetation like pingao sedge in trapping sand and building/stabilizing dunes at Muriwai Beach.
- How the interaction between aeolian sand transport processes and vegetative growth shapes the dunes at Muriwai Beach.
The document provides information and revision notes for a Level 3 Geography exam, including:
- The exam will take place on September 15 from 1:30-4:30pm in Option B hall or M14A. Students should bring specific supplies.
- The exam consists of 3 papers analyzing natural processes, cultural processes, and applying geographic skills.
- Suggested revision focuses on coastal processes at South Muriwai Beach and tourism development in Rotorua, NZ and Waikiki, Hawaii.
- Formats, criteria, and content that could be assessed are outlined for each paper.
This document provides an overview and revision of content for demonstrating understanding of how the cultural process of tourism development shapes geographic environments. It discusses several key parts to the standard, including the operation of the cultural process over time and space, factors that influence changes to the process, and effects on people and places. The document then provides examples of analyzing tourism development in Rotorua, New Zealand, breaking down elements like tourists, attractions, facilities, and how they interact and vary temporally and spatially. It suggests focusing answers on analyzing these elements and their links in order to score well on the exam.
CAMBRIDGE AS GEOGRAPHY REVISION: ROCKS AND WEATHERING - 3.2 WEATHERING AND ROCKSGeorge Dumitrache
Weathering is the breakdown of rocks through chemical and mechanical processes. There are two main types of weathering: chemical weathering involves changes to a rock's mineral composition, while mechanical weathering breaks rocks into smaller pieces without changing their composition. The rate and type of weathering depends on factors like climate, rock type, and rock structure. Limestone is particularly susceptible to weathering due to its permeability and solubility, which can form distinctive karst landscapes.
A2 Geography Revision for Coastal Environments, subchapter 8.3 Coral Reefs. It is suitable for Year 13 Geography, Cambridge Examination in November 2016. It contains: key terms and definitions, a topic summary, sketches and descriptions, additional work (6 questions for testing your knowledge) and some suggested websites.
Group Presentation
Semester 03
ER2412 Introduction to Oceanography
Department of Earth Resources Engineering
University of Moratuwa
This presentation is based on ocean currents in the world,sri lanka and monsoon system in sri lanka
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM ATMOSPHERIC DISTURBANCES. It contain case studies: Hurricane Katrina 2005, Cloud Seeding in New Zealand 1950-1970.
The document discusses different tropical environments and climates. It begins by explaining that the Inter Tropical Convergence Zone (ITCZ) on average is located about 50 north of the equator but varies seasonally based on the sun's position. It then states that the ITCZ is the most important factor in the migration of low pressure belts and seasonal shifts in tropical rains. It goes on to briefly describe the climates of tropical rainforests, tropical monsoons, and tropical savannas.
This document provides information on coastal landforms found in LEDC and MEDC countries. It describes both depositional landforms like beaches, spits, and tombolos, which are built up by material deposited by waves, and erosional landforms like cliffs and caves, which are shaped by erosion. It discusses processes like longshore drift that form features like spits, and provides examples of different coastal landforms like Chesil Beach in the UK and Spurn Head in England.
The document discusses coastal landforms and the processes that create them. It describes how waves, tides, and currents shape the coastal environment and lead to both erosional and depositional landforms. Erosional features include cliffs, headlands, sea caves, and stacks, which are formed by processes like abrasion and hydraulic action. Depositional landforms include beaches, bars, spits, and barrier islands, which are produced when sediment is transported and deposited by waves, currents, and biological activity.
1) The document discusses the geological action of wind and the landforms it creates through erosion, transportation, and deposition of materials.
2) Wind erosion occurs through deflation, abrasion, and attrition, which form erosional landforms like deflation hollows, ventifacts, yardangs, and pedestal rocks.
3) Transportation of eroded materials by wind leads to depositional landforms like barchans and other dune types that indicate the direction of prevailing winds. The geological action of wind thus shapes the surface of the Earth through both destructive and constructive processes.
The document summarizes three ways that water can be moved on Earth: waves, currents, and tides. Waves are caused by wind moving across water and come in the form of crests and troughs, including tsunamis from earthquakes or landslides. Currents are streams of water that flow through the ocean due to the movement of the Earth, winds, and rotation, transporting warm and cold water to different regions. Tides are rises and falls in sea levels caused by the gravitational pull of the Moon, which bulges the ocean facing it, resulting in high and low tides about twice a day.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...George Dumitrache
This document defines key terms related to weather processes and phenomena. It discusses topics like adiabatic lapse rates, air masses, altitude, clouds, condensation, humidity, instability, precipitation and more. Weather results from changes in atmospheric conditions, such as temperature and moisture levels, which can cause air masses to rise or fall. Various types of precipitation form through different processes, like convectional rainfall from rising warm air or orographic rainfall on the windward sides of mountains. Fog occurs when air is cooled to its dew point through advection or radiation.
The document discusses various coastal landforms created by erosion and deposition processes along shorelines. It describes landforms such as headlands and bays, cliffs and wave-cut platforms, caves, arches, stacks, and stumps which are formed by coastal erosion. Beaches and spits are landforms created by coastal deposition, with beaches forming in sheltered areas between high and low tide lines, and spits forming as narrow ridges projecting from the coast due to longshore drift depositing materials.
Surface currents are driven mainly by wind and move large amounts of water across oceans, influencing global climate. Deep currents form due to differences in water density from temperature and salinity and are not wind-driven. Major surface currents like the Gulf Stream distribute heat from the equator to poles, warming areas like northern Europe. El Niño is a periodic warming of tropical Pacific waters that alters weather worldwide and impacts fisheries and agriculture through changed rainfall and storms. Scientists monitor oceans to improve understanding and forecasts of El Niño events and their far-reaching climatic effects.
This document summarizes key concepts about temperature and radiation budgets:
- Temperature decreases with increasing altitude according to the environmental lapse rate. Temperature also varies daily, seasonally, and with location.
- Solar radiation that reaches Earth's surface varies with factors like latitude, day length, cloud cover, altitude, aspect, and albedo of the surface.
- Heat is transferred around the globe by ocean currents and winds, which move warm water and air toward the poles and cold water and air toward the equator. Evaporation and condensation also transfer heat via the latent heat of water vapor.
- Greenhouse gases in the atmosphere trap some outgoing long-wave radiation, contributing to the natural greenhouse effect
The document discusses various coastal landforms created by erosion and deposition processes. It explains that waves break as they approach land due to increased friction. Swash carries water up the beach while backwash carries it down. Larger waves in the southwest are due to greater wind fetch. Cliffs and wave-cut platforms form through erosion processes like abrasion. Caves, arches, stacks and stumps also form through erosion. Beaches form in sheltered areas due to stronger swash depositing sediment. Spits and bars form through longshore drift depositing sediment. Tombolos connect landmasses.
Here is another creative presentation by your slide maker on the topic "OCEAN CURRENTS OF THE WORLD". Hope you like it. If you like it then please, *like*, *Download* and *Share*.
By- Slide_maker4u (Abhishek Sharma)
*******For presentation Orders, contact me on the Email addresses Written below********
Email- Sharmaabhishek576@gmail.com
or
Sharmacomputers87@gmail.com
*******THANK YOU***************
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDOUS ENVIRONMENTS RESULTING FROM MASS MOVEMENTS. It contain case studies: Italian Mudslides 1998, New Zealand Landslip 1979, European Avalanches 1999.
This document provides an overview of coastal environments and processes. It defines coastal zones and features such as the littoral zone, beach, foreshore, and backshore. It describes factors that influence coastal areas like lithology, geological structures, processes, sea level changes and human impacts. Coastal processes discussed include waves, tides, storm surges, wave refraction, and marine erosion. The summary discusses key coastal landforms and how they are formed by coastal processes.
Waves are formed by wind blowing over the surface of the sea. The height and energy of waves depends on wind strength, duration, and fetch. There are two main types of waves - constructive waves which build land, and destructive waves which erode land. Coastal geology also influences landscapes. Discordant coasts have bands of rock at 90 degrees to the sea, creating headlands and bays as softer rocks erode faster. Concordant coasts have parallel rock bands, where erosion of harder rocks leads to fast erosion of softer rocks behind.
Group Presentation
Semester 03
ER2412 Introduction to Oceanography
Department of Earth Resources Engineering
University of Moratuwa
This presentation is based on ocean currents in the world,sri lanka and monsoon system in sri lanka
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDS RESULTING FROM ATMOSPHERIC DISTURBANCES. It contain case studies: Hurricane Katrina 2005, Cloud Seeding in New Zealand 1950-1970.
The document discusses different tropical environments and climates. It begins by explaining that the Inter Tropical Convergence Zone (ITCZ) on average is located about 50 north of the equator but varies seasonally based on the sun's position. It then states that the ITCZ is the most important factor in the migration of low pressure belts and seasonal shifts in tropical rains. It goes on to briefly describe the climates of tropical rainforests, tropical monsoons, and tropical savannas.
This document provides information on coastal landforms found in LEDC and MEDC countries. It describes both depositional landforms like beaches, spits, and tombolos, which are built up by material deposited by waves, and erosional landforms like cliffs and caves, which are shaped by erosion. It discusses processes like longshore drift that form features like spits, and provides examples of different coastal landforms like Chesil Beach in the UK and Spurn Head in England.
The document discusses coastal landforms and the processes that create them. It describes how waves, tides, and currents shape the coastal environment and lead to both erosional and depositional landforms. Erosional features include cliffs, headlands, sea caves, and stacks, which are formed by processes like abrasion and hydraulic action. Depositional landforms include beaches, bars, spits, and barrier islands, which are produced when sediment is transported and deposited by waves, currents, and biological activity.
1) The document discusses the geological action of wind and the landforms it creates through erosion, transportation, and deposition of materials.
2) Wind erosion occurs through deflation, abrasion, and attrition, which form erosional landforms like deflation hollows, ventifacts, yardangs, and pedestal rocks.
3) Transportation of eroded materials by wind leads to depositional landforms like barchans and other dune types that indicate the direction of prevailing winds. The geological action of wind thus shapes the surface of the Earth through both destructive and constructive processes.
The document summarizes three ways that water can be moved on Earth: waves, currents, and tides. Waves are caused by wind moving across water and come in the form of crests and troughs, including tsunamis from earthquakes or landslides. Currents are streams of water that flow through the ocean due to the movement of the Earth, winds, and rotation, transporting warm and cold water to different regions. Tides are rises and falls in sea levels caused by the gravitational pull of the Moon, which bulges the ocean facing it, resulting in high and low tides about twice a day.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...George Dumitrache
This document defines key terms related to weather processes and phenomena. It discusses topics like adiabatic lapse rates, air masses, altitude, clouds, condensation, humidity, instability, precipitation and more. Weather results from changes in atmospheric conditions, such as temperature and moisture levels, which can cause air masses to rise or fall. Various types of precipitation form through different processes, like convectional rainfall from rising warm air or orographic rainfall on the windward sides of mountains. Fog occurs when air is cooled to its dew point through advection or radiation.
The document discusses various coastal landforms created by erosion and deposition processes along shorelines. It describes landforms such as headlands and bays, cliffs and wave-cut platforms, caves, arches, stacks, and stumps which are formed by coastal erosion. Beaches and spits are landforms created by coastal deposition, with beaches forming in sheltered areas between high and low tide lines, and spits forming as narrow ridges projecting from the coast due to longshore drift depositing materials.
Surface currents are driven mainly by wind and move large amounts of water across oceans, influencing global climate. Deep currents form due to differences in water density from temperature and salinity and are not wind-driven. Major surface currents like the Gulf Stream distribute heat from the equator to poles, warming areas like northern Europe. El Niño is a periodic warming of tropical Pacific waters that alters weather worldwide and impacts fisheries and agriculture through changed rainfall and storms. Scientists monitor oceans to improve understanding and forecasts of El Niño events and their far-reaching climatic effects.
This document summarizes key concepts about temperature and radiation budgets:
- Temperature decreases with increasing altitude according to the environmental lapse rate. Temperature also varies daily, seasonally, and with location.
- Solar radiation that reaches Earth's surface varies with factors like latitude, day length, cloud cover, altitude, aspect, and albedo of the surface.
- Heat is transferred around the globe by ocean currents and winds, which move warm water and air toward the poles and cold water and air toward the equator. Evaporation and condensation also transfer heat via the latent heat of water vapor.
- Greenhouse gases in the atmosphere trap some outgoing long-wave radiation, contributing to the natural greenhouse effect
The document discusses various coastal landforms created by erosion and deposition processes. It explains that waves break as they approach land due to increased friction. Swash carries water up the beach while backwash carries it down. Larger waves in the southwest are due to greater wind fetch. Cliffs and wave-cut platforms form through erosion processes like abrasion. Caves, arches, stacks and stumps also form through erosion. Beaches form in sheltered areas due to stronger swash depositing sediment. Spits and bars form through longshore drift depositing sediment. Tombolos connect landmasses.
Here is another creative presentation by your slide maker on the topic "OCEAN CURRENTS OF THE WORLD". Hope you like it. If you like it then please, *like*, *Download* and *Share*.
By- Slide_maker4u (Abhishek Sharma)
*******For presentation Orders, contact me on the Email addresses Written below********
Email- Sharmaabhishek576@gmail.com
or
Sharmacomputers87@gmail.com
*******THANK YOU***************
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDOUS ENVIRONMENTS RESULTING FROM MASS MOVEMENTS. It contain case studies: Italian Mudslides 1998, New Zealand Landslip 1979, European Avalanches 1999.
This document provides an overview of coastal environments and processes. It defines coastal zones and features such as the littoral zone, beach, foreshore, and backshore. It describes factors that influence coastal areas like lithology, geological structures, processes, sea level changes and human impacts. Coastal processes discussed include waves, tides, storm surges, wave refraction, and marine erosion. The summary discusses key coastal landforms and how they are formed by coastal processes.
Waves are formed by wind blowing over the surface of the sea. The height and energy of waves depends on wind strength, duration, and fetch. There are two main types of waves - constructive waves which build land, and destructive waves which erode land. Coastal geology also influences landscapes. Discordant coasts have bands of rock at 90 degrees to the sea, creating headlands and bays as softer rocks erode faster. Concordant coasts have parallel rock bands, where erosion of harder rocks leads to fast erosion of softer rocks behind.
This document provides summaries of key concepts related to physical geography. It discusses the main features of rivers including the source, tributaries, confluence, watershed and mouth. It explains how rivers shape the land through erosion and how meanders and lakes are formed. It also summarizes coastal landforms including how waves erode and deposit material, and causes of cliff erosion. Additional topics covered include glaciation, rocks and weathering, plate tectonics, British weather/climate, and the world's main climates.
This document provides an introduction to describing natural landscapes. It discusses key components of natural landscapes including variations within a landscape from climatic, tectonic and erosion processes. It also addresses how human activities and cultural perspectives can impact natural landscapes. Settings like the Amazon Basin and Tongariro Volcanic Centre in New Zealand are given as examples. The formation of different landforms through geological processes like folding, faulting and volcanism are explained. Erosion, transportation and deposition processes are also summarized.
This document discusses coastal landforms and processes including constructive and destructive wave characteristics, erosion processes like abrasion and hydraulic action, cliff retreat and wave cut platforms. It also discusses coastal management strategies like hard engineering options such as sea walls, revetments and groynes, and soft engineering options like beach replenishment, cliff regrading and managed retreat. The document concludes with an example of coastal management at Swanage which uses beach replenishment, groynes, cliff regrading and drainage.
Equation of the Line ppt for grade 8 mathematicsROWELLJAYMALAPIT
Climate is determined by a location's long-term patterns of temperature and precipitation, which are influenced by several climate controls. The key climate controls are latitude, proximity to water, altitude/elevation, proximity to mountains, ocean currents, and prevailing winds. Latitude affects temperature and precipitation through its influence on solar radiation and atmospheric convection cells. Proximity to large bodies of water moderates temperatures and brings more precipitation. Higher elevations generally experience colder temperatures. Mountains can produce rain shadows on their leeward sides through atmospheric lifting and cooling effects. Ocean currents redistribute heat around the globe. Prevailing winds influence weather patterns.
This document discusses coastal erosion and mechanisms. It defines coastal terminology and describes the various agents that affect coastal erosion, including wind, waves, tides, and currents. It also examines the erosional and depositional landforms created by coastal processes, such as headlands, sea stacks, beaches, and barrier islands. Additionally, it covers the concepts of coastal erosion, longshore drift, and coastal deposition. The effects of coastal erosion are also addressed, as well as the importance of understanding coastal dynamics and implementing mitigation strategies to reduce erosion.
Presentation on the different factors controlling weathering. In this we discuss the basic concepts is weathering and explain in breif the various factors controlling them.
The physical environment chapter discusses the components that make up Earth's physical environment: land, air, water, and the living environment. It describes key landforms like mountains and rivers, as well as geological processes that create and modify landforms such as plate tectonics, folding, volcanism, and erosion. Weathering and erosion by forces such as water, wind, and plant growth gradually break rocks into sediment and transport material from one place to another over long periods of time, shaping the surface of the planet. Human activities and settlement patterns are also influenced by landforms and geological characteristics of different regions.
This document discusses sea breezes and their formation and forecasting. It notes that:
- Sea breezes form due to differential heating between land and water surfaces, with warmer land driving an onshore breeze.
- Their strength and inland penetration depend on factors like the land-sea temperature difference, coastline shape, terrain, and the prevailing synoptic-scale weather patterns.
- Forecasting sea breezes requires considering how the synoptic-scale flow will affect surface heating over land and the development of the sea breeze circulation. Onshore flow favors sea breezes while offshore flow impedes them.
This document provides an overview of coastal environments and processes. It begins with key thinking questions about coasts and their value. It then defines coasts and describes their main zones or parts. Two main factors that affect the coastal environment are tides and sea level changes. The document also discusses coastal erosion processes like abrasion and hydraulic action. Finally, it introduces coastal landforms like cliffs, shore platforms, headlands and bays that result from erosion.
The document discusses various coastal landforms created by waves and wind including beaches, sea cliffs, wave-cut platforms, stacks, spits, and barrier islands. It also examines different types of tides and their influence on coastal features. Additionally, it describes various dune types such as barchan, parabolic, transverse, and longitudinal dunes that are formed by wind erosion and transportation of sand particles. The document concludes by discussing loess deposits of wind-blown glacial sediment.
Coastal erosional processes and landforms lesson 4Ms Geoflake
The document discusses coastal erosion processes and landforms. It describes the four main erosion processes as corrosion, abrasion, solution, and hydraulic action (CASH). These processes break down and transport sediment, forming features like sea cliffs, caves, arches, stacks, and stumps. Waves erode the base of cliffs and headlands through processes like hydraulic action, creating wave-cut notches and platforms that eventually result in arches and isolated rock columns. Alternating hard and soft rock layers produce headlands and bays along discordant coastlines.
This document provides a quick revision on various topics for a geography exam, including regional winds like monsoons, local winds such as land and sea breezes, landforms caused by plate tectonics, and impacts of natural disasters. It discusses the monsoon winds between Asia and Australia, explaining the southwest and northeast monsoons. It also explains the phenomena of land and sea breezes. Regarding plate tectonics, it compares different plate boundary types and their associated landforms. Finally, it lists some factors that affect earthquake damage.
This document discusses factors that affect coastal environments. Coasts are dynamic and constantly changing due to natural factors like waves, tides, currents, geology and ecosystems, as well as human activities such as building ports, marinas, and tourism. Waves are generated by wind and their size depends on wind speed, duration and fetch. As waves approach shore, they slow down, grow taller and change shape, eventually breaking on the beach and releasing energy that erodes the coastline.
The document discusses several key topics related to meteorology and how weather conditions impact agriculture. It defines meteorology as the study of the atmosphere and weather, and agricultural meteorology as how weather impacts agricultural production. Several factors that influence regional climates are outlined, including latitude, pressure systems, altitude, proximity to bodies of water, ocean currents, winds and air masses. Understanding these relationships is important for agricultural planning and management.
The document provides an overview of an environmental management course. It discusses nine course topics related to human interactions with the environment, including rocks and minerals exploitation, energy/agriculture/water management, oceans/fisheries, natural hazards, atmosphere, population, and ecosystems. Assessment methods are not described in detail. The course aims to provide local and global perspectives on sustainability, human needs/values, and the future of the environment.
The document discusses various topics related to oceanography including ocean bottom relief, islands, coral reefs, coral bleaching, movement of ocean water through waves, currents and tides, and salinity of ocean water. It provides details on factors influencing ocean currents like rotation of Earth, air pressure, density gradients, and Coriolis force. Types of islands like continental, volcanic, coral and sandbar are described along with examples. Formation and types of coral reefs as well as conditions for coral growth are summarized.
Waves, tides, and currents are important components of ocean motion. Waves are caused by wind and transfer energy across the ocean surface, shaping coastlines through erosion and deposition. Tides are the daily rise and fall of sea levels caused by the gravitational pull of the moon and sun, forming tidal bulges. Major tide types include semidiurnal, spring, and neap tides. Ocean currents are large flows of water driven by factors like wind, the Coriolis effect, and temperature/density changes. Surface currents are wind-driven while deep currents flow more slowly due to density. The Gulf Stream transports warm water from the Gulf of Mexico north along the eastern US coast.
Introduces Oceanography: oceanic plates, continental shelf, abyssal plain, trenches, hydrothermal vents, black smoke, temperature stratification, water masses and circulation, coriolis effect, el nino, larvae and larval ecology.
Natural and cultural factors create differences within Tanzania. Natural factors like drought, soil erosion, and access to coastal regions impact rural areas more due to reliance on subsistence farming. Cultural factors such as colonial infrastructure investment in urban areas, political policies encouraging village settlements, and lack of rural employment and infrastructure exacerbate inequality. Differences also exist between gender due to traditional roles, education disparities, and limited female opportunities. The Maasai face distinct challenges from their nomadic traditions and low education. Tourist areas benefit economically from infrastructure investment and tertiary jobs related to natural attractions.
Factors contributing to differences in developmentTaka Geo
The Difference between Natural and cultural Factors in Differences in Development. Geography AS91242. This is really important ! learn it up good ! #geo4lyfe
This document provides guidance on constructing various types of graphs, including bar graphs, line graphs, climate graphs, percentage bar graphs, scatter plots, and pictographs. It explains the key elements that should be included in each graph, such as labeled axes, a title, legend/key, and scale. Examples of properly constructed graphs are also provided for each type to demonstrate how the guidance should be applied.
This document provides information and guidance for a Year 11 Geo exam on extreme natural events. It outlines the exam date, required materials, and examiner expectations. Volcanic eruptions are chosen as the natural event, with case studies of Mt. Tarawera in 1886 and Mt. Pinatubo in 1991 recommended for study. The document provides detailed descriptions of the natural processes leading to volcanic eruptions and the effects on cultural and natural environments. It also discusses characteristics making environments vulnerable and how different groups have responded over the short and long term. Diagrams are suggested to help explain concepts. Students are advised to thoroughly learn facts about two case studies.
This document provides a map and key of the Muriwai/Maori Bay coastal environment, showing selected natural features. The map displays the Muriwai/Maori Bay coastal area and marks important natural parts of the beach. A key below the map frame labels the different parts of a beach.
This document provides an overview of tourism development as a cultural process that can shape geographic environments. It discusses the operation of tourism development, including interactions between tourists, attractions, facilities, and regulators. It also addresses temporal variations in tourism development over time, dividing the process into four stages based on the Butler model from few tourists and attractions to a peak in tourism. Specific details are given about tourism development in Rotorua and Waikiki at different stages to demonstrate changes over time in these locations.
The borneo adventure pre trip meeting presentationTaka Geo
The document outlines a 10 day itinerary for travel through Malaysia, beginning in Auckland, New Zealand and ending back in Auckland. The itinerary includes domestic flights within Malaysia between several cities and destinations, including Kuala Lumpur, Kinabatangan River Lodge, Kuching, and others. Various activities are planned such as visiting orangutan centers, city tours, trekking, and exploring beaches and villages. Lodging is arranged throughout the trip, and contact information is provided in case of any questions regarding the itinerary.
This document provides essential information for New Zealanders travelling overseas, including:
- Advising travelers to log on to www.safetravel.govt.nz before departing to access travel advisories, register travel plans for emergency contact, and view travel checklists.
- Outlining the top 10 travel tips, including researching destinations, obtaining travel insurance and vaccinations, registering travel plans online, advising contacts of plans, obeying local laws, and safeguarding passports.
- Providing details on passport requirements including how to obtain or replace a passport in New Zealand or overseas, and tips for keeping passports secure.
The hawaii adventure final parents meetingTaka Geo
This document provides information about an upcoming trip to Hawaii from July 8-17. It includes details about flights, accommodations, activities planned each day including tours of Oahu and the Big Island, and practical tips about money, communication, and safety. Students will stay at the Ohana Malia Waikiki hotel and participate in activities like visiting Diamond Head, taking a round-the-island tour, shopping outlets, visiting volcanoes, beaches, and museums. Recommendations are given for mobile phones, money, and ensuring student safety during free time.
The document outlines the itinerary for Hawaiian Students Meeting in June 2014. The first day includes arriving in Honolulu at 9:45am after departing Auckland at 11:55pm, participating in The Amazing Race at 11:00am for $10, climbing Diamond Head in the afternoon, and having dinner at the Hard Rock Cafe for $30 with a night swim. Subsequent days include a grand circle island tour, shopping trips, a volcano day tour to Hilo, and free choice dinners. The document provides additional details on cash, insurance, power adapters, and meeting times.
The document outlines the standard format for presenting on a geographic issue. It should include:
1) A description of the issue including a map showing its location and how it relates to concepts. It should also discuss the size and natural/cultural characteristics of the area and effects.
2) Two proposed solutions to the issue with a brief description of each, including costs, locations, and people affected. A picture or map should also be included.
3) An explanation of how people's responses to the issue are influenced by their values and perceptions, including specific actions people took in response.
4) Choosing one solution and justifying why it is better than the alternatives, discussing strengths and weaknesses like
Travel insurance can be obtained without filling out forms, but those with medical conditions must call a medical line for assessment after the policy is issued, and there may be a surcharge. Laptops and cameras are covered according to the conditions specified on the given website. The website provides more details on travel insurance and should be read.
This document provides information for parents and students about the International Baccalaureate Diploma Programme (IBDP) at a school. It discusses the IB learner profile, which describes desirable student attributes like being inquirers, thinkers, communicators, and balanced. It also describes CAS (creativity, action, service), a required element where students actively learn outside the classroom through artistic endeavors, physical activities, and community service. The document outlines the goals of CAS and the roles of students and their advisors in planning and reflecting on CAS activities. Examples of successful past CAS projects are also provided.
Urbanization is the increase in the proportion of people living in cities and towns. It occurs as people move from rural to urban areas, usually as a country develops. In the UK, the London Docklands area experienced urban decline in the 1950s as larger ships could no longer access the port, leading to unemployment and deteriorating housing. In 1981, the London Docklands Development Corporation was established to redevelop the area, attracting new industries, renovating housing, and improving transport and leisure facilities through initiatives like the Docklands Light Railway. However, some oppose the changes as original residents can no longer afford to live there and new jobs do not match the skills of former dock workers.
This document provides information and deadlines for an upcoming trip, including needing passports by the end of the weekend and paying outstanding fees by early June. It also mentions an upcoming meeting to finalize last-minute details for the trip and checks that registration has been completed online. Additionally, it provides guidance on documenting activities in Managebac by including a title, description, and reflection, and notes the need to reflect regularly. Finally, it announces that the school will host visiting overseas schools as tour guides to raise money for projects, and outlines upcoming beach and school cleanup events.
The document provides information for students attending a meeting in Hawaii in May 2014. It includes details on room assignments with 4 beds per room and power adapters needed. An updated rooming list is available online. The itinerary is also set and available online. Students should bring a change of clothes and walking shoes. Forms need to be signed and returned soon. Information is provided on using cell phones overseas and internet access. What to bring for a volcano tour or other activities is outlined. Travel insurance needs to be arranged and medical conditions declared. Payment deadlines of $3000 by early June and $3200 by late June are noted along with payment details.
This document provides guidance and instructions for students to complete tasks related to analyzing and presenting geographic data from two beaches. It outlines seven tasks for students to: 1) Present data in three formats with proper conventions; 2) Analyze the data to describe differences between the beaches and explain why differences occur; 3) Draw conclusions related to the original research questions; 4) Evaluate the strengths and weaknesses of the research process and suggest alternative methods. Marking criteria are provided for each task with requirements to achieve, merit or excellence levels.
This document discusses a contemporary geographic issue in New Zealand - the need for a second harbour crossing in Auckland. It provides background on Auckland's population growth, reliance on the existing Auckland Harbour Bridge, and challenges of connecting the growing northern sector. Three options for addressing the issue are presented: building a new harbour bridge, a new tunnel, or doing nothing and promoting public transport. The task is to research and evaluate each option, and recommend the best course of action with detailed reasoning.
The document outlines a 10-day itinerary for a Borneo adventure trip, including:
- Flights from Auckland to Kuala Lumpur and Sandakan, with overnight stays in motels and lodges.
- Multi-day stay in Kinabatangan River Lodge, including nature cruises and visits to Oxbow Lake.
- Day trips to Sepilok Orangutan Rehabilitation Center and Semonggok Orangutan Rehab.
- Trek through countryside and local village, including river crossings and waterfall visit.
- Sightseeing in Kuching and Kuala Lumpur before returning flight to Auckland.
L1 Social Studies 1.1 practice external powerpointTaka Geo
This document provides instructions for an assessment on describing cultural change using the Vikings as a case study. Students will research how Viking culture changed from the 8th-11th centuries to modern cultures of Norway, Sweden and Denmark. They are to describe: the cultural change and groups involved; contrasting viewpoints on the change; and processes (like assimilation, colonization, integration of new ideas) that led to change and why these were important. Students will complete initial research, plan their response using a template, and have three periods to write their assessment response using open notes.
This presentation includes basic of PCOS their pathology and treatment and also Ayurveda correlation of PCOS and Ayurvedic line of treatment mentioned in classics.
Macroeconomics- Movie Location
This will be used as part of your Personal Professional Portfolio once graded.
Objective:
Prepare a presentation or a paper using research, basic comparative analysis, data organization and application of economic information. You will make an informed assessment of an economic climate outside of the United States to accomplish an entertainment industry objective.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
How to Fix the Import Error in the Odoo 17Celine George
An import error occurs when a program fails to import a module or library, disrupting its execution. In languages like Python, this issue arises when the specified module cannot be found or accessed, hindering the program's functionality. Resolving import errors is crucial for maintaining smooth software operation and uninterrupted development processes.
Biological screening of herbal drugs: Introduction and Need for
Phyto-Pharmacological Screening, New Strategies for evaluating
Natural Products, In vitro evaluation techniques for Antioxidants, Antimicrobial and Anticancer drugs. In vivo evaluation techniques
for Anti-inflammatory, Antiulcer, Anticancer, Wound healing, Antidiabetic, Hepatoprotective, Cardio protective, Diuretics and
Antifertility, Toxicity studies as per OECD guidelines
June 3, 2024 Anti-Semitism Letter Sent to MIT President Kornbluth and MIT Cor...Levi Shapiro
Letter from the Congress of the United States regarding Anti-Semitism sent June 3rd to MIT President Sally Kornbluth, MIT Corp Chair, Mark Gorenberg
Dear Dr. Kornbluth and Mr. Gorenberg,
The US House of Representatives is deeply concerned by ongoing and pervasive acts of antisemitic
harassment and intimidation at the Massachusetts Institute of Technology (MIT). Failing to act decisively to ensure a safe learning environment for all students would be a grave dereliction of your responsibilities as President of MIT and Chair of the MIT Corporation.
This Congress will not stand idly by and allow an environment hostile to Jewish students to persist. The House believes that your institution is in violation of Title VI of the Civil Rights Act, and the inability or
unwillingness to rectify this violation through action requires accountability.
Postsecondary education is a unique opportunity for students to learn and have their ideas and beliefs challenged. However, universities receiving hundreds of millions of federal funds annually have denied
students that opportunity and have been hijacked to become venues for the promotion of terrorism, antisemitic harassment and intimidation, unlawful encampments, and in some cases, assaults and riots.
The House of Representatives will not countenance the use of federal funds to indoctrinate students into hateful, antisemitic, anti-American supporters of terrorism. Investigations into campus antisemitism by the Committee on Education and the Workforce and the Committee on Ways and Means have been expanded into a Congress-wide probe across all relevant jurisdictions to address this national crisis. The undersigned Committees will conduct oversight into the use of federal funds at MIT and its learning environment under authorities granted to each Committee.
• The Committee on Education and the Workforce has been investigating your institution since December 7, 2023. The Committee has broad jurisdiction over postsecondary education, including its compliance with Title VI of the Civil Rights Act, campus safety concerns over disruptions to the learning environment, and the awarding of federal student aid under the Higher Education Act.
• The Committee on Oversight and Accountability is investigating the sources of funding and other support flowing to groups espousing pro-Hamas propaganda and engaged in antisemitic harassment and intimidation of students. The Committee on Oversight and Accountability is the principal oversight committee of the US House of Representatives and has broad authority to investigate “any matter” at “any time” under House Rule X.
• The Committee on Ways and Means has been investigating several universities since November 15, 2023, when the Committee held a hearing entitled From Ivory Towers to Dark Corners: Investigating the Nexus Between Antisemitism, Tax-Exempt Universities, and Terror Financing. The Committee followed the hearing with letters to those institutions on January 10, 202
বাংলাদেশের অর্থনৈতিক সমীক্ষা ২০২৪ [Bangladesh Economic Review 2024 Bangla.pdf] কম্পিউটার , ট্যাব ও স্মার্ট ফোন ভার্সন সহ সম্পূর্ণ বাংলা ই-বুক বা pdf বই " সুচিপত্র ...বুকমার্ক মেনু 🔖 ও হাইপার লিংক মেনু 📝👆 যুক্ত ..
আমাদের সবার জন্য খুব খুব গুরুত্বপূর্ণ একটি বই ..বিসিএস, ব্যাংক, ইউনিভার্সিটি ভর্তি ও যে কোন প্রতিযোগিতা মূলক পরীক্ষার জন্য এর খুব ইম্পরট্যান্ট একটি বিষয় ...তাছাড়া বাংলাদেশের সাম্প্রতিক যে কোন ডাটা বা তথ্য এই বইতে পাবেন ...
তাই একজন নাগরিক হিসাবে এই তথ্য গুলো আপনার জানা প্রয়োজন ...।
বিসিএস ও ব্যাংক এর লিখিত পরীক্ষা ...+এছাড়া মাধ্যমিক ও উচ্চমাধ্যমিকের স্টুডেন্টদের জন্য অনেক কাজে আসবে ...
A review of the growth of the Israel Genealogy Research Association Database Collection for the last 12 months. Our collection is now passed the 3 million mark and still growing. See which archives have contributed the most. See the different types of records we have, and which years have had records added. You can also see what we have for the future.
How to Add Chatter in the odoo 17 ERP ModuleCeline George
In Odoo, the chatter is like a chat tool that helps you work together on records. You can leave notes and track things, making it easier to talk with your team and partners. Inside chatter, all communication history, activity, and changes will be displayed.
2. In this session:
• It will be more like a lecture because of time
• I suggest you listen and understand rather than trying to
make copious notes
• I will make the power point available on knowledge net
so you can look at it in more detail later.
3. This standard is titled:
Demonstrate understanding of
how interacting natural processes
shape a New Zealand
geographic environment
4. This standard is titled:
Shape is how it was made
and modified and how it is
being modified now
Demonstrate understanding of
how interacting natural processes
shape a New Zealand
geographic environment
5. This standard is titled:
This is plural so you need more
than one process
Demonstrate understanding of
how interacting natural processes
shape a New Zealand
geographic environment
6. This standard is titled:
Demonstrate understanding of
how interacting natural processes
shape a New Zealand
geographic environment
Your geographic environment is the South Muriwai
Coastal Environment (SMCE)from Maori Bay to
Okiritoto Stream (learn this)
7. Hence to score marks you
must:
• 1. Analyse not just describe (always give
depth)
• 2. Use 2 different processes in the paper
• 3. Mention South Muriwai throughout
answers
8. We will break up this revision
session into:
• 1. Going over content
• 2. How To answer Questions
• 3. What to expect with this exam.
10. 3.1 CONTENT
• Demonstrate comprehensive understanding of how interacting
natural processes shape a New Zealand geographic environment
involves:
• • providing an insightful analysis of the interacting natural
processes and how they shape the environment
• • integrating comprehensive supporting case study evidence.
• An insightful analysis includes an analysis of the interaction
between the processes and
11. THE SIZE AND EXTENT OF THE
ENVIRONMENT
Okiritoto Stream
what is the
distance?
Maori Bay
12. ITS LOCATION
General: It is on the west
coast of the North Island
Specific: 40km NW of
Auckland CBD . It lies
between the Manukau and
Kaipara harbours at
36°49'00"S and 174°27'00"E
13. THE CHARACTERISTICS OF THE
SETTING
• These can be divided into the:
INPUTS
Elements
PROCESSES
Processes
OUTPUTS
Features
What the
‘things’ are
that make up
the
environment
The actions
that occur
between
elements
The result of
the
processes
Eg Wave
erosion
Eg a stack
Eg Sand
14. Lets look at these in detail: The Elements that
give it specific characteristics
WATER ELEMENTS
LAND ELEMENTS
AIR ELEMENTS
Waves- Average 1.5 m,
high energy due to
2,000km fetch over
Tasman
Relief – flat beach (0-5 degrees)
while headland up to 200m
Wind: Blows over
11knots 42% of time
from SW.
Currents – strong rips
Sediment - white is quartz and
feldspar (0.5mm diameter) and
black titano-magnetite
(0.25mm)
Geology: Headland of Manukau
Breccias while beach sandstone.
Vegetation: dune plants like
Spinifex and pingao, headland of
flax, Manuka and Pohutakawa.
Animals: 1,200 pairs of Gannets
15. Main Processes we study are:
HIGH SCALE
MIDDLE SCALE
SUB-PROCESS
WAVE ACTION
Wave Formation
Refraction
Reflection
Wave Transport and
deposition
Longshore drift
Wave Erosion
Hydraulic Action
Corrasion
Corrosion
Spray-splash action
Wind Transport
Saltation
(suspension and creep)
WIND ACTION
(AEOLIAN ACTION)
Wind deposition
NB: Any of these count as 2 different processes
16. Other processes you can
mention:
HIGH SCALE
LOWER SCALE
TECTONIC
Volcanism
Faulting
CLIMATOLOGICAL
Aerial weathering
BIOLOGICAL
Vegetation Growth
Biochemical weathering
Use these if answering about formation of features
(several processes) but avoid if asked to analyse ONE
process.
17. The Main Features and their
characteristics are:
FEATURE
CHARACTERISTICS
HEADLAND
400M long, cliffs 30m high and top of
headland 200m. Made of resistant
Manukau Breccias. Dense vegetation
on top of trees and flax.
STACK
30m high and 20m from headland.
More eroded landward side. Gannet
colony on top. Manukau Breccias.
BEACH
Foreshore 150m wide with small
berm, flat 1-5 degrees only . Black
ironsand accumulates at top.
DUNES
Av 8m, white sand dominates,
stablised by fast growing dune plants
with good root system. Plants
adapted to salt and wind.
PICTURE
19. These are all related:
ELEMENT ONE
PROCESS
FEATURE
ELEMENT TWO
WAVES
WAVE EROSION
GEOLOGY
STACK
20. Criteria 2: Natural processes that
operate
• A process is a series of actions.
• Therefore you must show this in your answer
• This happens first, then this and then this.
• Pick high scale processes as you have more to
talk about. Remember to analyse.
21. WAVE ACTION - due to strong winds, long fetch
• 1. High Energy Waves form WHY
• 2. Approach Muriwai environment from SW – WHY due to prevailing winds
• 3.Waves bend or refract off the headland WHY waves slow down here first as
hit shallow water.
• 4. Energy or orthogonals concentrates on headland WHY due to the refraction
of waves
• 5. When hit the headland they erode HOW by hydraulic action of pressure
differences, corrosion or chemical weathering or corrasion or battered by
sediment in waves. Weak areas are attacked between high and low tide mark
forming crevasses that get bigger.
• 6. Notch develops that over time becomes a cave. As on 3 sides becomes an
arch and roof weakened HOW by gravity, vegetation growth and biochemical
weathering so collapses to form an isolated stack.
22. WIND ACTION
• 1. Strong winds blow on shore WHY prevailing winds in SW belt.
• 2. On beach they pick up sediment and move it in 3 ways
suspension, saltation or creep WHY depends on size. Most at Muriwai
saltated.
• 3. Moves to backshore in bouncing fashion WHY light enough to be carried
by wind but weight brings back to land.
• 4. At backshore continues until wind strength reduced and deposition
occurs instead. WHY usually occurs when reach an object or plants on
dunes. Sets up zone of zero wind velocity.
• 5. Over time dunes grow in size WHY As plants are buried shoots grow
upwards effecting zone of zero wind.
23. Criteria 3:The distribution and formation
of the natural features
• Distribution refers to where they occur.
• Why do dunes occur at back of beach and not on
the headland?
• Why does the stack occur at end of headland
and not back of beach?
• All the result of what the characteristics of the
features are like.
24. How Features are Formed
• Suggest do either the stack or dunes.
• Often asks for several processes involved in the formation of
the feature
• Stack result of : volcanism (caused resistant rock), Tectonics
(push above sea), Wave Erosion, aerial weathering and
biochemical weathering above high tide level.
• Dunes result of: Saltation, Aeolian deposition and Vegetation
Growth
25.
26. Criteria 4: Spatial variations in the operation of
natural processes in the geographic environment
• What this means: Where a process happens most and
least.
• You must answer by saying where it dominates, happens
a lot, does not happen etc.
• This is due to differences in the elements as they are not
equally distributed in the environment. For Muriwai
break down into 3 sub areas of Muriwai
beach, Otakamiro Headland and Maori Bay.
27. MURIWAI BEACH
OTAKAMIRO HEADLAND
MAORI BAY
Wide flat area
Hilly
Flat beach but small and cliffs
at back
Wind onshore and
strong
Strong onshore wind
Winds confused by stack
Waves less energy as
orthogonals diverge
Waves strong as
orthogonals converge
Waves also confused by shape
Lots of loose
(unconsolidated)
sediment
No loose sediment only
solid rock
Loose sediment on beach but
more black sand
As wave erosion needs converging waves and hard rock happens most on
headland, a little at Maori Bay and only in storm conditions at Muriwai
Beach.
As saltation needs loose sediment and a wide flat area to operate this
occurs most at Muriwai beach, only a little at Maori Bay and not at all at
the headland.
28.
29. Criteria 5: Temporal variations in the
operation of natural processes in the
geographic environment
• This is similar but over time. Processes do not occur
consistently but happen more at some times (when elements
required are favourable) compared to other times when are
sparse.
• In our case the best examples relate to summer versus winter.
30. SUMMER
WINTER
Highs dominate in Tasman
Depressions dominate in Tasman
Produce gentle spiller waves and
light breezes
Produce plunger waves and strong winds
often of storm condition.
Wave Action: Gentle spiller waves have greater swash than backwash, deposit
more than remove so build up beach profile.
Strong plunger waves have stronger backwash than swash so remove more
sediment than deposit leaving flatter profile. Taken to sand bar.
Wind Action: Gentle breezes in summer mean that saltation is not as common.
As a result the dunes are not replenished as much as in storm conditions in
winter.
31.
32. • Wave Erosion
• 1. Building of solid wall in 80’s. No good as energy directed
downwards and wall collapsed.
• 2. Building of gabion cage in 90’s. Better as wave energy dissipates
through spaces between rocks. However in storms so much water
so a lot reflected off wall and onto the southern part of beach
causing excessive erosion. Had outcome of a flatter beach at
this end.
• 3. Rip Rap in 2005 means more spaces for storms and extra
protection. Outcome is that wave erosion is reduced.
• All actions deliberate and aim to protect access to Fisherman’s rock.
Now successful
33. • Wind Action
• 1. Some actions accidental such as building surf club tower. Sets up
zone of zero wind velocity and sand builds up against wall as wind
deposition increased. This caused it to be buried. Had to be moved
backwards 3 times.
• 2. Also effects of farming in 1880’s and dune surfing in 1980’s.
Remove protective vegetation cover so cannot stop saltation from
increasing.
• 3. Deliberate sand stabilisation schemes of 1931 and 1969 helped
to increase wind deposition by planting first marram grass and then
spinifex on dunes. First one too successful as dense vegetation so
dunes collapsed. Second better allowing some saltation to
continue. Outcome is stable dunes.
34. End of content
• Do you feel you understand this
better?
• Get up and have a 1 min break.
35. Part B: How To Answer
questions
• They are asked in 3 ways:
• 1. An Essay (diagrams may be included)
• 2. A diagram only (one or a series of them)
• 3. A diagram for (a) with a written component
for (b)
37. Rules for different grades:
• Be clear what the different grades are
awarded for
• There are 2 sorts of mark per question
• 1 refers to depth of answer
• 1 refers to use of specific information
38. Let’s look at depth of answer first:
• Analyse the operation of one process (forget environment
here)
• The waves come in and hit the headland
and cause erosion
• This gets an NA as does not analyse. How
is erosion caused?
39. • The waves come in and refract so that they
concentrate on the headland and erode it
where it is weaker
• This now would get an A as has some
explanation/ analysis in it
40. • The waves come in and slow down off the
headland first so that they refract or bend
which concentrates the energy of the
waves onto the headland. Sub-processes
of wave erosion such as hydraulic action
and corrosion then attack the rock where
it is weaker and break it down.
• This has some depth so gets a Merit.
41. To lift this further you need to give
technical understanding
• The wave velocity slows as it approaches the shoreline
due to the frictional drag caused when the wave hits the
bottom. This causes the wave to bend or refract and
concentrates the orthgonals or wave energy on the end
of the headland. Here processes such as hydraulic action
(pressure differentials when air is forced into
joints), corrasion (waves using sediment to batter the
rock) and corrosion (chemical breakdown of the minerals
in the rock by seawater) break down the resistant rock
between high and low water to form a notch.
42. Then you must add specific
information to this:
• First time it is linked to setting is equal to an A
• When 3 mentions made becomes an M
• When more than 3 used throughout the answer
becomes an E.
43. So if we take our Excellence
example it becomes:
• Waves at Muriwai have high energy due to the 2,000km
fetch across the Tasman sea and average 1 ½ m in height.
The wave velocity slows as it approaches the South
Muriwai shoreline due to the frictional drag caused when
the wave hits the bottom. This causes the wave to bend
or refract and concentrates the orthgonals or wave
energy on the end of Otakamiro headland. Here
processes such as hydraulic action (pressure differentials
when air is forced into joints), corrasion (waves using
sediment to batter the rock) and corrosion (chemical
breakdown of the minerals in the rock by seawater)
break down the resistant Manukau Breccia rock between
high and low water to form a notch.
44. What Are the other rules about
essays?
• 1. Read the question carefully and highlight key words
• 2. Do a rough plan on the planning page and keep to it.
• 3. It needs an introduction, body and conclusion
• 4. You must write in full sentences. Bullet points or note form
is only able to score a maximum of an A.
• 5. Use space as a guide to length needed. Aim to fill this.
• 6. Try to include at least one diagram even if rough and refer
to it in text.
45. Learn a few short cuts:
• Start with a standard paragraph that includes
your 3 specifics:
• South Muriwai beach is located 40km NW of
Auckland CBD and extends from Okiritoto stream
in the north to Maori Bay 5km south. (then
restate question)
• Specifics can also count in a map so include this.
46. What About Rules for
Diagrams
• It is important to establish if this is:
• 1. A stand alone diagram question
• 2. A diagram as part (a) with written part (b)
• 3. A diagram within an essay
47.
48.
49. Part 3 : What is this years exam
likely to look like?
50. Assessment Specifications
• Candidates will be provided with a choice of
TWO questions to answer.
• Candidates will be expected to answer ONE
question using both an annotated map or
diagram and a related written component.
• Both parts contribute toward the single grade
that will be awarded.
51. • Format of the assessment
• Candidates should use specific information and / or case
studies to illustrate their answers
•
• Equipment to bring
• Scientific calculator, coloured pencils, and a ruler.
• Candidates should use coloured pencils in their diagrams /
maps. Annotations on these diagrams / maps must be in pen.
Any work done in pencil will not be eligible for reconsideration.
52. How To Answer annotated
diagrams
• If asked to draw a map/diagram it must have its
FACKTS
• You must make it specific to your environment ie
Muriwai
• You must annotate it to show HOW something
happens.
53.
54. Finally:
• Remember to include at least 5 statistics in your answer
• Make it focus on Muriwai.
• Read the question twice and underline important words.
• GOOD LUCK FROM US ALL!!!