A PowerPoint for Year 10 Human Wellbeing (Geography) based on Australian Curriculum
If you download, send me an email and let me know how you found it/ how you used it.
markmodra@gmail.com
This document defines and describes the main types of weathering processes that occur at the Earth's surface: mechanical, chemical, and biological. Mechanical weathering involves physical breakdown through processes like frost wedging and abrasion without changing the rock's chemical composition. Chemical weathering decomposes rocks through reactions with substances like carbon dioxide, water, and oxygen. Biological weathering disintegrates rocks through organism activities like plant roots, lichen/algae growth, and burrowing. Different rock types and climates result in variable weathering rates.
This document provides an overview of geomorphological processes and environments. It begins with defining geomorphology as the scientific study of landforms and the processes that shape them. It then discusses various landform features seen on Earth's surface and how geomorphology seeks to understand the processes behind their formation. The document outlines different agents of geomorphic processes like rivers, wind, glaciers and waves. It categorizes geomorphic processes into terrestrial and extra-terrestrial processes, with terrestrial processes further divided into exogenetic and endogenetic processes. Key exogenetic processes discussed include weathering, erosion, transportation, deposition and mass movement, while endogenetic processes include faulting, folding, volcanism, earthquakes, land
Mass wasting refers to the downslope movement of soil, rock debris, and bedrock under the force of gravity. It is a form of erosion and transportation that can occur slowly over geologic time or suddenly during catastrophic events. The main types of mass wasting are slides, flows, falls, and creep. Factors that influence mass wasting include slope angle, rock/soil type, water content, climate, earthquakes/volcanic activity, and pre-existing weaknesses in bedrock. Common landslide types are slumps, debris flows, rock slides, and debris slides/slumps. Creep is a very slow form of downslope movement caused by processes like wetting/drying, freezing/thawing, and
This document provides an overview of maps and map projections. It defines what a map is, discusses scale and map projections, and classifies the main types of projections as cylindrical, conic, and planar. It then describes some commonly used projections in more detail, like the Mercator, UTM grid, Lambert Conformal Conic, and Albers Equal-Area Conic projections. The document concludes that map projections transform the spherical Earth into a flat plane and are fundamental to mapmaking.
The document discusses jet streams, which are narrow bands of strong wind that form in the upper atmosphere. Jet streams typically flow from west to east at speeds of up to 250 mph at altitudes between 8-16 km. They form along boundaries between hot and cold air masses, driven by pressure differences and the Coriolis effect from Earth's rotation. There are two main types of jet streams: the polar front jet at 50-60 degrees latitude and the subtropical jet at 30 degrees latitude. Jet streams play a key role in determining weather patterns and steering cyclonic storms.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive function. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
This document defines and describes the main types of weathering processes that occur at the Earth's surface: mechanical, chemical, and biological. Mechanical weathering involves physical breakdown through processes like frost wedging and abrasion without changing the rock's chemical composition. Chemical weathering decomposes rocks through reactions with substances like carbon dioxide, water, and oxygen. Biological weathering disintegrates rocks through organism activities like plant roots, lichen/algae growth, and burrowing. Different rock types and climates result in variable weathering rates.
This document provides an overview of geomorphological processes and environments. It begins with defining geomorphology as the scientific study of landforms and the processes that shape them. It then discusses various landform features seen on Earth's surface and how geomorphology seeks to understand the processes behind their formation. The document outlines different agents of geomorphic processes like rivers, wind, glaciers and waves. It categorizes geomorphic processes into terrestrial and extra-terrestrial processes, with terrestrial processes further divided into exogenetic and endogenetic processes. Key exogenetic processes discussed include weathering, erosion, transportation, deposition and mass movement, while endogenetic processes include faulting, folding, volcanism, earthquakes, land
Mass wasting refers to the downslope movement of soil, rock debris, and bedrock under the force of gravity. It is a form of erosion and transportation that can occur slowly over geologic time or suddenly during catastrophic events. The main types of mass wasting are slides, flows, falls, and creep. Factors that influence mass wasting include slope angle, rock/soil type, water content, climate, earthquakes/volcanic activity, and pre-existing weaknesses in bedrock. Common landslide types are slumps, debris flows, rock slides, and debris slides/slumps. Creep is a very slow form of downslope movement caused by processes like wetting/drying, freezing/thawing, and
This document provides an overview of maps and map projections. It defines what a map is, discusses scale and map projections, and classifies the main types of projections as cylindrical, conic, and planar. It then describes some commonly used projections in more detail, like the Mercator, UTM grid, Lambert Conformal Conic, and Albers Equal-Area Conic projections. The document concludes that map projections transform the spherical Earth into a flat plane and are fundamental to mapmaking.
The document discusses jet streams, which are narrow bands of strong wind that form in the upper atmosphere. Jet streams typically flow from west to east at speeds of up to 250 mph at altitudes between 8-16 km. They form along boundaries between hot and cold air masses, driven by pressure differences and the Coriolis effect from Earth's rotation. There are two main types of jet streams: the polar front jet at 50-60 degrees latitude and the subtropical jet at 30 degrees latitude. Jet streams play a key role in determining weather patterns and steering cyclonic storms.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive function. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
Gravity pulls the rocks, soils and debris on a downward slope, naturally, without any chemical change. This downward movement is called as mass -movement or mass-wasting.
Landslides, mudflows and rockfalls are all belonging to this category of geomorphic processes.
Mass-wasting may lead to severe natural disasters by affecting the life and building structures in different places. Understanding of mass-wasting will certainly help to mitigate the impacts of these hazards and plan the development activities.
Geological challenges & ecological effects of highway constructionAbhinav Anand
The document discusses the geological challenges and ecological effects of highway construction. It provides details on:
1) Engineering geology factors like lithology, structures, and weathering grade that influence the stability of rock slopes during highway construction in hilly terrain.
2) Case study of NH-52(A) highway in India which passes through hilly terrain and experiences slope failures.
3) Environmental impacts of highways like air and water pollution from vehicle emissions, as well as noise pollution and habitat fragmentation. Solutions to stabilize slopes and reduce impacts are also mentioned.
This document discusses sedimentary rocks, including their formation, classification, and characteristic textures and structures. Sedimentary rocks form through the lithification of sediments deposited under water. They are classified based on their composition into clastic rocks (formed from fragments of pre-existing rocks), chemical/evaporite rocks (formed by chemical precipitation), and organic rocks (containing organic matter). Key textures include grain size, shape, packing, and fabric. Common structures include stratification, lamination, cross-bedding, graded bedding, and ripple marks, which provide information about depositional environments.
This document summarizes the differentiation of the Earth. It discusses how the Earth initially formed as a molten mass and over time separated into layers with the heavier materials sinking to the center to form the core. The two main theories for this differentiation are homogeneous and heterogeneous accretion. Evidence from the Moon supports the Earth differentiating into layers early in its formation history around 4.5 billion years ago. The Earth is now composed of concentric layers that decrease in density from the iron-nickel core, to the silicate mantle, and finally the crust at the surface.
The document discusses the rock cycle, which describes how rocks constantly change form through various natural processes. Rocks can be broken down by weathering into sediments and then transported by erosion. These sediments may be deposited, compacted, and cemented to form sedimentary rocks. Increased heat and pressure can metamorphose sedimentary and igneous rocks. Melting of rocks forms magma that cools and solidifies into new igneous rocks. This cyclic process results in rocks continuously changing their shape and composition over geological time.
08 volcanism intrusive and extrusive featureskerrie95
This document discusses different types of volcanic features, both intrusive and extrusive. It defines intrusive features like dykes, sills, laccoliths and batholiths, which form underground from magma cooling and solidifying below the surface. Extrusive features like lava flows, cinder cones and composite volcanoes form above ground from magma erupting as lava. The document also categorizes different types of lava based on their viscosity and chemical composition, and classifies volcanoes based on the violence of their eruptions. It aims to help students understand the major forms of volcanic landforms and the geological processes that create them.
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.
Definition, classification & types of landslideTarikIslam9
General Information about Bangladesh
Bangladesh is consisted of a total land area of 147570 km² with hilly areas of 17,342 km² (8.5% of total area of Bangladesh).
Chattagram Hill tracts is the wide ranging hilly area in the southeastern part of the country. Rangamati, Bandarban and Khagrachari are three unique geographical and cultural landscape administrative districts in this region.
Landslides are a common hazard in the Chittagong Hill Districts (CHD) of Bangladesh. The communities that live on dangerous hill slopes in CHD repeatedly experience landslide hazards during the monsoon season, with casualties, economic losses and property damage.
This document provides course material for the course "Applied GIS" with the course code GeES2083. It outlines the course content and schedule of activities over 3 weeks. The course covers topics such as GIS data processing using ArcToolbox and Model Builder, spatial analysis techniques including interpolation, buffering, and hydrology, geo-data management, route networking, point pattern analysis, and 3D analysis. Students will be continuously assessed through labs and a group project. A final exam will also be administered.
Application of Basic Remote Sensing in GeologyUzair Khan
Application of basic remote sensing in Geology. This presentation tries to discriminate the lithology in the Landsat-7 scene located Karachi West. Although other enhanced methodology available to discriminate the rock types, here just a band ratios and simple band combination used for lithology identification.
This document provides an introduction to satellite remote sensing. It discusses key topics such as the definition of remote sensing, the stages of remote sensing including energy sources, sensors, and data interpretation. It also covers different types of remote sensing based on platform, orbital characteristics, energy sources, components, and spectral characteristics. Different sensors, image resolution, electromagnetic radiation properties, and interactions with the atmosphere and earth surface are described. The history and development of remote sensing techniques are briefly mentioned. In summary, the document provides a comprehensive overview of the fundamental concepts and components of remote sensing from multiple perspectives.
This document provides materials for a unit on maps and geography. It includes an overview of key concepts like continents, cardinal directions, and map types. Students will learn to identify locations on maps, interpret map symbols, and understand how geography influences culture. The unit introduces map essentials such as keys, grids, and timelines. Students will complete map-based assignments and analyze how maps reflect history, politics and economics. The goal is for students to understand how geography shapes lifestyle and viewpoints.
This is a very basic presentation about the rock cycle for my 7th grade science class. The first eleven slides are narrated. After slide 10 there is a YouTube video with a rock cycle song. Slides 12-26 are an interactive review quiz. Enjoy!
This document discusses mass wasting, which refers to the downslope movement of earth materials under the influence of gravity. It describes the various controls on mass wasting like gravity, water, and vegetation. Several types of mass wasting are classified and explained, including slides, flows, creeps, and falls. The document also covers causes of instability, prevention methods, and examples of destructive mass wasting events. The conclusion reiterates that mass wasting shapes landscapes and endangers human life.
Students will learn about avalanches through experiments simulating snowpack layers using flour, sugar, and mashed potatoes on an avalanche board. In a 7th grade activity, students will build snowpack models based on recipes from the teacher to test stability. A 10th grade activity has students analyze an actual avalanche forecast to design their own snowpack model, introducing concepts like slab avalanches and weak crust layers formed from water spraying. Both activities aim to deepen understanding of avalanche dynamics and how different snow crystal types, layer strengths, and weather patterns contribute to avalanche risk.
Applications of remote sensing in geological aspectsPramoda Raj
Remote sensing uses sensors on airborne or spaceborne platforms to detect and record electromagnetic radiation from the Earth's surface. It has two main phases - data acquisition through sensors and data analysis. In geology, remote sensing is used to map lithology, structural features, and monitor hazards. It helps identify rock types and structures that can indicate mineral or oil and gas deposits. Remote sensing provides synoptic data to study geomorphology, hydrology, and other Earth processes over large areas.
Slope, processes & development lesson 8Ms Geoflake
This document discusses slope processes and development. It defines key slope concepts like regolith, bedrock, and soil blankets. It describes three common slope shapes: convex, concave, and rectilinear. Factors that influence slope formation are also outlined, including climate, geology, regolith properties, and vegetation. Mechanisms of slope failure are then explained through concepts of shear strength, gravitational forces, angle of repose, and dynamic equilibrium.
This document provides an overview of glaciers, including their formation, movement, and important terminology. It describes the key parts of a glacier, including the accumulation and ablation zones. The document also discusses different types of glaciers and their varying speeds of movement. Finally, it covers the erosional and depositional landforms created by glaciers, such as moraines, eskers, and drumlins.
King's geomorphic model is based on the evolution of idealized hill slopes through four stages - waxing slope, free face, debris slope, and waning slope or pediment. The model involves the parallel retreat of scarps and formation of pediments, resulting in the development of a pediplain landscape over multiple cycles of scarp retreat and pedimentation. Each cycle progresses through youth, mature, and old stages similar to Davis' cycle of erosion. The model was developed based on King's extensive study of landscapes in South Africa.
Year 9 Connecting People with Place - Tourism FocusMark Modra
The document discusses how people perceive and connect with different places. It explains that a place is anywhere that people identify with and imbue with meaning. Places are interconnected in various ways through natural features and human activities like trade and transportation. The document also discusses how geographers use methods like questioning, models and criteria to better understand how people perceive places and the interconnections between various places. It provides examples of analyzing perceptions of places visited versus places only known through other sources. Finally, it discusses different types of tourism and their potential positive and negative impacts on places.
What is human wellbeing? A locally driven, three-dimensional perspective.
A presentation by Emily Woodhouse, WCS/UCL/Imperial College.
This presentation was given at the Expert Workshop on Equity, Justice and Well-being in Ecosystem Governance, held at the International Institute for Environment and Development (IIED) in London, March, 2015.
Gravity pulls the rocks, soils and debris on a downward slope, naturally, without any chemical change. This downward movement is called as mass -movement or mass-wasting.
Landslides, mudflows and rockfalls are all belonging to this category of geomorphic processes.
Mass-wasting may lead to severe natural disasters by affecting the life and building structures in different places. Understanding of mass-wasting will certainly help to mitigate the impacts of these hazards and plan the development activities.
Geological challenges & ecological effects of highway constructionAbhinav Anand
The document discusses the geological challenges and ecological effects of highway construction. It provides details on:
1) Engineering geology factors like lithology, structures, and weathering grade that influence the stability of rock slopes during highway construction in hilly terrain.
2) Case study of NH-52(A) highway in India which passes through hilly terrain and experiences slope failures.
3) Environmental impacts of highways like air and water pollution from vehicle emissions, as well as noise pollution and habitat fragmentation. Solutions to stabilize slopes and reduce impacts are also mentioned.
This document discusses sedimentary rocks, including their formation, classification, and characteristic textures and structures. Sedimentary rocks form through the lithification of sediments deposited under water. They are classified based on their composition into clastic rocks (formed from fragments of pre-existing rocks), chemical/evaporite rocks (formed by chemical precipitation), and organic rocks (containing organic matter). Key textures include grain size, shape, packing, and fabric. Common structures include stratification, lamination, cross-bedding, graded bedding, and ripple marks, which provide information about depositional environments.
This document summarizes the differentiation of the Earth. It discusses how the Earth initially formed as a molten mass and over time separated into layers with the heavier materials sinking to the center to form the core. The two main theories for this differentiation are homogeneous and heterogeneous accretion. Evidence from the Moon supports the Earth differentiating into layers early in its formation history around 4.5 billion years ago. The Earth is now composed of concentric layers that decrease in density from the iron-nickel core, to the silicate mantle, and finally the crust at the surface.
The document discusses the rock cycle, which describes how rocks constantly change form through various natural processes. Rocks can be broken down by weathering into sediments and then transported by erosion. These sediments may be deposited, compacted, and cemented to form sedimentary rocks. Increased heat and pressure can metamorphose sedimentary and igneous rocks. Melting of rocks forms magma that cools and solidifies into new igneous rocks. This cyclic process results in rocks continuously changing their shape and composition over geological time.
08 volcanism intrusive and extrusive featureskerrie95
This document discusses different types of volcanic features, both intrusive and extrusive. It defines intrusive features like dykes, sills, laccoliths and batholiths, which form underground from magma cooling and solidifying below the surface. Extrusive features like lava flows, cinder cones and composite volcanoes form above ground from magma erupting as lava. The document also categorizes different types of lava based on their viscosity and chemical composition, and classifies volcanoes based on the violence of their eruptions. It aims to help students understand the major forms of volcanic landforms and the geological processes that create them.
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.
Definition, classification & types of landslideTarikIslam9
General Information about Bangladesh
Bangladesh is consisted of a total land area of 147570 km² with hilly areas of 17,342 km² (8.5% of total area of Bangladesh).
Chattagram Hill tracts is the wide ranging hilly area in the southeastern part of the country. Rangamati, Bandarban and Khagrachari are three unique geographical and cultural landscape administrative districts in this region.
Landslides are a common hazard in the Chittagong Hill Districts (CHD) of Bangladesh. The communities that live on dangerous hill slopes in CHD repeatedly experience landslide hazards during the monsoon season, with casualties, economic losses and property damage.
This document provides course material for the course "Applied GIS" with the course code GeES2083. It outlines the course content and schedule of activities over 3 weeks. The course covers topics such as GIS data processing using ArcToolbox and Model Builder, spatial analysis techniques including interpolation, buffering, and hydrology, geo-data management, route networking, point pattern analysis, and 3D analysis. Students will be continuously assessed through labs and a group project. A final exam will also be administered.
Application of Basic Remote Sensing in GeologyUzair Khan
Application of basic remote sensing in Geology. This presentation tries to discriminate the lithology in the Landsat-7 scene located Karachi West. Although other enhanced methodology available to discriminate the rock types, here just a band ratios and simple band combination used for lithology identification.
This document provides an introduction to satellite remote sensing. It discusses key topics such as the definition of remote sensing, the stages of remote sensing including energy sources, sensors, and data interpretation. It also covers different types of remote sensing based on platform, orbital characteristics, energy sources, components, and spectral characteristics. Different sensors, image resolution, electromagnetic radiation properties, and interactions with the atmosphere and earth surface are described. The history and development of remote sensing techniques are briefly mentioned. In summary, the document provides a comprehensive overview of the fundamental concepts and components of remote sensing from multiple perspectives.
This document provides materials for a unit on maps and geography. It includes an overview of key concepts like continents, cardinal directions, and map types. Students will learn to identify locations on maps, interpret map symbols, and understand how geography influences culture. The unit introduces map essentials such as keys, grids, and timelines. Students will complete map-based assignments and analyze how maps reflect history, politics and economics. The goal is for students to understand how geography shapes lifestyle and viewpoints.
This is a very basic presentation about the rock cycle for my 7th grade science class. The first eleven slides are narrated. After slide 10 there is a YouTube video with a rock cycle song. Slides 12-26 are an interactive review quiz. Enjoy!
This document discusses mass wasting, which refers to the downslope movement of earth materials under the influence of gravity. It describes the various controls on mass wasting like gravity, water, and vegetation. Several types of mass wasting are classified and explained, including slides, flows, creeps, and falls. The document also covers causes of instability, prevention methods, and examples of destructive mass wasting events. The conclusion reiterates that mass wasting shapes landscapes and endangers human life.
Students will learn about avalanches through experiments simulating snowpack layers using flour, sugar, and mashed potatoes on an avalanche board. In a 7th grade activity, students will build snowpack models based on recipes from the teacher to test stability. A 10th grade activity has students analyze an actual avalanche forecast to design their own snowpack model, introducing concepts like slab avalanches and weak crust layers formed from water spraying. Both activities aim to deepen understanding of avalanche dynamics and how different snow crystal types, layer strengths, and weather patterns contribute to avalanche risk.
Applications of remote sensing in geological aspectsPramoda Raj
Remote sensing uses sensors on airborne or spaceborne platforms to detect and record electromagnetic radiation from the Earth's surface. It has two main phases - data acquisition through sensors and data analysis. In geology, remote sensing is used to map lithology, structural features, and monitor hazards. It helps identify rock types and structures that can indicate mineral or oil and gas deposits. Remote sensing provides synoptic data to study geomorphology, hydrology, and other Earth processes over large areas.
Slope, processes & development lesson 8Ms Geoflake
This document discusses slope processes and development. It defines key slope concepts like regolith, bedrock, and soil blankets. It describes three common slope shapes: convex, concave, and rectilinear. Factors that influence slope formation are also outlined, including climate, geology, regolith properties, and vegetation. Mechanisms of slope failure are then explained through concepts of shear strength, gravitational forces, angle of repose, and dynamic equilibrium.
This document provides an overview of glaciers, including their formation, movement, and important terminology. It describes the key parts of a glacier, including the accumulation and ablation zones. The document also discusses different types of glaciers and their varying speeds of movement. Finally, it covers the erosional and depositional landforms created by glaciers, such as moraines, eskers, and drumlins.
King's geomorphic model is based on the evolution of idealized hill slopes through four stages - waxing slope, free face, debris slope, and waning slope or pediment. The model involves the parallel retreat of scarps and formation of pediments, resulting in the development of a pediplain landscape over multiple cycles of scarp retreat and pedimentation. Each cycle progresses through youth, mature, and old stages similar to Davis' cycle of erosion. The model was developed based on King's extensive study of landscapes in South Africa.
Year 9 Connecting People with Place - Tourism FocusMark Modra
The document discusses how people perceive and connect with different places. It explains that a place is anywhere that people identify with and imbue with meaning. Places are interconnected in various ways through natural features and human activities like trade and transportation. The document also discusses how geographers use methods like questioning, models and criteria to better understand how people perceive places and the interconnections between various places. It provides examples of analyzing perceptions of places visited versus places only known through other sources. Finally, it discusses different types of tourism and their potential positive and negative impacts on places.
What is human wellbeing? A locally driven, three-dimensional perspective.
A presentation by Emily Woodhouse, WCS/UCL/Imperial College.
This presentation was given at the Expert Workshop on Equity, Justice and Well-being in Ecosystem Governance, held at the International Institute for Environment and Development (IIED) in London, March, 2015.
Integral city opening gateways to wellbeing in the human hive moscow - slid...Marilyn Hamilton
This document presents an overview of an Integral City model aimed at improving city well-being. It discusses four voices that make up a human hive (city-zen civic manager, civil society, business/entrepreneur, voice of integration). An Integral City is defined as serving as a reflective organ of the earth that builds individual and collective capacity. Key aspects of the model include using an Integral Vital Signs Monitor to track city well-being indicators across different levels and developing a community of practice to oversee indicator tracking and correct course as needed. The goal is to evolve cities as reflective organs that take care of individuals, communities and the environment.
The document outlines an agenda for a workshop on well-being. It includes definitions of well-being and resilience. Sections discuss influences on well-being like internal and external processes. Models for understanding alignment across different levels like mission and skills are presented. The workshop also focuses on increasing flexibility and understanding of self and others.
Place identity and environmental conditionsJenna Condie
This document discusses place identity and environmental conditions. It explores how place influences identity and interactions between people, with identity being multivoiced and dialogical. Living near railways can impact residents' sense of place through noise disruption, but they negotiate their agency and identities in adapting to this context. The document argues that both objective exposure measures and subjective responses to the environment must be considered to understand its influence, as no two people experience reality the same. Place identity matters for policymaking regarding behavior, health, well-being and social change in the face of environmental change.
The document summarizes China's population trends over time:
1) China implemented strict population control policies starting in the 1970s to reduce its high population growth rate, most notably the "one-child policy" limiting urban families to one child.
2) These policies were largely successful, reducing China's total fertility rate to 1.6 births per woman. However, they also led to societal issues like a preference for sons and a current gender imbalance.
3) China is now facing a new challenge of population aging as its population structure matures, creating support burdens for the one-child generation. The long-term impacts of these policies are still unfolding.
Geography unit 2 Part 2 - The effects of global connectionsMark Modra
This document discusses the effects of globalization and international trade on people, places, and the environment. It notes that global trade can benefit people through access to cheaper goods and new employment opportunities, but also has negatives like poor working conditions, loss of local jobs, and impacts on culture. Each stage of production and consumption (e.g. extracting materials, manufacturing, distribution) affects the natural environment. International tourism brings in revenue but can also negatively impact environments and local communities depending on the type (e.g. recreational, ecotourism). The document also discusses trends in tourism like increased travel and interest in authentic experiences.
Geography unit 2 Part 1 - connecting people and placesMark Modra
This document discusses how people connect to different places and people. It explores how technology, trade, and globalization have increased interconnections between places. People are connected through the goods and services they consume, which often come from many different places around the world due to global trade networks. Technology also influences interconnections by allowing people to connect and share information more quickly through the internet, social media, and digital communications. The document provides examples of how trade connects Australia to other countries through exports and the global supply chains that produce everyday items. Students are assigned tasks to reflect on how they are connected to other places through technology, trade, and consumption.
How did life change under the rule of shogunMark Modra
I have modified others people slides and used information from a number of sources. I do not have the rights to the photos and the content is from varying sources.
A main source was Oxford big ideas history 8, an amazing source.
How did the rise of the shoguns change societyMark Modra
I have modified others people slides and used information from a number of sources. I do not have the rights to the photos and the content is from varying sources.
A main source was Oxford big ideas history 8, an amazing source.
What was life in japan like before the shogunMark Modra
A look at the early years before Shogun rule.
I have modified others people slides and used information from a number of sources. I do not have the rights to the photos and the content is from varying sources.
A main source was Oxford big ideas history 8, an amazing source.
Japan is an archipelago of over 4,000 islands located in East Asia, just 500 miles from China. While Japan experiences mild weather and plenty of rainfall, it is also very mountainous with only 15% of land suitable for farming and short on natural resources. The geography of Japan emerged from underwater mountain ranges rising to the surface of the Pacific Ocean. Chinese culture also significantly influenced Japan, with adoption of Chinese writing, art styles, cuisine, and a strong central government, though Japanese nobles remained powerful.
1. The document proposes an integrated curriculum approach for a middle school focusing on well-being over a 10 week period and linking various subjects like languages, English, drama, health and PE.
2. It involves developing lesson plans for each subject and mind maps to show connections between topics to allow collaborative, in-depth learning across different classes.
3. Assessment of students would evaluate achievement of learning outcomes and subject goals as well as overall understanding of the well-being topic through various activities.
Voki is a web tool that allows users to create talking animated characters called Vokis to express themselves online. Users can customize the appearance and voice of their Voki character, choosing from a variety of options for its look, background, accent, and recorded or typed text. Once complete, the Voki can be published, shared on other websites, or embedded in blogs or other online spaces.
How to Build a Module in Odoo 17 Using the Scaffold MethodCeline George
Odoo provides an option for creating a module by using a single line command. By using this command the user can make a whole structure of a module. It is very easy for a beginner to make a module. There is no need to make each file manually. This slide will show how to create a module using the scaffold method.
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.
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 ...
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Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
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.