GEOGRAPHIC SKILLS: DOT MAPS. A dot distribution map, or dot density map, is a map type that uses a dot symbol to show the presence of a feature or a phenomenon. Dot maps rely on a visual scatter to show spatial pattern.
Map reading and interpretation involves examining maps to identify geographical information. Key skills for reading maps include identifying the title, scale, key, north direction, boundaries, and date. Drainage patterns like dendritic and trellised can be described from maps. Rock type is suggested by landforms, vegetation, and permeability. Climate can be inferred from latitude, altitude, water bodies, and vegetation. Topographical maps provide important geographical details about physical features, human activities, and population distribution.
Social geography examines how social relationships, identities, and inequalities form and are influenced by space. Social interaction is the foundation of society, taking various forms from individual to individual or group interactions. Social groups are characterized by regular interaction between members who develop roles and agreed upon procedures. There are various types of social groups including primary groups based on family and friends and secondary groups based on shared occupations or locations. A community is defined by geographic location while a society includes people in different places connected through direct and indirect social ties.
This document discusses GIS data analysis techniques including raster to vector conversion and spatial analysis through vector overlay. It provides information on various data types and models in GIS. Key analysis techniques covered are raster and vector data overlays, terrain mapping and analysis, and spatial interpolation methods. Specific vector and raster overlay methods like point-in-polygon, line-in-polygon and polygon-on-polygon are described. Spatial data editing techniques involving digitization errors and topological/non-topological editing are also summarized.
Applied geomorphology examines how landforms and geological processes impact society and how human activities affect landforms. It provides solutions to issues like coastal erosion, landslides, and river management. Applied geomorphologists create maps, models, and predictions to help scientists, engineers, and decision-makers address hazards, land use, natural resources, and environmental changes. They also advise on public policy regarding human-landform interactions.
This document discusses map scale and projections. It defines scale as the relationship between distances on a map and in reality. Scale can be indicated graphically using a bar scale or fractionally as a ratio. Larger scale maps show smaller areas in greater detail while smaller scale maps show larger areas with less detail. Map projections transfer the spherical Earth onto a flat surface, inevitably introducing some distortion of shapes, sizes or distances. Different projections prioritize conformality, equivalence or other properties depending on the map's intended use.
Glaciers form from accumulated snow that undergoes recrystallization into ice. They flow via gravity from accumulation zones where snowfall exceeds melting to ablation zones where melting exceeds snowfall. Glaciers powerfully erode, transport, and deposit sediment. They carve U-shaped valleys and leave behind landforms like moraines, drumlins, eskers and kettle lakes. Glaciers shape mountain and coastal landscapes through erosion and deposition.
The document provides information on key concepts related to maps and map reading, including:
1) Maps are graphical representations of physical and cultural features on Earth's surface, with symbols used to denote features. Scale allows large areas to be shown on small maps and is expressed verbally, as a ratio, or with a bar scale.
2) Grid references use a system of eastings and northings to precisely locate features on maps divided into grids. Contour lines and spot heights indicate land elevation and relief. Hachures and shading are also used to represent relief.
3) Maps use colors to represent different features - green for forests, blue for water, etc. Settlement patterns, drainage patterns, transportation
Map reading and interpretation involves examining maps to identify geographical information. Key skills for reading maps include identifying the title, scale, key, north direction, boundaries, and date. Drainage patterns like dendritic and trellised can be described from maps. Rock type is suggested by landforms, vegetation, and permeability. Climate can be inferred from latitude, altitude, water bodies, and vegetation. Topographical maps provide important geographical details about physical features, human activities, and population distribution.
Social geography examines how social relationships, identities, and inequalities form and are influenced by space. Social interaction is the foundation of society, taking various forms from individual to individual or group interactions. Social groups are characterized by regular interaction between members who develop roles and agreed upon procedures. There are various types of social groups including primary groups based on family and friends and secondary groups based on shared occupations or locations. A community is defined by geographic location while a society includes people in different places connected through direct and indirect social ties.
This document discusses GIS data analysis techniques including raster to vector conversion and spatial analysis through vector overlay. It provides information on various data types and models in GIS. Key analysis techniques covered are raster and vector data overlays, terrain mapping and analysis, and spatial interpolation methods. Specific vector and raster overlay methods like point-in-polygon, line-in-polygon and polygon-on-polygon are described. Spatial data editing techniques involving digitization errors and topological/non-topological editing are also summarized.
Applied geomorphology examines how landforms and geological processes impact society and how human activities affect landforms. It provides solutions to issues like coastal erosion, landslides, and river management. Applied geomorphologists create maps, models, and predictions to help scientists, engineers, and decision-makers address hazards, land use, natural resources, and environmental changes. They also advise on public policy regarding human-landform interactions.
This document discusses map scale and projections. It defines scale as the relationship between distances on a map and in reality. Scale can be indicated graphically using a bar scale or fractionally as a ratio. Larger scale maps show smaller areas in greater detail while smaller scale maps show larger areas with less detail. Map projections transfer the spherical Earth onto a flat surface, inevitably introducing some distortion of shapes, sizes or distances. Different projections prioritize conformality, equivalence or other properties depending on the map's intended use.
Glaciers form from accumulated snow that undergoes recrystallization into ice. They flow via gravity from accumulation zones where snowfall exceeds melting to ablation zones where melting exceeds snowfall. Glaciers powerfully erode, transport, and deposit sediment. They carve U-shaped valleys and leave behind landforms like moraines, drumlins, eskers and kettle lakes. Glaciers shape mountain and coastal landscapes through erosion and deposition.
The document provides information on key concepts related to maps and map reading, including:
1) Maps are graphical representations of physical and cultural features on Earth's surface, with symbols used to denote features. Scale allows large areas to be shown on small maps and is expressed verbally, as a ratio, or with a bar scale.
2) Grid references use a system of eastings and northings to precisely locate features on maps divided into grids. Contour lines and spot heights indicate land elevation and relief. Hachures and shading are also used to represent relief.
3) Maps use colors to represent different features - green for forests, blue for water, etc. Settlement patterns, drainage patterns, transportation
This document describes how to read and interpret contour lines on topographic maps. It contains the following key points:
1. Contour lines connect points of equal elevation and are used to depict the shape and elevation changes of landforms.
2. Cross-sections can be drawn from contour lines to show the side profile of landforms between two points.
3. The spacing and shapes of contour lines indicate different landforms - closely spaced lines indicate steep slopes while widely spaced lines show gentle slopes. Common landforms like hills, valleys, ridges and plateaus each have distinguishing contour patterns.
4. Interpreting contour lines allows describing the overall landscape and calculating elevation changes across an area. The document provides instructions
This document discusses map projections, which are methods for translating the three-dimensional surface of the Earth onto a two-dimensional map. It describes three types of developable projection surfaces - conic, cylindrical, and planar - that are used to create different map projections. Specific projections are then outlined, including what geometric properties they preserve or distort (shape, area, distance, direction) and their common uses. The document provides a detailed overview of different GIS map projection techniques.
Topics:
1. Mapping Concepts
2. Analysis with paper based Maps
3. Limitations of Paper based Maps
4. Computer Aided Cartography History and Development
5. GIS Definition
6. Advantage of Digital Maps
The document discusses topographic maps and their numbering systems in India. It provides details on:
1) Topographic maps represent relief and also show features like transportation and settlements. They contain information like names, scales, and features.
2) In India, the Survey of India prepares topographic maps. Maps are part of two series - the India and Adjacent Country Series and the International Map of the World Series.
3) The India and Adjacent Country Series covers India in grids numbered from 40-92 that are divided into degree, quadrant, and special sheets at various scales with contour intervals.
Origin of culture :Cultural hearth and cultural realm, cultural region.RAJKUMARPOREL
The document discusses the origin and development of cultural hearths and cultural regions around the world. It identifies the seven original cultural hearths as Mesopotamia, the Nile River Valley, the Aegean region, the Indus River Valley, the Ganges River Valley, the Wei-Huang Valley, and West Africa. These early hearths developed around major river systems and influenced the spread of culture. The document also outlines the major cultural realms of Occidental, Islamic, Indian, East Asian, and minor realms of Southeast Asia and Sub-Saharan Africa. It defines key terms like cultural area and cultural boundary.
The concept of GIS was first introduced in the early 1960s, and it was subsequently researched and developed as a new discipline. The GIS history views Roger Tomlinson as a pioneer of the concept, where the first iteration was designed to store, collate, and analyze data about land usage in Canada.
This document discusses different types of map projections used to represent the spherical earth on a flat surface. It describes how all projections involve some distortion of properties like shapes, areas, distances or directions. The key types are conformal, equivalent, and equidistant projections. It explains the concepts of projection surfaces like cones, cylinders and planes, as well as variables like the light source and orientation. Specific common projections are also outlined, such as Mercator, Lambert conformal conic, and azimuthal equidistant, along with their characteristic distortions and uses.
The quantitative revolution in geography began in the 1950s with Schaefer's critique of the traditional regional geography approach. Schaefer argued geography should seek general patterns and laws across regions using quantitative methods rather than focusing on unique regions. This sparked a major transformation in the field toward spatial analysis and modeling using statistics, mathematics, and later computers. By the 1960s, the "new geography" focused on rigorous theory testing and had largely replaced the older descriptive regional approach. However, criticisms emerged in the 1970s that quantitative methods dehumanized geography and were unable to fully explain human spatial patterns. This led to the rise of qualitative approaches. While quantitative geography declined, it resurged in the 1990s with new spatial analysis techniques
Davis and Penk proposed different models of the cycle of erosion. Davis' model involved three stages - youth, maturity, and old age - where a landscape evolves from high relief to a flat plain over time. Penk emphasized the relationship between uplift and erosion, with landforms resulting from their competition. Later theorists like King and Gilbert built on these ideas but acknowledged no single model explains all landscapes given different environments. While influential, both Davis and Penk's concepts have limitations and underwent criticism regarding assumptions about rates of uplift and erosion.
The document discusses map scales. It explains that maps are scaled down representations of areas of the world so they can fit on a sheet of paper. It states that map scales show the relationship between distances on a map and actual distances on the ground. Scales allow the determination of distances between places and the sizes of landmarks. The document also provides examples of how map scales can be expressed as statements, ratios, or linear scales.
This document discusses different types of erosional and depositional landforms created by river processes. It describes landforms such as V-shaped valleys and waterfalls that are created by erosion, and floodplains and deltas that are formed by deposition. It also explains the factors that influence fluvial erosion and the formation of various erosional features like interlocking spurs, rapids, and potholes.
Isopleth maps connect points of equal value through isolines to show variations and distributions of elements. Values can represent quantities, intensities or densities and common examples include isobars (equal pressure), isotherms (equal temperature), and isohyets (equal precipitation). Isopleth maps are constructed by marking data points, determining suitable interval values, joining equal points with smooth lines, and adding a key. They have various applications in climatology, demography, and showing altitude or terrain. Merits include scientific accuracy while demerits can include inaccuracies from interpolation of many data points.
This document summarizes geomorphic processes including exogenic processes like weathering, mass wasting, erosion and aggradation that modify the Earth's surface through physical and chemical means. Endogenic processes like volcanism and diastrophism involve subsurface movement of magma or rock. Extra-terrestrial processes include meteorite impacts that also shape landforms. The document discusses various agents and mechanisms of weathering, erosion, transportation and deposition of earth materials.
Topographic maps use contour lines to represent elevation and slope of land. Contour lines connect points of equal elevation and never cross. Closer lines indicate steeper slopes while widely spaced lines show more gentle slopes. Index contours are bold lines labeled with the elevation. A benchmark is a point of known exact elevation marked as B.M. on maps. Map scale relates distances on a map to actual distances on land and can be ratio, graphical, or verbal.
Geomorphology is the study of landforms and the processes that shape them. It is a branch of physical geography that analyzes relief features at different dimensions and scales. Relief features are organized into three orders based on size: first order includes continents and ocean basins shaped by plate tectics; second order consists of structural landforms like mountains and plateaus formed by constructional forces; third order comprises micro-level erosional and depositional landforms developed on second order features by exogenic processes like rivers and glaciers. Process geomorphology examines specialized subfields defined by the dominant shaping process, such as fluvial, glacial, coastal and karst landforms.
Types of Platforms
1. Airbrone Platforms
2. Spacebrone Platforms
Platforms are Vital Role in remote sensing data acquisition
Necessary to correct the position the remote sensors that collect data from the objects of interest
The study deals different terms, concept, definitions, theories of population, census statistics, maps and diagrams for representations of demographic data. You read it carefully until the last.
Projecting maps involves converting the spherical earth into a flat plane, which inevitably causes some distortion of properties like angles, areas, directions, and shapes. There are three main types of map projections - cylindrical, conical, and planar - which involve wrapping a lighted globe onto different geometric surfaces like a cylinder, cone, or flat plane. The Mercator projection specifically was created to aid navigation by representing lines of constant bearing as straight lines, though it distorts the relative sizes of land areas farther from the equator. The Universal Transverse Mercator (UTM) system divides the earth into zones and uses the Mercator projection locally in each to assign Cartesian coordinates.
This document discusses dot density maps, which use dots to represent the distribution and density of geographic phenomena across regions on a map. Each dot represents a single feature or quantity. When viewed as a whole, a dot map gives an impression of the overall distribution throughout the area. The document provides examples of dot maps being used to display medical geography data and compare population densities. It also outlines the common patterns, components, and steps to construct a dot density map.
Exploring our geographic world by tessie calimag bb.Tessie Calimag
Geography is the study of the Earth's physical features and human activities. It involves understanding locations, places, regions, and human-environment interactions. Some key tools used in geography are maps, atlases, geospatial technologies like GIS, and fieldwork. Maps show physical and political features and use symbols, scales, legends and other elements to convey spatial information. Different types of maps exist for various purposes. Geography helps us understand the world, our own country, and how humans and the environment impact one another in different places and regions.
This document describes how to read and interpret contour lines on topographic maps. It contains the following key points:
1. Contour lines connect points of equal elevation and are used to depict the shape and elevation changes of landforms.
2. Cross-sections can be drawn from contour lines to show the side profile of landforms between two points.
3. The spacing and shapes of contour lines indicate different landforms - closely spaced lines indicate steep slopes while widely spaced lines show gentle slopes. Common landforms like hills, valleys, ridges and plateaus each have distinguishing contour patterns.
4. Interpreting contour lines allows describing the overall landscape and calculating elevation changes across an area. The document provides instructions
This document discusses map projections, which are methods for translating the three-dimensional surface of the Earth onto a two-dimensional map. It describes three types of developable projection surfaces - conic, cylindrical, and planar - that are used to create different map projections. Specific projections are then outlined, including what geometric properties they preserve or distort (shape, area, distance, direction) and their common uses. The document provides a detailed overview of different GIS map projection techniques.
Topics:
1. Mapping Concepts
2. Analysis with paper based Maps
3. Limitations of Paper based Maps
4. Computer Aided Cartography History and Development
5. GIS Definition
6. Advantage of Digital Maps
The document discusses topographic maps and their numbering systems in India. It provides details on:
1) Topographic maps represent relief and also show features like transportation and settlements. They contain information like names, scales, and features.
2) In India, the Survey of India prepares topographic maps. Maps are part of two series - the India and Adjacent Country Series and the International Map of the World Series.
3) The India and Adjacent Country Series covers India in grids numbered from 40-92 that are divided into degree, quadrant, and special sheets at various scales with contour intervals.
Origin of culture :Cultural hearth and cultural realm, cultural region.RAJKUMARPOREL
The document discusses the origin and development of cultural hearths and cultural regions around the world. It identifies the seven original cultural hearths as Mesopotamia, the Nile River Valley, the Aegean region, the Indus River Valley, the Ganges River Valley, the Wei-Huang Valley, and West Africa. These early hearths developed around major river systems and influenced the spread of culture. The document also outlines the major cultural realms of Occidental, Islamic, Indian, East Asian, and minor realms of Southeast Asia and Sub-Saharan Africa. It defines key terms like cultural area and cultural boundary.
The concept of GIS was first introduced in the early 1960s, and it was subsequently researched and developed as a new discipline. The GIS history views Roger Tomlinson as a pioneer of the concept, where the first iteration was designed to store, collate, and analyze data about land usage in Canada.
This document discusses different types of map projections used to represent the spherical earth on a flat surface. It describes how all projections involve some distortion of properties like shapes, areas, distances or directions. The key types are conformal, equivalent, and equidistant projections. It explains the concepts of projection surfaces like cones, cylinders and planes, as well as variables like the light source and orientation. Specific common projections are also outlined, such as Mercator, Lambert conformal conic, and azimuthal equidistant, along with their characteristic distortions and uses.
The quantitative revolution in geography began in the 1950s with Schaefer's critique of the traditional regional geography approach. Schaefer argued geography should seek general patterns and laws across regions using quantitative methods rather than focusing on unique regions. This sparked a major transformation in the field toward spatial analysis and modeling using statistics, mathematics, and later computers. By the 1960s, the "new geography" focused on rigorous theory testing and had largely replaced the older descriptive regional approach. However, criticisms emerged in the 1970s that quantitative methods dehumanized geography and were unable to fully explain human spatial patterns. This led to the rise of qualitative approaches. While quantitative geography declined, it resurged in the 1990s with new spatial analysis techniques
Davis and Penk proposed different models of the cycle of erosion. Davis' model involved three stages - youth, maturity, and old age - where a landscape evolves from high relief to a flat plain over time. Penk emphasized the relationship between uplift and erosion, with landforms resulting from their competition. Later theorists like King and Gilbert built on these ideas but acknowledged no single model explains all landscapes given different environments. While influential, both Davis and Penk's concepts have limitations and underwent criticism regarding assumptions about rates of uplift and erosion.
The document discusses map scales. It explains that maps are scaled down representations of areas of the world so they can fit on a sheet of paper. It states that map scales show the relationship between distances on a map and actual distances on the ground. Scales allow the determination of distances between places and the sizes of landmarks. The document also provides examples of how map scales can be expressed as statements, ratios, or linear scales.
This document discusses different types of erosional and depositional landforms created by river processes. It describes landforms such as V-shaped valleys and waterfalls that are created by erosion, and floodplains and deltas that are formed by deposition. It also explains the factors that influence fluvial erosion and the formation of various erosional features like interlocking spurs, rapids, and potholes.
Isopleth maps connect points of equal value through isolines to show variations and distributions of elements. Values can represent quantities, intensities or densities and common examples include isobars (equal pressure), isotherms (equal temperature), and isohyets (equal precipitation). Isopleth maps are constructed by marking data points, determining suitable interval values, joining equal points with smooth lines, and adding a key. They have various applications in climatology, demography, and showing altitude or terrain. Merits include scientific accuracy while demerits can include inaccuracies from interpolation of many data points.
This document summarizes geomorphic processes including exogenic processes like weathering, mass wasting, erosion and aggradation that modify the Earth's surface through physical and chemical means. Endogenic processes like volcanism and diastrophism involve subsurface movement of magma or rock. Extra-terrestrial processes include meteorite impacts that also shape landforms. The document discusses various agents and mechanisms of weathering, erosion, transportation and deposition of earth materials.
Topographic maps use contour lines to represent elevation and slope of land. Contour lines connect points of equal elevation and never cross. Closer lines indicate steeper slopes while widely spaced lines show more gentle slopes. Index contours are bold lines labeled with the elevation. A benchmark is a point of known exact elevation marked as B.M. on maps. Map scale relates distances on a map to actual distances on land and can be ratio, graphical, or verbal.
Geomorphology is the study of landforms and the processes that shape them. It is a branch of physical geography that analyzes relief features at different dimensions and scales. Relief features are organized into three orders based on size: first order includes continents and ocean basins shaped by plate tectics; second order consists of structural landforms like mountains and plateaus formed by constructional forces; third order comprises micro-level erosional and depositional landforms developed on second order features by exogenic processes like rivers and glaciers. Process geomorphology examines specialized subfields defined by the dominant shaping process, such as fluvial, glacial, coastal and karst landforms.
Types of Platforms
1. Airbrone Platforms
2. Spacebrone Platforms
Platforms are Vital Role in remote sensing data acquisition
Necessary to correct the position the remote sensors that collect data from the objects of interest
The study deals different terms, concept, definitions, theories of population, census statistics, maps and diagrams for representations of demographic data. You read it carefully until the last.
Projecting maps involves converting the spherical earth into a flat plane, which inevitably causes some distortion of properties like angles, areas, directions, and shapes. There are three main types of map projections - cylindrical, conical, and planar - which involve wrapping a lighted globe onto different geometric surfaces like a cylinder, cone, or flat plane. The Mercator projection specifically was created to aid navigation by representing lines of constant bearing as straight lines, though it distorts the relative sizes of land areas farther from the equator. The Universal Transverse Mercator (UTM) system divides the earth into zones and uses the Mercator projection locally in each to assign Cartesian coordinates.
This document discusses dot density maps, which use dots to represent the distribution and density of geographic phenomena across regions on a map. Each dot represents a single feature or quantity. When viewed as a whole, a dot map gives an impression of the overall distribution throughout the area. The document provides examples of dot maps being used to display medical geography data and compare population densities. It also outlines the common patterns, components, and steps to construct a dot density map.
Exploring our geographic world by tessie calimag bb.Tessie Calimag
Geography is the study of the Earth's physical features and human activities. It involves understanding locations, places, regions, and human-environment interactions. Some key tools used in geography are maps, atlases, geospatial technologies like GIS, and fieldwork. Maps show physical and political features and use symbols, scales, legends and other elements to convey spatial information. Different types of maps exist for various purposes. Geography helps us understand the world, our own country, and how humans and the environment impact one another in different places and regions.
Exploring our geographic world by tessie calimag bb.Tessie Calimag
Geography is the study of the Earth's physical features and human activities. It helps us understand the world and our own country. Geography uses tools like maps to represent information about locations, physical characteristics, political boundaries, and other themes. Cartographers create maps using data from systems like GIS and satellites. Atlases contain collections of maps, graphs, and charts used as geographic resources. Regions, interactions between humans and the environment, and the movement of people also help define geography.
A map is a representation of a geographic area, usually showing terrain, political boundaries, or other features. Maps can be printed, computer-generated, or other forms. They all share common elements like projections that translate the spherical Earth onto a flat surface, scales to relate distances on the map to real-world distances, and coordinate systems like latitude and longitude to specify locations. Effective use of maps requires understanding these elements and being aware that maps have limitations due to human and technological factors.
GEOGRAPHIC SKILLS: CHOROPLETH MAPS.
A choropleth map is a thematic map in which areas are shaded or patterned in proportion to the measurement of the statistical variable being displayed on the map, such as population density or per-capita income.
This document provides an overview of geography and geographic concepts. It discusses the definition of geography as the study of the world's environment and human interaction within it. It also outlines key geographic tools like maps and atlases and concepts like the five themes of geography, map projections, grid systems and reading coordinates. The goal is to help readers understand geography and how to make, read and use maps.
GEOGRAPHIC SKILLS: FLOW-LINE MAPS.
Flow maps typically use lines to show the movement of people and goods between various locations. The lines are varied in width to represent the quantity of flow.
This document provides an introduction to geographic information systems (GIS). It defines GIS as a collection of hardware, software, and geographic data used to capture, store, analyze and display spatially referenced information. The document gives a brief history of GIS and describes its key components, including spatial data, attribute data, software, and users. It also explains different types of data layers, scales, and four common map types: choropleth, contour, dot, and symbol maps. The overall purpose of the document is to explain the basic concepts and applications of GIS.
Geography is the study of the world's environments and human-environment interactions. It has two components: physical geography, which examines the natural world, and human geography, which studies human cultures and activities. Maps are an important tool for geographers, as they can display large amounts of information visually. Different types of maps include political, physical, and thematic maps. Geographers use tools like GIS, aerial photography, and GPS to collect and analyze geographic data and create maps.
This chapter discusses key geographical skills like map reading, interpreting data representations, and conducting fieldwork investigations. It covers topics such as reading grid references, compass directions, scales, measuring distances, interpreting reliefs and landforms on maps, and analyzing photographs and satellite images. Various types of graphs like line graphs, bar graphs, pie charts, and climographs are introduced to represent geographical data. The three phases of fieldwork - pre-fieldwork, during fieldwork, and post-fieldwork - are also outlined.
This document discusses key geographical skills and investigations, including topographical map reading skills, geographical data techniques, and geographical investigations. It covers topics such as reading topographical maps, interpreting scales, measuring distances, describing relief features, identifying landforms, calculating gradients, interpreting map symbols, describing patterns of vegetation and land use, and explaining relationships between relief and land use. It also discusses using photographs, satellite images, and different types of graphs to depict and analyze geographical data.
Geography is the study of the earth and its features. It comes from Greek words meaning "to write or draw the earth." There are two main branches of geography - physical geography which studies natural features, and cultural geography which examines human activities and settlements. Key concepts in geography include location, place, regions, and the relationship between humans and the environment. Studying geography helps us understand the world and how people interact with the places where they live.
This document provides definitions and information about various tools and concepts used in geography. It discusses globes, maps, cartographers, map projections, and topographic maps. It describes how cartographers do their work through surveying, aerial photography, and satellite imagery. Key tools discussed include satellites like Landsat and GOES, as well as Geographic Information Systems (GIS) and Global Positioning Systems (GPS) which store and display geographic data. The document also outlines common elements of maps such as titles, labels, legends, and scales. It explains different types of map projections and maps like physical, political, and thematic maps.
The document discusses maps and globes. It defines maps as graphical representations of the earth's surface that show locations, sizes, and other features. It outlines different types of maps like road maps, weather maps, and political maps. Globes are described as small scale models of the earth that accurately portray distances and proportions. Key elements of maps like titles, legends, and scales are also summarized.
This document discusses the importance of statistics in geography. It notes that geography seeks to classify phenomena, compare locations, generalize patterns, and determine the influence of natural laws on humans. This makes geography a science that uses statistical techniques. Statistics help geographers understand spatial patterns and relationships between natural, physical, and social characteristics of places. Geography deals with spatial data that has locational attributes, so statistical analysis in geography considers the spatial aspects of data. Statistical techniques allow geographers to describe, summarize, analyze, and interpret spatial patterns in geographical data.
This document provides an overview of geography as an academic discipline, including its history, key concepts, and tools. It discusses what geography is, its main branches and subfields, and important elements like regions, human-environment interaction, and the five themes of geography. It also describes common map projections, symbolization, and technologies used in geography like GIS and GPS. Finally, it outlines some career opportunities in the field.
Human geography is the study of how human activity is spatially organized and how humans interact with their environment. Geographers use tools like maps, geographic information systems, and spatial analysis to understand relationships between location, culture, and the environment. Some key concepts in human geography include place, regions, diffusion, accessibility, and sense of place. Geographers study issues like globalization, development, and environmental concerns at various scales to help solve problems.
This chapter introduces the concepts of maps, including their purposes and how they can be manipulated. It discusses the five themes of geography: location, place, region, movement, and human-environmental interaction. It also explains how maps are simplified, scaled, aggregated, and projected in different types like reference, choropleth, proportional symbol, isoline, and dot maps. The chapter aims to illustrate how changing a map's properties can change its message.
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE SOURCESGeorge Dumitrache
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE
On February 27, 1933, the German parliament (Reichstag) building burned down. The Nazi leadership and its coalition partners used the fire to claim that Communists were planning a violent uprising. They claimed that emergency legislation was needed to prevent this. The resulting act, commonly known as the Reichstag Fire Decree, abolished a number of constitutional protections and paved the way for Nazi dictatorship.
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTXGeorge Dumitrache
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTX
Following Hitler’s appointment as chancellor the Nazis were finally in a position of power.
However, this power was limited, as the Nazis were just one party in a three party coalition government, under President Hindenburg.
This topic will explore how the Nazis managed to eliminate their opposition and consolidate ultimate power over Germany, whilst maintaining an illusion of democracy.
It will first explore this topic in chronological order, from the Reichstag Fire through to the death of President Hindenburg, and then explore it thematically in the last section. On the 31 January 1933, Hitler, conscious of his lack of a majority in the Reichstag, immediately called for new elections to try and strengthen his position. The Nazis aimed to increase their share of the vote so that they would have a majority in the Reichstag. This would allow them to rule unopposed and unhindered by coalition governments.
Over the next two months, they launched themselves into an intense election campaign.
On 27 February 1933, as the campaign moved into its final, frantic days, the Reichstag, the German Parliament building, was set on fire and burnt down. An atmosphere of panic and terror followed the event.
This continued when a young Dutch communist, Van der Lubbe was arrested for the crime.
The Nazi Party used the atmosphere of panic to their advantage, encouraging anti-communism. Göring declared that the communists had planned a national uprising to overthrow the Weimar Republic. This hysteria helped to turn the public against the communists, one of the Nazis main opponents, and 4000 people were imprisoned.
The day after the fire, Hindenburg signed the Emergency Decree for the Protection of the German People. On the 28 February 1933, President Hindenburg signed the Emergency Decree for the Protection of the German People. This decree suspended the democratic aspects of the Weimar Republic and declared a state of emergency.
This decree gave the Nazis a legal basis for the persecution and oppression of any opponents, who were be framed as traitors to the republic. People could be imprisoned for any or no reason.
The decree also removed basic personal freedoms, such as the freedom of speech, the right to own property, and the right to trial before imprisonment.
Through these aspects the Nazis suppressed any opposition to their power, and were able to start the road from democracy to a dictatorship. The atmosphere of uncertainty following the Reichstag Fire secured many voters for the Nazi party.
The SA also ran a violent campaign of terror against any and all opponents of the Nazi regime. Many were terrified of voting of at all, and many turned to voting for the Nazi Party out of fear for their own safety. The elections were neither free or fair.
On the 5 March 1933, the elections took place, with an extremely high turnout of 89%.
The Nazis secured 43.9% of the vote.
DEPTH STUDY GERMANY: NAZI REGIME - 04. HITLER BECOMING CHANCELLOR 1933George Dumitrache
Hitler was not immediately appointed chancellor after the success of the July 1932 elections, despite being leader of the largest party in the Reichstag. It took the economic and political instability (with two more chancellors failing to stabilise the situation) to worsen, and the support of the conservative elite, to convince Hindenburg to appoint Hitler.
Hitler was sworn in as the chancellor of Germany on the 30 January 1933. The Nazis were now in power.
DEPTH STUDY GERMANY: NAZI REGIME - 03. NAZI'S LITTLE SUCCESSGeorge Dumitrache
The document discusses the early success of the Nazi party in Germany. It notes that while the party made progress in organization and membership in its early years after 1919, it had little impact in elections initially. The Nazis received only 6.5% of the vote in their first national election in 1924. Later elections in 1928 saw their support decline further to just 2.6% as the German economy and political situation stabilized under Stresemann. While the Nazis appealed to specific groups frustrated with the Weimar Republic, they remained a small party with less than 30,000 members by 1925.
DEPTH STUDY GERMANY: NAZI REGIME - 02. NAZI PARTY IDEOLOGY IN 1920George Dumitrache
The document provides background information on the origins and early development of the Nazi party in Germany during the 1920s. It describes how the party began as the German Workers' Party led by Anton Drexler before Hitler joined in 1919 and became the leader in 1921. It also outlines some of the key aspects of the Nazi party platform outlined in the 25-point program, including nationalism, anti-Semitism, and a desire for more territory. Finally, it discusses Hitler's failed Munich Putsch coup attempt in 1923 and how he wrote Mein Kampf while in prison.
1) Post-war instability and economic crisis weakened established political systems in countries like Germany and Italy. 2) A sense of nationalism was used by fascist leaders to promote unity and scapegoat others for the nation's problems. 3) Charismatic leaders like Hitler and Mussolini were able to gain followers by promoting fascism as an alternative to communism and liberal democracy.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 10. THE FALL OF WEIMAR 1930-1933George Dumitrache
The document provides background information on the rise of the Nazi party in Germany between 1930-1933. It discusses how Germany's economic dependence on American loans led to the collapse of German industry following the 1929 Wall Street crash. This caused widespread unemployment, with over 6 million people jobless by 1932. As economic conditions deteriorated, support grew for the Nazis as they promised strong leadership and blamed Jews and communists for Germany's problems. The Nazis increased their Reichstag seats in elections in 1933 after Hitler became Chancellor, and he then used emergency powers to crush opposition and establish a one-party Nazi state in Germany.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 09. TABLES AND CARTOONSGeorge Dumitrache
The document discusses the Weimar Republic in Germany through tables and cartoons as part of a Cambridge IGCSE depth study on Germany. It provides information on the political and economic challenges faced by the Weimar Republic between 1919-1933 through statistical tables and illustrations. The depth study uses multiple visual elements to summarize key events and issues like inflation, unemployment, and the rise of extremism during this period of German history.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 08. NAZIS IN THE WILDERNESSGeorge Dumitrache
The “Lean Years” (also called the "wilderness" years) of Hitler and the Nazi Party in Germany refer to the period between 1924 and 1928 when the Nazi party did not have high levels of support and still suffered from humiliation over the Munich Putsch. Why where these years “lean”?
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 07. STRESEMMAN ERA 1924-1929George Dumitrache
Gustav Stresemann was appointed Chancellor of Germany in 1923 during the Weimar Republic period. As Chancellor and later as Foreign Minister, he implemented policies that helped stabilize Germany's economy and improve its international standing. This included establishing a new currency to end hyperinflation, crushing communist uprisings, and pursuing diplomatic agreements like the Locarno Pact to normalize Germany's relations with other European powers. However, the economic and political stability of the Weimar Republic remained fragile.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 06. THE BEER HALL PUTSCH 1923George Dumitrache
The Beer Hall Putsch, also known as the Munich Putsch, was a failed coup d'état by Nazi Party (Nationalsozialistische Deutsche Arbeiterpartei or NSDAP) leader Adolf Hitler, Generalquartiermeister Erich Ludendorff and other Kampfbund leaders in Munich, Bavaria, on 8–9 November 1923, during the Weimar Republic. Approximately two thousand Nazis marched on the Feldherrnhalle, in the city centre, but were confronted by a police cordon, which resulted in the deaths of 16 Nazi Party members and four police officers. Hitler escaped immediate arrest and was spirited off to safety in the countryside. After two days, he was arrested and charged with treason. The putsch brought Hitler to the attention of the German nation for the first time and generated front-page headlines in newspapers around the world. His arrest was followed by a 24-day trial, which was widely publicised and gave him a platform to express his nationalist sentiments to the nation. Hitler was found guilty of treason and sentenced to five years in Landsberg Prison, where he dictated Mein Kampf to fellow prisoners Emil Maurice and Rudolf Hess. On 20 December 1924, having served only nine months, Hitler was released. Once released, Hitler redirected his focus towards obtaining power through legal means rather than by revolution or force, and accordingly changed his tactics, further developing Nazi propaganda.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 05. HYPERINFLATIONGeorge Dumitrache
Hyperinflation affected the German Papiermark, the currency of the Weimar Republic, between 1921 and 1923, primarily in 1923. It caused considerable internal political instability in the country, the occupation of the Ruhr by France and Belgium, and misery for the general populace.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 03. THE TREATY OF VERSAILLES IMPACT ON...George Dumitrache
Thanks to the Treaty of Versailles, Germany's ability to produce revenue-generating coal and iron ore decreased. As war debts and reparations drained its coffers, the German government was unable to pay its debts. Some of the former World War I Allies didn't buy Germany's claim that it couldn't afford to pay.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 02. THE NOVEMBER REVOLUTION 1918George Dumitrache
The German Revolution or November Revolution was a civil conflict in the German Empire at the end of the First World War that resulted in the replacement of the German federal constitutional monarchy with a democratic parliamentary republic that later became known as the Weimar Republic. The revolutionary period lasted from November 1918 until the adoption of the Weimar Constitution in August 1919. Among the factors leading to the revolution were the extreme burdens suffered by the German population during the four years of war, the economic and psychological impacts of the German Empire's defeat by the Allies, and growing social tensions between the general population and the aristocratic and bourgeois elite.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 01. THE EFFECT OF WW1 ON GERMANYGeorge Dumitrache
The document summarizes the impact of World War 1 on Germany. It discusses how Germany initially found success on the Eastern Front and made advances on the Western Front in 1918 but was eventually overwhelmed as the US joined the war effort. Germany experienced political instability, economic devastation from blockades, widespread hunger and disease, and psychological trauma from defeat. The German people bitterly blamed leaders for the defeat, sowing seeds for the rise of the Nazis in the unstable Weimar Republic that followed the war.
QUESTIONS AND ANSWERS - LEAGUE OF NATIONS. The League of Nations was an international organization, headquartered in Geneva, Switzerland, created after the First World War to provide a forum for resolving international disputes.
This cartoon was likely published after the Stresa Pact was signed in early 1935, when Britain and France failed to raise the issue of Abyssinia with Mussolini and were perceived as turning a blind eye to his plans in hopes of keeping Italy as an ally against Germany. The cartoon directly criticizes the British and French policy of appeasing Mussolini, so the purpose was to criticize, not just inform. By criticizing the policy, the hope would be to influence and change the policy by swaying public opinion.
Manchurian Crisis. On September 18, 1931, an explosion destroyed a section of railway track near the city of Mukden. The Japanese, who owned the railway, blamed Chinese nationalists for the incident and used the opportunity to retaliate and invade Manchuria.
05. LEAGUE OF NATIONS - Great Depression and LON.pptxGeorge Dumitrache
GREAT DEPRESSION AND THE LEAGUE OF NATIONS. The Great Depression of 1930-33 meant people turned to extremist dictators such as Hitler and Mussolini, who were keen to invade other countries. This made it hard for the League to maintain peace. The League had some very ambitious plans and ideals – to stop war and make the world a better place.
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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.
Executive Directors Chat Leveraging AI for Diversity, Equity, and InclusionTechSoup
Let’s explore the intersection of technology and equity in the final session of our DEI series. Discover how AI tools, like ChatGPT, can be used to support and enhance your nonprofit's DEI initiatives. Participants will gain insights into practical AI applications and get tips for leveraging technology to advance their DEI goals.
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.
This presentation was provided by Steph Pollock of The American Psychological Association’s Journals Program, and Damita Snow, of The American Society of Civil Engineers (ASCE), for the initial session of NISO's 2024 Training Series "DEIA in the Scholarly Landscape." Session One: 'Setting Expectations: a DEIA Primer,' was held June 6, 2024.
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.
The simplified electron and muon model, Oscillating Spacetime: The Foundation...RitikBhardwaj56
Discover the Simplified Electron and Muon Model: A New Wave-Based Approach to Understanding Particles delves into a groundbreaking theory that presents electrons and muons as rotating soliton waves within oscillating spacetime. Geared towards students, researchers, and science buffs, this book breaks down complex ideas into simple explanations. It covers topics such as electron waves, temporal dynamics, and the implications of this model on particle physics. With clear illustrations and easy-to-follow explanations, readers will gain a new outlook on the universe's fundamental nature.
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. WHAT IS A DOT MAP?
• A dot distribution map, or dot density map, is a map
type that uses a dot symbol to show the presence of a
feature or a phenomenon.
• Dot maps rely on a visual scatter to show spatial
pattern.
4. DOT (DISTRIBUTION)
• A dot map uses dots to show the distribution (relative
density) of geographic phenomena between different
regions on a map.
• Each dot on a dot map represents a single feature or a
quantity (number value).
5.
6. OVERALL DISTRIBUTION
• When viewed as a whole, a dot map will give its
reader an impression of the overall distribution
(spread) of geographic phenomena throughout the
mapped area.
7. MEDICAL GEOGRAPHY
• Display of discrete data in the form of points in a map
can provide convincing evidence related to medical
geography.
• During the mid-1850s, cholera was a major concern.
• When a large outbreak occurred in London in 1854, Dr.
John Snow created a dot distribution map that settled a
debate between two schools of thought that cholera is
transmitted not through the inhalation of infected air,
but through the ingestion of contaminated water or
food.
8. Original map by John
Snow showing the
clusters of cholera
cases in the London
epidemic of 1854. The
pump is located at the
intersection of Broad
Street and Little
Windmill Street.
9. COMMON USE
• Dot maps are most commonly used to compare
population densities across a region.
10. HOW TO DO IT
1. Identify the geographic feature or phenomena being
mapped.
2. Verify the dot value. This can be done by reading the map’s
legend.
3. Identify the scale of the administrative regions shows on
the map (neighbourhoods, census areas, states or
countries).
4. Calculate the total value of features in each area of the
map.
5. Describe the distribution of the feature both within and
between different areas.
11. COMMON PATTERNS FOUND ON A MAP
1. CLUSTER – A group of people or features positioned or
occurring close together.
2. SCATTERED OR DISPERSED – Occurring or distributed over
widely spaced and irregular intervals.
3. GRID – A network of regularly spaced lines that cross one
another at right angles.
4. LINEAR – Arranged in or extending along a straight or
nearly straight line (river or coastline).
5. CONCENTRIC – Circles that share the same centre, the
larger surrounding the smaller.
6. RADIAL – Lines running directly from a centre point.
12.
13. STEPS TO CONSTRUCT A DOT MAP
1. Obtain a base map of the area or administrative regions
you wish to show.
2. Study the data to be mapped and decide on a dot value
(should be a rounded number).
3. Determine the number of dots required for each
administrative region.
4. Decide on an appropriate dot shape and size. As a general
guide, dots that are too small produce an overly sparse dot
pattern which is not very precise.
5. Place the correct number of dots within each
administrative boundary as determined in Step 2.