Spatial Analysis and Map Projections
Spatial Patterns and Analysis
Spatial Concepts
Spatial: Relates to space and the arrangement of geographic features on Earth's surface.
Spatial patterns examine how and where geographic features occur. Geographers analyze why these features are arranged in certain ways.
Example: The distribution of the 10 largest U.S. cities and the significance of their locations.
Distance
Absolute Distance:
Measurable distance in standard units.
Examples: feet, miles, kilometers.
Example: The absolute distance between Yosemite National Park and Rocky Mountain National Park is miles.
Relative Distance:
Measures social, cultural, or political differences or similarities between locations.
Cannot be depicted on maps directly.
Example: Income levels in a Brooklyn neighborhood, where areas a block apart may have vast differences in lifestyle due to income disparities.
Direction
Absolute Direction:
Cardinal directions: north, south, east, west.
Relative Direction:
Describes a location in reference to another.
Example: Giving directions to a classroom using landmarks and turns instead of cardinal directions and paces.
Clustering and Dispersal
Describe the organization of phenomena across an area.
Clustered: Phenomena are close together.
Example: Apartment buildings in New York City.
Dispersed: Phenomena are far apart.
Example: Farms in the Midwest.
Elevation
Measures the height of geographic features relative to sea level.
Map Features
Map Scale
Indicates the relationship between distance on the map and distance in the real world.
Represented as a ratio or a bar scale.
Direction
Indicated by a compass rose, showing cardinal directions (north, south, east, west) and sometimes intermediate directions.
Map Scale (versus Scale of the Map)
Map's Scale: Refers to distance representation on the map.
Scale of the Map: Refers to how much of the world is shown on the map.
Large Scale Map: Zooms into a particular area with more detail.
Small Scale Map: Zooms out to a national or global scale with less detail.
Types of Maps
Reference Maps
Display specific geographic locations.
Examples: road maps, political maps showing boundaries of states and countries.
Thematic Maps
Specialize in displaying geographic information, not just locations.
Choropleth Map
Visualizes data from specific geographic regions using different colors.
Example: A map showing the distribution of Anglicans in Australia, with darker greens indicating higher concentrations.
Cartogram
Distorts the size of geographic shapes to display differences in data.
Example: A cartogram showing countries sized according to their resources devoted to organic farming.
Australia appears much larger, indicating a high commitment to organic farming.
Graduated/Proportional Symbol Map
Uses symbols that grow in proportion to the data represented.
Example: A map of Europe showing countries' wealth, with larger symbols indicating wealthier countries.
Dot Distribution Map
Uses dots to visualize the location of certain data points.
Example: John Snow's map of cholera outbreak in London, where dots represented infections, revealing the source as a contaminated water pump.
Can also represent population distribution.
Isoline Map
Uses lines to depict changes in data.
Commonly used for elevation, where close lines indicate rapid changes (steep hill) and distant lines indicate slow changes (gradual descent).
Map Projections and Distortions
General Principles
All maps are selective and distorted because they represent a 3D object (Earth) on a 2D surface.
Specific Map Projections
Mercator Projection
Latitude and longitude lines meet at right angles, making it good for determining direction.
Distortion increases further from the Equator; land forms near the Equator are more accurate.
Greenland appears much larger than it is in reality.
Peter's Projection
Depicts continents according to the true size of their landmasses.
Shapes of landmasses are distorted.
Good Homolosine Projection
Accurately represents the shapes of landmasses but breaks up the oceans.
Polar Projection
Views the world from the North or South Pole.
Directions and land shapes are accurate near the middle, but distortion increases away from the center.
Robinson Projection
Distributes distortion to all parts of the map, serving as a compromise between Mercator and Peters projections.
Minimal distortion in land masses, making it a preferred choice for modern geographers.