- Isarithmic maps have two different forms: isometric maps, which show point data, and isopleth maps where data occurs over geographical areas. The map shown is an example of an isopleth map because the temperature exists at.Types of isolines Isolines are often given specific names beginning "iso-" according to the nature of the variable being mapped, although in many usages
- Also called: Isopleth Map, Isopleth. Isoline maps show a range of quantity. They show data as a third dimension on a map, making them good for mapping surface elevations or for weather data. Radar maps, temperature maps and rainfall maps are all isoline maps.
- For example, this map shows the population density in the year 2007 for the United States of America. For each state, the number of persons per square mile has been calculated. The states with a lower population density are shaded with a lighter gray color. The states of a higher population density are shaded with a dark gray color.
- Answer: Choropleths show how a variable changes across existing geographical features such as countries. They’re good for showing things like “intensity” or “density” - the classic example is population density maps . Use them when it’s important to show the real-world geography. Population densit.
- For example, topographic maps showing contours of equal elevation are probably the most common type of isopleth maps. Relief highs (hills) are shown by concentric contour isopleths, and depressions such as volcanic craters are shown by concentric contours with hachures pointing toward the center of the depression. Isopleths are drawn on weather ...