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  1. Equal-area and equidistant projections appear in the National Atlas. Other projections, such as the Miller Cylindrical and the Van der Grinten, are chosen occasionally for convenience, sometimes making use of existing base maps prepared by others. Some projections treat the Earth only as a sphere, others as either ellipsoid or sphere.

  2. Apr 6, 2015 · The Albers equal area conic is the typical projection for historical USGS maps of the lower 48, it being a general-purpose low-distortion compromise for mid-latitude short and wide extents. As a reference on map projections, I like the ESRI book Understanding Map Projections. Its first 30 pages are not unlike a short textbook, followed by ~70 ...

    • Determine What Projection Your Source Map Is in
    • Find The SRID of Your Target Projection
    • Convert The Shapefile to The New Projection
    • Save Your New Map with A Useful Filename

    This will vary with what kind of spatial file you’re using, but we’re assuming shapefile. A shapefile actually is a folder containing several files. There are sometimes more, but shapefiles almost always have a .shp, a .dbf and a .prj file. As you might have guessed, the projection information is in the .prj file. Here’s a .prj file from a Californ...

    There are a few ways you might find the SRID of the new projection you want. If you found the projection on a government mapping site, the site might list the EPSG IDof the projection. If you’re not lucky enough to have an SRID in hand, your next best friend is a search engine and spatialreference.org. For example, if you need to look up the Google...

    In Quantum GIS, this is as easy as right-clicking the layer you want to project, choose Save As, then choose Browse next to CRS (that stands for coordinate reference system), and search by EPSG.

    This seems like a minor point, but I have maybe 10 identical shapefiles of the California state border in different projections. Do yourself a favor and include the SRIDin the filename (e.g. california_border_4326.shp).

  3. The equal area projection retains the relative size of the area throughout a map. So that means at any given region in a map, it keeps the true size of features. While equal area projections preserve area, they distort shape and angles. But it cannot be conformal. Let’s review some advantages and examples of using this type of projection.

    • why is the national atlast equal area projection different from normal view1
    • why is the national atlast equal area projection different from normal view2
    • why is the national atlast equal area projection different from normal view3
    • why is the national atlast equal area projection different from normal view4
    • why is the national atlast equal area projection different from normal view5
  4. Dec 20, 2018 · Albers Equal Area Projections are equal area or equivalent projections, where angles and shape are distorted while preserving area. Thus, equal area projections are commonly used for thematic or quantitative mapping, especially when comparing or measuring areal data, such as when one is comparing national park sizes or the percentage of forested land within regions.

  5. Equal-area and equidistant projections appear in the National Atlas. Other projections, such as the Miller Cylindrical and the Van der Grinten, are chosen occasionally for convenience, sometimes making use of existing base maps prepared by others. Some projections treat the Earth only as a sphere, others as either ellipsoid or sphere.

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  7. How to Select the Right Projection. Keep in mind that all projections either disort or preserve one of the following properties: It is useful to think about projections grouped by the properties they preserve. Equal area projections. The British Columbia (BC) Albers Equal Area Conic projection is an example of an equal area projection.