ArcGIS Desktop

  • ArcGIS Pro
  • ArcMap

  • My Profile
  • Help
  • Sign Out
ArcGIS Desktop

ArcGIS Online

The mapping platform for your organization

ArcGIS Desktop

A complete professional GIS

ArcGIS Enterprise

GIS in your enterprise

ArcGIS Developers

Tools to build location-aware apps

ArcGIS Solutions

Free template maps and apps for your industry

ArcGIS Marketplace

Get apps and data for your organization

  • Documentation
  • Support
Esri
  • Sign In
user
  • My Profile
  • Sign Out

ArcMap

  • Home
  • Get Started
  • Map
  • Analyze
  • Manage Data
  • Tools
  • Extensions

Eckert I

  • Description
  • Projection properties
  • Usage
  • Limitations
  • Parameters
  • Sources

Description

The Eckert I projection is a compromise pseudocylindrical map projection with rectilinear meridians and an odd appearance. The projection is simple, but it has no practical use other than making a world map with an unusual shape.

The projection was introduced by Max Eckert in 1906. It is available in ArcGIS Pro 1.0 and later and in ArcGIS Desktop 8.0 and later.

An example of the Eckert I projection
The Eckert I compromise projection centered on Greenwich is shown.

Projection properties

The subsections below describe the Eckert I projection properties.

Graticule

Eckert I is a pseudocylindric projection. The meridians are regularly distributed straight lines interrupted at the equator. The central meridian is a straight line, half the length of the projected equator. The parallels are equally distributed straight lines, perpendicular to the central meridian. The poles are straight lines, half the length of equator. The graticule is symmetric across the equator and the central meridian.

Distortion

Eckert I is neither conformal nor equal area. It generally distorts shapes, areas, distances, directions, and angles. Scale is correct along the 47°10' North and South parallels and constant along any given parallel and meridian. Due to the discontinuity, distortion cannot be determined at the equator. Distortion values are symmetric across the equator and the central meridian.

Usage

The Eckert I projection has no practical use other than designing a world map with an unusual shape.

Limitations

Eckert I is supported on spheres only. For an ellipsoid, the semimajor axis is used for the radius. Some distortion properties are not maintained when an ellipsoid is used.

Parameters

Eckert I parameters are as follows:

  • False Easting
  • False Northing
  • Central Meridian

Sources

Canters, F. (2002). Small-scale Map Projection Design. London: Taylor & Francis.

Snyder, J. P. (1993). Flattening the Earth. Two Thousand Years of Map Projections. Chicago and London: University of Chicago Press.

Snyder, J. P. and Voxland, P. M. (1989). An Album of Map Projections. U.S. Geological Survey Professional Paper 1453.Washington, DC: United States Government Printing Office.

ArcGIS Desktop

  • Home
  • Documentation
  • Support

ArcGIS

  • ArcGIS Online
  • ArcGIS Desktop
  • ArcGIS Enterprise
  • ArcGIS
  • ArcGIS Developer
  • ArcGIS Solutions
  • ArcGIS Marketplace

About Esri

  • About Us
  • Careers
  • Esri Blog
  • User Conference
  • Developer Summit
Esri
Tell us what you think.
Copyright © 2021 Esri. | Privacy | Legal