Proceed to GeoCommunity Home Page


SpatialNewsGIS Data DepotGeoImaging ChannelGIS and MappingSoftwareGIS JobsGeoBids-RFPsGeoCommunity MarketplaceGIS Event Listings
HomeLoginAccountsAboutContactAdvertiseSearchFAQsForumsCartFree Newsletter

Sponsored by:


TOPICS
Download Data

Accounts

USGS DRGs

USGS DEMs

USGS DOQQs

FEMA Flood Data

VMAP

NWI

Gazetteer

Census/TIGER

Index Grids

About Data

Contact


SpatialNews Daily Newswire!
Subscribe now!

Latest Industry Headlines
SuperGeo to hold Biodiversity and Tourism GIS Training Courses
Merrick Awarded IDIQ by Corps of Engineers, Mobile District
Nottinghamshire Stops Vehicle Thieves in Their Tracks Thanks to Masternaut
GGP's GIS Addresses Corporate Information Needs in South Northamptonshire
ESRI GIS Services Available on Apps.gov

Latest GeoBids-RFPs
Wetland Inventories-OR
Photogrammetric Mapping-MO
Thermal Graphic Recorder-Canada
Surveying Services*Written in Polish
Geolocation Hardware-CA

Recent Job Opportunities
Marketing Specialist - Eonfusion - Full Time
Account Manager - Eonfusion - Full Time
GIS Developer
Senior GIS Applications Programmer

Recent Discussions
clr file DEM USGS
information or refrence for books
Opening .mxd file created in ArcGIS 9.3 ver
New GIS web: Using GIS architecture to play
Problem downloading e00 files - please help!
GISDataDepot - Data Projections

GISDataDepot > HelpDesk > Projections > Mollweide

Mollweide Projection

Carl B. Mollweide created this pseudo-cylindrical projection in 1805. It is an equal-area projection designed for small-scale maps.

The Mollweide projection has several alternate names: Babinet, Elliptical, Homolographic, and Homalographic

Method of Projection:
A pseudo-cylindrical equal-area projection. All parallels are straight lines and all meridians are equally spaced elliptical arcs, except the central meridian, which is a straight line. The poles are points.

Linear Graticule:
The Equator and central meridian.

Properties:

Shape: Shape is not distorted at the intersection of the central meridian and latitudes 4044' N and S. Distortion increases outward from these points and becomes severe at the edges of the projection.

Area: Equal-area.

Direction: Local angles are true only at the intersection of the central meridian and latitudes 4044' N and S. Direction is distorted elsewhere.

Distance:: Scale is true along latitudes 4044' N and S. Distortion increases with distance from these lines and becomes severe at the edges of the projection.

Limitations:
Useful only as a world map.

Uses and Applications:
Suitable for thematic or distribution mapping of the entire world, frequently in interrupted form.

Combined with the Sinusoidal to create Goode's Homolosine and Boggs.



Back to Top


Sponsored by:

For information
regarding
advertising rates
Click Here!

Copyright© 1995-2007 MindSites Group, LLC / Privacy Policy

GeoCommunity™, Wireless Developer Network™, GIS Data Depot®, and Spatial News™
including all logos and other service marks
are registered trademarks and trade communities of
MindSites Group, LLC