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{{POTD {{{1|{{{style|default}}}}}}
{{POTD {{{1|{{{style|default}}}}}}
|image=Polyconic projection SW.jpg
|image=American Polyconic projection.jpg
|size=380
|size=380
|title= [[Polyconic projection|American Polyconic projection]]
|title= [[Polyconic projection|American Polyconic projection]]
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|caption=
|caption=


The '''[[Polyconic projection|American Polyconic projection]]''' is a [[map projection]] conceptualized as "rolling" a cone tangent to the Earth at all parallels of latitude, rather than as a single cone as in a normal conic projection. Each parallel is a circular arc of true scale. The scale is also true on the central meridian of the projection. The projection was in common use by many map-making agencies of the United States from the time of its proposal by [[Ferdinand Rudolph Hassler]] in 1825 until the middle of the 20th century.
The '''[[Polyconic projection|American Polyconic projection]]''' is a [[map projection]] conceptualized as "rolling" a separate cone tangent to the Earth at each parallel of latitude, rather than a single cone as in a normal conic projection. Each parallel is a circular arc of true scale. The scale is also true on the central meridian of the projection. This projection was in common use by many map-making agencies of the United States from the time of its proposal by [[Ferdinand Rudolph Hassler]] in 1825 until the mid-20th century.


|credit=Photograph: [[User:JJ Harrison|JJ Harrison]]
|credit=Map: [[User:Strebe|Strebe]], using Geocart
}}<noinclude>[[Category:Wikipedia Picture of the day {{#time:F Y|{{SUBPAGENAME}}}}]]
}}<noinclude>[[Category:Wikipedia Picture of the day {{#time:F Y|{{SUBPAGENAME}}}}]]
</noinclude>
==See also==
*[[Template:POTD{{#ifeq:{{BASEPAGENAME}}|POTD protected||_protected}}/{{SUBPAGENAME}}]]</noinclude>

Latest revision as of 00:04, 19 March 2019

American Polyconic projection
The American Polyconic projection is a map projection conceptualized as "rolling" a separate cone tangent to the Earth at each parallel of latitude, rather than a single cone as in a normal conic projection. Each parallel is a circular arc of true scale. The scale is also true on the central meridian of the projection. This projection was in common use by many map-making agencies of the United States from the time of its proposal by Ferdinand Rudolph Hassler in 1825 until the mid-20th century.Map: Strebe, using Geocart