# Map Projections Classification

^{*}

*Geographies*

**2022**,

*2*(2), 274-285; https://doi.org/10.3390/geographies2020019 (registering DOI)

## Abstract

**:**

## 1. Introduction

#### 1.1. History

- The authors of the oldest known cylindrical and conic projections did not define their projections using indirect, developable surfaces. For example, Mercator, in the 16th century, did not use a cylindrical surface to define the projection now called Mercator’s cylindrical projection, or Lambert, in the 18th century, did not use a conical surface to define the projection now called Lambert’s conformal conic projection. On the contrary, after deriving the equations of that projection, Lambert [13] mentioned that the map made in that projection could be folded into a cone.
- It seems that developable surfaces related to map projections appear for the first time in the second half of the 19th century. D’Avezac-Macaya [4] referred to “les projections perspectives, les developements de surfaces osculatrices ou pénétrantes”, that is, tangent or secant surfaces, specifically “les développements cylindriques” and “cóniques”, and the catch-all “les systèmes conventionneles”. Snyder [3] did not find any earlier cartographic references to developable surfaces. Let us mention the famous older authors who dealt with map projections, not to mention developable surfaces: Lambert [13], Euler [14], Lagrange [15], Gauss [16] and Tissot [17].

#### 1.2. Conceptuality

- One of the most common classifications, and the one principally used by Snyder [3], is based on association, at least conceptually, to a developable surface.
- Map projections are mappings of a curved surface, most often a sphere or ellipsoid, into a plane. The introduction of developable surfaces as intermediate surfaces and the interpretation according to which a sphere or ellipsoid is first mapped to such a surface which then develops into a plane is a fabrication that generally does not correspond to reality. It is usually justified by the term conceptual [2] and explained by the claim that map projections are easier to interpret in this way.
- “The reference globe and developable surfaces are conceptual aids that help illustrate the projection process, but they are not used to create projections today. Rather, the field of mathematics is utilized to create projections, and so it is important to understand some of the basic mathematical manipulations used to project the Earth onto a map.” [9]. The first part of the first sentence is questionable because developable surfaces are not used in the projection process, in general. The rest of the quotation we fully accept. As everybody can see, there are no developable surfaces in the whole chapter 8.3 of the cited book.
- “The classification of projections according to developable surfaces (cylinder, cone, and plane) is useful for the comprehension of selecting projections and their parameters. However, while developable surfaces are a useful conceptual tool, it needs to be emphasized that most map projections cannot be constructed geometrically but are instead defined mathematically” [18]. It remains unclear why Šavrič et al. [18] mentioned the classification of map projections using developable surfaces when they are not used in their Projection Wizard.
- “While the concept of developable surfaces provides a nice way to visualize the basics of map projections, as stated before, the transformation is really driven by mathematical equations” [10]. The basics of map projections are not connected to developable surfaces at all.

#### 1.3. Prior Warning

- This approach to the classification of map projections is common. Map projections are typically classified according to the geometric surface from which they are derived: cylinder, cone or plane. However, such an approach is only correct at first glance. In fact, the opposite is true. Cylindrical projections are not called so because of the mapping on a cylindrical surface but because the map made in such a projection can be bent into a cylinder. Similarly, conic projections are not called so because of mapping to a conical surface but because a map made in a conic projection can be bent into a cone. More than 100 years ago, in a paper on map projections, Close and Clarke [19] wrote: “Conical projections are those in which the parallels are represented by concentric circles and the meridians by equally spaced radii. There is no necessary connexion between a conical projection and any touching or secant cone. The name conical is given to the group embraced by the above definition, because as is obvious, a projection so drawn can be round to form a cone.” In a well-known paper on the nomenclature and classification of map projections, Lee [20] explained: “Cylindric: projections in which the meridians are represented as a system of equidistant parallel straight lines, and the parallels by a system of parallel straight lines at right angles to the meridians.
- Conic: projections in which the meridians are represented as...
- Azimuthal: projections in which the meridians are represented as...

#### 1.4. Isometry

- Authors who nowadays describe map projections in great detail with the help of developable surfaces may not even be aware of the fact that, in this way, they introduce double mappings into the theory of map projections. First, the Earth’s sphere is mapped to the auxiliary developable surface, and then it is transformed in some way, e.g., by development, into a map in the plane. Double mappings have their role in the theory of map projections in some special cases, not in general. One should know that developing into a plane is isometry, i.e., such a mapping that preserves distances.
- The use of development surfaces in the definition of map projection is justified only for a small number of projections, projections in which the mapping is real and not conceptual to the corresponding developable surface. Namely, in addition to cylindrical and conic projections, there are many others, such as azimuthal, pseudocylindrical, pseudoconic, conditional, etc., which cannot be interpreted by mapping to a cylinder or cone surface. There are some attempts in that direction. For example, it is said that a pseudocylindrical projection is a mapping to a pseudocylinder but without saying what a pseudocylinder is [7]. Or that such a projection is interpreted as a mapping to an oval surface, without noticing that it is not a developable surface [8].
- In the context of the classification of projections into conical, cylindrical and azimuthal/plane, it is unnatural to use a plane as a developable surface. Namely, developing is isometry, and thus we see no purpose in developing plane into plane.
- Developing the auxiliary surface into a plane (Figure 2) preserves distances (isometry). This would then mean that the two selected parallels as standard parallels in all normal aspect projections are mapped to parallels that are at the same distance from each other. Is that possible? Of course not.

#### 1.5. Standard vs. Secant Parallels

- Authors who perceive map projections as mappings with the help of an auxiliary surface regularly distinguish the case of touching and cutting. For them, as a rule, the cross-sectional curve is also a curve without deformations. They take that fact for granted, without proof. However, it has been shown that standard parallels and secant parallels are two different concepts and that they generally do not coincide [21,22,23].
- “Where the ellipsoid and the map projection surface touch, in this case, intersect, there is no distortion. However, between the standard lines the map is under the ellipsoid and outside of them the map is above it.” [5,6]. From this quote, it is clear that van Sickle did not distinguish between secant and standard parallels.
- The use of developable surfaces leads to secant projections, i.e., mappings on the auxiliary developable surface that intersects the mapped surface and thence the conclusion that azimuthal projections can have at most one standard parallel and conic at most two. This is wrong because there are azimuthal and conic projections with several standard parallels [24,25].
- It is generally accepted that a secant projection is a mapping on an auxiliary surface that intersects a sphere or an ellipsoid and that the intersections of the secant conic and cylindrical projection are without deformations (Figure 3). Thus, for example, in ESRI’s dictionary [11], we were able to read several years ago: “Secant projection: A projection whose surface intersects the surface of a globe. A secant conic or cylindrical projection, for example, is recessed into a globe, intersecting it at two circles. At the lines of intersection, the projection is free from distortion.” This definition is not good. First, the intersection of two second-order surfaces is a fourth-order curve that generally does not consist of two circles. However, this shortcoming could be corrected by specifying the mutual position of the surface of the cone or cylinder and the sphere. However, the claim that the line of intersection of two surfaces is free of deformation cannot be an integral part of the definition because, in addition to being a claim, it is generally erroneous. However, it is so ingrained that it is almost regularly taken as true without evidence. The cited webpage is no longer available, but ESRI retains the term secant projection within the definitions of cylindrical and conical projections [11].

#### 1.6. Conclusions

- Instead of a conceptual approach that is also wrong in some parts, it is necessary to return to reality and not run away from mathematics. Let us just recall that the study of map projections was not so long ago called mathematical cartography.
- Explaining the mapping of a sphere or ellipsoid to the surface of a cylinder or cone is a convenient story, which, unfortunately, while avoiding the mathematical background of the process, leads to erroneous claims which, most likely, the authors are not aware of.

## 2. Map Projections Classification

- Properties of mapping or types of distortions;
- The shape of a (pseudo)graticule;
- Projection aspect, i.e., position of the axis of projection in relation to the axis of rotation of the sphere.

#### 2.1. Classification of Map Projections According to Types of Distortions

#### 2.2. Classification of Projections According to the Shape of the Pseudograticule

- Cylindrical projections are projections in which pseudomeridians are shown in mutually parallel straight lines and pseudoparallels in mutually parallel straight lines perpendicular to images of pseudomeridians (Figure 6a). Cylindrical projections are not mappings onto a cylindrical surface in general. A map made in a cylindrical projection can be folded into a cylindrical surface.
- Conic projections in the narrower sense are projections in which pseudomeridians are represented by straight lines that intersect at one point and pseudoparallels by concentric circular arcs, with the angle between any two pseudomeridians being less than the difference of the corresponding pseudogeographic longitudes (Figure 6b). Conic projections are not mappings onto a conical surface in general. A map made in a conic projection can be folded into a conical surface.
- Azimuthal projections are projections in which pseudomeridians are shown as straight lines that intersect at one point and pseudoparallels by concentric circles, with the angle between any two pseudomeridians being equal to the difference of the corresponding pseudogeographic longitudes (Figure 6c). Azimuthal projections are planar projections, but this is not their special characteristic because all map projections are mappings onto a plane.
- Pseudocylindrical projections are projections in which pseudomeridians are represented by curves symmetrical with respect to the middle pseudomeridian mapped as a straight line and pseudoparallels as mutually parallel straight lines perpendicular to the image of the central pseudomeridian (Figure 6d).
- Pseudoconic projections are projections in which pseudomeridians are represented by curves symmetric with respect to the middle pseudomeridian mapped as a straight line and pseudoparallels as arcs of concentric circles (Figure 6e).
- Polyconic projections are projections in which pseudomeridians are mapped as curves symmetric with respect to the central pseudomeridian which is mapped as a straight line, and pseudoparallels are mapped as eccentric circles whose centers are on the central pseudomeridian (Figure 6f).
- Circular projections are projections in which pseudomeridians are mapped as arcs of circles symmetrical in relation to the central pseudomeridian which is mapped as a straight line, and pseudoparallels are mapped as arcs of circles whose centers are on the central pseudomeridian (Figure 6g).
- Other projections are projections in which pseudomeridians and pseudoparallels are mapped as more complex curves (Figure 6h).

#### 2.3. Classification of Projections According to the Aspect of Projection

- The normal aspect is the aspect in which the axis of projection coincides with the axis of the sphere, and the pseudograticule coincides with the graticule (Figure 7a).
- The transverse aspect is the aspect in which the axis of projection is perpendicular to the axis of the sphere (Figure 7b).
- The oblique aspect is an aspect that is neither normal nor transverse (Figure 7c).
- It should be emphasized that instead of the normal, transverse and oblique aspect of map projection, the terms normal, transverse and oblique projection are also used. The pseudograticule is also called in the literature the network of verticals and almucantars, and the image of that network in the projection plane is a normal cartographic network, i.e., a network that has a simpler shape in a given group of projections than any other network [26].

## 3. Conclusions

- Most map projections in their definition do not have an auxiliary surface.
- The application of the auxiliary/intermediate developable surface can lead to the wrong conclusion about the distortion distribution—standard parallels (parallels with zero distortion) and secant parallels generally do not coincide.
- It is not recommended to classify map projections based on the developable surfaces because such a classification (1) cannot fit many map projections, (2) implicitly or explicitly gives a high weight to the developable surfaces in the theory of map projection which they do not deserve, (3) misleads that standard parallels and secant parallels are one and the same, which is not true in general, and (4) states the wrong conclusion that there are other developable surfaces (pseudocylinders, ovals) by which pseudocylindrical and other map projections can be defined.
- Cylindrical, conical and azimuthal projections belong to the classification of map projections according to the shape of the graticule in normal aspect projections. In such a classification, naturally enter pseudocylindrical, pseudoconical, polyconic and other projections.

- According to kinds of distortions: conformal, equal-area, equidistant and other;
- According to aspect: normal, transversal, oblique;
- According to the form of the graticule in normal aspect: cylindrical, conic, azimuthal, pseudoconic, pseudocylindrical, polyconic, circular and others.

## Author Contributions

## Funding

## Data Availability Statement

## Acknowledgments

## Conflicts of Interest

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**Figure 1.**The three developable projection surfaces: cylinder, cone and plane. (Only half of the cylinder and cone are shown.) By permission of Charles Preppernau, the author of the image.

**Figure 2.**(

**a**) Cylindrical surface cut from base to base and development of the cylindrical surface. (

**b**) Conical surface cut from base to apex and development of the conical surface.

**Figure 3.**Illustration of standard parallels as secant parallels. Source: Deetz and Adams [26], page 80. This is a misguided approach accompanied by the caption: "Diagram illustrating the intersection of a cone and sphere along two standard parallels". In other words, for Deetz and Adams (and many others) standard parallels and secant parallels are identical. The proof is missing, and this is a fake.

**Figure 5.**Image of the graticule (black) and the pseudograticule (blue) in the oblique Mollweide projection.

**Figure 6.**Classification of projections according to the shape of the pseudograticule. It is also the graticule in normal aspect projections (see next section): (

**a**) cylindrical; (

**b**) conic; (

**c**) azimuthal; (

**d**) pseudocylindrical; (

**e**) pseudoconic; (

**f**) polyconic; (

**g**) circular; (

**h**) other.

**Figure 7.**Image of the graticule in the Mollweide (

**a**) normal aspect projection, (

**b**) transverse aspect projection, (

**c**) oblique aspect projection.

**Figure 8.**North America in (

**a**) normal conic, (

**b**) oblique azimuthal and (

**c**) transverse cylindrical projection.

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Lapaine, M.; Frančula, N.
Map Projections Classification. *Geographies* **2022**, *2*, 274-285.
https://doi.org/10.3390/geographies2020019

**AMA Style**

Lapaine M, Frančula N.
Map Projections Classification. *Geographies*. 2022; 2(2):274-285.
https://doi.org/10.3390/geographies2020019

**Chicago/Turabian Style**

Lapaine, Miljenko, and Nedjeljko Frančula.
2022. "Map Projections Classification" *Geographies* 2, no. 2: 274-285.
https://doi.org/10.3390/geographies2020019