The other systems

The view that makes a line a point

Descriptive geometry's first drill is to look at an edge from a direction perpendicular to it, so it draws at true length, and then along it, so it draws as a point. Both are the same identity — the imaged length is the true length times the sine of the angle to the ray — and the sine holds to 1e-12 across the whole sweep of directions.

Worth reading first: Parallel projection is not primitive perspective · What isometric actually means.

A first-year descriptive geometry course spends several weeks on a drill. Given a line drawn in two views, construct a third view in which it appears at its true length; then construct a fourth in which it appears as a single point; then, from those, the true shape of a plane face containing it.

Drawn on paper the drill is a sequence of operations with folding lines, transfer distances and rules about which measurement comes from which view. It reads like a recipe, and it is one — but the recipe is not an approximation to anything, and that makes it unusual on this site. Almost every taught construction the wrong field measures turns out to be a rule of thumb standing in for a projection. This one is a projection, written as an instruction.

True length, point view, true shapeThree views of one face, differing only in the direction they are taken along. The first is chosen perpendicular to the marked edge, so that edge is at true length, 1.3928 m. The second is taken along that edge, so the edge is a point and the face is a line. The third is along the face's own normal, and the face is at true shape — 1.3232 m². Nothing is measured off the paper; each is the projection the chosen direction produces.true length1.3928 mpoint viewthe edge is one pointtrue shape1.3232 m²one face, three ray directionseach step is a choice of direction, not a construction on the paper
Fig. 1 The three steps, each a projection along a stated direction rather than a construction on the paper. Perpendicular to the marked edge: the edge draws at true length, 1.3928 m. Along the edge: it draws as a point and the face draws as a line. Along the face’s normal: the face draws at true shape, 1.3232 m².

One identity, read three ways

An orthographic projection drops the component of everything along the ray direction. So for a segment v\mathbf{v} and a unit ray direction d^\hat{\mathbf{d}}, what survives is the part of v\mathbf{v} perpendicular to d^\hat{\mathbf{d}}, and its length is

vsinθ|\mathbf{v}| \sin\theta

where θ\theta is the angle between the segment and the ray. That is the whole of it, and the drill’s two headline constructions are its two extreme values.

θ=90°\theta = 90°: true length. The ray is perpendicular to the segment, nothing is dropped, and the drawn length is the real one.

θ=0\theta = 0: point view. The ray is along the segment, everything is dropped, and the segment draws as a single point.

How long a line looks, against the direction it is looked alongA sine, exactly — the worst departure over the sweep is 6e-16. At 0° the line images as a point and the view is the drawing office's point view; at 90° it images at true length, and every direction perpendicular to it does, which is a whole circle of them rather than one lucky choice.00.2500.5000.7501050100150angle between the ray direction and the line (°)imaged ÷ true lengthtrue length — a circle of directionspoint viewone segment, every viewing directionsine to 6e-16
Fig. 2 The imaged length as a fraction of the true one, against the angle between the ray direction and the line. A sine — the worst departure across the sweep is 6e-16. The two constructions the drawing office names are the two ends of it, and everything between is the foreshortening a view happens to apply.

True length is a circle of directions, not a construction

The drill’s phrasing hides something worth saying out loud. It asks the student to construct the auxiliary view that shows the line at true length, as if there were one.

There is a whole circle of them. Any direction perpendicular to the segment gives sinθ=1\sin\theta = 1, and the directions perpendicular to a given line in space form a plane — so a whole circle of unit directions, a one-parameter family, each of which draws the line at exactly its own length.

That is why the drill is a drill rather than a search. The student is not finding the direction that works; every direction in a circle works, and the folding line’s placement chooses one of them for reasons of layout — which view it can take its transfer distances from, and where the new view will fit on the sheet.

The same is true of the point view: a segment has exactly one direction along it, up to sign, so the point view is unique. True length is a circle and point view is a point, and the asymmetry is a fact about the geometry rather than about the teaching.

Why a second auxiliary is needed for a face

A plane face needs the same argument one dimension up, and the count changes.

The area of a face’s image is its true area times the cosine of the angle between the face’s normal and the ray direction — the same dropping of a component, applied to a two-dimensional patch. The face draws at true shape only when the ray is along its normal, and that is one direction rather than a circle.

The same face, square on and notThe area of a face's image is its true area times the cosine of the angle between the ray direction and the face's normal — 0.8290 here, so 1.3232 m² of face draws 1.0970 m² of picture. Only the view along the normal shows the shape; every other view shows a foreshortening that cannot be undone without knowing which one it was.square on · 1.323 m²and not · 1.097 m²the ratio is the cosine, 0.8290one face, two ray directions
Fig. 3 One face, drawn along its own normal and along a direction 34° off it. The ratio of the two areas is the cosine, 0.8290, exactly — 1.3232 m² of face drawing 1.0970 m² of picture. A foreshortened face cannot be un-foreshortened without knowing which direction did it.
The same face, square on and notThe area of a face's image is its true area times the cosine of the angle between the ray direction and the face's normal — 0.5299 here, so 1.3232 m² of face draws 0.7012 m² of picture. Only the view along the normal shows the shape; every other view shows a foreshortening that cannot be undone without knowing which one it was.square on · 1.323 m²and not · 0.701 m²the ratio is the cosine, 0.5299one face, two ray directions
Fig. 4 The same face at 58°: the cosine is 0.5299 and the drawn area is 0.7012 m². Nothing about the outline says which of these two it is — a foreshortened square and a genuine rectangle draw the same picture.

So the drill’s first auxiliary cannot reach the true shape in one step. It brings an edge of the face to true length; the second, taken along that edge, puts the face edge-on; and the third, perpendicular to that edge-on line, is along the normal. The steps are three because the constraints are three, and a course that presented the sequence as a convention would be leaving out the only reason it has to be a sequence.

What the standard three views are

The front, top and side views are auxiliary views with the direction chosen once and for all, and the choice is made for exactly the property this essay is about.

A rectilinear part has its edges along three perpendicular directions. Look along one of them, and the other two are at θ=90°\theta = 90° — true length, both of them — while the third is at θ=0\theta = 0 and draws as a point. So each standard view shows two of the part’s three families of edges at true length, which is what makes the drawing dimensionable with a ruler.

One cube in 3 parallel drawing systemsEvery one preserves midpoints exactly. What separates them is the axis scales, printed beneath each — isometric's are all 0.8165, which is equal and is not 1. elevation's are 1.000, 1.000 and 0.000.elevationx 1.000y 1.000z 0.000cabinetx 1.000y 1.000z 0.500isometricx 0.816y 0.816z 0.816axis scales measured from the drawingall 3 preserve midpoints
Fig. 5 Elevation beside two systems that give up its property. Its axis scales are 1.000, 1.000 and 0.000 — two axes at true length and the third dropped entirely, which is the sine law at its two ends in a single picture.

An axonometric view gives that up on purpose. Looking along a direction off all three axes puts every family at some intermediate θ\theta, so nothing is at true length and every edge is foreshortened by its own factor — which is what the axis scales are, and why they satisfy an identity rather than being free.

Squares of the three axis scales, summedAn orthographic projection has two orthonormal picture axes, so its three foreshortening ratios always satisfy sx² + sy² + sz² = 2 — to 4e-16 across 24 sampled viewing directions and every named axonometric system. Cavalier and military give 3 and cabinet 2.25, which is the arithmetic saying none of the three is the ORTHOGRAPHIC projection of anything — and, as the recovery shows, saying nothing at all about whether they are projections.2 — every orthographic projectionisometric · axonometric 0.816 · 0.816 · 0.8162.0000dimetric · axonometric 0.943 · 0.943 · 0.4712.0000trimetric · axonometric 0.876 · 0.966 · 0.5482.0000cavalier · oblique 1.000 · 1.000 · 1.0003.0000cabinet · oblique 1.000 · 1.000 · 0.5002.2500elevation · orthographic 1.000 · 1.000 · 0.0002.0000military · planometric 1.000 · 1.000 · 1.0003.0000isometric's three equal scales are forced to √(2/3) = 0.816497not chosen — the identity leaves no other value
Fig. 6 The identity the three foreshortening factors obey: their squares sum to 2, to 4e-16 across 24 viewing directions. It is the sine law summed over three perpendicular families — an orthographic projection keeps exactly two dimensions of the three, and the accounting has to come out.

The measurement a foreshortened view supports, and the one it does not

There is a practical rule buried here that the drill never quite states, and it is the reason a drawing office cares which view a length is taken from.

A length measured in a view is vsinθ|\mathbf{v}|\sin\theta, and θ\theta is not observable in that view. So a ruler laid on a drawing measures something true only when the reader knows the segment’s direction independently — which, in a standard view of a rectilinear part, they do.

That is exactly the failure the ruler essay measures on an isometric drawing: the same physical length draws at different lengths depending on which way it runs, so a single scale bar is wrong for everything except the directions it was drawn for.

The image of a circle in the xy plane, in 4 systemscavalier draws this plane isotropically — the circle stays a circle at 1.0000, so a length in it can be taken off the paper with a ruler whichever way it runs. The others draw it as an ellipse, and the ratio printed under each is the factor a ruler is wrong by between the best direction and the worst.isometric0.57741 : 1.732dimetric0.88191 : 1.134cavalier1.0000a circlemilitary0.57741 : 1.732the xy plane's drawn ellipseratio of the ellipse's axes, sampled
Fig. 7 The same question asked of a whole plane rather than a line: the image of a circle lying in it. Where the ratio is 1.0000 the plane is drawn isotropically and a ruler works in every direction within it; everywhere else the number is the factor a ruler is wrong by between the best direction and the worst.

The scale bar problem, stated exactly

A drawing carries one scale bar and an isometric drawing has three foreshortenings, so the bar is right for at most one family of directions and wrong for the rest. Two consequences follow and they are usually confused with each other.

The first is that a length off the paper needs a direction before it can be converted, and the direction has to come from the reader’s understanding of the object rather than from the picture. The second is that a length not along any axis has a foreshortening of its own, lying somewhere between the extremes, and no scale bar can be drawn for it at all.

Which is why axonometric drawings are illustrations and orthographic views are documents. The illustration shows the object; the document is the thing a length is taken from.

The drill checked against the projection it claims to produce

The site’s habit is that a taught construction is drawn beside the projection it is supposed to produce, so it can be checked rather than trusted. Run that here and the three steps come out exact:

  • the edge’s imaged length in the first auxiliary equals its true length to 1e-16 of a metre;
  • its imaged length in the second is zero to the same precision, which is what “a point” means numerically;
  • the face’s imaged area in the third equals its true area to 1e-16 of a square metre.

Those are not tolerances. They are the arithmetic saying the construction is an identity, and it is worth contrasting with the numbers the same treatment produces elsewhere on this site: the four-centre ellipse falls 5.72% short at the ends of its major axis, the by-eye depth division misplaces a post by metres, and the taught cone of vision turns out to be a statement about the reader rather than the picture.

The four-centre ellipse, and the ellipseThe four arcs are tangent to the rhombus at the four side midpoints and touch the true conic at exactly those four points. Everywhere else they are wrong, worst at the ends of the major axis, where the construction falls 5.72% short — and its minor axis is 3.53% too long, so a hole drawn this way is the wrong shape as well as the wrong size.true ellipse — axis ratio 0.5774four arcs — 5.72% short along the major axisthe four tangent points are exactworst departure 5.72% of the semi-major axis
Fig. 8 For contrast, a drawing-office construction that is not an identity. The four-centre ellipse touches the true conic at exactly four points and is wrong everywhere else — 5.72% short at the ends of the major axis. Both constructions are taught the same way; only one of them is the projection it claims to be.

Where the drill’s transfer distances come from

Worth one paragraph, because it is the part of the recipe that looks most like bookkeeping and is in fact the whole content.

Constructing a new view on paper means computing, for each point, its two coordinates in the new picture. One of them is shared with the view being projected from — the direction in the picture plane that both views have in common, which is why the new view is drawn “folded” about a line. The other is the coordinate along the old view’s ray direction, which the old view dropped and which some earlier view still has.

So the transfer distances are the recovery of the coordinate the previous projection destroyed, taken from a view that did not destroy it. The drill is a sequence of projections precisely because each one drops a different component, and the sheet as a whole holds all three.

That is also why two views are enough to start from and one is not. One orthographic view has dropped a coordinate outright, and no construction on the paper can supply it.

Three views, and two solids that draw themA stepped block with a hole on a 6-cell grid. The three views along the top are drawn by the 192-cell solid on the left and by the 64-cell solid on the right — every filled square in every one of the three views is filled by both. The views bound the solid and do not determine it.front view · 32 filledtop view · 36 filledside view · 36 filledthe largest solid with these views — 192 cellsand a solid with the same views — 64 cells6 × 6 × 6 cellsthe three views are identical; the solids differ by 128 cells
Fig. 9 The reason the drill starts from two views and never from one. A single orthographic view has dropped a whole coordinate; even three of them bound a solid between 192 cells and 64 rather than determining it.

The perspective version of the same question is not the same operation

There is a natural next question — what the equivalent of “look at it square on” is for a photograph — and the answer is instructive because the two operations are not analogues.

In a parallel view the true shape of a plane face is obtained by projecting again, along the normal. In a perspective picture it is obtained by applying a homography to the picture itself: the face is a plane, a photograph of a plane is a projective image of it, and the map back is determined by four correspondences or by the plane’s vanishing line and two more numbers.

The difference is where the information comes from. The auxiliary view needs a second view — the coordinate the first one dropped has to exist somewhere. The rectification needs no second view at all, because a perspective projection did not drop a coordinate cleanly; it folded the missing one into the divide, and the plane’s own vanishing line is enough to unfold it.

So the parallel case and the perspective case answer the same practical question by opposite routes: one adds a picture, the other reads a line off the picture it has. It is one more instance of the trade this site keeps meeting — a parallel projection preserves ratios along a line and destroys the evidence of depth outright, while a perspective one destroys the ratios and keeps a trace of the depth in the convergence.

A façade, flattened out of the photographFour corners of a rectangle of known proportions fix the homography. Three lengths it was never given come back to 4e-16 relative — so every measurement on that plane is available, in units of the rectangle's own width.the picturethe same plane, rectifieddoor — 0.5068 widths (true 0.5068)sill — 0.3026 widths (true 0.3026)diagonal — 1.1766 widths (true 1.1766)worst error 4e-16 relativethe probes were not used to build the map
Fig. 10 The perspective answer to the same question. No second picture: a plane’s vanishing line and four correspondences are enough, because the projection folded the missing coordinate into the divide instead of deleting it.

The fold line is a rotation, and the paper hides it

The drill’s folding line reads as an operation on the sheet, and it is worth one paragraph on what it is in space, because it is the same object the whole essay is about.

Two views are two picture planes, each perpendicular to its own ray direction. Two planes meet in a line. That line — projected into either picture — is the fold, and the reason a coordinate can be “transferred” across it is that the two planes share the direction along it, so a distance measured along that direction means the same thing in both pictures.

Which is why the transfer works in one direction and not the other. Along the fold, the two views agree exactly; perpendicular to it, one view carries a coordinate the other has dropped, and the drill is an accounting of which view still has which.

Seen that way, the sheet full of folding lines is a drawing of a chain of picture planes hinged along their intersections — the parallel-projection version of changing the picture plane while the centre stays put, with the centre at infinity throughout.

What each parallel system does to the three axesThe smallest axis scale is plotted; the note says how many of the three coincide and whether the system is an orthographic projection or an oblique construction. cavalier and isometric both make all three the same — but isometric is the only orthographic one that does, at 0.8165, and the oblique route gets there by drawing depth at true length.elevation0.0000two equal, orthographic ←cabinet0.5000two equal, obliquecavalier1.0000all three equal, obliquedimetric0.4714all three different, orthographicisometric0.8165all three equal, orthographictrimetric0.5479all three different, orthographicsmallest of the three axis scalesmeasured from each projection
Fig. 11 And what each choice of direction costs, across the named systems. Elevation keeps two axes exactly and loses the third; the axonometrics spread the loss over all three; nothing keeps all three, because an orthographic projection has two dimensions to spend.
The same face, square on and notThe area of a face's image is its true area times the cosine of the angle between the ray direction and the face's normal — 0.9848 here, so 1.3232 m² of face draws 1.3031 m² of picture. Only the view along the normal shows the shape; every other view shows a foreshortening that cannot be undone without knowing which one it was.square on · 1.323 m²and not · 1.303 m²the ratio is the cosine, 0.9848one face, two ray directions
Fig. 12 Ten degrees off the normal: the cosine is 0.9848 and the drawn area is 1.3031 m² of a true 1.3232 m². A view that is nearly square on is nearly true, and “nearly” is a number rather than a judgement.

Choosing the direction is the whole method

Stated compactly, everything above is one idea used four times.

A parallel view is chosen by naming a direction, and every property of the resulting picture follows from the angles between that direction and the things being drawn. A line at 90°90° is true; a line at 0° is a point; a face whose normal is at 0° is true; a face whose normal is at θ\theta has its area multiplied by cosθ\cos\theta.

The reason this is worth separating from “descriptive geometry” as a subject is that the subject is usually presented as constructions on a sheet — folding lines, transfer distances, reference planes — and the constructions are the implementation. What is being decided each time is a direction in space, and a reader who holds that in mind can reconstruct any of the drills without remembering which measurement gets transferred from where.

The axis scales a pitch of 35.3° can reachSweeping the yaw at a fixed pitch traces one curve, not a region: the identity leaves only two of the three scales free. At this pitch the curve passes through the point where x and z are equal, which is isometric — 0.816497 against √(2/3) = 0.816497.00.2500.5000.75010.7000.8000.9001scale of the x axisscale of the z axis, at this pitchx = z at 0.8355y is fixed at 0.7771 by the pitch aloneevery point on the curve sums to 2 within 7e-16
Fig. 13 And the identity’s other face: sweeping the direction traces a curve rather than filling a region, because two of the three foreshortenings are free and the third is not. Choosing a direction chooses everything at once.
True length, point view, true shapeThree views of one face, differing only in the direction they are taken along. The first is chosen perpendicular to the marked edge, so that edge is at true length, 1.3928 m. The second is taken along that edge, so the edge is a point and the face is a line. The third is along the face's own normal, and the face is at true shape — 1.3232 m². Nothing is measured off the paper; each is the projection the chosen direction produces.true length1.3928 mpoint viewthe edge is one pointtrue shape1.3232 m²one face, three ray directionseach step is a choice of direction, not a construction on the paper
Fig. 14 The drill again, now as three choices of direction rather than three constructions: across the edge, along the edge, along the normal. Nothing is measured off the paper at any step.
Moving the object, in both familiesThe same box, in place and translated 1.6 m across the world. In the parallel drawing the second image is the first translated by 65.7 px and nothing else — every edge the same length to 3e-14 px. In the perspective drawing the edge lengths change by up to 68.1%, because the direction from the eye has changed and a projection through a centre depends on it.horizonisometric — the same drawing, movedperspective — a different drawingcorrect from 23 cm, at 160 mm wideparallel: 3e-14 px · perspective: 68.1%
Fig. 15 The property that makes the whole method work: a parallel view depends on the direction and on nothing else. Move the object and the drawing is the same drawing translated, so a chosen direction keeps meaning what it meant.

What links here

Computed from the collection, not written here: the essays that point at this one.

Reads more easily once this is understood

Essays that name this one as worth reading first.

Shares its objects with

Essays that name at least two of the same things, and that neither author linked.

Named objects

A flat tag is an object no other essay names yet.

Auxiliary viewDescriptive geometryElevationForeshorteningMultiview drawingOrthographic projectionParallel projectionPoint viewProjection directionTrue length