The eye that moves

A seam breaks direction, not size

An eight-metre road crossing the first join of a three-station landscape is drawn 215.4 px wide under either band's rule, identically, and a six-metre post 161.5 px tall under either — the eye's height cancels out of any size taken at one depth. What does not cancel is where those sizes sit. The road's edges are turned 23.2° from each other and the post's foot lands 64.6 px out of place, and a painter butting two bands can absorb the offset and can never absorb the turn.

Worth reading first: Three distances in one landscape · The point you have to stand at.

The stations are also a staircase ended by noticing that a join stays ambiguous only while nothing crosses it, and that a painter laying mist across a seam is doing what the ambiguity requires. That leaves a question it did not ask: what exactly happens to a thing that does cross.

The answer is sharper than “a discontinuity”. Some of a crossing object’s measurements come through the join completely unchanged, to the last digit, and others do not come through at all — and the split between them is clean enough to state as a rule.

The eye cancels out of a size and not out of a place

A level eye at height HH draws a point at depth dd and world height YY on the row py+f(HY)/dp_y + f(H-Y)/d. Take two points at the same depth — the foot and top of a post, the two edges of a road — and subtract. The HH appears in both rows and cancels: a post of height pp is drawn fp/dfp/d tall and a road of width ww is drawn fw/dfw/d wide, and neither expression contains the eye at all.

So every size measured at one depth survives a change of station exactly, and every position does not.

Every size crosses the join unchanged; a post's foot lands 70.0 px outAt the join at 70 m, measured under both bands' rules: a six-metre post is drawn 60.0 px tall under either, and an eight-metre road 80.0 px wide under either — the eye's height cancels out of any size taken at one depth, because such a size is a difference of two rows and the eye appears in both. What does not cancel is where those rows are: the post's foot sits 70.0 px apart under the two rules, and the road's edges are turned 25.0° from each other. An object spanning a seam is not distorted. It is dislocated — every part of it the right size, in the wrong place.a post's drawn heightunchangeda road's drawn widthunchangedthe post's foot, in rows70.0 pxand the road's edges turn 25.0°measured under both bands' rulessizes survive, positions do not
Fig. 1 Measured under both bands’ rules at the join at 70 m: a six-metre post is drawn 60.0 px tall under either, an eight-metre road 80.0 px wide under either, and the post’s foot lands 70.0 px apart between the two. Sizes cross; places do not.

At the first join a six-metre post is 161.5 px tall under the near band’s rule and 161.5 px under the far band’s. An eight-metre road is 215.4 px wide under either. Those are not agreements to a tolerance; the two expressions are the same expression.

And the post’s foot sits 64.6 px apart under the two rules — which is the riser the staircase reading has to draw, arriving from the other direction. A join does not distort what crosses it. It dislocates it: every part the right size, in the wrong place.

It is worth being exact about how large a class that is, because “every size at one depth” covers most of what a reader of a picture actually measures. The height of a figure, the width of a boat, the span of a bridge, the gap between two posts standing side by side, the diameter of a wheel seen edge-on: all of them are differences of two rows or two columns taken at one depth, and every one of them crosses a join untouched. A reader who checked a crossing object’s proportions for evidence of the seam would find none, however carefully they looked, because there is none to find.

Three bands, three recovered elevations: 1.6, 4.0, 11.0 mThe same three-station landscape [three distances in one landscape] built, with the camera height of each band read back out of nothing but its own ground samples — a linear fit in one over depth, a total-least-squares fit, the same one that puts a horizon through several points. All three come back within 3.6e-15 m of the true elevation, so a reader handed only the marks recovers 1.60 m, 4.00 m, 11.00 m without being told any of them.recovered 1.60 m8–26 mrecovered 4.00 m26–70 mrecovered 11.00 m70–200 melevation recovered from each band's own marksnot read off a ledger
Fig. 2 The three bands’ own rules, each fitted from its own marks. What differs between them is a single number — the slope of the fit — and that number is the one quantity a size at fixed depth does not contain.

The reason is the same one the staircase reading rests on: the eye’s height enters the row of a ground point only through HYH - Y, so any operation that differences two points at one depth removes it. That essay used the fact to show a reader cannot separate the eye from the ground. Here it shows a reader cannot detect the seam from proportions. One algebraic fact, two consequences, and both of them are about what the marks do not contain.

The turn is what nothing absorbs

The dislocation splits again, and this second split is the one that matters to a painter.

Three distances in one landscape established the freedom a painter has at a join: the bands are not projected into one frame but laid out, each butted against the last, so a uniform vertical offset between two bands is free. That is why the measurable cost of a seam was reported as a change of rate rather than as an offset — the offset is absorbed by where the bands are placed on the sheet.

A post’s displaced foot is exactly such an offset, and butting the bands is exactly the operation that nulls it at the join depth. So the 64.6 px is not, on its own, something a reader sees.

An angle is different.

A road crossing the join turns 23.2° and keeps its widthA straight road 8 m wide running in depth through the join at 26 m. Its two edges image on lines through the principal point whose drawn angle is atan(2H/w), so the near band draws them at 21.8° and the far band at 45.0° — a turn of 23.2°. At the join itself the road is drawn 215.4 px wide under either band, identically, because the eye's height cancels out of a size taken at one depth. A painter butting two bands chooses a vertical offset, and an offset moves a line without turning it, so the width is free and the turn is not.the join, 26 mnear band: 21.8°far band: 45.0°215 px wide under either8 m roadturns 23.2°, keeps its width
Fig. 3 A straight road eight metres wide running in depth through the join at 26 m. Its edges are drawn at 21.8° under the near band and 45.0° under the far one — a turn of 23.2° — while at the join itself the road is 215.4 px wide under either.

A road’s edge runs from the principal point outward: both its coordinates fall as 1/d1/d, uu as f(w/2)/df(w/2)/d and vv as fH/dfH/d, so the edge images on a straight line through the principal point whose slope is 2H/w2H/w. The angle it is drawn at is a function of the eye’s height. The near band draws an eight-metre road’s edges at 21.8°, the far band at 45.0°, and the second join turns them again from 45.0° to 70.0°.

A translation moves a line without turning it. So the painter’s offset — the one freedom the layout provides — cannot touch the 23.2°, and a road crossing the first join arrives on the other side visibly bent. Every other continuous thing running in depth does the same: a river, a wall, a line of poplars, the sides of a valley.

The second join turns them further, and by a comparable amount — 45.0° to 70.0°, a turn of 25.0°. So a feature running through the whole picture, which is what a river in a towering-distance landscape is, is bent twice, by 23.2° and then by 25.0°, for a total of 48.2° between the direction it is drawn at nearest the viewer and the direction it is drawn at furthest away. A road entering the picture at 21.8° from the horizontal leaves it at 70.0°.

That is the placement-invariant signal a seam produces, and it is the reason the join has to be empty. Not because a discrepancy would be visible in principle, but because twenty-three degrees is not a discrepancy.

Why a size is not a length

One qualification keeps the rule from being broader than it is, and it is the qualification that makes it a rule rather than a slogan.

A size survives only if it is taken at one depth. A length measured down the picture — the drawn extent of a stretch of road between two marked depths, the run of a river between two bends — is a difference of two rows at two different depths, and the eye’s height does not cancel out of that. It is exactly the quantity the convention exists to change: the far band gets more picture for its depth range precisely because the eye is higher, and that gain is 6.9 times what one camera would have allowed.

So the split is not between sizes and positions in any loose sense. It is between quantities that are differences at fixed depth — which lose the eye — and everything else, which keeps it. A stretch of road from 16 m to 26 m is drawn at one length under the near band’s rule and at quite another under the far band’s, and the ratio is the rate change the seam was reported as costing in the first place.

That is why a reader cannot use a crossing object’s proportions as evidence about the seam and can use its rate of foreshortening. The first is a fixed-depth difference and the second is not.

The worst thing to run across a seam

The kink depends on the crossing object’s width, and not monotonically, which gives a painter something useful.

The kink is worst at 4 m and falls away at both endsThe turn a crossing object's edges take at the first join, against its width. A very narrow thing is drawn steeply under both bands and a very wide one shallowly under both, so the kink is largest in between — 24.8° at 4 m, against 10.2° at 1 m and 2.1° at 128 m. A painter with something that must cross a seam wants it either very narrow or very broad, and the worst possible choice is a thing whose width sits between the two eye heights.0102000.50011.502width of the thing crossing the seam (m, log scale)turn at the join (°)24.8° at 4 mthe first joinworst 24.8°
Fig. 4 The turn a crossing object’s edges take at the first join, against its width. 10.2° for a road a metre wide, 24.8° at four metres, 23.2° at eight, 8.3° at thirty-two and 2.1° at a hundred and twenty-eight.

A very narrow thing is drawn nearly vertically under both bands, because 2H/w2H/w is large for both; a very broad one is drawn nearly horizontally under both, because 2H/w2H/w is small for both. The turn is largest in between — 24.8° at four metres, for eye heights of 1.6 m and 4 m — and falls away at both ends: 10.2° at one metre and 2.1° at a hundred and twenty-eight.

So the worst possible thing to run across a seam is something whose width sits near the two eye heights, which is to say a path, a stream, a track — exactly the features a landscape runs in depth. And the safest are a thread and a plain: a footpath narrow enough to read as a line, or a stretch of open water broad enough that its edges are nearly level anyway.

Whether painters knew that is not a question any measurement here answers. What can be said is that the geometry rewards the two extremes and punishes the middle, and that the middle is where most receding features of a landscape sit.

The turn is the riser, read sideways

The two joins turn a road by 23.2° and 25.0°, and those numbers are not independent of anything already measured.

The step a reader would have to see is 103% of a band, not a detailFor the stepped reading to be the one a reader is looking at, the ground would have to be seen dropping at each join — 2.40 m at 26 m and 7.00 m at 70 m. Drawn, those risers are 64.6 px and 70.0 px, against bands whose whole drawn extent is 96.9 px and 67.7 px — 67% and 103% of the band above each join. The two readings are not separated by a subtlety but by a cliff, and a convention that lays mist across its joins is what keeps that cliff off the page.join at 26 m64.6 pxjoin at 70 m140.0 pxthe riser the stepped reading must drawup to 207% of its band
Fig. 5 The riser the staircase reading needs at each join — 64.6 px and 70.0 px. The same two numbers are the displacement of a crossing post’s foot, and the turn in a crossing road is what that displacement does to a line rather than to a point.

A post’s foot is displaced 64.6 px at the first join and 70.0 px at the second, and those are the riser heights the staircase reading has to draw. A road’s edge is a line through the principal point, and displacing every one of its points by the amount a post’s foot is displaced is exactly what turns it: the displacement is vertical and proportional to 1/d1/d, which is the same 1/d1/d the edge’s own coordinates fall as, so the displaced line is another line through the principal point at a different angle.

So the three quantities reported about this join — the apparent ground drop in metres, the riser in pixels, and the turn in degrees — are one quantity in three currencies. A landscape that changes its rule halfway up reported it in metres of depicted ground; the staircase reading in pixels of a cliff face; here in degrees of a bent road. The reason to have all three is that only the last one is invariant under what a painter is free to do, and only the first is stated in the world rather than on the page.

How much room a painter actually has

A join is one depth. An object blocks it only by spanning it, so an object of depth-extent ee rules out an interval of candidate join depths ee long, and the question of how constrained a painter is becomes arithmetic.

Scatter through the landscape’s own depth range — 8 m to 200 m — six features with depth-extents of 3, 3, 6, 6, 12 and 20 metres, which is a thinly populated scene rather than a crowded one, and 44.1 m of the 192 m range is blocked. Seventy-seven per cent of depths remain available, which is a good deal of room.

That is worth stating because the constraint is easy to overstate once its cost in degrees is known. A seam must fall where nothing crosses, and in an ordinary landscape most depths qualify. The constraint bites not on whether a join can be placed but on where — and it explains a practice rather than forbidding one.

There is a second reading of that figure worth taking. The blocked intervals are where a join cannot go, and they are set by the depth-extent of the features rather than by how many there are — six features of three metres block eighteen metres of range and one feature of eighteen blocks the same. So a landscape with a few large receding things in it is more constrained than one with many small ones, even though the second looks busier. A valley with one long river running its length is nearly unjoinable; a plain scattered with copses is almost entirely free.

That inverts the intuition a crowded picture suggests, and it is a consequence of the join being a depth rather than a region. Nothing is blocked by being near the join; only by straddling it.

It also explains the mist directly. A painter who wants a join at a particular depth, for reasons about the picture rather than about the scene, can always make that depth empty by putting something in front of it. Mist, cloud and a bank of trees do not hide a discontinuity; they remove the objects that would have crossed it, which is a different operation and a complete one.

The difference matters for how the convention should be described. Hiding a discontinuity is a patch over a defect, and a reader who found the patch would have found the defect. Removing the crossing objects leaves a picture with no defect in it anywhere: every band is an exact projection, every size crosses correctly, and there is nothing at the join to be inconsistent because there is nothing at the join. It is the same move a divergent picture’s surfaces make when they are drawn square to one another — not a flaw concealed but a case avoided.

What this does not settle

It does not measure any painting. The landscape here is constructed from three stated cameras, and nothing about where any real painter put a seam is claimed or checked. The three stations are the ones this field has used throughout, chosen to make the arithmetic legible rather than to match a practice, and a convention worked at other heights would turn a road by other angles — larger ones, since the turn grows with the difference between the stations.

It does not say the turn is the only signal. It is the only one a vertical offset cannot absorb, which is a narrower claim. A painter has one freedom at each join and the turn survives it; whether some other freedom a painter might take — scaling a band, or shearing it — would absorb the turn as well is a question about a layout nobody here has drawn.

It does not price the horizontal. Everything above concerns objects running in depth. A thing lying across the picture rather than into it spans one depth, so it has no join to cross, and the whole question is about receding features.

It does not distinguish the two readings of the landscape. A crossing object’s turn is a property of the marks, so it is the same turn under the several-station reading and the staircase one. Under the staircase reading the road is not bent by a change of rule at all — it genuinely runs up a bank and its direction genuinely changes, which is what a road climbing a terrace does. The two accounts agree about the 23.2° and disagree about what it means, which is the shape the staircase reading is entirely about.

It does not settle what a viewer notices. Twenty-three degrees is large as a geometric quantity; whether a reader of a painting registers it as wrong, or reads it as a bend in the road, is about seeing rather than about projection, and nothing here bears on it. The claim is that the turn is present and that no placement removes it.

It does not model an object that is not straight. A road is taken as a straight run in depth, so its edges are straight lines through the principal point and a turn is a well-defined angle. A winding river has a drawn direction that changes anyway, and separating the turn a seam adds from the turn the river already has is a different measurement — and probably an easier one to hide a seam inside, which is worth someone’s attention.

And the free-depth share is a property of a scene rather than a result. Seventy-seven per cent is what six stated features leave; a crowded valley would leave less and an empty plain more. The number is here to say that the constraint has a size, not to say what the size is in general.

Still open: what a seam does to a shadow

One kind of receding feature has not been asked, and it is the one whose geometry is already a projection of its own.

A shadow cast across the ground by a low sun runs in depth, so it crosses joins like a road — but a shadow’s direction on the page is set by the sun’s own vanishing point, not by the object that casts it, and that vanishing point is a property of the camera drawing it. Two bands drawn from two stations share a horizon, so they share the row a sun’s vanishing point sits on; whether they share the point is a different question, and it decides whether the shadows of two objects in different bands converge on one place or on two.

The measurement that settles it places a single sun over a several-station landscape, draws each band’s shadows by that band’s own camera, and asks whether a reader fitting a common light to the whole picture finds one — and if not, how far apart the two lights sit, in the same currency the station disagreement was reported in. A picture whose shadows point at two suns is a much louder failure than a road that bends, and it would put a second constraint on where a join can go.

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.

Depth compressionElevationFree parameterMoving viewpointPiecewise mapSeamStation-disagreementStation point