This page is the "no surprise left behind" companion to the parent derivation . The rule is always the same one line:
Before we compute anything, three plain-word reminders so no symbol sneaks in undefined:
Definition The three symbols we will lean on
n = refractive index of a medium: a pure number saying "how much light is slowed here." Bigger n = light travels slower. See Refractive Index .
c = speed of light in empty vacuum (a fixed universal constant, about 3 × 1 0 8 m/s ).
v = speed of light inside a medium . They are tied together by v = c / n : a bigger n makes v smaller, i.e. light crawls in dense stuff.
"Optically dense" means larger n (light slow); "optically rare" means smaller n (light fast). "Denser" here is about index , not weight — so glass (n = 1.5 ) is optically denser than water (n = 1.33 ).
Now let us map out every kind of situation this single equation can hand you. If a case is not in the table below, it does not exist for Snell's law.
Every refraction problem is one (or a blend) of these cells. The last column names the example that nails it.
#
Case class
What is special
Example
A
Rare → dense (n 1 < n 2 )
ray bends toward normal, θ 2 < θ 1
Ex 1
B
Dense → rare (n 1 > n 2 )
ray bends away from normal, θ 2 > θ 1
Ex 2
C
Normal incidence (θ 1 = 0 )
degenerate: ray goes straight, no bend
Ex 3
D
Grazing incidence (θ 1 → 9 0 ∘ )
limiting: biggest possible bend into a denser medium
Ex 4
E
Critical angle (θ 2 = 9 0 ∘ )
boundary of existence; beyond it → no refraction
Ex 5
F
Beyond critical (sin θ 2 > 1 )
total internal reflection, "no answer" is the answer
Ex 6
G
Same index (n 1 = n 2 )
degenerate: no boundary optically, θ 2 = θ 1
Ex 7
H
Given speeds not indices
rewrite Snell with v ; a translation twist
Ex 8
I
Real-world word problem
pool/coin apparent-depth style geometry
Ex 9
J
Exam twist: angle from surface
trap — convert 9 0 ∘ − ϕ first
Ex 10
Intuition The whole family lives on one dial — read the figure
Fix n 1 , n 2 and turn θ 1 from 0 ∘ up to 9 0 ∘ . Watch what sin θ 2 = n 2 n 1 sin θ 1 does. The figure below plots exactly this. The teal curve is rare→dense (n 1 = 1 , n 2 = 1.5 ): it stays comfortably below the dashed plum line at height 1 , so a refracted ray always exists — but it can never climb past sin θ 2 = 0.667 (the teal dot at θ 1 = 9 0 ∘ ). The orange curve is dense→rare (n 1 = 1.5 , n 2 = 1 ): it does reach the plum line, and the orange dot marks the exact incidence — the critical angle 41. 8 ∘ — where sin θ 2 = 1 . To the right of that dot the orange curve would need sin θ 2 > 1 , which is impossible: that is total internal reflection.
Worked example Air into water
Light in air (n 1 = 1.00 ) strikes water (n 2 = 1.33 ) at θ 1 = 4 5 ∘ . Find θ 2 .
Forecast: water is optically denser (bigger n ), so guess θ 2 smaller than 4 5 ∘ — the ray tucks toward the normal.
Write Snell: n 1 sin θ 1 = n 2 sin θ 2 .
Why this step? It is the only relation linking the two angles.
Solve for the unknown sine: sin θ 2 = n 2 n 1 sin θ 1 = 1.33 1.00 × sin 4 5 ∘ = 1.33 0.7071 = 0.5317 .
Why this step? We isolate sin θ 2 because θ 2 is what we want.
Undo the sine: θ 2 = arcsin ( 0.5317 ) = 32. 1 ∘ .
Why this step? arcsin answers "which angle has this sine?" — it undoes sin .
Verify: 32. 1 ∘ < 4 5 ∘ ✔ (bent toward normal, matching forecast). Cross-check the product: 1.33 × sin 32. 1 ∘ = 1.33 × 0.5317 = 0.707 = 1.00 × sin 4 5 ∘ ✔.
Worked example Water into air
The same water (n 1 = 1.33 ) to air (n 2 = 1.00 ), now θ 1 = 3 0 ∘ . Find θ 2 .
Forecast: leaving an optically dense medium into a rarer one (smaller n ) — ray should bend away from normal, so θ 2 > 3 0 ∘ .
Snell: 1.33 sin 3 0 ∘ = 1.00 sin θ 2 .
Why this step? Same master equation, indices just swapped roles.
sin θ 2 = 1.33 × 0.5 = 0.665 .
Why this step? Multiply because n 2 = 1 leaves sin θ 2 alone on the right.
θ 2 = arcsin ( 0.665 ) = 41. 7 ∘ .
Why this step? Invert the sine to recover the angle.
Verify: 41. 7 ∘ > 3 0 ∘ ✔. Note 0.665 < 1 , so a real refracted ray still exists — we have not hit the critical angle yet (that comes in Ex 5).
Worked example Straight-in beam
A laser enters glass (n 2 = 1.5 ) from air (n 1 = 1.0 ) exactly along the normal, θ 1 = 0 ∘ .
Forecast: shining straight in — there is no "sideways" to bend toward, so guess θ 2 = 0 ∘ , no bend.
Snell: 1.0 sin 0 ∘ = 1.5 sin θ 2 .
Why this step? Plug the degenerate input in rather than assume the answer.
sin 0 ∘ = 0 , so 0 = 1.5 sin θ 2 ⇒ sin θ 2 = 0 .
Why this step? A zero on the left forces the right side to zero.
θ 2 = arcsin ( 0 ) = 0 ∘ .
Why this step? The only angle in [ 0 , 9 0 ∘ ] with sine 0 is 0 ∘ .
Verify: The ray passes straight through undeviated — this is why looking straight down into water does not shift what you see. The speed inside the glass still drops (recall v = c / n from the definitions above: bigger n ⇒ smaller v ), but the direction does not. ✔
Worked example Skimming the surface into glass
Light in air (n 1 = 1.0 ) grazes glass (n 2 = 1.5 ) at θ 1 = 89. 9 ∘ (almost along the surface). Find θ 2 , and the largest θ 2 ever possible entering this glass.
Forecast: the most extreme sideways entry. There must be a maximum θ 2 it can reach — guess it is set by θ 1 = 9 0 ∘ .
sin θ 2 = 1.5 1.0 sin 89. 9 ∘ = 1.5 0.99999 = 0.66666 .
Why this step? We push θ 1 to its physical ceiling to find the ceiling on θ 2 .
θ 2 = arcsin ( 0.66666 ) = 41. 8 ∘ .
Why this step? Invert to get the actual refracted angle.
The absolute max as θ 1 → 9 0 ∘ : sin θ 2 m a x = n 2 n 1 = 1.5 1 = 0.6667 ⇒ θ 2 m a x = 41. 8 ∘ .
Why this step? sin 9 0 ∘ = 1 is the biggest the numerator can be, so this is the largest refracted angle glass will ever show from air.
Verify: This is exactly the teal dot in the s01 figure: the teal curve's ceiling is sin θ 2 = 0.667 , i.e. 41. 8 ∘ . Every ray from air enters this glass within a cone of half-angle 41. 8 ∘ . Notice this number equals the critical angle of Ex 5 — refraction and total internal reflection are mirror images of the same equation. ✔
Worked example Just barely escaping
Light travels from glass (n 1 = 1.5 ) toward air (n 2 = 1.0 ). For which θ 1 = θ c does the refracted ray skim the surface, θ 2 = 9 0 ∘ ?
Forecast: dense→rare bends away , so at some incidence the ray will lie flat along the surface. Guess θ c is a bit above 4 0 ∘ .
Set θ 2 = 9 0 ∘ : 1.5 sin θ c = 1.0 sin 9 0 ∘ = 1.0 .
Why this step? θ 2 = 9 0 ∘ is the last moment a refracted ray exists — the definition of critical.
sin θ c = n 1 n 2 = 1.5 1.0 = 0.6667 .
Why this step? Solve for the incidence sine; note it equals the ratio of indices , rare over dense.
θ c = arcsin ( 0.6667 ) = 41. 8 ∘ .
Why this step? Invert the sine.
Verify: Same 41. 8 ∘ as Ex 4 — the entry cone and the escape cone match, as they must. The figure below draws this exact geometry: the plum incident ray rises through the teal glass, and the orange refracted ray lies flat along the boundary at θ 2 = 9 0 ∘ , with the little plum arc marking θ c = 41. 8 ∘ from the dotted normal. See Critical Angle and Total Internal Reflection . ✔
Worked example Trying to refract past the limit
Same glass→air (n 1 = 1.5 , n 2 = 1.0 ), but now θ 1 = 5 0 ∘ , which is bigger than θ c = 41. 8 ∘ . Find θ 2 .
Forecast: we are past the critical angle — guess there is no refracted ray at all.
sin θ 2 = 1.0 1.5 sin 5 0 ∘ = 1.5 × 0.766 = 1.149 .
Why this step? Blindly apply Snell and watch what happens to the number.
sin θ 2 = 1.149 > 1 .
Why this step? A sine can never exceed 1 — this signals no real angle solves the equation.
Therefore no refracted ray exists : all the light reflects back into the glass — total internal reflection .
Why this step? The impossible sine is the mathematics telling us the light cannot leave.
Verify: arcsin ( 1.149 ) is undefined for real angles ✔. On the s01 figure this is where the orange curve has already passed its intersection with the plum line — it would need to go above height 1 . This is precisely why optical fibres trap light: rays inside strike the wall past θ c every time. ✔
Worked example Glass on identical glass
Two blocks of the same glass (n 1 = n 2 = 1.5 ) are pressed together with no gap. Light hits the join at θ 1 = 6 0 ∘ . Find θ 2 .
Forecast: if the media are identical, there is no real interface for light — guess θ 2 = 6 0 ∘ , straight through.
Snell: 1.5 sin 6 0 ∘ = 1.5 sin θ 2 .
Why this step? Test the degenerate equal-index case directly.
Cancel the common 1.5 : sin θ 2 = sin 6 0 ∘ .
Why this step? Dividing both sides by the shared index isolates the sines.
θ 2 = 6 0 ∘ .
Why this step? Equal sines (both in [ 0 , 9 0 ∘ ] ) mean equal angles.
Verify: No bending — consistent with "no optical boundary." This is why an object dropped in liquid of matching index seems to vanish: no refraction, no visible edge. ✔
Worked example Snell in disguise
Medium 1 lets light travel at v 1 = 2.0 × 1 0 8 m/s ; medium 2 at v 2 = 1.5 × 1 0 8 m/s . A ray hits the boundary at θ 1 = 4 0 ∘ . Find θ 2 . (Here v is the speed of light inside each medium , from the definitions above.)
Forecast: v 2 < v 1 means light is slower in medium 2, i.e. it is optically denser (n = c / v larger), so guess θ 2 < 4 0 ∘ .
Rewrite Snell with speeds. Since n = c / v (with c the vacuum speed, a shared constant): v 1 c sin θ 1 = v 2 c sin θ 2 ; cancel c to get v 1 sin θ 1 = v 2 sin θ 2 .
Why this step? The problem hands speeds, not indices — translate first, and c cancels because it is the same on both sides.
Solve: sin θ 2 = sin θ 1 ⋅ v 1 v 2 = sin 4 0 ∘ × 2.0 1.5 = 0.6428 × 0.75 = 0.4821 .
Why this step? Isolate the unknown sine using the speed form.
θ 2 = arcsin ( 0.4821 ) = 28. 8 ∘ .
Why this step? Invert the sine.
Verify: 28. 8 ∘ < 4 0 ∘ ✔ — slower medium, bends toward normal, matching the forecast. See Refractive Index . ✔
Worked example The coin at the bottom of the pool
A coin sits at true depth h = 1.20 m under water (n 1 = 1.33 , water below; air n 2 = 1.00 above). Looking almost straight down, how deep does it appear ?
Forecast: water bends the escaping rays away from the normal, fooling your eye into thinking the coin is shallower — guess h app < 1.20 m .
Look at the figure first. A ray leaves the coin C , travels up through the water a horizontal step s to the surface point P , then refracts into air. Your eye extends the air ray backward (dashed) to where it seems to come from — a point directly above the coin but at the shallower apparent depth h app . Both the true ray (from depth h ) and the apparent ray (from depth h app ) share the same horizontal step s at P , so their tangents are what we compare.
At P , the water-side angle from the normal is θ 1 with tan θ 1 = s / h ; the air-side angle is θ 2 with tan θ 2 = s / h app .
Why this step? Both right triangles share the horizontal s ; the tangent (opposite s over adjacent depth) links each angle to its depth.
For near-vertical viewing both angles are tiny, and for small angles sin θ ≈ tan θ . Snell n 1 sin θ 1 = n 2 sin θ 2 becomes n 1 tan θ 1 ≈ n 2 tan θ 2 .
Why this step? Replacing sin by tan (valid only for small angles) lets us feed in the depth expressions.
Substitute the tangents: n 1 h s = n 2 h app s . The s cancels, leaving h n 1 = h app n 2 , so h app = h ⋅ n 1 n 2 = 1.20 × 1.33 1.00 .
Why this step? The shared s cancels, and rearranging isolates the apparent depth.
h app = 1.20 × 0.7519 = 0.902 m .
Why this step? Plug the numbers.
Verify: 0.902 m < 1.20 m ✔ — the coin looks about 0.30 m shallower, exactly the everyday illusion. Units: metres × (dimensionless ratio) = metres ✔.
Worked example The classic trap
A ray in air (n 1 = 1.0 ) makes an angle of ϕ = 2 5 ∘ with the water surface (not the normal). Water has n 2 = 1.33 . Find the refraction angle θ 2 (from the normal, as usual).
Forecast: 2 5 ∘ from the surface is a shallow, grazing ray — its angle from the normal is large. Guess θ 1 near 6 5 ∘ .
Convert to the normal: θ 1 = 9 0 ∘ − ϕ = 9 0 ∘ − 2 5 ∘ = 6 5 ∘ .
Why this step? Snell's law is defined from the normal; the surface angle and normal angle are complements.
Snell: sin θ 2 = n 2 n 1 sin θ 1 = 1.33 1.0 sin 6 5 ∘ = 1.33 0.9063 = 0.6814 .
Why this step? Now the standard equation applies with the correct incidence angle.
θ 2 = arcsin ( 0.6814 ) = 42. 9 ∘ .
Why this step? Invert the sine.
Verify: If you had forgotten to convert and plugged 2 5 ∘ , you would get sin θ 2 = sin 2 5 ∘ /1.33 = 0.318 , i.e. 18. 5 ∘ — a wrong, much smaller answer. The complement step is what saves you. See the parent note "angle from surface" mistake. ✔
Recall One-line summary of the matrix
Turn the incidence dial from 0 ∘ to 9 0 ∘ : normal incidence ⇒ no bend; rare→dense always refracts (bends toward normal, cone capped at θ 2 m a x ); dense→rare bends away until the critical angle, past which it is total internal reflection; equal indices ⇒ no bend; and always convert surface-angles to normal-angles first.
Which cell has "no real answer," and why? Cell F (beyond critical): sin θ 2 > 1 is impossible, so the light totally internally reflects.
For dense→rare, what marks the last refracting angle? The critical angle θ c = arcsin ( n 2 / n 1 ) , where θ 2 = 9 0 ∘ .
Why does normal incidence give no bending? sin 0 ∘ = 0 forces sin θ 2 = 0 , so θ 2 = 0 ∘ .