Visual walkthrough — Trigonometric ratios in right triangle — sin, cos, tan, cosec, sec, cot
This is the picture-first companion to Trigonometric ratios in right triangle — sin, cos, tan, cosec, sec, cot.
Step 1 — Draw a corner and a slanted line
WHAT. Start with two lines meeting at a single point. One line is flat (call it the ground). The other tips upward from the same point at some tilt. Mark the tilt with a small arc and give it a name: θ (the Greek letter theta, just a label for "the angle").
WHY. Everything in trigonometry is a question about how tilted something is. Before we can measure the tilt with numbers, we need one clean angle to point at. A single corner with one arc is the smallest possible picture of "an angle."
PICTURE. In the figure, the horizontal ink line is the ground, the orange line is the tilt, and the little arc between them is θ. Nothing else exists yet — no triangle, no lengths.

Step 2 — Drop a wall to close the triangle
WHAT. Walk a little way out along the slanted orange line and stop at a point — call it . From , drop a perfectly vertical line straight down until it hits the ground. That vertical line is the wall. The corner where the wall meets the ground is a right angle — a perfect 90° square corner.
WHY. A single angle floating in space cannot be measured with a ruler. But the moment we drop that vertical wall, three sides appear and we have a triangle — and not just any triangle, one with a guaranteed square corner. That square corner is the anchor that makes every ratio below behave predictably (it is what Pythagoras theorem needs).
PICTURE. Look at the small square symbol at the bottom-right corner — that is the mark for "exactly 90°." The three sides are now:
- the ground (bottom, from the corner to the foot of the wall),
- the wall (the vertical teal line up to ),
- the slope (the orange line from the corner up to ).

Step 3 — Name the three sides relative to θ
WHAT. Give each side a role-name, but read the names from θ's point of view:
- Hypotenuse : the slope — the side facing away from the right angle. Always the longest.
- Opposite : the wall — the side sitting across the room from θ (θ cannot touch it).
- Adjacent : the ground — the side θ leans on (it forms one arm of the angle, and it is not the hypotenuse).
WHY. These are not fixed labels stuck to fixed sides. They are jobs relative to θ. If we had chosen the angle at instead, the wall and ground would swap the "opposite/adjacent" jobs. Naming by role — not by position — is exactly what lets one set of formulas work for every angle.
PICTURE. The three sides are colour-coded and labelled with , , . Follow the dashed arrow from θ: it points across the triangle to the opposite side, and along the triangle to the adjacent side.

Step 4 — Grow the triangle and watch the lengths change but ratios stay fixed
WHAT. Keep the tilt θ exactly the same, but slide further out along the slope. Every side gets longer. Now put a smaller copy next to it (slide closer). We get a family of nested triangles, all with the same angle θ.
WHY. Here is the deep move. The raw side lengths are useless as a description of the angle — they change the instant you resize the triangle. But their ratios do not. If the big triangle is a -times scaled copy of the small one, then
- = length of the opposite side (small triangle),
- = length of the hypotenuse (small triangle),
- = the scale factor (how many times bigger the second triangle is),
- = the stretched sides of the big triangle,
- the 's cancel top and bottom — that is the whole point.
This is exactly the Similar triangles fact: same angles ⇒ proportional sides ⇒ equal ratios. So a ratio of two sides is a number that belongs to the angle, not the triangle.
PICTURE. Three nested triangles share the corner and the angle θ. Their walls have different heights, but the ratio (wall ÷ slope) is written next to each — the same value every time.

Step 5 — Freeze the three primary ratios: sin, cos, tan
WHAT. There are exactly three ways to pick two of our three sides and put one over the other (in the "natural" order). We give each a name:
Term by term:
- — how tall is the wall compared to the slope. Big when the triangle is steep.
- — how far out the ground reaches compared to the slope. Big when the triangle is flat.
- — wall against ground: the steepness / slope of the orange line.
WHY these three? They are the three independent comparisons available. The mnemonic SOH-CAH-TOA is just this figure compressed into letters: Sine=Opp/Hyp, Cos=Adj/Hyp, Tan=Opp/Adj.
PICTURE. The triangle is shown three times, each highlighting the two sides that go into one ratio (numerator glowing on top, denominator underneath), with the value bar drawn beside it.

Step 6 — Flip them over to get cosec, sec, cot
WHAT. Take each ratio and turn it upside down. Flipping a fraction just swaps numerator and denominator, and we name the three flips:
- (cosecant) = — the flip of sine.
- (secant) = — the flip of cosine.
- (cotangent) = — the flip of tangent.
WHY. Nothing new is created — these are the same three side-pairs read the other way round. They exist because, in the pre-calculator era, having the flipped version already tabulated saved a division. Notice the pairing rule: the "co" in cosecant partners with sine (no "co"), and secant partners with cosine — the names deliberately cross.
PICTURE. Each primary ratio's fraction bar is shown, then a curved arrow flips it, revealing its reciprocal partner. Same two sides, swapped positions.

Step 7 — The two edge cases: what happens at and
WHAT. Squeeze θ down toward , then swing it up toward , and watch the sides.
θ → 0° (triangle collapses flat). The wall shrinks to nothing: , while the slope and ground become the same length: . And the flip — division by zero, undefined. The wall has no height to compare against.
θ → 90° (triangle stands straight up). Now the ground shrinks: , and the wall equals the slope: . blows up because a vertical line has no horizontal run — its steepness is "infinite."
WHY show this. These are the boundary posts. Any confusion later ("why is undefined?") is answered right here by watching a side become zero and land in a denominator. Nothing between and can surprise you once you've seen both ends.
PICTURE. Two collapsing triangles side by side: the left one flattening (wall → 0), the right one standing up (ground → 0), each labelled with the ratio that becomes 0, 1, or undefined.

Recall Why is
undefined? Because and the opposite side has shrunk to ::: we would be dividing by zero, which has no meaning.
Step 8 — A worked triangle, drawn to scale
WHAT. Take the classic 3-4-5 triangle: opposite , adjacent . Find the hypotenuse with Pythagoras theorem, then read off all six ratios.
- , — the squares built on each leg,
- their sum is the square on the hypotenuse,
- recovers the length.
Now the six:
WHY. Concrete numbers pin the abstract picture down. And there is a free consistency check hidden inside (foreshadowing Trigonometric identities): This is just Pythagoras theorem divided through by — the triangle checking its own arithmetic.
PICTURE. The 3-4-5 triangle drawn true-to-scale on the grid, sides labelled 3, 4, 5, with all six ratio values listed beside their matching side-pairs.

The one-picture summary
Everything above lives in one master diagram: one right triangle, its three sides (, , ) each labelled, and around it the six ratios each shown as "this side over that side." The vertical-vs-horizontal reading of / hints at where this all leads next — see Unit circle definition of trig functions and Components of vectors.

Recall Feynman retelling — the whole walkthrough in plain words
I drew a flat line and tipped a second line off it; the gap between them is my angle θ. To measure that tilt I dropped a straight-down wall from a point on the tilted line, making a triangle with a perfect square corner. I named the sides by how they relate to θ: the long slanted one is the hypotenuse, the wall across from θ is the opposite, the ground θ rests on is the adjacent. Then I noticed something magical — if I make the triangle bigger or smaller but keep the same tilt, the actual lengths change, yet the ratio of any two sides stays frozen, because both sides scale by the same amount and the scale cancels. So a ratio of sides is really a fingerprint of the angle itself. There are three natural ratios: wall-over-slope is sine, ground-over-slope is cosine, wall-over-ground is tangent (the steepness). Flip each upside down and you get cosec, sec, cot — same sides, read backwards. I checked the extremes: flatten the triangle and the wall vanishes so sine hits 0 and cosine hits 1; stand it straight up and the ground vanishes so cosine hits 0, sine hits 1, and tangent blows up. Finally I tested a real 3-4-5 triangle: Pythagoras gave the hypotenuse 5, all six ratios fell out as clean fractions, and came back to exactly 1 — the triangle checking its own homework.
Recall Quick self-test
Which side is "opposite" for angle θ? ::: The one θ cannot touch — it faces θ across the triangle (the wall). Why do trig ratios ignore triangle size? ::: Scaling multiplies both sides by the same factor , which cancels in the ratio. What is and why? ::: Undefined — the adjacent side is 0, so divides by zero.