The Law of Reflection

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reflection angle of incidence angle of reflection normal specular

Core Idea

When a wave strikes a surface, the angle of reflection equals the angle of incidence, both measured from the normal (the line perpendicular to the surface at the point of contact). This law holds for all wave types — water waves, sound, and light. Specular reflection (smooth surface) produces clear images; diffuse reflection (rough surface) scatters light in many directions, making objects visible but not mirror-like.

How It's Best Learned

Shine a laser at a mirror and measure incident and reflected angles with a protractor. Then compare reflection from a mirror vs. from matte paper to distinguish specular and diffuse reflection.

Common Misconceptions

Explainer

You've already worked with angles — measuring them, classifying them as acute, right, and obtuse. The law of reflection applies this geometric machinery to a specific physical situation: what happens when a wave hits a surface. The rule is simple: the angle of incidence equals the angle of reflection, with both angles measured from the normal — the imaginary line perpendicular to the surface at the point of contact.

The normal is the essential reference line, and it is where most errors happen. A ray arriving at 30° from the surface has an angle of incidence of 60° (measured from the normal, not the surface — these are complementary). It reflects at 60° on the other side of the normal, leaving at 30° from the surface. Students who measure from the surface get the complement, and their calculations fall apart. The correct habit is always: draw the normal first, then measure from it.

Specular reflection occurs from smooth, mirror-like surfaces. When a surface is smooth at the scale of the wave's wavelength, all the surface normals point in the same direction. Parallel incoming rays reflect as parallel outgoing rays — you get a clear, geometrically precise image. Diffuse reflection occurs from rough surfaces like paper, walls, or skin. Microscopically, the surface normals point in countless different directions. At each tiny point, the law of reflection holds perfectly — the angle of incidence equals the angle of reflection at that microscopic facet. But because neighboring facets face different directions, parallel incoming rays scatter outward in all directions. This is why matte objects are visible from any angle (they scatter light toward your eye from many directions) but don't form images.

The law holds for all wave types — water waves, sound, and light — because it follows from the general physics of wave reflection at boundaries, not from anything special about light. If you've ever heard your voice echo off a wall or seen ripples bounce off the edge of a tub, you've observed the same law at work. The universality is part of what makes this such a fundamental result.

Practice Questions 5 questions

Prerequisite Chain

Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsCenter of MassConservation of Linear MomentumElastic CollisionsInelastic CollisionsCoefficient of RestitutionCollision Analysis and Real-World ApplicationsTwo-Body Collisions in the Center-of-Mass FrameReduced Mass and Two-Body ProblemsKinematics in Two DimensionsProjectile MotionCircular Motion: KinematicsSimple Harmonic MotionWave Motion: Definition and ClassificationTransverse Wave Characteristics and PropertiesWave Properties: Wavelength, Frequency, and AmplitudeThe Law of Reflection

Longest path: 91 steps · 429 total prerequisite topics

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