Mathematics Formulas
Number Systems
Number Theory
Number Set Hierarchy
Natural Numbers
Counting numbers
Whole Numbers
Natural numbers + zero
Integers
Positive and negative whole numbers
Rational Numbers
Can be expressed as a fraction
Operations
BODMAS
Order of operations (Order = powers & roots)
Indices / Exponents
Multiplying
Dividing
Power of a power
Power of a product
Power of a fraction
Negative index
Fractional index
Zero index
Any non-zero number to the power 0 is 1
Index of one
Algebra
Expanding
Distributive Law
Double Brackets
FOIL method
Factorisation
Common Factor (HCF)
Take out the common factor
Difference of Two Squares
Perfect Square (+)
Perfect Square (-)
Grouping
Simultaneous Equations
Elimination Method
Make coefficients equal, then add or subtract. Same sign → subtract. Different sign → add.
Quadratics
General Quadratic
Quadratic Formula
Completing the Square
Vertex at (-h, k). Axis of symmetry: x = -h
Finding h
From ax² + bx + c
Finding k
k is the min/max value of the function
Finding k (alternative)
Equivalent formula for k
Discriminant
D > 0: two roots. D = 0: one root. D < 0: no real roots.
Axis of Symmetry
Or x = -h from completed square form
Variation
Direct Variation
k is the constant of variation
Inverse Variation
As x increases, y decreases
Properties of Operations
Commutative (Addition)
Order does not matter
Commutative (Multiplication)
Order does not matter
Associative (Addition)
Grouping does not matter
Associative (Multiplication)
Grouping does not matter
Additive Identity
0 is the identity for addition
Multiplicative Identity
1 is the identity for multiplication
Additive Inverse
Multiplicative Inverse
Scientific Notation
Standard Form
Large: n positive. Small: n negative.
Large Number Example
Move decimal left → positive power
Small Number Example
Move decimal right → negative power
Relations, Functions & Graphs
Quadratics
Difference of Two Squares
General Quadratic
Quadratic Formula
Discriminant
D > 0: two real roots, D = 0: one root, D < 0: no real roots
Functions
Function Notation
f(x) means "the value of f at x"
Inverse Function
Swap x and y, then solve for y. f(f⁻¹(x)) = x
Composite Function
Apply g first, then f. Note: fg ≠ gf in general.
Quadratic Graphs
Completed Square Form
Turning point at (−h, k)
Axis of Symmetry
Vertical line through the turning point
Consumer Arithmetic
Profit, Loss & Discount
Discount
Profit
When Selling Price > Cost Price
Loss
When Selling Price < Cost Price
Percentage Profit
Percentage Loss
Simple Interest
Simple Interest
P = Principal, R = Rate (%), T = Time (years)
Amount (SI)
Find Principal
Find Rate
Find Time
Compound Interest
Compound Interest
P = Principal, R = Rate (%), n = years
Depreciation
Use negative sign for depreciation
Taxes & Charges
Sales Tax
Total = Price + Tax
Hire Purchase
Extra paid = HP Price − Cash Price
Currency Conversion
Or Local = Foreign ÷ Rate
Markup
Same as profit. Often expressed as % of cost price.
Measurement
Plane Shapes
Perimeter
Area of Triangle
Area (base x height)
b = base, h = perpendicular height
Area (two sides + angle)
When you know two sides and the included angle
Heron's Formula
where s = (a+b+c)/2 (semi-perimeter)
Common Plane Shapes
Area of Parallelogram
Area of Square
Area of Rectangle
Area of Trapezium
Half the sum of parallel sides times height
Area of Circle
Circumference
Area of Sector
Fraction of the circle area
Arc Length
Fraction of the circumference
Solids & Prisms
Volume of Prism
Cross-sectional area times length
Volume of Cuboid
length times width times height
Volume of Cylinder
Volume of Sphere
Volume of Cone
Surface Area
SA of Cuboid
SA of Cylinder
SA of Sphere
SA of Cone
s = slant height
Speed, Distance & Time
Speed
Speed = Distance ÷ Time
Distance
Time
Average Speed
NOT the average of two speeds
D-T Graph: Gradient = Speed
Steeper line = faster speed. Flat line = stationary. Downward = returning.
S-T Graph: Gradient = Acceleration
Steeper = accelerating faster. Flat = constant speed. Downward = decelerating.
S-T Graph: Area = Distance
Use area of trapezium/triangle/rectangle to calculate
D-T Graph Shapes
Line going UP = moving away. FLAT line = stationary. Line going DOWN = returning.
S-T Graph Shapes
Line going UP = accelerating. FLAT line = constant speed. Line going DOWN = decelerating.
Geometry
Basic Angle Facts
Angles on a Straight Line
Supplementary angles
Angles at a Point
Full rotation
Vertically Opposite Angles
Formed by two intersecting lines
Complementary Angles
Two angles that add to 90°
Supplementary Angles
Two angles that add to 180°
Triangles
Angle Sum of Triangle
Interior angles of any triangle
Exterior Angle Theorem
Exterior angle = sum of two interior opposite angles
Isosceles Triangle
Equilateral Triangle
Parallel Lines
Alternate Angles
Z-shape between parallel lines. The angles inside the Z are equal.
Corresponding Angles
F-shape between parallel lines. The angles at matching positions are equal.
Co-interior Angles
C-shape (or U-shape) between parallel lines. The angles add to 180°.
Transformations
Translation
Shape, size, orientation preserved. No fixed points.
Reflection
Shape, size preserved. Orientation reversed. Mirror line is perpendicular bisector of object-image pairs.
Rotation
Shape, size preserved. Orientation preserved.
Finding Centre of Rotation
Join object to image points, find perpendicular bisectors — they intersect at the centre
Enlargement
k > 1: bigger. 0 < k < 1: smaller. k < 0: inverted.
Scale Factor
Finding Centre of Enlargement
Draw lines through corresponding object-image points — they intersect at the centre
Area Scale Factor
Area of image = k² × area of object
Similar Figures
Similar Triangles
Same shape, different size. All corresponding angles are equal and sides are in the same ratio.
Similar Figures Definition
Corresponding angles equal. Corresponding sides in proportion (same ratio).
Congruence
Congruent Figures Definition
All corresponding sides and angles are equal. One fits exactly on top of the other.
Congruence Tests
SSS: 3 sides equal. SAS: 2 sides + included angle. ASA: 2 angles + included side. RHS: right angle + hypotenuse + side.
Coordinate Geometry
Equation of Line
Slope-Intercept Form
m = gradient, c = y-intercept
Point-Slope Form
When you know gradient and a point
Distance, Midpoint & Gradient
Distance Formula
Midpoint Formula
Gradient Formula
Gradient Rules
Parallel Lines
Parallel lines have equal gradients
Perpendicular Lines
Product of gradients = -1
Regular Polygons
Sum of Interior Angles
n = number of sides
One Interior Angle
Sum of Exterior Angles
Always 360 degrees for any convex polygon
One Exterior Angle
Sets
Sets Formula
Trigonometry
Basic
Pythagoras Theorem
c = hypotenuse; right-angle triangles only
Trigonometric Ratios
Sine
Cosine
Tangent
Advanced
Cosine Rule
For any triangle
Sine Rule
Sine Rule (alt)
Use this form when finding an angle
Circle Theorems
Angle in Semi-circle
The angle in a semi-circle is 90 degrees
Angles in Same Segment
Angles from a common chord in the same segment are equal
Centre vs Circumference
The angle at the centre is twice the angle at the circumference from the same chord
Cyclic Quadrilateral
Opposite angles in a cyclic quadrilateral are supplementary (add to 180 degrees)
Perpendicular from Centre
A line from the centre perpendicular to a chord bisects the chord. Conversely, a line from the centre to the midpoint of a chord meets it at 90°.
Equal Tangents
The two tangents from an external point to a circle are equal in length
Alternate Segment
The angle between the tangent and chord equals the angle in the alternate segment
Tangent-Radius
The angle between the tangent and the radius is 90 degrees
Statistics & Probability
Central Tendency
Mean (ungrouped)
Sum of all values ÷ number of values
Mean (frequency table)
Sum of (frequency × value) ÷ total frequency
Estimated Mean (grouped)
xₘ = class midpoint (midpoint of each class interval)
Median Position
Middle value when data is ordered. Median is also Q₂ (the second quartile).
Mode
Can have more than one mode, or no mode
Measures of Spread
Range
Interquartile Range
Spread of the middle 50% of data
Semi-Interquartile Range
Standard Deviation
Measures how spread out values are from the mean. Higher σ = more spread out (less consistent). Lower σ = closer to mean (more consistent). No calculation required at CSEC.
Q₁ Position
Lower quartile — 25% of data below
Q₃ Position
Upper quartile — 75% of data below
Probability
Probability of Event
0 ≤ P(A) ≤ 1
Complement
Probability of event NOT happening
P(A or B) — Mutually Exclusive
Events cannot happen at the same time
P(A and B) — Independent
Events do not affect each other
Grouped Data
Class Midpoint
Used for estimating mean of grouped data
Class Width
Vectors & Matrices
Matrices
Identity Matrix
Matrix Multiplication
Determinant, Adjoint & Inverse
Determinant
For A = (a b; c d)
Adjoint
Swap a with d, negate b and c
Inverse Matrix
Only exists if det is not 0
Transformation Matrices
Reflection in x-axis
Reflection in y-axis
Reflection in y = x
Reflection in y = -x
Rotation 90 degrees clockwise
Rotation 180 degrees
Rotation 270 degrees clockwise
Translation
x = horizontal, y = vertical movement
Vectors
Triangle Law
Column Vector
Magnitude
Unit Vector
Magnitude = 1
Parallel Vectors
Have a common scalar factor
Collinear Vectors
Parallel + share a common point means same line
Symbols & Formula Sheet
This section shows the symbols and formulae typically provided on the formula sheet in the CSEC Mathematics examination.